Multiproxy analyses of stratigraphy and palaeoenvironment of the late Palaeolithic Grabow floodplain site, northern Germany. / Tolksdorf, Johann Friedrich; Turner, Falko; Kaiser, Knut; Eckmeier, Eileen; Stahlschmidt, Mareike; Housley, Rupert A.; Breest, Klaus; Veil, Stephan.

In: Geoarchaeology, Vol. 28, No. 1, 15.02.2013, p. 50-65.

Research output: Contribution to journalArticle

Published
  • Johann Friedrich Tolksdorf
  • Falko Turner
  • Knut Kaiser
  • Eileen Eckmeier
  • Mareike Stahlschmidt
  • Rupert A. Housley
  • Klaus Breest
  • Stephan Veil

Abstract

Changing river courses and fluctuations of the water table were some of the
most fundamental environmental changes that humans faced during the Late
Glacial, particularly as these changes affected areas intensively used for settlement and resource exploitation. Unfortunately, only a few stratigraphies
have been documented in the North European plain that show the interaction
between river development, vegetation history, and occupation by Late
Palaeolithic humans. Here, we present the results of detailed stratigraphical
studies (pedology, archaeology, chrono-, tephra-, and palynostratigraphy) at
the Federmesser site Grabow 15 located in the broad Elbe River valley. The
research aimed to produce a model of site formation based on a multiproxy approach, relating the local evidence to the palaeoenvironmental and settlement
history of the wider region. After deposition of fluvial sands during the Late
Pleniglacial in a braided setting, the river course developed locally toward a
meandering system at the transition from the Older Dryas to the Allerød, while
periodic flooding led to the deposition of floodplain sediments during the early
Allerød. The floodplain was settled by people of the earliest “Federmessergruppen,” who are believed to have chosen this open floodplain area along the river for collecting and processing amber of local origin. Their artifacts became embedded in the aggrading floodplain sediments. In the late Allerød, floodplain sedimentation ceased and a Fluvisol-type soil developed, indicating a trend toward geomorphic stability. The Fluvisol was then covered by silty floodplain sediments due to a rising water level during the late Younger Dryas resulting in the cessation of human occupation in the area. Subsequent organic-rich Late Glacial/Holocene sediments preserved the settlement remains to the present.
Original languageEnglish
Pages (from-to)50-65
Number of pages16
JournalGeoarchaeology
Volume28
Issue number1
Early online date7 Dec 2012
DOIs
Publication statusPublished - 15 Feb 2013
This open access research output is licenced under a Creative Commons Attribution-NonCommercial-NoDerivs 3.0 Unported License.

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