TY - JOUR

T1 - Optically stimulated luminescence dating of young fluvial deposits of the Middle Elbe River Flood Plains using different age models

AU - Kunz, Alexander

AU - Pflanz, Dorte

AU - Weniger, Tobias

AU - Urban, Brigitte

AU - Krüger, Frank

AU - Chen, Yue-Gau

PY - 2014/3

Y1 - 2014/3

N2 - In the last few decades optically stimulated luminescence (OSL) dating has become an im-portant tool in geochronological studies. The great advantage of the method, i.e. dating the deposi-tional age of sediments directly, can be impaired by incomplete bleaching of grains. This can result in a scattered distribution of equivalent doses (DE), leading to incorrect estimation of the depositional age. Thoroughly tested protocols as well as good data analysis with adequate statistical methods are important to overcome this problem. In this study, samples from young fluvial sand and flood plain deposits from the Elbe River in northern Germany were investigated to compare its depositional ages from different age models with well-known historical dates. Coarse grain quartz (100-200 μm and 150-250 μm) and polymineral fine grains (4-11 μm) were dated using the single aliquot regenerative (SAR) dose protocol. The paleodose (DP) was calculated from the DE data set using different ap-proaches. Results were compared with the development of the Elbe River, which is well-documented by historical records and maps covering the last 1,000 years. Depending on the statistical approach it can be demonstrated that depositional ages significantly differ from the most likely depositional age. For the investigated coarse grain quartz samples all ages calculated from the MAM-3UL, including their uncertainties, are within the historical documented age. Results of the polymineral fine grain samples are overestimating the historically documented depositional age, indicating undetectable in-complete bleaching. This study shows the importance of using an adequate statistical approach to cal-culate reliable OSL ages from fluvial sediments.

AB - In the last few decades optically stimulated luminescence (OSL) dating has become an im-portant tool in geochronological studies. The great advantage of the method, i.e. dating the deposi-tional age of sediments directly, can be impaired by incomplete bleaching of grains. This can result in a scattered distribution of equivalent doses (DE), leading to incorrect estimation of the depositional age. Thoroughly tested protocols as well as good data analysis with adequate statistical methods are important to overcome this problem. In this study, samples from young fluvial sand and flood plain deposits from the Elbe River in northern Germany were investigated to compare its depositional ages from different age models with well-known historical dates. Coarse grain quartz (100-200 μm and 150-250 μm) and polymineral fine grains (4-11 μm) were dated using the single aliquot regenerative (SAR) dose protocol. The paleodose (DP) was calculated from the DE data set using different ap-proaches. Results were compared with the development of the Elbe River, which is well-documented by historical records and maps covering the last 1,000 years. Depending on the statistical approach it can be demonstrated that depositional ages significantly differ from the most likely depositional age. For the investigated coarse grain quartz samples all ages calculated from the MAM-3UL, including their uncertainties, are within the historical documented age. Results of the polymineral fine grain samples are overestimating the historically documented depositional age, indicating undetectable in-complete bleaching. This study shows the importance of using an adequate statistical approach to cal-culate reliable OSL ages from fluvial sediments.

KW - Environmental planning

KW - age model

KW - elbe river floodplain

KW - fluvial sand

KW - north germany

KW - optically stimulated luminescence dating

UR - http://www.scopus.com/inward/record.url?scp=84896779499&partnerID=8YFLogxK

U2 - 10.2478/s13386-013-0140-7

DO - 10.2478/s13386-013-0140-7

M3 - Journal articles

VL - 41

SP - 36

EP - 56

JO - Geochronometria

JF - Geochronometria

SN - 1733-8387

IS - 1

ER -