ECOLOGY Ecology is the study of the relationship between living organisms and the environment or surrounding. The living organisms are the flora and fauna. Ecological studies can be directly towards a particular organism or a single species, communities or an ecosystem. The word ecology originates from a Greek word ‘oikos’ meaning a home. Two types of ecological studies namely autecology and synecology are commonly carried out. Autecology is the study of the relationship between a single species and the environment in relation to its environment. Synecology is the study of the relationship between communities or different populations of organisms in a given environment i.e. the study of the relationship between all plants and animals in a particular area to the environment. Description of ecological terms 1. Species This is a group of organisms or individuals capable of interbreeding to produce fertile off springs. 2. Population This is a group of organisms or individuals of the same species which occupy a particular area or habitat at the same point and time. The population size of a given species changes with time and changes in environmental factors. 3. Habitat This is a place or physical area where the organism or species lives in an ecosystem. 4. Community This refers to all populations that occupy a particular area at a given time. This implies that all plants, animals and fungi in a particular area form a community therefore a community is a group of plants and animals of different species living together in a certain environment i.e. plant and animal community. 5. Ecological niche Is the role and position any species has within its habitat, and its interactions with living and non-living environment. A niche describes how an organism meets its need for food and shelter, how it survives, and how it reproduces; therefore reduces intra specific competition for resources. An ecological niche describes the functional position and role of an organism within its environment An ecological niche will be comprised of various components, including: 1 | Ecology Endriyo Phillip. The habitat in which the organism lives The activity patterns of the organism (e.g. periods of time during which it is active) The resources it obtains from the environment (e.g. food source, territorial boundaries, etc.) The interactions that occur with other species in the region (e.g. competition / predator-prey relationships) Types of Niches Some species may not be able to occupy their entire niche due to the presence or absence of other species The fundamental niche is the entire set of conditions under which an organism can survive and reproduce (i.e. where it can live) The realised niche is the set of conditions actually used by a given organism after interactions with other species are taken into account (i.e. where it does live) Fundamental versus Realised Niche Niche Differentiation Niche differentiation describes the way by which competing species use the environment differently in order to exist If two species with identical niches compete, two distinct outcomes are possible: Competitive exclusion: One species will use the resources more efficiently and drive the other species to local extinction Resource partitioning: Two species will alter their use of the niche to avoid direct competition, allowing for co-existence 2 | Ecology Endriyo Phillip. Species interaction In nature no species exists in total isolation – all organisms interact with both the abiotic environment and other organisms If two species interact directly within a shared environment, they share a positive association (they co-exist) If interactions within an environment are mutually detrimental to both species, they share a negative association (do not co-exist) Positive Associations 1. Predator-Prey Relationships Predation is a biological interaction whereby one organism (predator) hunts and feeds on another organism (prey) Because the predator relies on the prey as a food source, their population levels are inextricably intertwined 3 | Ecology Endriyo Phillip. If the prey population drops (e.g. due to over-feeding), predator numbers will dwindle as intra-specific competition increases If the prey population rises, predator numbers will increase as a result of the overabundance of a food source Predator-Prey Relationships (Arctic Fox vs Snowshoe Hare) 2. Symbiotic Relationships Symbiosis describes the close and persistent (long-term) interaction between two species Symbiotic relationships can be obligate (required for survival) or facultative (advantageous without being strictly necessary) Symbiotic relationships can be beneficial to either one or both organisms in the partnership: o Mutualism – Both species benefit from the interaction (anemone protects clownfish, clownfish provides fecal matter for food) o Commensalism – One species benefits, the other is unaffected (barnacles are transported to plankton-rich waters by whales) o Parasitism – One species benefits to the detriment of the other species (ticks and fleas feed on the blood of their canine host) Types of Symbiotic Relationships 4 | Ecology Endriyo Phillip. Negative Associations 1. Competition Competition describes the interaction between two organisms whereby the fitness of one is lowered by the presence of the other Competition can be intraspecific (between members of same species) or interspecific (between members of different species) Limited supplies of resources (e.g. food, water, territory) usually triggers one of two types of responses: o Competitive exclusion – One species uses the resources more efficiently, driving the other species to local extinction o Resource partitioning – Both species alter their use of the environment to divide the resources between them Competitive Exclusion vs Resource Partitioning 5 | Ecology Endriyo Phillip. 6. Ecosystem An ecosystem is an ecological unit consisting of a community of living organisms and its physical environment. Such a unit will consist of plants, animals and microorganisms as well as non-living components like water, soil, air and light. Or An ecosystem refers to the interaction between living organisms and non-living components of the environment or habitat to form a self-supporting system e.g. in a pond or aquatic ecosystem. It consists of phytoplanktons, saprophytes, zooplanktons as the biotic component (living) whose interaction with dead decaying organic matter or recycle for self-sustainability. 7. Biosphere This is part of the earth inhabited by living organisms. The biosphere comprises of terrestrial and aquatic ecosystem. The biosphere is subdivided into bio-geographical regions each inhabited by species of plants and animals that are favored by unique conditions of such areas. Bio-geographical regions are also subdivided into particular areas called biomass/biomes’. Biome refers to a large recognizable community formed as a result of interaction between regional climates with regional biomes e.g. tropical rain forests, tropical savanna, desert, temperate region. The biome is divided into zones e.g. forests biome forms the ground level and canopy. The lake forms the limnetic zone, littoral zone, benthos and profundal zone, each zone supporting a particular type of organisms. Terrestrial biomes The two most important environment variables for life on land are rainfalls and temperature. Basing on these facts the terrestrial biome is further subdivided into; (a) Tropical rain forests These are formed whenever, it’s hot [24-280C] and wet throughout the year. The vegetation of tropical rain forest has a distinctive structure, with very tall tree which project above the rest of the forest canopy, beneath these emergent is a second layer of large tree which, together with emergent make up a continuous canopy. A third tree layer is made up of smaller tree which complete their cycle without ever reaching the canopy. Still nearer the ground are young trees, palms vine and herbs. By the time sunlight reaches the forest floor, most of it has already been intercepted so that it’s dark with relatively sparse vegetation. Many organisms live in the canopy. The soils of tropic rain forest are generally poor probably because decomposition occurs very quickly due to high temperature and any other available nutrient are rapidly taken up by plant or leached due to high rainfall. (b) Temperate deciduous forest. The north temperature zone lies between tropical of Cancer and artic cycle. The southern temperature zone lies between tropical of Capricorn and Antarctic cycle. 6 | Ecology Endriyo Phillip. In these two zones is where the temperature deciduous forest likely to be found, dominated by oak, hazel, beech The major problem in this biome is that half of the year is winter when the temperature is too low for life. To survive in this condition, organisms have developed the following adaptations. a) Loss of leaves by the trees in winter to reduce on water loss by guttation. b) small animals hibernate c) birds migrate to tropics during winter d) some animals have accumulated a lot of fast to prevent heat loss in winter e) some have short life cycle in of 3-6 months and survive in a dormant stage in winter (c) Desert For example, Sahara Desert in Northern Africa is characteristic by scarce irregular rainfall and sandy soil. To survive in the desert organism have developed the following adaptations. i. Small plants and animals have got very short life cycle; For instance, plants may germinate, mature, flower in a few weeks following occasioned rainfall, and then survive in form of seeds during the long dry spell. ii. To overcome shortage of water, the camel; use metabolic water and its body is very resistant to dehydration; certain frogs can survive for years without water by burying themselves deep into the sand. When it rains they dig themselves out, mate, and lay their eggs in shallow puddles. Here the tadpole grows very quickly, metamorphosing into adults before the puddle disappears. iii. The camel has got broad feet not to sink in the sand. iv. Some plant such cactus store water in their fleshly stems. (d) Tundra It occurs in northern Canada and Asia. It is characterized by long winter and very short growing season. For this reason, it contains no tree neither small mammals but plants with very short life cycle and bigger animals with a lot of fats deposits e.g., Reindeer Aquatic biomes 7 | Ecology Endriyo Phillip. Most important variable that affect organism which live in water are Salinity nutrient availability depth of water how permanent is the water body tide strength Salinity Aquatic organisms have got a problem of osmoregulation at different salinities. Consequently, organisms are only adapted differently to this problem in freshwater and marine water. And those that can survive in freshwater cannot survive in marine water and vice versa Nutrient availability The most important nutrient in water are the nitrates and phosphate. Lake with low phosphate and nitrate (oligotrophic) contain more species than lakes with high levels of nitrates and phosphates (eutrophic lakes) In eutrophic lakes, the high levels of nitrates and phosphate promote high growth rates of algae and other photosynthetic organisms. This, in turn, supports a large number of aerobic bacteria that decompose the dead photosynthetic organisms. However, the aerobic bacteria take up more oxygen from water thus oxygen concentration may fall below that, can support the life of big organisms. Depth of water Shallow water may not be able to support big animals like whales. Small ponds may dry up which has a profound effect on the organism that can only survive in water. Tidal strength Distribution of organism on the shores is affected tide strength; very strong tides, it prevents the growth of plant near the lake and big animals in water. Ecotones are boundary zone between two biomes or ecosystem where one merges into the other. ECOSYSTEM It is natural unit of environment composed of living (biotic) and non-living (abiotic) components whose interactions lead to a self-sustaining system. (i) Water (aquatic) ecosystems may be fresh water bodies (e.g. lakes, ponds, rivers) or marine water bodies (e.g. sea, ocean). Organisms in water may be of large size (nektons) e.g. fish, whales, turtles or very tiny (planktons) e.g. phytoplanktons and zooplanktons. (ii) Land (terrestrial) ecosystems include forests, deserts, savanna, etc 8 | Ecology Endriyo Phillip. THE MAJOR COMPONENTS OF AN ECOSYSTEM a) Abiotic / non-living things: these are physical and chemical factors that influence living organisms on land (terrestrial) ecosystems and in water (aquatic). Examples of abiotic components: climatic factors, which include; Temperature, Light, Wind, Humidity, rainfall etc soil (edaphic) factors e.g. Soil pH, Soil air, Inorganic particles, Soil water , Organic matter (dead organic matter and living organisms), Soil temperature etc Topography Other physical factors e.g fire and wave action etc Question. How do abiotic factors affect the distribution and abundance of organisms? (i) Climatic factors Temperature a. Affects physiological processes (respiration, photosynthesis, and growth etc) in organisms which in turn influence their distribution. b. Ultimate heating and cooling of rocks cause air to break and crack into small pieces and finally form soil. c. These changes in turn may result into migration of organisms’ e.g birds to avoid over heating or freezing. d. Low temperatures inactivate enzymes while excessive temperatures denature enzymes. e. High temperature increase transpiration and sweating f. Low temperatures break dormancy of some plants. g. Temperatures stimulate flowering in some plants e.g cabbage (vernalisation) h. Exposure to low temperature (stratification) stimulate germination in some seeds after imbibitions. Organisms have evolved to have structural, physiological and behavioral adaptations to maintain their temperature in an optimum range. (i) Adaptations of animals for life in hot and dry deserts. Structural adaptations, a) Large body extremities e.g ear lobes; to increase surface area over which heat is lost. b) Small sized; to increase the surface area to volume ratio, for heat loss c) Some animals like the camel, have long skinny non fatty legs to increase heat loss during locomotion d) Little or no fur to reduce on insulation, and increase amount of heat lost e) Thin subcutaneous fat layer under the skin to increase heat loss from the body f) Have tissues tolerant to extreme temperature changes, maintaining the body’s main functions Physiological adaptations Enzymes work under a high optimum temperature range to maintain metabolism during day and night. Behavioral adaptations 9 | Ecology Endriyo Phillip. Most are nocturnal, i.e. most active at night, when temperatures are relatively low Aestivation(seasonal response by animals to drought or excessive heat during which they become dormant, and the metabolic rate followed by body temperature fall to the minimum required for maintaining the vital activities of the body) ; allows them to survive extremes of hot temperatures e E.g. African lungfish burrows into mud till the dry season ends, earthworms , garden snails , desert rats, termites also aestivate Movement with some body parts raised to minimize direct contact with hot grounds e.g desert snakes Salivation of the neck and legs ; increasing heat loss by evaporation e.g in tortoise (ii).adaptations of animals for life in cold environments Structural adaptations Thick layer of fat under the skin; to increase on insulation by avoiding heat loss Small body extremities to reduce the surface area over which heat is lost Large sized; thus small surface area to volume ratio; reducing amount of heat lost to the surrounding Thick fur; to increase on insulation Tissues tolerant to extreme changes in temperature; maintaining their normal functions in the body Physiological adaptations Enzymes work under a high optimum temperature range to maintain metabolism during day and night Behavioral adaptations Hibernation (is seasonal response by animals to cold temperature during which they become dormant, body temperature and metabolic rate fall to the minimum required for maintaining the vital activities of the body) The animals, said to be in ‘deep sleep’ ably reduce energy needs to survive the winter when food is scarce allowing them survive extreme cold conditions e.g in polar bears. Gathering in groups to warm themselves e.g. penguins Rain fall; Amount of rainfall in a given area determines the abundance, distribution and types of plants in the area Ecological significances of water Habitat for many aquatic organisms e.g. frogs, fish etc. Raw material for photosynthesis; main energy source for body processes of other organisms High thermal capacities; acting as cooling agent for terrestrial organisms e.g plants during transpiration, some animals during sweating. Agent for fruit, seed, spore, larva and gamete dispersal Condition for germination Highly transparent; therefore allowing light to reach aquatic organisms, for photosynthesis; and aquatic predators to locate their prey 10 | Ecology Endriyo Phillip. Important factor in decay and decomposition; therefore increases in recycling of nutrients in an ecosystem. Humidity; Amount of water in the atmosphere; Affects the rate at which water evaporates from organisms i.e. Low humidity results to increasing evaporation while high humidity causes low rate of evaporation; through stomata of leaves in plants. Accordingly, organisms within areas of low humidity are adapted to avoid excessive loss of water by; Having reduced number of sweat glands e.g in kangaroo rat Presence of leaf spines in cactus plants; to reduce surface area over which water is lost through transpiration. Controls other activities of animals like feeding, hunting, and movements e.g earth worms experience a larger ecological niche when the environment is humid. Controls opening and closure of stomata; therefore affecting rate of photosynthesis and transpiration. Wind / air currents; It influences the following, Dispersal or migration of flying mammals, winged insects; thus reducing the level of competition. Pollination Dispersal of seeds and spores; increasing the spread of non-motile organisms’ e.g fungi and some bacteria. Takes part in rain formation Current and wave formation in seas and lakes enables distribution of mineral salts. Increase transpiration; thus promoting water and mineral salt uptake from the soil by plant roots Increases evaporation and reduces sweating. Causes physical damage to vegetation and soils e.g soil erosion. Increases dissolution of oxygen in aquatic bodies; thereby increasing aerobic activities of organisms. Light (intensity, quality, and duration) Influences many physiological activities of organisms’ i.e. It is a source of energy for photolysis (breakdown of water during photosynthesis.). Absence of light causes etiolation (elongation of shoot inter nodes). Induces flowering in long-day plants e.g. barley, but inhibits flowering in short day plants. Phototropism, by redistributing auxins on the darker sides of shoots and roots, with cells on darker side elongating more than those on illuminated side. Germination ; some seeds are positively photoblastic; germination only in presence of light while other do not require light to germinate.