Glacial–interglacial ocean climate variability from planktonic foraminifera during the Mid-Pleistocene transition in the temperate Southwest Pacific, ODP Site 1123

Planktonic foraminiferal assemblages and artificial neural network estimates of sea-surface temperature (SST) at ODP Site 1123 (41°47.2'S, 171°29.9'W; 3290 m deep), east of New Zealand, reveal a high-resolution history of glacial–interglacial (G–I) variability at the Subtropical Front (STF...

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Veröffentlicht in:	Palaeogeography, palaeoclimatology, palaeoecology palaeoclimatology, palaeoecology, 2008-04, Vol.260 (1-2), p.202-229
Hauptverfasser:	Crundwell, Martin, Scott, George, Naish, Tim, Carter, Lionel
Format:	Artikel
Sprache:	eng
Schlagworte:	Antarctic Climate forcing Deglacial Glacial Interglacial Marine Mid-Pleistocene transition Ocean climate Planktonic foraminifera Southern hemisphere Southwest Pacific Tropics
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