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Ch. 20 The Ocean Basins
Ch. 20 The Ocean Basins

... Oceans interact with atmosphere  influence climate and weather patterns Part of natural processes (ecosystems, biogeochemical cycles, plate tectonics) Habitat for many organisms Food source ...
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... dioxide. The timing of the oceanic carbon dioxide uptake is one of the most critical factors in determining the strength of the expected climate change during the coming decades and centuries. A correct quantification of the oceanic carbon sink is essential for human societies to plan ahead: (1) How ...
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... material from its surface all the way to its center. Objects colliding with Earth helped to cause Earth to grow hot enough that heavy elements such as iron and nickel melted. The material composing Earth gradually separated into several layers, with the denser material being located near the center. ...
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Post Test Study Guide Answer Key 1. HMS Challenger: first voyage

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Anoxic event



Oceanic anoxic events or anoxic events (Anoxia conditions) refer to intervals in the Earth's past where portions of oceans become depleted in oxygen (O2) at depths over a large geographic area. During some of these events, euxinia develops - euxinia refers to anoxic waters that contain H2S hydrogen sulfide. Although anoxic events have not happened for millions of years, the geological record shows that they happened many times in the past. Anoxic events coincide with several mass extinctions and may contribute to these events. These mass extinctions include some that geobiologists use as time markers in biostratigraphic dating. It is believed oceanic anoxic events are strongly linked to slowing of ocean circulation, climatic warming and elevated levels of greenhouse gases. Enhanced volcanism (through the release of CO2 and other greenhouse gases) is the proposed central external trigger for the development of these events.
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