What caused the Paleocene and Eocene periods to be so warm?

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The Paleocene and Eocene epochs, occurring 35 to 65 million years ago, were characterized by significantly warmer global temperatures, although Antarctica was not tropical but rather a temperate rainforest. During this time, Antarctica remained at the South Pole, experiencing long nights of 4-5 months, which differentiates its climate from modern tropical regions. The closure of Drake's Passage and the openness of the Panama Isthmus likely influenced oceanic currents, yet the specifics of paleo-oceanic currents remain largely unknown. While deep ocean currents were warmer than today, the overall temperature gradient between the equator and the poles was smaller, suggesting a more uniformly warm planet rather than just regional warming. The discussion highlights the complexity of climate variations over the 20 million years of these epochs, emphasizing that while the planet was considerably warmer, it was not uniformly tropical.
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Paleocene and Eocene were very warm, due to only tropical-like Antarctica findings? 35-65 myr ago, Antarctica would still be at south pole. And one would have a long night of 4-5 months; so not entirely like our tropics. Has the literature assumed that the entire planet is very warm? Drake's passage was closed, and Panama isthmus was probably open. Nothing is known about paleo-oceanic currents. Was a warm current perhaps wrapped around Antarctica; hence only regional warming?
 
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At it's warmest during those periods, Antarctica was not tropical like.
Instead, the polar regions were at most a temperate rainforest.

Deep ocean currents are known to have been much warmer than they are now.
The tropics were larger and the temperature gradient between the equator and poles smaller. Clearly not a case of regional warming.

Still, you are referring to a period of 20 million years.
There was lots of variation over that time; but yes a considerably warmer period.
 
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