OFR 151.pdf - CRC LEME

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Partridge, A.D., Trigg, K.R., Montgomerie, N.R. and Blevin, J.E., 2003. Open file micropalaeontology and palynology data from offshore Tasmania. Geoscience Australia Record 2003/07 [CD version]. Petrozzo, M.R., 2002. Palaeoceanographic and palaeoclimatic inferences from Late Cretaceous planktonic foraminiferal assemblages from the Exmouth Plateau (ODP Sites 762 and 763, eastern Indian Ocean). Marine Micropalaeontology 45: 117-150. Pickett, J.W., 2003. Stratigraphic relationship of laterite at Little Bay near Marouba, New South Wales. Australian Journal of Earth Sciences 50: 63-68. Pidgeon, R.T., Brander, T. and Lippolt, H.J., 2004. Late Miocene (U+Th)- 4 He ages of ferruginous nodules from lateritic duricrust, Darling Range, Western Australia. Australian Journal of Earth Sciences 51: 901-909. Piper, K.J., Fitzgerald, F.M.G. and Rich, T.G., 2006. Mesozoic to Early Quaternary mammal faunas of Victoria, south-east Australia. Palaeontology 49: 1237-1262. Poole, I., 2002. Systematics of Cretaceous and Tertiary Nothofagoxylon: implications for Southern Hemisphere biogeography and evolution of the Nothofagaceae. Australian Systematic Botany 15: 247-276. Quilty, P.G., 2001. Late Eocene foraminifers and palaeoenvironment, Cascade Seamount, southwest Pacific Ocean: implications for seamount subsidence and Australia-Antarctic Eocene correlation. Australian Journal of Earth Sciences 48: 633-641. Read, J., Hope, G.S. and Hill, R.S., 2005. Phytogeography and climatic analysis of Nothofagus subgenus Brassospora in New Guinea and New Caledonia. Australian Journal of Botany 53: 297-312. Roshier, D.A., Whetton, P.H., Allan, R.J. and Robertson, A.I., 2001. Distribution and persistence of temporary wetland habitats in arid Australia in relation to climate. Austral Ecology 26: 371-384. Royer, D.L., Osborne, C.P. and Beerling, D.J., 2002. High CO2 increases the freezing sensitivity of plants: implications for paleoclimatic reconstructions from fossil floras. Geology 30: 963-966. Sajjadi, F. and Playford, G., 2002a. Systematic and stratigraphic palynology of Late Jurassicearliest Cretaceous strata of the Eromanga basin, Queensland, Australia. Part one. Palaeontographica Abt. B 261: 1-97. Sajjadi, F. and Playford, G., 2002b. Systematic and stratigraphic palynology of Late Jurassicearliest Cretaceous strata of the Eromanga Basin, Queensland, Australia. Part two. Palaeontographica Abt. B 261: 99-165. Sandiford, M., 2003. Geomorphic constraints on the Late Neogene tectonics of the Otway Range, Victoria. Australian Journal of Earth Sciences 50: 69-80. Schimel, D. and Baker, D., 2002. The wildfire factor. Nature 420: 29-30. Shakesby, R.A. and Doerr, S.H., 2006. Wildfire as a hydrological and geomorphological agent. Earth Science Reviews 74: 269-307. Sharp, K.R., 2004. Cenozoic volcanism, tectonism and stream derangement in the Snowy Mountains and northern Monaro, New South Wales. Australian Journal of Earth Sciences 51: 67-83. Sinclair, N. and Monteil, E., 2004. New palynology of the Casterton Formation, Sawpit-1, Otway Basin., Australia. Geoscience Australia Record 2004/03: 1-10. Sniderman, K., Pillans, B and O’Sullivan, P.B., 2003. Palynological evidence for Plio- Pleistocene vegetation and climate cyclicity in upland Victoria, Australia. Quaternary Australasia July 2003: 30-32. Sniderman, J.M.K., Pillans, B., O’Sullivan, P.B. and Kershaw, A.P., 2007. Climate and vegetation in southeastern Australia respond to Southern Hemisphere insolation forcing in the late Pliocene-early Pleistocene. Geology 35: 41-44. Sutherland, F.L., Graham, I.T., Forsyth, S.M., Zwingmann, H. and Everard, J.L., 2006. The Tamar Trough revisited: correlations between sedimentary beds, basalts, their ages and valley evolution, north Tasmania. Papers and Proceedings of the Royal Society of Tasmania 140: 49-72. 17
