OFR 151.pdf - CRC LEME

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Lindsay, J.M. and Harris, W.K., 1964. Morphett Street and Victoria Bridges foundation stratigraphy. Geological Survey of South Australia Palaeontological Report 1964/5 (unpublished). Lockey, M.G., 1998. The vertebrate track record. Nature 396: 429-432. Lu, G. and Keller, G., 1993. The Paleocene-Eocene transition in the Antarctic Indian Ocean: inferences from planktic foraminifera. Marine Micropaleontology 21: 101-141. Luly, J., Sluiter, I.R. and Kershaw, A.P., 1980. Pollen studies of Tertiary brown coals: preliminary analyses of lithotypes, Latrobe Valley, Victoria. Monash Publications in Geography 23: 1-78. Lupia, R., Lidgard, S. and Crane, P.R., 1999. Comparing palynological abundance and diversity: implications for biotic replacement during the Cretaceous angiosperm radiation. Paleobiology 25: 305-340. Mabberley, D.J., 1989. The Plant Book: a Portable Dictionary of the Higher Plants. Cambridge University Press, Cambridge. 707 pp. Mackness, B.S., Whitehead, P.W. and McNamara, G.C., 2000. New potassium-argon basalt date in relation to the Pliocene Bluff Downs Local Fauna, northern Australia. Australian Journal of Earth Sciences 47: 807-811. Mackensen, A. and Ehrmann, W.U., 1992. Middle Eocene through early Oligocene climatic history and paleoceanography in the Southern Ocean: stable oxygen and carbon isotopes from ODP sites on Maud Rise and Kerguelen Plateau. Marine Geology 108: 1-27. MacLeod, K.M. and Huber, B.T., 1996. Reorganization of deep ocean circulation accompanying a Late Cretaceous extinction event. Nature 380: 422-425. Macphail, M.K., 1979. Vegetation and climates in Southern Tasmania since the last glaciation. Quaternary Research 11: 306-341. Macphail, M.K., 1980. Natural regeneration processes in Tasmanian forests: a long-term perspective based on pollen analysis. Search 11: 184-190. Macphail, M.K., 1986. 'Over the Top': pollen-based reconstructions of past alpine floras and vegetation in Tasmania. In: B.A. Barlow (Editor), Flora and Fauna of Alpine Australasia: Ages and Origins. CSIRO/Australian Systematic Botany Society, Melbourne, pp. 173-204. Macphail, M.K., 1991. Cooking up our data. Palynological and Palaeobotanical Society of Australasia Newsletter 22: 5-8. Macphail, M.K., 1993. Palynological Analysis, Shell Wild Dog-1, VIC-P-28, Torquay Subbasin, Victoria. Consultant Palynological Services (unpublished). Macphail, M.K., 1994a. Impact of the K/T event on the southeast Australian flora and vegetation: mass extinction, niche disruption or nil? Palaeoaustral 1: 9-13. Macphail, M.K., 1994b. Palynological analysis, 80-184 m, Yallalie-1, EP 321, Western Australia. Geological Survey of Western Australia Palaeontological Report (unpublished). Macphail, M.K., 1996a. A habitat for the enigmatic Wynyardia bassiana Spencer 1901, Australia’s first described Tertiary land mammal? Alcheringa 20: 227-243. Macphail, M.K., 1996b. Neogene environments in Australia 1: re-evaluation of microfloras associated with important Early Pliocene marsupial remains at Grange Burn, southwest Victoria. Review of Palaeobotany and Palynology 92, 307-328. 147
Macphail, M.K., 1996c. A provisional palynostratigraphic framework for Tertiary organic facies in the Burt Plain, Hale, Ngalia, Santa Teresa, Ti-tree and Waite Basins, Northern Territory. AGSO Record 1996/58: 1-21. Macphail, M.K., 1997a. Palynostratigraphy of Late Cretaceous to Tertiary Basins in the Alice Springs District, Northern Territory. AGSO Record 1997/13: 1-27. Macphail, M.K., 1997b. Late Neogene climates in Australia: fossil pollen- and spore-based estimates in retrospect and prospect. Australian Journal of Botany 45: 425-464. Macphail, M.K., 1997c. Comment on M. Pole (1994): ‘The New Zealand flora-entirely long distance dispersal’. Journal of Biogeography 24: 113-117. Macphail, M.K., 1999. Palynostratigraphy of the Murray Basin, inland southeastern Australia. Palynology 23: 199-242. Macphail, M.K., 2000. Sequestration of the Australian flora. Australian Systematic Botany Society Newsletter 102: 21-25. Macphail, M.K. and Hill, R.S., 1994. K-Ar dated palynofloras in Tasmania 1: Early Oligocene Proteacidites tuberculatus Zone sediments, Wilmot Dam, northwestern Tasmania. Papers and Proceedings of the Royal Society of Tasmania 128: 1-15. Macphail, M.K. and Hos, D.P.C., 1990. Palynological report on Copa-1, Otway Basin for Cultus Petroleum Australia NL. International Stratigraphic Consultants (unpublished). Macphail, M.K. and Kellett, J.R., 1993. Palynostratigraphy of the Bookpurnong Beds and related late Miocene-Early Pliocene facies in the central-west Murray Basin, part 1: dinoflagellates. AGSO Journal of Australian Geology and Geophysics 14: 371-382. Macphail, M.K. and Truswell, E.M., 1989. Palynostratigraphy of the central west Murray Basin. BMR Journal of Australian Geology and Geophysics 11: 301-331. Macphail, M.K. and Truswell, E.M., 1993. Palynostratigraphy of the Bookpurnong Beds and related late Miocene-Early Pliocene facies in the central-west Murray Basin, part 2: spores and pollen. AGSO Journal of Australian Geology and Geophysics 14: 383- 409. Macphail, M. and Truswell, E.M., 2000. Palynological analysis of core catcher samples, Site 1166a, Prydz Bay, East Antarctica. Part 1: 142.5-220.84 mbsf. AGSO Report 15 July (unpublished). Macphail, M.K., Hill, R.S., Forsyth, S.J. and Wells, P.M., 1991. A Late Oligocene-Early Miocene cool climate flora in Tasmania. Alcheringa 15: 87-106. Macphail, M.K., Colhoun, E.A., Kiernan, K and Hannan, D., 1993. Glacial climates in the Antarctic region during the late Paleogene: evidence from northwest Tasmania, Australia. Geology 21: 145-148. Macphail, M.K., Jordan, G.J. and Hill, R.S., 1993. Key periods in the evolution of the Cenozoic vegetation and flora in western Tasmania 1: the Early-Middle Pleistocene. Australian Journal of Botany 41, 673-707. Macphail, M.K., Kellett, J.R., Rexilius, J.P. and O’Rorke, M.E., 1993. The “Geera Clay equivalent”: a regressive marine unit in the Renmark Group that sheds new light on the age of the Mologa weathering surface in the Murray Basin. AGSO Journal of Australian Geology and Geophysics 14: 47-63. Macphail, M.K., Alley, N.F., Truswell, E.M. and Sluiter, I.R.K., 1994. Early Tertiary vegetation: evidence from spores and pollen. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 189-261. 148
Page 1 and 2:
CRCLEME Cooperative Research Centre
Page 3 and 4:
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
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 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
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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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