Data

 

96 datasets found! (Query time: 4 ms)

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81. Darby, DA (2009): (Table 1) Ice drift distances and times based on a reconstruction of the Arctic Ocean at 15 Ma and today (Exp302, ACEX)

    Size:

    134 data points

    https://doi.org/10.1594/PANGAEA.711528 - Score: 7.635
82. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 1) Core recovery summary and vertical core offsets (affine) for the meters composite depth and revised meters composite depth scales of Hole 302-M0003A

    Size:

    18 data points

    https://doi.org/10.1594/PANGAEA.707027 - Score: 7.635
83. O'Regan, M; Sakamoto, T; King, JW (2008): (Table 1) Core recovery summary and vertical core offsets (affine) for the meters composite depth and revised meters composite depth scales of Hole 302-M0004A

    Size:

    252 data points

    https://doi.org/10.1594/PANGAEA.707032 - Score: 7.635
84. Spofforth, DJA; Pälike, H; Green, DRH (2008): Chemical composition of Eocene sediments of Hole 302-M0004A

    Size:

    7550 data points

    https://doi.org/10.1594/PANGAEA.659167 - Score: 7.635
85. Vogt, C (2008): Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 302-M0002A

    Size:

    1985 data points

    https://doi.org/10.1594/PANGAEA.704649 - Score: 7.635
86. Vogt, C (2008): Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 302-M0003A

    Size:

    87 data points

    https://doi.org/10.1594/PANGAEA.704650 - Score: 7.635
87. März, C; Vogt, C; Schnetger, B et al. (2011): Inorganic geochemistry of IODP Hole 302-M0002A

    Size:

    5372 data points

    https://doi.org/10.1594/PANGAEA.786426 - Score: 7.635
88. Krylov, AA; Andreeva, IA; Vogt, C et al. (2008): (Table 1) Relative abundance of terrigenous minerals of Hole 302-M0002A

    Size:

    265 data points

    https://doi.org/10.1594/PANGAEA.707421 - Score: 7.635
89. O'Regan, M; Moran, K; Baxter, CDP et al. (2012): (Table 2) Average elastic properties of sedimentary subunits where consolidation samples were taken from different Holes of IODP Expedition 302

    Size:

    24 data points

    https://doi.org/10.1594/PANGAEA.788556 - Score: 7.635
90. Boucsein, B; Stein, R (2008): Macerals in sediments

    Abstract:

    The study of particulate organic matter (OM) in Arctic Ocean sediments from the Late Cretaceous to the Eocene (IODP Expedition 302) has revealed detailed information about the aquatic/marine OM fluxes, biological sources, preservation and export of terrestrial material. Here, we present detailed data from maceral analysis, vitrinite reflectance measurements and organic geochemistry. During the Campanian/Paleocene, fluxes of land-derived OM are indicated by reworked and oxidized macerals (vitrinite, inertinite) and terrigenous liptinite (cutinite, sporinite). In the Early Eocene, drastic environmental changes are indicated by peaks in aquatic OM (up to 40-45%, lamalginite, telalginite, liptodetrinite, dinoflagellate cysts) and amorphous OM (up to 50% bituminite). These events of increased aquatic OM flux, similar to conditions favoring black shale deposition, correlate with the global d13C events "Paleocene/Eocene Thermal Maximum" (PETM) and "Elmo-event". […]

    Size:

    2 datasets

    https://doi.org/10.1594/PANGAEA.690523 - Score: 6.402

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