(are negatively photoblastic) 11 | Ecology Endriyo Phillip. Stomatal opening and closure; with most plant species opening their stomata during day (when there is light) and closing during night (in absence of light/darkness). Predation ; (hunting and killing of prey by predators require certain levels of illumination and visibility) Courtship; with some animals preferring light so as to carry out courtship while others prefer darkness Light breaks dormancy of seeds. Stimulates synthesis of vitamin D in mammals; where lipids(sterols) in the dermis are converted to vitamin D by uv light It enables the mechanisms photoreceptions in eyes Absence of light results in failure of chlorophyll formation in plants i.e. plant remains yellow, and leaves fail to expand. Photoperiod affects migratory and reproductive behaviour in various animals e.g. sunlight polarised by water acts as a compass for migration of salmon fish. Necessary for the germination of certain seeds e.g. lettuce (ii) Topography.; Refers to the nature of the landscape, which includes features like mountains, valleys, lakes etc. High altitude is associated with, low atmospheric pressure; low average temperatures, increased wind speed; decreased partial pressures of oxygen, thus few organisms live permanently here. Slope reduces water logging and there is a lot of soil erosion preventing proper plant establishment especially at steep slopes At low altitudes, average temperatures are high, high atmospheric pressure, partial pressures of oxygen are high, and in some places there is water logging. Assignment. Describe different adaptations of organisms that live in high altitude. (iii). Edaphic (soil) factors, Soil formed by chemical and physical weathering of rocks, possess both living components(living organisms like bacteria, fungi, algae and animals like protozoans, nematodes earthworms, insects, burrowing mammals) and non-living components (particles of various sizes) Also present are; mineral salts, water, organic matter, and grasses. Soil Ph. Influences physical properties of soil and availability of certain minerals to plants, thus affecting their distribution in soil; i.e. tea and coffee plants thrive well in acidic soils Affects activity of decomposers e.g in acidic medium, the rate of decomposition is reduced, subsequently recycling of matter in an ecosystem reduced. Water content; Varies markedly in any well-defined soil, Any finely drained soil holding much water as possible is said to be at full capacity 12 | Ecology Endriyo Phillip. Addition of more water which cannot be drained away leads to water logging; and anaerobic conditions, affecting mineral ion uptake by active transport, subsequently affecting osmotic uptake of water, due to decreased osmotic potential gradient, causing plants to dry out. Plants like rice, marshes, and sedges have developed air spaces among root tissues, allowing some diffusion of oxygen from aerial parts to help supply the roots. Biotic content; Microorganisms like bacteria and fungi carry out decomposition of dead organic material, therefore recycling nutrients back to the soil. Burrowing organisms e.g. earthworms improve drainage and aeration by forming air spaces in the soil. Earthworms also improve soil fertility by mixing of soil, as they bring leached minerals from lower layers within reach of plant roots. They also improve humus content, by pulling leaves into their burrows Also press soil through their bodies making its texture fine. Air content; Spaces between soil particles is filled with air from which plant roots obtain oxygen by diffusion for aerobic respiration, Also essential for aerobic respiration by micro-organisms in the soil that decompose the humus. (iv) Salinity; Is the measure of salt concentration in aquatic bodies and soil water. Determines the osmotic pressure of water; therefore the organisms have developed structural, behavioral, and physiological adaptations to osmoregulate in the respective salt concentration, ( read adaptations of fresh water fish, marine water fish and migratory fish to their osmoregulatory problems). Mineral salts in water affect the distribution of plant species, which in turn affects the animals that depend on plants for food. Plants growing in soils deficient of certain salts, e.g insectivorous plants in nitrogen deficient soils, obtain nitrogen feeding on insects. Significances of mineral salts to plants Mineral salts together with other solutes determine the osmotic pressure of cells and body fluids Determinants in anion and cation balance in cells, e.g Na+ and Cl-, involved in transmission of nerve impulses Constituents of certain pigments like haemoglobin, and chlorophyll containing iron and magnesium respectively. Metabolic activators; some ions activate enzymes, e.g chloride ions activate salivary amylase, magnesium activate enzymes in phosphate metabolism, and phosphorus as phosphate is required in activation of sugars during Glycolysis in tissue respiration. Mineral salts like potassium are involved in formation of cell membrane and opening of stomata; Development of stem and root e.g. calcium pectate in formation of plant cell wall etc. 13 | Ecology Endriyo Phillip. (v) Fire; Types of fire Natural fires; are set up by natural causes like lightening, volcanic eruptions etc. Artificial fires; are set up by man either intentionally or carelessly Wild fires; burn in the direction of wind Early fires; set up at beginning of dry season Prescribed fires; under ecological management where prevention measures are taken when setting up the fire. Properties of fire Fire intensity; is the heat content of the fire, Depends on environmental factors such as wind, temperature as well as the amount and type of vegetation. Fire duration; is the time taken by the fire to destroy a given area. Fire severity; is measured in terms of major vegetation destroyed by the fire. Ecological effects of fire Positive effects Removes old leaves and stimulates trees and grasses to produce new buds. Breaks dormancy (seed dormancy), incase seed coats are hard and impermeable. Causes release of mineral nutrients in form ash; on burning organic matter, releasing nitrate and phosphate compounds into soil, and subsequently improving on soil fertility. Improves on visibility of organisms such as predators, prey, mates allowing them easily carry out their activities. Improves on food productivity in terms of quality, quantity and productivity, because after burning new species with high protein content grows. Destroys pests Controls undesirable plant species and weeds Negative effects Increase soil erosion; leading soil infertility Kills slow moving animals e.g snails, earthworms Destruction of habitat for most of the animal species may leading migration or extinction Increases fire resistant species. Reduction in population density and biodiversity. Destroys food for animals like herbivores which may lead to starvation and eventually death. Air pollution by products such as carbon monoxide and carbon dioxide, increasing on global warming. Adaptations of plants to fire Thick succulent shoot system to reduce the effects of heat. Grasses grow in tussocks to protect the young growing buds. Some tree stems are succulent i.e. store water in parenchyma cells to reduce on the effects of fire heat. 14 | Ecology Endriyo Phillip. Many plants are annuals to avoid fire severity in form of seeds, which may be underground. Some trees have heat resistant tissues. (b). Biotic / living components: these are the plants, animals and decomposers. Functions of Ecosystem The functions of the ecosystem are as follows: 1. It regulates the essential ecological processes, supports life systems and renders stability. 2. It is also responsible for the cycling of nutrients between biotic and abiotic components. 3. It maintains a balance among the various trophic levels in the ecosystem. 4. It cycles the minerals through the biosphere. 5. The abiotic components help in the synthesis of organic components that involve the exchange of energy. So the functional units of an ecosystem or functional components that work together in an ecosystem are: Productivity – It refers to the rate of biomass production. Energy flow – It is the sequential process through which energy flows from one trophic level to another. The energy captured from the sun flows from producers to consumers and then to decomposers and finally back to the environment. Decomposition – It is the process of breakdown of dead organic material. The top-soil is the major site for decomposition. Nutrient cycling – In an ecosystem nutrients are consumed and recycled back in various forms for the utilisation by various organisms. Types of Ecosystem An ecosystem can be as small as an oasis in a desert, or as big as an ocean, spanning thousands of miles. There are two types of ecosystem: Terrestrial Ecosystem Aquatic Ecosystem Terrestrial Ecosystem Terrestrial ecosystems are exclusively land-based ecosystems. There are different types of terrestrial ecosystems distributed around various geological zones. They are as follows: 1. Forest Ecosystem 2. Grassland Ecosystem 3. Tundra Ecosystem 15 | Ecology Endriyo Phillip. 4. Desert Ecosystem Aquatic ecosystems are ecosystems present in a body of water. These can be further divided into two types, namely: 1. Freshwater Ecosystem 2. Marine Ecosystem The freshwater ecosystem is an aquatic ecosystem that includes lakes, ponds, rivers, streams and wetlands. These have no salt content in contrast with the marine ecosystem. Freshwater community consists of an array of organisms depending on the physiochemical and biological characteristics of the freshwater environment. Freshwater habitats are divided into two major categories, lotic (lotus = washed, or running water), and lentic (lenis = calm, or standing water) habitats. Lotic habitats are those existing in relatively fast running streams, springs, rivers and brooks. Lentic habitats are represented by the lakes, ponds, and swamps. The above classification of the freshwater environments is based on two conditions: currents and the ratio of the depth to surface area. Since lakes and ponds often contain currents or at least wave action and since streams often harbor quiet pools or calm backwaters, the difference between lotic and lentic waters is not very precise. However, temperature, light, currents, amount of respiratory gases, and concentration of biogenic salts are important limiting factors influencing the organisms of all freshwater habitats. Lentic Community: Lentic waters are generally divided into three zones or sub-habitats: littoral, limnetic, and pro-fundal. A small pond may consist entirely of littoral zone. However, a deep lake with an abruptly sloping basin may possess an extremely reduced littoral zone. Lake Zonation: (a) Littoral zone: The littoral zone adjoins the shore (and is thus the home of rooted plants) and extends down to a point called the light compensation level, or the depth at which the rate of photosynthesis equals the rate of respiration. Within the littoral zone producers are of two main types: rooted or benthic plants, and phytoplankton (plant plankton) or floating green plants, which are mostly algae. The littoral zone is the home of greater variety of consumers than are the other zones. The zooplankton (animal plankton) of the littoral zone is rather characteristic and differs from that of the limnetic zone in preponderance of heavier, less buoyant crustaceans which often cling to plants or rest on the bottom when not actively moving their appendages. Important groups of littoral 16 | Ecology Endriyo Phillip. zooplankton are large, weak-swimming species of Daphia and Simocephalus, some species of copepods, many families of ostracods and some rotifers. The nekton of littoral zone is often rich in species and numbers. Adult and larval diving beetles and various adult Hemipetra are conspicuous. Various Diptera larvae and pupae remain suspended in the water, often near the surface. Pond fish, frogs, turtles, and water snakes are almost exclusively the members of the littoral zone community. Tadpoles of the frogs are important primary consumers, feeding on algae and other plant material. Periphyton of the littoral zone exhibits a zonation paralleling that of the rooted plants, but many species occur almost throughout the littoral zone. Among the periphyton forms, for example, pond snails, damselfly nymphs and climbing dragonfly nymphs, rotifers, flatworms, bryozoa, hydra, and midge larvae rest on, or are attached to stems and leaves of the plants. Another group containing both primary and secondary consumers may be found resting or moving on the bottom or beneath silt or plant debris— for example, sprawling odonata nymphs (which have flattened rather than cylindrical bodies), crayfish, isopods, and certain mayfly nymphs. Descending more deeply into the bottom mud are burrowing odonata and ephemeroptera, clams, true worms, snails, chironomids (midges), and other diptera larvae. (b) Limnetic Zone: The limnetic zone includes all the waters beyond the littoral zone and down to the light compensation level. The limnetic zone derives its oxygen content from the photosynthetic activity of phytoplankton and from the atmosphere immediately over the lake’s surface. The atmospheric source of oxygen becomes significant primarily when there is some surface disturbance of water caused by wind action or human activity. The community of the limnetic zone is composed only of plankton, nekton, and sometimes neuston (organisms resting or swimming on the surface). Phytoplankton producers consist of diatoms, green algae, blue- green algae, and algae- like green flagellates, chiefly the dinoflagellates. The limnetic zooplankton consists of few species but the number of individuals may be large. Copepods, cladocerans, and rotifers are generally of first importance; but their species are largely different from those found in the littoral zone. The limnetic nekton consists almost entirely offish. In ponds, the fish of the limnetic zone are the same as those of the littoral zone, but in large bodies of water a few species may be restricted to the limnetic zone. (C) Profundal Zone: The bottom and deep water area of a lake, which is beyond the depth of effective light penetration is called the pro-fundal zone. In north-temperate latitudes, where winters are long and severe, this zone has the