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Paleoecology

Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

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Page 1: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Paleoecology

Page 2: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Four Earth Systems

Atmosphere

Lithosphere

Hydrosphere

Biosphere

Page 3: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Organisms interacting with their physical environment

• Limiting factors: determine diversity and abundance in environment

Page 4: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Time out for vocab

• Diversity:• Number of different kinds of organisms (e.g., #

of species, # of families)• Abundance• Number of organisms

Page 5: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Organisms interacting with their physical environment

• Limiting factors: determine diversity and abundance in environment.

• Determine what organisms can live in a given environment

Page 6: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Limiting Factors

• Temperature• Oxygen• Salinity• Depth• Substrate

Page 7: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

• Affects– Physiological rates– CO2 & O2 solubility (⬆Temp, solubility)

– Salt solubility (⬆Temp, solubility)

Temperature

• Determined by latitude, ocean circulation, depth

• Usually stable – most organisms have narrow tolerances

Page 8: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

How does temperature vary

• Increase in latitude:

• Increase in depth:

• Relation to Ocean circulation

Page 9: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://www.nasa.gov/mission_pages/aquarius/multimedia/gallery/pia14786.htmlhttp://www.esrl.noaa.gov/psd/map/clim/sst.shtml

Page 10: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Oxygen

• Affects– Metabolic rates through respiration

• Determined by– Turbulence– Plant production– Biodensity– Decomposition

• Oceans have been typically stratified with respect to oxygen

Page 11: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere
Page 12: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Oceans now and then

• Now: – Global conveyor belt carries oxygenated water

around the world’s oceans

• Then:– Deep water typically anoxic

Page 13: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Cold water falls off the edge of the shallow (oxygenated) Arctic sea, then makes its way

around the bottom of the world’s oceans

Page 14: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Salinity

• Variation– Normal 35 ‰ (parts per thousand)– Greatest variability in near shore environments– Affected by evaporation , precipitation

Page 15: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://www.nasa.gov/mission_pages/aquarius/multimedia/gallery/pia14786.html

Page 16: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Salinity

• Tolerances– Most organisms have narrow tolerances• Osmotic pressure

– Exceptions: oysters, mussels, snails, some crustaceans

Page 17: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Depth

• 3 intertwined variables– Light

• Photic zone to 200 m in open ocean, much less closer to land• Surface ecosystems based on primary producers• Bottom ecosystems based on material drifting down

– Pressure– Carbonate Compensation Depth (CCD): below 3000-

4000 ft., water is undersaturated with CO2 – calcite & aragonite skeletons dissolve

Page 18: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Substrate

• Organisms specialize for specific substrates– Rocky: attached filter feeders, borers, grazers,

mobile & immobile predators– Mud: deposit feeders, other infauna– Sand: mobile filter feeders and predators, few

grazers or deposit feeders

Page 19: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Understanding common environments

• Rocky intertidal – between high and low tides• Muddy intertidal – tide flats• Sandy subtidal – below wave base, shallow

water

Page 20: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere
Page 21: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Work on your environmentEnvironment Rocky intertidal Muddy intertidal Sandy subtidal

Temperature Varies, hot to cool Varies, warm Constant, normal

Oxygen Varies, high when tide is up

Varies, high to low Constant, medium

Salinity Varies, evaporation in pools, rain

Varies, evaporation, rain

Constant, normal

Depth Well lit,High energy

Well lit,Low energy

Lit, depends on sediment input, lowish

Substrate hardground muddy Sand – it moves

Adaptations Holdfasts, cement themselves down, cover themselves up, trap a bit of water, tough cuticle, borers,

Infaunal, deposit feeders, filter feeder, burrowing, trap water in burrows, salinity adaptations

Mobile, epifaunal, fewer deposit feeder, snowshoes, filter feeders

Page 22: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Water Masses

• Oceans are divided into surprisingly stable masses of water with relatively uniform temperature & salinity conditions

• Properties of a water mass are determined by latitude and circulation patterns

• Results in Biotic Provinces

Page 23: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://pubs.usgs.gov/of/2010/1251/figure3.html

Page 24: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://geology.cnsm.ad.csulb.edu/people/bperry/geology303/geol303text.html

Page 25: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Disrupted by cyclic

perturbations

http://sealevel.jpl.nasa.gov/science/elninopdo/learnmoreninonina/

El Nino: warm water flows W to E

across Pacific

La Nina: persistent cold water in

tropical latitudes

Page 26: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Biological environment

• Competition: organisms compete for same resource– Food– Space– Light

• Think of examples from our field trip

Page 27: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Biological environment

• Interference competition:– Organisms aren’t directly competing, but their use

of the environment interferes with each other– E.g. Humans & habitat disruption (freeways)– Biologic bulldozers

Page 28: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Biological Environment

• Predation & parasitism– Eliminates some species from some environments– Evidence in fossil record• Shell breakage• Teeth holes

Page 29: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://www.ucmp.berkeley.edu/about/flat_stanley07.php

Page 30: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

Symbiosis

• Organisms live together• Mutualism – for mutual benefit– Zooxanthellae

Page 31: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

How does mutualism evolve?

• One example:– Some nudibranchs retain zooxanthellae from the

coral that they eat.– Gut has transparent pockets that hold the

chloroplasts from the algae– If the nudibranch retains the entire algae and the

algae is able to reproduce: mutualism– Natural selection could drive the nudibranch to

provide algae a safe place to live

Page 32: Paleoecology. Four Earth Systems Atmosphere Lithosphere Hydrosphere Biosphere

http://www.seaslugforum.net/solarpow.htm

This nudibranch has lived 10 months without food in the lab, using the chloroplasts it took from the algae to photosynthesize and make sugars.

This nudibranch keeps living algae in its tissues.