OFR 151.pdf - CRC LEME

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Morgan, R., 1977. Palynology of Tertiary (Miocene) sediments from AFMECO ELF RDH 8 and 7, Frome Embayment, N.S.W. New South Wales Geological Survey Palaeontological Report 1977/061 (unpublished). Morgan, R., 1978. Paleocene microfloras from near Tamworth, N.S.W. New South Wales Geological Survey Palaeontological Report 1978/318 (unpublished). Morgan, R., 1980. Palynostratigraphy of the Australian Early and Middle Cretaceous. Memoirs of the Geological Survey of New South Wales (Palaeontology) 18: 1-153. Morgan, R., 1986a. Palynology of Duntroon-1, Duntroon Basin, South Australia. BHP Palaeontological Report (unpublished). Morgan, R., 1986b. Palynological analysis of Amoco Yolla-1, T/14P, Bass Basin. Amoco Australia Palaeontological Report (unpublished). Morgan, R. and Hooker, N., 1993a. Palynology of Troas-1, offshore Otway Basin, South Australia. Morgan Palaeo Associates (unpublished). Morgan, R. and Hooker, N., 1993b. Final palynology of BHPP Vivonne-1, Duntroon Basin, South Australia. Morgan Palaeo Associates (unpublished). Morgan, R. and Hooker, N., 1993c. Final palynology of BHPP Borda-1, Duntroon Basin, South Australia. Morgan Palaeo Associates (unpublished). Morgan, R. and Hooker, N., 1993d. Final palynology of BHPP Greenly-1, Duntroon Basin, South Australia. Morgan Palaeo Associates (unpublished). Morley, R.J., 1998. Palynological evidence for plant dispersals in the SE Asia region in relation to plate tectonics and climate. In: R. Hall and J. Holloway (Editors), Biogeography and Geological Evolution of SE Asia. Bakhuys Publishers, Leyden, pp. 177-200. Morton, J.G.G., Hill, A.J., Parker, G. and Tabassi, A., 1994. Towards a unified stratigraphy for the Otway Basin. AGSO Record 1994/14: 7-12. Moulton, K.L. and Berner, R.A., 1998. Quantification of the effects of plants on weathering: studies in Iceland. Geology 26: 895-898. Muller, R.D., Lim, V.S.L. and Isern, A.R., 2000. Late Tertiary tectonic subsidence on the northeast Australian passive margin: response to dynamic topography. Marine Geology 162: 337-352. Mutterlose, J. and Kessels, K., 2000. Early Cretaceous calcareous nannofossils from high latitudes: implications for palaeobiogeography and palaeoclimate. Palaeogeography, Palaeoclimatology, Palaeoecology 160: 347-372. Naeem, S., 1999. Power behind diversity’s throne. Nature 401: 653-654. Nelson, C.S. and James, N.P., 2000. Marine cements in mid-Tertiary cool-water shelf limestones of New Zealand and southern Australia. Sedimentology 47: 609-629. Nettleton, W.D., Olson, C.G. and Wysocki, D.A., 2000. Paleosol classification: problems and solutions. Catena 41: 61-92. Nix, H.A., 1982. Environmental determinants of biogeography and evolution in Terra Australis. In: W.A. Barker and P.J.M. Greeenslade (Editors), Evolution of the Flora and Fauna of Arid Australia. Peacock Publications, Frewville, pp. 47-66. Nix, H.A., 1991. An environmental analysis of Australian rainforests. Special Australian Heritage Publication Series 7: 1-26. Norris, R.D. and Wilson, P.A., 1998. Low-latitude sea-surface temperatures for the mid- Cretaceous and the evolution of planktic foraminifera. Geology 26: 823-826. 153
Norris, R.D. and Rohl, U., 1999. Carbon cycling and chronology of climatic warming during the Palaeocene/Eocene transition. Nature 401: 775-778. Norris, R.D., Huber, B.T. and Self-Trail, J., 1999. Synchroneity of the K-T oceanic mass extinction and meteorite impact: Blake Nose, western North Atlantic. Geology 27: 419-422. Norvick, M. and Burger, D., 1975. Palynology of the Cenomanian of Bathurst Island, Northern Territory, Australia. BMR Bulletin 151: 1-20. Nott, J.F. and Owen, J.A.K., 1992. An Oligocene palynoflora from the middle Shoalhaven catchment N.S.W. and the Tertiary evolution of flora and climate in the southeast Australian highlands. Palaeogeography, Palaeoclimatology, Palaeoecology 95: 135- 151. Nott, J. and Purvis, A.C., 1995. Geomorphic and tectonic significance of Early Cretaceous lavas on the coastal plain, southern New South Wales. Australian Journal of Earth Sciences 42: 145-149. Nott, J.F., Idnurm, M. and Young, R.W., 1991. Sedimentology, weathering, age and geomorphological significance of Tertiary sediments on the far south coast of New South Wales. Australian Journal of Earth Sciences 38: 357-373. Nowak, R.S., Nowak, C.L. and Tausch, R.J., 2000. Probability that a fossil absent from a sample is also absent from the paleolandscape. Quaternary Research 54: 144-154. O'Brien, E.M., 1998. Water-energy dynamics, climate and prediction of woody plant species richness: an interim general model. Journal of Biogeography 25: 379-398. Odgen, J., Stewart, G.H. and Allen, R.B., 1996. Ecology of New Zealand 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. 25-82. Ollier, C.D., 1991. Laterite profiles, ferricrete and landscape evolution. Zeitschrift für Geomorphologie NF 35: 165-173. Orr, M., 1996. Discussion. Geomorphic and tectonic significance of Early Cretaceous lavas on the coastal plain, southern New South Wales. Australian Journal of Earth Sciences 43: 687-688. Owen, J.A.K., 1988. Miocene palynomorph assemblages from Kiandra, New South Wales. Alcheringa 12: 269-297. Pain, C.F., Wilford, J.R. and Dohrenwend, J.C., 1998. Regolith-landform evolution of Cape York Peninsula: implications for mineral exploration. In: G. Taylor and C. Pain (Editors), New Approaches to an Old Continent. 3 rd Australian Regolith Conference, Kalgoorlie 2-9 May. Co-operative Research Centre for Landscape Evolution and Mineral Exploration, Perth/Canberra, pp. 55-66. Palyfreyman, W.D. Guide to the geology of Australia. Bureau of Mineral Resources Bulletin 181: 1-111. Palmieri, V.,1971. Tertiary subsurface biostratigraphy of the Capricorn Basin. Reports of the geological Survey of Queensland 52: 1-18. Palmieri, V., 1984. Neogene foraminifera from GSQ Sandy Cape 1-3R bore, Queensland: a biostratigraphic appraisal. Palaeogeography, Palaeoclimatology, Palaeoecology 46: 165-183. Parrish, J.T. and Spicer, R.A., 1988. Late Cretaceous terrestrial vegetation: a near-pole temperature curve. Geology 16: 22-25. Parrish, J.T., Spicer, R.A., Douglas, J.G., Rich, T.H. and Vickers-Rich, P., 1991. Continental climate near the Albian South Pole and comparison with climate near the North Pole. 154
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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
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Similarly it is difficult to summar
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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 152 and 153: McGowran, B. and Beecroft, A., 1985
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
Page 202 and 203: 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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