n-alcohol characteristics of Arctic soils, comparing different large herbivore grazing intensities under permafrost and non-permafrost conditions ...
These data originate from soil samples collected on several field campaigns, aiming at identifying impacts of large herbivore activity on soil carbon storage and degradation in permafrost (northeastern Siberia (68.51 °N, 161.50 °E); campaign in July 2019) and seasonally frozen Arctic ground (norther...
Main Authors: | , , , , , |
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Format: | Dataset |
Language: | English |
Published: |
PANGAEA
2023
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Subjects: | |
Online Access: | https://dx.doi.org/10.1594/pangaea.963259 https://doi.pangaea.de/10.1594/PANGAEA.963259 |
Summary: | These data originate from soil samples collected on several field campaigns, aiming at identifying impacts of large herbivore activity on soil carbon storage and degradation in permafrost (northeastern Siberia (68.51 °N, 161.50 °E); campaign in July 2019) and seasonally frozen Arctic ground (northern Finland (69.15 °N, 27.00 °E); campaigns in September 2020 and June 2022).The samples were collected in transects across grazing intensity gradients, spanning over 5 different intensities:1 - no grazing / exclosure sites (Siberia: 23 years; Finland: 50 years)2 - occasional animal migration (Siberia: year-round; Finland: seasonal)3 - daily animal migration (Siberia: year-round; Finland: seasonal)4 - high-frequency daily animal migration (Siberia: year-round; Finland: seasonal)5 - pasture / supplementary feeding sites (Siberia: year-round; Finland: seasonal)Samples cover different ground types and seasonalities, which are marked out in the site names:B - drained thermokarst basinU - Yedoma uplandP - peatM - mineral ... |
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