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...
Main Authors: | , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2000
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Subjects: | |
Online Access: | https://doi.pangaea.de/10.1594/PANGAEA.729180 https://doi.org/10.1594/PANGAEA.729180 |