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Geological evolution of the Hampshire Basin (southern England) during a global climate transition from ‘hothouse’ to ‘coolhouse’ in the Palaeogene

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Barnet_2023_GT_Geological_evolution_CC.pdf (4.577Mb)
Date
29/03/2023
Author
Barnet, James Stewart Kinmond
Keywords
QE Geology
3rd-DAS
SDG 13 - Climate Action
SDG 14 - Life Below Water
MCC
Metadata
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Abstract
Palaeogene sediments of the Hampshire Basin were a sensitive recorder of fluctuations in climate and eustatic sea level as Earth's climate transitioned from the global early Eocene ‘hothouse’ to the early Oligocene ‘coolhouse’, accompanied by the first permanent continent-scale glaciation of Antarctica at the Eocene/Oligocene boundary. A study of the Palaeogene sediments of the Hampshire Basin is not only interesting from a palaeoclimate perspective, but the marine middle Eocene formations are renowned for containing some of the most abundant and diverse Palaeogene fossil assemblages in the world. In this article, I take you on a tour of the geological evolution of the Hampshire Basin from the end of the Paleocene through to the Pleistocene. I highlight some of the best exposures where sediments can be studied at outcrop and representative fossil assemblages can be collected, along with the economic and archaeological significance of these Palaeogene sediments.
Citation
Barnet , J S K 2023 , ' Geological evolution of the Hampshire Basin (southern England) during a global climate transition from ‘hothouse’ to ‘coolhouse’ in the Palaeogene ' , Geology Today , vol. 39 , no. 2 , pp. 54-61 . https://doi.org/10.1111/gto.12423
Publication
Geology Today
Status
Peer reviewed
DOI
https://doi.org/10.1111/gto.12423
ISSN
0266-6979
Type
Journal article
Rights
Copyright © 2023 The Authors. Geology Today published by The Geological Society of London and The Geologists’ Association and John Wiley & Sons Ltd. This is an open access article under the terms of the Creative Commons Attribution License, which permits use, distribution and reproduction in any medium, provided the original work is properly cited.
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  • University of St Andrews Research
URI
http://hdl.handle.net/10023/27300

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