Mass extinctions Flashcards

1
Q

Background rate of extinction

A

average number of FAMILIES (easier to tell apart) going extinct, figure it out by examining the fossil record (limits in the fossil record)

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2
Q

Chronospecies

A

single species changing morphologically, genetically, or ecologically over a long time scale- identify them as a separate species

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3
Q

Psuedoextinction

A

when a species is presumed extinct but has actually just become a different species

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4
Q

Rates of extinction

A

historically, 0.1/ million/ year

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5
Q

Biotic mechanisms of extinction

A

competitive exclusion by a closely related species, prey species develops unbeatable defense, new predator, disease

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6
Q

evolutionary causes for extinction vulnerability

A

poor disperser, at or near the top of the food chain, small range, rare, low genetic variability, specialized requirements, large body size

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7
Q

abiotic mechanisms of extinction

A

niche/habitat no longer supports species, climate fluctuations, sea level change, meteorites, volcanism

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8
Q

Mass extinction

A

extinction of a large number of unrelated species over a short period of geological time- global distribution

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9
Q

similarities of background and mass extinction

A

can both have multiple causes, both change evolutionary history

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10
Q

difference of background and mass extinction

A

different outcomes, mass extinctions= whole communities removed, previously minor species become dominant- fundamental changes

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11
Q
  1. End Ordovician mass extinction
A

49% animal genera lost- marine organisms suffered most, caused by: volcanic activity depositing silicate materials- CO2 in air deposited in sea, less CO2 in atmosphere and less greenhouse effect- colder, & land moves to the south pole- glacier formation- less water in oceans

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12
Q
  1. Late Devonian
A

20% of families, 70-80% of animal species lost, shallow water species impacted- dominant reef builders lost, unusually long, no single cause, combination of silicate weathering cooling globe and phosphorus erosion

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13
Q

Devonian plant hypothesis

A

large number of plants led to global cooling and lack of oxygen in oceans, CO2 in atmosphere combines with water to form carbonic acid- falls as acid rain and weathers silicates- bicarbonate erodes and ends up in ocean- CO2 in atmosphere sequestered as limestone in ocean- sped up by plants- break apart rocks and also secrete own acids

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14
Q

Formation of dead zones

A

chemical weathering of rocks by plants releases phosphorus- erodes to ocean, leads to algal blooms- algae dies and drifts down- bacteria uses oxygen to break down algae- low oxygen levels in that area

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15
Q
  1. End Permian
A

“the great dying”- 70% terrestrial vertebrates 96% marine species lost- all life today descendants of the few survivors here; causes- series of massive volcanic eruptions- release CO2, methane, SO2 and burned coal deposits- global warming; lost half of oxygen content; ocean salinity increased- deep water circulation more difficult; buildup of dead matter and dead zones

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16
Q
  1. End Triassic
A

76% species extinct- left empty niches on land led to rapid diversification of dinosaurs; no clear cause: gradual climate change; more minor asteroid impact; massive volcanic eruption

17
Q
  1. End Cretaceous
A

75% plant and animals species extinct- only smaller tetrapods survived, end of dinosaurs, followed by rise of mammals - rapid adaptive radiation; causes: impact hypothesis massive bolide impact, threw cloud of particles into atmosphere- global winter- interfered with photosynthesis by blocking sunlight; proof of impact in crater and iridium sediment buildup in rock layers; Deccan Traps (india)- massive basalt floods produced similar effect as previously with volcanic activity; both contributed

18
Q

Press-pulse hypothesis

A

first even stresses environment, second even then occurs and causes a greater-than-expected impact

19
Q

Sixth Mass Extinction

A

human impact, high rate of extinction- fast

20
Q

Planned extinction

A

directed human efforts to drive species to extinction- “pest” species