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View article: Loss of Earth system resilience during early Eocene transient global warming events
Loss of Earth system resilience during early Eocene transient global warming events Open
Superimposed on long-term late Paleocene–early Eocene warming (~59 to 52 million years ago), Earth’s climate experienced a series of abrupt perturbations, characterized by massive carbon input into the ocean-atmosphere system and global wa…
View article: Early Eocene hyperthermals as carbon cycle tipping points?
Early Eocene hyperthermals as carbon cycle tipping points? Open
Gradual global warming might trigger the release of large amounts of carbon from natural reservoirs such as submarine methane hydrates and permafrost, exacerbating the effects of human-caused carbon emissions. These "tipping points" in the…
View article: Loss of Earth System Resilience during Early Eocene Global Warming Events
Loss of Earth System Resilience during Early Eocene Global Warming Events Open
The Paleocene-Eocene Thermal Maximum (PETM; 56 Ma) and Eocene Thermal Maximum 2 and 3 (ETM2; 54.06 Ma and ETM3; 52.87 Ma) were three of a series of abrupt climate and carbon cycle perturbations, characterized by massive carbon input into t…