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The palaeoclimatic significance of the Devonian-Carboniferous boundary

The palaeoclimatic significance of the Devonian-Carboniferous boundary
The palaeoclimatic significance of the Devonian-Carboniferous boundary
PALAEOCLIMATE, CLIMATIC CHANGES, GEOLOGY
p.103
Marshall, J.E.A.
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Astin, T.R.
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Evans, F.
d568907f-a84d-461a-89f5-748b7207f712
Almond, J.
22c190de-0e99-4c4a-81c9-696bb4a56ad3
Marshall, J.E.A.
cba178e3-91aa-49a2-b2ce-4b8d9d870b06
Astin, T.R.
5e5a163d-19b8-42ec-8b5a-2f87cef476c3
Evans, F.
d568907f-a84d-461a-89f5-748b7207f712
Almond, J.
22c190de-0e99-4c4a-81c9-696bb4a56ad3

Marshall, J.E.A., Astin, T.R., Evans, F. and Almond, J. (2002) The palaeoclimatic significance of the Devonian-Carboniferous boundary. Palaeontology Newsletter, 51, p.103.

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More information

Published date: 2002
Keywords: PALAEOCLIMATE, CLIMATIC CHANGES, GEOLOGY

Identifiers

Local EPrints ID: 2197
URI: http://eprints.soton.ac.uk/id/eprint/2197
PURE UUID: 482c7480-96e0-481a-baeb-bdd3b2f4d224
ORCID for J.E.A. Marshall: ORCID iD orcid.org/0000-0002-9242-3646

Catalogue record

Date deposited: 17 May 2004
Last modified: 10 Nov 2021 02:35

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Contributors

Author: J.E.A. Marshall ORCID iD
Author: T.R. Astin
Author: F. Evans
Author: J. Almond

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