970 resultados para Drake, Francis, approximately 1540-1596
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Text (in Versform) in d. Platte graviert
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Alexander Mair Aug. Vind.
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Signatur des Originals: S 36/F01527
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Signatur des Originals: S 36/F01528
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Signatur des Originals: S 36/F05320
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Signatur des Originals: S 36/F05321
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Signatur des Originals: S 36/F09538
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Signatur des Originals: S 36/F10310
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Signatur des Originals: S 36/F10584
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Signatur des Originals: S 36/F11720
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Signatur des Originals: S 36/G04311
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Hot brines in depressions of the central Red Sea contain thousands of times more iron, manganese and other metals than . After removal of salts, approximately half of sediments from these depressions consists of iron hydroxides and they are enriched in zinc, copper, lead and molybdenum. Hydrothermal deposits with the same complex of metals, located along the coast of the Red Sea, are correlated with faults and may be due to occurrences of Tertiary volcanism. Brines of similar composition are known in the Cheleken Peninsula. Certain geological and geochemical data indicate that such brines are of relatively deep origin.
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This data was collected during a cruise across Drake Passage in the Southern Ocean in February 2009. This data consists of coccolithophore abundance, calcification and primary production rates, carbonate chemistry parameters and ancillary data of macronutrients, chlorophyll-a, average mixed layer irradiance, daily irradiance above the sea surface, euphotic and mixed layer depth, temperature and salinity.