Issue Date
1983-01-01Keywords
Huon pineStanley River
Lagarostrobos franklinii
Tasmania Australia
Australia
Australasia
Holocene
Cenozoic
Quaternary
wood
geochronology
C 14
carbon
dates
isotopes
radioactive isotopes
absolute age
Metadata
Show full item recordCitation
McPhail, S., Barbetti, M., Francey, R., Bird, T., & Dolezal, J. (1983). 14C variations from Tasmanian trees—preliminary results. Radiocarbon, 25(3), 797-802.Publisher
American Journal of ScienceJournal
RadiocarbonAdditional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
Huon pine is endemic to Tasmania. It has well-defined annual rings, may live for over 2000 years, and is particularly resistant to decay. Celery-top pine has similar characteristics and may live for 800 years. As part of a multi-disciplinary study of these trees and their habitat, a simple wood pretreatment method for isotope analysis is described. The solvent-acid-alkali-acid sequence yields a value of Delta-14C = -16 +/- 6% for AD 1941-45 Huon pine heartwood; Delta-4C for extracts containing various proportions of post-AD 1955 carbon are also presented. Delta-14C measurements on super-canopy and subcanopy leaves from Celery-top pines are compared and used to place an upper limit of 10% on the amount of sub-canopy CO2 assimilated by sapling leaves, originating from decaying litter-mass. 14C ages from well-preserved logs illustrate the potential for a continuous Holocene chronology from 7400 years BP to the present. A 12,000-year-old Celery-top log has also been found.Type
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200006202