Phanerozoic paleotemperatures: The earth's changing climate during the last 540 million years
This study provides a comprehensive and quantitative estimate of how global temperatures
have changed during the last 540 million years. It combines paleotemperature …
have changed during the last 540 million years. It combines paleotemperature …
Intergovernmental Panel on Climate Change (IPCC). Global carbon and other biogeochemical cycles and feedbacks
It is unequivocal that the increases in atmospheric carbon dioxide (CO2), methane (CH4)
and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …
and nitrous oxide (N2O) since the pre-industrial period are caused by human activities. The …
Rhyacian intermittent large igneous provinces sustained Great Oxidation Event: evidence from North China craton
To better understand the sustaining mechanism of the Great Oxidation Event (GOE), strata
and igneous suites especially large igneous provinces (LIPs) during the GOE's late stage …
and igneous suites especially large igneous provinces (LIPs) during the GOE's late stage …
[HTML][HTML] Paleocene/Eocene carbon feedbacks triggered by volcanic activity
Abstract The Paleocene–Eocene Thermal Maximum (PETM) was a period of geologically-
rapid carbon release and global warming~ 56 million years ago. Although modelling …
rapid carbon release and global warming~ 56 million years ago. Although modelling …
Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum
The Paleocene-Eocene Thermal Maximum (PETM) is recognized by a major negative
carbon isotope (δ13C) excursion (CIE) signifying an injection of isotopically light carbon into …
carbon isotope (δ13C) excursion (CIE) signifying an injection of isotopically light carbon into …
The seawater carbon inventory at the Paleocene–Eocene Thermal Maximum
The Paleocene–Eocene Thermal Maximum (PETM)(55.6 Mya) was a geologically rapid
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …
carbon-release event that is considered the closest natural analog to anthropogenic CO2 …
[HTML][HTML] Massive methane fluxing from magma–sediment interaction in the end-Triassic Central Atlantic Magmatic Province
Exceptional magmatic events coincided with the largest mass extinctions throughout Earth's
history. Extensive degassing from organic-rich sediments intruded by magmas is a possible …
history. Extensive degassing from organic-rich sediments intruded by magmas is a possible …
Abrupt Northwest Atlantic deep-sea oxygenation decline preceded the Palaeocene-Eocene Thermal Maximum
Reconstruction of oceanic redox conditions across the Palaeocene-Eocene Thermal
Maximum (PETM,∼ 55.93 Ma) provides crucial information on potential PETM triggers and …
Maximum (PETM,∼ 55.93 Ma) provides crucial information on potential PETM triggers and …
Eustatic change across the Paleocene-Eocene Thermal Maximum in the epicontinental Tarim seaway
Abstract The Paleocene-Eocene Thermal Maximum (PETM) offers an excellent opportunity
to study the ecological and environmental responses to global warming. Discussing the so …
to study the ecological and environmental responses to global warming. Discussing the so …
[HTML][HTML] Assessing the importance of thermogenic degassing from the Karoo Large Igneous Province (LIP) in driving Toarcian carbon cycle perturbations
The emplacement of the Karoo Large Igneous Province (LIP) occurred synchronously with
the Toarcian crisis (ca. 183 Ma), which is characterized by major carbon cycle perturbations …
the Toarcian crisis (ca. 183 Ma), which is characterized by major carbon cycle perturbations …