Temporal variation of bacterial community and nutrients in Tibetan glacier snowpack
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Published:2022-04-11
Issue:4
Volume:16
Page:1265-1280
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ISSN:1994-0424
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Container-title:The Cryosphere
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language:en
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Short-container-title:The Cryosphere
Author:
Chen Yuying,Liu Keshao,Liu Yongqin,Vick-Majors Trista J.,Wang Feng,Ji Mukan
Abstract
Abstract. The Tibetan Plateau harbors the largest number of
glaciers outside the polar regions, which are the source of several major
rivers in Asia. These glaciers are also major sources of nutrients for
downstream ecosystems, while there is a little amount of data available on the nutrient
transformation processes on the glacier surface. Here, we monitored the
carbon and nitrogen concentration changes in a snowpit following a snowfall
in the Dunde Glacier of the Tibetan Plateau. The association of carbon and
nitrogen changes with bacterial community dynamics was investigated in the
surface and subsurface snow (depth at 0–15 and 15–30 cm, respectively)
during a 9 d period. Our results revealed rapid temporal changes in
nitrogen (including nitrate and ammonium) and bacterial communities in both
surface and subsurface snow. Nitrate and ammonium concentrations increased
from 0.44 to 1.15 mg L−1 and 0.18 to 0.24 mg L−1 in the surface snow and
decreased from 3.81 to 1.04 and 0.53 to 0.25 mg L−1 in the subsurface
snow over time. Therefore, we suggest that the surface snow is not
nitrogen-limited, while the subsurface snow is associated with nitrogen
consumption processes and is nitrogen-limited. The nitrate concentration
co-varied with bacterial diversity, community structure, and the predicted
nitrogen fixation and nitrogen assimilation/denitrification-related genes
(narG), suggesting nitrogen could mediate bacterial community changes. The
nitrogen limitation and enriched denitrification-related genes in subsurface
snow suggested stronger environmental and biotic filtering than those in
surface snow, which may explain the lower bacterial diversity, more
pronounced community temporal changes, and stronger biotic interactions.
Collectively, these findings advance our understanding of bacterial
community variations and bacterial interactions after snow deposition and
provide a possible biological explanation for nitrogen dynamics in snow.
Funder
National Key Research and Development Program of China Chinese Academy of Sciences National Natural Science Foundation of China
Publisher
Copernicus GmbH
Subject
Earth-Surface Processes,Water Science and Technology
Reference86 articles.
1. Amato, P., Hennebelle, R., Magand, O., Sancelme, M., Delort, A.-M.,
Barbante, C., Boutron, C., and Ferrari, C.: Bacterial characterization of
the snow cover at Spitzberg, Svalbard, FEMS Microbiol. Ecol., 59,
255–264, 2007. 2. Amoroso, A., Domine, F., Esposito, G., Morin, S., Savarino, J., Nardino, M.,
Montagnoli, M., Bonneville, J. M., Clement, J. C., Ianniello, A., and Beine,
H. J.: Microorganisms in dry polar snow are involved in the exchanges of
reactive nitrogen species with the atmosphere, Environ. Sci. Technol., 44,
714–719, https://doi.org/10.1021/es9027309, 2010. 3. Anesio, A. M. and Laybourn-Parry, J.: Glaciers and ice sheets as a biome,
Trends Ecol. Evol., 27, 219–225,
https://doi.org/10.1016/j.tree.2011.09.012, 2012. 4. Antony, R., Sanyal, A., Kapse, N., Dhakephalkar, P. K., Thamban, M., and
Nair, S.: Microbial communities associated with Antarctic snow pack and
their biogeochemical implications, Microbiol. Res., 192, 192–202,
https://doi.org/10.1016/j.micres.2016.07.004, 2016. 5. Beine, H. J., Dominè, F., Ianniello, A., Nardino, M., Allegrini, I., Teinilä, K., and Hillamo, R.: Fluxes of nitrates between snow surfaces and the atmosphere in the European high Arctic, Atmos. Chem. Phys., 3, 335–346, https://doi.org/10.5194/acp-3-335-2003, 2003.
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