Allow us to refresh your memory: it was the Paleocene-Eocene Thermal Maximum, a 200,000-year period of rapid carbon release and global warming that turned Earth's oceans acidic and saw terrestrial ...
The event is known as the Palaeocene-Eocene Thermal Maximum (PETM) but the cause of the warming is still debated. Huge amounts of carbon entered into the atmosphere at the time along with methane.
Just how much carbon was injected into the atmosphere during the Paleocene-Eocene Thermal Maximum, or PETM, as scientists now call the fever period, is uncertain. But they estimate it was roughly ...
The Artstor website will be retired on Aug 1st. Journal of Paleontology Vol. 57, No. 6, Nov., 1983 New Late Paleocene Molluscs from the Sim... New Late Paleocene Molluscs from the Simi Hills, Ventura ...
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