Temperature reconstruction of sediment core SO9-93KL ...

The Toba volcanic event, one of the largest eruptions during the Quaternary, is documented in marine sediment cores from the northeastern Arabian Sea. On the crest of the Murray Ridge and along the western Indian continental margin, we detected distinct concentration spikes and ash layers of rhyolit...

Full description

Bibliographic Details
Main Authors: Schulz, Hartmut, Emeis, Kay-Christian, Erlenkeuser, Helmut, von Rad, Ulrich, Rolf, Christian
Format: Article in Journal/Newspaper
Language:English
Published: PANGAEA 2002
Subjects:
Online Access:https://dx.doi.org/10.1594/pangaea.735955
https://doi.pangaea.de/10.1594/PANGAEA.735955
id ftdatacite:10.1594/pangaea.735955
record_format openpolar
spelling ftdatacite:10.1594/pangaea.735955 2024-09-15T18:09:51+00:00 Temperature reconstruction of sediment core SO9-93KL ... Schulz, Hartmut Emeis, Kay-Christian Erlenkeuser, Helmut von Rad, Ulrich Rolf, Christian 2002 application/zip https://dx.doi.org/10.1594/pangaea.735955 https://doi.pangaea.de/10.1594/PANGAEA.735955 en eng PANGAEA https://dx.doi.org/10.1006/qres.2001.2291 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Piston corer BGR type SO90 Sonne Center for Marine Environmental Sciences MARUM article Collection Supplementary Publication Series of Datasets 2002 ftdatacite https://doi.org/10.1594/pangaea.73595510.1006/qres.2001.2291 2024-07-03T13:16:23Z The Toba volcanic event, one of the largest eruptions during the Quaternary, is documented in marine sediment cores from the northeastern Arabian Sea. On the crest of the Murray Ridge and along the western Indian continental margin, we detected distinct concentration spikes and ash layers of rhyolithic volcanic shards near the marine isotope stage 5-4 boundary with the chemical composition of the "Youngest Toba Tuff". Time series of the Uk'37-alkenone index, planktic foraminiferal species, magnetic susceptibility, and sediment accumulation rates from this interval show that the Toba event occurred between two warm periods lasting a few millennia. Using Toba as an instantaneous stratigraphic marker for correlation between the marine- and ice-core chronostratigraphies, these two Arabian Sea climatic events correspond to Greenland interstadials 20 and 19, respectively. Our data sets thus depict substantial interstadial/stadial fluctuations in sea-surface temperature and surface-water productivity. We show that ... : Supplement to: Schulz, Hartmut; Emeis, Kay-Christian; Erlenkeuser, Helmut; von Rad, Ulrich; Rolf, Christian (2002): The Toba Volcanic Event and Interstadial/Stadial Climates at the Marine Isotopic Stage 5 to 4 Transition in the Northern Indian Ocean. Quaternary Research, 57(1), 22-31 ... Article in Journal/Newspaper Greenland ice core DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Piston corer BGR type
SO90
Sonne
Center for Marine Environmental Sciences MARUM
spellingShingle Piston corer BGR type
SO90
Sonne
Center for Marine Environmental Sciences MARUM
Schulz, Hartmut
Emeis, Kay-Christian
Erlenkeuser, Helmut
von Rad, Ulrich
Rolf, Christian
Temperature reconstruction of sediment core SO9-93KL ...
topic_facet Piston corer BGR type
SO90
Sonne
Center for Marine Environmental Sciences MARUM
description The Toba volcanic event, one of the largest eruptions during the Quaternary, is documented in marine sediment cores from the northeastern Arabian Sea. On the crest of the Murray Ridge and along the western Indian continental margin, we detected distinct concentration spikes and ash layers of rhyolithic volcanic shards near the marine isotope stage 5-4 boundary with the chemical composition of the "Youngest Toba Tuff". Time series of the Uk'37-alkenone index, planktic foraminiferal species, magnetic susceptibility, and sediment accumulation rates from this interval show that the Toba event occurred between two warm periods lasting a few millennia. Using Toba as an instantaneous stratigraphic marker for correlation between the marine- and ice-core chronostratigraphies, these two Arabian Sea climatic events correspond to Greenland interstadials 20 and 19, respectively. Our data sets thus depict substantial interstadial/stadial fluctuations in sea-surface temperature and surface-water productivity. We show that ... : Supplement to: Schulz, Hartmut; Emeis, Kay-Christian; Erlenkeuser, Helmut; von Rad, Ulrich; Rolf, Christian (2002): The Toba Volcanic Event and Interstadial/Stadial Climates at the Marine Isotopic Stage 5 to 4 Transition in the Northern Indian Ocean. Quaternary Research, 57(1), 22-31 ...
format Article in Journal/Newspaper
author Schulz, Hartmut
Emeis, Kay-Christian
Erlenkeuser, Helmut
von Rad, Ulrich
Rolf, Christian
author_facet Schulz, Hartmut
Emeis, Kay-Christian
Erlenkeuser, Helmut
von Rad, Ulrich
Rolf, Christian
author_sort Schulz, Hartmut
title Temperature reconstruction of sediment core SO9-93KL ...
title_short Temperature reconstruction of sediment core SO9-93KL ...
title_full Temperature reconstruction of sediment core SO9-93KL ...
title_fullStr Temperature reconstruction of sediment core SO9-93KL ...
title_full_unstemmed Temperature reconstruction of sediment core SO9-93KL ...
title_sort temperature reconstruction of sediment core so9-93kl ...
publisher PANGAEA
publishDate 2002
url https://dx.doi.org/10.1594/pangaea.735955
https://doi.pangaea.de/10.1594/PANGAEA.735955
genre Greenland
ice core
genre_facet Greenland
ice core
op_relation https://dx.doi.org/10.1006/qres.2001.2291
op_rights Creative Commons Attribution 3.0 Unported
https://creativecommons.org/licenses/by/3.0/legalcode
cc-by-3.0
op_doi https://doi.org/10.1594/pangaea.73595510.1006/qres.2001.2291
_version_ 1810447445370339328