Age model of sediment core GeoTü SL167


The age model of sediment core GeoTü SL167 is based on 14C AMS measurements of planktonic foraminifera and is calibrated with the BACON v. 2.5.6 software for R (Blaauw & Christen, 2011) and a marine reservoir age of ΔR = 93 ± 61 years. The ΔR is based on the weighted mean of two regional marine reservoir corrections (Muscat) by Southon et al. (2002) using the marine calibration database (Reimer and Reimer, 2001, Gravity core GeoTü SL167, was retrieved at station no. 960 during R.V. METEOR cruise M74/1b in 2007 (Bohrmann et al., 2010) from the northwestern Arabian Sea off Oman, at 22°37.2'N, 59°41.5'E, 774 m water depth, core recovery 7.39 m. The sediment core was retrieved for the reconstruction of circulation and productivity changes in the eastern Mediterranean Sea during the late Quaternary with particular focus on changes in the Indian monsoon system.

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Metadata Access
Creator Burdanowitz, Nicole ORCID logo; Schmiedl, Gerhard ORCID logo; Gaye, Birgit; Munz, Philipp ORCID logo; Schulz, Hartmut
Publisher PANGAEA
Publication Year 2024
Funding Reference German Research Foundation Crossref Funder ID 390683824 EXC 2037: Climate, Climatic Change, and Society (CLICCS)
Rights Creative Commons Attribution 4.0 International;
OpenAccess true
Resource Type Dataset
Format text/tab-separated-values
Size 147 data points
Discipline Earth System Research
Spatial Coverage (59.691 LON, 22.619 LAT); Oman Margin