A stable-isotope record for the Late Quaternary from the East Tasman Plateau
Abstract
The oxygen-isotope record of planktic foraminifers from a short core from the East Tasman Plateau is briefly presented. Results indicate a low sedimentation rate of the order of 1 cm/year for the last450,000 years. Brief mention is made to the correlation of this core with other standard isotopic curves for the Late Quaternary.
Fields of Study & Subjects
Geology and Paleoclimatology Research
Marine and environmental studies
Paleontology and Stratigraphy of Fossils
Publication details
- Journal / source
- CRC Press eBooks
- Pages
- 197–201
- Publication date
- 2 February 2026
- Language
- EN
- Document type
- Book chapter