Biology 20C - Fall 1998
ECOLOGY AND EVOLUTIONARY BIOLOGY
Lecture 26 - Ecosystems
An ecosystem is a relatively closed system (more or less isolated from other ecosystems) whose limits are defined by two major processes, Energy Flow and Bio-Geo-Chemical Cycling. It consists of all the organisms (individuals, populations, communities), resources and abiotic conditions co-existing within a geographical area.
An ecosystem is the most inclusive, and usually the largest, of all ecological concepts. Ecosystems range in scale from small systems like ponds, small islands or mountain tops; through regional systems like the Serengeti Plains of Africa; up to the scale of the whole earth (or biosphere).
Properties of Ecosystems: These primarily build on and extend aspects of the trophic structure and trophic organization of the communities within the ecosystem.
There are several similar ways to describe the role of each individual, population or species within an ecosystem:
1. How it uses other organisms
Producer: synthesizes new living tissues
Consumer: eats (or metabolizing) tissues
Decomposer: breaks tissues and/or biological molecules into inorganic materials.
2. The main source of energy
Autotroph: fixes energy from abiotic sources.
Photo-autotroph: fixes solar energy (via photosynthesis) into organic molecules
Chemo-autotroph: uses chemical energy from inorganic molecules
Heterotroph: obtains energy by consuming and metabolizing organic molecules from
other organisms (i.e. all consumers and decomposers)
3. What it eats
Plant: Uses inorganic nutrients, solar energy
Herbivore: Eats plant tissues
Carnivore (Predator): Eats animal tissues
Detritivore: Eats dead animal/plant tissues
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Plants |
Primary producers |
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Herbivores |
2o Secondary producers |
1o Primary consumers |
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1o Predators/parasites |
3o Tertiary producers |
2o Secondary consumers |
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2o Predators/parasites |
4o Quaternary producers |
3o Tertiary consumers |
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etc. |
etc. |
etc. |
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1o Detritivores |
1o Decomposers |
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2o Detritivores |
2o Decomposers |
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etc. |
etc. |
ENERGY FLOW, Energetics and Energy Budgets
Energy flow is a directional, irreversible process. However, the rate and timing of energy transfers are highly variable as a result of physiological and ecological processes. It is also inefficient, with
large amounts of energy radiated into space as heat at each step in the process:
Photo-autotrophic: sun è biotic (è abiotic ) è space
Chemo-autotrophic: abiotic è biotic (è abiotic ) è space
Productivity is the process by which energy (or carbon) is incorporated within the organic molecules of new living tissues. It is a Rate, measured in such units as: J m-2 d-1 or gC m-2 d-1
Gross primary productivity (GPP) is the rate at which new organic molecules are produced within the tissues of plants from abiotic energy and nutrients by photosynthesis. (Less than 1-2% of solar energy reaching the Earth's surface is fixed in organic molecules).
Net primary productivity (NPP) is the rate at which new plant tissues are created.
Net respiration rate (NRR) is the rate at which energy or carbon is returned to the abiotic world as "waste" products of maintenance of body mass and metabolism. ( NPP = GPP - NRR )
In analogous ways, Gross and Net Secondary Productivity measure the rates at which herbivores convert plant tissues into animal molecules and tissues; Gross and Net Tertiary Productivity measure the rates at which carnivores convert herbivore tissues; etc.
At each transfer between trophic levels, approximately 90% of the energy consumed is lost, mainly as heat during respiration. Hence energetic efficiency, measuring the proportion of energy at one trophic level than is retained in new production at the next trophic level averages about 10% (5% to 20%). The efficiency is lowest in decomposer transfers where vast amounts of heat are lost as organic molecules are broken into simple inorganic molecules.
Pyramids of Productivity are used to visualize productivity and efficiency at each trophic level. In closed systems these are always conical.
Standing Crop or Biomass is used to measure the accumulated products of production present at each trophic level at a specified instant. Biomass is the total mass of tissue, usually expressed as dry weight ( e.g. g m-2 ) or total carbon (e.g. gC m-2 ). Changes in biomass equals NPP - NRR.
Standing crop can be visualized as: Pyramids of Biomass, Pyramids of Carbon, Pyramids of Numbers.
