Event layer chronology from Lake Suigetsu (Japan, SG06 Project) for the last 40 kyr

DOI

Event layers in lake sediments are indicators of past extreme events, mostly the results of floods or earthquakes. Detailed characterisation of the layers allows the discrimination of the sedimentation processes involved, such as surface runoff, landslides or subaqueous slope failures. These processes can then be interpreted in terms of their triggering mechanisms. Here we present a 40 kyr event layer chronology from Lake Suigetsu, Japan. The event layers were characterised using a multi-proxy approach, employing light microscopy and µXRF for microfacies analysis. The vast majority of event layers in Lake Suigetsu was produced by flood events (362 out of 369), allowing the construction of the first long-term, quantitative (with respect to recurrence) and well dated flood chronology from the region. The flood layer frequency shows a high variability over the last 40 kyr, and it appears that extreme precipitation events were decoupled from the average long-term precipitation. For instance, the flood layer frequency is highest in the Glacial at around 25 kyr BP, at which time Japan was experiencing a generally cold and dry climate. Other cold episodes, such as Heinrich Event 1 or the Late Glacial stadial, show a low flood layer frequency. Both observations together exclude a simple, straightforward relationship with average precipitation and temperature. We argue that, especially during Glacial times, changes in typhoon genesis/typhoon tracks are the most likely control on the flood layer frequency, rather than changes in the monsoon front or snow melts. Spectral analysis of the flood chronology revealed periodic variations on centennial and millennial time scales, with 220 yr, 450 yr and a 2000 yr cyclicity most pronounced. However, the flood layer frequency appears to have not only been influenced by climate changes, but also by changes in erosion rates due to, for instance, earthquakes.

Project: Suigetsu Varves 2006

Supplement to: Schlolaut, Gordon; Brauer, Achim; Marshall, Michael H; Nakagawa, Takeshi; Staff, Richard A; Ramsey, Christopher Bronk; Lamb, Henry F; Bryant, Charlotte L; Naumann, Rudolf; Dulski, Peter; Brock, Fiona; Yokoyama, Yusuke; Tada, Ryuji; Haraguchi, Tsuyoshi; Suigetsu 2006 Project members (2014): Event layers in the Japanese Lake Suigetsu 'SG06' sediment core: description, interpretation and climatic implications. Quaternary Science Reviews, 83, 157-170

Identifier
DOI https://doi.org/10.1594/PANGAEA.821829
Related Identifier IsSupplementTo https://doi.org/10.1016/j.quascirev.2013.10.026
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.821829
Provenance
Creator Schlolaut, Gordon; Brauer, Achim ORCID logo; Marshall, Michael H ORCID logo; Nakagawa, Takeshi ORCID logo; Staff, Richard A (ORCID: 0000-0002-8634-014X); Ramsey, Christopher Bronk ORCID logo; Lamb, Henry F ORCID logo; Bryant, Charlotte L; Naumann, Rudolf; Dulski, Peter; Brock, Fiona ORCID logo; Yokoyama, Yusuke ORCID logo; Tada, Ryuji; Haraguchi, Tsuyoshi; Suigetsu 2006 Project members
Publisher PANGAEA
Publication Year 2014
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Representation
Resource Type Supplementary Publication Series of Datasets; Collection
Format application/zip
Size 3 datasets
Discipline Earth System Research
Spatial Coverage (135.883 LON, 35.583 LAT); Lake Suigetsu, Honshu, Japan