warmest water (4°C) in the lake in winter and coldest water in summer. The major community consists of bacteria and fungi and three groups of animal consumers: 17 | Ecology Endriyo Phillip. (a) Blood worms, or haemoglobin containing chironomid larvae and annelids, (b) Small clams, and (c) Phantom larvae, or Chaoborus (corethra). The first two groups are benthic forms, the last are plankton that regularly move up into the limnetic zone at night and down to the bottom during the day. All the animals of the pro-fundal zone are adapted to withstand periods of low oxygen concentration, whereas many bacteria are anaerobic. Large numbers of bacteria in the bottom ooze constantly bring about decomposition of the organic matter (plant debris, animal remains, and excreta) that accumulates on the bottom. Eventually the organic sediments are mineralized and nitrogen and phosphorus are put back into circulation in the form of soluble salts. In this way, the pro-fundal zone provides rejuvenated nutrients, which are carried by currents and swimming animals to other zones. Ecological classification of fresh water organisms Organisms in water can be classified depending on their life form which is based on their mode of life. The following terms are used: 1. Neuston: These are organisms resting or swimming on the surface of water. Such organisms may be supported by the surface film or cling to the surface film from beneath or swim in the upper waters. Examples include pond skaters, air breathing diving beetles, water boat men, floating plants like duck weed, bladder work, etc. 2. Plankton (floating): This is a mass of floating small plants (phytoplankton) and animals (zooplankton) whose movements and distribution are more or less dependent on currents. Their powers of locomotion are restricted to small vertical movements or to catching prey. Examples include arolia, Pistoia, water burg, tadpole, etc. 3. Nekton: 18 | Ecology Endriyo Phillip. These are free-swimming organisms that can swim against water currents. Some of them are small e.g. swimming insects while others are large e.g. bony fish, amphibians, etc. 4. Benthos: These are organisms attached or resting on the bottom or living in the bottom sediments. Most of them feed on fresh water organisms in ponds and lakes. They may also be classified depending on the sub i) Littoral zone: This is the shallow-water region with light penetration to the bottom. Such a zone is typically occupied by plants in natural ponds and lakes. ii) Limnetic zone: This is the open water zone to the depth of effective light penetration. The community in this zone is composed of plankton, nekton and sometimes Neuston. In shallow ponds, this zone is absent. The total illuminated depth including the littoral and limnetic zone is referred to as the euphotic zone. iii) Profundal: This is the bottom and deep water area which is beyond the depth of effective light penetration. This zone is often absent in ponds. Factors affecting productivity of the lake Temperature Nutrient availability Salinity Water current Pollution Warm temperature provide optimum medium for aquatic organisms distribution as well as enzymes involved in photosynthesis. Cool temperature of bottom water inactivate enzyme and affect distribution of phytoplankton thus reduced productivity. Availability of nutrients in water due to decomposition of organic matter like sewage, dead organisms and fertilizers washed off from farm and water would lead to algal blooming or eutrophication of phytoplanktons. This would instead increase productivity since phytoplanktons are many. Man’s activities that harm the environment. With the recent increase in the human population, there has been over exploitation of natural resources. The marine biome Marine regions cover about three-fourths of the Earth's surface and include oceans, coral reefs, and estuaries. Marine algae supply much of the world's oxygen supply and take in a huge amount of atmospheric carbon dioxide. The evaporation of the seawater provides rainwater for the land. Oceans The largest of all the ecosystems, oceans are very large bodies of water that dominate the Earth's surface. Like ponds and lakes, the ocean regions are separated into separate zones: intertidal, pelagic, abyssal, and benthic. All four zones have a great diversity of species. Some say that the ocean contains the 19 | Ecology Endriyo Phillip. richest diversity of species even though it contains fewer species than there are on land. The intertidal zone is where the ocean meets the land — sometimes it is submerged and at other times exposed, as waves and tides come in and out. Because of this, the communities are constantly changing. On rocky coasts, the zone is stratified vertically. Where only the highest tides reach, there are only a few species of algae and mollusks. In those areas usually submerged during high tide, there is a more diverse array of algae and small animals, such as herbivorous snails, crabs, sea stars, and small fishes. At the bottom of the intertidal zone, which is only exposed during the lowest tides, many invertebrates, fishes, and seaweed can be found. The intertidal zone on sandier shores is not as stratified as in the rocky areas. Waves keep mud and sand constantly moving, thus very few algae and plants can establish themselves — the fauna include worms, clams, predatory crustaceans, crabs, and shorebirds. The pelagic zone includes those waters further from the land, basically the open ocean. The pelagic zone is generally cold though it is hard to give a general temperature range since, just like ponds and lakes, there is thermal stratification with a constant mixing of warm and cold ocean currents. The flora in the pelagic zone include surface seaweeds. The fauna include many species of fish and some mammals, such as whales and dolphins. Many feed on the abundant plankton. The benthic zone is the area below the pelagic zone, but does not include the very deepest parts of the ocean (see abyssal zone below). The bottom of the zone consists of sand, slit, and/or dead organisms. Here temperature decreases as depth increases toward the abyssal zone, since light cannot penetrate through the deeper water. Flora are represented primarily by seaweed while the fauna, since it is very nutrient-rich, include all sorts of bacteria, fungi, sponges, sea anemones, worms, sea stars, and fishes. The deep ocean is the abyssal zone. The water in this region is very cold (around 3° C), highly pressured, high in oxygen content, but low in nutritional content. The abyssal zone supports many species of invertebrates and fishes. Mid-ocean ridges (spreading zones between tectonic plates), often with hydrothermal vents, are found in the abyssal zones along the ocean floors. Chemosynthetic bacteria thrive near these vents because of the large amounts of hydrogen sulfide and other minerals they emit. These bacteria are thus the start of the food web as they are eaten by invertebrates and fishes. Coral reefs Coral reefs are widely distributed in warm shallow waters. They can be found as barriers along continents (e.g., the Great Barrier Reef off Australia), fringing islands, and atolls. Naturally, the dominant organisms in coral reefs are corals. Corals are interesting since they consist of both algae (zooanthellae) and tissues of animal polyp. Since reef waters tend to be nutritionally poor, corals obtain nutrients through the algae via photosynthesis and also by extending tentacles to obtain plankton from the water. Besides corals, the fauna include several species of microorganisms, invertebrates, fishes, sea urchins, octopuses, and sea stars. Estuaries 20 | Ecology Endriyo Phillip. Estuaries are areas where freshwater streams or rivers merge with the ocean. This mixing of waters with such different salt concentrations creates a very interesting and unique ecosystem. Microflora like algae, and macroflora, such as seaweeds, marsh grasses, and mangrove trees (only in the tropics), can be found here. Estuaries support a diverse fauna, including a variety of worms, oysters, crabs, and waterfowl. THE MAJOR BIOTIC / LIVING COMPONENTS OF ECOSYSTEMS 1. Producers, Are autotrophs capable of synthesizing complex organic food materials from simple inorganic food raw materials e.g carbon dioxide and water. Examples include; large green terrestrial plants e.g trees, shrubs, grass. For aquatic ecosystem, the producers are microscopic algae, blue green bacteria. Others are flagellates like euglena, chlamydomonas etc. They are collectively called Phytoplanktons (microscopic marine producers) NB; Some producers use chemical energy derived from breakdown of chemical compounds like sulphur to convert carbon dioxide and water into high energy compounds like carbohydrates e.g sulphur bacteria i.e. they are chemosynthetic. 2. Consumer: Are organisms that get energy and nutrients by feeding on other organisms or their remains. They are classified as; (i) Primary consumers (Herbivore): A consumer that eats plants. E.g. insects, birds, most mammals (grazers), In aquatic ecosystem, they include; water fleas, fish, crabs, mollusks, and protozoans, collectively known as zooplanktons (microscopic marine consumers). (ii) Secondary consumers (Carnivore): A consumer that eats other animals. E.g. birds of prey like eagle, kites, kingfishers; and lions, cheetahs, tigers, hyenas, snakes, big fish. (iii) Tertiary consumers: These feed on both primary and secondary consumers. Can be predators that hunt and kill others for food or scavengers (animals that feed on dead organisms but do not kill them. E.g. vultures, hyenas, marabou stocks etc. (iv) Omnivore: A consumer that eats both plants and animals .e.g. man, pigs, etc. 3. Decomposer: 21 | Ecology Endriyo Phillip. An organism that feeds on dead organic matter. Classified into; (i) Detrivores/ macro decomposers; An animal that eats detritus (dead and waste matter not eaten by consumers). E.g earth worms, rag worms, mites, maggots, wood lice, termites etc. (ii) Saprophyte: A microbe (bacterium or fungus) that lives on detritus. Importance of decomposition: (1) It enables dead bodies to be disposed off which, if left would accumulate everywhere. (2) Recycles nutrients to be used by other organisms e.g. Mineral salts are released from dead bodies into soil for plant growth. (3) Unlocks trapped energy in the body of dead organisms. ENERGY FLOW THROUGH AN ECOSYSTEM The sun is the primary source of energy in the ecosystem. Light energy is trapped by photosynthetic organisms (green plants, algae, and some bacteria); converted into chemical energy by during photosynthesis. It is then transferred from one feeding level to another through feeding relationships like food chains or food webs. Most of the energy from sun getting the earth’s surface is reflected by vegetation, soil, and water or absorbed and radiated to atmosphere; leaving only between 5%-10% for the producers to make use of. Along the food chain, only a small proportion of the available energy is transferred from one feeding level to another; much energy is lost as heat during sweating and evaporation, excretion , respiration, egestion, and some remains locked up in indigestible parts of the plant like cellulose, or bones, hooves, hair, skin etc. of animals. The number of organisms decrease at each successive feeding level because of the great energy losses, so the energy left in organisms is little to support large numbers of top consumers; limiting the length of food chain( not exceeding five trophic levels( feeding level in a food chain containing given amount of energy). All green plants, and some bacteria, are photoautotrophic – they use sunlight as a source of energy This makes light the initial source of energy for almost all communities In a few ecosystems the producers are chemoautotrophic bacteria, which use energy derived from chemical processes Light energy is absorbed by photoautotrophs and is converted into chemical energy via photosynthesis This light energy is used to make organic compounds (e.g. sugars) from inorganic sources (e.g. CO2) Heterotrophs ingest these organic compounds in order to derive their chemical energy (ATP) When organic compounds are broken down via cell respiration, ATP is produced to fuel metabolic processes Overview of Photosynthesis 22 | Ecology Endriyo Phillip. Energy flow in an ecosystem Energy enters most ecosystems as sunlight, where it is converted into chemical energy by producers (via photosynthesis) This chemical energy is stored in carbon compounds (organic molecules) and is transferred to heterotrophs via feeding Trophic Levels The position an organism occupies within a feeding sequence is known as a trophic level Producers always occupy the first trophic level in a feeding sequence Primary consumers feed on producers and hence occupy the second trophic level Further consumers (e.g. secondary, tertiary, etc.) may occupy subsequent trophic levels The trophic levels in a community are: Food Chains A food chain shows the linear feeding relationships between species in a community Arrows represent the transfer of energy and matter as one organism is eaten by another (arrows point in direction of energy flow) The first organism in a food chain is always a producer, followed by consumers (primary, secondary, tertiary, etc.) 23 | Ecology Endriyo Phillip. Examples of Food Chains in Different Habitats Grassland food chain Marine food chain Pond food chain Food webs A food web is a diagram that shows how food chains are linked together into more complex feeding relationships A food web is more representative of actual feeding pathways within an ecosystem because: Organisms can have more than one food source Organisms can have more than one predator This means that, unlike a food chain, organisms in a food web can occupy more than one trophic level Hint: When constructing food webs, position organisms at their highest trophic level (keeps all arrows pointing in same direction) Example of a Food Web (Pond Ecosystem) 24 | Ecology Endriyo Phillip. Ecological pyramids Ecological pyramids show the relative amounts of a specific component at the different trophic levels of an ecosystem. The three main types of ecological pyramids measure species numbers, biomass and energy Pyramid of Numbers A pyramid of numbers shows the relative number of organisms at each stage of a food chain These are usually shaped like pyramids, as higher trophic levels cannot be sustained if there are more predators than prey However, the shape may be distorted if a food source is disproportionately large in size / biomass compared to the feeder. For example, a large number of caterpillars may feed on a single oak tree and many fleas may feed off a single dog host Pyramid of Biomass A pyramid of biomass shows the total mass of organisms at each stage of a food chain These pyramids are almost always upright in shape, as biomass diminishes along food chains as CO2 and waste is released An exception to this rule is found in marine ecosystems, where zooplankton have a large total biomass than phytoplankton. This is because phytoplankton replace their biomass at such a rapid rate and so can support a larger biomass of zooplankton Pyramid of Energy A pyramid of energy shows the amount of energy trapped per area in a given time period at each stage of a food chain These pyramids are always upright in shape, as energy is lost along food chains (either used in respiration or lost as heat) Each level in the pyramid will be roughly one tenth the size of the preceding level as energy transformations are 10% efficient 25 | Ecology Endriyo Phillip. Examples of Ecological Pyramids for a Specific Food Chain Energy loss Energy stored in organic molecules (e.g. sugars and lipids) can be released by cell respiration to produce ATP This ATP is then used to fuel metabolic reactions required for growth and homeostasis A by-product of these chemical reactions is heat (thermal energy), which is released from the organism Not all energy stored in organic molecules is transferred via heterotrophic feeding – some of the chemical energy is lost by: Being excreted as part of the organism’s faeces Remaining unconsumed as the uneaten portions of the food Energy Transformations in Living Organisms The chemical energy produced by an organism can be converted into a number of forms, including: Kinetic energy (e.g. during muscular contractions) Electrical energy (e.g. during the transmission of nerve impulses) Light energy (e.g. producing bioluminescence) All of these reactions are exothermic and release thermal energy (heat) as a byproduct Living organisms cannot turn this heat into other forms of usable energy This heat energy is released from the organism and is lost from the ecosystem (unlike nutrients, which are recycled) 26 | Ecology Endriyo Phillip. Hence ecosystems require a continuous influx of energy from an external source (such as the sun) Energy Transformations in Ecosystems Energy efficiency When energy transformations take place in living organisms the process is never 100% efficient Most of the energy is lost to the organism – either used in respiration, released as heat, excreted in Feaces or unconsumed Typically energy transformations are ~10% efficient, with about 90% of available energy lost between trophic levels The amount of energy transferred depends on how efficiently organisms can capture and use energy (usually between 5 – 20%) As energy is lost between trophic levels, higher trophic levels store less energy as carbon compounds and so have less biomass Biomass is the total mass of a group of organisms – consisting of the carbon compounds contained in the cells and tissues Because carbon compounds store energy, scientists can measure the amount of energy added to organisms as biomass Biomass diminishes along food chains with the loss of carbon dioxide, water and waste products (e.g. urea) to the environment Because energy and biomass is lost between each level of a food chain, the number of potential trophic levels are limited 27 | Ecology Endriyo Phillip. Higher trophic levels receive less energy / biomass from feeding and so need to eat larger quantities to obtain sufficient amounts Because higher trophic levels need to eat more, they expend more energy (and biomass) hunting for food If the energy required to hunt food exceeds the energy available from the food eaten, the trophic level becomes unviable Representation of Energy Flow Along a Food Chain Bio magnification Because energy transformations are only ~10% efficient, higher trophic levels must consume more prey to meet energy needs If a pollutant is ingested by living organisms, it will become concentrated at higher trophic levels as they eat more exposed prey The increase of a substance (such as a pollutant) in a particular organisms is called bioaccumulation The increase in the concentration of a substance at a particular trophic level is called bio magnification Bioaccumulation refers to how pollutants enter a food chain, whereas bio magnification refers to the tendency of pollutants to concentrate as they move from one trophic level to the next. Because pollutants become concentrated by bio magnification, higher trophic levels are more susceptible to their toxic effects The pesticide DDT caused egg-shell thinning and population declines in species of birds that fed on exposed insects Heavy metals (like mercury) released into waterways via industrial processes may become concentrated in fish Ecological productivity In ecology, production (or productivity) refers to the rate of generation of biomass in an ecosystem 28 | Ecology Endriyo Phillip. It is usually expressed in units of mass per area per time (e.g. kg m–2 day–1) Primary Production Primary production describes the production of chemical energy in organic compounds by producers The main source of energy for primary production is sunlight, but a fraction may be driven by chemosynthesis by lithotrophs Primary production may be categorised as one of two types: Gross primary production (GPP) is the amount of chemical energy as biomass that a producer creates in a given length of time Net primary production (NPP) is the amount of chemical energy that is not consumed by respiration (NPP = GPP – respiration) Secondary Production Secondary production describes the generation of biomass by heterotrophic organisms (consumers) This biomass generation is driven by the transfer of organic compounds between trophic levels via feeding Secondary production may also be categorised according to gross (total) and net (usable) amounts of biomass Ecological Productivity Estimating population size To determine the abundance of different species living in a community. It's impossible to count every individual living thing in a habitat, so ecologists use special techniques and formulas to make an educated guess. The Importance of Population Estimation 29 | Ecology Endriyo Phillip. Without data, ecologists cannot predict how a community will change over time. A change in one species population may have a knock-on effect on another population. Population dynamics looks at the effect that various factors have on the size of a population over time. Populations experience constant change. It can fluctuate either up or down, depending on several potential causes. Population dynamics can have a major influence on the stability, development, and growth of a population. Change Potential Causes Increase Decrease Birth Immigration Good environmental conditions High resource availability Death Emigration Harsh environmental conditions Competition for resources Disease Human activities Population estimations can detect if a population is experiencing a significant decline. Such a decline could present an issue for the species because small populations experience a greater risk of extinction. Why? They tend to have lower genetic diversity, making them more vulnerable to environmental changes and inheriting harmful genes. A change in population dynamics can have a domino effect on the entire community. All species in a community rely on each other for food, resources, pollination, shelter, and oxygen. A sudden decline of one species could lead to the fall of another, which causes the reduction of another, and another… Methods of Estimating Population Size Ecologists estimate population size using three different sampling methods. Quadrats and transects are used for plants or sessile (unmoving) animals, whilst the mark-recapture method is used for mobile organisms. THE QUADRAT METHOD A quadrat is a square frame of a fixed size used to outline a sample area. Before quadrat sampling, quadrat locations are determined using random coordinates within the study site. This prevents bias, ensuring an even spread of quadrats and species. Additionally, it is essential to understand the area of the study site. For square or rectangular habitats, multiply the length and width. However, many habitats will require the use of grid references. 30 | Ecology Endriyo Phillip. Grid references indicate a location on a map using grid lines. These lines are identified using letters and numbers. For example, on a 4x4 grid, the reference could be B2, with this representing: two cells in →→ and one down↓. The quadrat is placed on the ground using random, predetermined coordinates. The individuals within the quadrat are identified and counted. A quadrat of 1 m2 was placed in a rock pool. Three barnacles and four limpets were inside the area of the quadrat. Sometimes, estimating percentage cover is a more suitable method than counting individuals. A gridded quadrat is used to calculate percentage cover. This is a quadrat which is split into smaller squares. The dominant species is determined by seeing which is more present within each square, and from this, the estimated percentage cover can be calculated. A gridded quadrat of 1 m2 was placed in a meadow. It contained 25 smaller squares, each equivalent to 4% of the quadrat's area (100/25 = 4%). Thirteen squares were primarily grass, eight were mainly moss, and the remaining four were bare soil. This translates to an estimated percentage cover of: 13 squares x 4% = 52% grass 8 squares x 4% = 32% moss 4 squares x 4% = 16% bare soil Multiple quadrat samples are taken to build up a representation of the entire habitat. The Transect Method A transect is a line placed through a habitat. It used to measure vegetation frequency systematically. Continuous transects record vegetation along the entire length of the transect line. As a result, they are best suited for shorter distances. Interrupted transects are used to record vegetation at regular intervals along the line. Transects often measure vegetation changes in successional habitats. Successional habitats gradually change from one end to the other. The soils, plants and animals present will vary as you move through the habitat. Dunes are an example of successional habitats. They change from exposed sandy slopes to established grasslands and forests. The species present in this habitat depend on abiotic (non-living) factors: Proximity to the sea Salinity Wind exposure Soil composition 31 | Ecology Endriyo Phillip. And biotic (living) factors: The existing species that are present Kite diagrams are used to show how vegetation frequency changes along atransect. The area of the graph shows frequency - the wider the chart, the higher the frequency. These diagrams give an overall impression of how a successional habitat changes. The Mark-Recapture Method Ecologists capture animals and mark them with tags, paint, markings, or bands. The marked animals are then released back into their environment, where they naturally mix with the rest of the population. Animals with a hard shell are easy to mark. Unsplash Later, a second animal sample is collected. This will likely include some marked individuals (known as recaptures) and some unmarked individuals. How are animals safely captured? Longworth traps capture small mammals with bait. Pitfall traps catch arthropods that live on the ground Beating trays are used to collect arthropods living on plants Pooters are used to suck insects into a small chamber (don't worry, you can't suck them into your mouth accidentally!) Nets are used to sample freshwater organisms of varying sizes. The ratio of marked to unmarked individuals allows ecologists to estimate the population size. The mark-recapture method assumes that the larger the population, the lower the percentage of individuals recaptured. Estimation Methods: Pros and Cons Method Pros Cons Quadrats and Transects MarkRecapture Easy to use Affordable Low labour intensity Can rapidly detect population declines It can be physically demanding to use Inconsistency or incorrect quadrat size leads to errors Many assumptions about the population Animals may change behaviour to avoid or permit capture Estimating Population Size: Formulas Once data has been collected, it needs to be extrapolated to estimate the population size for the entire habitat. 32 | Ecology Endriyo Phillip. The Quadrat Formulae The formula required for extrapolating quadrat data depends on how the data was collected. Counting Individuals To estimate the population size, the habitat area is divided by the quadrat area and multiplied by the mean. The following formula can be used: Suppose an ecologist found a mean of 3 thistles within each 1 m 2 quadrat. The total habitat size was 12,000 m2. From this calculation, it can be concluded that there are 36,000 thistles in the population. Percentage Cover To estimate the population size, calculate the mean percentage cover and multiply this by 100 to obtain a percentage. Suppose an ecologist measured the percentage of moss cover for ten quadrats in a moorland habitat. From this calculation, it can be concluded that the moorland habitat has 68.9% moss coverage. The Mark-Recapture Formula The formula for the mark-recapture method is known as the Lincoln Index. 33 | Ecology Endriyo Phillip. Suppose an ecologist captured and marked 15 snails during the first sample. They then caught 21 in the second sample; 3 were already marked as they had been captured in the first sample. Using the Lincoln Index formula, the ecologist can conclude that there are 105 snails in the population. Estimating Population Size: Activity Estimating population size isn't as difficult as it sounds. All you need is a large open space (such as a school playing field or local park) and some measuring apparatus. Aim: Estimate the population size of a chosen plant species in a habitat using the quadrat method (counting individuals). You may need to decide the appropriate estimation method for some activities. Pay attention to the chosen species and the nature of the habitat. Equipment: Quadrat Two 10 m tape measures Clipboard Pen Paper Method: 1. Measure the size of your chosen habitat. Select your quadrat locations using random coordinates within the habitat. 2. At your first coordinates, extend the tape measures to their maximum length. Lay them on the ground, perpendicular to each other, to form a right angle. This will create an area of 100 m2. 3. Use a random number generator to obtain two numbers between 0 and 100. You will use these as coordinates within your 100 m2 area. 4. Place the quadrat at the random coordinates. Count and record the number of individuals of your chosen species present within the quadrat. 5. Take nine more random samples within the 100 m2 area. 6. Repeat this process at the predetermined quadrat locations within the habitat. 7. Estimate the total population size. Control Variables: 34 | Ecology Endriyo Phillip. Quadrat size Number of quadrat samples taken Counting method Risks: Cuts or stings Allergies Adverse weather conditions POPULATION GROWTH CURVES Exponential & logistic growth How populations grow when they have unlimited resources (and how resource limits change that pattern). In exponential growth, a population's per capita (per individual) growth rate stays the same regardless of population size, making the population grow faster and faster as it gets larger. In nature, populations may grow exponentially for some period, but they will ultimately be limited by resource availability. In logistic growth, a population's per capita growth rate gets smaller and smaller as population size approaches a maximum imposed by limited resources in the environment, known as the carrying capacity (K). Exponential growth produces a J-shaped curve, while logistic growth produces an S-shaped curve. In theory, any kind of organism could take over the Earth just by reproducing. For instance, imagine that we started with a single pair of male and female rabbits. If these rabbits and their descendants reproduced at top speed for 7 years, without any deaths, we would have enough rabbits to cover the entire district. if we used E. coli bacteria instead, we could start with just one bacterium and have enough bacteria to cover the Earth with a 1-foot layer in just 36 hours. But this is not possible. Why, then, don't we see these populations getting as big as they theoretically could? E. coli, rabbits, and all living organisms need specific resources, such as nutrients and suitable environments, in order to survive and reproduce. These resources aren’t unlimited, and a population can only reach a size that match the availability of resources in its local environment. Population ecologists use a variety of mathematical methods to model population dynamics (how populations change in size and composition over time). Some of these models represent growth without environmental constraints, while others include "ceilings" determined by limited resources. Mathematical models of populations can be used to accurately describe changes occurring in a population and, importantly, to predict future changes. To understand the different models that are used to represent population dynamics, let's start by looking at a general equation for the population growth rate (change in number of individuals in a population over time): 35 | Ecology Endriyo Phillip. In this equation, dN/dT is the growth rate of the population in a given instant, N is population size, T is time, and r is the per capita rate of increase –that is, how quickly the population grows per individual already in the population. If we assume no movement of individuals into or out of the population, r is just a function of birth and death rates. You can learn more about the meaning and derivation of the equation here: The equation above is very general, and we can make more specific forms of it to describe two different kinds of growth models: exponential and logistic. When the per capita rate of increase (r) takes the same positive value regardless of the population size, then we get exponential growth. When the per capita rate of increase (r) decreases as the population increases towards a maximum limit, then we get logistic growth. Exponential growth Bacteria grown in the lab provide an excellent example of exponential growth. In exponential growth, the population’s growth rate increases over time, in proportion to the size of the population. Let’s take a look at how this works. Bacteria reproduce by binary fission (splitting in half), and the time between divisions is about an hour for many bacterial species. To see how this exponential growth, let's start by placing 1000 bacteria in a flask with an unlimited supply of nutrients. After 1 hour: Each bacterium will divide, yielding 2000 bacteria (an increase of 1000 bacteria). 