Stable isotope signatures of Holocene syngenetic permafrost in the Thule District (NW Greenland)

Holocene permafrost peat from sites in the Thule District, NW Greenland, was studied for organic matter composition, i.e. TOC, TN, δ13C and δ15N. The material was obtained from radiocarbon-dated drill cores reaching 320 cm below surface (bs) in core GL3 (76.03288°N, 67.61811°W) and 198 cm bs in core SI1 (76.56908°N, 70.04099°W). Furthermore, the isotopic composition (δ18O and δD) of one GL3 ice wedge was analysed.

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Cite this as

Wetterich, Sebastian, Davidson, Thomas A, Meyer, Hanno (2019). Dataset: Stable isotope signatures of Holocene syngenetic permafrost in the Thule District (NW Greenland). https://doi.org/10.1594/PANGAEA.907403

DOI retrieved: 2019

Additional Info

Field Value
Imported on November 30, 2024
Last update November 30, 2024
License CC-BY-4.0
Source https://doi.org/10.1594/PANGAEA.907403
Author Wetterich, Sebastian
Given Name Sebastian
Family Name Wetterich
More Authors
Davidson, Thomas A
Meyer, Hanno
Source Creation 2019
Publication Year 2019
Resource Type application/zip - filename: Wetterich-etal_2019
Subject Areas
Name: Chemistry

Name: Lithosphere

Related Identifiers
Title: Stable isotope signatures of Holocene syngenetic permafrost trace seabird presence in the Thule District (NW Greenland)
Identifier: https://doi.org/10.5194/bg-2019-71
Type: DOI
Relation: IsSupplementTo
Year: 2019
Source: Biogeosciences Discussions
Authors: Wetterich Sebastian , Davidson Thomas A , Bobrov Anatoly A , Opel Thomas , Windirsch Torben , Johansen Kasper L , González-Bergonzoni Ivan , Mosbech Anders , Jeppesen Erik .