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A Pronounced Dry Event Recorded Around 4.2 ka in Brine Sediments from the Northern Red Sea

Datos Bibliográficos

ID24085408
AutoresHelge W Arz (0000-0002-1997-1718, GFZ Helmholtz Centre for Geosciences, autor de correspondencia), Frank Lamy (0000-0001-5952-1765, GFZ Helmholtz Centre for Geosciences), Jürgen Pätzold (0000-0001-8074-4103, University of Bremen)
Año2006
Volumen66
Número3
Páginas432-441
Fecha de publicación2006-11-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary Research (JOURNAL)
Identificadores de la revistaISSN: 0033-5894 • E-ISSN: 1096-0287
EditorialCambridge University Press (CUP) (PUBLISHER)
DOI10.1016/j.yqres.2006.05.006
OpenAlexW2015490689
IdiomaEN
Citas recibidas51
Referencias citadas52

Partly laminated sediments were sampled from the brine-filled, anoxic Shaban Deep basin in the northern Red Sea. At about 4200 cal yr BP more than two millennia of anoxic sedimentation is replaced by a sub-oxic facies strongly suggesting the episodic absence of the brine. At the same time stable oxygen isotopes from surface dwelling foraminifera show a sharp increase (within less than 100 yr) pointing to a strong positive salinity anomaly at the sea surface. This major evaporation event significantly enhanced the renewal of deep water and the subsequent ventilation of the small Shaban Deep basin. The timing and strength of the reconstructed environmental changes around 4200 cal yr BP suggest that this event is the regional expression of a major drought event, which is widely observed in the neighboring regions, and which strongly affected Middle East agricultural civilizations.

Anoxic waters · Brine · Facies · Foraminifera · Geochemistry · Salinity · Sea level · Structural basin · Geology · Geology and Paleoclimatology Research · Isotope Analysis in Ecology · Marine and environmental studies · Oceanography · Paleontology

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Obras citantes distintas51
Citas por año2,55
Intervalo de citas2006 - 2025 (20)
Velocidad de citaciónrecent
Altamente citadoNo
Tipos de citaNeutras: 46
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