36 | Ecology Endriyo Phillip. After 2 hours: Each of the 2000 bacteria will divide, producing 4000 (an increase of 2000 bacteria). After 3 hours: Each of the 4000 bacteria will divide, producing 8000 (an increase of 4000 bacteria). The key concept of exponential growth is that the population growth rate —the number of organisms added in each generation—increases as the population gets larger. And the results can be dramatic: after 1 day (24 cycles of division), our bacterial population would have grown from 1000 to over 16 billion! When population size, N, is plotted over time, a J-shaped growth curve is made. we get exponential growth when r (the per capita rate of increase) for our population is positive and constant. While any positive, constant r can lead to exponential growth, you will often see exponential growth represented with an r of 𝑟𝑚𝑎𝑥 𝒓𝒎𝒂𝒙 is the maximum per capita rate of increase for a particular species under ideal conditions, and it varies from species to species. For instance, bacteria can reproduce much faster than humans, and would have a higher maximum per capita rate of increase. The maximum population growth rate for a species, sometimes called its biotic potential, is expressed in the following equation: Logistic growth Exponential growth is not a very sustainable state of affairs, since it depends on infinite amounts of resources (which tend not to exist in the real world). Exponential growth may happen for a while, if there are few individuals and many resources. But when the number of individuals gets large enough, resources start to get used up, slowing the growth rate. Eventually, the growth rate will plateau, or level off, making an S-shaped curve. The population size at which it levels off, which represents the maximum population size a particular environment can support, is called the carrying capacity, or K. 37 | Ecology Endriyo Phillip. We can mathematically model logistic growth by modifying our equation for exponential growth, using an r (per capita growth rate) that depends on population size (N) and how close it is to carrying capacity (K). Assuming that the population has a base growth rate of𝑟𝑚𝑎𝑥 , when it is very small, we can write the following equation: At any given point in time during a population's growth, the expression K−N tells us how many more individuals can be added to the population before it hits carrying capacity. (K−N)/K is the fraction of the carrying capacity that has not yet been “used up.” The more carrying capacity that has been used up, the more the (K−N)/K term will reduce the growth rate. When the population is tiny, N is very small compared to K. The (K−N)/K term becomes approximately (K/K) or 1, giving us back the exponential equation. This fits with our graph above: the population grows near-exponentially at first, but levels off more and more as it approaches K. What factors determine carrying capacity? Basically, any kind of resource important to a species’ survival can act as a limit. For plants, the water, sunlight, nutrients, and the space to grow are some key resources. For animals, important resources include food, water, shelter, and nesting space. Limited quantities of these resources results in competition between members of the same population, or intraspecific competition (intra- = within; -specific = species). Intraspecific competition for resources may not affect populations that are well below their carrying capacity—resources are plentiful and all individuals can obtain what they need. However, as population size increases, the competition intensifies. In addition, the accumulation of waste products can reduce an environment’s carrying capacity. 38 | Ecology Endriyo Phillip. Examples of logistic growth Yeast, a microscopic fungus used to make bread and alcoholic beverages, can produce a classic S-shaped curve when grown in a test tube. In the graph shown below, yeast growth levels off as the population hits the limit of the available nutrients. (If we followed the population for longer, it would likely crash, since the test tube is a closed system – meaning that fuel sources would eventually run out and wastes might reach toxic levels). In the real world, there are variations on the “ideal” logistic curve. We can see one example in the graph below, which illustrates population growth in harbor seals in Washington State. In the early part of the 20th century, seals were actively hunted under a government program that viewed them as harmful predators, greatly reducing their numbers. Since this program was shut down, seal populations have rebounded in a roughly logistic pattern. A shown in the graph above, population size may bounce around a bit when it gets to carrying capacity, dipping below or jumping above this value. Its common for real populations to oscillate (bounce back and forth) continually around carrying capacity, rather than forming a perfectly flat line. 39 | Ecology Endriyo Phillip. Population size and density To study the demographics of a population, we'll want to start off with a few baseline measures. One is simply the number of individuals in the population, or population size—N. Another is the population density, the number of individuals per area or volume of habitat. Size and density are both important in describing the current status of the population and, potentially, for making predictions about how it could change in the future: Larger populations may be more stable than smaller populations because they’re likely to have greater genetic variability and thus more potential to adapt to changes in the environment through natural selection. A member of a low-density population—where organisms are sparsely spread out—might have more trouble finding a mate to reproduce with than an individual in a high-density population. Species distribution Often, in addition to knowing the number and density of individuals in an area, ecologists will also want to know their distribution. Species dispersion patterns— or distribution patterns—refer to how the individuals in a population are distributed in space at a given time. The individual organisms that make up a population can be more or less equally spaced, dispersed randomly with no predictable pattern, or clustered in groups. These are known as uniform, random, and clumped dispersion patterns, respectively. Uniform dispersion. In uniform dispersion, individuals of a population are spaced more or less evenly. One example of uniform dispersion comes from plants that secrete toxins to inhibit growth of nearby individuals—a phenomenon called allelopathy. We can also find uniform dispersion in animal species where individuals stake out and defend territories. Random dispersion. In random dispersion, individuals are distributed randomly, without a predictable pattern. An example of random dispersion comes from dandelions and other plants that have wind-dispersed seeds. The seeds spread widely and sprout where they happen to fall, as long as the environment is favorable—has enough soil, water, nutrients, and light. Clumped dispersion. In a clumped dispersion, individuals are clustered in groups. A clumped dispersion may be seen in plants that drop their seeds straight to the ground—such as oak trees—or animals that live in groups— 40 | Ecology Endriyo Phillip. schools of fish or herds of elephants. Clumped dispersions also happen in habitats that are patchy, with only some patches suitable to live in. As you can see from these examples, dispersion of individuals in a population provides more information about how they interact with each other—and with their environment—than a simple density measurement. Life tables, survivorship, & age-sex structure These are tools ecologists use to describe the present state of a population and predict its future growth. To predict if a population will grow or shrink, ecologists need to know birth and death rates for organisms at different ages as well as the current age and sex makeup of the population. Life tables summarize birth and death rates for organisms at different stages of their lives. Survivorship curves are graphs that show what fraction of a population survives from one age to the next. An age-sex pyramid is a "snapshot" of a population in time showing how its members are distributed among age and sex categories. Governments around the world keep records of human birth and death rates—not just for the overall population of a country but also for specific groups within it, broken down by age and sex. Often, this data is arranged in summary tables called life tables. Enterprising insurance companies make good use of these life tables, taking the probability of death at a given age and using it to calculate insurance rates that, statistically, guarantee a tidy profit. Ecologists often collect similar information for the species they study, but they don't do it to maximize profits! They do it to gain knowledge and, often, to help protect species. Take, for example, ecologists concerned about the endangered white rhinoceros. They might follow a group of rhinoceros from birth to death. Each year, they would record how many rhinoceros had survived and how many babies had been born. From this data, they could better understand the life history, or typical survival and reproduction pattern, of their rhinoceros group. What's the use of a life history? In some cases, ecologists are just curious about how organisms live, reproduce, and die. But there is also a practical reason to collect life history data. By combining birth and death rates with a "snapshot" of the current population—how many old and young organisms there are and whether they are male or female—ecologists can predict how a population is likely to grow or shrink in the future. This is particularly important in the case of an endangered species, like the rhinoceros in our example. Life tables A life table records matters of life and death for a population—literally! It summarizes the likelihood that organisms in a population will live, die, and/or reproduce at different stages of their lives. Taking a look at a basic life table that just shows survival—rather than survival and reproduction. Specifically, we'll focus on the Dall mountain sheep, a wild sheep of northwestern North America. 41 | Ecology Endriyo Phillip. This data was collected by an ecologist named Olaus Murie who hiked around Mount McKinley National Park in Alaska for several years in the 1930s and 1940s. Every time he came across the skull of a dead Dall mountain sheep, he used the size of its horns to estimate how old it must have been when it died. From the ages of the 608 skulls he discovered, he estimated survival and death rates for the sheep across their lifespans. The table below is based on Murie's skull collection data. To make it easier to read, the table is standardized to a population of 1000 sheep. As we look through the table, we can picture what will happen, on average, to those 1000 sheep— specifically, how many will survive or die in each age bracket. In the first row we see that 1000 sheep are born, reach an age of zero. Of those sheep, 54 will die before they reach 0.5 years of age. That makes for a death, or mortality, rate of 54/1000, or 0.054, which is recorded in the far-right column. Number surviving at Number dying Age-specific mortality rate— Age beginning of age in age interval fraction of individuals alive at interval in interval out of 1000 out of 1000 beginning of interval that die years born born during the interval 0–0.5 1000 54 0.054 0.5–1 946 145 0.1533 1–2 801 12 0.015 2–3 789 13 0.0165 3–4 776 12 0.0155 4–5 764 30 0.0393 5–6 734 46 0.0627 6–7 688 48 0.0698 7–8 640 69 0.1078 8–9 571 132 0.2312 9–10 439 187 0.426 10–11 252 156 0.619 11–12 96 90 0.9375 12–13 6 3 0.5 13–14 3 3 1 By looking at the life table, we can see when the sheep have the greatest risk of death. One high-risk period is between 0.5 and 1 years; this reflects that very young sheep are easy prey for predators and may die of exposure. The other period 42 | Ecology Endriyo Phillip. where the death rate is high is late in life, starting around age eight. Here, the sheep are dying of old age. This is a relatively bare-bones life table; it only shows survival rates, not reproduction rates. Many life tables show both survival and reproduction. If we added reproduction to this table, we would have another column listing the average number of lambs produced per sheep in each age interval. Survivorship curves Life tables are hard to read. Instead survival data as a graph is used, as a survivorship curve. A survivorship curve shows what fraction of a starting group is still alive at each successive age. For example, the survivorship curve for Dall mountain sheep is shown below: The graph makes it nice and clear that there's a small dip in sheep survival early on, but most of the sheep die relatively late in life. Different species have differently shaped survivorship curves. In general, we can divide survivorship curves into three types based on their shapes: 43 | Ecology Endriyo Phillip. Type I. Humans and most primates have a Type I survivorship curve. In a Type I curve, organisms tend not to die when they are young or middle-aged but, instead, die when they become elderly. Species with Type I curves usually have small numbers of offspring and provide lots of parental care to make sure those offspring survive. Type II. Many bird species have a Type II survivorship curve. In a Type II curve, organisms die more or less equally at each age interval. Organisms with this type of survivorship curve may also have relatively few offspring and provide significant parental care. Type III. Trees, marine invertebrates, and most fish have a Type III survivorship curve. In a Type III curve, very few organisms survive their younger years. However, the lucky ones that make it through youth are likely to have pretty long lives after that. Species with this type of curve usually have lots of offspring at once—such as a tree releasing thousands of seeds—but don't provide much care for the offspring. Age-sex structure How can we use the birth and death rates from a life table to predict if a population will grow or shrink? To do this effectively, we need to look at a population in its present state. For instance, suppose we have two populations of buffalos: one made up mostly of young, reproductive-aged female buffalos and one made up mostly of male buffalos past their reproductive years. Even if these populations are the same size and share a life table—have the same reproduction and survival rates at a given age—they are likely to follow different paths. The first population is likely to grow because it has many buffalos that are in prime position to produce baby buffalos. The second population is likely to shrink because it has many buffalos that are close to death and can no longer reproduce. So, who's currently in a population makes a big difference when we are thinking about future population growth! Information about the age-sex structure of a population is often shown as a population pyramid. The x-axis shows the percent of the population in each category, with males to the left and females to the right. The y-axis shows age groups from birth to old age. 44 | Ecology Endriyo Phillip. It's common to see population pyramids used to represent human populations. In fact, there are specific shapes of pyramids that tend to be associated with growing, stable, and shrinking human populations, as shown below. Countries with rapid population growth have a sharp pyramid shape in their age structure diagrams. That is, they have a large fraction of younger people, many of whom are of reproductive age or will be soon. This pattern often shows up for countries that are economically less developed, where lifespan is limited by access to medical care and other resources. Areas with slow growth, including more economically developed countries like the United States, still have age-sex structures with a pyramid shape. However, the pyramid is not as sharp, meaning that there are fewer young and reproductive-aged people and more old people relative to rapidly growing countries. Other developed countries, such as Italy, have zero population growth. The age structure of these populations has a dome or silo shape, with an even greater percentage of middle-aged and old people than in the slow-growing example. Finally, some developed countries actually have shrinking populations. This is the case for Japan33cubed. The population pyramid for these countries typically pinches inward towards its base, reflecting that young people are a small fraction of the population. The basic principles of these human examples hold true for many populations in nature. Large fractions of young and reproductive individuals mean a population is likely to grow. Large fractions of individuals past reproductive age mean a population is likely to shrink. Life history strategies How organisms allocate energy to maximize the number of offspring they leave behind. The life history of a species is the pattern of survival and reproduction events typical for a member of the species (essentially, its