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The Radiocarbon Ages of Different Organic Components in the Mires of Eastern Australia

Published online by Cambridge University Press:  15 November 2018

Len Martin
Affiliation:
School of Biological Earth and Environmental Sciences, UNSW Australia, Sydney, NSW2052, Australia
James Goff
Affiliation:
School of Biological Earth and Environmental Sciences, UNSW Australia, Sydney, NSW2052, Australia
Geraldine Jacobsen
Affiliation:
Institute for Environmental Research, The Australian Nuclear Science and Technology Organisation, Locked Bag 2001, Kirrawee DC, NSW2232, Australia
Scott Mooney*
Affiliation:
School of Biological Earth and Environmental Sciences, UNSW Australia, Sydney, NSW2052, Australia
*
*Corresponding author. Email: [email protected].

Abstract

Radiocarbon (14C) dating is widely used to determine the age of organic material in palaeoenvironmental research. Here we compare 14C dates (n=17) resulting from macro-charcoal (>250 μm), short-lived plant macrofossils and pollen-rich residues isolated from two mire environments in eastern Australia. In most samples we found that short-lived plant macrofossils were the youngest organic component, the charcoal samples most often fell into the middle and the pollen-rich residues consistently returned older dates than the other samples. Although pollen-rich residues have been widely used for 14C dating in Australasia we suggest some caution in their use, perhaps because in our fire-prone environments these samples often also contain fine charcoal and other oxidative resistant organic matter that is older than the surrounding sediment matrix. The macro-charcoal samples also often returned older calibrated ages compared to short-lived plant macrofossils from the same depth, although this difference was relatively small (<245 years). Our results demonstrate that 14C dating of short-lived plant macrofossils are likely to yield more accurate chronologies and we advocate their routine use in palaeoenvironmental research when they are available.

Type
Research Article
Copyright
© 2018 by the Arizona Board of Regents on behalf of the University of Arizona 

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