https://doi.pangaea.de/10.1594/PANGAEA.995171Zander, Paul DPaul DZander0000-0001-7340-4768Max Planck Institute for ChemistryBöhl, DanielDanielBöhlMax Planck Institute for ChemistrySirocko, FrankFrankSirocko0000-0002-3131-0613Johannes Gutenberg-Universität MainzAuderset, AlexandraAlexandraAuderset0000-0002-6316-4980University of SouthamptonMartínez-García, AlfredoAlfredoMartínez-GarcíaMax Planck Institute for ChemistryHaug, Gerald HGerald HHaugMax Planck Institute for ChemistryPANGAEA2026EuropeGDGTsLacustrine-palustrine sedimentPaleoclimateEvent labelSample IDDEPTH, sediment/rockAgeLongitude of eventLatitude of eventElevation of eventSample massIsoprenoid acyclic glycerol dialkyl glycerol tetraetherIsoprenoid monocyclic glycerol dialkyl glycerol tetraetherIsoprenoid dicyclic glycerol dialkyl glycerol tetraetherIsoprenoid tricyclic glycerol dialkyl glycerol tetraetherCrenarchaeolCrenarchaeol isomerBranched glycerol dialkyl glycerol tetraether, IIIaBranched glycerol dialkyl glycerol tetraether, IIIa'Branched glycerol dialkyl glycerol tetraether, IIIa''Branched glycerol dialkyl glycerol tetraether, IIIbBranched glycerol dialkyl glycerol tetraether, IIIb'Branched glycerol dialkyl glycerol tetraether, IIIcBranched glycerol dialkyl glycerol tetraether, IIIc'Branched glycerol dialkyl glycerol tetraether, IIaBranched glycerol dialkyl glycerol tetraether, IIa'Branched glycerol dialkyl glycerol tetraether, IIbBranched glycerol dialkyl glycerol tetraether, IIb'Branched glycerol dialkyl glycerol tetraether, IIcBranched glycerol dialkyl glycerol tetraether, IIc'Branched glycerol dialkyl glycerol tetraether, IaBranched glycerol dialkyl glycerol tetraether, IbBranched glycerol dialkyl glycerol tetraether, IcTemperature, air, mean of months, above freezingCommentCable Core DrillingPiston corer, UWITECFreeze corerHigh Performance Liquid Chromatography (HPLC)BayMBT - Bayesian calibration for the branched GDGT MBT5Me proxyCalculated according to Raberg et al. (2021)2017-09-01T00:00:00/2017-09-30T00:00:00Dataset10.5194/cp-20-841-202410.1594/PANGAEA.96427510.1016/j.gca.2021.04.03810.5194/bg-18-3579-202110.1038/s41598-022-22464-x10.1038/s41561-021-00786-19496 data pointstext/tab-separated-valuesCreative Commons Attribution 4.0 InternationalIsoprenoid and branched GDGTs were measured in soils and lake sediment samples from the Eifel Volcanic field. The modern samples were used to understand sources of GDGTs in sediments, while sediment core samples from Schalkenmehrener Maar, Holzmaar, and Auel Maar were used to reconstruct temperatures during the past 60,000 years. Age model information and additional proxy data from the ELSA-20 stack are found in Sirocko et al., 2021 and Sirocko et al., 2022This is a revised version of doi:10.1594/PANGAEA.964277. Temperature reconstruction was removed for 3 data points that were not included in the final published reconstruction.
Empty cells correspond to measurements of GDGTs below the detection limit.6.5949334786.87916341150.119343450.28246449Aueler Maar, Eifel, GermanyLake Holzmaar, Eifel, GermanySchalkenmehrener Maar, Eifel, GermanySwiss National Science Foundationhttps://doi.org/10.13039/501100001711206731Molecular perspectives on hydroclimate response to rapid temperature change in Central Europe during the last glacial cycle