lifecycle). Life history patterns evolve by natural selection, and they represent an "optimization" of tradeoffs between growth, survival, and reproduction. One tradeoff is between number of offspring produced and the amount of energy (both physical resources and parental care) put into each offspring. Timing of first reproduction is another tradeoff. Early reproduction lowers the chance of dying without offspring, but later reproduction may allow organisms to have more or healthier offspring or to provide better care. 45 | Ecology Endriyo Phillip. Members of some species reproduce only once (semelparity), while members of other species can reproduce multiple times (iteroparity). What is a "life history"? What does your life history look like? In the world of ecology, that question doesn't refer to the many challenges and successes you've experienced, or to the friendships you've made along the way. Instead, when we're talking about life history in ecology, we're thinking about basic demographic features of a population or species – the kind of things that would appear in a life table. That includes when organisms first reproduce, how many offspring they have in each round of reproduction, and how many times reproduction occurs. For humans, life history involves a late start to reproduction, few offspring, and the ability to reproduce multiple times. We can define the life history of a species as its lifecycle, and in particular, the lifecycle features related to survival and reproduction. Life history is shaped by natural selection and reflects how members of a species distribute their limited resources among growth, survival, and the production of offspring. Life history strategies and natural selection All living things need energy and nutrients to grow, maintain their bodies, and reproduce. In nature, these resources are in limited supply, and there is often competition for access to them (e.g., to sunlight and minerals for plants or food sources for animals). Thus, each organism will have non-infinite resources to divide among activities like growth, body maintenance, and reproduction. What does it mean for an organism to allocate its limited resources "well" in this context? From an evolutionary standpoint, it means that the resources are distributed among the potential activities (growth, maintenance, reproduction) in a way that maximizes fitness, or the number of offspring the organism leaves in the next generation. Organisms with inherited traits that cause them to distribute their resources in a more effective way will tend to leave more offspring than organisms lacking these traits, causing the traits to increase in the population over generations by natural selection. Over very long periods of time, this process results in species with life history strategies, or collections of life history traits (number of offspring, timing of reproduction, amount of parental care, etc.), that are well-adapted for their role and environment. The optimal life history strategy may be different for each species, depending on its traits, environment, and other constraints. Parental care and fecundity One major tradeoff in life history strategies is between number of offspring and a parent's investment in the individual offspring. Basically, this is a "quantity versus quality" question: an organism can have many offspring that each represent a relatively small energy investment, or few offspring that each represent a relatively large energy investment. 46 | Ecology Endriyo Phillip. To put this more formally, we can say that fecundity tends to be inversely related to the amount of energy invested per offspring. Fecundity is an organism's reproductive capacity (the number of offspring it's capable of producing). The higher the fecundity of an organism, the less energy it's likely to invest in each offspring, both in terms of direct resources – such as fuel reserves placed in an egg or seed – and in terms of parental care. Organisms that produce large numbers of offspring tend to make a relatively small energy investment in each, and don't usually provide much parental care. The offspring are "on their own," and the idea is that enough are produced that some will survive (even if the odds for any one are low). Organisms that make few offspring usually make a large energy investment in each offspring and often provide lots of parental care. These organisms are effectively "putting their eggs in one basket" (literally, in some cases!) and are heavily invested in the survival of each offspring. As for so many cases in biology, these are general trends and not universal rules. The main point is just that when organisms have many offspring, they can't invest as much energy in any single offspring. When they have fewer, they can (and must) invest more energy to ensure those offspring's survival. Example 1: Many offspring, low investment/parental care A typical sea snail produces hundreds of eggs at a pop, and these eggs hatch to yield baby snails that are pretty self-sufficient from the get-go. In fact, the baby snails in the first 10% of eggs that hatch will enthusiastically eat their slowerhatching siblings for breakfast. Cannibalism aside, this example is a good illustration of one common type of parental investment strategy. Sea snails and many other marine invertebrates provide little (if any) care to their offspring. Instead, they use most of their energy budget to make lots of offspring, each of which is relatively small. The sea snail isn't even that impressive when it comes to numbers—a female sea urchin might release 100,000,000,000 eggs. In species with this type of strategy, offspring are often self-sufficient at an early age. Still, since not much energy is invested in each offspring, they tend to be small and come into the world with low energy reserves. This makes the offspring vulnerable to predation, so many or most will not survive—instead, it's their sheer numbers that ensure the survival of the population. Example 2: Few offspring, high investment/parental care To see a strategy at the opposite end of the spectrum, let's consider the giant panda. Panda females typically have just one cub each time they reproduce, and the young cub is far from self-sufficient. Animal species like the elephant, which have few offspring during each reproductive event, often give extensive parental care. They may also produce larger, more energetically "expensive" offspring. The newborn elephant may look tiny, but compared to a hatching sea snail, it's massive! Species with this type of high-investment strategy use much of their energy budget to care for their offspring, sometimes at the expense of their own health. 47 | Ecology Endriyo Phillip. This type of strategy is common in mammals, including humans and kangaroos as well as pandas. The babies of these species are relatively helpless at birth and need to develop quite a bit before they become self-sufficient. Fecundity and investment tradeoffs in plants The same broad patterns seen in animals also apply to plants. Of course, plants aren't going to provide parental care in the same way that animals do. However, they can still produce either large numbers of energetically "cheap" seeds or small numbers of energetically "expensive" seeds. For example, plants with low fecundity, such as coconuts and chestnuts, produce small numbers of energy-rich seeds, each of which has a good chance of germinating into a new organism. Plants with high fecundity, such as orchids, take the opposite approach: they usually make many small, energy-poor seeds, each of which has a relatively low chance of surviving. Timing of first reproduction (early vs. late) When a species starts reproducing is another important part of its life history—and another place where we see trade-offs and lots of variation among species. Some types of plants and animals start reproducing early, while others delay much longer. What are the pros and cons of these strategies? Organisms that reproduce early have less risk of leaving no offspring at all, but this may be at the expense of their growth or health. For example, small fish like silverfish use their energy to reproduce early in life, but since they throw all their energy to reproduction, they don't reach the size that would give them defense against predators. Organisms that reproduce at a later age often have greater fecundity or are better able to provide parental care. On the flip side, they run a greater risk of not surviving to reproductive age. For example, larger fish, like the shark, use their energy to grow to a size that gives them more protection. As a consequence, they delay reproduction, so there's more chance that they will die before reproducing (or before they've reproduced to their maximum). In general, age at first reproduction is linked to the lifespan of a species. Shortlived species often start reproducing early, while long-lived species are more likely to delay reproduction. This is a good reminder that a life history strategy is an integrated "solution" to the problem of leaving as many offspring as possible, and that any one part (e.g., age of first reproduction) only makes sense in light of others (e.g., lifespan). Single vs. multiple reproductive events Another important characteristic of life history relates to how many times an organism reproduces over its lifetime. For some species, reproduction is a onetime, all-out event, and the organism doesn't survive much beyond that one event. In other species, opportunities for reproduction come around multiple times, or even many times, throughout the organism's lifetime. To apply a little ecology vocab, we can split species into two groups: 48 | Ecology Endriyo Phillip. Those that can reproduce only once (semelparity) Those that can reproduce multiple times over their lifetime (iteroparity) Semelparity In semelparity, a member of a species reproduces only once during its lifetime and then dies. Species with this pattern use up most of their resource budget in a single reproductive event, sacrificing their health to the point that they do not survive. Examples of species that display semelparity are bamboo, which flowers once and then dies, and the Chinook salmon, which uses most of its energy reserves to migrate from the ocean to its freshwater nesting area, where it reproduces and then dies. Iteroparity In iteroparity, individuals of a species reproduce repeatedly during their lives. Iteroparity can take different forms, depending on the reproductive cycles of the organisms involved. Species that display iteroparity don't put all of their resources into a single reproductive event, as there's a fitness benefit (an opportunity to have more offspring) in surviving to reproduce more times. Some animals are able to mate only once per year, but can survive through multiple mating seasons. The pronghorn antelope is an example of an animal that has a seasonal estrus cycle (“heat”). Estrus is a hormonally induced physiological condition that prepares the body for successful mating. Females of species with estrus cycles mate only during the estrus phase of the cycle. A different pattern is observed in primates, including humans and chimpanzees, which may attempt reproduction at any time during their reproductive years. However, the menstrual cycles of the females make pregnancy likely only a few days per month during ovulation. Population regulation What factors limit population sizes? Key points In nature, population size and growth are limited by many factors. Some are density-dependent, while others are density-independent. Density-dependent limiting factors causes a population's per capita growth rate to change—typically, to drop—with increasing population density. One example is competition for limited food among members of a population. Density-independent factors affect per capita growth rate independent of population density. Examples include natural disasters like forest fires. Limiting factors of different kinds can interact in complex ways to produce various patterns of population growth. Some populations show cyclical oscillations, in which population size changes predictably in a cycle. All populations on Earth have limits to their growth. Even populations of bunnies— that reproduce like bunnies!—don't grow infinitely large. What exactly are these environmental limiting factors? Broadly speaking, we can split the factors that 49 | Ecology Endriyo Phillip. regulate population growth into two main groups: density-dependent and densityindependent. Density-dependent limiting factors Imagine a population of organisms—let's say, deer—with access to a fixed, constant amount of food. When the population is small, the limited amount of food will be plenty for everyone. But, when the population gets large enough, the limited amount of food may no longer be sufficient, leading to competition among the deer. Because of the competition, some deer may die of starvation or fail to have offspring, decreasing the per capita—per individual—growth rate and causing population size to plateau or shrink. In this scenario, competition for food is a density-dependent limiting factor. In general, we define density-dependent limiting factors as factors that affect the per capita growth rate of a population differently depending on how dense the population already is. Most density-dependent factors make the per capita growth rate go down as the population increases. This is an example of negative feedback that limits population growth. Density-dependent limiting factors can lead to a logistic pattern of growth, in which a population's size levels off at an environmentally determined maximum called the carrying capacity. Sometimes this is a smooth process; in other cases, though, the population may overshoot carrying capacity and be brought back down by density-dependent factors. Density-dependent limiting factors tend to be biotic—living organism-related—as opposed to physical features of the environment. Some common examples of density-dependent limiting factors include: Competition within the population. When a population reaches a high density, there are more individuals trying to use the same quantity of resources. This can lead to competition for food, water, shelter, mates, light, and other resources needed for survival and reproduction. Predation. Higher-density populations may attract predators who wouldn’t bother with a sparser population. When these predators eat individuals from the population, they decrease its numbers but may increase their own. Disease and parasites. Disease is more likely to break out and result in deaths when more individuals are living together in the same place. Parasites are also more likely to spread under these conditions. Waste accumulation. High population densities can lead to the accumulation of harmful waste products that kill individuals or impair reproduction, reducing the population’s growth. Density-dependent regulation can also take the form of behavioral or physiological changes in the organisms that make up the population. For example, rodents called lemmings respond to high population density by emigrating in groups in search of a new, less crowded place to live. This process has been misinterpreted as a mass suicide of sorts in popular culture because the lemmings sometimes die while trying to cross bodies of water. 