OFR 151.pdf - CRC LEME

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Table A (cont.) Biostratigraphy Backhouse 2006 [Albian Gearle Siltstone, southern Carnarvon Basin, Western Australia] Crouch et al. 2001 [PETM event] Jordan and Hill 2002 [Cenozoic plant macrofossil sites in Tasmania] Laurie and Foster 2001 [Mesozoic plant microfossils] Macphail 2002 [Tasmanian Offshore Zone, Tasmania] Macphail, 2004a [palynostratigraphic data, Denmark and Bremer Sub-basins, SW Western Australia] Macphail, 2004b [palynostratigraphic data, St. George Basin, SE Queensland] Monteil et al. 2004 [palynostratigraphic data, Otway Basin] Oosting 2004 [Barremian-Aptian dinoflagellates] Oosting et al. 2006 [interhemispheric correlation of Barremian-Aptian dinocyst assemblages] Partridge et al. 2003 [palynostratigraphic data, offshore Tasmania] Quilty 2001 [Australia-Antarctic correlation] Sajjadi and Playford 2002a [Late Jurassic-earliest Cretaceous palynostratigraphy, Eromanga Basin, Queensland] Sajjadi and Playford 2002b [Late Jurassic-earliest Cretaceous palynostratigraphy, Eromanga Basin, Queensland Sinclair and Monteil 2004 [palynostratigraphic data, Otway Basin] Taylor and Haig 2001 [Barremian foraminifera, Carnarvon Basin, Western Australia] Tosolini et al. 2002 [correlation using Early Cretaceous megaspore assemblages] Williams et al. 2004 [Late Cretaceous-Neogene dinocyst events in the Southern Ocean] Palaeobotany, palaeontology, palaeoecology Archer et al. 2001 [vertebrate palaeoecology] Barnes et al. 2001 [Tertiary Cunoniaceae] Brooks et al 2003 [long term control on floodplain vegetation] Burslem et al. 2001 [diversity of modern rainforests] Carpenter et al. 2004 [Early Eocene flora, Mt. Hotham, eastern Victoria] Dettmann and Clifford 2002 [Tertiary Anacardiaceae] Dettmann and Clifford 2003 [Miocene flora, Bundaberg Trough, SE Queensland] Greenwood et al. 2001 [Tertiary Banksia, central Australia] Hill 2001 [Nothofagus evolution and palaeoecology] Hill and Brodribb 2001 [onset of xeromorphy in the Casuarinaceae and Banksieae] Hill and Paull 2003 [Tertiary Cupressaceae in Tasmania] Hill and Whang 2000 [Miocene Podocarpaceae] Hocknall 2005 [Late Cenozoic faunas, Queensland] Itzstein-Davey 2004 [Late Eocene Proteaceae] Levin 2004 [ecological speciation] Mackensen et al. 2003 [decomposition rates of woody detritus] Macphail and Hill 2001 [Australian Tertiary Mimosaceae] Macphail and Hill 2002 [Poaceae] Martin 2001 [Tertiary Convolvulaceae] Martin 2002 [Tertiary Malpighiaceae] Martin 2003 [Tertiary Onagraceae] McLaughlin 2001 [floristic impact of the break-up of Gondwana] Morley 2000 [evolution of tropical and paratropical rainforests] Piper et al. 2006 [Mesozoic-Early Quaternary mammal faunas of Victoria] Poole 2002 [Cretaceous-Tertiary Nothofagus] Read et al. 2005 [phytogeography and climatic analysis of Nothofagus subgenus Brassospora] Roshier et al. 2001 [temporary wetlands in arid Australia] Sniderman et al. 2003 [Plio-Pleistocene vegetation, Central Highlands, Victoria] Swenson et al. 2001 [Nothofagus biogeography] Wignell 2001 [volcanism and wildfires] 9
Figure A: Generalised climatic curve of the Cretaceous and Palaeogene derived from deep-sea oxygen isotope data (from Zachos et al. 2001). Note: Gradstien and Ogg. 2004. have shifted the age ranges some stages. 10
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: Table A (cont.) Basin and related s
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
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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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in the Bass Basin, the basal Seaspr
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Similarly it is difficult to summar
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However, the data are emphatic that
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margin of plateau were cooler (~7 0
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fossil taxa that are morphologicall
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during Late Pleistocene glacial max
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SECTION 8 (CONCLUSIONS) Climatic in
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• On present indications, Early C
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TABLE 8a: INFERRED CRETACEOUS PALAE
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8.2 Results in prospect (recommenda
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The 10 μm sieved, oxidised extract
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phenology. The method also provides
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SECTION 9 (REFERENCES) Acton, G.D.
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Ashley, P.M., Duncan, R.A. and Feeb
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Birks, H.J.B. and Gordon, A.D., 198
Page 130 and 131:
Burnham, R.J., 1989. Relationships
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Clarke, J.D.A., 1994. Evolution of
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Dettmann, M.E. and Playford, G., 19
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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
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Hill, R.S., 1994b. Nothofagus smith
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Holland, S.M. and Patzkowsky, M.E.,
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Australia: paleoceanographic implic
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Lindsay, J.M. and Harris, W.K., 196
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Macphail, M.K., Colhoun, E.A. and F
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McGowran, B. and Beecroft, A., 1985
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Morgan, R., 1977. Palynology of Ter
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Abstracts of the Annual General Mee
Page 158 and 159:
Raymo, M.E., Grant, B., Horowitz, M
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Sereno, P.C., 1999. The evolution o
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Taylor, G., 1998. Prediction of mod
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Webb, L.G., 1968. Environmental rel
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Zachos, J.C., Stott, L.D. and Lohma
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APPENDIX 1 CRETACEOUS DATA 167
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1. TIME SLICE K-1 Age Range: Berria
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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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