Scholarship & Research

Permanent URI for this communityhttps://scholarworks.montana.edu/handle/1/1

Browse

Search Results

Now showing 1 - 2 of 2
  • Thumbnail Image
    Item
    Eight genome sequences of bacterial, environmental isolates from Canada Glacier, Antarctica
    (American Society for Microbiology, 2024-08) Smith, Heidi J.; Dieser, Markus; Foreman, Chrstine M.
    Sediments in cryoconite holes and meltwater streams in the McMurdo Dry Valleys, Antarctica, provide both substrates and conditions that support life in an arid polar desert. Here, we report the genomic sequences of eight environmental, bacterial isolates from Canada Glacier cryoconite holes and stream. These isolates span three major phyla.
  • Thumbnail Image
    Item
    Clothing Textiles as Carriers of Biological Ice Nucleation Active Particles
    (American Chemical Society, 2024-03) Teska, Christy J.; Dieser, Markus; Foreman, Christine M.
    Microplastics have littered the globe, with synthetic fibers being the largest source of atmospheric microplastics. Many atmospheric particles can act as ice nucleators, thereby affecting the microphysical and radiative properties of clouds and, hence, the radiative balance of the Earth. The present study focused on the ice-nucleating ability of fibers from clothing textiles (CTs), which are commonly shed from the normal wear of apparel items. Results from immersion ice nucleation experiments showed that CTs were effective ice nucleators active from −6 to −12 °C, similar to common biological ice nucleators. However, subsequent lysozyme and hydrogen peroxide digestion stripped the ice nucleation properties of CTs, indicating that ice nucleation was biological in origin. Microscopy confirmed the presence of biofilms (i.e., microbial cells attached to a surface and enclosed in an extracellular polysaccharide matrix) on CTs. If present in sufficient quantities in the atmosphere, biological particles (biofilms) attached to fibrous materials could contribute significantly to atmospheric ice nucleation.
Copyright (c) 2002-2022, LYRASIS. All rights reserved.