CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE
International audience Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean 513C values were 0.46 ø/00 lower during the last glacial maximum than during the Late IIolocene. The geographic distribution of 5•3C was altered by changes in the product...
Published in: | Paleoceanography |
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Format: | Article in Journal/Newspaper |
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1988
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Online Access: | https://hal.science/hal-03550978 https://hal.science/hal-03550978/document https://hal.science/hal-03550978/file/Paleoceanography%20-%20June%201988%20-%20Curry%20-%20Changes%20in%20the%20distribution%20of%2013C%20of%20deep%20water%20CO2%20between%20the%20Last%20Glaciation.pdf https://doi.org/10.1029/PA003i003p00317 |
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ftccsdartic:oai:HAL:hal-03550978v1 2023-05-15T17:25:23+02:00 CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE Curry, W., Duplessy, J.C., Labeyrie, L., Shackleton, N. Woods Hole Oceanographic Institution (WHOI) Centre des Faibles Radioactivités Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS) Godwin Laboratory for Palaeoclimate Research Department of Earth Sciences Cambridge, UK University of Cambridge UK (CAM)-University of Cambridge UK (CAM) 1988-06 https://hal.science/hal-03550978 https://hal.science/hal-03550978/document https://hal.science/hal-03550978/file/Paleoceanography%20-%20June%201988%20-%20Curry%20-%20Changes%20in%20the%20distribution%20of%2013C%20of%20deep%20water%20CO2%20between%20the%20Last%20Glaciation.pdf https://doi.org/10.1029/PA003i003p00317 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/PA003i003p00317 hal-03550978 https://hal.science/hal-03550978 https://hal.science/hal-03550978/document https://hal.science/hal-03550978/file/Paleoceanography%20-%20June%201988%20-%20Curry%20-%20Changes%20in%20the%20distribution%20of%2013C%20of%20deep%20water%20CO2%20between%20the%20Last%20Glaciation.pdf doi:10.1029/PA003i003p00317 info:eu-repo/semantics/OpenAccess ISSN: 0883-8305 Paleoceanography https://hal.science/hal-03550978 Paleoceanography, 1988, 3 (3), pp.317-341. ⟨10.1029/PA003i003p00317⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 1988 ftccsdartic https://doi.org/10.1029/PA003i003p00317 2023-02-12T15:34:23Z International audience Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean 513C values were 0.46 ø/00 lower during the last glacial maximum than during the Late IIolocene. The geographic distribution of 5•3C was altered by changes in the production rate of nutrient-depleted deep water in the North Atlantic. During the Late Holocene, North Atlantic Deep Water, with high 513C values and low nutrient values, can be found throughout the Atlantic Ocean, and its effects can be traced into the southern ocean where it mixes with recirculated Pacific deep water. During the glaciation, decreased production of North Atlantic Deep Water allowed southern ocean deep water to penetrate farther into the North Atlantic and across low-latitude fracture zones into the eastern Atlantic. Mean southern ocean 5•3C values during the glaciation are lower than both North Atlantic and Pacific 5•3C values, suggesting that production of nutrient-depleted water occurred in both oceans during the glaciation. Enriched •3C values in shallow cores within the Atlantic Ocean indicate the existence of a nutrient-depleted water mass above 2000 m in this ocean. Article in Journal/Newspaper North Atlantic Deep Water North Atlantic Southern Ocean Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Pacific Southern Ocean Paleoceanography 3 3 317 341 |
institution |
Open Polar |
collection |
Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) |
op_collection_id |
ftccsdartic |
language |
English |
topic |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Curry, W., Duplessy, J.C., Labeyrie, L., Shackleton, N. CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience Carbon isotopic measurements on the benthic foraminiferal genus Cibicidoides document that mean deep ocean 513C values were 0.46 ø/00 lower during the last glacial maximum than during the Late IIolocene. The geographic distribution of 5•3C was altered by changes in the production rate of nutrient-depleted deep water in the North Atlantic. During the Late Holocene, North Atlantic Deep Water, with high 513C values and low nutrient values, can be found throughout the Atlantic Ocean, and its effects can be traced into the southern ocean where it mixes with recirculated Pacific deep water. During the glaciation, decreased production of North Atlantic Deep Water allowed southern ocean deep water to penetrate farther into the North Atlantic and across low-latitude fracture zones into the eastern Atlantic. Mean southern ocean 5•3C values during the glaciation are lower than both North Atlantic and Pacific 5•3C values, suggesting that production of nutrient-depleted water occurred in both oceans during the glaciation. Enriched •3C values in shallow cores within the Atlantic Ocean indicate the existence of a nutrient-depleted water mass above 2000 m in this ocean. |
author2 |
Woods Hole Oceanographic Institution (WHOI) Centre des Faibles Radioactivités Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Centre National de la Recherche Scientifique (CNRS) Godwin Laboratory for Palaeoclimate Research Department of Earth Sciences Cambridge, UK University of Cambridge UK (CAM)-University of Cambridge UK (CAM) |
format |
Article in Journal/Newspaper |
author |
Curry, W., Duplessy, J.C., Labeyrie, L., Shackleton, N. |
author_facet |
Curry, W., Duplessy, J.C., Labeyrie, L., Shackleton, N. |
author_sort |
Curry, W., |
title |
CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
title_short |
CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
title_full |
CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
title_fullStr |
CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
title_full_unstemmed |
CHANGES IN THE DISTRIBUTION OF 513C OF DEEP WATER ZCO2 BETWEEN THE LAST GLACIATION AND THE HOLOCENE |
title_sort |
changes in the distribution of 513c of deep water zco2 between the last glaciation and the holocene |
publisher |
HAL CCSD |
publishDate |
1988 |
url |
https://hal.science/hal-03550978 https://hal.science/hal-03550978/document https://hal.science/hal-03550978/file/Paleoceanography%20-%20June%201988%20-%20Curry%20-%20Changes%20in%20the%20distribution%20of%2013C%20of%20deep%20water%20CO2%20between%20the%20Last%20Glaciation.pdf https://doi.org/10.1029/PA003i003p00317 |
geographic |
Pacific Southern Ocean |
geographic_facet |
Pacific Southern Ocean |
genre |
North Atlantic Deep Water North Atlantic Southern Ocean |
genre_facet |
North Atlantic Deep Water North Atlantic Southern Ocean |
op_source |
ISSN: 0883-8305 Paleoceanography https://hal.science/hal-03550978 Paleoceanography, 1988, 3 (3), pp.317-341. ⟨10.1029/PA003i003p00317⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1029/PA003i003p00317 hal-03550978 https://hal.science/hal-03550978 https://hal.science/hal-03550978/document https://hal.science/hal-03550978/file/Paleoceanography%20-%20June%201988%20-%20Curry%20-%20Changes%20in%20the%20distribution%20of%2013C%20of%20deep%20water%20CO2%20between%20the%20Last%20Glaciation.pdf doi:10.1029/PA003i003p00317 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1029/PA003i003p00317 |
container_title |
Paleoceanography |
container_volume |
3 |
container_issue |
3 |
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317 |
op_container_end_page |
341 |
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1766116798556536832 |