Last glacial jetting of cold waters through the subtropical convergence zone in the southwest Pacific off eastern New Zealand, and some geological implications

Recent evidence suggests that the Subtropical Convergence (STC) zone east of New Zealand shifted little from its modern position along Chatham Rise during the last glaciation, and that offshore surface waters north of the STC zone cooled only slightly. However, at nearshore core site P69 (2195 m dep...

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Bibliographic Details
Published in:Palaeogeography, Palaeoclimatology, Palaeoecology
Main Authors: Nelson, C.S., Hendy, I.L., Neil, H.L., Hendy, C.H., Weaver, P.P.E.
Format: Article in Journal/Newspaper
Language:unknown
Published: 2000
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/108783/
https://doi.org/10.1016/S0031-0182(99)00134-0