Articles | Volume 20, issue 2
https://doi.org/10.5194/bg-20-365-2023
https://doi.org/10.5194/bg-20-365-2023
Research article
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24 Jan 2023
Research article | Highlight paper |  | 24 Jan 2023

Permafrost degradation and nitrogen cycling in Arctic rivers: insights from stable nitrogen isotope studies

Adam Francis, Raja S. Ganeshram, Robyn E. Tuerena, Robert G. M. Spencer, Robert M. Holmes, Jennifer A. Rogers, and Claire Mahaffey

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EGUsphere, https://doi.org/10.5194/egusphere-2026-4372,https://doi.org/10.5194/egusphere-2026-4372, 2026
This preprint is open for discussion and under review for Biogeosciences (BG).
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Cited articles

Amon, R. M. W., Rinehart, A. J., Duan, S., Louchouarn, P., Prokushkin, A., Guggenberger, G., Bauch, D., Stedmon, C., Raymond, P. A., Holmes, R. M., McClelland, J. W., Peterson, B. J., Walker, S. A., and Zhulidov, A. V.: Dissolved organic matter sources in large Arctic rivers, Geochim. Cosmochim. Ac., 94, 217–237, https://doi.org/10.1016/J.GCA.2012.07.015, 2012. 
Anisimov, O. and Reneva, S.: Permafrost and changing climate: the Russian perspective, Ambio, 35, 169–175, https://doi.org/10.1579/0044-7447(2006)35[169:pacctr]2.0.co;2, . 
Beermann, F., Langer, M., Wetterich, S., Strauss, J., Boike, J., Fiencke, C., Schirrmeister, L., Pfeiffer, E.-M., and Kutzback, L.: Permafrost thaw and liberation of inorganic nitrogen in Eastern Siberia, Permafrost Perigl., 28, 605–618, https://doi.org/10.1002/ppp.1958, 2017. 
Berhe, A. A., Harte, J., Harden, J. W., and Torn, M. S.: The Significance of the Erosion-induced Terrestrial Carbon Sink, BioScience, Narnia, 57, 337–346, https://doi.org/10.1641/B570408, 2007. 
Botrel, M., Bristow, L. A., Altabet, M. A., Gregory-Eaves, I., and Maranger, R.: Assimilation and nitrification in pelagic waters: insights using dual nitrate stable isotopes (δ15N, δ18O) in a shallow lake, Biogeochemistry, Springer International Publishing, 135, 221–237, https://doi.org/10.1007/s10533-017-0369-y, 2017. 
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Editorial statement
Vast areas of permafrost are being degraded by climate change, which can release substantial quantities of nutrients into rivers and the ocean. This study shows how nitrogen isotopes can be used to determine how climate change affects the fluxes of nitrogen to the Arctic Ocean through permafrost melt.
Short summary
Climate change is causing extensive permafrost degradation and nutrient releases into rivers with great ecological impacts on the Arctic Ocean. We focused on nitrogen (N) release from this degradation and associated cycling using N isotopes, an understudied area. Many N species are released at degradation sites with exchanges between species. N inputs from permafrost degradation and seasonal river N trends were identified using isotopes, helping to predict climate change impacts.
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