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
|Collections||ANU Research Publications|
|Source:||Geophysical Research Letters|
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