Planktonic foraminiferal δ¹⁸O and δ¹³C values, derived sea-surface temperatures from d18O and selected planktonic foraminiferal species for core P69 of Hawke Bay off eastern North Island

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
Main Authors: Nelson, Campbell S, Hendy, Ingrid L, Neil, Helen L, Hendy, Chris H, Weaver, Philip PE
Format: Dataset
Language:English
Published: PANGAEA 2000
Subjects:
GC
P69
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.729180
https://doi.org/10.1594/PANGAEA.729180