Data

 

96 datasets found! (Query time: 12 ms)

<< PREV | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | NEXT >>

81. Onodera, J; Takahashi, K (2012): (Table 2) The mean abundances of silicoflagellates of each group from IODP Exp302

    Size:

    170 data points

    https://doi.org/10.1594/PANGAEA.787453 - Score: 7.752
82. Stein, R (2007): Analysis of organic carbon from Hole 302-M0004C

    Size:

    740 data points

    https://doi.org/10.1594/PANGAEA.548677 - Score: 7.752
83. Vogt, C (2008): Relative mineral abundances from bulk fraction X-ray diffraction data of Hole 302-M0004A

    Size:

    13424 data points

    https://doi.org/10.1594/PANGAEA.704658 - Score: 7.752
84. Martinez, NC; Murray, RW; Dickens, GR et al. (2009): (Table 2b) Trace element analysis of sediments from IODP Exp302 sites

    Size:

    1664 data points

    https://doi.org/10.1594/PANGAEA.787156 - Score: 7.752
85. Krylov, AA; Andreeva, IA; Vogt, C et al. (2008): (Table 3) Abundance of clay minerals of Hole 302-M0002A

    Size:

    70 data points

    https://doi.org/10.1594/PANGAEA.707423 - Score: 7.752
86. Vogt, C (2008): Sum peak hight and area intensities of bulk X-ray diffraction data of Hole 302-M0004A

    Size:

    1185 data points

    https://doi.org/10.1594/PANGAEA.704651 - Score: 7.752
87. Spofforth, DJA; Pälike, H; Green, DRH (2008): Element concentration of sediments of Hole 302-M0002A

    Size:

    1278 data points

    https://doi.org/10.1594/PANGAEA.659168 - Score: 7.752
88. Backman, J; Jakobsson, M; Frank, M et al. (2008): (Table 1) Age estimates of lithostratigraphic units of Hole 302-M0004A

    Size:

    4 data points

    https://doi.org/10.1594/PANGAEA.705519 - Score: 7.752
89. Gleason, JD; Thomas, DJ; Moore, TC et al. (2012): (Table 2) Nd-Sr isotopic compositions of bulk leach fractions in Eocene sediment from IODP Exp302

    Size:

    104 data points

    https://doi.org/10.1594/PANGAEA.787110 - Score: 7.752
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: 6.581

<< PREV | 1 | 2 | 3 | 4 | 5 | 6 | 7 | 8 | 9 | 10 | NEXT >>