Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton
Variations in the assemblage and abundance of coccoliths reveal changes in oceanic and atmospheric dynamics in the Guyana Basin over the last climatic cycle, mainly linked to latitudinal variations in the ITCZ (Intertropical Convergence Zone). Records of the N ratio (a palaeoproductivity index of co...
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ftubarcepubl:oai:diposit.ub.edu:2445/120509 2024-02-11T10:04:53+01:00 Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton López-Otálvaro, G.E. Flores Villarejo, José Abel Sierro Sánchez, Francisco Javier Cacho Lascorz, Isabel Grimalt Obrador, Joan Michel, E. Cortijo, E. Labeyrie, L. 2009-04-02 13 p. application/pdf http://hdl.handle.net/2445/120509 eng eng Copernicus Publications Reproducció del document publicat a: https://doi.org/10.5194/ee-4-1-2009 eEarth, 2009, vol. 4, p. 1-13 Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) https://doi.org/10.5194/ee-4-1-2009 1815-381X http://hdl.handle.net/2445/120509 580260 cc-by (c) López-Otálvaro, G.E. et al., 2009 http://creativecommons.org/licenses/by/3.0/es info:eu-repo/semantics/openAccess Paleoclimatologia Guyana Paleoceanografia Plistocè Paleoclimatology Paleoceanography Pleistocene info:eu-repo/semantics/article info:eu-repo/semantics/publishedVersion 2009 ftubarcepubl https://doi.org/10.5194/ee-4-1-2009 2024-01-24T01:03:30Z Variations in the assemblage and abundance of coccoliths reveal changes in oceanic and atmospheric dynamics in the Guyana Basin over the last climatic cycle, mainly linked to latitudinal variations in the ITCZ (Intertropical Convergence Zone). Records of the N ratio (a palaeoproductivity index of coccolithophores) allowed us to monitor nutri-thermocline fluctuations. Nannofossil accumulation rates (NAR) vary closely with the N ratio, indicating a strong correlation between these two palaeoproductivity proxies. Decreases in the N ratio and NAR values suggest lower palaeoproductivity during glacial substages, indicating a deep nutri-thermocline (deep stratification of the mixed layer) as a consequence of the piling up of warm water dragged by the NEC. This setting was favoured by the southern shift of the ITCZ and Trade winds which blew perpendicular to the Guyana coast. By contrast, increases in the N ratio and NAR values revealed higher palaeoproductivity during interglacial substages, suggesting a shoaling of the nutri-thermocline. This scenario is favoured by a northward displacement of the ITCZ with the southeast Trade winds blowing alongshore. Additionally, palaeoproductivity changes during substages of Marine Isotope Stage (MIS) 6-5 are of much higher amplitude than those recorded in substages of MIS 4-2 and the early Holocene. Similarities between the palaeoproductivity and the 65° N summer insolation records, suggest a link between the depth of nutri-thermocline, the latitudinal migration of the ITCZ and ice-sheet changes in the Northern Hemisphere. Article in Journal/Newspaper Ice Sheet Dipòsit Digital de la Universitat de Barcelona eEarth 4 1 1 13 |
institution |
Open Polar |
collection |
Dipòsit Digital de la Universitat de Barcelona |
op_collection_id |
ftubarcepubl |
language |
English |
topic |
Paleoclimatologia Guyana Paleoceanografia Plistocè Paleoclimatology Paleoceanography Pleistocene |
spellingShingle |
Paleoclimatologia Guyana Paleoceanografia Plistocè Paleoclimatology Paleoceanography Pleistocene López-Otálvaro, G.E. Flores Villarejo, José Abel Sierro Sánchez, Francisco Javier Cacho Lascorz, Isabel Grimalt Obrador, Joan Michel, E. Cortijo, E. Labeyrie, L. Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
topic_facet |
Paleoclimatologia Guyana Paleoceanografia Plistocè Paleoclimatology Paleoceanography Pleistocene |
description |
Variations in the assemblage and abundance of coccoliths reveal changes in oceanic and atmospheric dynamics in the Guyana Basin over the last climatic cycle, mainly linked to latitudinal variations in the ITCZ (Intertropical Convergence Zone). Records of the N ratio (a palaeoproductivity index of coccolithophores) allowed us to monitor nutri-thermocline fluctuations. Nannofossil accumulation rates (NAR) vary closely with the N ratio, indicating a strong correlation between these two palaeoproductivity proxies. Decreases in the N ratio and NAR values suggest lower palaeoproductivity during glacial substages, indicating a deep nutri-thermocline (deep stratification of the mixed layer) as a consequence of the piling up of warm water dragged by the NEC. This setting was favoured by the southern shift of the ITCZ and Trade winds which blew perpendicular to the Guyana coast. By contrast, increases in the N ratio and NAR values revealed higher palaeoproductivity during interglacial substages, suggesting a shoaling of the nutri-thermocline. This scenario is favoured by a northward displacement of the ITCZ with the southeast Trade winds blowing alongshore. Additionally, palaeoproductivity changes during substages of Marine Isotope Stage (MIS) 6-5 are of much higher amplitude than those recorded in substages of MIS 4-2 and the early Holocene. Similarities between the palaeoproductivity and the 65° N summer insolation records, suggest a link between the depth of nutri-thermocline, the latitudinal migration of the ITCZ and ice-sheet changes in the Northern Hemisphere. |
format |
Article in Journal/Newspaper |
author |
López-Otálvaro, G.E. Flores Villarejo, José Abel Sierro Sánchez, Francisco Javier Cacho Lascorz, Isabel Grimalt Obrador, Joan Michel, E. Cortijo, E. Labeyrie, L. |
author_facet |
López-Otálvaro, G.E. Flores Villarejo, José Abel Sierro Sánchez, Francisco Javier Cacho Lascorz, Isabel Grimalt Obrador, Joan Michel, E. Cortijo, E. Labeyrie, L. |
author_sort |
López-Otálvaro, G.E. |
title |
Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
title_short |
Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
title_full |
Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
title_fullStr |
Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
title_full_unstemmed |
Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
title_sort |
late pleistocene palaeoproductivity patterns during the last climatic cycle in the guyana basin as revealed by calcareous nannoplankton |
publisher |
Copernicus Publications |
publishDate |
2009 |
url |
http://hdl.handle.net/2445/120509 |
genre |
Ice Sheet |
genre_facet |
Ice Sheet |
op_relation |
Reproducció del document publicat a: https://doi.org/10.5194/ee-4-1-2009 eEarth, 2009, vol. 4, p. 1-13 Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) https://doi.org/10.5194/ee-4-1-2009 1815-381X http://hdl.handle.net/2445/120509 580260 |
op_rights |
cc-by (c) López-Otálvaro, G.E. et al., 2009 http://creativecommons.org/licenses/by/3.0/es info:eu-repo/semantics/openAccess |
op_doi |
https://doi.org/10.5194/ee-4-1-2009 |
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eEarth |
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