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Significance of dark CO2 fixation in arctic soils

The result's identifiers

  • Result code in IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60076658%3A12310%2F18%3A43897454" target="_blank" >RIV/60076658:12310/18:43897454 - isvavai.cz</a>

  • Result on the web

    <a href="https://reader.elsevier.com/reader/sd/pii/S0038071717307010?token=97D5E440A8ECC43EAA67A30DD8DAEEC05CCED4807E2037319AD5E1970FDF4415779A0EB53EBDA30050A95EBDB43E578C" target="_blank" >https://reader.elsevier.com/reader/sd/pii/S0038071717307010?token=97D5E440A8ECC43EAA67A30DD8DAEEC05CCED4807E2037319AD5E1970FDF4415779A0EB53EBDA30050A95EBDB43E578C</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1016/j.soilbio.2017.12.021" target="_blank" >10.1016/j.soilbio.2017.12.021</a>

Alternative languages

  • Result language

    angličtina

  • Original language name

    Significance of dark CO2 fixation in arctic soils

  • Original language description

    The occurrence of dark fixation of CO2 by heterotrophic microorganisms in soil is generally accepted, but its importance for microbial metabolism and soil organic carbon (C) sequestration is unknown, especially under C limiting conditions. To fill this knowledge gap, we measured dark (CO2)-C-13 incorporation into soil organic matter and conducted a C-13-labelling experiment to follow the C-13 incorporation into phospholipid fatty acids as microbial biomass markers across soil profiles of four tundra ecosystems in the northern circumpolar region, where net primary productivity and thus soil C inputs are low. We further determined the abundance of various carboxylase genes and identified their microbial origin with metagenomics. The microbial capacity for heterotrophic CO2 fixation was determined by measuring the abundance of carboxylase genes and the incorporation of C-13 into soil C following the augmentation of bioavailable C sources. We demonstrate that dark CO2 fixation occurred ubiquitously in arctic tundra soils, with increasing importance in deeper soil horizons, presumably due to increasing C limitation with soil depth. Dark CO2 fixation accounted on average for 0.4, 1.0, 1.1, and 16% of net respiration in the organic, cryoturbated organic, mineral and permafrost horizons, respectively. Genes encoding anaplerotic enzymes of heterotrophic microorganisms comprised the majority of identified carboxylase genes. The genetic potential for dark CO2 fixation was spread over a broad taxonomic range. The results suggest important regulatory function of CO2 fixation in C limited conditions. The measurements were corroborated by modeling the long-term impact of dark CO2 fixation on soil organic matter. Our results suggest that increasing relative CO2 fixation rates in deeper soil horizons play an important role for soil internal C cycling and can, at least in part, explain the isotopic enrichment with soil depth.

  • 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

    Result was created during the realization of more than one project. More information in the Projects tab.

  • Continuities

    P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Others

  • Publication year

    2018

  • Confidentiality

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

Data specific for result type

  • Name of the periodical

    Soil Biology &amp; Biochemistry

  • ISSN

    0038-0717

  • e-ISSN

  • Volume of the periodical

    119

  • Issue of the periodical within the volume

    APR 2018

  • Country of publishing house

    GB - UNITED KINGDOM

  • Number of pages

    11

  • Pages from-to

    11-21

  • UT code for WoS article

    000428496700002

  • EID of the result in the Scopus database

    2-s2.0-85040237897