History of Earth & Human Society: Biodiversity and Climate Trends

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This flashcard set covers the geological history of Earth's biodiversity, major mass extinction events, the carbon cycle, and the impacts of human-induced climate change.

Last updated 7:44 PM on 4/29/26
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17 Terms

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Ediacaran fossils

Simple-shaped Macroscopic fossils of organisms thought to be animals that first appear in rocks deposited approximately 565565 million years ago.

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Cambrian Explosion

A period occurring from 541โˆ’520541-520 MYA characterized by the rapid diversification of aquatic life and the appearance of most modern body plans.

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Biomineralization

A key innovation during the Cambrian period involving the development of hard parts such as skeletons made of silica, calcium carbonate, and calcium phosphate.

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Substrate Revolution

The shift toward active burrowing by marine organisms that occurred during the Cambrian Explosion.

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Tiktaalik

A transitional fossil displaying both fish and tetrapod traits, including wrist-like bones for support, gills for underwater breathing, and primitive lungs for breathing air.

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Evolution of woody plants

An event between 400โˆ’350400-350 MYA that caused a dramatic decline in atmospheric CO2CO_2 levels through biological influence on geological cycles.

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The Big Five

A series of rare mass extinction events among complex, multicellular organisms that have significantly altered the course of evolution.

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End-Permian Extinction

The most devastating mass extinction occurring 252252 million years ago, resulting in the loss of ~90โˆ’96%90-96\% of marine species and ~70%70\% of terrestrial species.

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Cretaceous Mass Extinction

An event approximately 6565 MYA caused by a large asteroid impact (Chicxulubย crater\text{Chicxulub crater}) and volcanic activity (Deccanย Traps\text{Deccan Traps}) that eliminated ~75%75\% of species, including non-avian dinosaurs.

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Mass Extinction (Definition)

A short period of time when at least 75%75\% of species are lost.

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Amphibians

Often called the 'canary of the gold mine' for ecosystems because their narrow environmental tolerances and gas exchange through skin make them sensitive to disruption.

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Greenhouse Gases

Atmospheric components such as CO2CO_2, water vapor, and methane (CH4CH_4) that absorb and trap heat; excessive levels put life at risk through increased greenhouse effect.

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Sedimentary rock

The largest and typically long-term reservoir for carbon within the global carbon cycle.

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Keeling Curve

A record of atmospheric CO2CO_2 levels over the past 6060 years showing a seasonal pattern based on plant photosynthesis and a steady long-term increase.

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The Deadly Trio

The three effects of increasing CO2CO_2 on the oceans: increased temperature (warming), decreased pH (acidification), and decreased capacity to store oxygen (deoxygenation).

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Positive Feedbacks

Destabilizing climate processes such as soil respiration increases or permafrost thawing that release more CO2CO_2 and CH4CH_4, strengthening the greenhouse effect.

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CO2 Fertilization

The phenomenon where increased atmospheric CO2CO_2 increases photosynthesis and plant growth, though often resulting in decreased nutrient quality for crops.