OFR 151.pdf - CRC LEME

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Birks, H.J.B. and Gordon, A.D., 1985. Numerical method in Quaternary Pollen Analysis. Academic Press, London. 317 pp. Bishop, P. and Bamber, R.K., 1985. Silicified wood of Early Miocene Nothofagus, Acacia and Myrtaceae (aff. Eucalyptus B) from the upper Lachlan Valley, New South Wales. Alcheringa 9: 221-228. Blackburn, D.T., 1981. Tertiary megafossil flora of Maslin Bay, South Australia: numerical taxonomic study of selected leaves. Alcheringa 5: 9-28. Blackburn, D.T. and Sluiter, I.R.K., 1994. The Oligo-Miocene coal floras of southeastern Australia. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 328-367. Blevin, J., 1991. Geological cross sections of the Eyre, Denman and Ceduna Basins. BMR Record 1991/13: 1-29. Blunier, T., 2000. “Frozen” methane escapes from the sea floor. Science 288: 68-69. Bohacs, K and Suter, J., 1997. Sequence stratigraphic distribution of coaly rocks: fundamental controls and paralic examples. American Association of Petroleum Geologists Bulletin 81: 1612-1639. Boharty, S.M. and Harwood, D.M., 1998. Southern Ocean Pliocene paleotemperature variation from high-resolution silicoflagellate biostratigraphy. Marine Micropaleontology 33: 241-272. Boland, D.J. and 7 co-authors, 1994. Forest Trees of Australia. CSIRO Publications, Melbourne. 687 pp. Bolger, P.F., 1991. Lithofacies variation as a consequence of Late Cenozoic tectonic and palaeoclimatic events in the onshore Gippsland Basin. Geological Society of Australia Special Publication 18: 158-180. Bond, B.J., Farnsworth, B.T., Coulombe, R.A. and Winner, W.E., 1999. Foliar physiology and biochemistry in response to light gradients in conifers with varying shade tolerance. Oecologia 120: 183-192. Bottomley, R., Grieve, R., York, D. and Masaitis, V., 1997. The age of the Popigai impact event and its relation to events at the Eocene/Oligocene boundary. Nature 388: 365- 368. Bourman, R.P., 1993. Perennial problems in the study of laterite. Australian Journal of Earth Sciences 40: 387-401. Bowler, J.M., 1976. Aridity in Australia: age, origins and expression in aeolian landforms and sediments. Earth Science Reviews 12: 279-310. Bowler, J.M., 1982. Aridity in the late Tertiary and Quaternary of Australia. In: W.R. Barker and P.J.M. Greenslade (Editors), Evolution of the Flora and Fauna of Arid Australia. Australian Systematic Botany Society/Peacock Publications, Frewville, pp. 35-45. Bradshaw, M.T., Yeates, A.N., Beynon, R.M., Brakel, A.T., Langford, R.P., Totterdell, J.M. and Yeung, M., 1988. Palaeogeographic evolution of the North West Shelf region. In: P.G. Purcell and R.R. Purcell (Editors), The North West Shelf Australia. Petroleum Exploration Society of Australia, Perth, pp. 29-54. Bralower, T.J. Arthur, M.A., Leckie, R.M., Sliter, W.V., Allard, D.J. and Schlanger, S.O., 1994. Timing and paleoceanography of oceanic dysoxia/anoxia in the Late Barremian to Early Aptian (Early Cretaceous). Palaios 9: 335-369. Bralower, T.J. and 7 co-authors 1997. High resolution studies of the late Paleocene thermal maximum and circum-Caribbean volcanism: is there a causal link? Geology 25: 963- 966. 127
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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
Page 78 and 79: 6.7 Time Slice K-6. Late Campanian-
Page 80 and 81: 7.1. Global backdrop SECTION 7 (TER
Page 82 and 83: Explanations for the PETM are centr
Page 84 and 85: East Antarctica and strengthening o
Page 86 and 87: 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 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 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
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Inferred climate The combined data
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Dettmann et al. (1992) have argued
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3. TIME SLICE K-3 Age Range: Cenoma
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3.2.2 North-East Australia 1. Carpe
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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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