Sediment deposition in the late Holocene abyssal Black Sea with climatic and chronological implications

B. J. Hay; M. A. Arthur; W. E. Dean; E. D. Neff; S. Honjo

doi:10.1016/s0198-0149(10)80031-7

Sediment deposition in the late Holocene abyssal Black Sea with climatic and chronological implications

B. J. Hay
, M. A. Arthur
, W. E. Dean
, E. D. Neff
, S. Honjo

Geosciences

Research output: Contribution to journal › Article › peer-review

105 Scopus citations

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

Original language	English (US)
Pages (from-to)	S1211-S1235
Journal	Deep-Sea Research, Part A
Volume	38
Issue number	Suppl. 2A
DOIs	https://doi.org/10.1016/s0198-0149(10)80031-7
State	Published - 1991

All Science Journal Classification (ASJC) codes

General Environmental Science
General Earth and Planetary Sciences

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10.1016/s0198-0149(10)80031-7

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@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",

}

TY - JOUR

T1 - Sediment deposition in the late Holocene abyssal Black Sea with climatic and chronological implications

AU - Hay, B. J.

AU - Arthur, M. A.

AU - Dean, W. E.

AU - Neff, E. D.

AU - Honjo, S.

N1 - 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.

PY - 1991

Y1 - 1991

N2 - 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

AB - 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

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U2 - 10.1016/s0198-0149(10)80031-7

DO - 10.1016/s0198-0149(10)80031-7

M3 - Article

AN - SCOPUS:0026307926

SN - 0198-0149

VL - 38

SP - S1211-S1235

JO - Deep-Sea Research, Part A

JF - Deep-Sea Research, Part A

IS - Suppl. 2A

ER -

Sediment deposition in the late Holocene abyssal Black Sea with climatic and chronological implications

Abstract

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