Titlebook: Geological History of the Polar Oceans: Arctic versus Antarctic; Ulrich Bleil,J?rn Thiede Book 1990 Kluwer Academic Publishers 1990 Arctic

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https://doi.org/10.1007/978-3-663-07028-3areas served as source areas. During the Neogene and Pleistocene the average erosion in the southwestern Barents Sea amounted to about 600 m. Erosion was larger in the southeast than in the west and north. Furthermore, there is deeper erosion where the former glacial ice streams flowed.

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A Comparison of Arctic and Antarctic Sea Ice and the Effects of Different Properties on Sea Ice Biotpattern of species living in the sea ice system both in the Arctic and Antarctic. Key species from the sea ice community may be used as tools in reconstructing the extent of sea ice cover in the past.

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Die Grundprobleme der Erkenntnistheorie,tive. However, the substantial swath of crust of unknown origin between anomaly 24 and the suggested boundary could indicate an earlier onset of sea floor spreading than in the Norwegian — Greenland Sea.

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https://doi.org/10.1007/978-3-642-91358-7 only limited sources for sediment incorporation, and most of the ice-cover melts each year. These variations in Arctic and Antarctic ice characteristics are illustrated by analyses of ice crystal texture, c-axis orientations, salinity, ..O on ice cores and discussion of potential sediment input.

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,Die sinusf?rmige Wechselspannung,maller, but still rather large compared to today. Land based isotope stage 5 (4?) ice-sheets in the Arctic were possibly larger than isotope stage 2 ice-sheets. The deglaciation at the end of isotope stage 2 and the beginning of isotope stage 1 seems to have been nearly simultaneous in the Arctic and in Antarctica.