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Coral Reefs

, 30:1101 | Cite as

Disappearance of Acropora from the Marquesas (French Polynesia) during the last deglacial period

  • G. Cabioch
  • C. C. Wallace
  • M. T. McCulloch
  • H. Zibrowius
  • P. Laboute
  • B. Richer de Forges
Note

Abstract

The major reef-building coral genus Acropora has never been recorded, living or fossil, from the Marquesas Islands in the central Pacific Ocean, which are characterized by limited modern reef formations. During the “Musorstom 9” cruise in 1997, investigations of marine platforms representing drowned reef systems revealed for the first time the presence of two Acropora species as fossils at seven Marquesas islands. The predominant species was Acropora valida, which was widespread in the archipelago and dated between 7.4 and 48.6 ka, providing evidence of an earlier Pacific distribution pattern broader than previously observed. It is proposed that disappearance of Acropora after 7.4 ka was linked to climatic events probably ENSO events controlling the distribution of corals and coral reefs in the eastern Pacific without excluding alternatively the effects of an increase in sea-level rise.

Keywords

Marquesas Acropora Fossil Climate Biogeography 

Notes

Acknowledgments

The authors wish to thank the director of IRD-Tahiti and Captain R. Proner and crew of the IRD R/V “Alis” for their help and assistance during the cruise. Paul Muir and Antoine Jorre are thanked for assistance with photography and SEM of the fossils and Paul Muir with figures. We greatly appreciate the assistance provided by Dr Graham Mortimer in the U-series age determinations undertaken at the Research School of Earth Sciences at the Australian National University. Our thanks are extended to the Topic Editor of Coral Reefs, B. Riegl, and two anonymous reviewers.

References

  1. Bard E, Hamelin B, Arnold M, Montaggioni LF, Cabioch G, Faure G, Rougerie F (1996) Deglacial sea level record from Tahiti corals and the timing of global meltwater discharge. Nature 382:241–244Google Scholar
  2. Blanchon P (2011) Meltwater pulses. In: Hopley D (ed) Encyclopedia of modern coral reefs, Structure, form and process. Series Encyclopedia of Earth Sciences, Springer , 1st edn, pp 683–690Google Scholar
  3. Brousse R, Chevalier JP, Denizot M, Salvat B (1978) Etude géomorphologique des Iles Marquises. Cahiers du Pacifique 21:9–74Google Scholar
  4. Cabioch G, Montaggioni L, Frank N, Seard C, Sallé E, Payri C, Pelletier B, Paterne M (2008) Successive reef depositional events along the Marquesas foreslopes (French Polynesia) since 26 ka. Mar Geol 254:18–34Google Scholar
  5. Chevalier JP (1978) Les coraux des Iles Marquises. Cahiers du Pacifique 21:243–283Google Scholar
  6. Clouard V (2000) Etude géodynamique et structurale du volcanisme de la Polynésie française de 84 MA à l’actuel. Thèse de l’Université de Polynésie française, p 262Google Scholar
  7. Crossland C (1927) Marine ecology and coral formations in the Panama region, Galapagos and Marquesas Islands and the atoll of Napuka. Trans R Soc Edinburgh 55:531–554Google Scholar
  8. Davis WM (1928) The coral reef problem. Am Geogr Soc, Spec Publ 9:1–596Google Scholar
  9. Fairbanks RG (1989) A 17,000-year glacio-eustatic sea level record:influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature 342:637–642Google Scholar
  10. Gagan MK, Hendy EJ, Haberle SG, Hantoro WS (2004) Post-glacial evolution of the Indo-Pacific warm pool and El Niño-Southern Oscillation. Quaternary Int 118–119:127–143Google Scholar
  11. Glynn PW, Ault JS (2000) A biogeographic analysis and review of the far eastern Pacific coral reef region. Coral Reefs 19:1–23Google Scholar
  12. Macintyre IG, Glynn PW, Toscano MA (2007) The demise of a major Acropora palmata bank-barrier reef off the southeast coast of Barbados, West Indies. Coral Reefs 26:765–773Google Scholar
  13. McCulloch M, Taviani M, Montagna P, Lopez Correa M, Remia A, Mortimer G (2010) Proliferation and demise of deep-sea corals in the Mediterranean during the Younger Dryas. Earth Planet Sci Lett 298:143–152Google Scholar
  14. Pickett JW, Thompson CH, Kelley RA, Roman D (1985) Evidence of higher sea level during isotopic stage 5C in Queensland, Australia. Quaternary Res 24:103–114Google Scholar
  15. Richer de Forges B, Poupin J, Laboute P (1999) La campagne MUSORSTOM 9 dans l’archipel des îles Marquises (Polynésie française). Compte-rendu et liste des stations. In: Crosnier A (ed) Résultats des campagnes MUSORSTOM, vol. 20. Mémoires du Muséum national d’Histoire naturelle 180:9–29Google Scholar
  16. Rougerie F, Wauthy B, Rancher J (1992) Le récif barrière ennoyé des Iles Marquises et l’effet d’île par endo-upwelling. Compte-Rendu Acad Sci Paris II 315:677–682Google Scholar
  17. Von Prahl H, Mejia A (1985) Primer informede un coral acroporido, Acropora valida (Dana, 1846) (Scleractinia; Astrocoeniina; Acroporidae) para el Pacifico Americano. Rev Biol Trop 33:39–43Google Scholar
  18. Wallace CC (1999) Staghorn corals of the world—a revision of the genus Acropora (Scleractinia; Astrocoeniina; Acroporidae) worldwide, with emphasis on morphology, phylogeny and biogeography. CSIRO Publ, Collingwood. AustraliaGoogle Scholar

Copyright information

© Springer-Verlag 2011

Authors and Affiliations

  • G. Cabioch
    • 1
  • C. C. Wallace
    • 2
  • M. T. McCulloch
    • 3
  • H. Zibrowius
    • 4
  • P. Laboute
    • 6
  • B. Richer de Forges
    • 5
  1. 1.IRD (Institut de Recherche pour le Développement), UMR LOCEAN/IPSLBondy CedexFrance
  2. 2.Museum of Tropical QueenslandTownsvilleAustralia
  3. 3.School of Earth and EnvironmentThe University of Western Australia and ARC Centre of Excellence in Coral Reef StudiesCrawleyAustralia
  4. 4.Station Marine d’Endoume, rue de la Batterie des LionsMarseilleFrance
  5. 5.IRD, UMR 7138Nouméa CedexNew Caledonia
  6. 6.Nouméa CedexNew Caledonia

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