Publications

5617 to 5628 of 14011 results

1. Ecological niches and geographic distributions of lanternfishes

   Lanternfishes (Myctophidae) dominate fish diversity and biomass within the mesopelagic ocean between 200-1000m deep. In the face of exploitation and climate change there is a need to predict their current […]

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2. The status of birds at Signy Island, South Orkney Islands

   Read more of: The status of birds at Signy Island, South Orkney Islands

3. Sedimentology, palynology and structure of Humps Island, northern Antarctic Peninsula

   Read more of: Sedimentology, palynology and structure of Humps Island, northern Antarctic Peninsula

4. The structural glaciology of George VI Ice Shelf, Antarctic Peninsula

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5. The structure of Wordie Ice Shelf, Antarctic Peninsula

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6. Ecophysiological studies of terrestrial free-living nematodes on Signy Island

   Read more of: Ecophysiological studies of terrestrial free-living nematodes on Signy Island

7. Comparisons of sea level and bottom pressure measurements at Drake Passage

   Tide gauge and atmospheric sea level pressure measurements from each side of Drake Passage are compared with multiyear time series of bottom pressure at 500 m depth. Synthetic subsurface pressure […]

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8. Stable-isotope/air-temperature relationships in ice cores from Dolleman Island and the Palmer Land plateau, Antarctic Peninsula

   Whilst stable-isotope analysis of ice cores yields the best quantitative evidence for past climate, there remains considerable uncertainty about the detailed relationship between the isotopic composition and air temperature. Analysis […]

   Read more of: Stable-isotope/air-temperature relationships in ice cores from Dolleman Island and the Palmer Land plateau, Antarctic Peninsula

9. Localized basal freezing within George VI Ice Shelf, Antarctica

   Hobbs Pool is an area of thin ice shelf situated within George VI Ice Shelf, Antarctica. Thicker ice shelf surrounding Hobbs Pool isolates the upper 155 m of the water […]

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10. Mesozoic and cenozoic plutonic development in the Andes of central Chile (30°30′–32°30′S)

    Mesozoic and Cenozoic granitoids of this segment of the Andes occur in three N/S-trending belts: western (WB), central (CB), and eastern (EB). The WB is formed by the Mincha and […]

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11. Cambrian-Ordovician magmatism in the Thiel Mountains, Transantarctic Mountains, and implications for the Beardmore orogeny

    New field and laboratory studies result in a redefinition of the three main lithostratigraphic units of the Thiel Mountains. These are (1) the Thiel Mountains porphyry, a massive hypersthene-bearing monzonite, […]

    Read more of: Cambrian-Ordovician magmatism in the Thiel Mountains, Transantarctic Mountains, and implications for the Beardmore orogeny

12. Isotope evidence for the origin of Andean granites.

    Read more of: Isotope evidence for the origin of Andean granites.