OFR 151.pdf - CRC LEME

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Exon, N.F. and 28 co-authors, 2002. Drilling reveals climatic consequences of Tasmanian Gateway opening. Transactions of the American Geophysical Union 83: 253, 258-259. Exon, N.F., Kennett, J.P. and Malone, M.J., 2004a. 1. Leg 189 synthesis: Cretaceous- Holocene history of the Tasmanian Gateway. In Exon, N.F., Kennett, J.P. and Malone, M.J. (Editors) Proceedings ODP Scientific Results 189: 1-37. Exon, N.F. and 5 co-authors, 2004b. Tectono-sedimentary history of uppermost Cretaceous through Oligocene sequences from the Tasmanian region, a temperate Antarctic margin. Geophysical Monograph Series 151: 319-344. Exon, N.F., Hill, P.J., Mitchell, C. and Post, A., 2005. Nature and origin of the submarine Albany canyons off southwest Australia. Australian Journal of Earth Sciences 52: 101- 115. Forsyth, A. and Nott, J., 2003. Evolution of drainage patterns on Cape York Peninsula, northeast Queensland. Australian Journal of Earth Sciences 50: 145-155. Frakes, L.A. and Barron, E.J., 2001. Phanerozoic general circulation model and quantitative climate data for Australia. Australian Journal of Earth Sciences 48: 643-655. Fujioka, T. and 5 co-authors, 2005. Global cooling initiated stony deserts in central Australia 2-4 Ma, dated by cosmogenic 21 Ne- 10 Be. Geology 33: 993-996. Gallagher, S.J. and 5 co-authors, 2003. The Pliocene climatic and environmental evolution of southeastern Australia: evidence from the marine and terrestrial realm. Palaeogeography, Palaeoclimatology, Palaeoecology 193: 349-382. Gammon, P.R. and James, N.P., 2001. Palaeogeographical influence of Late Eocene biosiliceous sponge-rich sedimentation, southern Western Australia. Sedimentology 48: 559-584. Gibbs, S.J., Brown, P.R., Sessa, J.A., Bralower, T.J. and Wilson, P.A., 2006. Nannoplankton extinction and origination across the Paleocene-Eocene Thermal maximum. Science 314: 1770-1773. Gradstein, F.M. and Ogg, J. G., 2004. Geologic Time Scale 2004 – why, how, and where next! Lethaia 37: 175-181. Greenwood, D.R., Haines, P.W. and Steart, D.C., 2001. New species of Banksieaeformis and a Banksia ‘cone’ (Proteaceae) from the Tertiary of central Australia. Australian Systematic Botany 14: 871-890. Helby, R., Morgan, R. and Partridge, A.D., 2004. Updated Jurassic-Early Cretaceous dinocyst zonation. NWS Australia. Geoscience Australia Publication ISBN: 1 920871 01 2. Heim, J.A., Vasconelos, P.M., Shuster, D.L., Farley, K.A. and Broadbent, G., 2006. Dating paleochannel iron ore by (U-Th)/He analysis of supergene goethite, Hamersley province, Australia. Geology 34: 173-176. Heine, C. and Muller, D., 2005. Late Jurassic rifting along the Australian North West Shelf: margin geometry and spreading ridge configuration. Australian Journal of Earth Sciences 52: 27-29. Hill, P.J. and Exon, N.F., 2004. Tectonics and basin development of the Tasmanian Offshore Zone incorporating results from Deep Ocean Drilling. Geophysical Monograph Series 151: 19-42. Hill, R.S., 2001. Biogeography, evolution and palaeoecology of Nothofagus (Nothofagaceae): the contribution of the fossil record. Australian Journal of Botany 49: 321-332. Hill, R.S. and Whang, S.S., 2000. Dacrycarpus (Podocarpaceae) macrofossils from Miocene sediments at Elands, eastern Australia. Australian Systematic Botany 13: 395-408. Hill, R.S. and Brodribb, T.J., 2001. Macrofossil evidence for the onset of xeromorphy in Australian Casuarinaceae and tribe Banksieae (Proteaceae). Journal of Mediterranean Ecology 2: 127-126. Hill, R.S. and Cristophel, D.C., 2001. Two new species of Dacrydium (Podocarpaceae) based on vegetative fossils from Middle Eocene sediments at Nelly Creek, central Australia. Australian Systematic Botany 14: 193-205. Hill, R.S. and Paull, R., 2003. Fitzroya (Cupressaceae) macrofossils from Cenozoic sediments in Tasmania, Australia. Review of Palaeobotany and Palynology 126: 145-152. 13
