Late Quaternary dinoflagellate cysts from the Black, Marmara and Aegean seas: variations in assemblages, morphology and paleosalinity
- 17 August 2001
- journal article
- Published by Elsevier in Marine Micropaleontology
- Vol. 43 (1-2) , 155-178
- https://doi.org/10.1016/s0377-8398(01)00006-8
Abstract
No abstract availableKeywords
This publication has 32 references indexed in Scilit:
- Oscillating Quaternary water levels of the Marmara Sea and vigorous outflow into the Aegean Sea from the Marmara Sea–Black Sea drainage corridorMarine Geology, 1999
- Paleoclimatic and paleoceanographic conditions leading to development of sapropel layer S1 in the Aegean SeaPalaeogeography, Palaeoclimatology, Palaeoecology, 1995
- Late glacial-Holocene paleoclimatic and paleoceanographic evolution of the Aegean Sea: micropaleontological and stable isotopic evidenceMarine Micropaleontology, 1995
- Origin of late glacial—Holocene hemipelagic sediments in the Aegean Sea: clay mineralogy and carbonate cementationMarine Geology, 1995
- Cyst production in four species of neritic dinoflagellatesJournal of Plankton Research, 1995
- Late Quaternary chronology of the southern Black Sea basinGeo-Marine Letters, 1994
- Iunconsistencies in Accumulation Rates of Black Sea Sediments Inferred from Records of Laminae and 210PbPaleoceanography and Paleoclimatology, 1992
- Achomosphaera argesensis: A new dinoflagellate species from the early pliocene of the southern carpathians foredeep, RomaniaReview of Palaeobotany and Palynology, 1989
- Sinking characteristics of dinoflagellate cysts1Limnology and Oceanography, 1985
- Late-Pleistocene and Holocene history of the Black Sea as indicated by stable-isotope studiesJournal of Geophysical Research, 1972