Articles | Volume 14, issue 7
Clim. Past, 14, 1035–1049, 2018
https://doi.org/10.5194/cp-14-1035-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Clim. Past, 14, 1035–1049, 2018
https://doi.org/10.5194/cp-14-1035-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
11 Jul 2018
Research article
| 11 Jul 2018
Dynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal Maximum
Tom Dunkley Jones et al.
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Cited
17 citations as recorded by crossref.
- Constraints on the onset duration of the Paleocene–Eocene Thermal Maximum S. Turner 10.1098/rsta.2017.0082
- Increased frequency of extreme precipitation events in the North Atlantic during the PETM: Observations and theory W. Rush et al. 10.1016/j.palaeo.2021.110289
- Negative carbon isotope excursions: an interpretive framework P. Vervoort et al. 10.1088/1748-9326/ab3318
- Alluvial record of an early Eocene hyperthermal within the Castissent Formation, the Pyrenees, Spain L. Honegger et al. 10.5194/cp-16-227-2020
- Turnover and stability in the deep sea: Benthic foraminifera as tracers of Paleogene global change L. Alegret et al. 10.1016/j.gloplacha.2020.103372
- Climate-driven hydrological change and carbonate platform demise induced by the Paleocene–Eocene Thermal Maximum (southern Pyrenees) J. Li et al. 10.1016/j.palaeo.2021.110250
- Linking geological heritage and geoethics with a particular emphasis on palaeontological heritage: the new concept of ‘palaeontoethics’ D. DeMiguel et al. 10.1007/s12371-021-00595-3
- Geochemical indications for the Paleocene-Eocene Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM-2) hyperthermals in terrestrial sediments of the Canadian Arctic L. Reinhardt et al. 10.1130/GES02398.1
- Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al. 10.1029/2021PA004232
- Solar System chaos and the Paleocene–Eocene boundary age constrained by geology and astronomy R. Zeebe & L. Lourens 10.1126/science.aax0612
- Large-scale, astronomically paced sediment input to the North Sea Basin during the Paleocene Eocene Thermal Maximum S. Jin et al. 10.1016/j.epsl.2021.117340
- Biotic and stable-isotope characterization of the Toarcian Ocean Anoxic Event through a carbonate–clastic sequence from Somerset, UK I. Boomer et al. 10.1144/SP514-2020-263
- Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea E. Stokke et al. 10.5194/cp-17-1989-2021
- Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum P. Pogge von Strandmann et al. 10.1126/sciadv.abh4224
- Stratigraphy of the Paleocene continental sedimentary succession of the northern Pyrenean basin (Corbières, southern France) using δ13Corg isotopes A. Maufrangeas et al. 10.1144/jgs2019-084
- Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change S. Jones et al. 10.1038/s41467-019-12957-1
- Environmental instability during the latest Paleocene at Zumaia (Basque-Cantabric Basin): The bellwether of the Paleocene-Eocene Thermal Maximum L. Alegret et al. 10.1016/j.palaeo.2018.02.018
16 citations as recorded by crossref.
- Constraints on the onset duration of the Paleocene–Eocene Thermal Maximum S. Turner 10.1098/rsta.2017.0082
- Increased frequency of extreme precipitation events in the North Atlantic during the PETM: Observations and theory W. Rush et al. 10.1016/j.palaeo.2021.110289
- Negative carbon isotope excursions: an interpretive framework P. Vervoort et al. 10.1088/1748-9326/ab3318
- Alluvial record of an early Eocene hyperthermal within the Castissent Formation, the Pyrenees, Spain L. Honegger et al. 10.5194/cp-16-227-2020
- Turnover and stability in the deep sea: Benthic foraminifera as tracers of Paleogene global change L. Alegret et al. 10.1016/j.gloplacha.2020.103372
- Climate-driven hydrological change and carbonate platform demise induced by the Paleocene–Eocene Thermal Maximum (southern Pyrenees) J. Li et al. 10.1016/j.palaeo.2021.110250
- Linking geological heritage and geoethics with a particular emphasis on palaeontological heritage: the new concept of ‘palaeontoethics’ D. DeMiguel et al. 10.1007/s12371-021-00595-3
- Geochemical indications for the Paleocene-Eocene Thermal Maximum (PETM) and Eocene Thermal Maximum 2 (ETM-2) hyperthermals in terrestrial sediments of the Canadian Arctic L. Reinhardt et al. 10.1130/GES02398.1
- Eutrophication and Deoxygenation Forcing of Marginal Marine Organic Carbon Burial During the PETM N. Papadomanolaki et al. 10.1029/2021PA004232
- Solar System chaos and the Paleocene–Eocene boundary age constrained by geology and astronomy R. Zeebe & L. Lourens 10.1126/science.aax0612
- Large-scale, astronomically paced sediment input to the North Sea Basin during the Paleocene Eocene Thermal Maximum S. Jin et al. 10.1016/j.epsl.2021.117340
- Biotic and stable-isotope characterization of the Toarcian Ocean Anoxic Event through a carbonate–clastic sequence from Somerset, UK I. Boomer et al. 10.1144/SP514-2020-263
- Rapid and sustained environmental responses to global warming: the Paleocene–Eocene Thermal Maximum in the eastern North Sea E. Stokke et al. 10.5194/cp-17-1989-2021
- Lithium isotope evidence for enhanced weathering and erosion during the Paleocene-Eocene Thermal Maximum P. Pogge von Strandmann et al. 10.1126/sciadv.abh4224
- Stratigraphy of the Paleocene continental sedimentary succession of the northern Pyrenean basin (Corbières, southern France) using δ13Corg isotopes A. Maufrangeas et al. 10.1144/jgs2019-084
- Large Igneous Province thermogenic greenhouse gas flux could have initiated Paleocene-Eocene Thermal Maximum climate change S. Jones et al. 10.1038/s41467-019-12957-1
Latest update: 25 May 2022
Short summary
The Paleocene–Eocene Thermal Maximum (PETM) is a transient global warming event associated with a doubling of atmospheric carbon dioxide concentrations. Here we document a major increase in sediment accumulation rates on a subtropical continental margin during the PETM, likely due to marked changes in hydro-climates and sediment transport. These high sedimentation rates persist through the event and may play a key role in the removal of carbon from the atmosphere by the burial of organic carbon.
The Paleocene–Eocene Thermal Maximum (PETM) is a transient global warming event associated with...
