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    Production of methane and gaseous compounds by surface microbial activity in a small pockmark field, Dunmanus Bay, Ireland


    O’Reilly, S.S. and Jordan, S.F. and Monteys, X. and Simpson, A.J. and Allen, C.C.R. and Szpak, M. and Murphy, B.T. and McCarron, Stephen and Soong, R. and Wu, B. and Jenne, A. and Grey, A. and Kellegher, B.P. (2021) Production of methane and gaseous compounds by surface microbial activity in a small pockmark field, Dunmanus Bay, Ireland. Estuarine, Coastal and Shelf Science, 255. p. 107340. ISSN 0272-7714

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    Abstract

    Marine pockmarks are globally widespread seabed depressions, conventionally thought to be formed by the accumulation and expulsion of microbial and thermogenic gas. However, other putative fluids and processes have been implicated in pockmark formation and gas escape to the atmosphere may be underestimated. Given the complex spectrum of aquatic settings, morphologies and sizes, there may also exist a spectrum of physical, chemical and biological processes that form pockmarks. Pockmarks in shallow coastal waters are now understood to be widespread, but the influence of physical dynamics (e.g. tides, storms, etc.), terrestrial processes and anthropogenic activities add considerable spatiotemporal complexity and uncertainty to our understanding of these features. Here, we revisit a field of small (ca. 2 m diameter), shallow (

    Item Type: Article
    Keywords: Biogeochemical analysis; Cores; Dunmanus; Marine pockmarks; Microbial contribution;
    Academic Unit: Faculty of Social Sciences > Geography
    Item ID: 16622
    Identification Number: https://doi.org/10.1016/j.ecss.2021.107340
    Depositing User: Dr. Stephen McCarron
    Date Deposited: 18 Oct 2022 13:59
    Journal or Publication Title: Estuarine, Coastal and Shelf Science
    Publisher: Elsevier
    Refereed: No
    URI:
    Use Licence: This item is available under a Creative Commons Attribution Non Commercial Share Alike Licence (CC BY-NC-SA). Details of this licence are available here

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