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The Paleocene-Eocene Thermal Maximum: A perturbation of carbon cycle, climate, and biosphere with implications for the future
During the Paleocene-Eocene Thermal Maximum (PETM),∼ 56 Mya, thousands of
petagrams of carbon were released into the ocean-atmosphere system with attendant …
petagrams of carbon were released into the ocean-atmosphere system with attendant …
[HTML][HTML] Hydrological and associated biogeochemical consequences of rapid global warming during the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM) hyperthermal,~ 56 million years
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
ago (Ma), is the most dramatic example of abrupt Cenozoic global warming. During the …
Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a geologically rapid
warming period associated with carbon release, which caused a marked increase in the …
warming period associated with carbon release, which caused a marked increase in the …
Impact of warming on aquatic body sizes explained by metabolic scaling from microbes to macrofauna
Rising temperatures are associated with reduced body size in many marine species, but the
biological cause and generality of the phenomenon is debated. We derive a predictive …
biological cause and generality of the phenomenon is debated. We derive a predictive …
Climate, oxygen, and the future of marine biodiversity
The ocean enabled the diversification of life on Earth by adding O2 to the atmosphere, yet
marine species remain most subject to O2 limitation. Human industrialization is intensifying …
marine species remain most subject to O2 limitation. Human industrialization is intensifying …
Cenozoic mass extinctions in the deep sea: What perturbs the largest habitat on Earth?
E Thomas - 2007 - pubs.geoscienceworld.org
Deep-sea benthic foraminifera live in the largest habitat on Earth, constitute an important
part of its benthic biomass, and form diverse assemblages with common cosmopolitan …
part of its benthic biomass, and form diverse assemblages with common cosmopolitan …
Environmental changes during the Cretaceous-Paleogene mass extinction and Paleocene-Eocene thermal maximum: implications for the Anthropocene
Abstract The Cretaceous-Paleogene boundary (KPB) mass extinction (~ 66.02 Ma) and the
Paleocene-Eocene Thermal Maximum (PETM)(~ 55.8 Ma) are two remarkable climatic and …
Paleocene-Eocene Thermal Maximum (PETM)(~ 55.8 Ma) are two remarkable climatic and …
Coupled microbial bloom and oxygenation decline recorded by magnetofossils during the Palaeocene–Eocene Thermal Maximum
Understanding marine environmental change and associated biological turnover across the
Palaeocene–Eocene Thermal Maximum (PETM;~ 56 Ma)—the most pronounced Cenozoic …
Palaeocene–Eocene Thermal Maximum (PETM;~ 56 Ma)—the most pronounced Cenozoic …
Long-term legacy of massive carbon input to the Earth system: Anthropocene versus Eocene
Over the next few centuries, with unabated emissions of anthropogenic carbon dioxide
(CO2), a total of 5000 Pg C may enter the atmosphere, causing CO2 concentrations to rise to …
(CO2), a total of 5000 Pg C may enter the atmosphere, causing CO2 concentrations to rise to …
Modern seawater acidification: the response of foraminifera to high-CO2 conditions in the Mediterranean Sea
The seas around the island of Ischia (Italy) have a lowered pH as a result of volcanic gas
vents that emit carbon dioxide from the sea floor at ambient seawater temperatures. These …
vents that emit carbon dioxide from the sea floor at ambient seawater temperatures. These …