A revised age for the Kawakawa/Oruanui tephra, a key marker for the Last Glacial Maximum in New Zealand

The Kawakawa/Oruanui tephra (KOT) is a key chronostratigraphic marker in terrestrial and marine deposits of the New Zealand (NZ) sector of the southwest Pacific. Erupted early during the Last Glacial Maximum (LGM), the wide distribution of the KOT enables inter-regional alignment of proxy records an...

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Veröffentlicht in:	Quaternary science reviews 2013-08, Vol.74, p.195-201
Hauptverfasser:	Vandergoes, Marcus J., Hogg, Alan G., Lowe, David J., Newnham, Rewi M., Denton, George H., Southon, John, Barrell, David J.A., Wilson, Colin J.N., McGlone, Matt S., Allan, Aidan S.R., Almond, Peter C., Petchey, Fiona, Dabell, Kathleen, Dieffenbacher-Krall, Ann C., Blaauw, Maarten
Format:	Artikel
Sprache:	eng
Schlagworte:	14C dating Chronostratigraphy Isochron Kawakawa/Oruanui tephra Last Glacial Maximum (LGM) Marine Marine reservoir ages New Zealand NZ climate event stratigraphy Oruanui eruption Paleoclimate Southwest Pacific Tephrochronology
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