Coral Reefs

, Volume 35, Issue 3, pp 783–794 | Cite as

Holocene reef evolution in a macrotidal setting: Buccaneer Archipelago, Kimberley Bioregion, Northwest Australia

  • Tubagus SolihuddinEmail author
  • Michael J. O’Leary
  • David Blakeway
  • Iain Parnum
  • Moataz Kordi
  • Lindsay B. Collins


This study uses information derived from cores to describe the Holocene accretion history of coral reefs in the macrotidal (up to 11 m tidal range) Buccaneer Archipelago of the southern Kimberley coast, Western Australia. The internal architecture of all cored reefs is broadly similar, constituting well-preserved detrital coral fragments, predominantly branching Acropora, in a poorly sorted sandy mud matrix. However, once the reefs reach sea level, they diverge into two types: low intertidal reefs that maintain their detrital character and develop relatively narrow, horizontal or gently sloping reef flats at approximately mean low water spring, and high intertidal reefs that develop broad coralline algal-dominated reef flats at elevations between mean low water neap and mean high water neap. The high intertidal reefs develop where strong, ebb-dominated, tidal asymmetry retains seawater over the low tide and allows continued accretion. Both reef types are ultimately constrained by sea level but differ in elevation by 3–4 m.


Reef geomorphology Holocene reef growth Sea level Rhodoliths Coralline algal reefs 



The Kimberley Reef Geomorphology Project 1.3.1 was funded by the Western Australian State Government and partners of the Western Australian Marine Science Institution. This research was assisted by the Bardi Jawi and Mayala people through their advice and consent to access their traditional lands. The Kimberley Marine Research Station at Cygnet Bay provided vessel support and access to research facilities. Thanks to Giada Bufarale for assistance with subsurface interpretations and to Alexandra Stevens for improvement of the manuscript.


