OFR 151.pdf - CRC LEME

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McGowran, B. and Beecroft, A., 1985. Guembelitria in the early Tertiary of southern Australia and its palaeogeographic significance. Department of Mines and Energy Special Publication 5: 247-261. McGowran, B. and Li, Q., 1997. Miocene climatic oscillation recorded in the Lakes Entrance oil shaft, southern Australia: reappraisal of the planktonic record. Micropaleontology 43: 129-148. McGowran, B., Harris, W.K. and Lindsay, J.M., 1970. The Maslin Bay flora, South Australia. Neu Jahrbuch fur Geologie und Palaontologie 8: 481-485. 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. McGowran, B. and 17 Co-authors. 2000. Australasian biogeography: the Palaeogene and Neogene record. Memoir of the Association of Australasian Palaeontologists 23: 405- 470. McKenzie, J.A., 1999. From desert to deluge in the Mediterranean. Nature 400: 613-614. McLoughlin, S., 1996. Early Cretaceous macrofloras of Western Australia. Records of the Western Australian Museum 18: 19-65. McLoughlin, S. and Hill, R.S., 1996. The succession of Western Australian Phanerozoic terrestrial floras. In: S.D. Hopper (Editor), Gondwana Heritage: Past, Present and Future of the Western Australia Biota. Surrey Beatty and Sons, Chipping Norton, pp. 61-80. McLoughlin, S. and 6 co-authors, 1995a. Oldest Cretaceous sequence, Giralia Anticline, Carnarvon Basin, Western Australia: late Hauterivian-Barremian. AGSO Journal of Australian Geology and Geophysics 15: 445-468. McLoughlin, S., Drinnan, A.N. and Rozefelds, A.C., 1995b. A Cenomanian flora from the Winton Formation, Eromanga Basin, Queensland, Australia. Memoirs of the Queensland Museum 38: 273-313. McMinn, A., 1980. Palynology of the Tertiary Duaringa Oil Shale, Queensland. New South Wales Geological Survey Palaeontological Report 1980/14 (unpublished). McMinn, A., 1981a. Late Tertiary palynology of DM Glenmore DDH 1. New South Wales Geological Survey Palaeontological Report 1981/17 (unpublished). McMinn, A., 1981b. A Miocene palynoflora from the Home Rule kaolin deposit. New South Wales Geological Survey Quarterly Notes 43: 1-4. McMinn, A., 1981c. Pliocene palynology of a sample from Wingecarribee Swamp. New South Wales Geological Survey Palaeontological Report 1981/7 (unpublished). McMinn, A., 1986a. Late Cretaceous sediments near Kempsey: Smiths Creek drilling program. New South Wales Geological Survey Palaeontological Report 86/6 (unpublished). McMinn, A., 1986b. Palynology of Claremont Avery-1, Murray Basin. New South Wales Geological Survey Palaeontological Report 1986/2 (unpublished). McMinn, A., 1987. Miocene palynology of DM Elsmore DDH 2 and 3, near Inverell. New South Wales Geological Survey Palaeontological Report 1987/2 (unpublished). McMinn, A., 1988. Tertiary palynology in the Inverell area. New South Wales Geological Survey Palaeontological Report 1988/1 (unpublished). 151
McMinn, A., 1989a. Early Tertiary palynology of sediment from Rileys Sugarloaf, near Bowral. New South Wales Geological Survey Palaeontological Report 1989/364 (unpublished). McMinn, A., 1989b. Tertiary palynology of Glen Innes DDH 107. New South Wales Geological Survey Palaeontological Report 1989/021 (unpublished). McMinn, A., 1989c. Tertiary palynology of a sample from Glen Innes DDH 110. New South Wales Geological Survey Palaeontological Report 1989/223 (unpublished). McMinn, A., 1989d. Eocene palynology of Glen Innes DDH 105. New South Wales Geological Survey Palaeontological Report 1989/363 (unpublished). McMinn, A., 1989e. Tertiary palynology in the Inverell area. New South Wales Geological Survey Quarterly Notes 76: 2-10. McMinn, A., 1989f. Middle Tertiary palynology of two samples from Ebor Falls. New South Wales Geological Survey Palaeontological Report 1989/374 (unpublished). Megirian, D., 1994. Approaches to marsupial biochronology in Australia and New Guinea. Alcheringa 18: 259-274. Melosh, H.J., 1995. Impact craters: around and around we go. Nature 376: 386-387. Meunier, J.D., Colin, F. and Alarcon, C., 1999. Biogenic silica storage in soils. Geology 27: 835-838. Miall, A., 1995. Whither stratigraphy? Sedimentary Geology 100: 5-20. Miller, K.G., Wright, J.D. and Fairbanks, R.G., 1991. Unlocking the ice house: Oligocene- Miocene oxygen isotopes, eustacy and margin erosion. Journal of Geophysical Research 96: 6829-6848. Miller, K.G., Barrera, E., Olsson, R.K., Sugarman, P.J. and Savin, S.M., 1999. Does ice drive early Maastrichtian eustacy? Geology 27: 783-786. Milne, L., 1988. Palynology of a late Eocene lignitic sequence from the western margin of the Eucla Basin, Western Australia. Memoirs of the Association of Australasian Palaeontologists 5: 285-310. Milnes, A.R. and Twidale, C.R., 1983. An overview of silicification in Cainozoic landscapes of arid central and southern Australia. Australian Journal of Soil Research 21: 387- 410. Milnes, A.R., Bournam, R.P. and Northcote, K., 1985. Field relationships of ferricretes and weathered zones in southern South Australia: a contribution to laterite studies. Australian Journal of Soil Research 23: 441-465. Molnar, P. and England, P., 1990. Late Cenozoic uplift of mountain ranges and global climate change: chicken or egg? Nature 346: 29-34. Montuire, S., Girard, D. and Girard, C., 1998. Adaptation to environmental change: communities need more time than species. Palaontologische Zeitschrift 72: 241-248. Moore, G.T., Hayashida, D.N., Ross, C.A. and Johnson, S.R., 1992. Paleoclimate of the Kimmeridgian/Tithonian (Late Jurassic) world: I. Results using a general circulation model. Palaeogeography, Palaeoclimatology, Palaeoecology 93: 113-150. Moore, W.R., Baillie, P.W., Forsyth, S.M., Hudspeth, J.W., Richardson, R.G. and Turner, N.J., 1984. Boobyalla Sub-basin: a Cretaceous onshore extension of the southern edge of the Bass Basin. APEA Journal 24: 110-117. Morat, Ph., Veillon, J.M. and McKee, H.S., 1986. Floristic relationships of New Caledonian rainforest phanerogams. Telopea 26: 631-679. 152
