Articles | Volume 14, issue 3
https://doi.org/10.5194/cp-14-303-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-14-303-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Synchronizing early Eocene deep-sea and continental records – cyclostratigraphic age models for the Bighorn Basin Coring Project drill cores
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, 28359, Germany
Ursula Röhl
MARUM – Center for Marine Environmental Sciences, University of Bremen, Bremen, 28359, Germany
Roy H. Wilkens
Hawaii Institute of Geophysics & Planetology, University of Hawaii,
Honolulu, HI, 96822, USA
Philip D. Gingerich
Museum of Paleontology, University of Michigan, Ann Arbor,
Michigan,
48109-1079, USA
William C. Clyde
Department of Earth Sciences, University of New Hampshire, 56 College
Rd., Durham, NH 03824, USA
Scott L. Wing
Department of Paleobiology, P.O. Box 37012, National Museum of Natural
History, Smithsonian Institution, Washington, D.C. 20013 USA
Gabriel J. Bowen
Department of Geology & Geophysics, University of Utah, Salt Lake
City, UT 84112, USA
Mary J. Kraus
Department of Geological Sciences, University of Colorado at Boulder,
UCB 399, Boulder, CO 80309, USA
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42 citations as recorded by crossref.
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- Palynostratigraphy of the lower Paleogene Margaret Formation at Stenkul Fiord, Ellesmere Island, Nunavut, Canada M. Sudermann et al. 10.1080/01916122.2020.1861121
- Elevated physical weathering exceeds chemical weathering of clays during the Paleocene-Eocene Thermal Maximum in the continental Bighorn Basin (Wyoming, USA) K. Ji et al. 10.1016/j.palaeo.2023.111445
- Abrupt Northwest Atlantic deep-sea oxygenation decline preceded the Palaeocene-Eocene Thermal Maximum P. Xue et al. 10.1016/j.epsl.2023.118304
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- Paleoenvironment reconstruction of the eastern Tethys during the pre-onset excursion preceding the PETM Y. Dong et al. 10.1016/j.palaeo.2024.112234
- 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
- Orbital modulation of an intensified hydrological cycle during the Paleocene-Eocene Thermal Maximum J. Zhang et al. 10.1016/j.epsl.2024.118693
- Early Eocene Thermal Maximum 3: Biotic Response at Walvis Ridge (SE Atlantic Ocean) E. Thomas et al. 10.1029/2018PA003375
- Multiple early Eocene carbon isotope excursions associated with environmental changes in the Dieppe-Hampshire Basin (NW Europe) S. Garel et al. 10.1051/bsgf/2020030
- Carbon Isotope Record of Trace n‐alkanes in a Continental PETM Section Recovered by the Bighorn Basin Coring Project (BBCP) A. Baczynski et al. 10.1029/2019PA003579
- Astronomically forced late Paleocene-early Eocene climate variability in the Subei Basin, East China J. Liu et al. 10.1016/j.gloplacha.2023.104350
- Increased export production during recovery from the Paleocene–Eocene thermal maximum constrained by sedimentary Ba isotopes L. Bridgestock et al. 10.1016/j.epsl.2018.12.036
- Statistical approaches for improved definition of carbon isotope excursions J. Eldrett et al. 10.1016/j.earscirev.2024.104851
- Delays, Discrepancies, and Distortions: Size‐Dependent Sediment Mixing and the Deep‐Sea Record of the Paleocene‐Eocene Thermal Maximum From ODP Site 690 (Weddell Sea) B. Hupp & D. Kelly 10.1029/2020PA004018
- Orbital phasing of the Paleocene-Eocene Thermal Maximum V. Piedrahita et al. 10.1016/j.epsl.2022.117839
- 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
- Spatiotemporal distribution of global mercury enrichments through the Paleocene-Eocene Thermal Maximum and links to volcanism S. Jin et al. 10.1016/j.earscirev.2023.104647
- Assessing the preservation of orbital signals across different sedimentary environments: Insights from stochastic sedimentation modeling M. Wang et al. 10.1016/j.epsl.2024.118866
- Dynamics of sediment flux to a bathyal continental margin section through the Paleocene–Eocene Thermal Maximum T. Dunkley Jones et al. 10.5194/cp-14-1035-2018
- Astronomical Pacing of Middle Eocene Sea‐Level Fluctuations: Inferences From Shallow‐Water Carbonate Ramp Deposits T. Brachert et al. 10.1029/2023PA004633
- The large decline in carbonate δ238U from a PETM section at Tingri (South Tibet) was driven by local sea-level changes, not global oceanic anoxia Q. Zhang et al. 10.1016/j.epsl.2023.118164
- Benthic foraminiferal turnover across the Dan-C2 event in the eastern South Atlantic Ocean (ODP Site 1262) G. Arreguín-Rodríguez et al. 10.1016/j.palaeo.2021.110410
- Carbon isotope and mammal recovery from extreme greenhouse warming at the Paleocene–Eocene boundary in astronomically-calibrated fluvial strata, Bighorn Basin, Wyoming, USA B. van der Meulen et al. 10.1016/j.epsl.2019.116044
- Surface ocean warming and acidification driven by rapid carbon release precedes Paleocene-Eocene Thermal Maximum T. Babila et al. 10.1126/sciadv.abg1025
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Discussed (final revised paper)
Discussed (preprint)
Latest update: 14 Dec 2024
Short summary
Here we present a high-resolution timescale synchronization of continental and marine deposits for one of the most pronounced global warming events, the Paleocene–Eocene Thermal Maximum, which occurred 56 million years ago. New high-resolution age models for the Bighorn Basin Coring Project (BBCP) drill cores help to improve age models for climate records from deep-sea drill cores and for the first time point to a concurrent major change in marine and terrestrial biota 54.25 million years ago.
Here we present a high-resolution timescale synchronization of continental and marine deposits...