Articles | Volume 8, issue 2
https://doi.org/10.5194/essd-8-439-2016
https://doi.org/10.5194/essd-8-439-2016
23 Sep 2016
 | 23 Sep 2016

Biogeochemical data from terrestrial and aquatic ecosystems in a periglacial catchment, West Greenland

Tobias Lindborg, Johan Rydberg, Mats Tröjbom, Sten Berglund, Emma Johansson, Anders Löfgren, Peter Saetre, Sara Nordén, Gustav Sohlenius, Eva Andersson, Johannes Petrone, Micke Borgiel, Ulrik Kautsky, and Hjalmar Laudon

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Using ground-penetrating radar, topography and classification of vegetation to model the sediment and active layer thickness in a periglacial lake catchment, western Greenland
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Cited articles

Anderson, N. J., Harriman, R., Ryves, D. B., and Patrick, S. T.: Dominant factors controlling variability in the ionic composition of West Greenland lakes, Arct. Antarct. Alp. Res., 33, 418–425, 2001.
Anderson, N. J., Brodersen, K. P., Ryves, D. B., McGowan, S., Johansson, L. S., Jeppesen, E., and Leng, M. J.: Climate versus in-lake processes as controls on the development of community structure in a low-Arctic lake (South-West Greenland), Ecosystems, 11, 307–324, https://doi.org/10.1007/s10021-007-9123-y, 2008.
Anderson, N. J., D'Andrea, W., and Fritz, S. C.: Holocene carbon burial by lakes in SW Greenland, Glob. Change Biol., 15, 2590–2598, https://doi.org/10.1111/j.1365-2486.2009.01942.x, 2009.
Appleby, P. G.: Three decades of dating recent sediments by fallout radionuclides: a review, Holocene, 18, 83–93, https://doi.org/10.1177/0959683607085598, 2008.
Bronk Ramsey, C.: Bayesian analysis of radiocarbon dates, Radiocarbon, 51, 337–360, 2009.
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This paper presents a biogeochemical and ecological data set from the Kangerlussuaq region, western Greenland. The data set is used to conceptualize and model terrestrial and limnic ecosystems as well as the land–lake linkage. Both biotic and abiotic data is presented and will be used for biogeochemical mass-balance and transport calculations. The data set constitutes an important source in order to understand and describe accumulation and flow of matter within periglacial landscapes.
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