These pyramids may vary in form depending on turnover rate (average longevity and other LHC), efficiency of transfer, species composition and diversity, and recent history of each trophic level. Inverted pyramids indicate that turnover rate slows markedly as one moves up trophic levels
BIOGEOCHEMICAL CYCLING (Nutrient Cycling)
In accord with the Law of Conservation of Matter (atoms can be transformed in chemical reactions, but not created nor destroyed), materials remain within closed ecosystems, but may be cycled back and forth within and between the biotic and abiotic components of the ecosystem.
(abiotic ç è abiotic) ç è (biotic ç è biotic)
Biogeochemical cycling has up to five main compartments (Campbell Fig 49- 8)
BIOSPHERE |
Biotic |
Cycling within the biosphere closely follows the pathways of trophic webs. |
ATMOSPHERE |
Atmospheric |
Gaseous phase |
HYDROSPHERE |
Aquatic |
Oceans, freshwater, ice, groundwater |
PEDOSPHERE |
Soils |
(may include groundwater) |
GEOSPHERE |
Rocks |
(includes sources and sinks) |
Biogeochemical cycling is usually studied by concentrating on a single element or molecule, and following its chemical pathways within and between through the abiotic and biotic components. A particular cycle may not include all the components, and the rates, frequencies and forms of the pathways vary greatly for different elements, and among different kinds of ecosystems. Within each component the nutrient may be available or unavailable for use by the organisms
Ecosystem studies usually focus on essential or limiting nutrients, those that set upper limits on standing crop and productivity at each trophic level. Different nutrients have very different availabilities, recycling rates, and residence times within the biosphere
Water Cycle: (Campbell: Fig 49- 9)
Original source |
Cometary bombardment ( > 4Gya ) |
Current source |
Volcanism |
Main form |
H2O |
Main Compartments |
All |
Biosphere residence |
Very short (minutes to weeks) |
Reservoir |
Oceans |
Sink |
Minerals |
Roles |
Medium for all biochemical processes |
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Transports, stores and buffers other nutrients |
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Buffers chemical/physical environment |
Carbon Cycle: (Campbell: Fig 49- 10)
Source - original |
Cometary bombardment |
Source - current |
Volcanism |
Main form |
CO2 ; organic molecules |
Main Compartment |
Biosphere |
Biosphere residence |
May be many generations |
Reservoir |
Atmosphere |
Sink |
Limestones; fossil fuels |
Roles |
Basis of life |
Oxygen Cycle: (usually treated as a subset of the carbon cycle)
Source - original |
Atmospheric CO2 |
Source - current |
Photosynthesis |
Main form |
O2, CO2 |
Main Compartments |
Biosphere, Atmosphere |
Biosphere residence |
Very short, often seconds to hours |
Reservoir |
Atmosphere |
Sink |
Limestones |
Roles |
Oxidative environment and biochemistry |
Nitrogen Cycle: (Campbell: Fig 49- 11)
Source - original |
Atmosphere |
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Source - current |
Rocks |
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Main form |
NO3, NH4, NH3 |
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Main Compartments |
Soils |
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Biosphere residence |
Prolonged conservation |
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Reservoir |
Atmosphere |
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Sink |
Rocks |
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Roles |
Essential for protein synthesis |
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Often the chronic limiting nutrient for ecosystems |
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Largely mediated by prokaryotic micro-organisms |
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Nitrogen fixation |
N2 è NH4 |
enters biosphere |
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Nitrification |
NH4 è NO3 |
available to plants |
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Ammonification |
NO3 è NH4 |
biosphere recycling |
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Denitrification |
NO3 è N2 |
leaves biosphere |
Phosphorus Cycle: (Campbell: Fig 49- 12)
Source - original |
Rocks |
Source - current |
Weathering of rocks |
Main form |
PO4 |
Main Compartments |
Geological |
Biosphere residence |
Short - often < 1 generation |
Reservoir |
Soils, unconsolidated sediments |
Sink |
Sedimentary rocks |
Roles |
Essential nucleic acids, ATP, membranes, lipids |
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Frequently the acute limiting nutrient for ecosystems |
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Readily leached |
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Extremely reactive, binds to particulates; precipitates readily |
Bio-Accumulation or Bio-Magnification: (Campbell: Fig 49- 16)
Carbon Dioxide Cycle: (Campbell: Fig 49- 17)