Lecture 14 Flashcards

1
Q

Deep Time

A

The concept of geologic time, spanning billions of years, which includes the formation of Earth, the evolution of life, and the development of modern ecosystems.

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2
Q

Geological Time Scale

A

A system of chronological dating that divides Earth’s history into eons, eras, periods, epochs, and ages.

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3
Q

Cenozoic Epochs

A

The epochs most relevant to human evolution: Paleocene, Eocene, Oligocene, Miocene, Pliocene, Pleistocene, Holocene, and the proposed Anthropocene.

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4
Q

Cynodonts

A

Small, mammal-like reptiles that evolved into the first true mammals during the Mesozoic era.

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5
Q

K-Pg Extinction Event

A

The Cretaceous-Paleogene extinction event (66 Ma) that wiped out the dinosaurs, opening ecological niches for mammals, including primates.

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6
Q

Plate Tectonics

A

The theory that Earth’s lithosphere is divided into plates that move and interact, influencing climate, ecosystems, and the distribution of continents and oceans.

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7
Q

Continental Drift

A

The gradual movement of continents across Earth’s surface, driven by plate tectonics.

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8
Q

Paleocene-Eocene Thermal Maximum (PETM)

A

A period of rapid global warming around 56 million years ago, coinciding with the origin of crown primates.

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9
Q

Antarctic Circumpolar Current

A

An ocean current that formed around 30 Ma, isolating Antarctica and leading to greater global temperature differences.

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10
Q

East African Rift Valley

A

A prominent example of continental rifting, which created diverse habitats and played a key role in human evolution.

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11
Q

Milankovitch Cycles

A

Long-term changes in Earth’s orbit and tilt that drive climate fluctuations. Includes eccentricity, obliquity, and precession.

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12
Q

Eccentricity

A

Changes in the shape of Earth’s orbit around the Sun, occurring on a ~100,000-year cycle.

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13
Q

Obliquity

A

Changes in Earth’s axial tilt, varying between 22.2° and 24.5°, occurring on a ~41,000-year cycle.

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14
Q

Precession

A

The wobble in Earth’s rotational axis, occurring on a ~26,000-year cycle, affecting the relationship between Earth’s tilt and eccentricity.

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15
Q

Glaciation

A

The formation and movement of glaciers, which significantly impact global climate and sea levels.

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16
Q

Oxygen Isotopes

A

Used to track past climate changes. Oxygen-16 is lighter and more common in glacial ice, while Oxygen-18 is heavier and more common in ocean water during glacial periods.

17
Q

Interglacial Periods

A

Warm periods between glacial periods when glaciers retreat and sea levels rise.

18
Q

Glacial Periods

A

Cold periods when glaciers advance, trapping lighter oxygen isotopes and lowering sea levels.

19
Q

Paleocene Primates

A

Early primates that evolved after the K-Pg extinction, including plesiadapiforms.

20
Q

Crown Primates

A

The group of primates that includes all living primates and their common ancestor, originating during the PETM.

21
Q

Crown Anthropoids

A

The group of primates that includes monkeys, apes, and humans, originating around 30 Ma.

22
Q

Crown Hominoids

A

The group of primates that includes all apes (lesser apes, great apes, and humans), originating around 20 Ma.

23
Q

Hominins

A

The group of primates on the human lineage, including Homo, Australopithecus, and others, originating around 5-7 Ma.

24
Q

Messinian Salinity Crisis

A

A period around 5.96–5.33 Ma when the Mediterranean Sea nearly dried up, leading to significant climate and ecological changes.

25
Q

Genus Homo

A

The genus to which modern humans belong, originating around 2.5 Ma during the onset of modern glaciation.

26
Q

Faunal Interchange

A

The exchange of species between continents, such as when Africa collided with Eurasia around 20 Ma, leading to the migration of species between the two landmasses.

27
Q

Uplift of Eastern African Highlands

A

The geological uplift that blocked humid Indian Ocean air, leading to drier conditions in Africa and the formation of savannas, which influenced human evolution.

28
Q

Anthropocene

A

A proposed epoch marking significant human impact on Earth’s geology and ecosystems, beginning around the Industrial Revolution.