OFR 151.pdf - CRC LEME

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Raymo, M.E., Grant, B., Horowitz, M. and Rau, G.H., 1996. Mid-Pliocene warmth: stronger greenhouse and stronger conveyer. Marine Micropaleontology 27: 313-326. Read, J., 1990. Some effects of acclimatisation temperature on net photosynthesis in some tropical and extra-tropical Australasian Nothofagus species. Journal of Ecology 78: 100-112. Read, J. and Brown, M.J., 1996. Ecology of Australian Nothofagus Forests. In: T.T. Veblen, R.S. Hill and J. Read (Editors), The Ecology and Biogeography of Nothofagus Forests. Yale University Press, New Haven, pp. 131-181. Read, J. and Francis, J., 1992. Responses of some Southern Hemisphere Trends in Ecology and Evolution species to a prolonged dark period and their implications for highlatitude Cretaceous and Tertiary floras. Palaeogeography, Palaeoclimatology, Palaeoecology 99: 271-290. Read, J. and Hill, R.S., 1985. Photosynthetic responses to light of Australian and Chilean Nothofagus species and some co-occurring canopy species, and their importance in understanding rainforest dynamics. New Phytologist 101: 731-742. Read, J. and Hope, G.S., 1989. Foliar frost resistance of some evergreen tropical and extratropical Australasian Nothofagus species. Australian Journal of Botany 37: 361-373. Read, J. and Hope, G.S., 1996. Ecology of Nothofagus forests of New Guinea and New Caledonia. In: T.T. Veblen, R.S. Hill and J. Read (Editors), The Ecology and Biogeography of Nothofagus Forests. Yale University Press, New Haven, pp. 200- 256. Rees, P. McA., Gibbs, M.T., Ziegler, A.M., Kutzbach, J.E. and Behling, P.J., 1999. Permian climates: evaluating model predictions using global paleobotanical data. Geology 27: 891-894. Rexilius, J.P., 1985. Sequence boundaries and condensed sequences across the Latrobe Group-Seaspray Group boundary. Esso Australia Ltd. Palaeontological Report 1985/6 (unpublished). Rexilius, J., 1989. Micropalaeontological analysis Alpha North-1, Carnarvon Basin. International Stratigraphic Consultants P/L, Cottesloe (unpublished). Reuter, G., 2000. A logical system of paleopedological terms. Catena 41: 93-109. Rhea, D.K., Zachos, J.C., Owen. R.M. and Gingerich, P.D., 1990. Global change at the Paleocene-Eocene boundary: climatic and evolutionary consequences of tectonic events. Palaeogeography, Palaeoclimatology, Palaeoecology 79: 117-128. Rich, P.V. and 6 co-authors, 1988. Evidence for low temperatures and biologic diversity in Cretaceous high latitudes of Australia. Science 242: 1403-1406. Ridgway, K.D., Sweet, A.R. and Cameron, A.R., 1995. Climatically induced floristic changes across the Eocene-Oligocene transition in northern high latitudes, Yukon Territory, Canada. Geological Society of America Bulletin 107: 676-696. Rinaldo, A., Dietrich, W.E., Rigon, R., Vogel, G.K. and Rodriguez-Iturbe, I., 1995. Geomorphic signatures of varying climate. Nature 374: 632-635. Robert. C. and Chamley, H., 1990. Palaeoenvironmental significance of clay mineral associations at the Cretaceous-Tertiary passage. Palaeogeography, Palaeoclimatology, Palaeoecology 79: 205-219. Rohl, U., Brawlower, T.J., Norris, R.D. and Wefer, G., 2000. New chronology for the late Paleocene thermal maximum and its environmental implications. Geology 28: 927- 930. 157
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CRCLEME Cooperative Research Centre
Page 3 and 4:
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
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Similarly it is difficult to summar
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However, the data are emphatic that
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margin of plateau were cooler (~7 0
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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 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 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
Page 202 and 203: APPENDIX 2 TERTIARY DATA 201
Page 204 and 205: 1. TIME SLICE T-1 Age Range: Paleoc
Page 206 and 207: 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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