Biblioteca Digital

66 resultados para fan cultures

Pore water geochemistry of Nile Deep Sea Fan seep sediments measured during the BIONIL expedition in 2006 at station M70/2b_785

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Pore water geochemistry of Nile Deep Sea Fan seep sediments measured during the BIONIL expedition in 2006 at station M70/2a_770_PUC-51

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Pore water geochemistry of Nile Deep Sea Fan seep sediments measured during the BIONIL expedition in 2006 at station M70/2a_773_PUC-40

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(Table 4) Fractional abundance and indices for brGDGTs and crenarchaeol in surface sediments from the Congo deep sea river fan

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Pore water geochemistry of Nile Deep Sea Fan seep sediments measured during the BIONIL expedition in 2006 at station M70/2b_812_PUC-48

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Elemental sulfur concentration in various cold seep sediments of the Nile Deep Sea Fan

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(Table S1) Total organic carbon and concentration of C-35 aminoBHPs in ODP Site 175-1075 Congo Fan sediments

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(Table 2) Pb isotope composition of K-feldspars from sediments of the Bengal Fan

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(Table 1) Carbonate constituents and quartz in the sand-sized fraction in Mississippi Fan sediments, DSDP Hole 96-615

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(Table 2) Sediment constituents and quartz in the sand-sized fraction, West Florida slope and Eastern Mississippi Fan, during USGS R/V Gyre cruises G80-6A and G81-8

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(Table 2) Biomarker data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the glacial stage MIS 6a

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(Table 6) Pollen data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the glacial stage MIS 6a

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(Table 6) Pollen data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the interglacial stage MIS 5e

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(Table 3) Isotope data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the glacial stage MIS 6a

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(Table 3) Isotope data from nine sites on a north-south transect from the Congo Fan (4°S) to the Cape Basin (30°) representing the glacial stage MIS 2

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