Eocene-Oligocene boundary in New Zealand

The planktonic foraminifera Hantkenina, Globigerapsis and Pseudohastigerina micra are widely distributed throughout the world and their last appearance has generally been considered to mark the top of the Eocene. Hornibrook stated that H. alabamensis, G. index and P. micra make their last appearance...

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Bibliographic Details
Main Author: Srinivasan, M. S.
Format: Article in Journal/Newspaper
Language:unknown
Published: Nature Publishing Group 1965
Subjects:
QE Geology
New Zealand
Planktonic foraminifera
Online Access:http://repository.ias.ac.in/51168/
http://www.nature.com/nature/journal/v207/n4996/abs/207514a0.html
id ftindianacasci:oai:repository.ias.ac.in:51168
record_format openpolar
spelling ftindianacasci:oai:repository.ias.ac.in:51168 2023-05-15T18:00:30+02:00 Eocene-Oligocene boundary in New Zealand Srinivasan, M. S. 1965-07-31 http://repository.ias.ac.in/51168/ http://www.nature.com/nature/journal/v207/n4996/abs/207514a0.html unknown Nature Publishing Group Srinivasan, M. S. (1965) Eocene-Oligocene boundary in New Zealand Nature, 207 . pp. 514-515. ISSN 0028-0836 QE Geology Article PeerReviewed 1965 ftindianacasci 2013-01-20T11:47:58Z The planktonic foraminifera Hantkenina, Globigerapsis and Pseudohastigerina micra are widely distributed throughout the world and their last appearance has generally been considered to mark the top of the Eocene. Hornibrook stated that H. alabamensis, G. index and P. micra make their last appearance in the Runangan Stage, and consequently regarded the Runangan-Whaingaroan boundary as the Eocene-Oligocene boundary in New Zealand. Article in Journal/Newspaper Planktonic foraminifera Indian Academy of Sciences: Publication of Fellows New Zealand
institution Open Polar
collection Indian Academy of Sciences: Publication of Fellows
op_collection_id ftindianacasci
language unknown
topic QE Geology
spellingShingle QE Geology
Srinivasan, M. S.
Eocene-Oligocene boundary in New Zealand
topic_facet QE Geology
description The planktonic foraminifera Hantkenina, Globigerapsis and Pseudohastigerina micra are widely distributed throughout the world and their last appearance has generally been considered to mark the top of the Eocene. Hornibrook stated that H. alabamensis, G. index and P. micra make their last appearance in the Runangan Stage, and consequently regarded the Runangan-Whaingaroan boundary as the Eocene-Oligocene boundary in New Zealand.
format Article in Journal/Newspaper
author Srinivasan, M. S.
author_facet Srinivasan, M. S.
author_sort Srinivasan, M. S.
title Eocene-Oligocene boundary in New Zealand
title_short Eocene-Oligocene boundary in New Zealand
title_full Eocene-Oligocene boundary in New Zealand
title_fullStr Eocene-Oligocene boundary in New Zealand
title_full_unstemmed Eocene-Oligocene boundary in New Zealand
title_sort eocene-oligocene boundary in new zealand
publisher Nature Publishing Group
publishDate 1965
url http://repository.ias.ac.in/51168/
http://www.nature.com/nature/journal/v207/n4996/abs/207514a0.html
geographic New Zealand
geographic_facet New Zealand
genre Planktonic foraminifera
genre_facet Planktonic foraminifera
op_relation Srinivasan, M. S. (1965) Eocene-Oligocene boundary in New Zealand Nature, 207 . pp. 514-515. ISSN 0028-0836
_version_ 1766169611863064576

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