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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 3 | Copyright
Clim. Past, 12, 713-727, 2016
https://doi.org/10.5194/cp-12-713-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 21 Mar 2016

Research article | 21 Mar 2016

A distal 140 kyr sediment record of Nile discharge and East African monsoon variability

Werner Ehrmann1, Gerhard Schmiedl2, Martin Seidel1, Stefan Krüger1, and Hartmut Schulz3 Werner Ehrmann et al.
  • 1Universität Leipzig, Institut für Geophysik und Geologie, Talstraße 35, 04103 Leipzig, Germany
  • 2Universität Hamburg, Centrum für Erdsystemforschung und Nachhaltigkeit, Bundesstraße 55, 20146 Hamburg, Germany
  • 3Universität Tübingen, Fachbereich Geowissenschaften, Hölderlinstraße 12, 72074 Tübingen, Germany

Abstract. Clay mineral assemblages in a sediment core from the distal Nile discharge plume off Israel have been used to reconstruct the late Quaternary Nile sediment discharge into the eastern Mediterranean Sea (EMS). The record spans the last ca. 140kyr. Smectite abundances indicate the influence of the Blue Nile and the Atbara River that have their headwaters in the volcanic rocks of the Ethiopian Highlands. Kaolinite abundances indicate the influence of wadis, which contribute periodically to the suspension load of the Nile.

Due to the geographical position, the climate and the sedimentary framework of the EMS is controlled by two climate systems. The long-term climate regime was governed by the African monsoon that caused major African humid periods (AHPs) with enhanced sediment discharge at 132 to <126 (AHP 5), 116 to 99 (AHP4), and 89 to 77ka (AHP3). They lasted much longer than the formation of the related sapropel layers S5 (>2kyr), S4 (3.5kyr), and S3 (5kyr). During the last glacial period (Marine Isotope Stages (MISs) 4–2), the long-term changes in the monsoonal system were superimposed by millennial-scale changes in an intensified midlatitude glacial system. This climate regime caused short but pronounced drought periods in the Nile catchment, which are linked to Heinrich events and alternate with more humid interstadials.

The clay mineral record further implies that feedback mechanisms between vegetation cover and sediment discharge of the Nile are detectable but of minor importance for the sedimentary record in the southeastern Mediterranean Sea during the investigated African humid periods.

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