PANGAEA_963851 X-ray fluorescense (XRF) core scanning from sediment core HZM19, Holzmaar (West-Eifel Volcanic Field, Germany) García, María Luján; Birlo, Stella; Zahajská, Petra; Wienhues, Giulia; Grosjean, Martin; Zolitschka, Bernd X-ray fluorescense (XRF) core scanning from sediment core HZM19, Holzmaar (West-Eifel Volcanic Field, Germany) 2024-09-23 PANGAEA Dataset https://doi.pangaea.de/10.1594/PANGAEA.963851 Investigator María Luján García garcia@uni-bremen.de Earth Science Section Section position Depth, composite AGE Zone Silicon (centered log ratio) Potassium (centered log ratio) Manganese (centered log ratio) Iron (centered log ratio) Logarithmic scattering ratio, ln incoherent/coherent geoscientificInformation Climate changes HZM19 lakes Pigments Piston corer, UWITEC Sediments varves XRF-core scanning Calculated, based on VT22 (Birlo et al., 2023) X-ray fluorescence core scanner, Cox Analytical, ITRAX, Cr-tube 30kV 55mA 2019-08-11 2019-08-17 Complete 50.11667 50.11667 6.883333 6.883333 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

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Bremen Bremen 28359 Germany online 59920 data points text/tab-separated-values García, María Luján; Birlo, Stella; Zahajská, Petra; Wienhues, Giulia; Grosjean, Martin; Zolitschka, Bernd (2024): Ecological responses to solar forcing during the Homerian Climate Anomaly recorded by varved sediments from Holzmaar, Germany. The Holocene, https://doi.org/10.1177/09596836241275008 Croudace, Ian W; Rothwell, Robin Guy (2015): Micro-XRF Studies of Sediment Cores. Developments in Paleoenvironmental Research, Springer Netherlands, Dordrecht, 17, https://doi.org/10.1007/978-94-017-9849-5

XRF measurements in 0.2 to 1 mm increments with an ITRAX XRF core scanner (Cox Analytics) and Cr tube (Croudance et al. 2015, doi:10.1007/978-94-017-9849-5 ). The sediment core HZM19 was collected in 2019, from Holzmaar, West-Eifel Volcanic Field in Germany using a UWITEC Piston Corer. The sediment core was collected to reconstruct environmental and climate changes of Holzmaar for the last 16,000 years cal BP. Particularly in this data set we cover between 2450-2950 cal BP. ** For all details see the full metadata description at "https://doi.pangaea.de/10.1594/PANGAEA.963851"! ** Funding information: * Georg Forster Research Fellowship for postdoctoral researchers (for the Alexander von Humboldt funding) * Central Research Development Fund (CRDF) of the University of Bremen, 04 Independent Project for Postdocs - Funding objective B

http://en.wikipedia.org/wiki/Kyr AGE https://doi.org/10.1007/978-94-017-9849-5 Micro-XRF Studies of Sediment Cores https://doi.org/10.1177/09596836241275008 Ecological responses to solar forcing during the Homerian Climate Anomaly recorded by varved sediments from Holzmaar, Germany https://doi.org/10.5194/gchron-5-65-2023 Calculated, based on VT22 (Birlo et al., 2023) DIF 9.4 2024-09-23 2026-05-07