Relative Elevation of Late Pleistocene High Sea Level Stands: Barbados Uplift Rates and their Implications
- 1 June 1973
- journal article
- Published by Cambridge University Press (CUP) in Quaternary Research
- Vol. 3 (1) , 147-153
- https://doi.org/10.1016/0033-5894(73)90061-6
Abstract
Calculations confirm that the uplift of Barbados during the past 130,000 yr has been at nearly constant relative rates in the Clermont and Christ Church standard traverses, and that sea levels responsible for Barbados terraces I (82,000 yr B.P.) and II (105,000 yr B.P.) attained approximately the same level which was 20–25 m below the level represented by Barbados III (125,000 yr B.P.).Preference for the correlation of Barbados III with the prominent first interglacial 18O peak in stage 5 is stated once again. Further, correlation with Eemian and Pangaion of the European pollen record is suggested.Keywords
This publication has 13 references indexed in Scilit:
- Oxygen Isotope and Palaeomagnetic Stratigraphy of Equatorial Pacific Core V28-238: Oxygen Isotope Temperatures and Ice Volumes on a 105 Year and 106 Year ScaleQuaternary Research, 1973
- The Last Interglacial: Paleotemperatures and ChronologyScience, 1971
- Pleistocene PaleotemperaturesScience, 1970
- Insolation changes, ice volumes, and the O18 record in deep‐sea coresReviews of Geophysics, 1970
- Caribbean Cores P6304-8 and P6304-9: New Analysis of Absolute Chronology. A ReplyScience, 1969
- Interglacial High Sea Levels and the Control of Greenland Ice by the Precession of the EquinoxesScience, 1969
- Caribbean Cores P6304-8 and P6304-9: New Analysis of Absolute ChronologyScience, 1969
- The Astronomical Theory of Climatic Change: Barbados DataThe Journal of Geology, 1969
- Absolute Dating of Caribbean Cores P6304-8 and P6304-9Science, 1969
- Milankovitch Hypothesis Supported by Precise Dating of Coral Reefs and Deep-Sea SedimentsScience, 1968