PANGAEA_963850
Magnetic Susceptibility from sediment core HZM19, Holzmaar (West-Eifel Volcanic Field, Germany)
García, María Luján; Birlo, Stella; Zahajská, Petra; Wienhues, Giulia; Grosjean, Martin; Zolitschka, Bernd
Magnetic Susceptibility from sediment core HZM19, Holzmaar (West-Eifel Volcanic Field, Germany)
2024-09-23
PANGAEA
Dataset
https://doi.pangaea.de/10.1594/PANGAEA.963850
Investigator
María Luján
García
garcia@uni-bremen.de
Earth Science
Depth, composite
AGE
Magnetic susceptibility
geoscientificInformation
Climate changes
HZM19
lakes
Pigments
Piston corer, UWITEC
Sediments
varves
XRF-core scanning
Calculated, based on VT22 (Birlo et al., 2023)
Magnetic susceptibility meter, Bartington MS2E sensor, 4 mm increments
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
Leobener Str.
Bremen
Bremen
28359
Germany
online
11984 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
Nowaczyk, Norbert R: Logging of Magnetic Susceptibility. In: Last, WM, Smol, JP (eds.), Tracking Environmental Change Using Lake Sediments, Developments in Paleoenvironmental Research, 1, Kluwer Academic Publishers, Dordrecht, 155-170, https://doi.org/10.1007/0-306-47669-X_8
Magnetic susceptibility (MS) measurements in 4 mm increments with a Bartington MS2E sensor mounted to a measuring bench (Nowaczyk, 2002, doi:10.1007/0-306-47669-X_8). 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.963850"! ** 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/10.1007/0-306-47669-X_8
Logging of Magnetic Susceptibility
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