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Seasonal Snowpack Microbial Ecology and Biogeochemistry on a High Arctic Ice Cap Reveals Negligible Autotrophic Activity During Spring and Summer Melt

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F23%3A43907463" target="_blank" >RIV/60076658:12310/23:43907463 - isvavai.cz</a>

  • Result on the web

    <a href="https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022JG007176" target="_blank" >https://agupubs.onlinelibrary.wiley.com/doi/epdf/10.1029/2022JG007176</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1029/2022JG007176" target="_blank" >10.1029/2022JG007176</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Seasonal Snowpack Microbial Ecology and Biogeochemistry on a High Arctic Ice Cap Reveals Negligible Autotrophic Activity During Spring and Summer Melt

  • Original language description

    Snowpack ecosystem studies are primarily derived from research on snow-on-soil ecosystems. Greater research attention needs to be directed to the study of glacial snow covers as most snow cover lies on glaciers and ice sheets. With rising temperatures, snowpacks are getting wetter, which can potentially give rise to biologically productive snowpacks. The present study set out to determine the linkage between the thermal evolution of a snowpack and the seasonal microbial ecology of snow. We present the first comprehensive study of the seasonal microbial activity and biogeochemistry within a melting glacial snowpack on a High Arctic ice cap, Foxfonna, in Svalbard. Nutrients from winter atmospheric bulk deposition were supplemented by dust fertilization and weathering processes. NH4+ and PO43- resources in the snow therefore reached their highest values during late June and early July, at 22 and 13.9 mg m-2, respectively. However, primary production did not respond to this nutrient resource due to an absence of autotrophs in the snowpack. The average autotrophic abundance on the ice cap throughout the melt season was 0.5 &amp; PLUSMN; 2.7 cells mL-1. Instead, the microbial cell abundance was dominated by bacterial cells that increased from an average of (39 &amp; PLUSMN; 19 cells mL-1) in June to (363 &amp; PLUSMN; 595 cells mL-1) in early July. Thus, the total seasonal biological production on Foxfonna was estimated at 153 mg C m-2, and the glacial snowpack microbial ecosystem was identified as net-heterotrophic. This work presents a seasonal &quot;album&quot; documenting the bacterial ecology of glacial snowpacks. Most research attention has been given to snow covers lying on top of soil ecosystems, and therefore we do not know enough about the ecology of glacial snowpack ecosystems. This is a major knowledge gap, given that most of the world&apos;s snow cover lies over glaciers, ice caps and ice sheets. This study shows that during the melt season on a High Arctic ice cap, Foxfonna in Svalbard, nutrients are most available during the peak of summer (June-early July transition period), but a shortage of photosynthesizing microbes can mean that they largely remain in situ until transported downstream by meltwater runoff. Processes with the capacity to generate high concentrations of essential nutrients such as N and P in snow and meltwater could therefore be described, because the primary producers did not sequester them. In contrast, an increase in bacterial cell numbers was observed during the same period. The glacial snowpack ecosystem was therefore net-heterotrophic due to the absence of autotrophs and proliferation of bacterial cells. Since the nutrient demand of the bacterial biomass is low, the ecosystem releases carbon, nitrogen, and phosphorus, rather than fixes it. Nutrients delivered by snow from marine and continental sources were supplemented by the dissolution of dust deposited from local sourcesAutotrophic communities were conspicuous by their absence within a High Arctic glacial snowpack during summerSecondary bacterial production therefore dominated the entire summer, with a superimposed ice layer of refrozen snowmelt providing temporary storage for low concentrations of nutrients and cells

  • Czech name

  • Czech description

Classification

  • Type

    J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database

  • CEP classification

  • OECD FORD branch

    10618 - Ecology

Result continuities

  • Project

  • Continuities

    I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2023

  • Confidentiality

    S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Data specific for result type

  • Name of the periodical

    Journal of Geophysical Research-Biogeosciences

  • ISSN

    2169-8953

  • e-ISSN

    2169-8961

  • Volume of the periodical

    128

  • Issue of the periodical within the volume

    10

  • Country of publishing house

    US - UNITED STATES

  • Number of pages

    15

  • Pages from-to

  • UT code for WoS article

    001073289700001

  • EID of the result in the Scopus database

    2-s2.0-85173761495