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Stratigraphy and timing of eolianite deposition on Rottnest Island, Western Australia

Published online by Cambridge University Press:  20 January 2017

Paul J. Hearty
Paul J. Hearty*
Affiliation:
School of Earth Sciences, James Cook University, Townsville, Queensland, 4811 Australia
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Abstract

Over 100 whole-rock amino acid racemization (AAR) ratios from outcrops around Rottnest Island (32.0° S Latitude near Perth) indicate distinct pulses of eolian deposition during the late Quaternary. Whole-rock d-alloisoleucine/l-isoleucine (A/I) ratios from bioclastic carbonate deposits fall into three distinct modal classes or “aminozones.” The oldest, Aminozone E, averages 0.33 ± 0.04 (n = 21). Red palaeosol and thick calcrete generally cap the Aminozone E deposits. A younger Aminozone C averages 0.22 ± 0.03 (n = 63); comprising two submodes at 0.26 ± 0.01 (n = 14) and 0.21 ± 0.02 (n = 49). Multiple dune sets of this interval are interrupted by relatively weak, brown to tan “protosols.” A dense, dark brown rendzina palaeosol caps the Aminozone C succession. Ratios from Holocene dune and marine deposits (“Aminozone A”) center on 0.11 ± 0.02 (n = 15), comprising submodes of 0.13 ± 0.01 (9) and 0.09 ± 0.01 (6). Calibration of A/I averages from Aminozones E and A are provided by U/Th and 14C radiometric ages of 125,000 yr (marine oxygen isotope stage (MIS) 5e and 2000–6000 14C yr B.P. (MIS 1), respectively. The whole-rock A/I results support periodic deposition initiated during MIS 5e, continuing through MIS 5c, and then peaking at the end of MIS 5a, about 70,000–80,000 yr ago. Oceanographic evidence indicates the area was subjected to much colder conditions during MIS 2–4 (10,000 to 70,000 yr ago), greatly slowing the epimerization rate. Eolianite deposition resumed in the mid Holocene (∼6000 yr ago) up to the present. The A/I epimerization pathway constructed from Rottnest Island shows remarkable similarity to that of Bermuda in the North Atlantic (32° N Latitude). These findings suggest that, like Bermuda, the eolian activity on Rottnest occurred primarily during or shortly after interglacial highstands when the shoreline was near the present datum, rather than during glacial lowstands when the coastline was positioned 10–20 km to the west.

Keywords

Western AustraliaLate QuaternaryWhole-rock amino acid racemizationCarbonate eolianiteSea-level changes
Type
Research Article
Information
Quaternary Research , Volume 60 , Issue 2 , September 2003 , pp. 211 - 222
Copyright
University of Washington

