Ecosystem Ecology:
1. Trophic relationships determine the routes of energy
flows and chemical cycling in an ecosystem
An
ecosystem consists of all the organisms living in a community as well as all
the abiotic factors with which they interact.
The
dynamics of an ecosystem involve two processes: energy flow and chemical
cycling.
The
transformation of energy can be followed by grouping the species in a community
into trophic levels of feeding relationships.
2. Decomposition
connects all trophic levels
The organisms
that feed as detritivores often form a major link
between the primary producers and the consumers in an ecosystem.
The
organic material that makes up the living organisms in an ecosystem gets
recycled.
3. The laws of physics and chemistry apply to ecosystems
The law of conservation of energy applies to
ecosystems.
We can potentially trace all the energy from its
solar input to its release as heat by organisms.
The second law of thermodynamics allows us to
measure the efficiency of the energy conversions.
4. An ecosystems energy budget depends on primary
production
5. In aquatic ecosystems, light
and nutrients limit primary production
6. In terrestrial ecosystems,
temperature, moisture, and nutrients limit primary production
7. The efficiency of energy transfer between trophic
levels is usually less
than 20%
Trophic
efficiency is the percentage of production transferred from one trophic level
to the next.
Pyramids
of production represent the multiplicative loss of energy from a food chain.
8. Herbivores consume a small percentage of vegetation:
the green world hypothesis
According to the green worl
hypothesis, herbivores consume relatively little plant biomass because they
are held in check by a variety of factors including:
Plants have defenses against herbivores
Nutrients, not energy supply, usually limit
herbivores
Abiotic factors limit herbivores
Intraspecific competition can limit herbivore
numbers
Interspecific interactions check herbivore
densities
9. Biological and geologic processes move nutrients
between organic and inorganic compartments
A
general model of chemical cycling.
There
are four main reservoirs of elements and processes that transfer elements
between reservoirs.
Reservoirs
are defined by two characteristics, whether it contains organic or inorganic
materials, and whether or not the materials are directly usable by organisms.
The
nitrogen cycle.
Nitrogen
enters ecosystems through two natural pathways.
Atmospheric
deposition, where usable nitrogen is added to the soil by rain or dust.
Nitrogen
fixation, where certain prokaryotes convert N2 to minerals that can be used to
synthesize nitrogenous organic compounds like amino acids.
In
addition to the natural ways, industrial production of nitrogen-containing
fertilizer contributes to nitrogenous materials in ecosystems.
The
direct product of nitrogen fixation is ammonia, which picks up H + and becomes ammonium
in the soil (ammonification), which plants can use.
Certain
aerobic bacteria oxidize ammonium into nitrate, a process called nitrification.
Nitrate
can also be used by plants.
Some
bacteria get oxygen from the nitrate and release N2 back into the atmosphere
(denitrification).
The
phosphorous cycle.
organisms
require phosphorous for many things.
This
cycle is simpler than the others because phosphorous does not come from the
atmosphere.
Phosphorus
occurs only in phosphate, which plants absorb and use for organic synthesis.
Humus
and soil particles bind phosphate, so the recycling of it tends to be
localized.
10. Decomposition rates largely determine the rates of
nutrient cycling
11. Nutrient cycling is strongly regulated by vegetation
12. The human population is disrupting chemical cycles
throughout the biosphere
13. Combustion of
fossil fuels is the main cause of acid precipitation
14. Toxins can become concentrated in successive trophic
levels of food webs
15. Human activities may be causing climate change by
increasing carbon dioxide concentration in the atmosphere
16. Human activities are depleting atmospheric ozone