Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropoda
- 1 February 1991
- journal article
- Published by American Geophysical Union (AGU) in Paleoceanography and Paleoclimatology
- Vol. 6 (1), 83-98
- https://doi.org/10.1029/90pa01881
Abstract
No abstract availableKeywords
This publication has 42 references indexed in Scilit:
- Distributional pattern of planktonic foraminifers and pteropods in surface waters and top core sediments of the Red Sea, and adjacent areas controlled by the monsoonal regime and other ecological factorsDeep Sea Research Part A. Oceanographic Research Papers, 1989
- Climatic Changes of the Last 18,000 Years: Observations and Model SimulationsScience, 1988
- Seasonal variation in the flux of euthecosomatous pteropods collected in a deep sediment trap in the Sargasso SeaDeep Sea Research Part A. Oceanographic Research Papers, 1988
- The chronology of the last Deglaciation: Implications to the cause of the Younger Dryas EventPaleoceanography and Paleoclimatology, 1988
- Quaternary paleo-oceanography, pteropod preservation and stable-isotope record of the Red SeaPalaeogeography, Palaeoclimatology, Palaeoecology, 1986
- Stratigraphic and paleoceanographic significance of Late Quaternary pteropods from deep-sea cores in the Gulf of Aqaba (Elat) and northernmost Red SeaMarine Micropaleontology, 1982
- The Surface of the Ice-Age EarthScience, 1976
- O18/O16 and C13/C12 Ratios of Fossils from the Hot-Brine Deep Area of the Central Red SeaPublished by Springer Nature ,1969
- Pteropods in the Hot Brine Sediments of the Red SeaPublished by Springer Nature ,1969
- Isotopic Composition and Origin of the Red Sea and Salton Sea Geothermal BrinesScience, 1966