_version_ 1867169459687391232
author Nuber, Sophie
Rae, James W B
Zhang, Xu
Andersen, Morten L
Dumont, Matthew
Mithan, T Huw
Sun, Yuchen
de Boer, Bas
Hall, Ian R
Barker, Stephen
author_facet Nuber, Sophie
Rae, James W B
Zhang, Xu
Andersen, Morten L
Dumont, Matthew
Mithan, T Huw
Sun, Yuchen
de Boer, Bas
Hall, Ian R
Barker, Stephen
collection Datos científicos de ciencias marinas y ambientales
contents Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Here we present planktonic foraminifera-based stack of oxygen isotopes as proxy for surface salinity from the surface Indian Ocean. We find that Indian Ocean surface salinity (along with temperature) increases during glacial intensification. We link this phenomenon to dynamics in the Indonesian Archipelago.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_955728
institution PANGAEA
language en
publishDate 2023
publisher PANGAEA
record_format pangaea
spellingShingle Indian Ocean surface oxygen isotopes of seawater (ice volume corrected) stack - proxy for sea surface salinity
Nuber, Sophie
Rae, James W B
Zhang, Xu
Andersen, Morten L
Dumont, Matthew
Mithan, T Huw
Sun, Yuchen
de Boer, Bas
Hall, Ian R
Barker, Stephen
361-U1476; Abashiri; ABS; AGE; CALYPSO; Calypso Corer; CD129; Charles Darwin; COMPCORE; Composite Core; Exp361; GeoB10038-4; Giant piston corer; GPC; Gravity corer (Kiel type); GS900963; Ice volume corrected; IMAGES VII - WEPAMA; Indian Ocean; Japan; Joides Resolution; KAL; Kasten corer; Marion Dufresne (1972); Marion Dufresne (1995); MD012378; MD01-2378; MD104; MD122; MD65; MD90-963; MD96-2048; Monitoring station; MONS; oxygen isotope ratios; Oxygen isotopes; PABESIA; PC; PEGASE; Percentile 95; Piston corer; planktic foraminifera; Salinity; Temperature; Sea surface salinity; Sea surface temperature; SEYMAMA/SHIVA; SL; SO184/1; Sonne; South African Climates (Agulhas LGM Density Profile); SW Indian Ocean; Timor Sea; TY93-929; WIND; WIND-28K; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, standard score
Indian Ocean surface circulation is an important part of the global ocean conveyor belt, and is connected via two important gateways including the Indonesian Throughflow, and the Agulha Leakage. Changes in the surface hydrography of the Indian Ocean may therefore impact on the global overturning circulation. Here we present planktonic foraminifera-based stack of oxygen isotopes as proxy for surface salinity from the surface Indian Ocean. We find that Indian Ocean surface salinity (along with temperature) increases during glacial intensification. We link this phenomenon to dynamics in the Indonesian Archipelago.
title Indian Ocean surface oxygen isotopes of seawater (ice volume corrected) stack - proxy for sea surface salinity
topic 361-U1476; Abashiri; ABS; AGE; CALYPSO; Calypso Corer; CD129; Charles Darwin; COMPCORE; Composite Core; Exp361; GeoB10038-4; Giant piston corer; GPC; Gravity corer (Kiel type); GS900963; Ice volume corrected; IMAGES VII - WEPAMA; Indian Ocean; Japan; Joides Resolution; KAL; Kasten corer; Marion Dufresne (1972); Marion Dufresne (1995); MD012378; MD01-2378; MD104; MD122; MD65; MD90-963; MD96-2048; Monitoring station; MONS; oxygen isotope ratios; Oxygen isotopes; PABESIA; PC; PEGASE; Percentile 95; Piston corer; planktic foraminifera; Salinity; Temperature; Sea surface salinity; Sea surface temperature; SEYMAMA/SHIVA; SL; SO184/1; Sonne; South African Climates (Agulhas LGM Density Profile); SW Indian Ocean; Timor Sea; TY93-929; WIND; WIND-28K; δ18O, seawater, reconstructed; δ18O, seawater, reconstructed, standard score
url https://doi.org/10.1594/PANGAEA.955728