Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum-Reference-Cited by-同舟云学术

Extreme warmth and heat-stressed plankton in the tropics during the Paleocene-Eocene Thermal Maximum

Published:2017-03-03 Issue:3 Volume:3 Page:
ISSN:2375-2548
Container-title:Science Advances
language:en
Short-container-title:Sci. Adv.

Author:

Frieling Joost¹,Gebhardt Holger²,Huber Matthew³^ORCID,Adekeye Olabisi A.⁴,Akande Samuel O.⁴,Reichart Gert-Jan⁵⁶^ORCID,Middelburg Jack J.⁵^ORCID,Schouten Stefan⁵⁶^ORCID,Sluijs Appy¹

Affiliation:

1. Marine Palynology and Paleoceanography, Laboratory of Palaeobotany and Palynology, Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Heidelberglaan 2, 3584CS Utrecht, Netherlands.

2. Geologische Bundesanstalt, Neulinggasse 38, A 1030 Wien, Austria.

3. Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, IN 47906, USA.

4. Department of Geology and Mineral Sciences, University of Ilorin, P.M.B. 1515, Kwara State, Nigeria.

5. Department of Earth Sciences, Faculty of Geosciences, Utrecht University, Heidelberglaan 2, 3584CS Utrecht, Netherlands.

6. NIOZ Royal Netherlands Institute for Sea Research, Department of Marine Microbiology and Biogeochemistry, and Utrecht University, ’t Horntje, Texel, Netherlands.

Abstract

During rapid global warming 56 million years ago, tropical sea surface temperatures exceeded 36°C and stressed eukaryotic plankton.

Funder

European Research Council

Nederlandse Organisatie voor Wetenschappelijk Onderzoek

VW-Foundation

German Academic Exchange Service London

Nigerian Petroleum Technology Development Fund

Ministerie van Onderwijs, Cultuur en Wetenschap

Publisher

American Association for the Advancement of Science (AAAS)

Subject