OFR 151.pdf - CRC LEME

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SECTION 9 (REFERENCES) Acton, G.D. and Kettles, W.A., 1996. Geological and palaeomagnetic constraints on the formation of weathered profiles near Inverell, eastern Australia. Palaeogeography, Palaeoclimatology, Palaeoecology 126: 211-225. Adam, P., 1994. Australian Rainforests. Oxford University Press, Melbourne. 308 pp. Adams, J., Maslin, M. and Thomas, E., 1999. Sudden climatic transitions during the Quaternary. Progress in Physical Geography 23: 1-36. Adler, R., 1999. All dried up: forest fires are upsetting the global weather machine. New Scientist 16 October: 15. Aharon, P.L., Goldstein, S.L., Wheeler, C.W. and Jacobson, G., 1993. Sea-level events in the South Pacific linked with the Messinian salinity crisis. Geology 21: 771-775. Alexander, J., Fielding, C.R. and Jenkins, G., 1999. Plant material deposition in the tropical Burdekin River, Australia: implications for ancient fluvial sediments. Palaeogeography, Palaeoclimatology, Palaeoecology 153: 105-125. Alley, N.F., 1983a. Palynology of selected samples from Lake Eyre Bore 8A and Jackboot Bore. Geological Survey of South Australia Palaeontological Report 1983/4 (unpublished). Alley, N.F., 1983b. Palynology of selected Cainozoic samples from Tarcoola 1: 100,000 Map Sheet. Geological Survey of South Australia Palaeontological Report 1983/76 (unpublished). Alley, N.F., 1986. Ages and depositional environments of deposition of sediments in Clayton- 3 well, Eromanga Basin. Geological Survey of South Australia Palaeontological Report 1986/34 (unpublished). Alley, N.F., 1987. Middle Eocene age of the megafossil flora at Golden Grove, South Australia: preliminary report and comparison with the Maslin Bay flora. Geological Survey of South Australia Palaeontological Report 1987/57 (unpublished). Alley, N.F., 1988. Age and correlation of palynofloras from the type Cadna-owie Formation, southwestern Eromanga Basin. Memoir of the Association of Australasian Palaeontologists 5: 187-194. Alley, N.F., 1989. Palynological dating and correlation of Tertiary sediments in the Freeling area. Geological Survey of South Australia Palaeontological Report 1989/57 (unpublished). Alley, N.F., 1993. Palynological dating of borehole samples from the Polda Basin area, Eyre Peninsula. Geological Survey of South Australia Report Book 93/2 (unpublished). Alley, N.F., 1998. Cainozoic stratigraphy, palaeoenvironments and geological evolution of the Lake Eyre Basin. Palaeogeography, Palaeoclimatology, Palaeoecology 144: 239- 263. Alley, N.F. and Beecroft, A., 1993. Foraminiferal and palynological evidence from the Pidinga Formation and its bearing on Eocene sea level events and palaeochannel activity, eastern Eucla Basin, South Australia. Memoir of the Association of Australasian Palaeontologists 15: 375-393. Alley, N.F. and Benbow, M.C., 1989. Late Eocene palynofloras from the Pidinga Formation, SADME Ooldea Range 6, eastern Eucla Basin. Geological Survey of South Australia Quarterly Geological Notes 11: 2-12. Alley, N.F. and Broadbridge, L.M., 1992. Middle Eocene palynofloras from the One Tree Hill area, St. Vincent Basin, South Australia. Alcheringa 16: 241-267. 123
Alley, N.F. and Clarke, J.D.A., 1992. Stratigraphy and palynology of Mesozoic sediments from the Great Australian Bight area, southern Australia. BMR Journal of Geology and Geophysics 13: 113-129. Alley, N.F., Benbow, M.C. and Krieg, G.W., 1996. Dating and correlation of Early Cretaceous drillhole samples, southwestern South Australia. Geological Survey of South Australia Quarterly Geological Notes 129: 2-9. Alley, N.F., Kreig, G.W. and Callen, R.A., 1996. Early Tertiary Eyre Formation, lower Nelly Creek, southern Lake Eyre Basin, Australia: palynological dating of macrofloras and silcrete, and palaeoclimatic interpretations. Australian Journal of Earth Sciences 43: 71-84. Alley, N.F., Clarke, J.D.A., Macphail, M. and Truswell, E.M., 1999. Sedimentary infillings