OFR 151.pdf - CRC LEME

More documents

Recommendations

Info

Abstracts of the Annual General Meeting of the Geological Society of America 23: 302. Partridge, A.D., 1976. The geological expression of eustacy in the Early Tertiary of the Gippsland Basin, Australia. APEA Journal 16: 73-79. Partridge, A.D., 1993. Palynological analysis of four samples from deep leads near Stawell, Victoria. Biostrata Report 1993/21 (unpublished). Partridge, A.D., 1997. Palynological analysis of bore samples from Tertiary palaeochannels in Western Australia. Biostrata Report 1997/19 (unpublished). Partridge, A.D., 1999. Late Cretaceous to Tertiary Geological Evolution of the Gippsland Basin, Victoria,, 2 Volumes. Unpublished PhD Thesis, Latrobe University, Melbourne. 439 pp. Paul, C.R.C. and Mitchell, S.F., 1994. Is famine a common factor in marine mass extinctions? Geology 22: 679-682. Pearson, P.N. and Palmer, M.R., 1999. Middle Eocene seawater pH and atmospheric carbon dioxide concentrations. Science 284: 1824-1826. Pederson, J., Pazzaglia, F. and Smith, G., 2000. Ancient hillslope deposits: missing links in the study of climate controls on sedimentation. Geology 28: 27-30. Pekar, S. and Miller, K.G., 1996. New Jersey Oligocene “icehouse” sequences (ODP Leg 150X) correlated with global δ 18 O and Exxon eustatic records. Geology 24: 567-570. Pell, S.D., Williams, I.S. and Chivas, A.R., 1997. The use of protolith zircon-age fingerprints in determining the protosource areas for some Australian dune sands. Sedimentary Geology 109: 233-260. Peres, C., 1999. Tropical forest disturbance and dynamics in Southeast Asia. Trends in Ecology and Evolution 14: 217-218. Peters, M.D. and Christophel, D.C., 1978. Austrosequoia wintonensis, a new taxodiaceous cone from Queensland, Queensland. Canadian Journal of Botany 56: 3119-3128. Peterson, L.C., 1998. The late Paleocene thermal maximum. Geotimes February: 52. Pickett, J.W. and McMinn, A., 1983. Foraminifera and palynomorphs from Water Resources Commission bore Box Creel PWP. New South Wales Geological Survey Palaeontological Report 1983/6 (unpublished). Pickett, J.W., Macphail, M.K., Partridge, A.D. and Pole, M.S., 1997. Middle Miocene palaeotopography at Little Bay, near Marouba, New South Wales. Australian Journal of Earth Sciences 44: 509-518. Pickett, J.W., Smith, N., Bishop, P.M., Hill, R.S., Macphail, M.K. and Holmes, W.B.K., 1990. A stratigraphic evaluation of Ettingshausen’s New England Tertiary plant localities. Australian Journal of Earth Sciences 37: 293-303. Pillans, B., 1998. Regolith Dating Methods: a guide to numerical dating techniques. Cooperative Research Centre for Landscape Evolution and Mineral Exploration, Canberra. 30 pp. Pirrie, D., Doyle, P., Marshall, J.D. and Ellis, G., 1995. Cool Cretaceous climates – new data from the Albian of Western Australia. Journal of the Geological Society of London 152: 739-742. Pitt, G.M., Benbow, M.C. and Barnes, L.C., 1976. Report on drilling in the Tallaringa Palaeodrainage System, 1976. Geological Survey of South Australia Palaeontological Report 1976/76 (unpublished). 155
Playford, G., Haig, D.W. and Dettmann, M.E., 1975. A mid-Cretaceous microfossil assemblages from the Great Artesian Basin, northwestern Queensland. Neus Jahrbuch fur Geologie und Palaontologie 149: 333-362. Plummer, P., 1998. Five may not be first. Geology Today November-December: 220. Poag, C.W. and 6 co-authors, 1992. Deep Sea Drilling Project Site 612 bolide event: new evidence of a late Eocene impact wave deposit and a possible impact site. Geology 20: 771-774. Pole, M., 1992. Eocene vegetation from Hasties, north-eastern Tasmania. Australian Systematic Botany 5: 431-475. Pole, M.S. and Bowman, D.M.J.S., 1996. Tertiary plant fossils from Australia’s Top End. Australian Systematic Botany 9: 113-126. Pole, M. and Douglas, J.G., 1999. Bennettitales, Cycadales and Gingkoales from the mid Cretaceous of the Eromanga Basin, Queensland, Australia. Cretaceous Research 20: 523-538. Pole, M. and Macphail, M.K., 1996. Eocene Nypa from Regatta Point, Tasmania. Review of Palaeobotany and Palynology 92: 55-67. Pole, M.S., Hill, R.S., Green, N. and Macphail, M.K., 1993. The Oligocene Berwick Quarry Flora – rainforest in a drying environment. Australian Systematic Botany 6: 399-427. Powis, G. and Partridge, A.D., 1980. Palynological analysis of Jerboa-1, Eyre Basin, Western Australia. Esso Australia Ltd. Palaeontological Report 1980/15 (unpublished). Preisinger, A. and 10 co-authors, 1986. The Cretaceous/Tertiary boundary in the Gosau Basin, Austria. Nature 322: 794-799. Prentice, I.C., Cramer, W., Harrison, S.P., Leemans, R., Monserud, R.A. and Solomon, A.M., 1992. A global biome model based on plant physiology and dominance, soil properties and climate. Journal of Biogeography 19: 117-134. Prentice, I.C. and Webb, T., 1998. BIOME 6000: reconstructing global mid-Holocene vegetation patterns from palaeoecological records. Journal of Biogeography 25: 997- 1005. Price, G.D., 1998. Prediction of modern bauxite occurrence: implications for climatic reconstruction – reply. Palaeogeography, Palaeoclimatology, Palaeoecology 142: 257-258. Price, G.D., Valdes, P.J. and Sellwood, B.W., 1997. Prediction of modern bauxite occurrence: implications for climatic reconstruction. Palaeogeography, Palaeoclimatology, Palaeoecology 131: 1-13. Price, G.D., Valdes, P.J. and Sellwood, B.W., 1998. A comparison of GCM simulated Cretaceous ‘greenhouse’ and ‘icehouse’ climates: implications for the sedimentary record. Palaeogeography, Palaeoclimatology, Palaeoecology 142: 123-138. Quilty, P.G., 1977. Cenozoic sedimentation cycles in Western Australia. Geology 5: 336-340. Quilty, P.G., 1994. The background: 144 million years of Australian palaeoclimate and palaeogeography. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 14-43. Raine, I., 1994. Terrestrial K/T boundary studies in New Zealand. Palaeoaustral 2: 9-12. Ramstein, G., Fluteau, F., Besse, J. and Joussaume, S., 1997. Effect of orogeny, plate motion and land-sea distribution on Eurasian climate change over the past 30 million years. Nature 386: 788-795. 156
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 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
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 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
show all

OFR 151.pdf - CRC LEME

Create successful ePaper yourself

Delete template?

Save as template?