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...
Published in: | Geological Magazine |
---|---|
Main Author: | |
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 |
id |
crcambridgeupr:10.1017/s0016756800025887 |
---|---|
record_format |
openpolar |
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 |
_version_ |
1792502622228316160 |