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Prokaryotic Diversity and Distribution in Different Habitats of an Alpine Rock Glacier-Pond System

Research output: Contribution to journalArticle

  • I. Mania
  • R. Gorra
  • N. Colombo
  • M. Freppaz
  • M. Martin
  • A. M. Anesio
Original languageEnglish
Pages (from-to)70-84
Number of pages15
JournalMICROBIAL ECOLOGY
Volume78
Issue number1
Early online date13 Oct 2018
DOIs
DateAccepted/In press - 4 Oct 2018
DateE-pub ahead of print - 13 Oct 2018
DatePublished (current) - 1 Jul 2019

Abstract

Rock glaciers (RG) are assumed to influence the biogeochemistry of downstream ecosystems because of the high ratio of rock:water in those systems, but no studies have considered the effects of a RG inflow on the microbial ecology of sediments in a downstream pond. An alpine RG-pond system, located in the NW Italian Alps has been chosen as a model, and Bacteria and Archaea 16S rRNA genes abundance, distribution and diversity have been assessed by qPCR and Illumina sequencing, coupled with geochemical analyses on sediments collected along a distance gradient from the RG inflow. RG surface material and neighbouring soil have been included in the analysis to better elucidate relationships among different habitats. Our results showed that different habitats harboured different, well-separated microbial assemblages. Across the pond, the main variations in community composition (e.g. Thaumarchaeota and Cyanobacteria relative abundance) and porewater geochemistry (pH, DOC, TDN and NH4+) were not directly linked to RG proximity, but to differences in water depth. Some microbial markers potentially linked to the presence of meltwater inputs from the RG have been recognised, although the RG seems to have a greater influence on the pond microbial communities due to its contribution in terms of sedimentary material.

    Research areas

  • 16S rRNA, Alpine pond, Microbial ecology, Rock glacier, Sediments

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  • Full-text PDF (accepted author manuscript)

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

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  • Full-text PDF Supplementary Material

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

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  • Full-text PDF Supplementary Material 1

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

    Accepted author manuscript, 268 KB, PDF document

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  • Full-text PDF Supplementary Material 2

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

    Accepted author manuscript, 123 KB, PDF document

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  • Full-text PDF Supplementary Material 3

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

    Accepted author manuscript, 309 KB, PDF document

    Licence: Other

  • Full-text PDF Supplementary Material 4

    Rights statement: This is the accepted author manuscript (AAM). The final published version (version of record) is available online via Springer Link at https://doi.org/10.1007/s00248-018-1272-3 . Please refer to any applicable terms of use of the publisher.

    Accepted author manuscript, 162 KB, PDF document

    Licence: Other

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