Biomes Large land vegetation types Climate or average weather conditions, profoundly influences life, producing distinctive vegetation types in various parts of world Distribution of grasslands, rain forest, tundra mainly influenced by prevailing temperature and rainfall Figure 6.16 Figure 6.17 Deserts Receive less than 25 cm of sporadic rainfall per year Hot deserts—Sahara Temperate—Mojave Cold—Atacama in Chile Deserts Plants and animals adapted to water conservation Plants may get water from fog, thick epidermis, fuzz Animals may never drink, get water from food, nocturnal Major deserts found along 30° north and south due to air circulation Deserts Large interior area of land masses away from oceans Rain shadow Fragile Desertification—due to overgrazing and loss of topsoil Figure 6.24a Grasslands Dry, sometimes produce large biomass 25-100 cm of rainfall/year Extremes in temperature Tall grass prairie—converted to cropland in North America: 90% Mixed grass Short grass: high plains closer to Rockies Grassland Erosion—loss of topsoil resulting from overfarming—no cover crops and excessive grazing of even the deep roots Grasslands Adapted to extremes in temperature Seasonality of precipitation types—snow in winter, rain in summer Deep rooted grasses Accumulation of dead plants produces thick, organic topsoils May be fire adapted Grasslands Temperate: Prairies Steppes P a m pa s Veldt Tropical: Savanna Figure 6.19a Figure 6.23a Chaparral or Mediterranean Cool rainy winters, hot dry summers Evergreen funky-looking shrubs, occasional pines and scrub oaks, grasses Small, leathery leaves Rodents, reptiles, birds Fire adapted Chaparral Drier areas—sagebrush scrub Great basin in North America Sahel (border of Sahara)—thornbush scrub Figure 6.27a Temperate Deciduous Forests Deciduous—lose leaves Temperate—midlatitude, cold in winter, warm in summer 75-200 cm rain/yr Great Lakes to eastern seaboard of US, south to Gulf of Mexico Original vegetation of most of Europe and eastern Canada Temperate Forests Maple, oak and beech are common trees Woody and herbaceous understory Wide variety of animals Massive habitat destruction wherever it occurs Figure 6.18a Conifer Forests Cone bearing trees in temperate areas, but with sandy soils (nutrient and water poor) Leaves are waxy needles of varying length to prevent extensive water loss Southern Pine Forests Conifer Forests Long warm growing season Commercial forests Boreal Forests: northern hemisphere only 45° to 60° north Pines, hemlocks, spruce, cedar, fir Taiga Conifer Forests Edge of boreal Forest gives rise to tundra Dry, cold, short growing season Figure 6.26a Temperate Rainforest Heavy rainfall Fertile soils Objects of contention over land use Olympic National Forest and Seashore Figure 6.20a Tundra Cold, low-lying area of north Low-growing shrubs, mosses, lichens, sedges 25 cm rain Marshy areas, shallow lakes Permafrost restricts water movement and root growth Short growing season—50 days Figure 6.25a Tropical Rain Forests 220-450 cm rain/year Hot all year Lush vegetation (high productivity) Poor soils—rapid decomposition prevents soil from building up Biogeochemical cycle—heavy on the bio Amazon basin, Central America, equatorial Africa, parts of Southeast Asia Tropical Rainforest Lock up tremendous amounts of carbon in vegetation—carbon sink Enormous species diversity (300 species in one hectare) Potential source of medicine and other commercial products Plants and animals –biocentric conservation Figure 6.21a Tropical Dry Forests Wet and dry seasons Hot all year Tropical evergreen or partly deciduous forest with Open woodland and grassy savannas Better soils Heavily exploited Aquatic Systems Marine Ocean Coral reefs Tidal wetlands Barrier islands Freshwater Lakes wetlands Oceans Coastal zone from high tide mark to point where continental self drops off Intertidal zone—between high and low tide Open ocean extends out from coastal zone Pelagic—vertical distance from ocean surface to ocean floor Benthic zone—ocean floor Photic zone—to 100 m below surface Figure 16.8 Oceans Productivity –highest near coast, low in open ocean Coastal zone productive—waves bring in nutrients, carry away waste, exposure to sun Oceans: coastal areas 10% of ocean area, 90% of species Great fisheries 75% of Earth’s surface Figure 16.6 Oceans Open oceans-- less productivity than deserts Open oceans—nutrient poor Most productive near poles, rich in phyto and zooplankton Coral Reefs Shallow tropical oceans Limestone deposits from generations of coral polyps Coral-polyps—animals and algae Biodiversity—great 2% ocean floor 25% ocean species Coral Reefs In peril Bleached coral reefs Algae die, then rest of polyp Ocean warming, ozone depletion, pollution Coral reef watch Where river flows into ocean Mix of salt and freshwater High nutrient load Supports all stages of life Buffer between ocean and land Sponge—capable of absorbing water Prevent surges from ocean narrow sandy islands Continental shelf is shallow Protect lagoons and salt marshes from storm damage Vacation homes upset sand deposition Fresh Water Systems Cover only 2.1% of earth’s surface Lakes, rivers, other water Littoral zone—shallow water along edge, plants can root Limnetic--vertical zone—vertical region from surface to point that light can deliver light for photosynthesis Estuaries Barrier Islands Fresh Water Systems Profundal zone—deepest layers, light can’t penetrate Thermocline—temperature drop off Fresh Water systems Eutrophic lakes—nutrient rich Artificial—human activities: fertilizer runoff, sewage, detergents, bedrock disturbance Overabundance of nutrients—algal blooms, as algae die, dissolved O2 consumed by decomposition, not enough O2 for other organisms Oligotrophic lakes—nutrient poor Fresh Water Wetlands Inundated with water at least part of year Swamps, bogs, tidal marshes High biological productivity Habitat for migratory birds Reduced by 55% since arrival of Europeans in US Wetlands Big push for conservation or reclamation Swamps—wetlands with trees Marshes—no trees Bogs—saturated ground Fens—fed by groundwater