CSIRO Publishing blank image blank image blank image blank imageBooksblank image blank image blank image blank imageJournalsblank image blank image blank image blank imageAbout Usblank image blank image blank image blank imageShopping Cartblank image blank image blank image You are here: Journals > Australian Journal of Botany   
Australian Journal of Botany
Journal Banner
  Southern Hemisphere Botanical Ecosystems
 
blank image Search
 
blank image blank image
blank image
 
  Advanced Search
   

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

blue arrow e-Alerts
blank image
Subscribe to our Email Alert or RSS feeds for the latest journal papers.

red arrow Connect with us
blank image
facebook   youtube

red arrow PrometheusWiki
blank image
PrometheusWiki
Protocols in ecological and environmental plant physiology

 

Article << Previous     |     Next >>   Contents Vol 30(1)

Exine Ultrastructure of Myrtaceous Pollen

PA Gadek and HA Martin

Australian Journal of Botany 30(1) 75 - 86
Published: 1982

Abstract

Exine ultrastructure has been determined by transmission electron microscopy analysis of the grains of a number of species of Myrtaceae, chosen to represent some of the diversity of sculpture and structure that can be observed using light microscopy and scanning electron microscopy. The species all show a typical angiosperm exine differentiation consisting of two chemically different layers, an electron-dense ektexine and a less dense endexine divided by a very thin electron-transparent lamella. They all differ, however, from the typical angiosperm architecture by the presence of a somewhat unstructured, granulate infratectal layer and a granular/alveolate endexinous layer around the pores. Species differences relate to the granulate coiumellate organization of the infractectal layer, the extent or density of tectal perforations and the presence and thickness of a foot layer around the grain.



Full text doi:10.1071/BT9820075

© CSIRO 1982

blank image >
 
PDF (956 KB) $25
 Export Citation
 Print
  
  
Subscriber Login
Username:
Password:  

    
Legal & Privacy | Contact Us | Help

CSIRO

© CSIRO 1996-2013