OFR 151.pdf - CRC LEME

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Macphail, M.K., Colhoun, E.A. and Fitzsimmons. S.J., 1995. Key periods in the evolution of the Cenozoic vegetation and flora in western Tasmania: the Late Pliocene. Australian Journal of Botany 43: 505-526. Macphail, M.K., Hill, K., Partridge, A.D. and Truswell, E.M., 1995. ‘Wollemi Pine’ - old pollen records for a newly discovered genus of gymnosperms. Geology Today 11: 48- 50. Macphail, M.K., Jacobson, G. and Pemberton, M., 1999. Peat mounds of southwest Tasmania: possible origins. Australian Journal of Earth Sciences 46: 667-677. Macphail, M.K., Partridge, A.D. and Truswell, E.M., 1999. Fossil pollen records of the problematical primitive angiosperm family Lactoridaceae in Australia. Plant Systematics and Evolution 214: 199-210. Markgraf, V. McGlone, M. and Hope, G., 1995. Neogene palaeoenvironmental and palaeoclimatic change in southern temperate ecosystems – a southern perspective. Trends in Ecology and Evolution 10: 143-146. Marshall, N., 1984. Late Cretaceous dinoflagellates from the Perth Basin, Western Australia. Unpublished PhD. Thesis, University of Western Australia. Marshall, N., 1988. A Santonian dinoflagellate assemblage from the Gippsland Basin, southeastern Australia. Association of Australasian Palaeontologists Memoir 5: 195- 215. Marshall, N., 1989. An unusual assemblage of algal cysts from the late Cretaceous, Gippsland Basin, southeastern Australia. Palynology 13: 21-56. Martin, H.A., 1973. Upper Tertiary palynology in southern New South Wales. Special Publication of the Geological Society of Australia 4: 35-54. Martin, H.A., 1974. The identification of some Tertiary pollen belonging to the family Euphorbiaceae. Australian Journal of Botany 25: 271-291. Martin, H.A., 1977. The history of Ilex (Aquifoliaceae) with special reference to Australia: evidence from pollen. Australian Journal of Botany 25: 655-673. Martin, H.A., 1980. Stratigraphic palynology from shallow bores in the Namoi and Gwydir River Valleys, north-central New South Wales. Journal and Proceedings of the Royal Society of New South Wales 113: 81-87. Martin, H.A., 1981. Stratigraphic palynology of the Castlereagh River Valley, New South Wales. Journal and Proceedings of the Royal Society of New South Wales 114: 77- 84. Martin, H.A., 1985. The stratigraphic palynology of Squid-1 and Tasmanian Devil-1, Bass Basin. Kimberley Oil and Gas NL Palaeontological Report (unpublished). Martin, H.A., 1986. Tertiary stratigraphy, vegetation and climate of the Murray Basin in New South Wales. Journal and Proceedings of the Royal Society of New South Wales 119: 43-53. Martin, H.A., 1987. Cainozoic history of the vegetation and climate of the Lachlan River Valley region, New South Wales. Proceedings of the Linnean Society of New South Wales 109: 213-257. Martin, H.A., 1988. Stratigraphic palynology of the Lake Menindee region, northwest Murray Basin, New South Wales. Journal and Proceedings of the Royal Society of New South Wales 121: 1-9. Martin, H.A., 1990. The palynology of the Namba Formation in the Wooltana-1 bore, Callabonna Basin (Lake Frome), South Australia, and its relevance to Miocene grasslands in central Australia. Alcheringa 14: 247-255. 149
Martin, H.A., 1991a. Dinoflagellate and spore pollen biostratigraphy of the S.A.D.M.E. MC63 bore, western Murray Basin. Alcheringa 15: 107-144. Martin, H.A., 1991b. Tertiary stratigraphic palynology and palaeoclimate of the inland river systems in New South Wales. Special Publications of the Geological Society of Australia 18: 181-194. Martin, H.A., 1993. The palaeovegetation of the Murray Basin, Late Eocene to mid-Miocene. Australian Systematic Botany 6: 491-531. Martin, H.A., 1994. Australian Tertiary phytogeography. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 104-142. Martin, H.A., 1997a. The use of ecological tolerances for the reconstruction of Tertiary palaeoclimates. Australian Journal of Botany 45: 475-492. Martin, H.A., 1997b. The stratigraphic palynology of bores along the Darling River, downstream from Bourke, New South Wales. Proceedings of the Linnean Society of New South Wales 118: 51-67. Martin, H.A., 1998a. Tertiary climate evolution and the development of aridity in Australia. Proceedings of the Linnean Society of New South Wales 119: 115-136. Martin, H.A., 1998b. Late Cretaceous-Cainozoic palynology of the Poonarunna No. 1 well, central Australia. Transactions of the Royal Society of South Australia 122: 89-138. Martin, H.A., 1999a. The stratigraphic palynology of the Macquarie River Valley, western New South Wales. Department of Water Resources (unpublished). Martin, H.A., 1999b. The palynology of core samples from Bore No. GW 096000, west of Narromine, N.S.W. Report prepared for Land and Water Conservation, Dubbo (unpublished). Martin, H.A., 2000. Re-assignment of the affinities of the fossil pollen type Tricolpites trioblatus Mildenhall and Pocknall to Wilsonia (Convolvulaceae) and a reassessment of the ecological interpretations. Review of Palaeobotany and Palynology 111: 237- 251. Martin, H.A. and McMinn, A., 1993. 10: Palynology of Sites 815 and 823: The Neogene vegetation history of coastal northeastern Australia. Proceedings of the Ocean Drilling Program, Scientific Results 133: 115-123. Martin, H.A. and McMinn, A., 1994. Late Cainozoic vegetation history of northwestern Australia from the palynology of a deep sea core ODP Site 765. Australian Journal of Botany 42: 95-102. Martin, H.A., Worrall, L. and Chalson, J., 1987. The first occurrence of the Paleocene Lygistepollenites balmei Zone in the Eastern Highlands region, New South Wales. Australian Journal of Earth Sciences 34: 359-365. Martin, H.A., Macphail, M.K. and Partridge, A.D., 1997. Tertiary Alangium (Alangiaceae) in Eastern Australia. Review of Palaeobotany and Palynology 94: 111-122. McCarthy, P.J., Faccini, U.F. and Plint, A.G., 1998. Evolution of an ancient coastal plain: palaeosols, interfluves and alluvial architecture in a sequence stratigraphic framework, Cenomanian Dunvegan Formation, NE British Columbia, Canada. Sedimentology 46: 861-891. McCarthy, P.J. and Plint, A.G., 1998. Recognition of interfluve sequence boundaries: integrating paleopedology and sequence stratigraphy. Geology 26: 387-390. McGowran, B., 1989. The later Eocene transgressions in southern Australia. Alcheringa 13: 45-68. 150
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CRCLEME Cooperative Research Centre
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Electronic copies of the publicatio
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and, for Tertiary continental seque
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2. Analysis of a Plio-Pleistocene l
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Table A (cont.) Basin and related s
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Figure A: Generalised climatic curv
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Carpenter, R.J., Hill, R.S., Greenw
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Hill, S.M., Eggleton, R.A. and Tayl
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Macphail, M.K. and Stone, M.S., 200
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Swenson, U., Backlund, McLoughlin,
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EXECUTIVE SUMMARY This review prese
