Development of a Robust 14C Chronology for Lynch's Crater (North Queensland, Australia) Using Different Pretreatment Strategies
Author
Turney, Chris S. M.Bird, M. I.
Fifield, L. K.
Kershaw, A. P.
Cresswell, R. G.
Santos, G. M.
di Tada, M. L.
Hausladen, P. A.
Youping, Z.
Issue Date
2001-01-01Keywords
acid base acid stepped combustionLynch' s Crater
northern Queensland
Queensland Australia
oxidation
sedimentation
sedimentation rates
upper Quaternary
Australia
Australasia
Holocene
Pleistocene
upper Pleistocene
sediments
Cenozoic
Quaternary
methods
C 14
carbon
dates
isotopes
radioactive isotopes
absolute age
Metadata
Show full item recordCitation
Turney, C. S. M., Bird, M. I., Fifield, L. K., Kershaw, A. P., Cresswell, R. G., Santos, G. M., ... & Youping, Z. (2001). Development of a robust 14C chronology for Lynch's Crater (North Queensland, Australia) using different pretreatment strategies. Radiocarbon, 43(1), 45-54.Journal
RadiocarbonAdditional Links
http://radiocarbon.webhost.uits.arizona.edu/Abstract
Lynch's Crater in northeastern Australia provides a long, continuous record of environmental change within the Late Quaternary. Here, we present newly determined radiocarbon ages, using acid-base-acid stepped combustion (ABA-SC) and acid-base-wet oxidation stepped combustion (ABOX-SC) pretreatment strategies. The new results largely confirm the original untreated radiocarbon results for the uppermost 9 m of sediments, (ca. 35 ka BP). Below this depth, result from both pretreatment methods are in stratigraphic agreement and extend the dating of the record from 38 ka BP to about 48 ka BP, although an apparent increased sedimentation rate below 12 m is questionable. The scarcity of "charcoal" in several of the samples raises questions regarding the application of ABOX-SC to lake or swamp sediments, with evidence for contributions from younger, chemically resistant bacterial carbon along with fine "charcoal" in some samples. However, the extent to which this phenomenon is significant to the final age estimate appears to be sample specific, and is probably dependent upon the length of the wet oxidation step in the pretreatment.Type
Articletext
Language
enISSN
0033-8222ae974a485f413a2113503eed53cd6c53
10.1017/S0033822200031611