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

 

Plants

Primary producers

 

 

Herbivores

2o Secondary producers

1o Primary consumers

 

1o Predators/parasites

3o Tertiary producers

2o Secondary consumers

 

2o Predators/parasites

4o Quaternary producers

3o Tertiary consumers

 

etc.

etc.

etc.

 

1o Detritivores

1o Decomposers

 

2o Detritivores

2o Decomposers

 

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

 

Transports, stores and buffers other nutrients

 

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

Source - current

Rocks

Main form

NO3, NH4, NH3

Main Compartments

Soils

Biosphere residence

Prolonged conservation

Reservoir

Atmosphere

Sink

Rocks

Roles

Essential for protein synthesis

 

Often the chronic limiting nutrient for ecosystems

 

Largely mediated by prokaryotic micro-organisms

 

Nitrogen fixation

N2 è NH4

enters biosphere

 

Nitrification

NH4 è NO3

available to plants

 

Ammonification

NO3 è NH4

biosphere recycling

 

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

 

Frequently the acute limiting nutrient for ecosystems

 

Readily leached

 

Extremely reactive, binds to particulates; precipitates readily

 

Bio-Accumulation or Bio-Magnification: (Campbell: Fig 49- 16)

Carbon Dioxide Cycle: (Campbell: Fig 49- 17)