Response of Red Sea deep-water agglutinated foraminifera to water-mass changes during the Late Quaternary
- 1 September 1996
- journal article
- Published by Elsevier in Marine Micropaleontology
- Vol. 28 (3-4), 283-297
- https://doi.org/10.1016/0377-8398(96)00005-9
Abstract
No abstract availableKeywords
This publication has 11 references indexed in Scilit:
- Three hundred eighty thousand year long stable isotope and faunal records from the Red Sea: Influence of global sea level change on hydrographyPaleoceanography and Paleoclimatology, 1996
- Paleoenvironmental events during the last 13,000 years in the central Red Sea as recorded by pteropodaPaleoceanography and Paleoclimatology, 1991
- Glacio-eustatic sea-level control on Red Sea salinityNature, 1988
- On the sources, formation, and circulation of Red Sea deep waterJournal of Geophysical Research: Oceans, 1988
- Paleoceanographic record of the last glacial/interglacial cycle in the Red Sea and Gulf of AdenPalaeogeography, Palaeoclimatology, Palaeoecology, 1988
- Quaternary paleo-oceanography, pteropod preservation and stable-isotope record of the Red SeaPalaeogeography, Palaeoclimatology, Palaeoecology, 1986
- Late Quaternary biostratigraphy and paleotemperatures of the Red Sea and the Gulf of Aden based on planktonic foraminifera and pteropodsMarine Micropaleontology, 1985
- Paleoecological Relations of Foraminifera in a Desert-Enclosed Sea -The Gulf of Aqaba (Elat), Red SeaMarine Ecology, 1981
- Late Quaternary Paleoceanography of the Gulf of Aqaba (Elat), Red SeaQuaternary Research, 1980
- Circulation of the Red Sea in early summerDeep Sea Research (1953), 1961