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Windrose

34 datasets found! (Query time: 4 ms)

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  1. Thomas, AL; Fujita, K; Iryu, Y et al. (2012): Isotope analysis, age calculation and calcite concentration from IODP Hole 310-M0005D
    Supplement to:  Thomas, AL; Fujita, K; Iryu, Y et al. (2012): Assessing subsidence rates and paleo water-depths for Tahiti reefs using U-Th chronology of altered corals. Marine Geology
    Size:  2 datasets
    https://doi.org/10.1594/PANGAEA.787783 - Score: 18.408
  2. Asami, R; Felis, T; Deschamps, P et al. (2009): Stable oxygen isotope record and Sr/Ca ratios of corals from IODP Holes M0009D and M0023A
    Supplement to:  Asami, R; Felis, T; Deschamps, P et al. (2009): Evidence for tropical South Pacific climate change during the Younger Dryas and the Bølling-Allerød from geochemical records of fossil Tahiti corals. Earth and Planetary Science Letters
    Size:  2 datasets
    https://doi.org/10.1594/PANGAEA.736807 - Score: 18.103
  3. Seard, C; Camoin, G; Yokoyama, Y et al. (2011): Age analysis, aragonite and high magnesium calcite content from different IODP Holes from Exp 310
    Supplement to:  Seard, C; Camoin, G; Yokoyama, Y et al. (2011): Microbialite development patterns in the last deglacial reefs from Tahiti (French Polynesia; IODP Expedition #310): Implications on reef framework architecture. Marine Geology
    Size:  4 datasets
    https://doi.org/10.1594/PANGAEA.767366 - Score: 18.089
  4. Fujita, K; Omori, A; Yokoyama, Y et al. (2010): Benthic foraminifera and sea level analyses from IODP Hole 310-M0005D
    Supplement 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:  3 datasets
    https://doi.org/10.1594/PANGAEA.763766 - Score: 18.089
  5. Iryu, Y; Takahashi, Y; Fujita, K et al. (2012): Nongeniculate coralline algae from IODP Site 310-M0005D
    Related to:  Iryu, Y; Takahashi, Y; Fujita, K et al. (2010): Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310-M0005D, off Tahiti. Island Arc
    Size:  494 data points
    https://doi.org/10.1594/PANGAEA.788464 - Score: 16.769
  6. Felis, T; Merkel, U; Asami, R et al. (2012): Monthly Tahiti coral Sr/Ca and oxygen isotope data from IODP Hole 310-M0024A
    Supplement to:  Felis, T; Merkel, U; Asami, R et al. (2012): Pronounced interannual variability in tropical South Pacific temperatures during Heinrich Stadial 1. Nature Communications
    Size:  1068 data points
    https://doi.org/10.1594/PANGAEA.786743 - Score: 16.734
  7. Westphal, H; Heindel, K; Brandano, M et al. (2012): (Table 1) Different age analysis from IODP Site 310-M0018A
    Supplement to:  Westphal, H; Heindel, K; Brandano, M et al. (2010): Genesis of microbialites as contemporaneous framework components of deglacial coral reefs, Tahiti (IODP 310). Facies
    Size:  13 data points
    https://doi.org/10.1594/PANGAEA.788488 - Score: 16.734
  8. DeLong, K; Quinn, TM; Shen, CC et al. (2012): (Table A1) Uranium and Thorium determination from IODP Site 310-M0007B
    Supplement to:  DeLong, K; Quinn, TM; Shen, CC et al. (2010): A snapshot of climate variability at Tahiti at 9.5 ka using a fossil coral from IODP Expedition 310. Geochemistry, Geophysics, Geosystems
    Size:  18 data points
    https://doi.org/10.1594/PANGAEA.788536 - Score: 16.674
  9. Hathorne, EC; Felis, T; James, RH et al. (2011): Geochemical data for drilled powder samples from two fossil Porites corals from Integrated Ocean Drilling Program Expedition 310
    Supplement to:  Hathorne, EC; Felis, T; James, RH et al. (2011): Laser ablation ICP-MS screening of corals for diagenetically affected areas applied to Tahiti corals from the last deglaciation. Geochimica et Cosmochimica Acta
    Size:  1038 data points
    https://doi.org/10.1594/PANGAEA.756560 - Score: 16.674
  10. Inoue, M; Yokoyama, Y; Harada, M et al. (2010): (Table 1) Trace element and age analysis from the Porites coral from IODP Exp 310
    Supplement to:  Inoue, M; Yokoyama, Y; Harada, M et al. (2010): Trace element variations in fossil corals from Tahiti collected by IODP Expedition 310: Reconstruction of marine environments during the last deglaciation (15 to 9 ka). Marine Geology
    Size:  203 data points
    https://doi.org/10.1594/PANGAEA.763824 - Score: 16.674

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