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

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In summary, during the Paleocene and Eocene periods, Antarctica was much warmer than it is now, with only tropical-like findings. However, it was not entirely like the tropics, as the polar regions were at most a temperate rainforest. The literature has assumed that the entire planet was very warm during this time, with the closure of Drake's passage and the probable opening of the Panama isthmus. It is not known if a warm current was wrapped around Antarctica, leading to only regional warming. The deep ocean currents were also warmer during this time, with a larger tropical region and smaller temperature gradient between the equator and poles. This warm period lasted for 20 million years with significant variations.
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cph
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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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  • #3
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.
 

What is the Paleocene Eocene warming?

The Paleocene Eocene warming, also known as the Paleocene Eocene Thermal Maximum (PETM), was a period of rapid global warming that occurred approximately 55 million years ago. It was marked by a significant rise in carbon dioxide levels, leading to a greenhouse effect and a warming of the Earth's climate.

What caused the Paleocene Eocene warming?

The exact cause of the Paleocene Eocene warming is still debated among scientists. However, the most widely accepted theory is that it was triggered by a massive release of carbon into the atmosphere, possibly from the melting of methane hydrates, volcanic activity, or the burning of fossil fuels. This release of carbon then led to a positive feedback loop, further amplifying the warming trend.

How long did the Paleocene Eocene warming last?

The Paleocene Eocene warming lasted for approximately 200,000 years. This is a relatively short period of time in Earth's history, but the warming during this time was significant and had long-lasting effects on the planet's climate and ecosystems.

How did the Paleocene Eocene warming impact the Earth's ecosystems?

The Paleocene Eocene warming had a significant impact on the Earth's ecosystems. It led to the extinction of many species, particularly in the oceans, as the warming and acidification of the ocean waters made it difficult for marine organisms to survive. It also caused changes in vegetation patterns and the migration of species to more northern latitudes.

What can we learn from the Paleocene Eocene warming?

Studying the Paleocene Eocene warming can provide valuable insights into how the Earth's climate system responds to changes in carbon dioxide levels. It can also help us understand the potential impacts of future climate change and the importance of reducing carbon emissions to mitigate these effects. Additionally, it can provide information on the resilience of ecosystems and their ability to adapt to rapid changes in the Earth's climate.

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