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 …
[HTML][HTML] The legacy of the Tethys Ocean: Anoxic seas, evaporitic basins, and megalakes in the Cenozoic of Central Europe
At the end of the Eocene, the demise of the Tethys Ocean led to the formation of one of the
largest anoxic seas in the last 50 million years of Earth history. This long-lived anoxic water …
largest anoxic seas in the last 50 million years of Earth history. This long-lived anoxic water …
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 …
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 …
Spatial and Temporal Patterns in Petrogenic Organic Carbon Mobilization During the Paleocene‐Eocene Thermal Maximum
EH Hollingsworth, FJ Elling… - Paleoceanography …, 2024 - Wiley Online Library
Abstract The Paleocene‐Eocene Thermal Maximum (PETM) was a transient global warming
event and is recognized in the geologic record by a prolonged negative carbon isotope …
event and is recognized in the geologic record by a prolonged negative carbon isotope …
Tropical ocean temperatures and changes in terrigenous flux during the Paleocene-Eocene Thermal Maximum in southern Tibet
Abstract The Paleocene-Eocene Thermal Maximum (PETM,∼ 56 Ma) was an extreme
climate warming event of the early Cenozoic. The development and ecology of carbonate …
climate warming event of the early Cenozoic. The development and ecology of carbonate …
Biogeochemical responses to global warming during the Paleocene–Eocene Thermal Maximum in the eastern Tethys
Abstract The Paleocene–Eocene Thermal Maximum (PETM;∼ 56 Ma) represents a rapid
and sustained climatic perturbation that lasted for∼ 170 kyr and coincided with the …
and sustained climatic perturbation that lasted for∼ 170 kyr and coincided with the …
Middle Paleocene-early Eocene inter-regional correlations and palaeoclimatic changes in eastern Tethys Sea: Calcareous nannofossil evidence for Paleocene …
X Wang, D Xi, E Mattioli, G Wang, X Wan - Palaeogeography …, 2023 - Elsevier
Calcareous nannofossil assemblages from the interval covering the middle Paleocene to
early Eocene (P/E), studied in sediments from two sections located in the western Tarim …
early Eocene (P/E), studied in sediments from two sections located in the western Tarim …
Mechanisms of terrestrial organic matter accumulation across the Paleocene-Eocene thermal maximum in the Jianghan Basin, Central China
Marine settings provide major carbon sinks for organic carbon, and act as a key reservoir
that can sequester excess carbon during times of high CO 2 and global warming. Organic …
that can sequester excess carbon during times of high CO 2 and global warming. Organic …
Recognition of a cryptic maximum flooding surface in shallow marine carbonate sequences using geochemical (Y/Ho) proxy data
Since diagnostic primary depositional sedimentary structures and depth‐dependent grain‐
size trends are rarely preserved, building a comprehensive sequence stratigraphic …
size trends are rarely preserved, building a comprehensive sequence stratigraphic …