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CRCLEME Cooperative Research Centre
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Electronic copies of the publicatio
- Page 5 and 6: and, for Tertiary continental seque
- Page 7 and 8: 2. Analysis of a Plio-Pleistocene l
- Page 9 and 10: Table A (cont.) Basin and related s
- Page 11 and 12: Figure A: Generalised climatic curv
- Page 13 and 14: Carpenter, R.J., Hill, R.S., Greenw
- Page 15 and 16: Hill, S.M., Eggleton, R.A. and Tayl
- Page 17 and 18: Macphail, M.K. and Stone, M.S., 200
- Page 19 and 20: Swenson, U., Backlund, McLoughlin,
- Page 22 and 23: EXECUTIVE SUMMARY This review prese
- Page 24 and 25: Temperature Climates in palaeo-sout
- Page 26 and 27: SUMMARY OF INFERRED CRETACEOUS PALA
- Page 28 and 29: INTRODUCTION Mineral resources, whe
- Page 30 and 31: Professor B. Balme (Geology Departm
- Page 32: Section 7 (Tertiary climates) This
- Page 35 and 36: vegetation. Moreover, individual ta
- Page 37 and 38: 1.3 Flora, vegetation and climate 1
- Page 39 and 40: TABLE 2: Classification of vegetati
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- Page 43 and 44: Accordingly, only at sites with exc
- Page 45 and 46: 2.1.3 Palaeoecology Palaeoecology i
- Page 47 and 48: wind-pollinated trees and shrubs bu
- Page 49 and 50: 1. The usual practice of equating t
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- Page 53 and 54: 5. Facies architecture and lithostr
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- Page 65 and 66: 5.4 Time Slice K-1. Berriasian-Barr
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- Page 69 and 70: Palaeo-central Australia (~60-70 0
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- Page 81 and 82: In the Northern Hemisphere, the K/T
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Plio-Pleistocene. For example, the
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mountainous regions of Tasmania. Da
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110
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palaeolatitudes into the late Early
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Pliocene. The warm phase correlates
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TABLE 8b: INFERRED TERTIARY PALAEOC
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colleges usually hold extensive col
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2. Principal components analysis (P
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122
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Alley, N.F. and Clarke, J.D.A., 199
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Barron, E.J., 1985. Explanations of
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Bralower, T.J., Paull, C.K. and Lec
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Chappell, J., 1983. Thresholds and
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Day, M., 1999. Hell on earth: were
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Drinnan, A.N. and Chambers, T.C., 1
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Frakes, L.A. and Francis, J.E., 198
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Groves, R.H., 1999. Present vegetat
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Herngreen, G.F.W. and Chlonova, A.F
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Hill, R.S. and Scriven, L.J., 1997.
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Jarzen, D.M. and Dettmann, M.E., 19
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Kroon, D., Norris, R.D., Klaus, A.
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Macphail, M.K., 1996c. A provisiona
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Martin, H.A., 1991a. Dinoflagellate
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McMinn, A., 1989a. Early Tertiary p
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Norris, R.D. and Rohl, U., 1999. Ca
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Playford, G., Haig, D.W. and Dettma
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Rowett, A., 1993a. The use of dispe
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Specht, R.L., Dettmann, M.E. and Ja
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Twidale, C.R. and Campbell, E.M., 1
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Williams, G.E. and Douglas, J.G., 1
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166
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168
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Pteridosperms, cycads, bennettitale
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1.2.3 Central Australia 1. Eromanga
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palaeolatitude (~70 0 S). If correc
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Inferred climate The stems are beli
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Inferred climate The data confirm c
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Inferred climate The data confirm t
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3.2 Microfloras Partridge (1999) ha
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Inferred climate Dettmann et al. (1
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4.2.2 North-East Australia Deposits
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4.2.7 Tasmania 1. Bass Basin Turoni
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5.2.1 North-West Australia 1. Bonap
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192
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6.2.1 North-West Australia Late Cam
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Dacrydium and its extinct relation
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frequent only in occasional samples
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200
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202
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genera are Gymnostoma (Casuarinacea
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. The dominant angiosperm types in
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Araucariaceae (Araucaria) and Podoc
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Inferred climate The sequence recor
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212
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2.1.4 South-West Australia Inferred
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2.2.2 North-East Australia 1. South
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Taxodiaceae and Araucariaceae durin
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pollen dominance almost certainly w
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that Nothofagus (Brassospora) spp.
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224
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and Taxodiaceae (Hill et al. 1993,
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3.1.5 Central southern Australia 1.
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3.2 Microfloras Many of the macrofo
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3. Capricorn Basin Relative abundan
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abundances (1-30%) of Podocarpaceae
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due to orographic uplift of moist a
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index species of the Middle N. aspe
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(Dacrycarpus, Dacrydium), Cupanieae
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Data on Middle-Late Eocene microflo
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genera in this flora include Agathi
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(Dacrycarpus, Dacrydium with locall
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4.2.1 North-West Australia 1. North
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The diversity of Nothofagus spp. re
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Inferred climate Assuming the micro
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4.2.4 South-West Australia 1. Yilga
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Inferred climate The high relative
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pollen type during the Canthiumidit
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Araucaria (4-13%; av. 8%) and Notho
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such as Lagarostrobos, increases in
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species (Spinizonocolpites uvatus)
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Lophosoria, Dicksonia, Araucariacea
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4.3 Other Records 4.3.1 North-West
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270
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Miocene microfloras are dominated i
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The regional vegetation appears to
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5.2.6 South-East Australia Late Neo
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Inferred climate If the data merely