and development of major Tertiary palaeodrainage systems of south-central Australia. Special Publications of the International Society of Sedimentologists 27: 337-366. Anand, R.R., 1997. Distribution, classification and evolution of ferruginous materials over greenstones on the Yilgarn Craton – implications for mineral exploration. Geological Society of Australia Special Publication 20: 175-193. Anand, R.R., Smith, R.E. and Robertson, I.D.M., 1994. Classification and origins of laterites and ferruginous regolith materials in the Yilgarn Craton, Western Australia. Australian Geological Survey Record 1994/56: 2-3. Andreasson, F.P. and Schmitz, B., 2000. Temperature seasonality in the early middle Eocene North Atlantic region: evidence from stable isotope profiles of marine gastropod shells. Geological Society of America Bulletin 112: 628-640. Apthorpe, M., 1988. Cainozoic depositional history of the North West Shelf. In: P.G. Purcell and R.R. Purcell (Editors), The North West Shelf Australia. Petroleum Exploration Society of Australia, Perth, pp. 55-84. Arakel, A.V., 1991. Evolution of Quaternary duricrusts in Karinga Creek drainage system, central Australian groundwater discharge zone. Australian Journal of Earth Sciences 38: 333-347. Archangelsky, A., Andreis, R.R., Archangelsky, S. and Artabe, A., 1995. Cuticular characters adapted to volcanic stress in a new Cretaceous cycad leaf from Patagonia, Argentina. Considerations on the stratigraphy and depositional history of the Baqueró Formation. Review of Palaeobotany and Palynology 89: 213-233. Archer, M., Godthelp, H., Hand, S.J. and Megirian, D., 1989. Fossil mammals of Riversleigh, northeast Queensland: preliminary overview of biostratigraphy, correlation and environmental change. Australian Zoologist 25: 35-69. Archer, M., Hand, S.J. and Godthelp, H., 1994. Patterns in the history of Australia’s mammals and inferences about palaeohabitat. In: R.S. Hill (Editor), History of the Australian Vegetation: Cretaceous to Recent. Cambridge University Press, Cambridge, pp. 80- 103. Archer, M. and Wade, M., 1968. Results of the Ray E. Lemley expeditions. Part 1. The Allingham Formation and a new Pliocene vertebrate fauna from Queensland. Memoirs of the Queensland Museum 17: 379-397. Archibald, J.D., 1996. Fossil evidence for a Late Cretaceous origin of “hoofed” mammals. Science 272: 1150-1153. Arinobu, T., Ishiwatari, R., Kaiho, K. and Lamolda, M.A., 1999. Spike of pyrosynthetic polycyclic aromatic hydrocarbons associated with an abrupt decrease in δ 13 C of a terrestrial biomarker at the Cretaceous-Tertiary boundary at Caravaca, Spain. Geology 27: 723-726. 124
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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
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 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
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2. Officer Basin Dinoflagellates in
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2. TIME SLICE K-2 Age Range: Aptian
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Inferred climate The combined data
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Dettmann et al. (1992) have argued
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3. TIME SLICE K-3 Age Range: Cenoma
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3.2.2 North-East Australia 1. Carpe
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4. TIME SLICE K-4 Age Range: Turoni
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1. Otway Basin Limited data (Macpha
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5. TIME SLICE K-5 Age Range: Early
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Inferred climate The data indicate
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6. TIME SLICE K-6 Age Range: Late C
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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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