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AMS Radiocarbon and Varve Chronology from the Annually Laminated Sediment Record of Lake Meerfelder Maar, Germany

Published online by Cambridge University Press:  18 July 2016

Achim Brauer ,
Christoph Endres ,
Bernd Zolitschka  and
Jörg FW Negendank
Achim Brauer
Affiliation:
GeoForschungsZentrum (GFZ), Projektbereich 3.3, Sedimente und Beckenbildung, Telegrafenberg, D-14473 Potsdam, Germany. Email: brau@gfz-potsdam.de
Christoph Endres
Affiliation:
GeoForschungsZentrum (GFZ), Projektbereich 3.3, Sedimente und Beckenbildung, Telegrafenberg, D-14473 Potsdam, Germany. Email: brau@gfz-potsdam.de
Bernd Zolitschka
Affiliation:
GeoForschungsZentrum (GFZ), Projektbereich 3.3, Sedimente und Beckenbildung, Telegrafenberg, D-14473 Potsdam, Germany. Email: brau@gfz-potsdam.de
Jörg FW Negendank
Affiliation:
GeoForschungsZentrum (GFZ), Projektbereich 3.3, Sedimente und Beckenbildung, Telegrafenberg, D-14473 Potsdam, Germany. Email: brau@gfz-potsdam.de
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Abstract

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The Holocene varve chronology of annually laminated sediment sequences from Lake Meerfelder Maar agree for most of the record with dendro-calibrated accelerator mass spectronomy radiocarbon dates from the same site. Only between 9710 and 9950 cal BP does an offset of 240 yr appear between both data sets. At this position, a micro-disturbance in the varve succession has been detected by thin section analyses and was quantified in terms of missing varves. A comparison with the nearby record from Lake Holzmaar, as well providing high resolution AMS 14C and varve chronologies, revealed that such gaps (ca. 2% in time for the entire Holocene) are exceptional for these long-varved maar lake records. Moreover, since sections of missing years appear for both profiles at different stratigraphic positions, a combination of both the Meerfelder Maar and Holzmaar records enables us to bridge erroneous zones in varve chronologies. This confirms the high potential of two long-varved records in close vicinity to each other for the elimination of dating errors and for increasing chronological precision at a time resolution that is normally regarded as within the counting errors. Late Glacial varve and 14C data beyond the dendro-calibration from Meerfelder Maar and their tentative tele-connections to other high resolution data sets reveal unexplained age discrepancies in the calendar year time scale of about 200 years.

Type
Varve Chronologies
Information
Radiocarbon , Volume 42 , Issue 3 , 2000 , pp. 355 - 368
Copyright
Copyright © 2000 The Arizona Board of Regents on behalf of the University of Arizona 

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