Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences

A detailed record of alkenone-derived sea-surface temperatures (SSTs) offshore western New Zealand has been generated for the penultimate deglaciation and last interglacial. SSTs were 3.5 to 4.5°C warmer than present, peaking 4.5 thousand years ahead of

Bibliographic Details
Main Authors: Pelejero, Carles, Calvo, Eva, Logan, Graham A, De Deckker, Patrick
Format: Article in Journal/Newspaper
Language:unknown
Published: American Geophysical Union 2015
Subjects:
Online Access:http://hdl.handle.net/1885/87699
id ftanucanberra:oai:digitalcollections.anu.edu.au:1885/87699
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spelling ftanucanberra:oai:digitalcollections.anu.edu.au:1885/87699 2023-05-15T13:56:05+02:00 Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences Pelejero, Carles Calvo, Eva Logan, Graham A De Deckker, Patrick 2015-12-13T23:11:41Z http://hdl.handle.net/1885/87699 unknown American Geophysical Union 0094-8276 http://hdl.handle.net/1885/87699 Geophysical Research Letters Keywords: Isotopes Marine applications Thermal gradients Ice volume Sea-surface temperature (SST) Geophysics Quaternary sea surface temperature temporal variation Pacific Ocean Pacific Ocean (Southwest) Journal article 2015 ftanucanberra 2015-12-15T00:07:26Z A detailed record of alkenone-derived sea-surface temperatures (SSTs) offshore western New Zealand has been generated for the penultimate deglaciation and last interglacial. SSTs were 3.5 to 4.5°C warmer than present, peaking 4.5 thousand years ahead of Article in Journal/Newspaper Antarc* Antarctica Australian National University: ANU Digital Collections New Zealand Pacific
institution Open Polar
collection Australian National University: ANU Digital Collections
op_collection_id ftanucanberra
language unknown
topic Keywords: Isotopes
Marine applications
Thermal gradients
Ice volume
Sea-surface temperature (SST)
Geophysics
Quaternary
sea surface temperature
temporal variation
Pacific Ocean
Pacific Ocean (Southwest)
spellingShingle Keywords: Isotopes
Marine applications
Thermal gradients
Ice volume
Sea-surface temperature (SST)
Geophysics
Quaternary
sea surface temperature
temporal variation
Pacific Ocean
Pacific Ocean (Southwest)
Pelejero, Carles
Calvo, Eva
Logan, Graham A
De Deckker, Patrick
Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
topic_facet Keywords: Isotopes
Marine applications
Thermal gradients
Ice volume
Sea-surface temperature (SST)
Geophysics
Quaternary
sea surface temperature
temporal variation
Pacific Ocean
Pacific Ocean (Southwest)
description A detailed record of alkenone-derived sea-surface temperatures (SSTs) offshore western New Zealand has been generated for the penultimate deglaciation and last interglacial. SSTs were 3.5 to 4.5°C warmer than present, peaking 4.5 thousand years ahead of
format Article in Journal/Newspaper
author Pelejero, Carles
Calvo, Eva
Logan, Graham A
De Deckker, Patrick
author_facet Pelejero, Carles
Calvo, Eva
Logan, Graham A
De Deckker, Patrick
author_sort Pelejero, Carles
title Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
title_short Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
title_full Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
title_fullStr Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
title_full_unstemmed Marine Isotopic Stage 5e in the Southwest Pacific: Similarities with Antarctica and ENSO inferences
title_sort marine isotopic stage 5e in the southwest pacific: similarities with antarctica and enso inferences
publisher American Geophysical Union
publishDate 2015
url http://hdl.handle.net/1885/87699
geographic New Zealand
Pacific
geographic_facet New Zealand
Pacific
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_source Geophysical Research Letters
op_relation 0094-8276
http://hdl.handle.net/1885/87699
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