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CRCLEME Cooperative Research Centre
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Electronic copies of the publicatio
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and, for Tertiary continental seque
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2. Analysis of a Plio-Pleistocene l
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Table A (cont.) Basin and related s
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Figure A: Generalised climatic curv
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Carpenter, R.J., Hill, R.S., Greenw
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Hill, S.M., Eggleton, R.A. and Tayl
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Macphail, M.K. and Stone, M.S., 200
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Swenson, U., Backlund, McLoughlin,
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EXECUTIVE SUMMARY This review prese
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Temperature Climates in palaeo-sout
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SUMMARY OF INFERRED CRETACEOUS PALA
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INTRODUCTION Mineral resources, whe
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Professor B. Balme (Geology Departm
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Section 7 (Tertiary climates) This
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vegetation. Moreover, individual ta
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1.3 Flora, vegetation and climate 1
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TABLE 2: Classification of vegetati
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Figure 2: Relationship of different
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Accordingly, only at sites with exc
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2.1.3 Palaeoecology Palaeoecology i
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wind-pollinated trees and shrubs bu
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1. The usual practice of equating t
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1. Palaeontological evidence Like p
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5. Facies architecture and lithostr
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Subsequent developments include mel
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SECTION 4 (GEOGRAPHIC BOUNDARIES AN
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SECTION 5 (EARLY CRETACEOUS CLIMATE
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events on other continents and sugg
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If these considerations apply to th
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surrounding basins. Thick sands ero
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Haig and Lynch 1993, Erbacher et al
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SECTION 6 (LATE CRETACEOUS CLIMATES
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has highlighted the roles played by
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6.4.2 Palaeobotany Cenomanian flora
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Palaeo-southern Australia Dryland c
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6.7 Time Slice K-6. Late Campanian-
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7.1. Global backdrop SECTION 7 (TER
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Explanations for the PETM are centr
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East Antarctica and strengthening o
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amplifying, pacing and potentially
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southeastern Australia than elsewhe
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7.4 Time Slice T-1. Paleocene [65-5
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Palaeo-southern Australia Unlike no
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Palaeo-central Australia As for the
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7.6.2 Palaeobotany The palaeobotani
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Zone microfloras imply temporary wa
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in the Bass Basin, the basal Seaspr
Page 102 and 103: Similarly it is difficult to summar
Page 104 and 105: However, the data are emphatic that
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Page 108 and 109: fossil taxa that are morphologicall
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Page 112 and 113: SECTION 8 (CONCLUSIONS) Climatic in
Page 114 and 115: • On present indications, Early C
Page 116 and 117: TABLE 8a: INFERRED CRETACEOUS PALAE
Page 118 and 119: 8.2 Results in prospect (recommenda
Page 120 and 121: The 10 μm sieved, oxidised extract
Page 122 and 123: phenology. The method also provides
Page 124 and 125: SECTION 9 (REFERENCES) Acton, G.D.