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References

Bastian, L.V., (1996). Residual soil mineralogy and dune subdivision, Swan Coastal Plain, Western Australian. Australian Journal of Earth Sciences 43, 31 44.CrossRefGoogle Scholar
Bretz, J.H., (1960). Bermuda: a partially drowned late mature Pleistocene karst. Geological Society of America Bulletin 71, 1729 1754.CrossRefGoogle Scholar
Brooke, B., (2001). The distribution of carbonate eolianite. Earth Science Reviews 55, 135 164.Google Scholar
Collins, L.B., (1988). Sediments and history of the Rottnest Shelf, southwest Australia, a swell-dominated, non-tropical carbonate margin. Sedimentary Geology 60, 15 49.Google Scholar
Fairbridge, R.W., (1950). The geology and geomorphology of Point Peron, Western Australia. Royal Society of Western Australia Journal 34, 35 72.Google Scholar
Fairbridge, R.W., (1953). Australian Stratigraphy. University of Western Australia Text Books Board, Perth.Google Scholar
Fairbridge, R.W., and Teichert, C., (1953). Soil horizons and marine bands in the coastal limestones of Western Australia. Royal Society of New South Wales Journal and Proceedings 86, 68 87.CrossRefGoogle Scholar
Glassford, D.K., and Semeniuk, V., (1990). Stratification and disconformities in yellow sands of the Bassendean and Spearwood dunes, Swan Coastal Plain, south-western Australia. Journal of the Royal Society of Western Australia 72, 75 92.Google Scholar
Harmon, R.S., Mitterer, R.M., Kriausakul, N., Land, L.S., Schwarcz, H.P., Garrett, P., Larson, G.J., Vacher, H.L., and Rowe, M., (1983). U-series and amino acid racemization geochronology of Bermuda: implications for eustatic sea-level fluctuation over the past 250,000 years. Palaeogeography, Palaeoclimatology, Palaeoecology 44, 41 70.Google Scholar
Hearty, P.J., (2002). Revision of the late Pleistocene stratigraphy of Bermuda. Sedimentary Geology 153 (1–2.), 1–21.Google Scholar
Hearty, P.J., and Dai Pra, G., (1992). The age and stratigraphy of Quaternary coastal deposits along the Gulf of Taranto (south Italy). Journal of Coastal Research 8, 882 905.Google Scholar
Hearty, P.J., and Kaufman, D.S., (2000). Whole-rock aminostratigraphy and Quaternary sea-level history of the Bahamas. Quaternary Research 54, 163 173.Google Scholar
Hearty, P.J., Kaufman, D.S., Olson, S.L., and James, H.F., (2000). Stratigraphy and whole-rock amino acid geochronology of key Holocene and Last Interglacial carbonate deposits in the Hawaiian Islands. Pacific Science 54, 423 442.Google Scholar
Hearty, P.J., Vacher, H.L., and Mitterer, R.M., (1992). Aminostratigraphy and ages of Pleistocene limestones of Bermuda. Geological Society of America Bulletin 104, 471 480.2.3.CO;2>CrossRefGoogle Scholar
Hesp, P.A., Murray-Wallace, C.V., and Dortch, C.E., (1999). Aboriginal occupation on Rottnest Island, Western Australia, provisionally dated by Aspartic Acid Racemization assay of land snails to greater than 50,000 yr B.P.. Australian Archaeology 49, 7 12.CrossRefGoogle Scholar
Hewgill, F.R., Kendrick, G.W., Webb, R.J., and Wyrwoll, K.-H., (1983). Routine ESR dating of emergent Pleistocene marine units in Western Australia. Search 14, 215 217.Google Scholar
James, N.P., Collins, L.B., Bone, Y., and Hallock, P., (1999). Subtropical carbonates in a temperate realm: modern sediments on the southwest Australian shelf. Journal of Sedimentary Research 69, 1297 1321.CrossRefGoogle Scholar
Kendrick, G.W., Wyrwoll, K.-H., and Szabo, B.J., (1991). Pliocene-Pleistocene coastal events and history along the western margin of Australia. Quaternary Science Reviews 10, 419 439.CrossRefGoogle Scholar
Kinna, B., (2002). Biogenic sediment flux on Rottnest Island and the Perth region. Honours thesis, James Cook University, Townsville, Queensland, Australia.Google Scholar
Land, L.S., Mackenzie, F.T., and Gould, S.J., (1967). The Pleistocene history of Bermuda. Geological Society of America Bulletin 78, 993 1006.CrossRefGoogle Scholar
Logan, B.W., and Read, J.F., (1970). and Davies, G.R. History of carbonate sedimentation, Quaternary Epoch, Shark Bay, Western Australia. in: Carbonate Sedimentation and Environments, Shark Bay, Western Australia, American Association of Petroleum Geologists, pp. 38–84.Google Scholar
Ludwig, K.R., Muhs, D.R., Simmons, K.R., Halley, R.B., and Shinn, E.A., (1996). Sea-level records at ∼80 ka from tectonically stable platforms: Florida and Bermuda. Geology 24, 3 211 214.Google Scholar