  1. Brunnschweiller RO (1957) The geology of Dampier Peninsula, Western Australia. Department of National Development, Bureau of Mineral Resources, Geology and Geophysics, CanberraGoogle Scholar
  2. Buddemeier RW, Hopley D (1988) Turn-ons and turn-offs: causes and mechanisms of the initiation and termination of coral reef growth. Proc 6th Int Coral Reef Symp 1: 253–261Google Scholar
  3. Collins LB, O’Leary MJ, Stevens AM, Bufarale G, Kordi M, Solihuddin T (2015) Geomorphic patterns, internal architecture and reef growth in a macrotidal, high-turbidity setting of coral reefs from the Kimberley Bioregion. Australian Journal of Maritime and Ocean Affairs 7:12–22CrossRefGoogle Scholar
  4. Darwin CR (1842) The structure and distribution of coral reefs. Being the first part of the geology of the voyage of the ‘Beagle’. Smith, Elder and Co, LondonGoogle Scholar
  5. DEWHA (Department of the Environment, Water, Heritage and the Arts) (2008) A characterisation of the marine environment of the northwest marine region: Perth workshop report, a summary of an expert workshop convened in Perth, Western Australia, 5–6 September 2007. Commonwealth of Australia, HobartGoogle Scholar
  6. Embry AF, Klovan J (1971) A late Devonian reef tract on Northeastern Banks Island, NWT. Bulletin of Canadian Petroleum Geology 19:730–781Google Scholar
  7. Fonseca AC, Villaça R, Knoppers B (2012) Reef flat community structure of Atol das Rocas, northeast Brazil and southwest Atlantic. J Mar Biol 2012. [doi: 10.1155/2012/179128]
  8. Gherardi DFM, Bosence DWJ (2001) Composition and community structure of the coralline-algal reefs from Atol das Rocas, South Atlantic, Brazil. Coral Reefs 19:205–219CrossRefGoogle Scholar
  9. Gherardi DFM, Bosence DWJ (2005) Late Holocene reef growth and relative sea-level changes in Atol das Rocas, equatorial South Atlantic. Coral Reefs 24:264–272CrossRefGoogle Scholar
  10. Griffin TJ, Grey K (1990) Kimberley Basin. In: Memoir 3, Geology and mineral resources of Western Australia. Geological Survey of Western Australia, Perth, pp 293–304Google Scholar
  11. Hopley D, Smithers SG, Parnell KE (2007) The geomorphology of the Great Barrier Reef: development, diversity and change. Cambridge University Press, New YorkCrossRefGoogle Scholar
  12. Kennedy DM, Woodroffe CD (2002) Fringing reef growth and morphology: a review. Earth Sci Rev 57:255–277CrossRefGoogle Scholar
  13. Ladd HS, Ingerson E, Townsend RC, Russell M, Stevenson HK (1953) Drilling on Eniwetok Atoll, Marshall Islands. AAPG Bulletin 37:2257–2280Google Scholar
  14. Lambeck K, Rouby H, Purcell A, Sun Y, Sambridge M (2014) Sea level and global ice volumes from the Last Glacial Maximum to the Holocene. Proc Natl Acad Sci U S A 111:15296–15303CrossRefPubMedPubMedCentralGoogle Scholar
  15. Lough JM (1998) Coastal climate of Northwest Australia and comparisons with the Great Barrier Reef: 1960 to 1992. Coral Reefs 17:351–367CrossRefGoogle Scholar
  16. Lowe RJ, Falter JL (2015) Oceanic forcing of coral reefs. Annu Rev Mar Sci 7:43–66CrossRefGoogle Scholar
  17. Lowe RJ, Leon AS, Symonds G, Falter JL, Gruber R (2015) The intertidal hydraulics of tide-dominated reef platforms. J Geophys Res Oceans 120:4845–4868CrossRefGoogle Scholar
  18. Montaggioni LF (2005) History of Indo-Pacific coral reef systems since the last glaciation: development patterns and controlling factors. Earth Sci Rev 71:1–75CrossRefGoogle Scholar
  19. Neumann AC, Macintyre IG (1985) Reef response to sea level rise: keep-up, catch-up or give-up. Proc 5th Int Coral Reef Symp 3:105–110Google Scholar
  20. Pearce AF, Griffiths RW (1991) The mesoscale structure of the Leeuwin Current: a comparison of laboratory models and satellite imagery. J Geophys Res 96:16739–16757CrossRefGoogle Scholar
  21. Perry CT, Smithers SG, Gulliver P, Browne NK (2012) Evidence of very rapid reef accretion and reef growth under high turbidity and terrigenous sedimentation. Geology 40:719–722CrossRefGoogle Scholar
  22. Purcell S (2002) Intertidal reefs under extreme tidal flux in Buccaneer Archipelago, Western Australia. Coral Reefs 21:191–192Google Scholar
  23. Richards ZT, O’Leary MJ (2015) The coralline algal cascades of Tallon Island (Jalan) fringing reef. NW Australia. Coral Reefs 34:595CrossRefGoogle Scholar
  24. Solihuddin T, Collins LB, Blakeway D, O’Leary MJ (2015) Holocene coral reef growth and sea level in a macrotidal, high turbidity setting: Cockatoo Island, Kimberley Bioregion, northwest Australia. Mar Geol 359:50–60CrossRefGoogle Scholar
  25. Teichert C, Fairbridge RW (1948) Some coral reefs of the Sahul Shelf. Geogr Rev 28:222–249CrossRefGoogle Scholar
  26. Wilson BR (2013) The biogeography of the Australian North West Shelf: environmental change and life’s response. Elsevier, Burlington MAGoogle Scholar
  27. Wilson BR, Blake S (2011) Notes on the origin and biogeomorphology of Montgomery Reef, Kimberley, Western Australia. J R Soc West Aust 94:107–119Google Scholar
  28. Wilson BR, Blake S, Ryan D, Hacker J (2011) Reconnaissance of species-rich coral reefs in a muddy, macro-tidal, enclosed embayment, Talbot Bay, Kimberley, Western Australia. J R Soc West Aust 94:251–265Google Scholar

Copyright information

© Springer-Verlag Berlin Heidelberg 2016

Authors and Affiliations

  1. 1.Department of Applied GeologyCurtin UniversityBentleyAustralia
  2. 2.The Western Australian Marine Science InstitutionFloreatAustralia
  3. 3.Department of Environment and AgricultureCurtin UniversityBentleyAustralia
  4. 4.Fathom 5 Marine ResearchLathlainAustralia
  5. 5.Centre for Marine Science and TechnologyCurtin UniversityBentleyAustralia

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