Ecosystem Dynamics

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45 Terms

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original source of energy

Sun

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1st Law of Thermodynamics

“Energy cannot be created or destroyed”

Energy input must be continuous

Energy is converted to chemical energy stored in food

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2nd Law of Thermodynamics

“Every exchange of energy increases entropy”

Energy conversion is inefficient: some is lost as heat as it transfers through ecosystems

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Law of Conservation of Mass

“Matter cannot be created or destroyed”

Nutrient inputs must equal outputs

Chemicals/atoms are continuously recycled through the ecosystem

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trophic levels

any step in a nutritive series, or food chain, of an ecosystem, organised on the basis of feeding behavior

<p>any step in a nutritive series, or food chain, of an ecosystem, organised on the basis of feeding behavior</p>
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primary producers

photosynthesis; autotrophs

ie. plants, bacteria

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Trophic efficiency

percent of energy transferred from one level to the next

10% passes on to next level; 90% released as heat

<p>percent of energy transferred from one level to the next</p><p>10% passes on to next level; 90% released as heat</p>
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primary consumers

eat primary producers; heterotrophs

e.g. herbivores

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secondary consumers

eat primary consumers; heterotrophs

e.g. carnivores, insectivores, piscivores

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tertiary consumers

eat secondary consumers; heterotrophs

e.g. carnivores, insectivores, piscivores

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apex consumer/predator

highest link in energy cycle; is not eaten/preyed on by any other consumer

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decomposers

take leftover energy and matter from dead producers/consumers and return to environment

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conservation of matter

no matter is lost; may be changed in form but atoms in = atoms out

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biogeochemical cycles

cycles that involve molecules that are essential for life and how they circulate through an ecosystem/biosphere

ex. carbon, nitrogen, phosphorus, water

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water cycle

recycling of all water in the biosphere since it is essential to all life

ie. precipitation and evaporation

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carbon cycle

recycling of all carbon in the biosphere for organic molecules & energy (storage)

ex. photosynthesis and cellular respiration, sediments & rock

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nitrogen cycle

recycling of all nitrogen in the biosphere - essential component of amino acids, proteins, & DNA

Plants can use ammonium (NH4+) & nitrate (NO3-)

Animals can only use organic forms of nitrogen (amino acids)

ex. air (80% atmosphere); fixation in soil

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phosphorous cycle

recycling of all phosphorus in the biosphere - main component of nucleic acids, phospholipids, and ATP - local

ex. Marine sedimentary rocks, organisms, ocean, and soi

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evaporation

water molecules go from liquid to gaseous state

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water vapour

gaseous water

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condensation

water vapour returns to liquid droplets/solid cyrstals in the sky to form clouds

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precipitation

water falling from cloud onto land or body of waterr

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river

stream of flowing water; forms from runoff from precipitation

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sublimation

ice/snow to vapourtr

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transpiration

evaporation of water from the surface of plants

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freshwater

water with minimal ionic solutes; 2.5% of total water on planet, 68.9% of which is in glaciers, 30.8% in groundwater, and 0.3% in lakes and rivers

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Average residence time for water molecules

knowt flashcard image
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gross primary production (GPP)

total amount of energy acquired by primary producers (via photosynthesis or chemosynthesis) in an ecosystem; total amount of energy converted to organic molecules over time

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net primary productivity (NPP)

remaining usable amount of energy transmitted out of a producer after metabolic processes, heat, etc.; amount of stored energy available to consumers

NPP = GPP - Ra

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Primary Productivity in Aquatic Systems

light penetration, nutrient availability, micronutreients (minerals)

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Primary Productivity in Terrestrial Systems

driven by climate and vascular plants; temperature, moisture, nutrients

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Respiration by autotrophs (RA)

amount of energy used by photosynthesizing organisms (~1/2 of GPP)

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high productivity/NPP ecosystems

warm temperatures, high humidity and an influx of nutrients

ex. tropical wet rainforests and estuaries

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low productivity/NPP ecosystems

dry and either too hot or too cold for high rates of plant growth

ex. deserts and the Arctic

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Net Ecosystem Production (NEP)

amount of biomass accumulated by producers & consumers; tells us if the ecosystem is gaining or losing carbon over time

NEP = GPP - Rt

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Respiration by producers and consumers (Rt)

amount of energy used by ALL organisms in the ecosystem

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Carbon sinks

NEP > 0 ; net storage of carbon

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Carbon sources

NEP < 0; losing more carbon than is being stored in plants and animals

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Secondary production

amount of energy from food converted into new biomass

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Production Efficiency

percentage of energy from food used for growth and reproduction but not respiration; inversely related to energy demands

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Biomass pyramids

Shows how much BIOMASS is in each trophic level; can be inverted if there is exceptionally high turnover (consumption)

<p>Shows how much BIOMASS is in each trophic level; can be inverted if there is exceptionally high turnover (consumption)</p>
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Upwelling

brings nutrients from deeper water to the surface

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eutrophication

excessive influx of nutrients from agricultural runoff can cause exponential growth in algal and phytoplankton populations, depleting the water of oxygen, and negatively affecting the aquatic flora and fauna

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Food chain

Linear sequence of consumers, producers, and detritovores (who eats whom); Primary productivity and Loss of energy between trophic levels limits food chain length (<5 links)

<p>Linear sequence of consumers, producers, and detritovores (who eats whom); Primary productivity and Loss of energy between trophic levels limits food chain length (&lt;5 links)</p>
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Food web

A network of interconnected food chains

<p>A network of interconnected food chains</p>