Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments

The modern Atlantic Ocean, dominated by the interactions of North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW), plays a key role in redistributing heat from the Southern to the Northern Hemisphere. In order to reconstruct the evolution of the relative importance of these two water ma...

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Bibliographic Details
Main Authors: Volbers, Andrea N A, Henrich, Rüdiger
Format: Other/Unknown Material
Language:English
Published: PANGAEA 2004
Subjects:
06MT15_2
06MT41_3
Amazon Fan
Angola Basin
Ascencion Island
Brazil Basin
Cape Basin
Cardno Seamount
Ceara Rise
Continental Slope off Rio Paraiba do Sul
East Brazil Basin
Eastern Rio Grande Rise
Equatorial Atlantic
GeoB
GeoB1028-5
GeoB1031-4
GeoB1032-3
GeoB1041-3
GeoB1047-3
GeoB1048-2
GeoB1101-5
GeoB1105-4
GeoB1112-4
GeoB1114-3
GeoB1117-2
GeoB1117-3
GeoB1118-2
GeoB1119-2
GeoB1120-3
GeoB1214-1
GeoB1220-1
GeoB1309-2
GeoB1310-1
GeoB1311-2
GeoB1315-2
GeoB1408-2
GeoB1417-1
GeoB1418-1
GeoB1419-1
GeoB1419-2
GeoB1420-1
GeoB1421-1
GeoB1501-4
GeoB1503-1
GeoB1505-1
GeoB1508-4
GeoB1515-1
GeoB1523-1
GeoB1523-2
GeoB1701-4
Antarc*
Antarctic
NADW
North Atlantic Deep Water
North Atlantic
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.735719
https://doi.org/10.1594/PANGAEA.735719
id ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.735719
record_format openpolar
spelling ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.735719 2024-09-15T17:43:32+00:00 Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments Volbers, Andrea N A Henrich, Rüdiger MEDIAN LATITUDE: -17.040875 * MEDIAN LONGITUDE: -24.991789 * SOUTH-BOUND LATITUDE: -37.831667 * WEST-BOUND LONGITUDE: -53.703333 * NORTH-BOUND LATITUDE: 29.176667 * EAST-BOUND LONGITUDE: 17.543333 * DATE/TIME START: 1988-03-02T00:00:00 * DATE/TIME END: 1998-05-09T23:22:00 2004 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.735719 https://doi.org/10.1594/PANGAEA.735719 en eng PANGAEA Volbers, Andrea N A (2001): Planktic foraminifera as paleoceangraphic indicators: Production, preservation, and reconstruction of upwelling intensity. Implications from late quarternary South Atlantic sediments. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 184, 114 pp, urn:nbn:de:gbv:46-00101382-15 https://doi.pangaea.de/10.1594/PANGAEA.735719 https://doi.org/10.1594/PANGAEA.735719 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess Supplement to: Volbers, Andrea N A; Henrich, Rüdiger (2004): Calcium carbonate corrosiveness in the South Atlantic during the Last Glacial Maximum as inferred from changes in the preservation of Globigerina bulloides: A proxy to determine deep-water circulation patterns? Marine Geology, 204(1-2), 43-57, https://doi.org/10.1016/S0025-3227(03)00372-4 06MT15_2 06MT41_3 Amazon Fan Angola Basin Ascencion Island Brazil Basin Cape Basin Cardno Seamount Ceara Rise Continental Slope off Rio Paraiba do Sul East Brazil Basin Eastern Rio Grande Rise Equatorial Atlantic GeoB GeoB1028-5 GeoB1031-4 GeoB1032-3 GeoB1041-3 GeoB1047-3 GeoB1048-2 GeoB1101-5 GeoB1105-4 GeoB1112-4 GeoB1114-3 GeoB1117-2 GeoB1117-3 GeoB1118-2 GeoB1119-2 GeoB1120-3 GeoB1214-1 GeoB1220-1 GeoB1309-2 GeoB1310-1 GeoB1311-2 GeoB1315-2 GeoB1408-2 GeoB1417-1 GeoB1418-1 GeoB1419-1 GeoB1419-2 GeoB1420-1 GeoB1421-1 GeoB1501-4 GeoB1503-1 GeoB1505-1 GeoB1508-4 