(Table S1) Neodymium isotopic results from ODP Site 172-1063 ...

The Atlantic Meridional Overturning Circulation (AMOC) plays an important role in the Northern Hemisphere climate system. Significant interest went into the question of how excessive freshwater input through melting of continental ice can affect its overturning vigor and, hence, heat supply, to high...

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Bibliographic Details
Main Authors: Gutjahr, Marcus, Lippold, Jörg
Format: Dataset
Language:English
Published: PANGAEA 2011
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.830725
https://doi.pangaea.de/10.1594/PANGAEA.830725
id ftdatacite:10.1594/pangaea.830725
record_format openpolar
spelling ftdatacite:10.1594/pangaea.830725 2024-09-15T18:21:33+00:00 (Table S1) Neodymium isotopic results from ODP Site 172-1063 ... Gutjahr, Marcus Lippold, Jörg 2011 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.830725 https://doi.pangaea.de/10.1594/PANGAEA.830725 en eng PANGAEA https://dx.doi.org/10.1029/2011pa002114 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 DEPTH, sediment/rock AGE Neodymium-143/Neodymium-144 ratio Neodymium-143/Neodymium-144 ratio, error ε-Neodymium Number of measurements Composite Core Leg172 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2011 ftdatacite https://doi.org/10.1594/pangaea.83072510.1029/2011pa002114 2024-08-01T10:53:32Z The Atlantic Meridional Overturning Circulation (AMOC) plays an important role in the Northern Hemisphere climate system. Significant interest went into the question of how excessive freshwater input through melting of continental ice can affect its overturning vigor and, hence, heat supply, to higher northern latitudes. Such forcing can be tested by investigating its behavior during extreme iceberg discharge events into the open North Atlantic during the last glacial period, the so-called Heinrich events (HE). Here we present neodymium (Nd) isotope compositions of past seawater, a sensitive chemical water mass tag, extracted from sediments of Ocean Drilling Program Site 1063 in the western North Atlantic (Bermuda Rise), covering the period surrounding HE 2, the Last Glacial Maximum, and the early deglaciation. These data are compared with a record of the kinematic circulation tracer (231Pa/230Th)xs extracted from the same sediment core. Both tracers indicate significant circulation changes preceding intense ... : Supplement to: Gutjahr, Marcus; Lippold, Jörg (2011): Early arrival of Southern Source Water in the deep North Atlantic prior to Heinrich event 2. Paleoceanography, 26(2), PA2101 ... Dataset North Atlantic DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium
Number of measurements
Composite Core
Leg172
Joides Resolution
Ocean Drilling Program ODP
spellingShingle DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium
Number of measurements
Composite Core
Leg172
Joides Resolution
Ocean Drilling Program ODP
Gutjahr, Marcus
Lippold, Jörg
(Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
topic_facet DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium
Number of measurements
Composite Core
Leg172
Joides Resolution
Ocean Drilling Program ODP
description The Atlantic Meridional Overturning Circulation (AMOC) plays an important role in the Northern Hemisphere climate system. Significant interest went into the question of how excessive freshwater input through melting of continental ice can affect its overturning vigor and, hence, heat supply, to higher northern latitudes. Such forcing can be tested by investigating its behavior during extreme iceberg discharge events into the open North Atlantic during the last glacial period, the so-called Heinrich events (HE). Here we present neodymium (Nd) isotope compositions of past seawater, a sensitive chemical water mass tag, extracted from sediments of Ocean Drilling Program Site 1063 in the western North Atlantic (Bermuda Rise), covering the period surrounding HE 2, the Last Glacial Maximum, and the early deglaciation. These data are compared with a record of the kinematic circulation tracer (231Pa/230Th)xs extracted from the same sediment core. Both tracers indicate significant circulation changes preceding intense ... : Supplement to: Gutjahr, Marcus; Lippold, Jörg (2011): Early arrival of Southern Source Water in the deep North Atlantic prior to Heinrich event 2. Paleoceanography, 26(2), PA2101 ...
format Dataset
author Gutjahr, Marcus
Lippold, Jörg
author_facet Gutjahr, Marcus
Lippold, Jörg
author_sort Gutjahr, Marcus
title (Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
title_short (Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
title_full (Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
title_fullStr (Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
title_full_unstemmed (Table S1) Neodymium isotopic results from ODP Site 172-1063 ...
title_sort (table s1) neodymium isotopic results from odp site 172-1063 ...
publisher PANGAEA
publishDate 2011
url https://dx.doi.org/10.1594/pangaea.830725
https://doi.pangaea.de/10.1594/PANGAEA.830725
genre North Atlantic
genre_facet North Atlantic
op_relation https://dx.doi.org/10.1029/2011pa002114
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.83072510.1029/2011pa002114
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