Holocene Growth History of a Reef Complex on a Cool-Water Carbonate Margin: Easter Group of the Houtman Abrolhos, Eastern Indian Ocean
Marine Geology, 115 (1993) 29-46 29 Elsevier Science Publishers B.V., Amsterdam Holocene growth history of a reef complex on a cool-water carbonate margin: Easter Group of the Houtman Abrolhos, Eastern Indian Ocean L.B. Collins a, Z.R. Zhu a, K.-H. Wyrwoll b, B.G. Hatcher c, P.E. Playford d, A. Eisenhauer e'l , J.H. Chen e, G.J. Wasserburg e and G. Bonani f aSchool of Applied Geology, Curtin University of Technology, Perth, WA 6102, Australia bUniversity of Western Australia, Nedlands, WA 6009, Australia CDepartment of Oceanography, Dalhousie University, Halifax, N.S. B3H 4Jl, Canada dGeological Survey of Western Australia, East Perth, WA 6004, Australia eDivision of Geological and Planetary Sciences, California Institute of Technology, Pasadena, CA 91125, USA f lnstitut fiir Mittelenergiephysik der ETH Ziirich, ETH-Hoenggerberg, CH-8093 Zurich, Switzerland (Received March 5, 1993; revision accepted August 18, 1993) ABSTRACT Collins, L.B., Zhu, Z.R., Wyrwoll, K.-H., Hatcher, B.G., Playford, P.E., Eisenhauer, A., Chen, J.H., Wasserburg, G.J. and Bonani, G., 1993. Holocene growth history of a reef complex on a cool-water carbonate margin: Easter Group of the Houtman Abrolhos, Eastern Indian Ocean. Mar. Geol., 115: 29-46. The Houtman Abrolhos reefs, situated on the western continental margin of Australia, occupy a transitional position between cool-water shelf carbonate sediments to the south and more tropical environments to the north. Their existence at the outer limits of the geographical range for coral reef growth is a result of the warm, poleward-flowing Leeuwin Current. Though the modern reefs differ ecologically from tropical reefs, their geological characteristics have been little known until recently.
[Show full text]