Middle Pleistocene interglacial peat deposits from Northern Germany investigated by 230Th/U and palynology: Case studies from Wedel and Schöningen
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In: Zeitschrift der Deutschen Gesellschaft für Geowissenschaften, Vol. 168 , No. 3, 01.11.2017, p. 373 - 387.
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TY - JOUR
T1 - Middle Pleistocene interglacial peat deposits from Northern Germany investigated by 230Th/U and palynology
T2 - Case studies from Wedel and Schöningen
AU - Sierralta, Melanie
AU - Urban, Brigitte
AU - Linke, Gerhard
AU - Frechen, Manfred
PY - 2017/11/1
Y1 - 2017/11/1
N2 - Interstadial and interglacial deposits including peat layers are widespread in Northern Europe and enable us to reconstruct the past climate and vegetation history. Such reconstructions require a reliable and precise chronological framework. Uranium series dating, sedimentological and palynological investigations were performed on a peat deposit at Wedel in Schleswig-Holstein. Previous palynological studies suggested a Middle Pleistocene age for these interglacial deposits. The sediment sequence including a fen peat of 130 cm thickness at a depth of 14-15 m below surface was drilled and cored. Palynological results correlate well to the late Holsteinian Interglacial, but the radiometric age determination failed due to U-series open system behaviour. Comparison of results obtained at Wedel with those from Holsteinian Interglacial deposits in Northern Germany reveals the weakness of numerical age determinations. Furthermore, a brief discussion on radiometric data available of the Middle Pleistocene Reinsdorf Interglacial peat deposits at Schöningen is given, as the laboratory has performed further quality assurance processes. A spike calibration led to new calculations on isotope activities, resulting in higher values shifted by 5-7 % and corrections on published data of the same order. The age of the Reinsdorf Interglacial peat deposit 13 II-2c5 cannot be maintained as the assigned errors inhibit the calculation of reasonable mean ages nearby the methodological age limits.
AB - Interstadial and interglacial deposits including peat layers are widespread in Northern Europe and enable us to reconstruct the past climate and vegetation history. Such reconstructions require a reliable and precise chronological framework. Uranium series dating, sedimentological and palynological investigations were performed on a peat deposit at Wedel in Schleswig-Holstein. Previous palynological studies suggested a Middle Pleistocene age for these interglacial deposits. The sediment sequence including a fen peat of 130 cm thickness at a depth of 14-15 m below surface was drilled and cored. Palynological results correlate well to the late Holsteinian Interglacial, but the radiometric age determination failed due to U-series open system behaviour. Comparison of results obtained at Wedel with those from Holsteinian Interglacial deposits in Northern Germany reveals the weakness of numerical age determinations. Furthermore, a brief discussion on radiometric data available of the Middle Pleistocene Reinsdorf Interglacial peat deposits at Schöningen is given, as the laboratory has performed further quality assurance processes. A spike calibration led to new calculations on isotope activities, resulting in higher values shifted by 5-7 % and corrections on published data of the same order. The age of the Reinsdorf Interglacial peat deposit 13 II-2c5 cannot be maintained as the assigned errors inhibit the calculation of reasonable mean ages nearby the methodological age limits.
KW - Sustainability Science
KW - wedel
KW - peat
KW - schöningen
KW - interglacial
KW - holsteinian
KW - 230 th/u dating
KW - palynology
UR - http://www.scopus.com/inward/record.url?scp=85034626715&partnerID=8YFLogxK
U2 - 10.1127/zdgg/2017/0065
DO - 10.1127/zdgg/2017/0065
M3 - Journal articles
VL - 168
SP - 373
EP - 387
JO - Zeitschrift der Deutschen Gesellschaft für Geowissenschaften
JF - Zeitschrift der Deutschen Gesellschaft für Geowissenschaften
SN - 1860-1804
IS - 3
ER -