Palaeontology: Plankton in a greenhouse world

The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals.

Bibliographic Details
Published in:Nature Geoscience
Main Author: Langer, Gerald
Format: Article in Journal/Newspaper
Language:English
Published: 2013
Subjects:
04 - Palaeobiology
Ocean acidification
Online Access:http://eprints.esc.cam.ac.uk/2687/
http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf
http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg
http://www.nature.com/ngeo/journal/v6/n3/full/ngeo1750.html
https://doi.org/10.1038/ngeo1750
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spelling ftucambridgeesc:oai:eprints.esc.cam.ac.uk:2687 2023-05-15T17:49:45+02:00 Palaeontology: Plankton in a greenhouse world Langer, Gerald 2013-03 application/pdf image/jpeg http://eprints.esc.cam.ac.uk/2687/ http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg http://www.nature.com/ngeo/journal/v6/n3/full/ngeo1750.html https://doi.org/10.1038/ngeo1750 en eng http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg Langer, Gerald (2013) Palaeontology: Plankton in a greenhouse world. Nature Geoscience, 6 (3). pp. 164-165. ISSN 1752-0894, 1752-0908 DOI https://doi.org/10.1038/ngeo1750 <https://doi.org/10.1038/ngeo1750> 04 - Palaeobiology Article PeerReviewed 2013 ftucambridgeesc https://doi.org/10.1038/ngeo1750 2020-08-27T18:09:21Z The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals. Article in Journal/Newspaper Ocean acidification University of Cambridge, Department of Earth Sciences: ESC Publications Nature Geoscience 6 3 164 165
institution Open Polar
collection University of Cambridge, Department of Earth Sciences: ESC Publications
op_collection_id ftucambridgeesc
language English
topic 04 - Palaeobiology
spellingShingle 04 - Palaeobiology
Langer, Gerald
Palaeontology: Plankton in a greenhouse world
topic_facet 04 - Palaeobiology
description The Palaeocene–Eocene Thermal Maximum was marked by global warming and ocean acidification. Fossil and experimental analyses show that different species of marine calcifying algae responded very differently to the environmental upheavals.
format Article in Journal/Newspaper
author Langer, Gerald
author_facet Langer, Gerald
author_sort Langer, Gerald
title Palaeontology: Plankton in a greenhouse world
title_short Palaeontology: Plankton in a greenhouse world
title_full Palaeontology: Plankton in a greenhouse world
title_fullStr Palaeontology: Plankton in a greenhouse world
title_full_unstemmed Palaeontology: Plankton in a greenhouse world
title_sort palaeontology: plankton in a greenhouse world
publishDate 2013
url http://eprints.esc.cam.ac.uk/2687/
http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf
http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg
http://www.nature.com/ngeo/journal/v6/n3/full/ngeo1750.html
https://doi.org/10.1038/ngeo1750
genre Ocean acidification
genre_facet Ocean acidification
op_relation http://eprints.esc.cam.ac.uk/2687/1/Langer_ngeo1750.pdf
http://eprints.esc.cam.ac.uk/2687/2/Langer_ngeo1750-f1.jpg
Langer, Gerald (2013) Palaeontology: Plankton in a greenhouse world. Nature Geoscience, 6 (3). pp. 164-165. ISSN 1752-0894, 1752-0908 DOI https://doi.org/10.1038/ngeo1750 <https://doi.org/10.1038/ngeo1750>
op_doi https://doi.org/10.1038/ngeo1750
container_title Nature Geoscience
container_volume 6
container_issue 3
container_start_page 164
op_container_end_page 165
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