Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential

Surface sediment samples taken with a multiple corer from the Polar Front region along two profiles in the eastern South Atlantic sector between 35° and 57°S have been investigated for their benthic foraminiferal content. Live fauna was differentiated from the death assemblage. Based on the dead ass...

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Published in:Marine Micropaleontology
Main Authors: Mackensen, Andreas, Fütterer, Dieter, Grobe, Hannes, Schmiedl, G.
Format: Article in Journal/Newspaper
Language:unknown
Published: 1993
Subjects:
Online Access:https://epic.awi.de/id/eprint/2026/
https://doi.org/10.1016/0377-8398(93)90003-G
https://hdl.handle.net/10013/epic.12617
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spelling ftawi:oai:epic.awi.de:2026 2023-09-05T13:13:23+02:00 Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential Mackensen, Andreas Fütterer, Dieter Grobe, Hannes Schmiedl, G. 1993 https://epic.awi.de/id/eprint/2026/ https://doi.org/10.1016/0377-8398(93)90003-G https://hdl.handle.net/10013/epic.12617 unknown Mackensen, A. orcid:0000-0002-5024-4455 , Fütterer, D. , Grobe, H. orcid:0000-0002-4133-2218 and Schmiedl, G. (1993) Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential , Marine micropaleontology, 22 , pp. 33-69 . doi:10.1016/0377-8398(93)90003-G <https://doi.org/10.1016/0377-8398%2893%2990003-G> , hdl:10013/epic.12617 EPIC3Marine micropaleontology, 22, pp. 33-69 Article isiRev 1993 ftawi https://doi.org/10.1016/0377-8398(93)90003-G 2023-08-22T19:43:04Z Surface sediment samples taken with a multiple corer from the Polar Front region along two profiles in the eastern South Atlantic sector between 35° and 57°S have been investigated for their benthic foraminiferal content. Live fauna was differentiated from the death assemblage. Based on the dead assemblages, potential fossil assemblages (dead fauna reduced by non-resistant agglutinants) were calculated for comparison with upper Neogene core material.The distribution of the potential fossil assemblages defined by Q-mode principal component analysis mirrors the Recent hydrographic, as well as the trophic situation in the eastern South Atlantic (ocean circulation and productivity).Two Southern Component Bottom Water Faunas reflect the northward flow of Antarctic Bottom Water (AABW) and Lower Circum-Polar Deep Water (LCDW): an assemblage dominated by the arenaceous Multifidella nodulosa below the Calcite Compensation Depth (CCD), and a Nuttallides umbonifer dominated assemblage above the CCD. In the region of highest bio-silicious primary productivity, south of the Polar Front and north of the winter sea-ice limit, these faunas are overprinted by a Southern High-productivity Fauna, dominated by infaunal species such as Pullenia bulloides, Melonis pompilioides and M. zaandamae.North Atlantic Deep Water (NADW) meets the Circum-Polar Deep Water (CDW) at intermediate depth, as reflected in the distribution of the Northern Component Deep Water Fauna, dominated by Epistominella exigua. The high-productivity assemblage overprinting this fauna, the Northern High-productivity Fauna, is dominated by the shallow endobenthic Bulimina aculeata.A Strong Bottom-current Fauna, dominated by Angulogerina angulosa, characterizes areas between 400 and 900 m water depth with sandy sediment, independent from water mass characteristics and food supply. Article in Journal/Newspaper Antarc* Antarctic NADW Sea ice South Atlantic Ocean Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center) Antarctic Marine Micropaleontology 22 1-2 33 69
institution Open Polar
collection Alfred Wegener Institute for Polar- and Marine Research (AWI): ePIC (electronic Publication Information Center)
op_collection_id ftawi
language unknown
description Surface sediment samples taken with a multiple corer from the Polar Front region along two profiles in the eastern South Atlantic sector between 35° and 57°S have been investigated for their benthic foraminiferal content. Live fauna was differentiated from the death assemblage. Based on the dead assemblages, potential fossil assemblages (dead fauna reduced by non-resistant agglutinants) were calculated for comparison with upper Neogene core material.The distribution of the potential fossil assemblages defined by Q-mode principal component analysis mirrors the Recent hydrographic, as well as the trophic situation in the eastern South Atlantic (ocean circulation and productivity).Two Southern Component Bottom Water Faunas reflect the northward flow of Antarctic Bottom Water (AABW) and Lower Circum-Polar Deep Water (LCDW): an assemblage dominated by the arenaceous Multifidella nodulosa below the Calcite Compensation Depth (CCD), and a Nuttallides umbonifer dominated assemblage above the CCD. In the region of highest bio-silicious primary productivity, south of the Polar Front and north of the winter sea-ice limit, these faunas are overprinted by a Southern High-productivity Fauna, dominated by infaunal species such as Pullenia bulloides, Melonis pompilioides and M. zaandamae.North Atlantic Deep Water (NADW) meets the Circum-Polar Deep Water (CDW) at intermediate depth, as reflected in the distribution of the Northern Component Deep Water Fauna, dominated by Epistominella exigua. The high-productivity assemblage overprinting this fauna, the Northern High-productivity Fauna, is dominated by the shallow endobenthic Bulimina aculeata.A Strong Bottom-current Fauna, dominated by Angulogerina angulosa, characterizes areas between 400 and 900 m water depth with sandy sediment, independent from water mass characteristics and food supply.
format Article in Journal/Newspaper
author Mackensen, Andreas
Fütterer, Dieter
Grobe, Hannes
Schmiedl, G.
spellingShingle Mackensen, Andreas
Fütterer, Dieter
Grobe, Hannes
Schmiedl, G.
Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
author_facet Mackensen, Andreas
Fütterer, Dieter
Grobe, Hannes
Schmiedl, G.
author_sort Mackensen, Andreas
title Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
title_short Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
title_full Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
title_fullStr Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
title_full_unstemmed Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential
title_sort benthic foraminiferal assemblages from the eastern south atlantic polar front region between 35° and 57°s: distribution, ecology and fossilization potential
publishDate 1993
url https://epic.awi.de/id/eprint/2026/
https://doi.org/10.1016/0377-8398(93)90003-G
https://hdl.handle.net/10013/epic.12617
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
NADW
Sea ice
South Atlantic Ocean
genre_facet Antarc*
Antarctic
NADW
Sea ice
South Atlantic Ocean
op_source EPIC3Marine micropaleontology, 22, pp. 33-69
op_relation Mackensen, A. orcid:0000-0002-5024-4455 , Fütterer, D. , Grobe, H. orcid:0000-0002-4133-2218 and Schmiedl, G. (1993) Benthic foraminiferal assemblages from the eastern South Atlantic Polar Front region between 35° and 57°S: Distribution, ecology and fossilization potential , Marine micropaleontology, 22 , pp. 33-69 . doi:10.1016/0377-8398(93)90003-G <https://doi.org/10.1016/0377-8398%2893%2990003-G> , hdl:10013/epic.12617
op_doi https://doi.org/10.1016/0377-8398(93)90003-G
container_title Marine Micropaleontology
container_volume 22
container_issue 1-2
container_start_page 33
op_container_end_page 69
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