CSIRO Publishing Books Journals About Us Shopping Cart You are here: Journals > Australian Systematic Botany   
Australian Systematic Botany
  Taxonomy, Biogeography & Evolution of Plants
 
Search
 
 
  Advanced Search
   

Journal Home
About the Journal
Editorial Board
Contacts
Content
Current Issue
Just Accepted
All Issues
Special Issues
LAS Johnson Review Series
Sample Issue
For Authors
General Information
Notice to Authors
Submit Article
Open Access
For Referees
General Information
Review Article
Annual Referee Index
For Subscribers
Subscription Prices
Customer Service
Print Publication Dates

 Early Alert
Subscribe to our email Early Alert or RSS feeds for the latest journal papers.

 Brunonia
Brunonia, the predecessor journal to Australian Systematic Botany, is available online.

 Connect with us
facebook   youtube

 

Article << Previous     |     Next >>   Contents Vol 13(3)

Eucryphia (Cunoniaceae) reproductive and leaf macrofossils from Australian cainozoic sediments

Richard W. Barnes and Gregory J. Jordan

Australian Systematic Botany 13(3) 373 - 394

Abstract

The first fossil capsule of Eucryphia,E. reticulata R.W.Barnes & G.J.Jord. sp. nov.,is described from Lea River (Early Oligocene), and, like capsules of the twoextant South American species of E. glutinosa (Poepp. etEndl.) Baill. and E. cordifolia Cav., is large and has arelatively large number of valves. The capsule occurs with aEucryphia leaf macrofossil that was probably a leaflet from a compound leaf as it is highly falcate. The leaflet may be derived fromthe same parent plant as E. reticulata but in theabsence of an organic connection it is described as a new species,E. leaensis R.W.Barnes & G.J.Jord. sp. nov.Additional leaf macrofossil specimens of E. aberensisR.S.Hill from the type locality (Loch Aber; Middle–Late Eocene) and anew locality record for the species, Little Rapid River (Early Oligocene),indicate that the species had compound leaves formed by serrate and entiremargin leaflets. Another incomplete Eucryphia capsuleoccurs at Little Rapid River (Early Oligocene) but it is too poorly preservedto assign it to an extant or extinct species. It may be derived from the sameparent plant asE. aberensis, with which it occurs, but cannot be confirmed as there is no organic connection. A new leaf macrofossil with serrate margins, E. mucronata R.W.Barnes & G.J.Jord. sp. nov., is also described from ?Latest Eocene–EarlyOligocene sediments at Wilson’s Creek, central Tasmania. Leafmacrofossils previously assigned to E. aff.milliganii from Early Pleistocene sediments at RegattaPoint in western Tasmania are shown to be conspecific with the two extant Tasmanian species, E. lucida (Labill.) Baill. andE. milliganii Hook.f. ssp.milliganii on the basis of foliar hair distribution patterns and density. The oldest fossil Eucryphiaspecies, E. falcata R.S. Hill (Lake Bungarby; LatePaleocene), had compound leaves formed by leaflets with serrate margins, whichis possibly the plesiomorphic condition for all Cunoniaceae genera. WithinEucryphia, there has been an evolutionary trend towardssimple leaves with entire margins and well-developed peltiform cuticular extensions.



Full text doi:10.1071/SB99004

© CSIRO 2000

 
PDF (1.9 MB) $40
 Export Citation
 Print
  
  
Subscriber Login
Username:
Password:  

    


 
Top  Email this page
 
Legal & Privacy | Contact Us | Help

CSIRO

© CSIRO 1996-2012