Tag Archives: Triassic

Paleocene-Eocene Thermal Maximum caused by thawing permafrost?

In a new study reported in Nature, climate scientist Rob DeConto of the University of Massachusetts Amherst and colleagues elsewhere propose a simple new mechanism to explain the source of carbon that fed a series of extreme warming events about 55 million years ago, the Paleocene-Eocene Thermal Maximum (PETM), and a sequence of similar, smaller warming events afterward.

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Reefs took 1.5 million years to reappear after Permian-Triassic Mass Extinction

The Permian-Triassic Mass Extinction was the largest in our planet’s history. Enormous disruptions of the carbon cycle led to climate change, ocean acidification and ocean anoxia – and with an estimated 90 percent of all species dying out Earth almost … Continue reading →

Permian-Triassic mass extinction: 11,000 Gt CO2 worth of climate change led to microbial plagues that killed the world’s forests

New research shows an example of a missing link between climatic disruptions and biodiversity decline: killer microbes.

Triassic-Jurassic mass extinction caused by >16,000 Gt methane – from clathrates

Scientists of Utrecht University have investigated fossil leaves found in terrestrial late Triassic sediments and discovered a large carbon-13 depletion. That means 200,000,000 years ago The Methane Bomb went off.