Ecology Quiz 9 Flashcards
Ecological levels of Organization:
Biosphere - global processes
Ecosystem - Energy flux and cycling of nutrients
Community - Interactions among populations
Population - Population dynamics the unit of evolution
Organism - survival and reproduction the unit of natural selection
Ecosystem concept:
Ecosystem ecology:
Biogeochemical Cycles:
Major Biogeochemical Cycles:
Ecosystem concept:
“Though the organisms may claim our prime interest, when we are trying to think fundamentally, we cannot separate them from their special environments, with which they form one physical system.” Arthur G. Tansley, 1935
Can take organism out of their environment but they won’t function the same way
Ecosystem ecology:
The study of processes involving the ‘transformation’ and ‘flux of energy and chemical cycling in habitats.
These processes link the living components to non-living components.
Biotic + Abiotic interactions
Biogeochemical Cycles:
Elements and water cycle better abiotic and biotic components of ecosystems
Major Biogeochemical Cycles: water, carbon, nitrogen, and phosphorus
Trophic-Dynamic View of Ecosystems
Lindeman, R.L. (1942) The trophic-dynamic aspect of ecology. Ecology [1st rejected, then eventually published postmortem]
Linderman’s diagram described the movement of energy among groups of organisms at Cedar Bog Lake - trophic interactions of organism at cedar creek and the center is called the OOZE which is the primary producing and feeding the origins in the food web - the food web is carbon flow through bacteria
Pool =
Flux =
Pool = how much mass of an element is held in a biotic or abiotic component of an ecosystem
Flux = how much of an element moves out of a pool into another at a given time (rate)
Primary Production
The currency used for the measurement of primary production?
Energy in ecosystems originates with primary production by autotrophs(makes its own energy or carbon through acquisition of C02).
Primary production is the chemical energy generated by autotrophs, derived from fixation of CO2 in photosynthesis and chemosynthesis.
Primary production is the ultimate source of energy for all organisms, from bacteria to humans.
Energy assimilated by autotrophs is stored as carbon compounds in plant tissues - plant are primary producers in most ecosystem - energy from sun is harvest into chemical synthesis
Carbon is the currency used for the measurement of primary production.
Units: C mass/area/time (e.g. g/m-2/yr-1)
Gross Primary Production
Leaf Area Index (LAI) =
Gross primary production (GPP)—total amount of carbon fixed by autotrophs by photosynthesis in an ecosystem.
GPP depends on climate(temp and perception), which influences photosynthetic rate and the leaf area index (LAI).
Differences in allocation of resources within plants leads to differences in primary production - One key allocation decision is how many layers of leaves are produced:
Leaf Area Index (LAI) = leaf area / canopy area
LAI > 1 → more leaf area than canopy area, so there must be leaf overlap
LAI low is 0.25 and high is 1.5
Tremendous LAI variation among biomes:
Arctic tundra- LAI = 0.1 (<10% of ground area has leaf cover)
Moist tropical forests (Gabon, Africa) LAI ≈ 12 (= on average 12 leaves above every point on the forest floor)
Net Primary Production: NPP
Why is it Important?
Plants use about half of the carbon fixed in photosynthesis for respiration. All living plant tissues respire, but not all tissues photosynthesize (e.g., woody stems, roots).
Net primary production (NPP): NPP = GPP – respiration
NPP represents the biomass gained by the plant
Why is it Important?
NPP is the ultimate source of energy for all organisms in an ecosystem.
Variation in NPP is an indication of ecosystem health—changes in primary productivity can be symptomatic of stress or disturbance.
NPP is associated with the global carbon cycle (central to climate change).
Secondary Production
Energy derived from consumption of organic compounds produced by other organisms
Net secondary production depends on the “quality” of food (digestibility and nutrient content), and heterotroph physiology
Measuring NPP: Biomass harvest
Measuring NPP: Biomass dynamics
Measuring NPP: Biomass harvest:
- For many herbaceous plant communities, aboveground NPP estimates simply involve harvesting and weighing all the plant material in a sample area that is produced within a year…
- All the roots found in a 10 x 10 x 15 cm soil sample underneath one small annual wildflower
- Root production: more challenging to measure accurately. Difficult to distinguish between species and individuals grown together. Fine roots have fast dynamics (constantly growing and dying back); total root biomass at the season end can underestimate NPP allocated to roots
Measuring NPP: Biomass dynamics:
- Litterfall traps
- Dendrometer - diameter growth increment
- Rhizotron: Belowground NPP Dynamics
Measuring NPP: Gas Exchange
Enclose ecosystem within tent or structure: net change in [CO2] inside tent is a balance of GPP uptake and total respiration—net ecosystem production or net ecosystem exchange (NEE).
NEE = GPP – (AResp + HResp) or
Heterotrophic respiration (bacteria, detritivores, etc) must be subtracted to obtain NPP.
Negative value means losing carbon a net loss and no longer a carbon sink which means gain
Measuring NPP: Remote Sensing - Spectral signature
Biomass techniques are impractical for large or biologically diverse ecosystems
Chlorophyll concentrations can provide a proxy for GPP and NPP. They can be estimated using remote sensing methods that rely on reflection of solar radiation.
NDVI (Normalized Difference Vegetation Index): NDVI = (NIR – VIS) (NIR + VIS) This is then used to estimate C fixation
NDVI in Winter - Tan= low NDVI
NDVI in Summer - Dark Green= high NDVI
Environmental Controls on NPP
Water availability:
Temperature:
Nutrient Limitation of NPP:
Determination of the factors which control primary production is critical to understanding ecosystem function. NPP varies substantially over space and time through different ecosystems.
Water availability affects photosynthesis (on land) - primary driver of NPP:
Low water causes water stress and stomatal closure
At very high precipitation, NPP may decrease
Greater cloud cover
Lower sunlight
Leaching of nutrients
Soil saturation, which results in anoxic conditions
Temperature affects photosynthesis - with higher temp is higher photosynthesis
Enzyme activity and membrane fluidity
Nutrient Limitation of NPP:
Nutrients, particularly nitrogen & phosphorus, often control NPP
e.g., fertilization experiment in dry and wet alpine meadows
In the absence of a water limitation, soil nutrient availability is often implicated as the principal factor determining variation in primary production
Global Patterns of NPP: Land
Global Patterns of NPP: Oceans
Global Patterns of NPP: Land
NPP decreases in arid regions at about 25° N and S. Low water availability limits LAI and photosynthesis - desserts have no perception with low productivity
High latitudes have short growing seasons
Low temperatures constrain nutrient supply by lowering decomposition rates (limit nutrient cycling)
Low temperatures reduce photosynthesis
Freezing limits water availability
Global Patterns of NPP: Oceans
Ocean NPP peaks at mid-latitudes, where zones of upwelling are found
Trophic levels describe the
Feeding Relationships -
Many organisms do not fit neatly into one trophic level:
Trophic levels describe the feeding positions of groups of organisms in ecosystems
Omnivores feed at multiple trophic levels (e.g., coyote eat vegetation, herbivorous rodents, & other carnivores)
Intraguild predators do not merely feed on trophic levels below, but feed on other predators (each other)
Food Web Models
Some Limitations of Food Web Models
Diagrams showing connections between organisms and the food they consume
- Important tools to model ecological interactions
- Show energy flows among ecosystem components
- More organisms or species = more complexity
- A balance between clarity, simplicity and generality
Some Limitations of Food Web Models:
- Trophic interactions are dynamic - black bear consume diff organisms throughout the year
- Variable trophic interaction strength - some strong some weak
- Mutualists! Parasites! Microorganisms! - don’t consider these