@article{44f246f8f7414c7793b1fe8e1a231ff0,
title = "Sediment deposition in the late Holocene abyssal Black Sea with climatic and chronological implications",
abstract = "The temporal sedimentary patterns in the Late Holocene central eastern and western Black Sea are very similar. The sedimentary history was most visibly affected by the coccolithophorid species Emiliania huxleyi which briefly invaded the Black Sea for the first time ({"}First Invasion Period'), nearly disappeared again shortly afterwards ({"}Transition Sapropel'), but returned permanently several centuries later ({"}Final Invasion Period'). The temporary near-disappearance of E. huxleyi was probably caused by a temporary drop in salinity. -from Authors",
author = "Hay, {B. J.} and Arthur, {M. A.} and Dean, {W. E.} and Neff, {E. D.} and S. Honjo",
note = "Funding Information: Acknowledgements-We thank J. Broda and A. Gagnon, Woods Hole Oceanographic Institution, S. Derman, TurkishPetroleumCorporation,T.Konuk andM.Duman,DokuzEyltilUniversity,Izmir,andothermembers ofthescientificshipboardpartyoftheR.V.Knorr BlackSeacruise134-8,aswellastheveryco-operativeofficers and crew of the R.V. Knorr, for their support in the successful coring operation. Inorganic geochemical laboratoryworkwasaccomplishedbyD.Bankston(deceased)andL. Ball(ICPES),S.ManganiniandS.Carter (sample preparation), Woods Hole Oceanographic Institution. This research was partially funded by the National Science Foundation Grants Nos OCE-8614363 (Honjo) and OCE-8711741 (Arthur), and the U.S. Geological Survey Evolution of Sedimentary Basins Program.",
year = "1991",
doi = "10.1016/s0198-0149(10)80031-7",
language = "English (US)",
volume = "38",
pages = "S1211--S1235",
journal = "Deep-Sea Research, Part A",
issn = "0198-0149",
publisher = "Pergamon Press Ltd.",
number = "Suppl. 2A",
}