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Bibliographic Details
Main Authors: Shimkus, Kazimir M, Rozanov, Alexander G
Format: Dataset Open Access
Language:en
Published: PANGAEA 1999
Subjects:
Online Access:https://doi.org/10.1594/PANGAEA.760706
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author Shimkus, Kazimir M
Rozanov, Alexander G
author_facet Shimkus, Kazimir M
Rozanov, Alexander G
collection Datos científicos de ciencias marinas y ambientales
contents Results of a lithological study of bottom sediments in the Syrian region of the Mediterranean Sea during Cruise 27 of R/V Vityaz (1993) are reported. Suspended sediment discharge of the Nile River are of the greatest importance for terrigenous sedimentation in the SE part of the Mediterranean Sea, especially in deep-sea areas. Suspended load entering from the Syrian catchment area plays an important role in formation of recent shelf and slope deposits. Supply of aerosols from Syrian and Arabian deserts was distinguished by the patchiness of surface distribution of quartz. During Late Quaternary accumulation of terrigenous material supplied from both the Syrian and the Nile drainage areas was irregular. Sedimentation was remarkably enhanced during sapropel formation 7000-9000 years BP.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_760706
institution PANGAEA
language en
publishDate 1999
publisher PANGAEA
record_format pangaea
spellingShingle Composition of Upper Quaternary bottom sediments from the Syrian area of the Mediterranean Sea
Shimkus, Kazimir M
Rozanov, Alexander G
Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; Vy27-3941; Vy27-4007
Results of a lithological study of bottom sediments in the Syrian region of the Mediterranean Sea during Cruise 27 of R/V Vityaz (1993) are reported. Suspended sediment discharge of the Nile River are of the greatest importance for terrigenous sedimentation in the SE part of the Mediterranean Sea, especially in deep-sea areas. Suspended load entering from the Syrian catchment area plays an important role in formation of recent shelf and slope deposits. Supply of aerosols from Syrian and Arabian deserts was distinguished by the patchiness of surface distribution of quartz. During Late Quaternary accumulation of terrigenous material supplied from both the Syrian and the Nile drainage areas was irregular. Sedimentation was remarkably enhanced during sapropel formation 7000-9000 years BP.
title Composition of Upper Quaternary bottom sediments from the Syrian area of the Mediterranean Sea
topic Archive of Ocean Data; ARCOD; GC; Gravity corer; Mediterranean Sea; Vy27-3941; Vy27-4007
url https://doi.org/10.1594/PANGAEA.760706