Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota
Carbon isotope and benthic foraminiferal data from Blake Outer Ridge, a sediment drift in the western North Atlantic (Ocean Drilling Program Sites 994 and 997, water depth ~ 2800 m), document variability in the relative volume of Southern Component (SCW) and Northern Component Waters (NCW) over the...
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ftindianacasci:oai:repository.ias.ac.in:63269 2023-05-15T17:34:39+02:00 Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen 2011-03-15 http://repository.ias.ac.in/63269/ http://www.sciencedirect.com/science/article/pii/S0031018211000599 unknown Elsevier Science Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen (2011) Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota Palaeogeography, Palaeoclimatology, Palaeoecology, 302 (3-4). pp. 435-451. ISSN 0031-0182 QE Geology Article PeerReviewed 2011 ftindianacasci 2013-01-20T12:22:22Z Carbon isotope and benthic foraminiferal data from Blake Outer Ridge, a sediment drift in the western North Atlantic (Ocean Drilling Program Sites 994 and 997, water depth ~ 2800 m), document variability in the relative volume of Southern Component (SCW) and Northern Component Waters (NCW) over the last 7 Ma. SCW was dominant before ~ 5.0 Ma, at ~ 3.6-2.4 Ma, and 1.2-0.8 Ma, whereas NCW dominated in the warm early Pliocene (5.0-3.6 Ma), and at 2.4-1.2 Ma. The relative volume of NCW and SCW fluctuated strongly over the last 0.8 Ma, with strong glacial-interglacial variability. The intensity of the Western Boundary Undercurrent was positively correlated to the relative volume of NCW. Values of Total Organic Carbon (TOC) were > 1.5% in sediments older than ~ 3.8 Ma, and not correlated to high primary productivity indicators, thus may reflect lateral transport of organic matter. TOC values decreased during the intensification of the Northern Hemisphere Glaciation (NHG, 3.8-1.8 Ma). Benthic foraminiferal assemblages underwent major changes when the sites were dominantly under SCW (3.6-2.4 and 1.2-0.8 Ma), coeval with the 'Last Global Extinction' of elongate, cylindrical deep-sea benthic foraminifera, which has been linked to cooling, increased ventilation and changes in the efficiency of the biological pump. These benthic foraminiferal turnovers were neither directly associated with changes in dominant bottom water mass nor with changes in productivity, but occurred during global cooling and increased ventilation of deep waters associated with the intensification of the NHG. Article in Journal/Newspaper North Atlantic Indian Academy of Sciences: Publication of Fellows |
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Indian Academy of Sciences: Publication of Fellows |
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ftindianacasci |
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unknown |
topic |
QE Geology |
spellingShingle |
QE Geology Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
topic_facet |
QE Geology |
description |
Carbon isotope and benthic foraminiferal data from Blake Outer Ridge, a sediment drift in the western North Atlantic (Ocean Drilling Program Sites 994 and 997, water depth ~ 2800 m), document variability in the relative volume of Southern Component (SCW) and Northern Component Waters (NCW) over the last 7 Ma. SCW was dominant before ~ 5.0 Ma, at ~ 3.6-2.4 Ma, and 1.2-0.8 Ma, whereas NCW dominated in the warm early Pliocene (5.0-3.6 Ma), and at 2.4-1.2 Ma. The relative volume of NCW and SCW fluctuated strongly over the last 0.8 Ma, with strong glacial-interglacial variability. The intensity of the Western Boundary Undercurrent was positively correlated to the relative volume of NCW. Values of Total Organic Carbon (TOC) were > 1.5% in sediments older than ~ 3.8 Ma, and not correlated to high primary productivity indicators, thus may reflect lateral transport of organic matter. TOC values decreased during the intensification of the Northern Hemisphere Glaciation (NHG, 3.8-1.8 Ma). Benthic foraminiferal assemblages underwent major changes when the sites were dominantly under SCW (3.6-2.4 and 1.2-0.8 Ma), coeval with the 'Last Global Extinction' of elongate, cylindrical deep-sea benthic foraminifera, which has been linked to cooling, increased ventilation and changes in the efficiency of the biological pump. These benthic foraminiferal turnovers were neither directly associated with changes in dominant bottom water mass nor with changes in productivity, but occurred during global cooling and increased ventilation of deep waters associated with the intensification of the NHG. |
format |
Article in Journal/Newspaper |
author |
Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen |
author_facet |
Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen |
author_sort |
Bhaumik, Ajoy K. |
title |
Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
title_short |
Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
title_full |
Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
title_fullStr |
Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
title_full_unstemmed |
Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota |
title_sort |
blake outer ridge: late neogene variability in paleoceanography and deep-sea biota |
publisher |
Elsevier Science |
publishDate |
2011 |
url |
http://repository.ias.ac.in/63269/ http://www.sciencedirect.com/science/article/pii/S0031018211000599 |
genre |
North Atlantic |
genre_facet |
North Atlantic |
op_relation |
Bhaumik, Ajoy K. Gupta, Anil K. Thomas, Ellen (2011) Blake Outer Ridge: late Neogene variability in paleoceanography and deep-sea biota Palaeogeography, Palaeoclimatology, Palaeoecology, 302 (3-4). pp. 435-451. ISSN 0031-0182 |
_version_ |
1766133549023363072 |