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Biogeochemical Cycles

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BIOGEOCHEMICAL
CYCLES
General Ecology Lecture 3b
Instructor: ANGELI VALERA- MAG-ASO
Objectives::
Identify and describe
the flow of nutrients in
each biogeochemical
cycle.
Explain the impact
that humans have on
the biogeochemical
cycles.
What Sustains Life on Earth?
Solar
energy, the
cycling of
matter, and
gravity sustain
the earth’s life.
Figure 33-7
Two Secrets of Survival: Energy
Flow and Matter Recycle
An ecosystem survives by a
combination of energy flow and
matter recycling.
Sources and sinks:
domination of storage or
release process of a
specific material within a
reservoir
FLUX: exchange
between two
reservoirs
CYCLE: system of
connected reservoirs
that transfer and
conserve a specific
material
D. T. Krohne, General Ecology
Fig .Idealized
diagram of the
geologic
cycle, which
includes the
tectonic, hydrologic
, rock and
biogeochemical
cycles.
© 2003 John Wiley and Sons Publishers
WATER CYCLE
Condensation
Rain clouds
Transpiration
Precipitation
to land
Transpiration from
plants
Precipitation
Runoff
Surface runoff
(rapid)
Evaporation
Evaporation
from land
Precipitation
Evaporation
from ocean
Surface
runoff
(rapid)
Infiltration and
Percolation
Groundwater movement (slow)
Ocean storage
Precipitation
to ocean
Water’ Unique Properties
There are strong forces of attraction between
molecules of water.
Water exists as a liquid over a wide temperature
range.
Liquid water changes temperature slowly.
It takes a large amount of energy for water to
evaporate.
Liquid water can dissolve a variety of compounds.
compounds.
Water is the medium by which elements and other
materials move through the ecosystem
Water expands when it freezes.
Effects of Human Activities
on Water Cycle
We alter the water cycle by:
Withdrawing large amounts of freshwater.
Clearing vegetation and eroding soils.
Polluting surface and underground water.
Contributing to climate change.
CO2 & CH4
15%/year
Modified from D. T. Krohne, General Ecology
THE CARBON CYCLE
© 2003 John Wiley and Sons Publishers
Effects of Human Activities
on Carbon Cycle
We alter the
carbon cycle by
adding excess CO2
to the atmosphere
through:
Burning fossil fuels.
Clearing vegetation
faster than it is
replaced.
Figure 33-28
Fig 4.17 Global flux of carbon, 1850-1990.
© 2003 John Wiley and Sons Publishers
Idealized diagram illustrating photosynthesis
for a green plant (tree) and generalized
reaction.
© 2003 John Wiley and Sons Publishers
OXYGEN CYCLE
Major sources: photodissociation of water
vapor and photosynthesis
Comines with a wide range of substances
Ozone – produced by photochemical
reactions in the atmophere;
atmophere; essential to
reduce influx of UV radiation to Earth
FORMS OF NITROGEN
50% fertilizer
(Bacteria)
Modified from D. T. Krohne, General Ecology
NITROGEN CYCLE
NITROGEN CYCLE
© 2003 John Wiley and Sons Publishers
Nitrogen fixers:
Cyanobacteria
Free--living soil bacteria
Free
Bacteria associated
with roots of
leguminous plants
Actinomycetes
fungi, associated with
roots of alders and
other species of woody
plants
Effects of Human Activities
on the Nitrogen Cycle
We alter the nitrogen cycle by:
Adding gases that contribute to acid rain.
Adding nitrous oxide to the atmosphere through
farming practices which can warm the
atmosphere and deplete ozone.
Contaminating ground water from nitrate ions in
inorganic fertilizers.
Releasing nitrogen into the troposphere through
deforestation.
Effects of Human Activities
on the Nitrogen Cycle
Human activities
such as
production of
fertilizers now fix
more nitrogen
than all natural
sources
combined.
Figure 33-30
Critical Thinking Issue – How are Human
Activities Affecting the Nitrogen Cycle?
Effects of increased use of
nitrogen fertilizer:
• Increased nitric acid in soil:
• Leaching of magnesium and
potassium
• Increased aluminum levels
• Plant root damage
• Changes in microbe communities
• Fish kills
• Eutrophication of water bodies
• Nitrates in drinking water
• Global effects on plant based CO2 uptake
© 2003 John Wiley and Sons Publishers
Gaseous
phase
D. T. Krohne, General Ecology D. T. Krohne, General Ecology
Modified from D. T. Krohne, General Ecology
PHOSPHORUS CYCLE
mining
excretion
Fertilizer
Guano
agriculture
uptake by weathering
autotrophs
leaching, runoff
Marine
Dissolved
Food
in Ocean
Webs
Water
death,
decomposition
sedimentation
settling out
uplifting over
geologic time
Marine Sediments
uptake by
autotrophs
Dissolved
Land
in Soil Water,
Food
Lakes, Rivers
Webs
death,
decomposition
weathering
Rocks
PHOSPHORUS CYCLE
© 2003 John Wiley and Sons Publishers
Effects of Human Activities
on the Phosphorous Cycle
We remove large amounts of phosphate from
the earth to make fertilizer.
We reduce phosphorous in tropical soils by
clearing forests.
We add excess phosphates to aquatic
systems from runoff of animal wastes and
fertilizers.
SULFUR CYCLE
Water
Sulfur
trioxide
Acidic fog and
precipitation
Sulfuric acid
Ammonia
Oxygen
Sulfur dioxide
Ammonium
sulfate
Hydrogen sulfide
Plants
Dimethyl sulfide
Volcano
Industries
Animals
Ocean
Sulfate salts
Metallic
sulfide
deposits
Decaying matter
Sulfur
Hydrogen sulfide
Effects of Human Activities
on the Sulfur Cycle
We add sulfur dioxide to the atmosphere by:
Burning coal and oil
Refining sulfur containing petroleum
Convert sulfursulfur-containing metallic ores into free
metals such as copper, lead, and zinc releasing
sulfur dioxide into the environment – produce
acute toxicity and major damage to vegetation
(bleaching, defoliation and reduced growth);
significant part of acid rain; irritates respiratory
tract
Ecosystems and the Gaia Hypothesis
Ecosystem defined: a community
of organisms and it’s corresponding abiotic
environment through which matter cycles
and energy flows
• Wide
variation in ecosystems
• Boarders can be well defined or vague
• Can be natural or artificial, managed or
wild
• Wide range in scale
• Common to all ecosystems: energy flow
and cycling of matter
Gaia Hypothesis(es)
• Life has greatly affected the planetary
environment
• This alteration has allowed life to persist
• The Earth is a “super-organism” - Life controls
the environment in a fashion that is equivalent to
the way an organism controls its various systems
•Has not been accepted by all ecologists and
atmospheric scientists, but helps us to
understand the behavior of ecosystems and the
interaction of biogeochemical cycling.
The Gaia Hypothesis:
Is the Earth Alive?
Some have proposed that the earth’s various
forms of life control or at least influence its
chemical cycles and other earthearth-sustaining
processes.
The strong Gaia hypothesis: life controls the
earth’s lifelife-sustaining processes.
The weak Gaia hypothesis: life influences the
earth’s lifelife-sustaining processes.
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