Methane hydrate stability and anthropogenic climate change
D Archer - Biogeosciences, 2007 - bg.copernicus.org
Methane frozen into hydrate makes up a large reservoir of potentially volatile carbon below
the sea floor and associated with permafrost soils. This reservoir intuitively seems …
the sea floor and associated with permafrost soils. This reservoir intuitively seems …
Arctic hydrology during global warming at the Palaeocene/Eocene thermal maximum
Abstract The Palaeocene/Eocene thermal maximum represents a period of rapid, extreme
global warming∼ 55 million years ago, superimposed on an already warm world,,. This …
global warming∼ 55 million years ago, superimposed on an already warm world,,. This …
Two massive, rapid releases of carbon during the onset of the Palaeocene–Eocene thermal maximum
The Earth's climate abruptly warmed by 5–8° C during the Palaeocene–Eocene thermal
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
maximum (PETM), about 55.5 million years ago,. This warming was associated with a …
Orbital climate forcing of δ13C excursions in the late Paleocene–early Eocene (chrons C24n–C25n)
High‐resolution stable carbon isotope records for upper Paleocene–lower Eocene sections
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
at Ocean Drilling Program Sites 1051 and 690 and Deep Sea Drilling Project Sites 550 and …
Extreme warming of mid-latitude coastal ocean during the Paleocene-Eocene Thermal Maximum: Inferences from TEX86 and isotope data
Abstract Changes in sea surface temperature (SST) during the Paleocene-Eocene Thermal
Maximum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records …
Maximum (PETM) have been estimated primarily from oxygen isotope and Mg/Ca records …
Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary
The start of the Palaeocene/Eocene thermal maximum—a period of exceptional global
warming about 55 million years ago—is marked by a prominent negative carbon isotope …
warming about 55 million years ago—is marked by a prominent negative carbon isotope …
Stable carbon isotopes in paleoceanography: atmosphere, oceans, and sediments
A Mackensen, G Schmiedl - Earth-Science Reviews, 2019 - Elsevier
Carbon is one of the key elements in organisms and non-living compounds on Earth.
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
Carbon dioxide and methane are important greenhouse gases in the atmosphere, dissolved …
Chapter eighteen the use of oxygen and carbon isotopes of foraminifera in paleoceanography
AC Ravelo, C Hillaire-Marcel - Developments in marine geology, 2007 - Elsevier
Publisher Summary This chapter discusses the factors that must be taken into account when
interpreting paleoceanographic records derived from measurements of the oxygen and …
interpreting paleoceanographic records derived from measurements of the oxygen and …
Beyond methane: towards a theory for the Paleocene–Eocene thermal maximum
JA Higgins, DP Schrag - Earth and Planetary Science Letters, 2006 - Elsevier
Extreme global warmth and an abrupt negative carbon isotope excursion during the
Paleocene–Eocene Thermal Maximum (PETM) have been attributed to a massive release of …
Paleocene–Eocene Thermal Maximum (PETM) have been attributed to a massive release of …
Down the rabbit hole: Toward appropriate discussion of methane release from gas hydrate systems during the Paleocene-Eocene thermal maximum and other past …
GR Dickens - Climate of the Past, 2011 - cp.copernicus.org
Enormous amounts of 13 C-depleted carbon rapidly entered the exogenic carbon cycle
during the onset of the Paleocene-Eocene thermal maximum (PETM), as attested to by a …
during the onset of the Paleocene-Eocene thermal maximum (PETM), as attested to by a …