PANGAEA_925709 Magnetization intensities of redeposited Black Sea sediment from the last glacial Nowaczyk, Norbert R Magnetization intensities of redeposited Black Sea sediment from the last glacial 2020-12-14 PANGAEA Dataset https://doi.pangaea.de/10.1594/PANGAEA.925709 Investigator Norbert R Nowaczyk norbert.nowaczyk@gfz-potsdam.de Earth Science Magnetic field Detrital remanent magnetization intensity Detrital remanent magnetization Components, magnetic Action geoscientificInformation depositional remanent magnetization Complete unrestricted CC-BY-4.0: Creative Commons Attribution 4.0 International English PANGAEA Data Publisher for Earth & Environmental Science https://www.pangaea.de/ Data Center Contact Michael Diepenbroek info@pangaea.de

Leobener Str.

Bremen Bremen 28359 Germany online 430 data points text/tab-separated-values Nowaczyk, Norbert R (2021): Redeposition experiments with natural sediments from the SE Black Sea in magnetic fields between about 2 and 114 µT. Geophysical Journal International, 224(1), 271-289, https://doi.org/10.1093/gji/ggaa455

This data publication provides data on redeposition experiments with mud collected during paleomagnetic sampling of various cores from the Arkhangelsky Ridge, SE Black Sea, recovered during marine expedition M72/5 of German research vessel RV METEOR in 2007 and expedition MSM33 of German research vessel RV Maria S. Merian in 2013. The collected silici-clastic mud mostly originates from glacial sediments deposited during marine isotope stages (MIS) 2 to 4, and 6. The material (bulk/mixed sample) originates from 208m to 847m water depth, 41° 28.66'N to 42° 13.57'N in latitude, and 36° 29.53'E to 37° 11.68'E in longitude. Experiments were performed in order to check the (non-) linearity of the detrital remanent magnetization (DRM) of Black Sea sediments acquired in different magnetic fields. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.925709"! ** Component(s) of the ambient magnetic field set by the coils system. H - horizontal component V – vertical component vibr. - vibrating platform still – still platform

https://doi.org/10.1093/gji/ggaa455 Redeposition experiments with natural sediments from the SE Black Sea in magnetic fields between about 2 and 114 µT DIF 9.4 2020-12-14 2026-04-30