50 | Ecology Endriyo Phillip. Density-independent limiting factors The second group of limiting factors consists of density-independent limiting factors that affect per capita growth rate independent of how dense the population is. As an example, let's consider a wildfire that breaks out in a forest where deer live. The fire will kill any unlucky deer that are present, regardless of population size. An individual deer's chance of dying doesn't depend at all on how many other deer are around. Density-independent limiting factors often take the form of natural disasters, severe weather, and pollution. Unlike density-dependent limiting factors, density-independent limiting factors alone can’t keep a population at constant levels. That’s because their strength doesn’t depend on the size of the population, so they don’t make a "correction" when the population size gets too large. Instead, they may lead to erratic, abrupt shifts in population size. Small populations may be at risk of getting wiped out by sporadic, density-independent events. Population fluctuations In the real world, many density-dependent and density-independent limiting factors can—and usually do—interact to produce the patterns of change we see in a population. For example, a population may be kept near carrying capacity by density-dependent factors for a period then experience an abrupt drop in numbers due to a density-independent event, such as a storm or fire. However, even in the absence of catastrophes, populations are not always stably at carrying capacity. In fact, populations can fluctuate, or vary, in density in many different patterns. Some undergo irregular spikes and crashes in numbers. For instance, algae may bloom when an influx of phosphorous leads to unsustainable growth of the population. Other populations have regular cycles of boom and bust. Let's take a closer look at these cycles. Population cycles Some populations undergo cyclical oscillations in size. Cyclical oscillations are repeating rises and drops in the size of the population over time. If we graphed population size over time for a population with cyclical oscillations, it would look roughly like the wave below—though probably not quite as tidy! Where do these oscillations come from? In many cases, oscillations are produced by interactions between populations of at least two different species. For instance, 51 | Ecology Endriyo Phillip. predation, parasite infection, and fluctuation in food availability have all been shown to drive oscillations. These density-dependent factors don't always create oscillations, however. Instead, they only do so under the right conditions, when populations interact in specific ways. Interactions in communities Key points: An ecological community consists of all the populations of all the different species that live together in a particular area. Interactions between different species in a community are called interspecific interactions—inter- means "between." Different types of interspecific interactions have different effects on the two participants, which may be positive (+), negative (-), or neutral (0). The main types of interspecific interactions include competition (-/-), predation (+/-), mutualism, (+/+), commensalism (+/0), and parasitism (+/-). Introduction When we took a tour through population ecology, we mostly looked at populations of individual species in isolation. In reality, though, populations of one species are rarely—if ever!—isolated from populations of other species. In most cases, many species share a habitat, and the interactions between them play a major role in regulating population growth and abundance. Together, the populations of all the different species that live together in an area make up what's called an ecological community. For instance, if we wanted to describe the ecological community of a coral reef, we would include the populations of every single type of organism we could find, from coral species to fish species to the single-celled, photosynthetic algae living in the corals. For a healthy reef, that comes out to a whole lot of different species! Community ecologists seek to understand what drives the patterns of species coexistence, diversity, and distribution that we see in nature. A core part of how they address these questions is by examining how different species in a community interact with each other. Interactions between two or more species are called interspecific interactions—inter- means "between." Name Description Effect Competition Organisms of two species use the same limited resource and have a negative impact on each other. -/- Predation A member of one species, predator, eats all or part of the body of a member of another species, prey. +/- 52 | Ecology Endriyo Phillip. Name Description Effect Herbivory A special case of predation in which the prey species is a plant +/- Mutualism A long-term, close association between two species in which both partners benefit +/+ Commensalism A long-term, close association between two species in which one benefits and the other is unaffected +/0 Parasitism A long-term, close association between two species in which one benefits and the other is harmed +/- Overview: interspecies interactions Interspecies interactions can be broken into three main categories: competition, predation, and symbiosis. Let's take a closer look at each. Competition In interspecific competition, members of two different species use the same limited resource and therefore compete for it. Competition negatively affects both participants (-/- interaction), as either species would have higher survival and reproduction if the other was absent. Species compete when they have overlapping niches. That is, overlapping ecological roles and requirements for survival and reproduction. Competition can be minimized if two species with overlapping niches evolve by natural selection to utilize less similar resources, resulting in resource partitioning. Predation In predation, a member of one species—the predator—eats part or all of the living, or recently living, body of another organism—the prey. This interaction is beneficial for the predator, but harmful for the prey. Predation may involve two animal species, but it can also involve an animal or insect consuming part of a plant, a special case of predation known as herbivory. Predators and prey regulate each other's population dynamics. Also, many species in predator-prey relationships have evolved adaptations—beneficial features arising by natural selection—related to their interaction. On the prey end, these include mechanical, chemical, and behavioral defenses. Some species also have warning coloration that alerts potential predators to their defenses; other harmless species may mimic this warning coloration. Symbiosis Symbiosis is a general term for interspecific interactions in which two species live together in a long-term, intimate association. In everyday life, we sometimes use the term symbiosis to mean a relationship that benefits both parties. However, in 53 | Ecology Endriyo Phillip. ecologist-speak, symbiosis is a broader concept and can include close, lasting relationships with a variety of positive or negative effects on the participants. Mutualism In a mutualism, two species have a long-term interaction that is beneficial to both of them. For example, some types of fungi form mutualistic associations with plant roots. The plant can photosynthesize, and it provides the fungus with fixed carbon in the form of sugars and other organic molecules. The fungus has a network of threadlike structures called hyphae, which allow it to capture water and nutrients from the soil and provide them to the plant. Commensalism In a commensalism, two species have a long-term interaction that is beneficial to one and has no positive or negative effect on the other. For instance, many of the bacteria that inhabit our bodies seem to have a commensal relationship with us. They benefit by getting shelter and nutrients and have no obvious helpful or harmful effect on us. It's worth noting that many apparent commensalisms actually turn out to be slightly mutualistic or slightly parasitic when we look at them more closely. For instance, biologists are finding more and more evidence that our normal microbial inhabitants play a key role in health. Parasitism In a parasitism, two species have a close, lasting interaction that is beneficial to one, the parasite, and harmful to the other, the host (+/- interaction). Some parasites cause familiar human diseases. For instance, if there is a tapeworm living in your intestine, you are the host and the tapeworm is the parasite—your presence enhances the tapeworm's quality of life, but not vice versa! Ecological Succession Succession as progressive change in an ecological community. Primary vs. secondary succession. The idea of a climax community. Succession is a series of progressive changes in the composition of an ecological community over time. In primary succession, newly exposed or newly formed rock is colonized by living things for the first time. In secondary succession, an area previously occupied by living things is disturbed—disrupted—then recolonized following the disturbance. Have you ever looked at a landscape with a complex, diverse community of plants and animals—such as a forest—and wondered how it came to be? Once upon a time, that land must have been empty rock, yet today, it supports a rich ecological community consisting of populations of different species that live together and interact with one another. Odds are, that didn't happen overnight! Ecologists have a strong interest in understanding how communities form and change over time. In fact, they have spent a lot of time observing how complex communities, like forests, arise from empty land or bare rock. They study, for 54 | Ecology Endriyo Phillip. example, sites where volcanic eruptions, glacier retreats, or wildfires have taken place, clearing land or exposing rock. In studying these sites over time, ecologists have seen gradual processes of change in ecological communities. In many cases, a community arising in a disturbed area goes through a series of shifts in composition, often over the course of many years. This series of changes is called ecological succession. Succession often involves a progression from communities with lower species diversity—which may be less stable—to communities with higher species diversity— which may be more stable though this is not a universal rule. Primary Succession Primary succession occurs when new land is formed or bare rock is exposed, providing a habitat that can be colonized for the first time. For example, primary succession may take place following the eruption of volcanoes, such as those on the Big Island of Hawaii. As lava flows into the ocean, new rock is formed. On the Big Island, approximately 32 acres of land are added each year. What happens to this land during primary succession? First, weathering and other natural forces break down the substrate, rock, enough for the establishment of certain hearty plants and lichens with few soil requirements, known as pioneer species, see image below. These species help to further break down the mineral-rich lava into soil where other, less hardy species can grow and eventually replace the pioneer species. In addition, as these early species grow and die, they add to an ever-growing layer of decomposing organic material and contribute to soil formation. This process repeats multiple times during succession. At each stage, new species move into an area, often due to changes to the environment made by the preceding species, and may replace their predecessors. At some point, the community may reach a relatively stable state and stop changing in composition. However, it's unclear if there is always—or even usually—a stable endpoint to succession, as we'll discuss later in the article. Secondary succession 55 | Ecology Endriyo Phillip. In secondary succession, a previously occupied area is re-colonized following a disturbance that kills much or all of its community. A classic example of secondary succession occurs in oak and hickory forests cleared by wildfire. Wildfires will burn most vegetation and kill animals unable to flee the area. Their nutrients, however, are returned to the ground in the form of ash. Since a disturbed area already has nutrient-rich soil, it can be recolonized much more quickly than the bare rock of primary succession. Before a fire, the vegetation of an oak and hickory forest would have been dominated by tall trees. Their height would have helped them acquire solar energy, while also shading the ground and other low-lying species. After the fire, however, these trees do not spring right back up. Instead, the first plants to grow back are usually annual plants—plants that live a single year—followed within a few years by quickly growing and spreading grasses. The early colonizers can be classified as pioneer species, as they are in primary succession. Over many years, due at least in part to changes in the environment caused by the growth of grasses and other species, shrubs will emerge, followed by small pine, oak, and hickory trees. Eventually, barring further disturbances, the oak and hickory trees will become dominant and form a dense canopy, returning the community to its original state—its pre-fire composition. This process of succession takes about 150 years. The path and endpoint of succession The early ecologists who first studied succession thought of it as a predictable process in which a community always went through the same series of stages. They also thought that the end result of succession was a stable, unchanging final state called a climax community, largely determined by an area's climate. For instance, in the example above, the mature oak and hickory forest would be the climax community. Today, the idea of a set path for succession and a stable climax community have been called into question. Rather than taking a predetermined path, it appears that succession can follow different routes depending on the specifics of the situation. Also, although stable climax communities can form in some cases, this may be uncommon in many environments. Ecosystems may experience frequent disturbances that prevent a community from reaching an equilibrium state—or knock it quickly out of this state if it manages to get there. 56 | Ecology Endriyo Phillip. Cyclic Succession This is only the change in the structure of an ecosystem on a cyclic basis. Some plants remain dormant for the rest of the year and emerge all at once. This drastically changes the structure of an ecosystem. “A seral community is an intermediate stage of ecological succession advancing towards the climax community.” Man and the environment Effects of Population Growth on our Environment The factors responsible for environment degradation is population growth or population density. In particular, population density plays the most important role in shaping the socio-economic environment. Its effects are felt on the natural environment also. 1. Generation of Waste: Due to his destructive activities, man has dumped more and more waste in environment. As the man-made waste is not transformed, it causes degradation and the capacity of environment to absorb more waste is reduced. Further, waste leads to air and water pollution. 2. Threat to Biodiversity: Due to his destructive activities, man has extracted more and more minerals from the earth. Animals have been hunted and plants have disappeared. There has been loss of biodiversity. These have led to ecological imbalance. 3. Strain on Forests: Man has established new housing colonies. National highways and hydropower projects have been built and forests have been wiped out. These destructive activities have increased and led to ecological imbalance. 4. Urbanization: Rapid growth of population has led to urbanization which has adversely affected environment. Due to population pressure, natural resources in the cities are depleted at a fast rate due to population pressure. Moreover, population does not have proper sanitation facilities and pure drinking water. As a result, the health of the people is adversely affected. No doubt, urbanization reduces pressure on the rural environment, but it brings with if environmental damages through industrial growth, emissions and wastes. 5. Industrialization: 57 | Ecology Endriyo Phillip. Underdeveloped countries are following the policy of heavy industrialization which is causing environmental degradation. The establishment of such industries as fertilizers, iron and steel, chemicals and refineries have led to land, air and water pollution. 6. Land Degradation: Intensive farming and excessive use of fertilizers and pesticides have led to overexploitation of land and water resources. These have led to land degradation in the form of soil erosion, water logging and salination. 7. Transport Development: Environmental degradation is also due to transport development in the different parts of the world. The automobiles release huge quantities of poisonous gases such as carbon monoxide, nitrogen oxides and hydrocarbons. The development of ports and harbours have led to oil spills from ships adversely affecting fisheries, coral reefs, mangroves and landscapes. 8. Climatic Change: Climatic changes are irregular due to greenhouse gases. The thin skin of air that surrounds the planet is being affected by human activities as never before. Urban people are still being exposed to unaccepted levels of toxic pollutants. Further, forests are still being degraded by acid deposition generated by faraway industries, and greenhouse gases continue to accumulate in the atmosphere. 9. Productivity: Environmental degradation not only harms health but also reduces economic productivity. Dirty water, inadequate sanitation, air pollution and land degradation cause serious diseases on an enormous scale in developing countries like India. These, in turn, reduce the productivity levels in the country. To take specific instances, water pollution has led to declining fisheries in rivers, ponds and canals in both urban and rural areas. Water shortages have reduced economic activity in towns, and cities and villages. Soil and hazardous wastes have polluted ground water resources which cannot be used for agricultural and industrial production. Soil degradation leading to soil erosion, drought, etc. have led to siltation of reservoirs and blocking of river and canal transport channels. Deforestation has led to soil erosion and consequent loss of sustainable logging potential. Loss of bio-diversity has resulted in the loss of genetic resources. Last but not the least, atmospheric changes have given rise to disruption of marine food chain, damages to coastal infrastructure due to sea-rise and regional changes in agriculture productivity due to hurricanes in seas. Thus, environmental degradation undermines economic productivity of a nation. 