final exam Flashcards

prepare for exam (57 cards)

1
Q

When did the Earth form?

A

4600 million years ago (Ma)

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2
Q

When did the Phanerozoic Eon begin?

A

541 Ma

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3
Q

When did the Paleozoic Era end?

A

252 Ma

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4
Q

When did the Mesozoic Era end (and dinosaurs go extinct)?

A

66 Ma

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5
Q

What are the four main Eons, in order?

A

Hadean, Archean, Proterozoic, Phanerozoic

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6
Q

Which Eon is when life with hard parts first appeared?

A

Phanerozoic

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7
Q

What Eon was Earth a molten mess?

A

Hadean

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8
Q

During which Eon did the first simple life appear?

A

Archean

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9
Q

During which Eon did oxygen start building up?

A

Proterozoic

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10
Q

What are the 3 Eras of the Phanerozoic, in order?

A

Paleozoic, Mesozoic, Cenozoic

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11
Q

What Era was the “Age of Fishes” and land plants?

A

Paleozoic

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12
Q

What Era is known as the “Age of Dinosaurs”?

A

Mesozoic

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13
Q

What Era is known as the “Age of Mammals”?

A

Cenozoic

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14
Q

What are the 12 Periods of the Phanerozoic in order?

A

Cambrian, Ordovician, Silurian, Devonian, Carboniferous, Permian, Triassic, Jurassic, Cretaceous, Paleogene, Neogene, Quaternary

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15
Q

Mnemonic to remember the 12 periods?

A

“Come Over Some Day, Can People Try Juicing Cold Pineapple Now Quickly?”

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16
Q

Which Period did the Cambrian Explosion happen in?

A

Cambrian

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17
Q

Which Period ended with the biggest mass extinction?

A

Permian

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18
Q

Which Period did the dinosaurs go extinct?

A

Cretaceous

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19
Q

Paleozoic:

A

Cambrian, ordovician, silurian, Devonian, Carboniferous, permian

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20
Q

mesozoic:

A

Triassic, jurassic, cretaceous

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21
Q

Cenozoic:

A

paleogene, neogene, quaternary

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22
Q

Element:

A

A substance made of one type of atom, defined by the number of protons in its nucleus.

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23
Q

Radioactive Decay:

A

The process by which unstable atomic nuclei lose energy by emitting radiation, leading to a change in the number of protons or neutrons, transforming the element into another.

24
Q

Radioisotope Half-Life:

A

The time it takes for half of a sample of a radioactive isotope to decay.

25
Parent-Daughter Isotope Ratio:
Used in radiometric dating to calculate the age of rocks. The ratio of parent isotopes (unstable) to daughter isotopes (stable) reveals the amount of time that has passed since the rock formed.
26
Uranium-Lead (U/Pb) Decay:
Used to date zircon crystals in igneous rocks and volcanic ash beds. The half-life of 238U is 4.5 billion years.
27
Clair Patterson:
A scientist who used uranium-lead decay to determine the age of Earth, which is about 4.6 billion years. Patterson also worked to reduce lead contamination in the environment.
28
Oldest Zircon Crystals:
The oldest known zircon crystals date back to 4.4 billion years ago.
29
Radiocarbon Materials:
Only organic materials like wood, bone, and shell can be used for radiocarbon dating.
30
Radiocarbon Dating:
Uses 14C and is effective for dating organic materials up to about 50,000 years ago. It differs from other radioisotopes in that it has a short half-life and is mainly used for dating younger fossils and rocks.
31
Early Earth Atmosphere (Archean):
Composed mainly of carbon dioxide, water vapor, methane, and ammonia.
32
Miller-Urey Experiments:
These experiments simulated early Earth conditions and showed that organic compounds (like amino acids) could be formed from inorganic precursors.
33
Murchison Meteorite:
A meteorite that contains amino acids, suggesting that the "stuff of life" might have come from space.
34
RNA as Original Genetic Code:
Scientists believe RNA was the original genetic code because ribozymes (RNA molecules) can self-replicate, which is a key function in life.
35
Molecular Phylogeny:
Helps us understand where life may have originated, such as in deep-sea hydrothermal vents.
36
Stromatolites:
Layered rock structures formed by cyanobacteria, some of the oldest fossils on Earth (around 3.5 billion years old). They perform oxygenic photosynthesis.
37
Great Oxygenation Event (GOE):
The period around 2.4 billion years ago when oxygen levels in Earth's atmosphere significantly increased due to photosynthesis by cyanobacteria.
38
Ediacara Fauna:
The first known multicellular animals (metazoans) from around 600 million years ago.
39
Great Unconformity:
A gap in the rock record, thought to relate to changes in seawater chemistry and helped trigger the Cambrian Explosion.
40
Cambrian Explosion:
The rapid diversification of marine life during the Cambrian Period around 541 million years ago, marked by the appearance of animals with hard shells.
41
Evolution of Land Plants:Ordovician
First primitive land plants, like mosses.
42
Evolution of Land Plants:Silurian
Simple vascular plants.
43
Evolution of Land Plants:Devonian
First forests made of lycopods (seedless vascular plants) and the appearance of primitive gymnosperms.
44
Age of Coal (Carboniferous):
Land plants, particularly lycopods, dominated. This period saw the burial of large amounts of organic carbon, which lowered atmospheric CO2 levels and contributed to a cooler climate.
45
Devonian Period - Age of Fishes:
First jawed fishes appear, along with lobe-finned fishes, which eventually gave rise to tetrapods.
46
Tetrapod Evolution:
Early amphibians evolved from lobe-finned fishes (like Ichthyostega) in the Devonian.
47
Great Dying (Permo-Triassic Extinction):
Occurred around 252 million years ago, marking the end of the Paleozoic Era. The largest mass extinction in Earth's history, caused by volcanic activity (Siberian Traps) and CO2 release, leading to global warming, ocean acidification, and deoxygenation.
48
Amniotic Egg:
An important evolutionary step for reptiles, allowing them to reproduce on land without water.
49
Dinosaurs:
First appeared during the Triassic Period and evolved into the dominant terrestrial vertebrates. The key characteristic of dinosaurs is the mesotarsal joint in the ankle.
50
Pterosaurs
Flying reptiles that coexisted with dinosaurs, also possessing the mesotarsal joint.
51
Archaeopteryx:
A transitional fossil showing both dinosaurian and avian features, linking birds to dinosaurs.
52
Chicxulub Impact:
Evidence suggests an asteroid impact caused the end-Cretaceous mass extinction around 66 million years ago, leading to the extinction of the dinosaurs. Key evidence includes the Iridium Anomaly and the Chicxulub crater in Mexico.
53
Sahelanthropus:
One of the earliest known hominins, about 6-7 million years ago, showing evidence of upright bipedalism.
54
Australopithecines:
Early bipeds with small brains, like Lucy (Australopithecus afarensis) from around 3.6 million years ago.
55
Homo habilis:
The first species of the genus Homo, emerging around 2.5 million years ago.
56
Brain Size Cutoff:
600 cubic centimeters separates Australopithecus from the genus Homo.
57