The History of Life: Flashcards

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1
Q

One group of O2 generating bacterias, the __________, formed rock-like structures called __________, which are abundantly preserved in the fossil record.

A
  • Cyanobacteria

- Stromatolites

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2
Q

T/F: When O2 first appeared in the atmosphere, it was poisonous to most of the anaerobic prokaryotes that inhibited Earth at the time.

A

TRUE

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3
Q

Aerobic metabolism:

A

proceeds more rapidly, and harvests energy more efficiently, than anaerobic metabolism.

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4
Q

Further increases in atmospheric O2 concentrations in the late _______ enabled several groups of multicellular organisms to evolve.

A

Precambrian

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5
Q

The high concentrations of atmospheric O2 allowed the evolution of what?

A

giant flying insects and amphibians that could not survive in today’s atmosphere

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6
Q

The drying of the lowland swamps at the end of the _______ rapidly decreased the O2 concentration.

A

Permian

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7
Q

Biologists refer to the assemblage of all organisms of all kinds living at a particular time or place as a __________.

A

Biota

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8
Q

All of the plants living at a particular time or place are called its ______________; all of these animals are its ____________.

A

Flora………Fauna

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9
Q

Geologist divided earth’s history into eras and periods based on what ?

A

On their distinct fossil assemblages.

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10
Q

Multicellular life was largely or completely aquatic during the ___________.

A

Cambrian

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11
Q

What are evolutionary radiations?

A

Periods of such rapid diversification.

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12
Q

Why was there a Mass extinction toward the end of the Permian (about 250 MYA)?

A

Massive volcanic eruptions sent out debris which blocked sunlight and cooled the climate, resulting in the largest glaciers in Earths history.
Atmospheric Oxygen dropped by half, so animals couldn’t survive. Thus killing off about 96 percent of all multicellular species.

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13
Q

During the Jurassic period, Pangaea became fully divided into two large continents:

A

Laurasia (which drifted northward) and Gondwana (drifted Southward)

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14
Q

When did Laurasia and Gondwana begin to break apart into the continents we know today?

A

By the early Cretaceous (145-65 MYA)

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15
Q

We are living in the ______ period.

A

The Quaternary

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16
Q

What are the principles of stratigraphy:

A
  • Fossils of similar organisms are found in widely separated places on Earth
  • Certain fossils are always found in younger strata, and certain other fossils are always found in older strata
  • Organisms found in younger strata are more similar to modern organisms than are those found in older strata
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17
Q

What happens in the Half-life?

A
  • Half of the atoms in a radioisotope decay to become a different, stable (nonradioactive) isotope.
  • We use this to date fossils
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18
Q

Radiometric dating:

A
  • uses radioisotopes of carbon to date fossils

- Can date fossils that are less than 60,000 years old.

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19
Q

The history of life is divided into ________, which in return are subdivided into __________.

A

Eras…….Periods

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20
Q

What is continental Drift?

A

The movement of the lithospheric plates and the continents they carry

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21
Q

Why is continental Drift caused?

A

It is caused by convection currents in the magma, which move the plates and the continents that lie on top of them.

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22
Q

The position and sizes of the continents influence:

A
  • Oceanic circulation Patterns
  • Global Climates
  • Sea levels (influenced directly by plate tectonics)
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23
Q

T/F: Most mass extinctions of marine organisms have coincided with low sea levels.

A

True

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24
Q

How have volcanoes occasionally changed the history of life?

A

The collision of the continents 275 MYA, (during the Permian Period) formed a single land mass, causing a multitude of massive volcanic eruptions. Emissions from these eruptions blocked alot of sunlight,, creating the advance of glaciers and causing a drop in seal level.
-(responsible for playing part in our greatest mass extinction)

25
Q

A meteorite caused/contributed to a mass extinction when? And How do we know this to be true?

A
  • Occurred at the end of the Cretaceous Period (about 65 MYA)
  • There’s high concentration of Iridium found in rocks deposited during the Cretaceous
  • Scientists discover a circular crater, 180 km in diameter, buried beneath the Yucatan Peninsula of Mexico.
26
Q

What are the prevailing hypotheses about the cause of the mass extinction event (65 MYA)?

A

-Possibilities of Mass Extinction at the end of the Cretaceous:
1- Primary Explanation——> Crater hitting Earth
2- Climate cools during late Cretaceous due to Continental drift.
3- Spike in Volcanic activity (in India)

27
Q

The fossil record indicates that after Earth’s major mass extinction events, there is a great increase in biodiversity. Explain why an increase in biodiversity occurs after these mass extinctions:

A

-There’s an increase in biodiversity because of those organisms which survived (maybe a predator was killed off).

28
Q

The beginning of the Cambrian Period is marked in the fossil record by the “Cambrian Explosion.” What is meant by the “Cambrian Explosion?”

A
  • *(Occurring about 542 MYA)
  • Rapid increase of multicellular organisms
  • Lots and lots of animals and multicellular organisms fossils have been found here
  • It began before the Cambrian and the “explosion” took millions of years.
  • Multicellular life was largely or completely aquatic during this time (Cambrian)–If there was life on land, it probably was restricted to micro-organisms.
29
Q

What are the geological consequences of the movement of the continental plates? What have been the biological consequences of the movement of the continental plates?

