OFR 151.pdf - CRC LEME

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Harris, W.K., 1974. Biostratigraphy of two boreholes near the northern margin of the Willunga Sub-basin. Geological Survey of South Australia Palaeontological Report 1974/31 (unpublished). Harris, W.K., 1985. Middle to Late Eocene depositional cycles and dinoflagellate zones in southern Australia. Special Publications of the South Australian Department of Mines and Energy 5: 133-144. Harris, W.K. and Foster, C.B., 1972. Stratigraphy and palynology of the Polda Basin, Eyre Peninsula. Geological Survey of South Australia Palaeontological Report 1972/7 (unpublished). Harris, W.K. and Morgan, R., 1976. Eocene microfloras from the eastern Murray Basin, New South Wales. New South Wales Geological Survey Quarterly Notes 24: 1-6. Harris, W.K. and Twidale, C.R., 1991. Revised age for Ayers Rock and the Olgas. Transactions of the Royal Society of South Australia 115: 109. Hartley, T.G., 1986. Floristic relationships of the rainforest flora of New Guinea. Telopea 26: 619-630. Harwood, D.M., McMinn, A. and Quilty, P.G., 2000. Diatom biostratigraphy and age of the Pliocene Sørsdal Formation, Vestfold Hills, East Antarctica. Antarctic Science 12: 443-462. Hathaway, B., Duane, A.M., Cantrill, D.J. and Kelley, S.P., 1999. 40 Ar/ 39 Ar geochronology and palynology of the Cerro Negro Formation, South Shetland Islands, Antarctica: a new radiometric tie for Cretaceous terrestrial biostratigraphy in the Southern Hemisphere. Australian Journal of Earth Sciences 46: 593-606. Hattersley, P.W., 1983. The distribution of C3 and C4 grasses in Australia in relation to climate. Oecologia 57: 113-128. Hattersley, P.W., 1987. Variations in photosynthetic pathway. In: T.R. Soderstrom, K.W. Hilu, C.D.S. Campbell and M.E. Barkworth (Editors), Grass Systematics and Evolution. Smithsonian Institution Press, Washington, pp. 49-64. Haywood, A.M., Valdes, P.J. and Sellwood, B.W., 2000. Global scale palaeoclimate reconstruction of the middle Pliocene climate using the UKMO GCM: initial results. Global and Planetary Change 25: 239-256. Hecht, J., 1996. Pebbles that did for the dinosaurs. New Scientist 23 March: 17. Hekel, H., 1972. Pollen and spore assemblages from Queensland Tertiary sediments. Geological Survey of Queensland Palaeontological Paper 30: 1-29. Helby, R. and Partridge, A.D., 1985. Reconnaissance palynological analysis of Jacaranda-1, Bonaparte Basin. Esso Australia Ltd. Palaeontological Report 1985/30 (unpublished). Helby, R., Morgan, R. and Partridge, A.D., 1987. A palynological zonation of the Australian Mesozoic. Memoir of the Association of Australasian Palaeontologists 4: 1-94. Heller, P.L., Anderson, D.L. and Angevine, C.L., 1996. Is the middle Cretaceous pulse of rapid sea-floor spreading real or necessary? Geology 24: 491-494. Henderson, R.A., 1998. Eustatic and palaeoenvironmental assessment of the mid-Cretaceous Bathurst Island Group of the Money Shoals Platform, northern Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 138: 115-138. Herman, A.B. and Spicer, R.A., 1997. New palaeoclimate data from the Late Cretaceous Arctic: evidence for a warm polar ocean. Palaeogeography, Palaeoclimatology, Palaeoecology 128: 227-251. 139
Herngreen, G.F.W. and Chlonova, A.F., 1981. Cretaceous microfloral provinces. Pollen et Spores 23: 441-555. Hildebrand, A.R., Pilkington, M., Connors, M., Ortiz-Aleman, C. and Chavez, R.E., 1995. Size and structure of the Chicxulub crater revealed by horizontal gravity gradients and cenotes. Nature 376: 415-417. Hill, R.S., 1978. Two new species of Bowenia Hook. ex Hook.f. from the Eocene of eastern Australia. Australian Journal of Botany 26: 837-846. Hill, R.S., 1980. Three new Eocene cycads from eastern Australia. Australian Journal of Botany 28: 105-22. Hill, R.S., 1983a. Evolution of Nothofagus cunninghamii and its relationship to N. moorei as inferred from Tasmanian macrofossils. Australian Journal of Botany 31: 453-465. Hill, R.S., 1983b. Nothofagus macrofossils from the Tertiary of Tasmania. Alcheringa 7: 169- 183. Hill, R.S., 1984. Tertiary Nothofagus macrofossils from Cethana. Alcheringa 8: 81-86. Hill, R.S., 1986. Lauraceous leaves from the Eocene of Nerriga. Alcheringa 10: 327-351. Hill, R.S., 1987. Discovery of Nothofagus fruits corresponding to an important Tertiary pollen type. Nature 327: 56-58. Hill, R.S., 1988a. Australian Tertiary angiosperm and gymnosperm leaf remains – an updated catalogue. Alcheringa. 12: 207-219. Hill, R.S., 1988b. A re-investigation of Nothofagus muelleri (Ett.) Paterson and Cinnamomum nuytsii Ett. From the Late Eocene of Vegetable Creek. Alcheringa 12: 221-231. Hill, R.S., 1988c. Tertiary leaves of the tribe Banksieae (Proteaceae) from south-eastern Australia. Botanical Journal of the Linnean Society 97: 205-227. Hill, R.S., 1988d. Tertiary Isoetes from Tasmania. Alcheringa 12: 157-162. Hill, R.S., 1989a. New species of Phyllocladus (Podocarpaceae) macrofossils from southeastern Australia. Alcheringa 13: 193-208. Hill, R.S., 1989b. Early Tertiary leaves of the Menispermaceae from Nerriga, New South Wales. Alcheringa 13: 37-44. Hill, R.S., 1990a. Evolution of modern high latitude southern hemisphere flora: evidence from the Australian macrofossil record. Proceedings 3IOP Conference, Melbourne, pp. 31-42. Hill, R.S., 1990b. Araucaria (Araucariaceae) species from Australian Tertiary sediments- a micromorphological study. Australian Systematic Botany 3: 203-220. Hill, R.S., 1990c. Tertiary Proteaceae in Australia: a reinvestigation of Banksia adunca and Dryandra uniformis. Proceedings of the Royal Society of Victoria 102: 23-28. Hill, R.S., 1991. Leaves of Eucryphia (Eucryphiaceae) from Tertiary sediments in southeastern Australia. Australian Systematic Botany 4: 481-497. Hill, R.S., 1992a. Nothofagus: evolution from a southern perspective. Trends in Ecology and Evolution 7: 190-194. Hill, R.S., 1992b. Australian vegetation during the Tertiary: macrofossil evidence. Records of the Northern Territory Museum of Arts and Sciences 9: 1-10. Hill, R.S., 1994a. The history of selected Australian taxa. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 390-419. 140
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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
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 138 and 139: Godthelp, H., Archer, M., Cifelli,
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
Page 188 and 189: 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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