OFR 151.pdf - CRC LEME

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Godthelp, H., Archer, M., Cifelli, R., Hand, S.J. and Gilkeson, C.F., 1992. Earliest known Australian Tertiary mammal fauna. Nature 356: 514-516. Gorter, J.D., 1999. Evidence for a widespread Late Eocene (?) meteor bombardment of the northern Bonaparte Basin, offshore Northern Australia, and its effect on hydrocarbon prospectivity. PESA Journal 27: 25-40. Gorter, J.D. and Bayford, S.W., 2000. Possible impact origin for the Middle Miocene (Serravallian) Puffin Structure, Ashmore Platform, northwest Australia. Australian Journal of Earth Sciences 47: 707-714. Gotsch, J., Schroeder, R., Noe, S. and Flugel, E., 1993. Carbonate platforms as recorders of high-amplitude eustatic sea-level fluctuations: the late Albian apenninica-event. Basin Research 5: 197-212. Graham, A., 1994. Neotropical Eocene coastal floras and 18 O/ 16 O-estimated warmer vs cooler equatorial waters. American Journal of Botany 81: 301-306. Greenwood, D.R., 1987. Early Tertiary Podocarpaceae: megafossils from the Eocene Anglesea locality, Victoria, Australia. Australian Journal of Botany 35: 111-133. Greenwood, D.R., 1991. Middle Eocene megafloras from central Australia: earliest evidence for Australian sclerophyllous vegetation. American Journal of Botany Supplement 78: 114-115. Greenwood, D.R., 1992. Taphonomic constraints on foliar physiognomic interpretations of Late Cretaceous and Tertiary palaeoclimates. Review of Palaeobotany and Palynology 71: 149-190. Greenwood, D.R., 1994. Palaeobotanical evidence for Tertiary climates. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 44-59. Greenwood, D.R., 1996. Eocene monsoon forests in Central Australia. Australian Systematic Botany 9: 95-112. Greenwood, D.R. and Wing, S.L., 1995. Eocene continental climates and latitudinal temperature gradients. Geology 23: 1044-1048. Greenwood, D.R., Callen, R.A. and Alley, N.F., 1990. Tertiary macrofloras and Tertiary stratigraphy of Poole Creek Palaeochannel, Lake Eyre Basin. Abstracts: Australian Geological Congress, Hobart, February 1990. Greenwood, D.R., Vadala, A.J. and Douglas, J.G., 2000. Victorian Paleogene and Neogene macrofloras: a conspectus. Proceedings of the Royal Society of Victoria 112: 65-92. Gregory, R.T., Douthitt, C.B., Duddy, I.R., Rich, P.V. and Rich. T.H., 1989. Oxygen isotopic composition of carbonate concretions from the lower Cretaceous of Victoria, Australia: implications for the evolution of meteoric waters on the Australian continent in a paleopolar environment. Earth and Planetary Science Letters 92: 27-42. Grimes, K.G., 1980. The Tertiary geology of North Queensland. In: R.A. Henderson and P.J. Stephenson (Editors), The Geology and Geophysics of Northeastern Queensland. Geological Society of Australia, Brisbane, pp. 329-347. Grimes, K.G., 1982. Stratigraphic drilling report – GSQ Sandy Cape 1-3R. Queensland Mining Journal 83: 224-233. Grocke, D.R., 1998. Carbon-isotope analyses of fossil plants as a chemostratigraphic and palaeoenvironmental tool. Lethaia 31: 1-13. Groves, R.H., 1994. Australian Vegetation. 2 nd edition. Cambridge University Press, Cambridge. 562 pp. 137
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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
Page 88 and 89: southeastern Australia than elsewhe
Page 90 and 91: 7.4 Time Slice T-1. Paleocene [65-5
Page 92 and 93: Palaeo-southern Australia Unlike no
Page 94 and 95: Palaeo-central Australia As for the
Page 96 and 97: 7.6.2 Palaeobotany The palaeobotani
Page 98 and 99: Zone microfloras imply temporary wa
Page 100 and 101: 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
Page 106 and 107: margin of plateau were cooler (~7 0
Page 108 and 109: fossil taxa that are morphologicall
Page 110 and 111: during Late Pleistocene glacial max
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 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 152 and 153: McGowran, B. and Beecroft, A., 1985
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
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1. Otway Basin Limited data (Macpha
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5. TIME SLICE K-5 Age Range: Early
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Inferred climate The data indicate
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6. TIME SLICE K-6 Age Range: Late C
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Contrary to global cooling trends d
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Inferred climate The relatively goo
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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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