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Page 1 and 2: CRCLEME Cooperative Research Centre
Page 3 and 4: 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: Macphail, M.K. and Stone, M.S., 200
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
Page 41 and 42: Figure 2: Relationship of different
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
Page 51 and 52: 1. Palaeontological evidence Like p
Page 53 and 54: 5. Facies architecture and lithostr
Page 55 and 56: Subsequent developments include mel
Page 58 and 59: SECTION 4 (GEOGRAPHIC BOUNDARIES AN
Page 60 and 61: SECTION 5 (EARLY CRETACEOUS CLIMATE
Page 62 and 63: events on other continents and sugg
Page 64 and 65: If these considerations apply to th
Page 66 and 67: surrounding basins. Thick sands ero
Page 68 and 69:
Haig and Lynch 1993, Erbacher et al
Page 70 and 71:
SECTION 6 (LATE CRETACEOUS CLIMATES
Page 72 and 73:
has highlighted the roles played by
Page 74 and 75:
6.4.2 Palaeobotany Cenomanian flora
Page 76 and 77:
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 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 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
Page 204 and 205:
1. TIME SLICE T-1 Age Range: Paleoc
Page 206 and 207:
also include relatively frequent No
Page 208 and 209:
Inferred climate Some differences b
Page 210 and 211:
Microfloras preserved in the Lower
Page 212 and 213:
subtropical affinities are rare, hi
Page 214 and 215:
2. TIME SLICE T-2 Age Range: Early
Page 216 and 217:
Inferred climate Climates appear to
Page 218 and 219:
northern New South Wales. The assem
Page 220 and 221:
2.2.5 Central southern Australia Ha
Page 222 and 223:
a number of distinctive Proteaceae
Page 224 and 225:
Inferred climate The Regatta Point
Page 226 and 227:
3. TIME SLICE T-3 Age Range: Middle
Page 228 and 229:
2. Lake Torrens Basin Abundant leaf
Page 230 and 231:
Dominance is highly variable. For e
Page 232 and 233:
types (M.K. Macphail unpubl. data).
Page 234 and 235:
Dacrycarpus), Euphorbiaceae (Austro
Page 236 and 237:
(possibly upper mesotherm) and drie
Page 238 and 239:
Basin) on the Eyre Peninsula (Alley
Page 240 and 241:
explanation is that a warm water gy
Page 242 and 243:
several taxa, which first appear in
Page 244 and 245:
4. TIME SLICE T-4 Age Range: Oligoc
Page 246 and 247:
Inferred climate The southern limit
Page 248 and 249:
The lowest and possibly the oldest
Page 250 and 251:
Dominants include fresh to brackish
Page 252 and 253:
Based on the relative abundance of
Page 254 and 255:
(Morgan 1977, McMinn 1981a, Martin
Page 256 and 257:
common (up to 5-6%) in the middle s
Page 258 and 259:
Polypodiaceae, Palmae (Dicolpopolli
Page 260 and 261:
Strasburgeriaceae. Proprietary info
Page 262 and 263:
Rare taxa which first appear in the
Page 264 and 265:
Correlative microfloras in the onsh
Page 266 and 267:
impression of floristic impoverishm
Page 268 and 269:
(Lophosoria) reached Tasmania befor
Page 270 and 271:
2. Otway Basin Oxygen isotope strat
Page 272 and 273:
5. TIME SLICE T-5 Age Range: Late M
Page 274 and 275:
Casuarinaceae, Cunoniaceae, Elaeoca
Page 276 and 277:
maximum temperature of the hottest
Page 278 and 279:
Nothofagus-gymnosperm temperate rai
Page 280:
5.2.7 Tasmania Late Neogene sedimen
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