14C Dated Chronology of the Thickest and Best Resolved Loess/Paleosol Record of the LGM from SE Hungary Based on Comparing Precision and Accuracy of Age-Depth Models. Issue 2 (10th April 2020)

• Record Type: Journal Article
• Authors: Sümegi, Pál; Gulyás, Sándor; Molnár, Dávid; Szilágyi, Gábor; Sümegi, Balázs P; Törőcsik, Tünde; Molnár, Mihály
• Is Part Of: Radiocarbon. Volume 62:Issue 2(2020)
• Page Start: 403
• Page End: 417
• Publication Date: 2020-04-10
• Subjects: accumulation rates, -- accuracy, -- age-depth models, -- 14C AMS dates, -- loess/paleosol sequence, -- SE Hungary; Radiocarbon dating -- Periodicals; 930.1028505
• DOI: 10.1017/RDC.2019.154
• Languages: English
• ISSNs: 0033-8222

Abstract

ABSTRACT: The Madaras profile found at the northernmost fringe of Bácska loess plateau is one of the thickest and best-developed last glacial loess sequences of Central Europe. The 10-m profile corresponds to a period between 29 and 12 b2k. To unravel feedback to small-scale centennial climatic fluctuations at our site, recorded in the Greenland ice and North Atlantic marine cores, construction of a reliable chronology is needed. Reliability is expressed in terms of best achievable chronological precision. Accuracy however is based on choosing the model best describing the sedimentological features of our profile. Five different age-depth models had constructed and compared relying on 15 14 C dates using various statistical, probabilistic approaches to choose the model with the highest achievable precision. Accuracy was also evaluated using accumulation rates against stratigraphy. Models constructed using the computer program Bacon performed best in terms of achieving the best possible stratigraphic accuracy. Seven meters of the profile represents the period of the LGM. The average sedimentation time was 16.8 yr/cm with the highest confined to the period of the LGM. Calculated average sedimentation rates were 4 times higher than previously reported. The peak accumulation periods are dated to the nadir of the LGM.