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- <meta content="Hill, Robert S." name="eprints.creators_name" />
- <meta content="Jordan, Gregory J." name="eprints.creators_name" />
- <meta content="bob.hill@utas.edu.au" name="eprints.creators_id" />
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- <meta content="McCarthy, Patrick M." name="eprints.editors_name" />
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- <meta content="The Fossil Record of Ferns and Fern Allies in Australia" name="eprints.title" />
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- <meta content="260112" name="eprints.subjects" />
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- <meta content="pteridophytes, Australia, palynomorphs, macrofossils, spores, palynology, extinction, evolution" name="eprints.keywords" />
- <meta content="Flora of Australia series is co-published by CSIRO PUBLISHING and the Australian Biological Resources Study." name="eprints.note" />
- <meta content="Chapter Introduction: There is an excellent fossil record of ferns in Australia, and it provides an important source of
- information on the phylogeny and biogeography of living ferns. The most important elements of the
- fossil record are spores, sterile and fertile frond compressions and impressions, and the relatively
- rare but highly informative petrified remains, usually rhizomes and stems. Because ferns are such
- an ancient group of plants, much of the record cannot be applied directly to the extant flora.
- Although this causes problems in interpreting the fossil record, and affinities often remain unclear,
- the record relevant to living taxa is still imposing.
- Pteridophyte spores are well-preserved and frequently seen in a wide range of sediments and are of
- considerable taxonomic significance. Indeed, not only can spore wall ornamentation often be
- observed, ultrastructural features may also be visible. One limit to the taxonomic value of the spore
- record is the considerable convergence in spore morphology and anatomy in fossil and extant
- pteridophytes, especially ferns. The consequent problems with the identification of dispersed fossil
- spores are exacerbated by the frequent loss of the diagnostically important exospore.
- Fragments of vegetative fronds are comparatively uncommon in the fossil record. However, while
- these can sometimes be assigned to genera or families, identification is often impossible, because
- available characters such as frond shape and venation show considerable convergence. Conversely,
- fertile fronds tend to be much more useful, and those with in situ spores are among the most
- confidently and precisely identified of all plant fossils, as well as being useful in confirming or
- disproving the identity of dispersed fossil spores (e.g. Jordan et al., 1996). Tree fern stems and
- rhizomes are beautifully petrified under some special conditions that are still not fully understood
- and these can often be confidently identified.
- In this brief review we concentrate on fossils that bear directly on living ferns and their allies, and
- we provide examples that demonstrate particularly interesting biogeography or palaeoecology.
- While many of the early fern-like fossils appear quite similar to living forms (e.g. Baragwanathia
- W.H.Lang & Cookson and some extant Lycopodium species), these will not be dealt with here
- because they are too remote from the living flora to be significant. Although the dispersed spore
- record is difficult to summarise, we direct interested readers to the review articles of Dettmann
- (1994) and Macphail et al. (1994) on the dispersed spore record and the role of ferns and fern allies
- in the Australian flora over the last 100 million years or so." name="eprints.abstract" />
- <meta content="1998" name="eprints.date" />
- <meta content="published" name="eprints.date_type" />
- <meta content="48" name="eprints.number" />
- <meta content="CSIRO Publishing" name="eprints.publisher" />
- <meta content="Canberra" name="eprints.place_of_pub" />
- <meta content="29-36" name="eprints.pagerange" />
- <meta content="UNSPECIFIED" name="eprints.thesis_type" />
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- <meta content="0643059717" name="eprints.isbn" />
- <meta content="Flora of Australia" name="eprints.book_title" />
- <meta content="http://www.publish.csiro.au/nid/22/sid/6.htm" name="eprints.official_url" />
- <meta content="Balme, B.E. (1995), Fossil in situ spores and pollen grains: an annotated catalogue, Rev. Palaeobot. Palynol. 87: 81-323.
