28 citations as recorded by crossref.

1. Microbioerosion in Tahitian reefs: a record of environmental change during the last deglacial sea‐level rise (IODP 310) K. Heindel et al. https://doi.org/10.1111/j.1502-3931.2008.00140.x
2. Coral reef response to Quaternary sea‐level and environmental changes: State of the science G. Camoin & J. Webster https://doi.org/10.1111/sed.12184
3. Biological control of paleomagnetic remanence acquisition in carbonate framework rocks of the Tahiti coral reef S. Lund et al. https://doi.org/10.1016/j.epsl.2010.07.010
4. FORMATION OF DEGLACIAL MICROBIALITES IN CORAL REEFS OFF TAHITI (IODP 310) INVOLVING SULFATE-REDUCING BACTERIA K. HEINDEL et al. https://doi.org/10.2110/palo.2010.p10-032r
5. Quaternary coral reef complexes as powerful markers of long-term subsidence related to deep processes at subduction zones: Insights from Les Saintes (Guadeloupe, French West Indies) F. Leclerc & N. Feuillet https://doi.org/10.1130/GES02069.1
6. Sea-level rise during Termination II inferred from large benthic foraminifers: IODP Expedition 310, Tahiti Sea Level K. Fujita et al. https://doi.org/10.1016/j.margeo.2010.01.019
7. Comparison of 14C and U-Th Ages in Corals from IODP #310 Cores Offshore Tahiti N. Durand et al. https://doi.org/10.2458/azu_js_rc.v55i2.16134
8. Paleomagnetic record of the late Pleistocene reef sequence of Tahiti (French Polynesia): A contribution to the chronology of the deposits L. Ménabréaz et al. https://doi.org/10.1016/j.epsl.2010.03.002
9. Geomicrobiology of carbonate microbialites in the Tahiti reef R. Warthmann et al. https://doi.org/10.1144/SP418.8
10. Larger CO2 source at the equatorial Pacific during the last deglaciation K. Kubota et al. https://doi.org/10.1038/srep05261
11. Genesis of microbialites as contemporaneous framework components of deglacial coral reefs, Tahiti (IODP 310) H. Westphal et al. https://doi.org/10.1007/s10347-009-0207-3
12. Sea-level rise, environmental changes and their impact on reef development during the last deglaciation at Tahiti. IODP expedition 310: ‘Tahiti sea level’ G. Camoin et al. https://doi.org/10.1016/j.margeo.2026.107823
13. Microbialite development patterns in the last deglacial reefs from Tahiti (French Polynesia; IODP Expedition #310): Implications on reef framework architecture C. Seard et al. https://doi.org/10.1016/j.margeo.2010.10.013
14. Evidence for a slow subsidence of the Tahiti Island from GPS, DORIS, and combined satellite altimetry and tide gauge sea level records A. Fadil et al. https://doi.org/10.1016/j.crte.2011.02.002
15. A reconciled solution of Meltwater Pulse 1A sources using sea-level fingerprinting Y. Lin et al. https://doi.org/10.1038/s41467-021-21990-y
16. Fossil semi-endophytic species of Lithophyllum (Corallinaceae, Rhodophyta) from Tahiti, including L. kenjikonishii sp. nov., and their taphonomic signatures W. Woelkerling et al. https://doi.org/10.2216/13-129.1
17. Variation in deglacial coralgal assemblages and their paleoenvironmental significance: IODP Expedition 310, “Tahiti Sea Level” E. Abbey et al. https://doi.org/10.1016/j.gloplacha.2010.11.005
18. Reef response to sea-level and environmental changes during the last deglaciation: Integrated Ocean Drilling Program Expedition 310, Tahiti Sea Level G. Camoin et al. https://doi.org/10.1130/G32057.1
19. Earth surface environmental changes during the last two terminations Y. Yokoyama https://doi.org/10.4116/jaqua.49.337
20. Hydrolithon braganum sp. nov. (Corallinaceae, Rhodophyta), the first known exclusively fossil semi-endophytic coralline red alga W. Woelkerling et al. https://doi.org/10.2216/11-119.1
21. SEALEX — Internal reef chronology and virtual drill logs from a spreadsheet-based reef growth model M. Koelling et al. https://doi.org/10.1016/j.gloplacha.2008.07.011
22. FossilNewhousia imbricata(Dictyotales, Phaeophyceae) from Postglacial Coral Reef Deposits in Tahiti Y. Iryu https://doi.org/10.2517/2015PR018
23. Genesis of microbialites as contemporaneous framework components of deglacial coral reefs, Tahiti (IODP 310): COMMENT G. Camoin & C. Seard https://doi.org/10.1007/s10347-011-0264-2
24. Modern and Pleistocene large‐sized benthic foraminifers from Tahiti, French Polynesia, collected during IODP Expedition 310 K. Fujita & A. Omori https://doi.org/10.1111/iar.12069
25. Microbial composition of biofilms associated with lithifying rubble ofAcropora palmatabranches Y. Beltrán et al. https://doi.org/10.1093/femsec/fiv162
26. Coral reef response to extreme sea-level change: The meltwater pulse 1A in Tahiti - IODP expedition 310: Tahiti Sea Level G. Camoin et al. https://doi.org/10.1016/j.margeo.2026.107771
27. Sealevel history recorded in the Pleistocene carbonate sequence in IODP Hole 310‐M0005D, off Tahiti Y. Iryu et al. https://doi.org/10.1111/j.1440-1738.2010.00737.x
28. Coral indicators of past sea-level change: A global repository of U-series dated benchmarks F. Hibbert et al. https://doi.org/10.1016/j.quascirev.2016.04.019