lec 24: ecosystems & global ecology

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28 Terms

1
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humans

  • energy use accelerating & increasing

  • altered habitats

  • nutrient cycles disrupted

    • water

    • phosphorus & nitrogen

    • carbon

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autotrophs are inefficient are capturing solar energy

  • 0.8% incoming sunlight used by forest plants

  • 45% GPP into production of new biomass; rest used to respiration/was lost

  • photopigments absorb fraction of light wavelength

  • enzyme efficiency is temperature dependent

    • warmer conditions → faster

    • dryer conditions → photosynthesis stalls

<ul><li><p>0.8% incoming sunlight used by forest plants</p></li><li><p>45% GPP into production of new biomass; rest used to respiration/was lost</p></li><li><p>photopigments absorb fraction of light wavelength</p></li><li><p>enzyme efficiency is temperature dependent</p><ul><li><p>warmer conditions → faster</p></li><li><p>dryer conditions → photosynthesis stalls</p></li></ul></li></ul><p></p>
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primary producers (autotrophs)

inorganic compounds → chemical energy stored in sugars

  • primary source of energy flow in ecosystems

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gross primary productivity (GPP)

total chemical energy produced

<p>total chemical energy produced</p>
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primary producers use GPP

GPP = R + NPP (NPP = GPP - R)

  1. keep existing cells alive: cellular respiration (R)

    1. growth & reproduction: NPP energy

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biomass

total amount of chemical energy in organic material

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net primary productivity among geographic regions

  • deserts = low NPP

  • forests (tropical wet) = high NPP & high productivity

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net primary productivity among biomes

  • open oceans = low

    • majority of earth’s surface

  • topical wet forests = high

    • occupy modest amounts of earth’s surface

  • coral reefs = most productive

    • small surface area → limiting NPP contribution

<ul><li><p>open oceans = low</p><ul><li><p>majority of earth’s surface</p></li></ul></li><li><p>topical wet forests = high</p><ul><li><p>occupy modest amounts of earth’s surface</p></li></ul></li><li><p>coral reefs = most productive</p><ul><li><p>small surface area → limiting NPP contribution</p></li></ul></li></ul><p></p>
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food chain

series of steps

  • molecules & energy travels

<p>series of steps</p><ul><li><p>molecules &amp; energy travels</p></li></ul><p></p>
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grazing food chain

herbivores (primary consumers) & organisms that eat herbivores

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decomposer food chain

species eat dead remains

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food webs

compact way to summarize energy flow & documents complex trophic interactions

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nutrient cycle

  • energy eventually dissipates

  • sun replenishes energy

  • nutrients cycled through ecosystem

    • neither gained or lost

  • energy moves in form of biomass when organisms eat another

  • same energy source type = same trophic level (feeding)

<ul><li><p>energy eventually dissipates</p></li><li><p>sun replenishes energy</p></li><li><p>nutrients cycled through ecosystem</p><ul><li><p>neither gained or lost</p></li></ul></li><li><p>energy moves in form of biomass when organisms eat another</p></li><li><p>same energy source type = same trophic level (feeding)</p></li></ul><p></p>
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decomposers (detritivores)

feed on detritus (waste or dead remains)

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productivity declines at higher trophic levels

  • biomass greater @ lowest trophic

  • biomass declines at higher levels

  • 10% of energy transferred to next level

<ul><li><p>biomass greater @ lowest trophic</p></li><li><p>biomass declines at higher levels</p></li><li><p>10% of energy transferred to next level</p></li></ul><p></p>
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productivity pyramid

reports productivity & efficiency

  • productivity: biomass produced per unit of area yearly

  • efficiency: fraction of biomass transferred from one trophic level to the next

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10% rule masks variation

  • large mammals: more efficient biomass producers

    • smaller surface-area-to-volume ratio & lose less heat

  • ectotherms: more efficient biomass producers

    • don’t rely on oxidized sugars to keep warm

    • rely on environment & spend less energy on cellular respirations

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more efficient for humans to feed at lower trophic levels

humans as primary producers will receive the most energy due to one energy transfer

<p>humans as primary producers will receive the most energy due to one energy transfer</p>
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global water cycle

water evaporates out of oceans & precipitates over globe

  • water moves from lands to oceans via steams & groundwater (water in soil)

  • 0.5% water in lakes, rivers, & groundwater for drinking

  • most groundwater in aquifers

<p>water evaporates out of oceans &amp; precipitates over globe</p><ul><li><p>water moves from lands to oceans via steams &amp; groundwater (water in soil)</p></li><li><p>0.5% water in lakes, rivers, &amp; groundwater for drinking</p></li><li><p>most groundwater in aquifers</p></li></ul><p></p>
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aquifers

layers of porous rock, sand, & gravel saturated with water

  • closed aquifers have nonporous rock layers & take thousands of years to recharge

