Chapter 12 Flashcards

1
Q

What are extant species

A
  • species that are still present today

- species whose members died off are called extinct species

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2
Q

What are the five major mass extinctions that paleontologists recognize

A
  • End of Ordovician
  • Late Devonian
  • End Permian
  • End Triassic
  • End of Cretaceous
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3
Q

Which animals went extinct in the end of Ordovician

A
  • mainly marine invertebrates

- >at that time, terrestrial organisms only had begun to evolve

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4
Q

Which animals went extinct in the late Devonian

A

-marine invertebrates and some early vertebrate clades

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5
Q

Which animals went extinct in the End Permian

A

-marine invertebrates, insects, synapsids and anapsids

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6
Q

Which animals went extinct in the end of Triassic

A

-marine organisms and pseudosachians

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7
Q

Which animals went extinct in the end of the cretaceous

A

-marine invertebrates, marine reptiles, pterosaurs, dinosaurs and birds

  • land plants also lost many species and insect diversity fells
  • killed all non-avian dinosaurs
  • marine diapsids called mosasaurs and plesiosaurs died out
  • so did many varieties of corals, plankton and ammonites(squids and octopi)
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8
Q

Did mammals, turtles, corcodiles, amphibians and fish make it through the End-Cretaceous Extinction

A
  • yes
  • > although many of the larger species in these groups did not
  • it seems like large animals and photosynthetic organisms were the most likely to die off
  • > small animals and those that are semiaquatic had the best chance of surviving
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9
Q

Are all animals that survived the end cretaceous extinction around today?

A
  • no
  • > eg; champsosaurs are a good example
  • > they were crocodile like aquatic diapsids
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10
Q

Name some recent extinctions

A
  • Tasmanian tiger
  • passenger pigeon
  • the Carolina parakeet

-extinction of these species was the result of intense hunting and habitat loss

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11
Q

Are scientists predicting a sixth mass extinction event currently

A
  • yes
  • > the new mass extinction is being brought about by sudden global climactic change and large-scale ecosystem destruction and degradation
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12
Q

What is iridum

A
  • it is a rare element on earth

- >a common component of meteorites

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13
Q

What are tektites and shocked quartz

A

Tektites
->tiny pieces of rock that have been melted and cooled

Shocked Quartz

  • > form of mineral quats with a unique internal structure
  • > can only be created by a power exposure ot a shockwave
  • > like those created by a meteorite impact
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14
Q

Have scientists found a thin layer of grey clay between the Cretaceous and Paleogene boundary?

A
  • yes
  • > it is made up of iridum, tektites and shocked quartz
  • all three being present all over the globe would have required an enormous shower of large meteorites or a single tremendous meteroirite impact
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15
Q

What are cenotes

A

-they are limestone sinkholes

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16
Q

What did geologists in Mexico’s Yucatan Peninsula find

A
  • there were cenotes arranged in crescent shapes many miles long
  • each end of the crescent seemed to terminate at the end of the peninsula
  • > however, it was foundd that the cenotes did not actually terminate at the end of the peninsula but were pushed up
  • > it actually continued along the ocean floor and was a huge continuous ring over 180 km in diameter
  • note based on the crater’s size, it has been calculated that the meteorite made must have been 10 kilometres in diameter
  • > larger than Mount Everest
17
Q

Could the ice age have been responsible for the end Cretaceous extinction

A
  • the Cretaceous period was followed by an ice age
  • > while average global temperatures did fall after the Cretaceous, this temperature fall was gradual
  • > and it was million of years before a true ice age resulted
18
Q

What is the current prevailing theory for the cause of the End-Cretaceous extinction

A
  • the cause is more cosmic
  • > without a doubt, very large meteorite struck the Earth in the Yucatan peninsula at about the same time we see a mass extinction in the fossil record
  • the initial impact caused huge tsunamis and sent a great cloud of super-heated rock and dust high into the atmosphere
  • > the rocks and large pieces of debris quickly fell to the Earth and started wildfires
  • > smaller pieces of debris next began to fall and as they did, they were heated by air friction
  • > this hot dust raised global temperatures for hours after impact and cooked alive animals that were too large to seek shelter
19
Q

How did the residual haze after meteor impact photosynthetic plants

A
  • the residual haze would have reduced sunlight
  • > killing many photosynthetic organisms
  • > some scientists predicts that photosynthesis may have stopped for a decade
  • the reduced sunlight may also have brought on a sudden drop in global temperatures
  • > large active animals with high energy needs were highly susceptible to these catastrophes
  • note smaller omnivorous terrestrial animals like mammals, lizards, turtles or birds may have been able to survive as scavengers
  • > feeding on the carcasses of dead dinosaurs, fungi, rotts and decaying plant matter

-smaller animals with lower metabolism were best able to wait the disaster out

20
Q

Is there a chance that a complete or a nearly complete DNA strand of a dinosaur could be preserved

A
  • not very likely
  • > as DNA is a delicate substance and quickly breaks down over time

-even if DNA was found intact, cloning is a difficult process

21
Q

Can current birds DNA be used to created dinosaurs

A
  • it has been proposed that a dinosaur could be resurrected by hatching a bird with its advanced DNA sequences turned off and its ancient ancestral sequences turned back on
  • > for the moment, performing such genetic manipulations as well is beyond our understanding and technology