The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera

Summary Planktonic foraminifera are recorded for the first time from the St Erth Beds but they are small and very rare. A late Pliocene G. inflaia Zone age is postulated on the presence of Globorotalia inflata and dextrally coiled Neogloboquadrina pachyderma . It is suggested that the depth of water...

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Published in:Geological Magazine
Main Author: Graham Jenkins, D.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1982
Subjects:
Online Access:http://dx.doi.org/10.1017/s0016756800025887
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800025887
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spelling crcambridgeupr:10.1017/s0016756800025887 2024-03-03T08:46:34+00:00 The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera Graham Jenkins, D. 1982 http://dx.doi.org/10.1017/s0016756800025887 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800025887 en eng Cambridge University Press (CUP) https://www.cambridge.org/core/terms Geological Magazine volume 119, issue 2, page 201-205 ISSN 0016-7568 1469-5081 Geology journal-article 1982 crcambridgeupr https://doi.org/10.1017/s0016756800025887 2024-02-08T08:27:06Z Summary Planktonic foraminifera are recorded for the first time from the St Erth Beds but they are small and very rare. A late Pliocene G. inflaia Zone age is postulated on the presence of Globorotalia inflata and dextrally coiled Neogloboquadrina pachyderma . It is suggested that the depth of water at the time of deposition was much less than 100 m, possibly in the photic zone, and the palaeotemperature was in the range of 10–18 °C. Article in Journal/Newspaper Neogloboquadrina pachyderma Planktonic foraminifera Cambridge University Press Geological Magazine 119 2 201 205
institution Open Polar
collection Cambridge University Press
op_collection_id crcambridgeupr
language English
topic Geology
spellingShingle Geology
Graham Jenkins, D.
The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
topic_facet Geology
description Summary Planktonic foraminifera are recorded for the first time from the St Erth Beds but they are small and very rare. A late Pliocene G. inflaia Zone age is postulated on the presence of Globorotalia inflata and dextrally coiled Neogloboquadrina pachyderma . It is suggested that the depth of water at the time of deposition was much less than 100 m, possibly in the photic zone, and the palaeotemperature was in the range of 10–18 °C.
format Article in Journal/Newspaper
author Graham Jenkins, D.
author_facet Graham Jenkins, D.
author_sort Graham Jenkins, D.
title The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
title_short The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
title_full The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
title_fullStr The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
title_full_unstemmed The age and palaeoecology of the St Erth Beds, southern England, based on planktonic foraminifera
title_sort age and palaeoecology of the st erth beds, southern england, based on planktonic foraminifera
publisher Cambridge University Press (CUP)
publishDate 1982
url http://dx.doi.org/10.1017/s0016756800025887
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0016756800025887
genre Neogloboquadrina pachyderma
Planktonic foraminifera
genre_facet Neogloboquadrina pachyderma
Planktonic foraminifera
op_source Geological Magazine
volume 119, issue 2, page 201-205
ISSN 0016-7568 1469-5081
op_rights https://www.cambridge.org/core/terms
op_doi https://doi.org/10.1017/s0016756800025887
container_title Geological Magazine
container_volume 119
container_issue 2
container_start_page 201
op_container_end_page 205
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