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    <title>UTas ePrints - Evidence of Pleistocene plant extinction and diversity from Regatta Point, western Tasmania, Australia</title>
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    <meta content="Jordan, Gregory J." name="eprints.creators_name" />
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<meta content="Evidence of Pleistocene plant extinction and diversity from Regatta Point, western Tasmania, Australia" name="eprints.title" />
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<meta content="The Early Pleistocene Regatta Point sediments contain macrofossils that suggest that generic and specific rainforest diversity was higher in the region than it is today both locally and regionally, but the diversity was probably lower than it was for most of the Tertiary.  The sediments contain extinct species of conifers and angiosperms which have closest living relatives in a wide range of environments, mainly wet forests of warmer areas than western Tasmania, but also relatively cool and dry areas.  Simple models of climatically driven extinction explain these extinctions poorly.  It is more likely that there was a wide range of causes of extinctions.  New species, Acacia bulbosa, Rubus nebuloides, Quintinia tasmanensis, Oxylobium pungens, Laurophyllum australum and Myrtaceaephyllum pleistocenicum, are described." name="eprints.abstract" />
<meta content="1997-01" name="eprints.date" />
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<meta content="Augustinus PC, Macphail MK, Pollington MJ. in press.  Early Pleistocene stratigraphy and timing of the Bulgobac Glaciation, western Tasmania, Australia.  Palaeogeography, Palaeoclimatology, Palaeoecology.
Buchanan AM.  1995.  A census of the vascular plants of Tasmania.  Tasmanian Herbarium Occasional Papers 5.
Carpenter RJ, Hill RS, Jordan GJ.  1994.  Cenozoic vegetation in Tasmania: macrofossil evidence.  In: Hill RS, ed.  History of Australian Vegetation. Cretaceous to Recent.   Cambridge: Cambridge University Press, 189-261.
Carpenter RJ, Horwitz P.  1988.  Leaf litter in two southern Tasmanian creeks and its relevance to palaeobotany.  Papers and Proceedings of the Royal Society of Tasmania 122: 39-45
Christophel DC.  1994.  The early Tertiary macrofloras of continental Australia.  Evidence from spores and pollen.  In: Hill RS, ed.  History of Australian Vegetation. Cretaceous to Recent.   Cambridge: Cambridge University Press, 262-275.
Christophel DC, Lys SD.  1986.  Mummified leaves of two new species of Myrtaceae from the Eocene of Victoria, Australia.  Australian Journal of Botany 34: 649-692.
Colhoun EA, van der Geer G, Hill RS, Bird T.  1989.  Interglacial pollen and plant macrofossils from Langdon River, western Tasmania.  New Phytologist 111: 531-548.
Couper RA, McQueen DR. 1954. Pliocene and Pleistocene plant fossils of New Zealand and their climatic interpretation. New Zealand Journal of Science and Technology: 35, 398-420.
Crisp MD, Weston PH.  1987.  Cladistics and legume systematics, with an analysis of the Bossiaeae, Brongniartineae and Mirbelieae.  In: Stirton CH ed.  Advances in Legume Systematics, Part 3.   Kew: Royal Botanic Gardens, 65-130.
Currie DJ.  1991.  Energy and large-scale patterns of animal and plant species richness.  American Naturalist 137: 27-49.
Currie DJ, Paquin V.  1987.  Large-scale biogeographical patterns of species richness of trees.  Nature 329: 326-327.
Fitzsimons SJ, Colhoun EA.  1991.  Pleistocene glaciation of the King Valley, western Tasmania, Australia.  Quaternary Research 36: 135-156.
Fitzsimons SJ, Colhoun EA, van der Geer G, Hill RS.  1990.  Definition and character of the Regency Interglacial and Early-Middle Pleistocene stratigraphy in the King Valley, western Tasmania, Australia.  Boreas 19: 1-15.
George AS.  1981.  The genus Banksia L.f. (Proteaceae).  Nuytsia 3: 239-473.
Harland WB, Armstrong RL, Cox AV, Craig LE, Smith AG, Smith DG.  1990.  A Geologic Time Scale 1989.   New York: Cambridge University Press.
Hill RS.  1986.  Lauraceae leaves from the Eocene of Nerriga, New South Wales.  Alcheringa 10: 327-352.
Hill RS, Gibson N.  1986.  Distribution of potential macrofossils in Lake Dobson, Tasmania.  Journal of Ecology 74: 373-384.
Hill RS, Jordan GJ, Carpenter RS. 1993.  Tertiary macrofossils of the Taxodiaceae from Tasmania.  Australian Journal of Botany 6: 237-249.
Hill RS, Macphail MK.  1985.  A fossil flora from rafted Plio-Pleistocene mudstones at Regatta Point, Tasmania.  Australian Journal of Botany 33: 497-517.
