Articles | Volume 14, issue 1
https://doi.org/10.5194/cp-14-39-2018
© 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-14-39-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Tropical Atlantic climate and ecosystem regime shifts during the Paleocene–Eocene Thermal Maximum
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany
and Palynology, Department of Earth Sciences, Faculty of Geosciences,
Utrecht University, Heidelberglaan 2, 3584CS Utrecht, the Netherlands
Gert-Jan Reichart
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Princetonplein 9, 3584CC Utrecht, the Netherlands
NIOZ Royal Netherlands Institute for Sea Research, 1790AB Den Burg,
Texel, the Netherlands
Jack J. Middelburg
Department of Earth Sciences, Faculty of Geosciences, Utrecht
University, Princetonplein 9, 3584CC Utrecht, the Netherlands
Ursula Röhl
MARUM – Center for Marine Environmental Sciences, University of
Bremen, Leobener Straße 8, 28359, Bremen, Germany
Thomas Westerhold
MARUM – Center for Marine Environmental Sciences, University of
Bremen, Leobener Straße 8, 28359, Bremen, Germany
Steven M. Bohaty
Ocean and Earth Science, National Oceanography Centre Southampton,
University of Southampton, Waterfront Campus European Way Southampton, SO14
3ZH, UK
Appy Sluijs
Marine Palynology and Paleoceanography, Laboratory of Palaeobotany
and Palynology, Department of Earth Sciences, Faculty of Geosciences,
Utrecht University, Heidelberglaan 2, 3584CS Utrecht, the Netherlands
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- Record of Early to Middle Eocene paleoenvironmental changes from lignite mines, western India S. Khanolkar & J. Sharma
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- An early Cambrian greenhouse climate T. Hearing et al.
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- Palynology from ground zero of the Chicxulub impact, southern Gulf of Mexico V. Smith et al.
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- Synchronous tropical and polar temperature evolution in the Eocene M. Cramwinckel et al.
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- Cenozoic evolution of deep ocean temperature from clumped isotope thermometry A. Meckler et al.
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- Life and death in the Chicxulub impact crater: a record of the Paleocene–Eocene Thermal Maximum V. Smith et al.
- A high-resolution late Paleocene–early Eocene organic-walled dinoflagellate cyst zonation of the United States Atlantic Coastal Plain M. Nelissen et al.
- High Arctic late Paleocene and early Eocene dinoflagellate cysts A. Sluijs & H. Brinkhuis
- A review of the ecological affinities of marine organic microfossils from a Holocene record offshore of Adélie Land (East Antarctica) J. Hartman et al.
- Bartonian to Priabonian dinoflagellate cyst biostratigraphy and paleoenvironments of the M'karcha section in the Southern Tethys margin (Rif Chain, Northern Morocco) H. Slimani et al.
- The Paleocene–Eocene Thermal Maximum (PETM) interval in the southwestern Mediterranean Tethys at Morocco: New data from a high-resolution study of dinoflagellate cysts and palynofacies in the Rif Chain S. Aboutofail & H. Slimani
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- Environmental changes occurred during the Early Danian at the Rio Grande Rise, South Atlantic Ocean G. Krahl et al.
- Photosymbiosis in planktonic foraminifera across the Paleocene–Eocene thermal maximum J. Shaw et al.
- The future extent of the Anthropocene epoch: A synthesis C. Summerhayes et al.
- Simulation of Eocene extreme warmth and high climate sensitivity through cloud feedbacks J. Zhu et al.
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Saved (final revised paper)
Latest update: 06 May 2026
Short summary
Past periods of rapid global warming such as the Paleocene–Eocene Thermal Maximum are used to study biotic response to climate change. We show that very high peak PETM temperatures in the tropical Atlantic (~ 37 ºC) caused heat stress in several marine plankton groups. However, only slightly cooler temperatures afterwards allowed highly diverse plankton communities to bloom. This shows that tropical plankton communities may be susceptible to extreme warming, but may also recover rapidly.
Past periods of rapid global warming such as the Paleocene–Eocene Thermal Maximum are used to...