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Biogeochemical data from terrestrial and aquatic ecosystems in a periglacial catchment, West Greenland
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Number of Authors: 14
2016 (English)In: Earth System Science Data, ISSN 1866-3508, E-ISSN 1866-3516, Vol. 8, no 2, 439-459 p.Article in journal (Refereed) Published
Abstract [en]

Global warming is expected to be most pronounced in the Arctic where permafrost thaw and release of old carbon may provide an important feedback mechanism to the climate system. To better understand and predict climate effects and feedbacks on the cycling of elements within and between ecosystems in northern latitude landscapes, a thorough understanding of the processes related to transport and cycling of elements is required. A fundamental requirement to reach a better process understanding is to have access to high-quality empirical data on chemical concentrations and biotic properties for a wide range of ecosystem domains and functional units (abiotic and biotic pools). The aim of this study is therefore to make one of the most extensive field data sets from a periglacial catchment readily available that can be used both to describe present-day periglacial processes and to improve predictions of the future. Here we present the sampling and analytical methods, field and laboratory equipment and the resulting biogeochemical data from a state-of-the-art whole-ecosystem investigation of the terrestrial and aquatic parts of a lake catchment in the Kangerlussuaq region, West Greenland. This data set allows for the calculation of whole-ecosystem mass balance budgets for a long list of elements, including carbon, nutrients and major and trace metals. The data set is freely available and can be downloaded from PANGAEA: doi: 10.1594/PANGAEA.860961.

Place, publisher, year, edition, pages
2016. Vol. 8, no 2, 439-459 p.
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Earth and Related Environmental Sciences
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URN: urn:nbn:se:su:diva-135251DOI: 10.5194/essd-8-439-2016ISI: 000384596100002OAI: oai:DiVA.org:su-135251DiVA: diva2:1045032
Available from: 2016-11-08 Created: 2016-11-01 Last updated: 2016-11-08Bibliographically approved

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