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Data
34 datasets found! (Query time: 11 ms)
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Seard, C; Camoin, G; Yokoyama, Y et al. (2011): (Table 2) Age analysis and aragonite content from different IODP Holes from Exp 310
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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 |
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332 data points |
https://doi.org/10.1594/PANGAEA.767360 - Score: 4.991
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Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Table 4) Fatty acids and alcohols analysis and their compound-specific carbon isotopic values from different Holes of IODP Expedition 310
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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 |
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424 data points |
https://doi.org/10.1594/PANGAEA.788384 - Score: 4.991
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Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Table 2) Elemental contents expressed as ratios versus Ca from different Holes of IODP Expedition 310
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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 |
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50 data points |
https://doi.org/10.1594/PANGAEA.788365 - Score: 4.991
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Heindel, K; Birgel, D; Brunner, B et al. (2012): (Table 1) Microbialites from coral reefs off the volcanic islands Tahiti and Vanuatu and from the nonvolcanic sites Belize and the Maldives
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Heindel, K; Birgel, D; Brunner, B et al. (2012): Post-glacial microbialite formation in coral reefs of te Pacific, Atlantic, and Indian Oceans. Chemical Geology |
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131 data points |
https://doi.org/10.1594/PANGAEA.810378 - Score: 4.991
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Heindel, K; Birgel, D; Peckmann, J et al. (2012): (Supplement 2) All detected alcohols and their compound-specific carbon isotopic values from different Holes of IODP Expedition 310
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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 |
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440 data points |
https://doi.org/10.1594/PANGAEA.788380 - Score: 4.991
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Heindel, K; Wisshak, M; Westphal, H (2012): (Table 2) Water depths and the stratigraphical position from different Holes of IODP Expedition 310
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Heindel, K; Wisshak, M; Westphal, H (2009): Microbioerosion in Tahitian reefs: A record of environmental change during the last deglacial sea-level rise (IODP 310). Lethaia |
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72 data points |
https://doi.org/10.1594/PANGAEA.788219 - Score: 4.988
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Thomas, AL; Fujita, K; Iryu, Y et al. (2012): (Table 2) Age calculation and calcite concentration from IODP Hole 310-M0005D
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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 Thomas, AL; Henderson, GM; Deschamps, P et al. (2009): Penultimate deglacial sea-level timing from Uranium/Thorium dating of Tahitian corals. Science |
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176 data points |
https://doi.org/10.1594/PANGAEA.787782 - Score: 4.988
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Fujita, K; Omori, A; Yokoyama, Y et al. (2010): (Table SD1, Fig. 2) Benthic foraminiferal abundances, preservation states and thickness to diameter ratios from IODP Hole 310-M0005D
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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 |
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910 data points |
https://doi.org/10.1594/PANGAEA.763764 - Score: 4.988
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Heindel, K; Wisshak, M; Westphal, H (2012): (Table 3) Different age analysis from different Holes of IODP Expedition 310
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Heindel, K; Wisshak, M; Westphal, H (2009): Microbioerosion in Tahitian reefs: A record of environmental change during the last deglacial sea-level rise (IODP 310). Lethaia |
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68 data points |
https://doi.org/10.1594/PANGAEA.788222 - Score: 4.988
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Asami, R; Felis, T; Deschamps, P et al. (2009): Coral oxygen isotope and Sr/Ca data from IODP Hole M0009D, section 310-M0009D-7R-1
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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 |
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602 data points |
https://doi.org/10.1594/PANGAEA.736654 - Score: 4.95
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