  • open aquifers can be recharged by water percolating from surface

  • where humans extract freshwater

    • 40% beyond carrying capacity

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water table

upper limit of underground layer of soil saturated with stored water

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global nitrogen cycle

nitrogen added to ecosystems is unusable when reduced or fixed

  • atmospheric (N2) → ammonia (NH3) from lightning-driven reactions & enzyme-catalyzed reactions in bacteria

plants only use fixed nitrogen

adding nitrogen increases productivity

  • too much is harmful

    • nitrogen pollution from burning of fossil fuels → acid rain, climate change, depletion of ozone layer

    • decreased species diversity

    • eutrophication: overfertilization → algal blooms in aquatic ecosystems → oxygen-free dead zones

<p>nitrogen added to ecosystems is unusable when reduced or fixed</p><ul><li><p>atmospheric (N<sub>2</sub>) → ammonia (NH<sub>3</sub>) from lightning-driven reactions &amp; enzyme-catalyzed reactions in bacteria</p></li></ul><p>plants only use fixed nitrogen</p><p>adding nitrogen increases productivity</p><ul><li><p>too much is harmful</p><ul><li><p>nitrogen pollution from burning of fossil fuels → acid rain, climate change, depletion of ozone layer</p></li><li><p>decreased species diversity</p></li><li><p><strong>eutrophication</strong>: overfertilization → algal blooms in aquatic ecosystems → oxygen-free dead zones</p></li></ul></li></ul><p></p>
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global carbon cycle

  • ocean is largest reservoir, atmospheric reservoir is small but important

  • photosynthesis incorporates carbon → tissue

  • cellular respiration releases carbon from living organisms → atmosphere

  • human activities add carbon dioxide to atmosphere

  • burning fossil fuels move carbon from inactive geological reservoir in petroleum or coal form → active reservoir

<ul><li><p>ocean is largest reservoir, atmospheric reservoir is small but important</p></li><li><p>photosynthesis incorporates carbon → tissue</p></li><li><p>cellular respiration releases carbon from living organisms → atmosphere </p></li><li><p>human activities add carbon dioxide to atmosphere</p></li><li><p>burning fossil fuels move carbon from inactive geological reservoir in petroleum or coal form → active reservoir</p></li></ul><p></p>
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humans increase atmospheric carbon dioxide

  • cooking, heat, transportations, building, agriculture, manufacturing

  • energy comes from chemical sources in organic sources (wood, coal, oil, natural gas)

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fossil fuels

vast reservoirs lock inside remains of plants that died mya

  • energy dense

  • easily burned to produce energy

  • collected in vast pockets accessible to us (coal, oil, gas)

  • yield carbon dioxide as waste product of combustion

<p>vast reservoirs lock inside remains of plants that died mya</p><ul><li><p>energy dense</p></li><li><p>easily burned to produce energy</p></li><li><p>collected in vast pockets accessible to us (coal, oil, gas)</p></li><li><p>yield carbon dioxide as waste product of combustion</p></li></ul><p></p>
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greenhouse effect explains atmospheric warming

  • CO2 is greenhouse gas

    • traps heat radiated from earth that would be lost to space

    • can be absorbed by ocean

    • increase in atmospheric CO2

  • greenhouse effect is natural consequence of CO2’s physical properties

    • greenhouse gases include methane (CH4), water vapor, & nitrous oxide (N2O)

<ul><li><p>CO<sub>2</sub> is greenhouse gas</p><ul><li><p>traps heat radiated from earth that would be lost to space</p></li><li><p>can be absorbed by ocean</p></li><li><p>increase in atmospheric CO<sub>2</sub></p></li></ul></li><li><p>greenhouse effect is natural consequence of CO<sub>2</sub>’s physical properties</p><ul><li><p>greenhouse gases include methane (CH<sub>4</sub>), water vapor, &amp; nitrous oxide (N<sub>2</sub>O)</p></li></ul></li></ul><p></p>
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overall rise in atmospheric CO2 & temperature, but not in solar radiation

knowt flashcard image
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continued warming in the future

  • IPCC: 2017 temp exceeded pre-industrial levels by 1 C

    • increases of 1.5 - 2 degrees by 2100

    • 0.5 - 7 by 2300

  • will be past 5 million over next 100 years

temp variation

  • polar regions increase more than tropics

  • ecosystems at same latitudes experience large increases

  • some seasons change more

temp extremes will increase

<ul><li><p>IPCC: 2017 temp exceeded pre-industrial levels by 1 C</p><ul><li><p>increases of 1.5 - 2 degrees by 2100</p></li><li><p>0.5 - 7 by 2300</p></li></ul></li><li><p>will be past 5 million over next 100 years</p></li></ul><p>temp variation</p><ul><li><p>polar regions increase more than tropics</p></li><li><p>ecosystems at same latitudes experience large increases </p></li><li><p>some seasons change more</p></li></ul><p>temp extremes will increase</p><p></p>