Title of article :
Last Interglacial fossil elephant trackways dated by OSL/AAR in coastal aeolianites, Still Bay, South Africa
Author/Authors :
Roberts، نويسنده , , David L. and Bateman، نويسنده , , Mark D. and Murray-Wallace، نويسنده , , Colin V. and Carr، نويسنده , , Andrew S. and Holmes، نويسنده , , Peter J.، نويسنده ,
Issue Information :
روزنامه با شماره پیاپی سال 2008
Pages :
19
From page :
261
To page :
279
Abstract :
The impressive Pleistocene coastal aeolianite exposures in sea cliffs east of Still Bay on the west–southern coast of South Africa host a rich archive of fossil mammalian trackways, including the African elephant (Loxodonta africana). Neither the ichnofossils nor their host sediments have been described in any detail and chronologies remained uncertain. This paper presents a new optically stimulated luminescence (OSL) and amino acid racemisation (AAR) chronology (the first joint application of OSL/AAR dating in South Africa). This provides a temporal framework for assessing the palaeoenvironmental significance of dune sedimentation patterns, pedogenesis and ichnology. eistocene aeolianite exposures at Still Bay represent the recently eroded remnants of a dune cordon, mainly built by coalesced parabolic dune systems. Sedimentary facies are dominated by large-scale planar cross-stratification formed by foreset progradation in the nose and trailing arms of the dunes and low-angle bedding, chiefly representing sedimentation in low relief interdune terrain. The main dune building wind regime was westerly, associated with cyclonic polar frontal systems (as at the present time). The OSL and AAR dating demonstrate ages ranging from MIS 5e to 5b and termination of Pleistocene aeolian sedimentation at ∼ 90 ka. The Pleistocene aeolianite is separated from the overlying Holocene dunes (dated to ∼ 8 ka), by a major hiatus recorded by a horizon of intense pedogenesis. nt footprints were seen in profile, as casts on the underside of beds and as natural impressions. The taphonomic processes controlling the morphology and preservation of these unique ichnofossils were found to be complex. The presence of Loxodonta africana at Still Bay represents the southernmost occurrence of this species recorded to date and possibly, a closer proximity of woodland during MIS 5. This and other observations may indicate a higher moisture regime than at present. There is no available evidence that the elephants were predated by contemporary Middle Stone Age people.
Keywords :
Aeolianite , amino acid racemisation , Luminescence , Last Interglacial , Elephant trackways
Journal title :
Palaeogeography, Palaeoclimatology, Palaeoecology
Serial Year :
2008
Journal title :
Palaeogeography, Palaeoclimatology, Palaeoecology
Record number :
2296501
Link To Document :
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