Hill RS, Read J. 1987.  Endemism in Tasmanian cool temperate rainforest: alternative hypotheses.  Botanical Journal of the Linnean Society 95: 113-124.
Hnatiuk RJ.  1990.  Census of Australian Vascular Plants.  Australian Flora and Fauna Series.  No. 11.  Canberra: Australian Government Publishing Service.
Jarman SJ, Brown MJ, Kantvilas, G.  1984.  Rainforest in Tasmania.  Hobart: National Parks and Wildlife Service.
Jordan GJ.  1992.  Macrofossil Evidence for Quaternary Plant Extinction and Vegetation Change in Western Tasmania.  PhD. thesis, University of Tasmania, Australia.
Jordan GJ. 1995a.  Early-Middle Pleistocene leaves of extinct and extant Proteaceae from western Tasmania, Australia.  Botanical Journal of the Linnean Society 118: 19-35.
Jordan GJ.  1995b.  Extinct conifers and conifer diversity in the Early Pleistocene of western Tasmania.  Review of Palaeobotany and Palynology 84: 375-387.
Jordan GJ.  in press.  Contrasts between the climatic ranges of fossil and extant taxa: causes and consequences for palaeoclimatic estimates.  Australian Journal of Botany
Jordan GJ, Carpenter RJ, Hill RS.  1991.  Late Pleistocene vegetation and climate near Melaleuca Inlet, south-western Tasmania.  Australian Journal of Botany 39: 315-333.
Jordan GJ, Dalton PJ.  1995.  Mosses from Early-?Middle Pleistocene sediments in Western Tasmania.  Alcheringa 19: 291-296.
Jordan GJ, Hill RS.  1991.  Two new Banksia species from Pleistocene sediments in Western Tasmania.  Australian Systematic Botany 4: 499-511.
Jordan GJ, Hill RS.  1994.  Past and present variability in leaf length of evergreen members of Nothofagus subgenus Lophozonia related to ecology and populations dynamics.  New Phytologist 127: 377-390.
Jordan GJ, Hill RS.  1996.  The fossil record of the Epacridaceae.  Annals of Botany 77: 341-346.
Jordan GJ, Macphail MK, Barnes R, Hill RS.  1995.  An Early-Middle Pleistocene flora of subalpine affinities in lowland western Tasmania. Australian Journal of Botany 43: 231-242.
Kalkmann C.  1993.  Rosaceae.  In Kalkmann C, Kirkup DW, Nooteboom HP, Stevens PF, Wilde WJJO eds.  Flora Malesiana Series I Vol 11, Part 2.   The Hague: Foundation Flora Malesiana, 227-351.
Kershaw AP.  1984.  Late Cenozoic plant extinctions in Australia.  In Martin PS, Klein RG eds.  Quaternary extinctions : A Prehistoric Revolution.  Tucson: University of Arizona Press, 691-707.
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Kirkpatrick JB, Brown MJ. 1984. A numerical analysis of Tasmanian higher plant endemism. Botanical Journal of the Linnean Society 88: 165-183.
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Macphail MK, Alley N, Truswell EM, Sluiter IR.  1994.  Early Tertiary vegetation: evidence from spores and pollen.  In: Hill RS, ed.  History of Australian Vegetation. Cretaceous to Recent.   Cambridge: Cambridge University Press, 189-261.
Macphail MK, Colhoun EA.  1985.  Late last glacial vegetation, climates and fire activity in southwest Tasmania.  Search 16: 343-348.
Macphail MK, Colhoun EA, Fitzsimons S.  1995.  Key periods in the evolution of the Cenozoic vegetation and flora in western Tasmania.  1: The Late Pliocene.  Australian Journal of Botany43: 505-526.
Macphail MK, Jordan GJ, Hill RS.  1993.  Key periods in the evolution of the Tasmanian Cenozoic vegetation and flora.  1: The Early-Middle Pleistocene.  Australian Journal of Botany 41: 637-707.
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Oliver WRB.  1928.  The flora of the Waipaoa Series (Later Pliocene) of New Zealand.  Transactions of the New Zealand Institute 59: 287-303.
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Stebbins GL.  (1950).  Variation and Evolution in Plants.  New York: Columbia University Press.
Taylor A, Hopper S.  1988.  The Banksia Atlas.  Australian Flora and Fauna Series number 8.  Canberra: Australian Government Publishing Service.
