A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia

Typescript (photocopy) Thesis (PhD) -- University of Melbourne, School of Botany, 2003 Includes bibliographical references (leaves 255-270) The Late Paleocene (Thanetian, 58-60 Ma) Cambalong Creek macroflora from the Southern Highlands of New South Wales, Australia, represents an angiosperm�dominate...

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Main Author: Vadala, Anthony John.
Format: Doctoral or Postdoctoral Thesis
Language:English
Published: University of Melbourne 2003
Subjects:
Online Access:http://hdl.handle.net/11343/341589
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spelling ftumelbourne:oai:jupiter.its.unimelb.edu.au:11343/341589 2024-06-02T07:58:17+00:00 A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia Vadala, Anthony John. 2003 http://hdl.handle.net/11343/341589 English eng University of Melbourne THSS_b2785584-00001 http://hdl.handle.net/11343/341589 Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works. Plants Fossil -- Australia -- New South Wales Paleontology -- Paleocene Paleoclimatology -- Paleocene Angiosperms Southern Highlands (N.S.W.) PhD thesis 2003 ftumelbourne 2024-05-06T11:43:32Z Typescript (photocopy) Thesis (PhD) -- University of Melbourne, School of Botany, 2003 Includes bibliographical references (leaves 255-270) The Late Paleocene (Thanetian, 58-60 Ma) Cambalong Creek macroflora from the Southern Highlands of New South Wales, Australia, represents an angiosperm�dominated plant community growing at relatively high palaeolatitude (55-60�S) from a period experiencing global transition from conifer- to angiosperm-dominance. This period saw the earliest stages of separation of Australia from Antarctica, and the commencement of significant climatic and tectonic changes around Australia that contrasted with the relative climatic and tectonic stability of the Senonian-Early Paleocene. Fossils were identified primarily on the basis of cuticle morphology, and most taxa belong to families Cunoniaceae, Elaeocarpaceae, Proteaceae, Araucariaceae, Cupressaceae and Podocarpaceae that are either restricted to, or have greatest extant diversity in, the Southern Hemisphere. Many represent extinct branches of larger extant groups, and have suites of cuticle characters intermediate between those of the fossil and extant species to which they are most closely similar. Angiosperms comprise 65.6% of taxa in the macroflora. The largest single component is Lauraceae, constituting 25% of total taxa and 59.9% of total specimens. The eight species described include representatives of Beilschmiedia, Cryptocarya, Endiandra and Litsea, all of which are extant in Australia but have their largest centres of diversity in warm temperate habitats across Malesia and southeast Asia and Europe. Proteaceae, which have their highest extant diversity in the Southern Hemisphere, comprise 18.8 % of taxa in the macroflora, and include forms with affinities to five of the six extant tribes of subfamily Grevilleoideae: Banksieae, Embothrieae, Helicieae, Knightieae and Oriteae. These include 'sclerophyllous' forms related to Banksieae (Banksia and Dryandra), that are major components of the modern sclerophyllous flora of ... Doctoral or Postdoctoral Thesis Antarc* Antarctica The University of Melbourne: Digital Repository
institution Open Polar
collection The University of Melbourne: Digital Repository
op_collection_id ftumelbourne
language English
topic Plants
Fossil -- Australia -- New South Wales
Paleontology -- Paleocene
Paleoclimatology -- Paleocene
Angiosperms
Southern Highlands (N.S.W.)
spellingShingle Plants
Fossil -- Australia -- New South Wales
Paleontology -- Paleocene
Paleoclimatology -- Paleocene
Angiosperms
Southern Highlands (N.S.W.)
Vadala, Anthony John.
A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
topic_facet Plants
Fossil -- Australia -- New South Wales
Paleontology -- Paleocene
Paleoclimatology -- Paleocene
Angiosperms
Southern Highlands (N.S.W.)
description Typescript (photocopy) Thesis (PhD) -- University of Melbourne, School of Botany, 2003 Includes bibliographical references (leaves 255-270) The Late Paleocene (Thanetian, 58-60 Ma) Cambalong Creek macroflora from the Southern Highlands of New South Wales, Australia, represents an angiosperm�dominated plant community growing at relatively high palaeolatitude (55-60�S) from a period experiencing global transition from conifer- to angiosperm-dominance. This period saw the earliest stages of separation of Australia from Antarctica, and the commencement of significant climatic and tectonic changes around Australia that contrasted with the relative climatic and tectonic stability of the Senonian-Early Paleocene. Fossils were identified primarily on the basis of cuticle morphology, and most taxa belong to families Cunoniaceae, Elaeocarpaceae, Proteaceae, Araucariaceae, Cupressaceae and Podocarpaceae that are either restricted to, or have greatest extant diversity in, the Southern Hemisphere. Many represent extinct branches of larger extant groups, and have suites of cuticle characters intermediate between those of the fossil and extant species to which they are most closely similar. Angiosperms comprise 65.6% of taxa in the macroflora. The largest single component is Lauraceae, constituting 25% of total taxa and 59.9% of total specimens. The eight species described include representatives of Beilschmiedia, Cryptocarya, Endiandra and Litsea, all of which are extant in Australia but have their largest centres of diversity in warm temperate habitats across Malesia and southeast Asia and Europe. Proteaceae, which have their highest extant diversity in the Southern Hemisphere, comprise 18.8 % of taxa in the macroflora, and include forms with affinities to five of the six extant tribes of subfamily Grevilleoideae: Banksieae, Embothrieae, Helicieae, Knightieae and Oriteae. These include 'sclerophyllous' forms related to Banksieae (Banksia and Dryandra), that are major components of the modern sclerophyllous flora of ...
format Doctoral or Postdoctoral Thesis
author Vadala, Anthony John.
author_facet Vadala, Anthony John.
author_sort Vadala, Anthony John.
title A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
title_short A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
title_full A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
title_fullStr A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
title_full_unstemmed A late paleocene (early paleogene) leaf flora from Cambalong Creek, Southern Highlands, New South Wales, Australia
title_sort late paleocene (early paleogene) leaf flora from cambalong creek, southern highlands, new south wales, australia
publisher University of Melbourne
publishDate 2003
url http://hdl.handle.net/11343/341589
genre Antarc*
Antarctica
genre_facet Antarc*
Antarctica
op_relation THSS_b2785584-00001
http://hdl.handle.net/11343/341589
op_rights Copyright in works deposited in Minerva Access is retained by the copyright owner. The work may not be altered without permission from the copyright owner. Readers may only download, print and save electronic copies of whole works for their own personal non-commercial use. Any use that exceeds these limits requires permission from the copyright owner. Attribution is essential when quoting or paraphrasing from these works.
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