58 | Ecology Endriyo Phillip. 10. Technology: Presently, environmental pollution is caused by old technology which releases gases and pollutants causing chemical and industrial pressure on environment. Impact of Environment on Population: Polluted environment also affects adversely the health of people. Control/mitigation of the effects of populations on the environment. Agricultural and industrial development along with urbanization and spread of infrastructure combined with population growth has led to environmental degradation. Environmental degradation harms human health, reduces economic productivity and leads to the loss of amenities. The damaging effects of economic development on environmental degradation can be reduced by a judicious choice of economic and environmental policies and environmental investments. We discuss some policy measures as under: 1. Control of Population Growth: The rate of population growth should be curtailed through effective family planning measures. This is essential because the proportion of total population in the labour force will increase further in the years to come as a result of changes in the age structure of the population. The shifting of labour force from the rural to the secondary sector requires increase in agricultural productivity. Increased agricultural productivity helps in meeting the demand for raw materials of the expanding manufacturing sector. With increased productivity, less workers are required to produce raw materials for industry and food-grains for the population. It also increases agricultural surplus thereby raising saving and investment for economic development. So concerted efforts are needed to increase agricultural productivity through technological advancement. This will ultimately lead to commercialisation of agriculture and production for exports, thereby earning foreign exchange for further development. 2. Economic Development: The aim of population control is not only to bring about a decline in fertility rates but also to improve the quality of life of the people. These are possible through rapid economic development. It is not an illusion to believe that a reduction in population growth will automatically raise living standards. In fact, an effective family planning policy should be integrated with measures to accelerate economic development. 3. Improving Health and Nutrition: The food and nutrition security for the weaker sections in a developing country should not be considered as issues in the Nutrition Science but should be 59 | Ecology Endriyo Phillip. considered as part of right to work, right to health, right to education, right to information and right of the poor. In such a country, there are agricultural, health, population, nutrition, children and education policies. On the other hand, there are fiscal and budget revisions, exports, imports, taxation, price wage, employment policies and policy related to subsidies. Ultimately, all these policies affect life of the poor, their food and nutritionist security and health. As a leading nutritionist C. Gopalan notes: “Various types of food are needed for maximum nutrition and if they are all taken together and in proper proportions (systematic balanced diet), they can provide necessary nutrients. Guarantee of good nutrition and absence of hunger are not the same thing. Our first effort should be towards removing hunger of the poor, but our long-term goal should be to provide maximum nutrition to our people which is useful in bringing out their hereditary talents. Nutrition security is more important than food security. Nutrition security includes making our food base wider and varietal. ” Improving health and nutrition levels is an extremely important factor contributing to the social development of a developing country. Especially the people of the weaker sections of the society who do not take adequate advantage of health, family welfare and nutrition services, should be made aware of these facilities so that their health and nutrition status can be improved. 4. Reducing Poverty: Such development projects should be started which provide greater employment opportunities to the poor. The government should expand health and family planning services and education so as to reach the poor that will help reduce population growth. Further, making investments in providing civic amenities like the supply of drinking water, sanitation facilities, alternate habitats in place of slums, etc. will not only improve welfare but also environment. 5. Removing Subsidies: To reduce environmental degradation at no financial cost to the government, subsidies for resource use by the private and public sectors should be removed. Subsidies on the use of electricity, fertilisers, pesticides, diesel, petrol, gas, irrigation water, etc. lead to their wasteful use and environmental problems. Subsidies to capital intensive and highly polluting private and public industries lead to environmental degradation. Removing or reducing subsidies will bring both economic and environmental benefits to the country. 6. Clarifying and Extending Property Rights: Lack of property rights over excessive use of resources leads to degradation of environment. This leads to overgrazing of common or public lands, deforestation, and overexploitation of minerals, fish, etc. Clarifying and assigning ownership titles and tenurial rights to private owners will solve environmental problems. Places where the use of common lands, forests, irrigation systems, fisheries, etc. 60 | Ecology Endriyo Phillip. are regulated and rules for their proper use are laid down by the community, the ownership rights should be clearly specified in the administrative records. 7. Market Based Approaches: Besides regulator measures, there is urgent need for adopting market based approaches for the protection of environment. They aim at pointing to consumers and industries about the cost of using natural resources on environment. These costs are reflected in the prices paid for goods and services so that industries and ultimately the consumers are guided by them to reduce air and water pollution. The Market Based Instruments (MBIs) are in the form of environmental taxes that include pollution charges (emission tax/pollution taxes), marketable permits, depositor fund system, input taxes/product charges, differential tax rates and user administrative charges and subsidies for pollution abatement equipment for air and water resources. 8. Regulatory Policies: Regulatory polices also help in reducing environmental degradation. Regulators have to make decisions regarding prices, quantity and technology. In making decisions, they have to choose between the quantity or the price of pollution or resource use of technologies. The regulating authority has also to decide whether policies should target the environmental problem directly or indirectly. It lays down technical standards and regulations and charges on air, water and land pollutants. Regulators should be impartial in applying environmental standards to both public and private sector polluters or resources users. 9. Economic Incentives: Like regulatory policies, economic incentives relate to price, quantity and technology. Incentives are usually in the form of variable fees to resource users for the quantity of pollutants in air, water and land use. They are given rebates if less waste or pollution is generated than the emission standards laid down. 10. Public Participation: Public awareness and participation are highly effective to improve environmental conditions. Conducting of formal and informal education programmes relating to environment management and environmental awareness programmes can go a long way in controlling environmental degradation and keeping the environment clean. For instance, the scheme of eco-labelling of products helps consumers to identify products that are environment friendly. Public participation can also render costless and useful assistance in Afforestation, conservation of wildlife, management of parks, improvement of sanitation and drainage systems and flood control. Use of indigenous institutions, local voluntary organisations and NGOs can render much help in educating the masses about the harmful effects of environmental degradation and the benefits of keeping the environment clean. 61 | Ecology Endriyo Phillip. EutrophicationEutrophication is the process in which a water body becomes overly enriched with nutrients, leading to plentiful growth of simple plant life. The excessive growth (or bloom) of algae and plankton in a water body are indicators of this process. Eutrophication is considered to be a serious environmental concern since it often results in the deterioration of water quality and the depletion of dissolved oxygen in water bodies. Eutrophic waters can eventually become “dead zones” that are incapable of supporting life. Eutrophication may be defined as the inorganic nutrient enrichment of natural waters, leading to an increased production of algae and macrophytes. The term Eutrophication is more widely known in relation to human activities where the artificial introduction of plant nutrients has led to community changes and a deterioration of water quality in many freshwater systems. Aquatic ecosystems are home to several plant and animal life forms – both simple and complex. The process of eutrophication destroys the balance in these ecosystems by favouring the growth of simple plant life. This greatly decreases the biodiversity of the ecosystem by killing off several desirable species. Causes of Eutrophication The availability of nutrients such as nitrogen and phosphorus limits the growth of plant life in an ecosystem. When water bodies are overly enriched with these nutrients, the growth of algae, plankton, and other simple plant life is favoured over the growth of more complex plant life. How do Water Bodies Become Overly Enriched? Phosphorus is considered one of the primary limiting factors for the growth of plant life in freshwater ecosystems. Several sources also claim that the availability of nitrogen is an important limiting factor for the growth of algae. 62 | Ecology Endriyo Phillip. Phosphates tend to stick to the soil and are transported along with it. Therefore, soil erosion is a major contributor to the phosphorus enrichment of water bodies. Some other phosphorus-rich sources that enrich water bodies with the nutrient include: Fertilizers Untreated sewage Detergents containing phosphorus Industrial discharge of waste. Among these sources, the primary contributors to eutrophication include agriculture and industrial wastes. What Happens to the Huge Biomass of Algae in Eutrophic Waters? The excessive growth of algae in eutrophic waters is accompanied by the generation of a large biomass of dead algae. These dead algae sink to the bottom of the water body where they are broken down by bacteria, which consume oxygen in the process. Process of Eutrophication The overconsumption of oxygen leads to hypoxic conditions (conditions in which the availability of oxygen is low) in the water. The hypoxic conditions at the lower levels of the water body lead to the suffocation and eventual death of larger life forms such as fish. Classification of Eutrophication The process of eutrophication can be categorized into two types based on its root cause. 63 | Ecology Endriyo Phillip. Anthropogenic Eutrophication Anthropogenic eutrophication is caused by human activity – Agricultural farms, golf courses, lawns, etc. are supplied with nutrients by humans in the form of fertilizers. These fertilizers are washed away by rains and eventually find their way into water bodies such as lakes and rivers. When introduced to an aqueous ecosystem, the fertilizers supply plentiful nutrients to algae and plankton, resulting in the eutrophication of the water body. Overpopulation places a huge demand on industrial and agricultural expansion, which in turn leads to deforestation. When this occurs, the soil erodes more easily, resulting in increased soil deposits in water bodies. If the soil is rich in phosphorus, it can lead to eutrophication and severely damage the ecosystem in and around the water body. When sewage pipes and industrial wastes are directed to water bodies, the nutrients present in the sewage and other wastes increase the rate at which eutrophication occurs. Natural Eutrophication Natural eutrophication refers to the excessive enrichment of water bodies via natural events. For example, the nutrients from the land can be washed away in a flood and deposited into a lake or a river. These water bodies become overly enriched with nutrients, enabling the excessive growth of algae and other simple plant life. The process of natural eutrophication is much slower when compared to the process of anthropogenic eutrophication. This process is also somewhat dependant on the temperature of the environment. It may even be complemented by the temperature changes brought on by global warming. Effects of Eutrophication Primarily, the adverse effects of eutrophication on aquatic bodies include a decrease in biodiversity, increase in toxicity of the water body, and change in species dominance. Some other important effects of this process are listed below. Phytoplanktons grow much faster in such situations. These phytoplankton species are toxic and are inedible. Gelatinous zooplankton blooms fast in these waters. Increased biomass of epiphytic and benthic algae can be observed in eutrophic waters. Significant changes arise in the species composition of macrophytes and the biomass. The water loses its transparency and develops a bad smell and colour. The treatment of this water becomes difficult. Depletion of dissolved oxygen in the water body. Frequent fish kill incidents occur and many desirable fish species are removed from the water body. The populations of shellfish and harvestable fish are lowered. 64 | Ecology Endriyo Phillip. The aesthetic value of the water body diminishes significantly. Ecological Effects of Eutrophication Natural standing waters range from ultra-oligotrophic to eutrophic with progressive increase in productivity and related parameters. In addition to such general changes, eutrophication also affects the vertical structure of lakes with further implications for the biology of freshwater organisms. The transition from eutrophic to hypertrophic status is usually the result of human activities, and ultimately affects the whole ecological balance of the freshwater system. Decrease in Biodiversity When an aquatic ecosystem is enriched with nutrients by either natural or artificial means, the conditions become extremely beneficial to primary producers. Commonly, algae and other similar species utilize these nutrients and a huge increase in their population (algal bloom) is observed. These algal blooms hinder the flow of sunlight to the bottom of the aquatic body and also cause wide swings in the dissolved oxygen levels in the water. When the dissolved oxygen in the water reduces to an amount below the hypoxic level, many marine animals suffocate and die. This reduces the effective biodiversity of the water body. Increase in Water Toxicity A few algae are toxic to many plants and animals. When these algae bloom in eutrophic waters, they release neurotoxins and hepatotoxins. These toxins can also move up the food chain via shellfish or other marine animals and lead to the death of many animals. 65 | Ecology Endriyo Phillip. Toxic algal blooms can also be harmful to humans and are the root cause of many cases of neurotoxic, paralytic, and diarrhoetic shellfish poisoning. Invasion of New Species A limiting nutrient corresponding to a water body can be made abundant by the eutrophication process, leading to a shift in the species composition of the aquatic body and the ecosystem surrounding it. If a nitrogen deficient water body is suddenly enriched with it, many other competitive species might relocate to the water body and out-compete the original inhabitants of the ecosystem. One such example of a new species invading eutrophic conditions is the common carp, which has adapted to these conditions. READ AND MAKE NOTES ON POLLUTION AND CONSERVATION. 66 | Ecology Endriyo Phillip.
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