Publications

4213 to 4224 of 13961 results

1. Increases in penguin populations at Signy Island, South Orkney Islands

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2. Upper Cretaceous inoceramids (Bivalvia) from the James Ross Island group and their stratigraphical significance

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3. The occurrence of Anopaea (Bivalvia: Inoceramidae) in the Antarctic Peninsula

   The genus Anopaea represents a small but distinctive group of inoceramid bivalves that apparently remained functionally endobyssate. The somewhat unusual morphology (for an inoceramid) probably results from structural modifications tofacilitate […]

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4. Subglacial morphology in northern Palmer Land, Antarctic Peninsula

   Ice-thickness and surface-elevation data gathered from radio echo flights over the Antarctic Peninsula are presented as profiles for five major outlet glaciers in northern Palmer Land and as contour maps […]

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5. Antarctica: the final frontier for marine biological invasions

   Antarctica is experiencing significant ecological and environmental change, which may facilitate the establishment of non‐native marine species. Non‐native marine species will interact with other anthropogenic stressors affecting Antarctic ecosystems, such […]

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6. Preliminary bivalve zonation of the Latady Formation

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7. Ordovician of Antarctica – a review

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8. Geology of the Shackleton Range. IV, The dolerite dykes

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9. Supposed Precambrian and Palaeozoic tillites of Greater Antarctica

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10. Cephalopod remains in regurgitations of the wandering albatross Diomedea exulans L. at South Georgia

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11. Cephalopod remains in regurgitations of black-browed and grey-headed albatrosses at South Georgia

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12. Consistent multidecadal variability in global temperature reconstructions and simulations over the Common Era.

    Multidecadal surface temperature changes may be forced by natural as well as anthropogenic factors, or arise unforced from the climate system. Distinguishing these factors is essential for estimating sensitivity to […]

    Read more of: Consistent multidecadal variability in global temperature reconstructions and simulations over the Common Era.