Please use this identifier to cite or link to this item:
http://hdl.handle.net/2445/120509
Title: | Late Pleistocene palaeoproductivity patterns during the last climatic cycle in the Guyana Basin as revealed by calcareous nannoplankton |
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. |
Keywords: | Paleoclimatologia Guyana Paleoceanografia Plistocè Paleoclimatology Guyana Paleoceanography Pleistocene |
Issue Date: | 2-Apr-2009 |
Publisher: | Copernicus Publications |
Abstract: | 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. |
Note: | Reproducció del document publicat a: https://doi.org/10.5194/ee-4-1-2009 |
It is part of: | eEarth, 2009, vol. 4, p. 1-13 |
URI: | http://hdl.handle.net/2445/120509 |
Related resource: | https://doi.org/10.5194/ee-4-1-2009 |
ISSN: | 1815-381X |
Appears in Collections: | Articles publicats en revistes (Dinàmica de la Terra i l'Oceà) |
Files in This Item:
File | Description | Size | Format | |
---|---|---|---|---|
580260.pdf | 1.22 MB | Adobe PDF | View/Open |
This item is licensed under a Creative Commons License