Chapter 28 - Geology of the Houtman Abrolhos Islands

[1]  A. Tudhope,et al.  Sedimentary environments of the Central Region of the Great Barrier Reef of Australia , 1985, Coral Reefs.

[2]  I. Macintyre,et al.  Acropora palmata reef framework: A reliable indicator of sea level in the western atlantic for the past 10,000 years , 1982, Coral reefs.

[3]  K. Lambeck,et al.  Late Pleistocene and Holocene sea-level change along the Australian coast , 1990 .

[4]  G. Wasserburg,et al.  Holocene growth history of a reef complex on a cool-water carbonate margin: Easter Group of the Houtman Abrolhos, Eastern Indian Ocean , 1993 .

[5]  G. Wasserburg,et al.  High-precision U-series dating of Last Interglacial events by mass spectrometry: Houtman Abrolhos Islands, western Australia , 1993 .

[6]  G. Wasserburg,et al.  TIMS U-series dating and stable isotopes of the last interglacial event in Papua New Guinea , 1993 .

[7]  J. Beck,et al.  A Large Drop in Atmospheric 14C/12C and Reduced Melting in the Younger Dryas, Documented with 230Th Ages of Corals , 1993, Science.

[8]  G. Wasserburg,et al.  Late Quaternary evolution of coral reefs on a cool-water carbonate margin: the Abrolhos Carbonate Platforms, southwest Australia , 1993 .

[9]  G. Wasserburg,et al.  Holocene sea-level determination relative to the Australian continent: U/Th (TIMS) and 14C (AMS) dating of coral cores from the Abrolhos Islands , 1993 .

[10]  G. Wasserburg,et al.  Late Quaternary facies characteristics and growth history of a high latitutde reef complex: the Houtman Abrolhos carbonate platform eastern Indian Ocean , 1993 .

[11]  Tyler B. Coplen,et al.  Continuous 500,000-Year Climate Record from Vein Calcite in Devils Hole, Nevada , 1992, Science.

[12]  J. M. Landwehr,et al.  Mass-Spectrometric 230Th-234U-238U Dating of the Devils Hole Calcite Vein , 1992, Science.

[13]  T. Quinn Meteoric Diagenesis of Plio-pleistocene Limestones at Enewetak Atoll , 1991 .

[14]  R. G. Johnson Major Northern Hemisphere deglaciation caused by a moisture deficit 140 ka , 1991 .

[15]  J. Chappell,et al.  Post-glacial sea-level rise from a coral record at Huon Peninsula, Papua New Guinea , 1991, Nature.

[16]  K. Wyrwoll,et al.  Pliocene-Pleistocene coastal events and history along the western margin of Australia , 1991 .

[17]  G. Wasserburg,et al.  Precise chronology of the last interglacial period: 234U-230Th data from fossil coral reefs in the Bahamas , 1991 .

[18]  E. Bard,et al.  Calibration of the 14C timescale over the past 30,000 years using mass spectrometric U–Th ages from Barbados corals , 1990, Nature.

[19]  R. Fairbanks A 17,000-year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation , 1989, Nature.

[20]  H. Schwarcz,et al.  High-precision mass-spectrometric uranium-series dating of cave deposits and implications for palaeoclimate studies , 1989, Nature.

[21]  I. Macintyre Modern Coral Reefs of Western Atlantic: New Geological Perspective , 1988 .

[22]  L. Collins Sediments and history of the Rottnest Shelf, southwest Australia: a swell-dominated, non-tropical carbonate margin , 1988 .

[23]  J. Veron,et al.  Hermatypic corals of Western Australia , 1988 .

[24]  S. Boss,et al.  The significance of Halimeda as a space-occupier and sediment-producer, 1-750m, North Jamaica , 1988 .

[25]  H. Kirkman,et al.  Growth of the kelp Ecklonia radiata near the northern limit of its range in Western Australia , 1987 .

[26]  N. Shackleton Oxygen isotopes, ice volume and sea level , 1987 .

[27]  G. Wasserburg,et al.  238U234U230Th232Th systematics and the precise measurement of time over the past 500,000 years , 1987 .

[28]  W. Dullo Variation in Diagenetic Sequences: An Example from Pleistocene Coral Reefs, Red Sea, Saudi Arabia , 1986 .

[29]  C. Crossland,et al.  Seasonal variations in the rates of calcification and productivity in the coral Acropora formosa on a high-latitude reef , 1984 .

[30]  J. Chappell Evidence for smoothly falling sea level relative to north Queensland, Australia, during the past 6,000 yr , 1983, Nature.

[31]  David Hopley,et al.  The geomorphology of the Great Barrier Reef: Quaternary development of coral reefs , 1982 .

[32]  R. Harmon,et al.  Uranium series disequilibrium : applications to environmental problems , 1982 .

[33]  S. V. Smith The Houtman Abrolhos Islands: Carbon metabolism of coral reefs at high latitude1 , 1981 .

[34]  Peter J. Davies,et al.  A model of epicontinental reef growth , 1980, Nature.

[35]  G. Cresswell,et al.  Observations of a south-flowing current in the southeastern Indian Ocean , 1980 .

[36]  W. Adey Coral Reef Morphogenesis: A Multidimensional Model , 1978, Science.

[37]  I. Macintyre,et al.  Thickest recorded Holocene reef section, Isla Pérez core hole, Alacran Reef, Mexico , 1977 .

[38]  Creighton A. Burk,et al.  The geology of continental margins , 1974 .

[39]  E. G. Purdy Reef Configurations: Cause and Effect , 1974 .

[40]  J. Veevers Western Continental Margin of Australia , 1974 .

[41]  A. T. Buller,et al.  Modern temperate-water and warm-water shelf carbonate sediments contrasted , 1972 .

[42]  R. Matthews Carbonate diagenesis; equilibration of sedimentary mineralogy to the subaerial environment; coral cap of Barbados, West Indies , 1968 .

[43]  Hugh Edwards Islands Of Angry Ghosts , 1966 .

[44]  C. Darwin The Structure and Distribution of Coral Reefs , 1842 .