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 …
Toward an improved understanding of the marine barium cycle and the application of marine barite as a paleoproductivity proxy
Marine barite (BaSO4) is a relatively ubiquitous, though minor, component of ocean
sediments. Modern studies of the accumulation of barite in ocean sediments have …
sediments. Modern studies of the accumulation of barite in ocean sediments have …
Controls on the barium isotope compositions of marine sediments
The accumulation of barium (Ba) in marine sediments is considered to be a robust proxy for
export production, although this application can be limited by uncertainty in BaSO 4 …
export production, although this application can be limited by uncertainty in BaSO 4 …
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 …
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 …
Carbon sequestration during the Palaeocene–Eocene Thermal Maximum by an efficient biological pump
A perturbation of the carbon cycle and biosphere, linked to globally increased temperatures
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …
about 55.9 million years ago, characterized the Palaeocene–Eocene Thermal Maximum. Its …
Global decline in ocean ventilation, oxygenation, and productivity during the Paleocene-Eocene Thermal Maximum: Implications for the benthic extinction
The prominent global warming event at the Paleocene-Eocene boundary (55 Ma), referred
to as the Paleocene-Eocene Thermal Maximum (PETM), was characterized by rapid …
to as the Paleocene-Eocene Thermal Maximum (PETM), was characterized by rapid …
[HTML][HTML] Water column barium sulfate dissolution and shielding by organic matter aggregates: Implications for the pelagic barite proxy
Pelagic barite (BaSO 4) and related proxies are useful tools for reconstructing the marine
carbon cycle. The factors controlling pelagic barite dissolution in the ocean water column …
carbon cycle. The factors controlling pelagic barite dissolution in the ocean water column …
Increased export production during recovery from the Paleocene–Eocene thermal maximum constrained by sedimentary Ba isotopes
Abstract The Paleocene–Eocene thermal maximum (PETM;∼ 56 Ma) was a transient global
warming event associated with a huge perturbation to the global carbon cycle. Changes in …
warming event associated with a huge perturbation to the global carbon cycle. Changes in …
Bentho‐pelagic decoupling: The marine biological carbon pump during Eocene hyperthermals
Future environmental change may profoundly affect oceanic ecosystems in a complex way,
due to the synergy between rising temperatures, reduction in mixing and upwelling due to …
due to the synergy between rising temperatures, reduction in mixing and upwelling due to …