OFR 151.pdf - CRC LEME

More documents

Recommendations

Info

Evans, P.R., 1970b. Palynology of Hazelwood-1, Badcock-1, Launceston Basin, Tasmania. Esso Australia Palaeontological Report 1970/37 (unpublished). Evans, P.R. and Mulholland, R.D., 1969. Palynology of Esso Clam-1. Esso Australia Palaeontological Report 1969/15 (unpublished). Fairburn, W.A., 1998. The Willunga Embayment - a stratigraphic revision. MESA Journal 11: 35-41. Fairburn, W.A., 2000. Cainozoic stratigraphy of the Noarlunga Embayment. MESA Journal 18: 42-47. Falcon-Lang, H.J., 2000. The relationship between leaf longevity and growth ring markedness in modern conifer woods and its implication for palaeoclimatic studies. Palaeogeography, Palaeoclimatology, Palaeoecology 160: 317-328. Farley, K.A., Montanari, A., Shoemaker, E.M. and Shoemaker, C.S., 1998. Geochemical evidence for a comet shower in the Late Eocene. Science 280: 1250-1253. Feary, D.A., Davies, P.J., Pigram, C.J. and Symonds, P.A., 1991. Climatic evolution and control on carbonate deposition in northeast Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 89: 341-361. Filippelli, G.M., 1997. Intensification of the Asian monsoon and chemical weathering event in the late Miocene-early Pliocene: implications for late Neogene climatic change. Geology 25: 27-30. Flannery, T.F., 1984. Re-examination of the Quanbun Local Fauna, a Late Cenozoic vertebrate fauna from Western Australia. Records of the Western Australian Museum 11: 119-128. Flannery, T.F., Rich, T.H., Turnbull, W.D. and Lundelius, E.L., 1992. The Macropodoidea (Marsupialia) of the early Pliocene Hamilton local fauna, Victoria, Australia. Fieldiana Geology NS 25: 1-37. Flower, B.P. and Kennett, J.P., 1994. The middle Miocene climatic transition: East Antarctic ice sheet development, deep ocean circulation and global carbon cycling. Palaeogeography, Palaeoclimatology, Palaeoecology 108: 537-555. Floyd, A.G., 1989. Australian Rainforest of Mainland South-eastern Australia. Inkata Press, Melbourne. 420 pp. Foreman, D.B. and Walsh, N.G., 1993. Flora of Victoria Volume 1: Introduction. Inkata Press, Port Melbourne. 320 pp. Forsyth, S.M., 1979a. Draft report on Hagley Hole-6 2133-2560 ft. Tasmanian Department of Mines (unpublished). Forsyth, S.M., 1979b. Draft report on the palynology of drillholes in the Devonport-Port Sorell Sub-basin. Tasmanian Department of Mines (unpublished). Fortey, R., 1993. The Hidden Landscape. Jonathon Cape, London. 310 pp. Foster, C.B., 1982. Illustrations of Early Tertiary (Eocene) plant microfossils from the Yaamba Basin, Queensland. Geological Survey of Queensland Publication 381: 1-32. Fox, M.D., 1999. Present environmental influences on the Australian flora. In: A.E. Orchard (Editor). Flora of Australia Volume 1 (2 nd edition). ABRS/CSIRO, pp. 204-249. Frakes, L.A., 1997. Grossplots: a method for estimating the temperature state of the earth and of Australia. Cretaceous to Middle Miocene. Australian Journal of Botany 45: 359- 372. Frakes, L.A., 1999. Evolution of Australian environments. In: A.E. Orchard (Editor), Flora of Australia Volume 1 (2 nd edition). ABRS/CSIRO, Canberra, pp. 163-204. 135
Frakes, L.A. and Francis, J.E., 1988. A guide to Phanerozoic cold polar climates from highlatitude ice-rafting in the Cretaceous. Nature 333: 547-549. Frakes, L.A. and 21 co-authors 1987. Australian Cretaceous shorelines, stage by stage. Palaeogeography, Palaeoclimatology, Palaeoecology 59: 31-48. Frakes, L.A., Alley, N.F. and Deynoux, M., 1995. Early Cretaceous ice-rafting and climatic zonation in Australia. International Geological Review 37: 567-583. Francis, J.E. and Frakes, L.A., 1993. Cretaceous climates. Sedimentological Review 1: 17-30. Francis, J.E. and Hill, R.S., 1996. Fossil plants from the Pliocene Sirius Group, Transantarctic Mountains: evidence for climate from growth rings and fossil leaves. Palaios 11: 389- 396. Frank, T.D. and Arthur, M.A., 1999. Tectonic forcing of Maastrichtian ocean-climate evolution. Paleoceanography 14: 103-117. Frederiksen, N.O., 1991. Pulses of Middle Eocene to earliest Oligocene climatic deterioration in southern California and the Gulf Coast. Palaios 6: 564-571. Funder, S, Abrahamsen, N., Bennike, O. and Feyling-Hanssen, R.W., 1985. Forested Arctic: evidence from North Greenland. Geology 13: 542-546. Gammon, P.R., James, N.P., Clarke, J.D.A. and Bone, Y., 2000. Sedimentology and lithostratigraphy of Upper Eocene sponge-rich sediments, southern Western Australia. Australian Journal of Earth Sciences 47: 1087-1103. Gaston, K.J., 2000. Biodiversity: higher taxon richness. Progress in Physical Geography 24: 117-127. Gentilli, J., 1972. Australian Climate Patterns. Nelson, Melbourne. 285 pp. Gentilli, J., 1986. Climate. In: D.N. Jeans (Editor), The Natural Environment. Sydney University Press, Sydney, pp. 14-48. Geotimes, 1995. Model links ancient impact to volcanic eruptions. Geotimes May: 11. Gersonde, R. and 12 co-authors, 1997. Geological record and reconstruction of the late Pliocene impact of the Eltanin asteroid in the Southern Ocean. Nature 390: 357-363. Gestaldo, R.A. and Ferguson, D.K., 1998. Reconstructing Tertiary plant communities: introductory remarks. Review of Palaeobotany and Palynology 101: 3-6. Gibbons, A., 1997. Molecular evolution: did birds fly through the K-T extinctions with flying colours? Science 275: 1068. Gibson, T.G., Bybell, L.M. and Mason, D.B., 2000. Stratigraphic and climatic implications of clay mineral changes around the Paleocene/Eocene boundary of the northeastern US margin. Sedimentary Geology 134: 65-92. Glassford, D.K. and Semeniuk, V., 1995. Desert-aeolian origin of late Cenozoic regolith in arid and semi-arid southwestern Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 114: 131-166. Gleadow, A.J.W. and Duddy, I.R., 1981. Early Cretaceous volcanism and the early breakup of south-eastern Australia: evidence from fission track dating of volcanoclastic sediments. In: M.M. Creswell and P. Vella (Editors), Fifth International Gondwana Symposium. Wellington, New Zealand. Balkema Press, Rotterdam, pp. 295-300. Glenie, R.C. (Editor), 1986. Second South-eastern Australia Oil Exploration Symposium: Technical Papers. Petroleum Exploration Society of Australia Victorian and Tasmanian Branch, Melbourne. 469 pp. 136
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 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
show all

OFR 151.pdf - CRC LEME

Create successful ePaper yourself

Delete template?

Save as template?