High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water
The use of δ13C within foraminifera as a nutrient proxy is complicated by air-sea exchange processes that cause isotopic deviations due to equilibrium fractionation between the ocean and atmosphere. These effects can be resolved by the utilisation of proxies such as cadmium, which co-varies with pho...
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ftucambridgeesc:oai:eprints.esc.cam.ac.uk:2144 2023-05-15T13:55:44+02:00 High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water Cook, M.R. Elderfield, H. Zahn, R. Pahnke, K. 2006-08 application/pdf http://eprints.esc.cam.ac.uk/2144/ http://eprints.esc.cam.ac.uk/2144/1/Cook_Geochim_Acta_2006.pdf http://www.sciencedirect.com/science/article/pii/S001670370600411X en eng http://eprints.esc.cam.ac.uk/2144/1/Cook_Geochim_Acta_2006.pdf Cook, M.R. and Elderfield, H. and Zahn, R. and Pahnke, K. (2006) High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water. Geochimica et Cosmochimica Acta, 70 (18, Su). A109. 01 - Climate Change and Earth-Ocean Atmosphere Systems Article PeerReviewed 2006 ftucambridgeesc 2020-08-27T18:09:11Z The use of δ13C within foraminifera as a nutrient proxy is complicated by air-sea exchange processes that cause isotopic deviations due to equilibrium fractionation between the ocean and atmosphere. These effects can be resolved by the utilisation of proxies such as cadmium, which co-varies with phosphate in the modern ocean. Article in Journal/Newspaper Antarc* Antarctic University of Cambridge, Department of Earth Sciences: ESC Publications Antarctic |
institution |
Open Polar |
collection |
University of Cambridge, Department of Earth Sciences: ESC Publications |
op_collection_id |
ftucambridgeesc |
language |
English |
topic |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
spellingShingle |
01 - Climate Change and Earth-Ocean Atmosphere Systems Cook, M.R. Elderfield, H. Zahn, R. Pahnke, K. High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
topic_facet |
01 - Climate Change and Earth-Ocean Atmosphere Systems |
description |
The use of δ13C within foraminifera as a nutrient proxy is complicated by air-sea exchange processes that cause isotopic deviations due to equilibrium fractionation between the ocean and atmosphere. These effects can be resolved by the utilisation of proxies such as cadmium, which co-varies with phosphate in the modern ocean. |
format |
Article in Journal/Newspaper |
author |
Cook, M.R. Elderfield, H. Zahn, R. Pahnke, K. |
author_facet |
Cook, M.R. Elderfield, H. Zahn, R. Pahnke, K. |
author_sort |
Cook, M.R. |
title |
High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
title_short |
High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
title_full |
High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
title_fullStr |
High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
title_full_unstemmed |
High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water |
title_sort |
high resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in antarctic intermediate water |
publishDate |
2006 |
url |
http://eprints.esc.cam.ac.uk/2144/ http://eprints.esc.cam.ac.uk/2144/1/Cook_Geochim_Acta_2006.pdf http://www.sciencedirect.com/science/article/pii/S001670370600411X |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_relation |
http://eprints.esc.cam.ac.uk/2144/1/Cook_Geochim_Acta_2006.pdf Cook, M.R. and Elderfield, H. and Zahn, R. and Pahnke, K. (2006) High resolution trace metal analysis of benthic foraminifera reveal nutrient excursions in Antarctic Intermediate Water. Geochimica et Cosmochimica Acta, 70 (18, Su). A109. |
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1766262563274752000 |