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Mesozoic climates and oceans – a tribute to Hugh Jenkyns and Helmut Weissert

Abstract:
The study of past greenhouse climate intervals in Earth history, such as the Mesozoic, is an important, relevant, and dynamic area of research for many sedimentary geologists, geochemists, palaeontologists and climate modellers. The Mesozoic sedimentary record provides key insights into the mechanics of how the Earth system works under warmer conditions, providing examples of natural climate change and perturbations to ocean chemistry, including anoxia, that are of societal relevance for understanding and contextualizing ongoing and future environmental problems. Furthermore, the deposition of widespread organic-carbon-rich sediments (“black shales”) during the Mesozoic means that this is an era of considerable economic interest. In July 2015, an international group of geoscientists attended a workshop in Ascona, Switzerland to discuss all aspects of the Mesozoic world and to celebrate the four-decade-long contributions to our understanding of this fascinating era in Earth history made by Hugh Jenkyns (University of Oxford) and Helmut Weissert (ETH Zurich). This volume of Sedimentology arose from that meeting and contains papers inspired by (and co-authored by!) Hugh and Helmi. Here a brief introduction to the volume is provided that reviews aspects of Hugh and Helmi's major achievements; contextualizes the papers of the Thematic Issue; and discusses some of the outstanding questions and areas for future research.
Publication status:
Published
Peer review status:
Peer reviewed

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Publisher copy:
10.1111/sed.12349

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Institution:
University of Oxford
Oxford college:
St Cross College
Role:
Author


Publisher:
Wiley
Journal:
Sedimentology More from this journal
Volume:
64
Issue:
1
Pages:
1-15
Publication date:
2017-01-01
Acceptance date:
2016-11-21
DOI:
ISSN:
0037-0746 and 1365-3091


Keywords:
Pubs id:
pubs:671546
UUID:
uuid:3a37ec15-7758-4a32-8d57-f8bdac66611f
Local pid:
pubs:671546
Source identifiers:
671546
Deposit date:
2017-02-14

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