- Blackburn, D.T. & Sluiter, I.R.K. (1994), The Oligo-Miocene coal floras of southeastern Australia, in R.S.Hill (ed.), History of the Australian Vegetation: Cretaceous to Recent, pp. 328-367. Cambridge University Press, Cambridge.
- Carpenter, R.J. (1988), Early Tertiary Tmesipteris (Psilotaceae) macrofossil from Tasmania, Austral. Syst. Bot. 1: 171-176.
- Carpenter, R.J., Hill, R.S. & Jordan, G.J. (1994), Cenozoic vegetation in Tasmania: Macrofossil evidence, in R.S.Hill (ed.), History of Australian Vegetation: Cretaceous to Recent, pp. 276-298. Cambridge University Press, Cambridge,
- Churchill, D.M. (1969), The fossil occurrence of Lygodium in Australia, Neues Jahrb. Geol. Palkontol., Monatsh. 5: 257-265.
- Dettmann, M.E. (1986), Significance of the Cretaceous-Tertiary spore genus Cyatheacidites in tracing the origin and migration of Lophosoria (Filicopsida), Special Pap. Palaeontol. 35: 63-94.
- Dettmann, M.E. (1994), Cretaceous vegetation: the microfossil record, in R.S.Hill (ed.), History of Australian Vegetation: Cretaceous to Recent, pp. 143-170, Cambridge University Press, Cambridge.
- Dettmann, M.E. & Clifford, H.T. (1991) Spore morphology of Anemia, Mohria, and Ceratopteris (Filicales), Amer. J. Bot. 78: 303-325.
- Dettmann, M.E. & Clifford, H.T. (1992), Phylogeny and biogeography of Ruffordia, Mohria and Anemia (Schizaeaceae) and Ceratopteris (Pteridaceae): evidence from in situ and dispersed spores, Alcheringa 16: 269-314.
- Drinnan, A.N. & Chambers, T.C. (1986), Flora of the lower Cretaceous Koonwarra Fossil Bed (Korumburra Group), South Gippsland, Victoria, in P.A.Jell & J.Roberts (eds), Plants and Invertebrates from the Lower Cretaceous Koonwarra Fossil Bed, South Gippsland, Victoria, Mem. Assoc. Australas. Palaeontologists 3: 1-72.
- Gould, R.E. (1970), Palaeosmunda, a new genus of siphonostelic osmundaceous trunks from the Upper Permian of Queensland, Palaeontology 13: 10-28.
- Gould, R.E. (1972), Cibotium tasmanense sp. nov., a fossil tree-fern from the Tertiary of Tasmania, Austral. J. Bot. 20: 119-126.
- Hill, R.S. (1987), Tertiary Isoëtes from Tasmania, Alcheringa 12: 157-162.
- Hill, R.S., Forsyth, S.M. & Green, F. (1989), A new genus of osmundaceous stem from the Upper Triassic of Tasmania, Palaeontology 32: 287-296.
- Jordan, G.J. (1992), Macrofossil evidence for Quaternary Plant Extinction and Vegetation Change in Western Tasmania. Unpublished Ph.D. thesis, University of Tasmania, Hobart.
- Jordan, G.J., Carpenter, R.J. & Hill, R.S. (1991), Late Pleistocene vegetation and climate near Melaleuca Inlet, south-western Tasmania, Austral. J. Bot. 39: 499-511.
- Jordan G.J., Macphail, M.K., Barnes, R. & Hill, R.S. (1995), An Early-Middle Pleistocene flora of subalpine affinities in lowland western Tasmania, Austral. J. Bot. 43: 231-242.
- Jordan, G.J., Macphail, M.K. & Hill, R.S. (1996), A fertile pinnule fragment with spores of Dicksonia from Early Oligocene sediments in Tasmania, Rev. Palaeobot. Palynol. 92: 245-252.
