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Windrose

34 datasets found! (Query time: 5 ms)

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  1. Fujita, K; Omori, A; Yokoyama, Y et al. (2010): (Table SD1, Fig. 2) Thin section analysis from IODP Hole 310-M0005D
    Related to:  Fujita, K; Omori, A; Yokoyama, Y et al. (2010): Sea-level rise during Termination II inferred from large benthic foraminifers: IODP Expedition 310, Tahiti Sea Level. Marine Geology
    Size:  105 data points
    https://doi.org/10.1594/PANGAEA.763762 - Score: 14.789
  2. Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Table 1) Growth patterns of microbialites, water depths and applied methods from different Holes of IODP Expedition 310
    Related to:  Heindel, K; Birgel, D; Peckmann, J et al. (2010): Formation of deglacial microbialites in coral reefs off Tahiti (IODP 310) involving sulfate-reducing bacteria. Palaios
    Size:  170 data points
    https://doi.org/10.1594/PANGAEA.788364 - Score: 14.789
  3. Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Supplement 1) All detected fatty acids and their compound-specific carbon isotopic values from different Holes of IODP Expedition 310
    Related to:  Heindel, K; Birgel, D; Peckmann, J et al. (2010): Formation of deglacial microbialites in coral reefs off Tahiti (IODP 310) involving sulfate-reducing bacteria. Palaios
    Size:  496 data points
    https://doi.org/10.1594/PANGAEA.788387 - Score: 14.789
  4. Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Table 3) Analysis of non-carbonate fractions from different Holes of IODP Expedition 310
    Related to:  Heindel, K; Birgel, D; Peckmann, J et al. (2010): Formation of deglacial microbialites in coral reefs off Tahiti (IODP 310) involving sulfate-reducing bacteria. Palaios
    Size:  33 data points
    https://doi.org/10.1594/PANGAEA.788367 - Score: 14.789

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