Neodymium isotope record of the past 25 Ma in the Indian Ocean

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Autori principali: Gourlan, Alexandra T, Meynadier, Laure M, Allègre, Claude J
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2008
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author Gourlan, Alexandra T
Meynadier, Laure M
Allègre, Claude J
author_facet Gourlan, Alexandra T
Meynadier, Laure M
Allègre, Claude J
collection Datos científicos de ciencias marinas y ambientales
contents Changes in ancient oceanic current patterns have been strongly influenced by plate tectonics, particularly by the opening or closing of gateways between different oceans. Such modifications of oceanic circulation have important consequences on climate. We studied the Nd seawater isotopic composition of Indian and Pacific Ocean cores using Nd isotopes, which are good paleo-oceanographic tracers. We focused on the past 25 Ma which are marked by the closure of the Indonesian gateway as well as the Mediterranean connection. We show that a strong westerly oceanic surface current, which we refer to the Miocene Indian Ocean Equatorial Jet (MIOJet), linked the eastern and western Indian Ocean from 14 Ma to 3 Ma and infer that this major change in oceanic circulation probably induced important variations of global climate.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_707046
institution PANGAEA
language en
publishDate 2008
publisher PANGAEA
record_format pangaea
spellingShingle Neodymium isotope record of the past 25 Ma in the Indian Ocean
Gourlan, Alexandra T
Meynadier, Laure M
Allègre, Claude J
115-707A; 121-757B; 121-758A; 130-807A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg115; Leg121; Leg130; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean; West equatorial Pacific Ocean
Changes in ancient oceanic current patterns have been strongly influenced by plate tectonics, particularly by the opening or closing of gateways between different oceans. Such modifications of oceanic circulation have important consequences on climate. We studied the Nd seawater isotopic composition of Indian and Pacific Ocean cores using Nd isotopes, which are good paleo-oceanographic tracers. We focused on the past 25 Ma which are marked by the closure of the Indonesian gateway as well as the Mediterranean connection. We show that a strong westerly oceanic surface current, which we refer to the Miocene Indian Ocean Equatorial Jet (MIOJet), linked the eastern and western Indian Ocean from 14 Ma to 3 Ma and infer that this major change in oceanic circulation probably induced important variations of global climate.
title Neodymium isotope record of the past 25 Ma in the Indian Ocean
topic 115-707A; 121-757B; 121-758A; 130-807A; DRILL; Drilling/drill rig; Indian Ocean; Joides Resolution; Leg115; Leg121; Leg130; Ocean Drilling Program; ODP; South Indian Ridge, South Indian Ocean; West equatorial Pacific Ocean
url https://doi.org/10.1594/PANGAEA.707046