- Macphail, M.K., Alley, N.F., Truswell, E.M. & Sluiter, I.R.K. (1994), Early Tertiary vegetation: evidence from spores and pollen, in R.S.Hill (ed.), History of Australian Vegetation: Cretaceous to Recent, pp. 189-261. Cambridge University Press, Cambridge.
- Macphail, M.K., Jordan, G.J. & Hill, R.S. (1993), Key periods in the evolution of the flora and vegetation in western Tasmania I. The Early-Middle Pleistocene, Austral. J. Bot. 41:673-707.
- Neyland, M.G. (1986), Conservation and Management of Tree Ferns. National Parks and Wildlife Service, Hobart.
- Rozefelds, A.C., Christophel, D.C. & Alley, N.F. (1992), Tertiary occurrence of the fern Lygodium (Schizaeaceae) in Australia and New Zealand, Mem. Queensland Museum 32:203-222.
- Tidwell, W.D. (1987), A new species of Osmundacaulis (0. jonesii sp. nov.) from Tasmania, Australia, Rev. Palaeobot. Palynol. 52: 205-216.
- Tidwell, W.D. (1991), Lunea jonesii gen. et sp. nov., a new member of Guaireaceae from the mid-Mesozoic of Tasmania, Australia, Palaeontographica, Abt. B 223: 81-90.
- Tidwell, W.D. (1994), Ashicaulis, a new genus for some species of Millerocaulis (Osmundaceae), Sida 16: 253-261.
- Tidwell, W.D. & Jones, R. (1987), Osmundacaulis nerii, a new osmundaceous species from Tasmania, Australia, Palaeontographica, Abt. B 204: 181-191.
- Tidwell, W.D., Kim, J.-H. & Kimura, T. (1987), Mid-Mesozoic leaves from near Ida Bay, southern Tasmania, Australia, Pap. & Proc. Roy. Soc. Tasmania 121: 159-170.
- Tidwell, W.D., Munzing, G.E. & Banks, M.R. (1991), Millerocaulis species (Osmundaceae) from Tasmania, Australia, Palaeontographica, Abt. B 223: 91-105.
- Tidwell, W.D., Nishida, H. & Webster, N. (1989), Oguracaulis banksii gen. et sp. nov., a mid-Mesozoic tree-fern stem from Tasmania, Australia, Pap. & Proc. Roy. Soc. Tasmania 123: 15-25.
- Tidwell, W.D. & Pigg, K.B. (1993), New species of Osmundacaulis emend. from Tasmania, Australia, Palaeontographica, Abt. B 230: 141-158.
- Tidwell, W.D. & Rozefelds, A.C. (1990), Grammatocaulis donponii gen. et sp. nov., a permineralized fern from the Jurassic of Queensland, Australia, Rev. Palaeobot. Palynol. 66:147-158.
- Tidwell, W.D. & Skog, J.E. (1992), Two new fossil matoniaceous stem genera from Tasmania, Australia, Rev. Palaeobot. Palynol. 70: 263-277.
- Townrow, J.A. (1968), A fossil Selaginella from the Permian of New South Wales, J. Linn. Soc., Bot. 61: 13-23.
- Van Konijnenburg-Van Cittert, J.H.A. (1989), Dicksoniaceous spores from the Jurassic of Yorkshire, England, Rev. Palaeobot. Palynol. 67: 273-301.
- Van Konijnenburg-Van Cittert, J.H.A. (1991), Diversification of spores in fossil and extant Schizaeaceae, Systematics Asociation, Special Vol. 44: 103-118.
- Van Konijnenburg-Van Cittert, J.H.A. (1993), A review of Matoniaceae based on in situ spores, Rev. Palaeobot. Palynol. 78: 235-267.
