Shallow-water hydrothermal venting linked to the Palaeocene–Eocene Thermal Maximum
Abstract The Palaeocene–Eocene Thermal Maximum (PETM) was a global warming event
of 5–6° C around 56 million years ago caused by input of carbon into the ocean and …
of 5–6° C around 56 million years ago caused by input of carbon into the ocean and …
Spatiotemporal distribution of global mercury enrichments through the Paleocene-Eocene Thermal Maximum and links to volcanism
Abstract Mercury (Hg) concentrations and Hg isotopes have been widely used to fingerprint
geological volcanism. Mercury content, as a more accessible proxy, is more frequently used …
geological volcanism. Mercury content, as a more accessible proxy, is more frequently used …
The minerals ikaite and its pseudomorph glendonite: Historical perspective and legacies of Douglas Shearman and Alec K. Smith
This paper presents a historical perspective of the discovery of, and aspects of, glendonite
and ikaite, through the legacy of British mineralogists Douglas Shearman and Alec K. Smith …
and ikaite, through the legacy of British mineralogists Douglas Shearman and Alec K. Smith …
Mercury isotope evidence for protracted North Atlantic magmatism during the Paleocene-Eocene Thermal Maximum
Abstract The Paleocene-Eocene Thermal Maximum (PETM,∼ 56 Ma) was a major
hyperthermal event that has been linked to CO 2 release from the North Atlantic Igneous …
hyperthermal event that has been linked to CO 2 release from the North Atlantic Igneous …
Volatile metal emissions from volcanic degassing and lava–seawater interactions at Kīlauea Volcano, Hawai'i
Volcanoes represent one of the largest natural sources of metals to the Earth's surface.
Emissions of these metals can have important impacts on the biosphere as pollutants or …
Emissions of these metals can have important impacts on the biosphere as pollutants or …
Tracing North Atlantic volcanism and seaway connectivity across the paleocene–eocene thermal maximum (PETM)
There is a temporal correlation between the peak activity of the North Atlantic Igneous
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
Province (NAIP) and the Paleocene–Eocene Thermal Maximum (PETM), suggesting that the …
Paleocene–Eocene age glendonites from the Mid-Norwegian Margin–indicators of cold snaps in the hothouse?
The International Ocean Discovery Program (IODP) Expedition 396 to the mid-Norwegian
margin recovered> 1300 m of pristinely preserved, volcanic-ash-rich sediments deposited …
margin recovered> 1300 m of pristinely preserved, volcanic-ash-rich sediments deposited …
Fossils indicate marine dispersal in osteoglossid fishes, a classic example of continental vicariance
A Capobianco, M Friedman - Proceedings of the …, 2024 - royalsocietypublishing.org
The separation of closely related terrestrial or freshwater species by vast marine barriers
represents a biogeographical riddle. Such cases can provide evidence for vicariance, a …
represents a biogeographical riddle. Such cases can provide evidence for vicariance, a …
Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea
The Paleocene–Eocene Thermal Maximum (PETM;~ 55.9 Ma) was a period of rapid and
sustained global warming associated with significant carbon emissions. It coincided with the …
sustained global warming associated with significant carbon emissions. It coincided with the …
Marine diagenesis of tephra aided the Palaeocene-Eocene Thermal Maximum termination
Abstract The Palaeocene-Eocene Thermal Maximum (PETM) was a period of intense global
warming that began∼ 55.9 million years ago and lasted about 170,000 yrs. Various …
warming that began∼ 55.9 million years ago and lasted about 170,000 yrs. Various …