Standardized mineral data of sediment core EN18208 from Lake Ilirney (Chukotka, 
Russia)

Biskaborn, Boris K.; Pfalz, Gregor; Vyse, Stuart Andrew; Diekmann, Bernhard; Andreev, Andrei A.; Nowaczyk, N.; Heim, Birgit; Wieczorek, Mareike; Pestryakova, Luidmila A.; Herzschuh, Ulrike

doi:10.1594/PANGAEA.953389

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Standardized mineral data of sediment core EN18208 from Lake Ilirney (Chukotka, Russia)

Biskaborn, B. K., Pfalz, G., Vyse, S. A., Diekmann, B., Andreev, A. A., Nowaczyk, N., Heim, B., Wieczorek, M., Pestryakova, L. A., Herzschuh, U. (2023): Standardized mineral data of sediment core EN18208 from Lake Ilirney (Chukotka, Russia).
https://doi.org/10.1594/PANGAEA.953389

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Datensatz-Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5023295 Versions-Permalink: https://gfzpublic.gfz-potsdam.de/pubman/item/item_5023295_2

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Urheber:
Biskaborn, Boris K.¹, Autor
Pfalz, Gregor¹, Autor
Vyse, Stuart Andrew¹, Autor
Diekmann, Bernhard¹, Autor
Andreev, Andrei A.¹, Autor
Nowaczyk, N.², Autor
Heim, Birgit¹, Autor
Wieczorek, Mareike¹, Autor
Pestryakova, Luidmila A.¹, Autor
Herzschuh, Ulrike¹, Autor

Affiliations:
1External Organizations, ou_persistent22
24.3 Climate Dynamics and Landscape Evolution, 4.0 Geosystems, Departments, GFZ Publication Database, Deutsches GeoForschungsZentrum, ou_146046

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Schlagwörter: Sediment core

Zusammenfassung: This data set is part of a larger data harmonization effort to make lake sediment core data machine readable and comparable. Here we standardized mineral data of sediment core EN18208, retrieved in 2018 from Lake Ilirney (Chukotka, Russia) at 10.76 m water depth. The glacial lake Ilirney is situated in the forest tundra mountain area and has one outflow, one main inflow and several smaller inflows. It lies at an elevation of ca. 428 m a.s.l. with a surface area of ca. 30 km2 and a maximum lake water depth of estimated 44 m. The 10.76 m sediment core was retrieved by a UWITEC piston corer during the RU-Land_2018_Chukotka expedition of the Alfred Wegener Institute Helmholtz Centre for Polar and Marine Research (AWI, Germany, Potsdam) in cooperation with the North Eastern Federal State University (NEFU, Russia, Yakutsk). Bulk mineralogy was analysed by (x-ray diffractometry (XRD) using a (PHILIPS, Netherlands) PW1820 goniometer.