- " name="eprints.referencetext" />
- <meta content="Hill, Robert S. and Jordan, Gregory J. (1998) The Fossil Record of Ferns and Fern Allies in Australia. In: Flora of Australia. (48). CSIRO Publishing, Canberra, pp. 29-36. ISBN 0643059717" name="eprints.citation" />
- <meta content="http://eprints.utas.edu.au/1809/1/Preprint_of_fern_review.pdf" name="eprints.document_url" />
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- <meta content="The Fossil Record of Ferns and Fern Allies in Australia" name="DC.title" />
- <meta content="Hill, Robert S." name="DC.creator" />
- <meta content="Jordan, Gregory J." name="DC.creator" />
- <meta content="260112 Palaeontology" name="DC.subject" />
- <meta content="270401 Plant Systematics, Taxonomy and Phylogeny" name="DC.subject" />
- <meta content="260113 Palynology" name="DC.subject" />
- <meta content="Chapter Introduction: There is an excellent fossil record of ferns in Australia, and it provides an important source of
- information on the phylogeny and biogeography of living ferns. The most important elements of the
- fossil record are spores, sterile and fertile frond compressions and impressions, and the relatively
- rare but highly informative petrified remains, usually rhizomes and stems. Because ferns are such
- an ancient group of plants, much of the record cannot be applied directly to the extant flora.
- Although this causes problems in interpreting the fossil record, and affinities often remain unclear,
- the record relevant to living taxa is still imposing.
- Pteridophyte spores are well-preserved and frequently seen in a wide range of sediments and are of
- considerable taxonomic significance. Indeed, not only can spore wall ornamentation often be
- observed, ultrastructural features may also be visible. One limit to the taxonomic value of the spore
- record is the considerable convergence in spore morphology and anatomy in fossil and extant
- pteridophytes, especially ferns. The consequent problems with the identification of dispersed fossil
- spores are exacerbated by the frequent loss of the diagnostically important exospore.
- Fragments of vegetative fronds are comparatively uncommon in the fossil record. However, while
- these can sometimes be assigned to genera or families, identification is often impossible, because
- available characters such as frond shape and venation show considerable convergence. Conversely,
- fertile fronds tend to be much more useful, and those with in situ spores are among the most
- confidently and precisely identified of all plant fossils, as well as being useful in confirming or
- disproving the identity of dispersed fossil spores (e.g. Jordan et al., 1996). Tree fern stems and
- rhizomes are beautifully petrified under some special conditions that are still not fully understood
- and these can often be confidently identified.
- In this brief review we concentrate on fossils that bear directly on living ferns and their allies, and
- we provide examples that demonstrate particularly interesting biogeography or palaeoecology.
- While many of the early fern-like fossils appear quite similar to living forms (e.g. Baragwanathia
- W.H.Lang & Cookson and some extant Lycopodium species), these will not be dealt with here
- because they are too remote from the living flora to be significant. Although the dispersed spore
- record is difficult to summarise, we direct interested readers to the review articles of Dettmann
- (1994) and Macphail et al. (1994) on the dispersed spore record and the role of ferns and fern allies
- in the Australian flora over the last 100 million years or so." name="DC.description" />
- <meta content="CSIRO Publishing" name="DC.publisher" />
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- <h1 class="ep_tm_pagetitle">The Fossil Record of Ferns and Fern Allies in Australia</h1>
- <p style="margin-bottom: 1em" class="not_ep_block"><span class="person_name">Hill, Robert S.</span> and <span class="person_name">Jordan, Gregory J.</span> (1998) <xhtml:em>The Fossil Record of Ferns and Fern Allies in Australia.</xhtml:em> In: Flora of Australia. (48). CSIRO Publishing, Canberra, pp. 29-36. ISBN 0643059717</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/1809/1/Preprint_of_fern_review.pdf"><img alt="[img]" src="http://eprints.utas.edu.au/style/images/fileicons/application_pdf.png" border="0" class="ep_doc_icon" /></a></td><td valign="top"><a href="http://eprints.utas.edu.au/1809/1/Preprint_of_fern_review.pdf"><span class="ep_document_citation">PDF (Author Version)</span></a> - Full text restricted - Requires a PDF viewer<br />61Kb</td><td><form method="get" accept-charset="utf-8" action="http://eprints.utas.edu.au/cgi/request_doc"><input value="2285" name="docid" accept-charset="utf-8" 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://www.publish.csiro.au/nid/22/sid/6.htm">http://www.publish.csiro.au/nid/22/sid/6.htm</a></p><div class="not_ep_block"><h2>Abstract</h2><p style="padding-bottom: 16px; text-align: left; margin: 1em auto 0em auto">Chapter Introduction: There is an excellent fossil record of ferns in Australia, and it provides an important source of
- information on the phylogeny and biogeography of living ferns. The most important elements of the
- fossil record are spores, sterile and fertile frond compressions and impressions, and the relatively
- rare but highly informative petrified remains, usually rhizomes and stems. Because ferns are such
- an ancient group of plants, much of the record cannot be applied directly to the extant flora.
