Chapter 57 - Workforce3One
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Transcript Chapter 57 - Workforce3One
Chapter 57
Dynamics of ecosystems
What are Biogeochemical Cycles?
• Earth has fixed number of each type of atoms of
biological importance –recycled via biogeochemical
cycles
• Biogeochemical cycles- The atoms of various
chemical elements move through ecosystems –
involve biological organisms and processes +
geological (abiotic) systems and processes.
• Biogeochemical cycles includes processes that occur
on many spatial (cellular to planetary) and multiple
timescales from seconds (biochemical reactions) to
millennia (weathering of rocks)
Carbon cycle
• Figure 57.1-Photosynthesis by plants and algae
capture carbon in form of organic chemical
compounds (Co2 and HCO3-)
• Cellular respiration and combustion of fuels
return carbon to atmosphere (Co2 or HCO3-)
• Microbial methanogens (live in bottom of
water) – produce CH3 ---enter into atmosphere
as Co2.
• Decaying organisms also produce Co2
The water cycle-figure 57.2
• Water is a compound – Synthesized during cellular
respiration and broken during photosynthesis
• Enters atmosphere via evaporation (water resources
and plant) and transpiration (plant) and returns to
earth’s surface as precipitation
• Groundwater (available in oceans, lakes etc)
• Underground layers of rocks, sand and gravel
saturated with water – aquifers
• Aquifers are used and contaminated by humans
The Nitrogen cycle (figure 57.4)
• Plants and animals cannot use nitrogen (elemental
form) directly from atmosphere
• Nitrogen fixation- Synthesis of NH3 from N2
• Nitrification- Synthesis of NO3- from NH3
• Plants and algae utilize NH3 and NO3• Denitrification - some prokaryotes return back NH3
and NO3- as N2 to atmosphere
• Human and mammal excreta – Urea---converted to
NH3---- used by plants and algae
• Fertilizer application of N2- doubled the rate of
N2 transfer
Phosphorous cycle (figure 57.5)
• Phosphorous has no gaseous form – do not cycle through the
atmosphere
• Available in ecosystem – inorganic phosphate (PO4-)
• Released by weathering of rocks and it flows into oceans
where it is deposited in deep-sea sediments
• Plant and algae use PO4- present in soil or water
• Animals tap PO4- from plants and algae
• Remineralization- Decaying microbes break up organic
compounds in bodies of dead organisms- release as inorganic
PO4- plants and algae can reuse it
• Application of phosphorous fertilizers to soils
Energy flows through trophic levels
• Organic compounds are synthesized by
autotrophs – photoautotrophs and
chemoautotrophs – and utilized by
heterotrophs
• Energy passes from organism to organism,
each feeding level is called a trophic level,
and sequence through progressive trophic
levels – Food chain (figure 57.8)
Trophic levels
• Primary producers-Herbivores-Primary
carnivores-secondary carnivores-Detritivores
• Detritivores feed on dead matter of all other
tropic levels
• Detrius – dead organic matter
• Decomposers – subcategory of detritivores
Productivity
• Productivity of atrophic level is the rate at which the
organisms in trophic level are collectively synthesizing new
organic matter
• Primary productivity of autotrophs can be expressed as
Gross primary productivity (GPP) and Net primary
productivity (NPP)
• GPP – the rate at which the primary producers synthesize new
organic matter
• NPP= GPP - respiration of primary producers
• Productivity of a heterotroph tropic level – secondary
productivity
How trophic levels process energy?
• 1% of solar energy is captured for photosynthetic
processes.
• Most of the chemical bond energy ingested (figure
57.9 and 57.10) is lost in feces
• Some of the ingested energy is lost in fuelling
respiration
• Only some amount of ingested energy is used by the
animal (heterotroph or autotroph)
• In general, only about 10% of the energy of one
trophic level is available to the next trophic level
Ecological pyramids
• Ecological pyramids of energy flow, biomass
or numbers are upright.
• Happens when one trophic level has greater
biomass or more number of organisms than
trophic level below it (figure 57.13)
What are Trophic-Level Interactions
• Changes in species at any one trophic level may have
multiple effects on other trophic levels
• A trophic-cascade occurs when effects exerted at an
upper trophic level affect a lower level
• Top-down trophic effect occurs when changes in top
trophic level affect primary producers
• Bottom-up effect occurs when changes in primary
productivity affects higher trophic levels
• Species richness affect community stability –
community’s composition and ability to resist
disturbance
Island Biogeography
• Species area relationship can be explained by
colonization and extinction of species
(populating a geographic area or isolating)
• Smaller islands have fewer species than
large islands because of higher rates of
extinction
• Near islands have more species than far
islands because of higher rates of
colonization
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