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  1. Twenty‐thousand‐year gap between deglaciation and peat formation on sub‐Antarctic Marion Island attributed to climate and sea level change

    Radiocarbon dating of basal peats has been a key factor in determining minimum ages for deglaciation on sub-Antarctic islands. On Marion Island, peat bogs dominate the landscape below 300 m a.s.l., […]

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  2. Enzymes and biosurfactants of industrial interest produced by culturable fungi present in sediments of Boeckella Lake, Hope Bay, north‑east Antarctic Peninsula

    This study characterized cultivable fungi present in sediments obtained from Boeckella Lake, Hope Bay, in the north-east of the Antarctic Peninsula, and evaluated their production of enzymes and biosurfactants of […]

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  3. Population genetics of the deep-sea acorn barnacle Bathylasma hirsutum (Hoek, 1883) and the first report of its affiliation with a hydrothermal vent field

    Confined by the Mid-Atlantic Ridge and the European continental shelf, the deep-sea acorn barnacle Bathylasma hirsutum (Hoek, 1883) lives in the northeast Atlantic deep sea where it has been frequently […]

    Read more of: Population genetics of the deep-sea acorn barnacle Bathylasma hirsutum (Hoek, 1883) and the first report of its affiliation with a hydrothermal vent field
  4. Ground-based Remote Sensing of Aerosol, Clouds, Dynamics, and Precipitation in Antarctica – First results from the one-year COALA campaign at Neumayer Station III in 2023

    Novel observations of aerosol and clouds by means of ground-based remote sensing have been performed in Antarctica over the Ekström ice shelf on the coast of Dronning Maud Land at […]

    Read more of: Ground-based Remote Sensing of Aerosol, Clouds, Dynamics, and Precipitation in Antarctica – First results from the one-year COALA campaign at Neumayer Station III in 2023