GeoB1515-1 GeoB1523-1 GeoB1523-2 GeoB1701-4 dataset publication series 2004 ftpangaea https://doi.org/10.1594/PANGAEA.73571910.1016/S0025-3227(03)00372-4 2024-07-24T02:31:20Z The modern Atlantic Ocean, dominated by the interactions of North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW), plays a key role in redistributing heat from the Southern to the Northern Hemisphere. In order to reconstruct the evolution of the relative importance of these two water masses, the NADW/AABW transition, reflected by the calcite lysocline, was investigated by the Globigerina bulloides dissolution index (BDX?). The depth level of the Late Glacial Maximum (LGM) calcite lysocline was elevated by several hundred metres, indicating a more corrosive water mass present at modern NADW level. Overall, the small range of BDX? data and the gradual decrease in preservation below the calcite lysocline point to a less stratified Atlantic Ocean during the LGM. Similar preservation patterns in the West and East Atlantic demonstrate that the modern west–east asymmetry did not exist due to an expansion of southern deep waters compensating for the decrease in NADW formation. Other/Unknown Material Antarc* Antarctic NADW North Atlantic Deep Water North Atlantic PANGAEA - Data Publisher for Earth & Environmental Science ENVELOPE(-53.703333,17.543333,29.176667,-37.831667)
institution Open Polar
collection PANGAEA - Data Publisher for Earth & Environmental Science
op_collection_id ftpangaea
language English
topic 06MT15_2
06MT41_3
Amazon Fan
Angola Basin
Ascencion Island
Brazil Basin
Cape Basin
Cardno Seamount
Ceara Rise
Continental Slope off Rio Paraiba do Sul
East Brazil Basin
Eastern Rio Grande Rise
Equatorial Atlantic
GeoB
GeoB1028-5
GeoB1031-4
GeoB1032-3
GeoB1041-3
GeoB1047-3
GeoB1048-2
GeoB1101-5
GeoB1105-4
GeoB1112-4
GeoB1114-3
GeoB1117-2
GeoB1117-3
GeoB1118-2
GeoB1119-2
GeoB1120-3
GeoB1214-1
GeoB1220-1
GeoB1309-2
GeoB1310-1
GeoB1311-2
GeoB1315-2
GeoB1408-2
GeoB1417-1
GeoB1418-1
GeoB1419-1
GeoB1419-2
GeoB1420-1
GeoB1421-1
GeoB1501-4
GeoB1503-1
GeoB1505-1
GeoB1508-4
GeoB1515-1
GeoB1523-1
GeoB1523-2
GeoB1701-4
spellingShingle 06MT15_2
06MT41_3
Amazon Fan
Angola Basin
Ascencion Island
Brazil Basin
Cape Basin
Cardno Seamount
Ceara Rise
Continental Slope off Rio Paraiba do Sul
East Brazil Basin
Eastern Rio Grande Rise
Equatorial Atlantic
GeoB
GeoB1028-5
GeoB1031-4
GeoB1032-3
GeoB1041-3
GeoB1047-3
GeoB1048-2
GeoB1101-5
GeoB1105-4
GeoB1112-4
GeoB1114-3
GeoB1117-2
GeoB1117-3
GeoB1118-2
GeoB1119-2
GeoB1120-3
GeoB1214-1
GeoB1220-1
GeoB1309-2
GeoB1310-1
GeoB1311-2
GeoB1315-2
GeoB1408-2
GeoB1417-1
GeoB1418-1
GeoB1419-1
GeoB1419-2
GeoB1420-1
GeoB1421-1
GeoB1501-4
GeoB1503-1
GeoB1505-1
GeoB1508-4
GeoB1515-1
GeoB1523-1
GeoB1523-2
GeoB1701-4
Volbers, Andrea N A
Henrich, Rüdiger
Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
topic_facet 06MT15_2
06MT41_3
Amazon Fan
Angola Basin
Ascencion Island
Brazil Basin
Cape Basin
Cardno Seamount
Ceara Rise
Continental Slope off Rio Paraiba do Sul
East Brazil Basin
Eastern Rio Grande Rise
Equatorial Atlantic
GeoB
GeoB1028-5
GeoB1031-4
GeoB1032-3
GeoB1041-3
GeoB1047-3
GeoB1048-2
GeoB1101-5
GeoB1105-4
GeoB1112-4
GeoB1114-3
GeoB1117-2
GeoB1117-3
GeoB1118-2
GeoB1119-2
GeoB1120-3
GeoB1214-1
GeoB1220-1
GeoB1309-2
GeoB1310-1
GeoB1311-2
GeoB1315-2
GeoB1408-2
GeoB1417-1
GeoB1418-1
GeoB1419-1
GeoB1419-2
GeoB1420-1
GeoB1421-1
GeoB1501-4
