Articles | Volume 11, issue 7
https://doi.org/10.5194/cp-11-1009-2015
© Author(s) 2015. 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-11-1009-2015
© Author(s) 2015. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
The Paleocene–Eocene Thermal Maximum at DSDP Site 277, Campbell Plateau, southern Pacific Ocean
GNS Science, Lower Hutt, New Zealand
B. R. Hines
School of Geography, Environment and Earth Sciences, Victoria University of Wellington, New Zealand
K. Littler
Earth and Planetary Sciences, University of California – Santa Cruz, California, USA
Camborne School of Mines, University of Exeter, Penryn Campus, Cornwall, UK
V. Villasante-Marcos
Observatorio Geofísico Central, Instituto Geográfico Nacional, Madrid, Spain
D. K. Kulhanek
International Ocean Discovery Program, Texas A&M University, College Station, Texas, USA
C. P. Strong
GNS Science, Lower Hutt, New Zealand
J. C. Zachos
Earth and Planetary Sciences, University of California – Santa Cruz, California, USA
S. M. Eggins
Research School of Earth Sciences, The Australian National University, Canberra, ACT, Australia
L. Northcote
National Institute of Water and Atmosphere, Wellington, New Zealand
A. Phillips
GNS Science, Lower Hutt, New Zealand
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34 citations as recorded by crossref.
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32 citations as recorded by crossref.
- Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum J. Frieling et al. 10.1126/sciadv.1600891
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- Radiolarian size and silicification across the Paleocene-Eocene boundary and into the early Eocene S. Westacott et al. 10.1016/j.palaeo.2022.111287
- Structure and magnitude of the carbon isotope excursion during the Paleocene-Eocene thermal maximum Q. Zhang et al. 10.1016/j.gr.2017.02.016
- Coupled decline in ocean pH and carbonate saturation during the Palaeocene–Eocene Thermal Maximum M. Li et al. 10.1038/s41561-024-01579-y
- Variations on a Pathway to an Early Eocene Climate M. Henry & G. Vallis 10.1029/2021PA004375
- Revisiting carbonate chemistry controls on planktic foraminifera Mg / Ca: implications for sea surface temperature and hydrology shifts over the Paleocene–Eocene Thermal Maximum and Eocene–Oligocene transition D. Evans et al. 10.5194/cp-12-819-2016
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- The PhanSST global database of Phanerozoic sea surface temperature proxy data E. Judd et al. 10.1038/s41597-022-01826-0
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- Eocene-Oligocene southwest Pacific Ocean paleoceanography new insights from foraminifera chemistry (DSDP site 277, Campbell Plateau) F. Hodel et al. 10.3389/feart.2022.998237
- Eocene calcareous nannofossils from southern Tibet: Paleoceanographic implications for the closure of the eastern Tethys Ocean K. Hoshina et al. 10.1016/j.marmicro.2021.102031
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2 citations as recorded by crossref.
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Latest update: 13 Dec 2024
Short summary
Re-examination of a Deep Sea Drilling Project sediment core (DSDP Site 277) from the western Campbell Plateau has identified the initial phase of the Paleocene-Eocene Thermal Maximum (PETM) within nannofossil chalk, the first record of the PETM in an oceanic setting in the southern Pacific Ocean (paleolatitude of ~65°S). Geochemical proxies indicate that intermediate and surface waters warmed by ~6° at the onset of the PETM prior to the full development of the negative δ13C excursion.
Re-examination of a Deep Sea Drilling Project sediment core (DSDP Site 277) from the western...