- Although this causes problems in interpreting the fossil record, and affinities often remain unclear,
- the record relevant to living taxa is still imposing.
- Pteridophyte spores are well-preserved and frequently seen in a wide range of sediments and are of
- considerable taxonomic significance. Indeed, not only can spore wall ornamentation often be
- observed, ultrastructural features may also be visible. One limit to the taxonomic value of the spore
- record is the considerable convergence in spore morphology and anatomy in fossil and extant
- pteridophytes, especially ferns. The consequent problems with the identification of dispersed fossil
- spores are exacerbated by the frequent loss of the diagnostically important exospore.
- Fragments of vegetative fronds are comparatively uncommon in the fossil record. However, while
- these can sometimes be assigned to genera or families, identification is often impossible, because
- available characters such as frond shape and venation show considerable convergence. Conversely,
- fertile fronds tend to be much more useful, and those with in situ spores are among the most
- confidently and precisely identified of all plant fossils, as well as being useful in confirming or
- disproving the identity of dispersed fossil spores (e.g. Jordan et al., 1996). Tree fern stems and
- rhizomes are beautifully petrified under some special conditions that are still not fully understood
- and these can often be confidently identified.
- In this brief review we concentrate on fossils that bear directly on living ferns and their allies, and
- we provide examples that demonstrate particularly interesting biogeography or palaeoecology.
- While many of the early fern-like fossils appear quite similar to living forms (e.g. Baragwanathia
- W.H.Lang & Cookson and some extant Lycopodium species), these will not be dealt with here
- because they are too remote from the living flora to be significant. Although the dispersed spore
- record is difficult to summarise, we direct interested readers to the review articles of Dettmann
- (1994) and Macphail et al. (1994) on the dispersed spore record and the role of ferns and fern allies
- in the Australian flora over the last 100 million years or so.</p></div><table style="margin-bottom: 1em" border="0" cellpadding="3" class="not_ep_block"><tr><th valign="top" class="ep_row">Item Type:</th><td valign="top" class="ep_row">Book Chapter</td></tr><tr><th valign="top" class="ep_row">Additional Information:</th><td valign="top" class="ep_row">Flora of Australia series is co-published by CSIRO PUBLISHING and the Australian Biological Resources Study.</td></tr><tr><th valign="top" class="ep_row">Keywords:</th><td valign="top" class="ep_row">pteridophytes, Australia, palynomorphs, macrofossils, spores, palynology, extinction, evolution</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/260112.html">260000 Earth Sciences > 260100 Geology > 260112 Palaeontology</a><br /><a href="http://eprints.utas.edu.au/view/subjects/270401.html">270000 Biological Sciences > 270400 Botany > 270401 Plant Systematics, Taxonomy and Phylogeny</a><br /><a href="http://eprints.utas.edu.au/view/subjects/260113.html">260000 Earth Sciences > 260100 Geology > 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">1809</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">10 Sep 2007</td></tr><tr><th valign="top" class="ep_row">Last Modified:</th><td valign="top" class="ep_row">11 Feb 2008 11:02</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=1809;">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&eprintid=1809">item control page</a></p>
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