McGowran, B., Li, Q., Cann, J., Padley, D., McKirdy, D.M., and Shafik, S., (1997). Biogeographic impact of the Leeuwin Current in southern Australia since the late middle Eocene. Palaeogeography, Palaeoclimatology, Palaeoecology 136, 19 40.CrossRefGoogle Scholar
Miller, G.H., and Brigham-Grette, J., (1989). Amino acid geochronology: resolution and precision in carbonate fossils. Quaternary International 1, 111 128.Google Scholar
Mitterer, R.M., and Kriausakul, N., (1989). Calculation of amino acid racemization ages based apparent parabolic kinetics. Quaternary Science Reviews 8, 353 357.Google Scholar
Muhs, D., Simmons, K.R., and Steinke, B., (2002). Timing and warmth of the Last Interglacial period: new U-series evidence from Hawaii and Bermuda and a new fossil compilation for North America. Quaternary Science Reviews 21, 1355 1383.Google Scholar
Murray-Wallace, C.V., and Kimber, R.W.L., (1989). Quaternary marine aminostratigraphy: Perth Basin, Western Australia. Australian Journal of Earth Science 36, 553 568.Google Scholar
Murray-Wallace, C.V., Brooke, B.P., Cann, J.H., Belperio, A.P., and Bourman, R.P., (2001). Whole-rock aminostratigraphy of the Coorong, Coastal Plain, South Australia: towards a 1 million year record of sea-level highstands. Journal of the Geological Society of London 158, 111 124.Google Scholar
Murray-Wallace, C.V., Banerjee, D., Bourman, R.P., Olley, J.M., and Brooke, B.P., (2002). Optically stimulated luminescence dating of Holocene relict foredunes, Guichen Bay, South Australia. Quaternary Science Reviews 21, 1077 1086.CrossRefGoogle Scholar
Pen, L.J., and Green, J.W., (1983). Botanical exploration and vegetational changes on Rottnest Island. Journal of the Royal Society of Western Australia 66, 20 24.Google Scholar
Playford, P.E., (1988). Guidebook to the geology of Rottnest Island. Geological Society of Western Australia, Western Australia Division and Geological Survey, Guidebook 2.Google Scholar
Playford, P.E., (1997). Geology and hydrology of Rottnest Island, Western Australia. in: Vacher, H.L., Quinn, T., (Eds.), Geology and Hydrology of Carbonate Islands. Developments in Sedimentology 54, Elsevier, London., pp. 783–810.Google Scholar
Playford, P.E., Cockbain, A.E., Low, G.H., (1976). Geology of the Perth Basin. Western Australia. Western Australia Geological Survey Bulletin, 124 Google Scholar
Price, D.M., Brooke, B.P., and Woodroffe, C.D., (2001). Thermoluminescence dating of eolianites from Lord Howe Island and south-west Western Australia. Quaternary Science Reviews 20, 841 846.Google Scholar
Rutter, N.W., and Blackwell, B., (1995). Amino acid racemization dating. Rutter, N.W., and Catto, N.R. Dating Methods for Quaternary Deposits. Geological Association of Canada, Newfoundland. 125 167.Google Scholar
Semeniuk, V., and Glassford, D.K., (1988). Significance of eolian limestone lenses in quartz sand formations: an interdigitation of coastal and continental facies, Perth Basin, southwestern Australia. Sedimentary Geology 57, 199 209.Google Scholar
Sommerville, J.L., (1921). Evidence of uplift in the neighborhood of Perth. Journal of the Royal Society of Western Australia 6, 5 20.Google Scholar
Stirling, C.H., Esat, T.M., McCulloch, M.T., and Lambeck, K., (1995). High-precision U-series dating of corals from Western Australia and implications for the timing and duration of the Last Interglacial. Earth and Planetary Science Letters 135, 115 130.Google Scholar
Szabo, B.J., (1979). Uranium-series age of coral reef growth on Rottnest Island, Western Australia. Marine Geology 29, 11 15.Google Scholar
Teichert, C., (1950). Late Quaternary changes of sea-level at Rottnest Island, Western Australia. Proceedings of the Royal Society of Victoria 59, 63 79.Google Scholar
Vacher, H.L., and Hearty, P.J., (1989). History of stage-5 sea level in Bermuda with new evidence of a rise to present sea level during substage 5a. Quaternary Science Reviews 8, 159 168.CrossRefGoogle Scholar
Veeh, H.H., (1966). 230Th/238U and 234U/238U ages of Pleistocene high sea level stand. Journal of Geophysical Research 71, 3379 3386.Google Scholar
Wehmiller, J.F., (1984). Interlaboratory comparison of amino acid enantiomeric ratios in fossil Pleistocene mollusks. Quaternary Research 22, 109 120.Google Scholar
Wells, P.E., and Wells, G.M., (1994). Large-scale reorganization of ocean currents offshore Western Australia during the Late Quaternary. Marine Micropaleontology 24, 157 186.Google Scholar