Hill, S.M., Eggleton, R.A. and Taylor, G., 2003. Neotectonic disruption of silicified palaeovalley systems in intraplate, cratonic landscape: regolith and landscape evolution of the Mulculca range-front, Broken Hill Domain, New South Wales. Australian Journal of Earth Sciences 50: 691-707. Hocknall, S., 2005. Ecological succession during the Late Cainozoic of central-eastern Queensland: extinction of a diverse rainforest community. Memoirs of the Queensland Museum 51: 39-122. Holbourn, A., Kuhnt, W., Simo, J.A. and Li, Q., 2004. Middle Miocene isotope stratigraphy and palaeoceanographic evolution of the northwest and southwest Australian margins (Wombat Plateau and Great Australian Bight). Palaeogeography, Palaeoclimatology, Palaeoecology 208: 1-22. Holdgate, G.R., Smith, T.A.G., Gallagher, S.J. and Wallace, M.W., 2001. Geology of coalbearing Palaeogene sediments, onshore Torquay Basin, Victoria. Australian Journal of Earth Sciences 48: 657-679. Holdgate, G.R., Rodriquez, C., Johnstone, E.M., Wallace, M.W. and Gallagher, S.J., 2003a. The Gippsland Basin Top Latrobe Unconformity, and its expression in other SE Australian Basins. APEA Journal 2003: 149-172. Holdgate, G.R. and 6 co-authors, 2003b. Plio-Pleistocene tectonics and eustasy in the Gippsland Basin, southeast Australia: evidence from magnetic imagery and marine geological data. Australian Journal of Earth Sciences 50: 403-426. Holdgate, G.R., Wallace, M.W., Gallagher, S.J., Witten, R.B., Stats, B. and Wagstaff, B.E., 2006a. Cenozoic fault control on 'deep lead' palaeoriver systems, Central Highlands, Victoria. Australian Journal of Earth Sciences 53: 445-468. Holdgate, G.R. and 6 co-authors, 2006b. The Middle Miocene Yallourn coal seam – the last coal in Australia. International Journal of Coal Geology [online proof article]. Hou, B., Frakes, L.A., Alley, N.F. and Heithersay, P., 2003a. Evolution of beach placer shorelines and heavy-mineral deposition in the eastern Eucla Basin, South Australia. Australian Journal of Earth Sciences 50: 955-965. Hou, B., Frakes, L.A., Alley, N.F. and Clarke, J.D.A., 2003b. Characteristics and evolution of the Tertiary palaeovalleys in the northwest Gawler Craton, South Australia. Australian Journal of Earth Sciences 50: 215-230. Hou, B., Alley, N.F., Frakes, L.A., Stoian, L. and Cowley, W.M., 2006. Eocene stratigraphic succession in the Eucla Basin of South Australia and correlation to major regional sealevel events. Sedimentary Geology 183: 297-319. Huff, P.M., Wilf, P. and Azumah, E.J., 2003. Digital future for paleoclimate estimation from fossil leaves? Preliminary results. Palaios 18: 266-274. Husing, S.K., Hilgen, F.J., Abdul, A. and Krijgsman, W., 2006. Completing the Neogene geological timescale between 8.5 and 12.5 Ma. Earth and Planetary Science Letters 253: 340-358. Itzstein-Davey, F., 2004. A spatial and temporal Eocene palaeoenvironmental study focusing on the Proteaceae family, from Kambalda, Western Australia. Review of Palaeobotany and Palynology 131: 159-180. Jaques, A.L., Jaireth, S. and Walshe, J.L., 2002. Mineral systems of Australia: an overview of resources, settings and processes. Australian Journal of Earth Sciences 49: 623-660. Jahren, A.H., Arens, N.C., Sarmiento, G., Guerrero, J. and Amundsun, R., 2001. Terrestrial record of methane hydrate dissociation in the Early Cretaceous. Geology 29: 159-162. Jones, M.R., 2006. Cenozoic landscape evolution in central Queensland. Australian Journal of Earth Sciences 53: 433-444. Jordan, G.J. and Hill, R.S., 2002. Cenozoic plant macrofossil sites of Tasmania. Papers and Proceedings of the Royal Society of Tasmania 136: 127-139. Katz, M.E. Cramer, E.S., Mountain, G.S., Katz, S. and Miller, K.G., 2001. Uncorking the bottle: What triggered the Paleocene/Eocene thermal maximum event? Palaeoceanography 16: 549-563. 14
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: Carpenter, R.J., Hill, R.S., Greenw
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 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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