Page 126 and 127: Ashley, P.M., Duncan, R.A. and Feeb
Page 128 and 129: Birks, H.J.B. and Gordon, A.D., 198
Page 130 and 131: Burnham, R.J., 1989. Relationships
Page 132 and 133: Clarke, J.D.A., 1994. Evolution of
Page 134 and 135: Dettmann, M.E. and Playford, G., 19
Page 136 and 137: Evans, P.R., 1970b. Palynology of H
Page 138 and 139: Godthelp, H., Archer, M., Cifelli,
Page 140 and 141: Harris, W.K., 1974. Biostratigraphy
Page 142 and 143: Hill, R.S., 1994b. Nothofagus smith
Page 144 and 145: Holland, S.M. and Patzkowsky, M.E.,
Page 146 and 147: Australia: paleoceanographic implic
Page 148 and 149: Lindsay, J.M. and Harris, W.K., 196
Page 150 and 151: Macphail, M.K., Colhoun, E.A. and F
Page 154 and 155: Morgan, R., 1977. Palynology of Ter
Page 156 and 157: Abstracts of the Annual General Mee
Page 158 and 159: Raymo, M.E., Grant, B., Horowitz, M
Page 160 and 161: Sereno, P.C., 1999. The evolution o
Page 162 and 163: Taylor, G., 1998. Prediction of mod
Page 164 and 165: Webb, L.G., 1968. Environmental rel
Page 166 and 167: Zachos, J.C., Stott, L.D. and Lohma
Page 168 and 169: APPENDIX 1 CRETACEOUS DATA 167
Page 170 and 171: 1. TIME SLICE K-1 Age Range: Berria
Page 172 and 173: Australian assemblages, located on
Page 174 and 175: 2. Officer Basin Dinoflagellates in
Page 176 and 177: 2. TIME SLICE K-2 Age Range: Aptian
Page 178 and 179: Inferred climate The combined data
Page 180 and 181: Dettmann et al. (1992) have argued
Page 182 and 183: 3. TIME SLICE K-3 Age Range: Cenoma
Page 184 and 185: 3.2.2 North-East Australia 1. Carpe
Page 186 and 187: 4. TIME SLICE K-4 Age Range: Turoni
Page 188 and 189: 1. Otway Basin Limited data (Macpha
Page 190 and 191: 5. TIME SLICE K-5 Age Range: Early
Page 192 and 193: Inferred climate The data indicate
Page 194 and 195: 6. TIME SLICE K-6 Age Range: Late C
Page 196 and 197: Contrary to global cooling trends d
Page 198 and 199: Inferred climate The relatively goo
Page 200 and 201: Inferred climate As for regions to
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APPENDIX 2 TERTIARY DATA 201
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1. TIME SLICE T-1 Age Range: Paleoc
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also include relatively frequent No
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Inferred climate Some differences b
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Microfloras preserved in the Lower
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subtropical affinities are rare, hi
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2. TIME SLICE T-2 Age Range: Early
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Inferred climate Climates appear to
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northern New South Wales. The assem
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2.2.5 Central southern Australia Ha
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a number of distinctive Proteaceae
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Inferred climate The Regatta Point
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3. TIME SLICE T-3 Age Range: Middle
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2. Lake Torrens Basin Abundant leaf
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Dominance is highly variable. For e
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types (M.K. Macphail unpubl. data).
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Dacrycarpus), Euphorbiaceae (Austro
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(possibly upper mesotherm) and drie
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Basin) on the Eyre Peninsula (Alley
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explanation is that a warm water gy
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several taxa, which first appear in
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4. TIME SLICE T-4 Age Range: Oligoc
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Inferred climate The southern limit
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The lowest and possibly the oldest
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Dominants include fresh to brackish
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Based on the relative abundance of
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(Morgan 1977, McMinn 1981a, Martin
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common (up to 5-6%) in the middle s
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Polypodiaceae, Palmae (Dicolpopolli
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Strasburgeriaceae. Proprietary info
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Rare taxa which first appear in the
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Correlative microfloras in the onsh
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impression of floristic impoverishm
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(Lophosoria) reached Tasmania befor
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2. Otway Basin Oxygen isotope strat
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5. TIME SLICE T-5 Age Range: Late M
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Casuarinaceae, Cunoniaceae, Elaeoca
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maximum temperature of the hottest
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Nothofagus-gymnosperm temperate rai
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5.2.7 Tasmania Late Neogene sedimen
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