School of Science and the Environment, Manchester Metropolitan
University, Manchester, UK
Melissa Maher
School of Science and the Environment, Manchester Metropolitan
University, Manchester, UK
Jerome Blewett
School of Earth and Environmental Sciences and Williamson Research
Centre for Molecular Environmental Science, University of Manchester, Manchester, UK
now at: Organic Geochemistry Unit, School of Chemistry, Cabot Institute, University of Bristol, Bristol, UK
Ayça Doğrul Selver
School of Earth and Environmental Sciences and Williamson Research
Centre for Molecular Environmental Science, University of Manchester, Manchester, UK
Balıkesir University, Geological Engineering Department,
Balıkesir, Turkey
Department of Environmental Science and Analytical Chemistry (ACES)
and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden
Igor P. Semiletov
Pacific Oceanological Institute Far Eastern Branch of the Russian
Academy of Sciences, Vladivostok, Russia
International Arctic Research Center, University of Alaska, Fairbanks, USA
National Tomsk Research Polytechnic University, Tomsk, Russia
Bart E. van Dongen
School of Earth and Environmental Sciences and Williamson Research
Centre for Molecular Environmental Science, University of Manchester, Manchester, UK
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75
3,660
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Cumulative views and downloads
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Total article views: 2,709 (including HTML, PDF, and XML)
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1,950
689
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2,709
129
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PDF: 689
XML: 70
Total: 2,709
Supplement: 129
BibTeX: 57
EndNote: 59
Views and downloads (calculated since 11 Oct 2018)
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Total article views: 951 (including HTML, PDF, and XML)
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519
427
5
951
335
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HTML: 519
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Total: 951
Supplement: 335
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Total article views: 3,660 (including HTML, PDF, and XML)
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Total article views: 2,709 (including HTML, PDF, and XML)
Thereof 2,318 with geography defined
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Total article views: 951 (including HTML, PDF, and XML)
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Ongoing climate change in the Siberian Arctic region has the potential to release large amounts of carbon, currently stored in permafrost, to the Arctic Shelf. Degradation can release this to the atmosphere as greenhouse gas. We used Raman spectroscopy to analyse a fraction of this carbon, carbonaceous material, a group that includes coal, lignite and graphite. We were able to trace this carbon from the river mouths and coastal erosion sites across the Arctic shelf for hundreds of kilometres.
Ongoing climate change in the Siberian Arctic region has the potential to release large amounts...