GeoB1503-1
GeoB1505-1
GeoB1508-4
GeoB1515-1
GeoB1523-1
GeoB1523-2
GeoB1701-4
description The modern Atlantic Ocean, dominated by the interactions of North Atlantic Deep Water (NADW) and Antarctic Bottom Water (AABW), plays a key role in redistributing heat from the Southern to the Northern Hemisphere. In order to reconstruct the evolution of the relative importance of these two water masses, the NADW/AABW transition, reflected by the calcite lysocline, was investigated by the Globigerina bulloides dissolution index (BDX?). The depth level of the Late Glacial Maximum (LGM) calcite lysocline was elevated by several hundred metres, indicating a more corrosive water mass present at modern NADW level. Overall, the small range of BDX? data and the gradual decrease in preservation below the calcite lysocline point to a less stratified Atlantic Ocean during the LGM. Similar preservation patterns in the West and East Atlantic demonstrate that the modern west–east asymmetry did not exist due to an expansion of southern deep waters compensating for the decrease in NADW formation.
format Other/Unknown Material
author Volbers, Andrea N A
Henrich, Rüdiger
author_facet Volbers, Andrea N A
Henrich, Rüdiger
author_sort Volbers, Andrea N A
title Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
title_short Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
title_full Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
title_fullStr Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
title_full_unstemmed Dissolution index of Globigerina bulloides in recent and Last Glacial Maximum sediments
title_sort dissolution index of globigerina bulloides in recent and last glacial maximum sediments
publisher PANGAEA
publishDate 2004
url https://doi.pangaea.de/10.1594/PANGAEA.735719
https://doi.org/10.1594/PANGAEA.735719
op_coverage MEDIAN LATITUDE: -17.040875 * MEDIAN LONGITUDE: -24.991789 * SOUTH-BOUND LATITUDE: -37.831667 * WEST-BOUND LONGITUDE: -53.703333 * NORTH-BOUND LATITUDE: 29.176667 * EAST-BOUND LONGITUDE: 17.543333 * DATE/TIME START: 1988-03-02T00:00:00 * DATE/TIME END: 1998-05-09T23:22:00
long_lat ENVELOPE(-53.703333,17.543333,29.176667,-37.831667)
genre Antarc*
Antarctic
NADW
North Atlantic Deep Water
North Atlantic
genre_facet Antarc*
Antarctic
NADW
North Atlantic Deep Water
North Atlantic
op_source Supplement to: Volbers, Andrea N A; Henrich, Rüdiger (2004): Calcium carbonate corrosiveness in the South Atlantic during the Last Glacial Maximum as inferred from changes in the preservation of Globigerina bulloides: A proxy to determine deep-water circulation patterns? Marine Geology, 204(1-2), 43-57, https://doi.org/10.1016/S0025-3227(03)00372-4
op_relation Volbers, Andrea N A (2001): Planktic foraminifera as paleoceangraphic indicators: Production, preservation, and reconstruction of upwelling intensity. Implications from late quarternary South Atlantic sediments. Berichte aus dem Fachbereich Geowissenschaften der Universität Bremen, 184, 114 pp, urn:nbn:de:gbv:46-00101382-15
https://doi.pangaea.de/10.1594/PANGAEA.735719
https://doi.org/10.1594/PANGAEA.735719
op_rights CC-BY-3.0: Creative Commons Attribution 3.0 Unported
Access constraints: unrestricted
info:eu-repo/semantics/openAccess
op_doi https://doi.org/10.1594/PANGAEA.73571910.1016/S0025-3227(03)00372-4
_version_ 1810490552477548544

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