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Wilson KL, Johnson LAS.  1989.  Casuarinaceae.  In: George AS, ed.  Flora of Australia.  Vol. 3.  Canberra: Australian Government Publishing Service, 100-174." name="eprints.referencetext" />
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<meta content="The Early Pleistocene Regatta Point sediments contain macrofossils that suggest that generic and specific rainforest diversity was higher in the region than it is today both locally and regionally, but the diversity was probably lower than it was for most of the Tertiary.  The sediments contain extinct species of conifers and angiosperms which have closest living relatives in a wide range of environments, mainly wet forests of warmer areas than western Tasmania, but also relatively cool and dry areas.  Simple models of climatically driven extinction explain these extinctions poorly.  It is more likely that there was a wide range of causes of extinctions.  New species, Acacia bulbosa, Rubus nebuloides, Quintinia tasmanensis, Oxylobium pungens, Laurophyllum australum and Myrtaceaephyllum pleistocenicum, are described." name="DC.description" />
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    <h1 class="ep_tm_pagetitle">Evidence of Pleistocene plant extinction and diversity from Regatta Point, western Tasmania, Australia</h1>
    <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Jordan, Gregory J.</span> (1997) <xhtml:em>Evidence of Pleistocene plant extinction and diversity from Regatta Point, western Tasmania, Australia.</xhtml:em> Botanical Journal of the Linnean Society, 123 (1). pp. 45-71.</p><p style="margin-bottom: 1em" class="not_ep_block"></p><table style="margin-bottom: 1em" class="not_ep_block"><tr><td valign="top" style="text-align:center"><a href="http://eprints.utas.edu.au/1792/1/RPU_diversity_paper.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" class="ep_doc_icon" border="0" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/1792/1/RPU_diversity_paper.pdf"><span class="ep_document_citation">PDF</span></a> - Full text restricted - Requires a PDF viewer<br />5Mb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input accept-charset="utf-8" value="2269" name="docid" type="hidden" /><div class=""><input value="Request a copy" name="_action_null" class="ep_form_action_button" onclick="return EPJS_button_pushed( '_action_null' )" type="submit" /> </div></form></td></tr></table><p style="margin-bottom: 1em" class="not_ep_block">Official URL: <a href="http://dx.doi.org/10.1006/bojl.1996.0072">http://dx.doi.org/10.1006/bojl.1996.0072</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">The Early Pleistocene Regatta Point sediments contain macrofossils that suggest that generic and specific rainforest diversity was higher in the region than it is today both locally and regionally, but the diversity was probably lower than it was for most of the Tertiary.  The sediments contain extinct species of conifers and angiosperms which have closest living relatives in a wide range of environments, mainly wet forests of warmer areas than western Tasmania, but also relatively cool and dry areas.  Simple models of climatically driven extinction explain these extinctions poorly.  It is more likely that there was a wide range of causes of extinctions.  New species, Acacia bulbosa, Rubus nebuloides, Quintinia tasmanensis, Oxylobium pungens, Laurophyllum australum and Myrtaceaephyllum pleistocenicum, are described.</p></div><table style="margin-bottom: 1em" cellpadding="3" class="not_ep_block" border="0"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Article</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">The definitive version is available online at www.blackwell-synergy.com</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">macrofossils, pollen, spores, Cainozoic, extinction, quaternary, pleistocene, pliocene</td></tr><tr><th valign="top" class="ep_row">Subjects:</th><td valign="top" class="ep_row"><a href="http://eprints.utas.edu.au/view/subjects/270705.html">270000 Biological Sciences &gt; 270700 Ecology and Evolution &gt; 270705 Palaeoecology</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260112.html">260000 Earth Sciences &gt; 260100 Geology &gt; 260112 Palaeontology</a><br /><a href="http://eprints.utas.edu.au/view/subjects/270401.html">270000 Biological Sciences &gt; 270400 Botany &gt; 270401 Plant Systematics, Taxonomy and Phylogeny</a><br /><a href="http://eprints.utas.edu.au/view/subjects/270709.html">270000 Biological Sciences &gt; 270700 Ecology and Evolution &gt; 270709 Biogeography</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260113.html">260000 Earth Sciences &gt; 260100 Geology &gt; 260113 Palynology</a></td></tr><tr><th valign="top" class="ep_row">Collections:</th><td valign="top" class="ep_row">UNSPECIFIED</td></tr><tr><th valign="top" class="ep_row">ID Code:</th><td valign="top" class="ep_row">1792</td></tr><tr><th valign="top" class="ep_row">Deposited By:</th><td valign="top" class="ep_row"><span class="ep_name_citation"><span class="person_name">dr gregory j jordan</span></span></td></tr><tr><th valign="top" class="ep_row">Deposited On:</th><td valign="top" class="ep_row">02 Sep 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">11 Feb 2008 10:59</td></tr><tr><th valign="top" class="ep_row">ePrint Statistics:</th><td valign="top" class="ep_row"><a target="ePrintStats" href="/es/index.php?action=show_detail_eprint;id=1792;">View statistics for this ePrint</a></td></tr></table><p align="right">Repository Staff Only: <a href="http://eprints.utas.edu.au/cgi/users/home?screen=EPrint::View&amp;eprintid=1792">item control page</a></p>
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