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Temperature Climates in palaeo-sout
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SUMMARY OF INFERRED CRETACEOUS PALA
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INTRODUCTION Mineral resources, whe
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Professor B. Balme (Geology Departm
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Section 7 (Tertiary climates) This
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vegetation. Moreover, individual ta
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1.3 Flora, vegetation and climate 1
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TABLE 2: Classification of vegetati
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Figure 2: Relationship of different
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Accordingly, only at sites with exc
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2.1.3 Palaeoecology Palaeoecology i
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wind-pollinated trees and shrubs bu
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1. The usual practice of equating t
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1. Palaeontological evidence Like p
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5. Facies architecture and lithostr
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Subsequent developments include mel
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SECTION 4 (GEOGRAPHIC BOUNDARIES AN
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SECTION 5 (EARLY CRETACEOUS CLIMATE
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events on other continents and sugg
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If these considerations apply to th
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surrounding basins. Thick sands ero
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Haig and Lynch 1993, Erbacher et al
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SECTION 6 (LATE CRETACEOUS CLIMATES
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has highlighted the roles played by
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6.4.2 Palaeobotany Cenomanian flora
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Palaeo-southern Australia Dryland c
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6.7 Time Slice K-6. Late Campanian-
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7.1. Global backdrop SECTION 7 (TER
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Explanations for the PETM are centr
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East Antarctica and strengthening o
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amplifying, pacing and potentially
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southeastern Australia than elsewhe
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7.4 Time Slice T-1. Paleocene [65-5
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Palaeo-southern Australia Unlike no
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Palaeo-central Australia As for the
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7.6.2 Palaeobotany The palaeobotani
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Zone microfloras imply temporary wa
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Page 102 and 103: Similarly it is difficult to summar
Page 104 and 105: However, the data are emphatic that
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Page 108 and 109: fossil taxa that are morphologicall
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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 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
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Inferred climate As for regions to
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APPENDIX 2 TERTIARY DATA 201
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1. TIME SLICE T-1 Age Range: Paleoc
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also include relatively frequent No
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Inferred climate Some differences b
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Microfloras preserved in the Lower
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subtropical affinities are rare, hi
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2. TIME SLICE T-2 Age Range: Early
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Inferred climate Climates appear to
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northern New South Wales. The assem
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2.2.5 Central southern Australia Ha
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a number of distinctive Proteaceae
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Inferred climate The Regatta Point
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3. TIME SLICE T-3 Age Range: Middle
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2. Lake Torrens Basin Abundant leaf
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Dominance is highly variable. For e
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types (M.K. Macphail unpubl. data).
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Dacrycarpus), Euphorbiaceae (Austro
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(possibly upper mesotherm) and drie
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Basin) on the Eyre Peninsula (Alley
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explanation is that a warm water gy
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several taxa, which first appear in
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4. TIME SLICE T-4 Age Range: Oligoc
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Inferred climate The southern limit
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The lowest and possibly the oldest
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Dominants include fresh to brackish
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Based on the relative abundance of
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(Morgan 1977, McMinn 1981a, Martin
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common (up to 5-6%) in the middle s
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Polypodiaceae, Palmae (Dicolpopolli
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Strasburgeriaceae. Proprietary info
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Rare taxa which first appear in the
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Correlative microfloras in the onsh
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impression of floristic impoverishm
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(Lophosoria) reached Tasmania befor
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2. Otway Basin Oxygen isotope strat
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5. TIME SLICE T-5 Age Range: Late M
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Casuarinaceae, Cunoniaceae, Elaeoca
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maximum temperature of the hottest
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Nothofagus-gymnosperm temperate rai
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5.2.7 Tasmania Late Neogene sedimen
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