A
  • In response to plate tectonic processes such as continental drift and volcanic activity
  • Movement of plates have brought continents together at times and apart at other times.
  • Some of these dramatic changes in Earth’s physical parameters resulted in mass extinctions
30
Q

In the geological time scale, what events determine the end of one era and the beginning of another?

A

the Geological time scale has Era’s which are broken down into periods, the end of an Era, shows a mass extinction occurred.

31
Q

What is the principle behind radiometric dating of fossils?

A

It uses radioisotopes to determine an absolute date (since carbon 14 decays over time)
-We can also use Half-life for these radioisotopes

32
Q

What is the accuracy rate of radiometric dating technique?

A
  • C-14 dating is accurate for young fossils, however with older fossils, us of other radioisotopes will be needed
  • It has an accuracy of (plus or minus)+- 10%
33
Q

Why is fossilization rare?

A
  • It’s because whatever is being fossilized has to die, being covered by sediments, and it also has to escape destruction by heat, pressure, and erosion.
  • this is why the fossil record is incomplete.
34
Q

what are the Characteristics of organisms (species) that have left the best fossils?

A
  • They existed for a long time
  • They were abundant
  • they had large geographic ranges
  • They had hard parts (such as shells and skeletons)
35
Q

Who proposed the concept of continental drift? and in what decade?

A

German Meteorologist, Alfred Wegner in 1912

36
Q

In what decade had scientists collected enough evidence to confirm that continental rift was a real phenomenon?

A
  • In the 1960’s, evidence from geology, paleontology, and biology confirmed Wegner’s idea on continental drift
  • By 1960’s physical evidence and increased understanding of plate tectonics.
37
Q

What mass extinctions occurred around 250 MYA (at the time Pangaea was believed to have existed)? Explain the role of climate change in this mass extinction event.

A
  • Extinction of 96% of Earth’s species
  • Oxygen levels drop rapidly (from 30% to 15%)
  • (the Permian Extinction: which involved considerable loss of insect diversity!)
38
Q

What mass extinctions occurred 65 MYA? Explain the role of climate change in this mass extinction?

A
  • “The Cretaceous Extinctions”, mass extinction event, including the loss of the dinosaurs (most of them)
  • Caused by the Iridium that was sent out, after a giant asteroid known as the “Chicxulub Crater”
  • Modern continents were beginning to take shape
  • The climate cools due to continental drift and spike in volcanic activity (In India)
39
Q

Explain how the stratification of sedimentary rock can be used as a relative time scale for age of the fossils imbedded within it:

A

Because over time the sediments get covered, what is found on top, is relatively new, vice versa

40
Q

Paleozoic Era:

A
  • meaning “ancient animal”
  • sudden diversity of animals
  • Establishment of terrestrial animals/plants
  • –[Then mass extinction occurs]
41
Q

Mesozoic Era:

A
  • meaning “middle animal”
  • The age of reptiles
  • Mammals angiosperms
  • –[Mass extinction/Dino’s died off]
42
Q

Cenozoic Era:

A
  • meaning “recent animal”

- mammals, birds which remain now, angiosperm

43
Q

Pangaea:

A

All land masses together about 250 MYA

44
Q

Around 250 MYA (Paleozoic era)

A
  • Species evolving in isolation now together
  • loss of coastlines (90% marine lie died)
  • Ocean basins deeper, drainage of shallow coastal areas
  • Mass extinction
45
Q

The Permian Extinctions:

A
  • 90% of marine species extinct
  • terrestrial species impacted heavily
  • change of ocean currents—-> cool, dry, interior
46
Q

Laurasia and Gondwana:

A
  • Starts about 180 MYA in Mesozoic Era
  • Split into Northern and Southern land masses
  • Species evolving in isolation again (allopatric isolation)
47
Q

Modern continents begin to take shape:

A

Starting about 65 MYA

48
Q

Crash of the Indian Plate into Eurasia Plate:

A
  • Starts about 10 MYA

- forms the Himalayas

49
Q

What is Bio-geography?

A

The distribution of organisms on the planet

50
Q

Formation of Earth:

A

About 4.6 BYA

51
Q

First oceans:

A

About 3.8 BYA

52
Q

Origin of Life:

A

About 3.5 BYA

53
Q

Origin of Photosynthesis:

A

About 2.8 BYA

54
Q

First Eukaryotic Cells:

A

About 1.5 BYA

55
Q

About 542 MYA:

A

-Rapid increase of multicellular organisms aka “the Cambrian explosion”

56
Q

About 420 MYA:

A

-first vascular plants and terrestrial anthropods evolve (bugs/insects)

57
Q

About 65 MYA:

A
  • “The Cretaceous Extinctions”
  • Mass extinction event: loss of the dinos
  • Chicxulub Crater hit and sent Iridium out

-@ the end of the Cretaceous-Tertiary (K/T boundary)

58
Q

At the end of the Cretaceous we go to the Tertiary were:

A
  • There are flowering plants that are dominant on land
  • Rapid radiation of mammels
  • Increase in biodiversity