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Datasets with PANGAEA technical keyword @tahiti310exp

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  1. (Table 1) Microbialites from coral reefs off the volcanic islands Tahiti and Vanuatu and from the nonvolcanic sites Belize and the Maldives

    Heindel, Katrin; Birgel, Daniel; Brunner, Benjamin; Thiel, Volker; Westphal, Hildegard; Gischler, Eberhard; Ziegenbalg, Simone B; Cabioch, Guy; Sjovall, Peter; Peckmann, Jörn Ludwig

  2. (Table 1) Microbialites from coral reefs off the volcanic islands Tahiti and Vanuatu and from the nonvolcanic sites Belize and the Maldives

    Heindel, Katrin; Birgel, Daniel; Brunner, Benjamin; Thiel, Volker; Westphal, Hildegard; Gischler, Eberhard; Ziegenbalg, Simone B; Cabioch, Guy; Sjovall, Peter; Peckmann, Jörn Ludwig

  3. (Table 1) Microbialites from coral reefs off the volcanic islands Tahiti and Vanuatu and from the nonvolcanic sites Belize and the Maldives

    Heindel, Katrin; Birgel, Daniel; Brunner, Benjamin; Thiel, Volker; Westphal, Hildegard; Gischler, Eberhard; Ziegenbalg, Simone B; Cabioch, Guy; Sjovall, Peter; Peckmann, Jörn Ludwig

  4. (Table S1) Original element/Ca data for the OGA and Tahiti corals

    Hathorne, Ed C; Felis, Thomas; Suzuki, Atsushi; Kawahata, Hodaka; Cabioch, Guy
    [1] Previous studies have demonstrated the potential for the Li content of coral aragonite to record information about environmental conditions, but no detailed study of tropical corals exists. Here we present the Li and Mg to Ca ratios at a bimonthly to monthly resolution over 25 years in two modern Porites corals, the genus most often used for paleoclimate reconstructions in the tropical Indo-Pacific. A strong relationship exists between coral Li/Ca and locally measured SST, indicating that coral Li/Ca can be used to reconstruct tropical SST variations. However, Li/Ca ratios of the skeleton deposited during 1979-1980 do not track local...

  5. (Table S1) Original element/Ca data for the OGA and Tahiti corals

    Hathorne, Ed C; Felis, Thomas; Suzuki, Atsushi; Kawahata, Hodaka; Cabioch, Guy
    [1] Previous studies have demonstrated the potential for the Li content of coral aragonite to record information about environmental conditions, but no detailed study of tropical corals exists. Here we present the Li and Mg to Ca ratios at a bimonthly to monthly resolution over 25 years in two modern Porites corals, the genus most often used for paleoclimate reconstructions in the tropical Indo-Pacific. A strong relationship exists between coral Li/Ca and locally measured SST, indicating that coral Li/Ca can be used to reconstruct tropical SST variations. However, Li/Ca ratios of the skeleton deposited during 1979-1980 do not track local...

  6. Thermal conductivity, IODP Expedition 310

    Expedition 310 Scientists

  7. Thermal conductivity, IODP Expedition 310

    Expedition 310 Scientists

  8. Thermal conductivity, IODP Expedition 310

    Expedition 310 Scientists

  9. Description of lithologic section units of Hole 310-M0026A

    Expedition 310 Scientists

  10. Description of lithologic section units of Hole 310-M0026A

    Expedition 310 Scientists

  11. Description of lithologic section units of Hole 310-M0026A

    Expedition 310 Scientists

  12. Description of lithologic section units of Hole 310-M0025B

    Expedition 310 Scientists

  13. Description of lithologic section units of Hole 310-M0025B

    Expedition 310 Scientists

  14. Description of lithologic section units of Hole 310-M0025B

    Expedition 310 Scientists

  15. Description of lithologic section units of Hole 310-M0025A

    Expedition 310 Scientists

  16. Description of lithologic section units of Hole 310-M0025A

    Expedition 310 Scientists

  17. Description of lithologic section units of Hole 310-M0025A

    Expedition 310 Scientists

  18. Description of lithologic section units of Hole 310-M0024A

    Expedition 310 Scientists

  19. Description of lithologic section units of Hole 310-M0024A

    Expedition 310 Scientists

  20. Description of lithologic section units of Hole 310-M0024A

    Expedition 310 Scientists

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