Data

 

96 datasets found! (Query time: 2 ms)

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81. 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: 7.915
82. Spofforth, DJA; Pälike, H; Green, DRH (2008): Element concentration of sediments of Hole 302-M0004A

    Size:

    108 data points

    https://doi.org/10.1594/PANGAEA.659169 - Score: 7.915
83. 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: 7.915
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: 7.915
85. Waddell, LM; Moore, TC (2008): (Table 3) Stable isotope data from the analysis of fish bones and the calculated salinity range in IODP Exp302

    Size:

    379 data points

    https://doi.org/10.1594/PANGAEA.733925 - Score: 7.915
86. 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: 7.915
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: 7.915
88. Onodera, J; Takahashi, K (2012): (Appendix 1) Major silicoflagellate skeletons from IODP Exp302

    Size:

    5211 data points

    https://doi.org/10.1594/PANGAEA.787516 - Score: 7.915
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: 7.915
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: 6.549

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