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The climatic cooling of the last 55.5 million years has been caused by __________________.

A. the ongoing breakup of Pangaea into separate continents
B. continental masses moving into polar latitudes
C. snow and ice accumulating on polar landmasses, increasing albedo
D. the uplifts of the Tibetan Plateau/Himalaya Mountains in Asia and the Colorado Plateau in the western United States deflecting west-to-east atmospheric circulation in the midlatitudes
E. All of these choices are correct.

1 Answer

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Final answer:

The climatic cooling over the last 55.5 million years has been caused by a combination of the breakup of Pangaea, continental movement into polar regions, increased albedo from snow and ice accumulation, and significant geological uplifts that changed atmospheric circulation. All provided choices contribute to this cooling trend.

Step-by-step explanation:

The climatic cooling of the last 55.5 million years has been influenced by a combination of factors that include continental drift, changes in the Earth's surface and atmosphere, and variations in solar radiation. The correct answer to the question is E. All of these choices are correct.

For instance, the ongoing breakup of Pangaea into separate continents (A) has tremendously impacted ocean and atmospheric circulation, redistributing heat across the planet. Moreover, as continental masses moved into polar latitudes (B), their presence in these regions led to changes in climate dynamics, including ice sheet formation. Accumulation of snow and ice on polar landmasses increased albedo (C), resulting in greater solar reflectivity and further cooling. Lastly, major geological uplifts, such as the rise of the Tibetan Plateau/Himalaya Mountains and the Colorado Plateau (D), have altered atmospheric circulation patterns, which in turn have influenced the climate.

All these factors together have contributed to the gradual cooling trend of Earth's climate over the last 55.5 million years, leading to the formation of permanent ice sheets in regions like Antarctica, largely driven by decreases in atmospheric CO2 and shifts in ocean currents.

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