(Table 1) Nd isotope ratios of ODP Leg 208 samples ...

We present new Nd isotope records from Walvis Ridge Ocean Drilling Program (ODP) sites 1262–1264 (southeastern Atlantic) spanning the past 24 Ma to investigate the Neogene evolution of Atlantic thermohaline circulation. The new data indicate that deepwater epsilon-Nd(t) values from ODP Site 1262 dec...

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Bibliographic Details
Main Authors: Thomas, Deborah J, Via, Rachael K
Format: Dataset
Language:English
Published: PANGAEA 2007
Subjects:
AGE
Online Access:https://dx.doi.org/10.1594/pangaea.833136
https://doi.pangaea.de/10.1594/PANGAEA.833136
id ftdatacite:10.1594/pangaea.833136
record_format openpolar
spelling ftdatacite:10.1594/pangaea.833136 2024-09-15T18:17:14+00:00 (Table 1) Nd isotope ratios of ODP Leg 208 samples ... Thomas, Deborah J Via, Rachael K 2007 text/tab-separated-values https://dx.doi.org/10.1594/pangaea.833136 https://doi.pangaea.de/10.1594/PANGAEA.833136 en eng PANGAEA https://dx.doi.org/10.1029/2006pa001297 Creative Commons Attribution 3.0 Unported https://creativecommons.org/licenses/by/3.0/legalcode cc-by-3.0 Event label DEPTH, sediment/rock AGE Neodymium-143/Neodymium-144 ratio Neodymium-143/Neodymium-144 ratio, error ε-Neodymium T ε-Neodymium, error Drilling/drill rig Leg208 Joides Resolution Ocean Drilling Program ODP dataset Supplementary Dataset Dataset 2007 ftdatacite https://doi.org/10.1594/pangaea.83313610.1029/2006pa001297 2024-08-01T10:51:52Z We present new Nd isotope records from Walvis Ridge Ocean Drilling Program (ODP) sites 1262–1264 (southeastern Atlantic) spanning the past 24 Ma to investigate the Neogene evolution of Atlantic thermohaline circulation. The new data indicate that deepwater epsilon-Nd(t) values from ODP Site 1262 decrease from -11.0 at 10.6 Ma to -12.5 by 7.3 Ma. This decrease parallels the Nd isotope trends contained in Fe-Mn crust records from the northwestern Atlantic; however, the shift at ODP Site 1262 (4755 m water depth) occurred up to ~6 Ma earlier than the corresponding changes in crust records from the Atlantic and earlier than any Atlantic site shallower than 2700 m paleowater depth. Recent interpretations of the rapid decrease in Fe-Mn crust Nd epsilon-Nd(t)ss values invoke changes in weathering inputs to the Labrador Sea region rather than a fundamental change in deepwater convection in the Labrador Sea. However, the new evidence for significant depth stratification of the Nd isotope signal in the southeastern ... : DEPTH, sediment/rock is given in mcd. ... Dataset Labrador Sea DataCite
institution Open Polar
collection DataCite
op_collection_id ftdatacite
language English
topic Event label
DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium T
ε-Neodymium, error
Drilling/drill rig
Leg208
Joides Resolution
Ocean Drilling Program ODP
spellingShingle Event label
DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium T
ε-Neodymium, error
Drilling/drill rig
Leg208
Joides Resolution
Ocean Drilling Program ODP
Thomas, Deborah J
Via, Rachael K
(Table 1) Nd isotope ratios of ODP Leg 208 samples ...
topic_facet Event label
DEPTH, sediment/rock
AGE
Neodymium-143/Neodymium-144 ratio
Neodymium-143/Neodymium-144 ratio, error
ε-Neodymium T
ε-Neodymium, error
Drilling/drill rig
Leg208
Joides Resolution
Ocean Drilling Program ODP
description We present new Nd isotope records from Walvis Ridge Ocean Drilling Program (ODP) sites 1262–1264 (southeastern Atlantic) spanning the past 24 Ma to investigate the Neogene evolution of Atlantic thermohaline circulation. The new data indicate that deepwater epsilon-Nd(t) values from ODP Site 1262 decrease from -11.0 at 10.6 Ma to -12.5 by 7.3 Ma. This decrease parallels the Nd isotope trends contained in Fe-Mn crust records from the northwestern Atlantic; however, the shift at ODP Site 1262 (4755 m water depth) occurred up to ~6 Ma earlier than the corresponding changes in crust records from the Atlantic and earlier than any Atlantic site shallower than 2700 m paleowater depth. Recent interpretations of the rapid decrease in Fe-Mn crust Nd epsilon-Nd(t)ss values invoke changes in weathering inputs to the Labrador Sea region rather than a fundamental change in deepwater convection in the Labrador Sea. However, the new evidence for significant depth stratification of the Nd isotope signal in the southeastern ... : DEPTH, sediment/rock is given in mcd. ...
format Dataset
author Thomas, Deborah J
Via, Rachael K
author_facet Thomas, Deborah J
Via, Rachael K
author_sort Thomas, Deborah J
title (Table 1) Nd isotope ratios of ODP Leg 208 samples ...
title_short (Table 1) Nd isotope ratios of ODP Leg 208 samples ...
title_full (Table 1) Nd isotope ratios of ODP Leg 208 samples ...
title_fullStr (Table 1) Nd isotope ratios of ODP Leg 208 samples ...
title_full_unstemmed (Table 1) Nd isotope ratios of ODP Leg 208 samples ...
title_sort (table 1) nd isotope ratios of odp leg 208 samples ...
publisher PANGAEA
publishDate 2007
url https://dx.doi.org/10.1594/pangaea.833136
https://doi.pangaea.de/10.1594/PANGAEA.833136
genre Labrador Sea
genre_facet Labrador Sea
op_relation https://dx.doi.org/10.1029/2006pa001297
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.83313610.1029/2006pa001297
_version_ 1810455248410509312