Abstract:The Single Stage AMS radiocarbon facility at the Australian National University has operated for the past 14 years. This paper presents the pretreatment methods used for the major sample types dated and reflects on whether quality assurance protocols can adequately detect altered materials. The majority of fossil samples dated by the facility are from tropical and arid environments where diagenesis of both organic samples and carbonates is often severe. A large proportion of the samples submitted cannot be dat… Show more
“…Pretreatment of charcoal at the ANU Radiocarbon Centre 53 consisted of physical cleaning with a scalpel followed by Acid-Base-Acid (ABA) chemical treatment: The samples were washed in hot HCl, rinsed and treated with multiple hot NaOH washes, then the NaOH insoluble fraction was treated with hot HCl, filtered, rinsed, and dried. After each treatment samples were rinsed in ultrapure water at least three times or until the water remains colourless.…”
Archaeological evidence attests multiple early dispersals of Homo sapiens out of Africa, but genetic evidence points to the primacy of a single dispersal 70-40 ka. Laili in Timor-Leste is on the southern dispersal route between Eurasia and Australasia and has the earliest record of human occupation in the eastern Wallacean archipelago. New evidence from the site shows that, unusually in the region, sediment accumulated in the shelter without human occupation, in the window 59–54 ka. This was followed by an abrupt onset of intensive human habitation beginning ~44 ka. The initial occupation is distinctive from overlying layers in the aquatic focus of faunal exploitation, while it has similarities in material culture to other early Homo sapiens sites in Wallacea. We suggest that the intensive early occupation at Laili represents a colonisation phase, which may have overwhelmed previous human dispersals in this part of the world.
“…Pretreatment of charcoal at the ANU Radiocarbon Centre 53 consisted of physical cleaning with a scalpel followed by Acid-Base-Acid (ABA) chemical treatment: The samples were washed in hot HCl, rinsed and treated with multiple hot NaOH washes, then the NaOH insoluble fraction was treated with hot HCl, filtered, rinsed, and dried. After each treatment samples were rinsed in ultrapure water at least three times or until the water remains colourless.…”
Archaeological evidence attests multiple early dispersals of Homo sapiens out of Africa, but genetic evidence points to the primacy of a single dispersal 70-40 ka. Laili in Timor-Leste is on the southern dispersal route between Eurasia and Australasia and has the earliest record of human occupation in the eastern Wallacean archipelago. New evidence from the site shows that, unusually in the region, sediment accumulated in the shelter without human occupation, in the window 59–54 ka. This was followed by an abrupt onset of intensive human habitation beginning ~44 ka. The initial occupation is distinctive from overlying layers in the aquatic focus of faunal exploitation, while it has similarities in material culture to other early Homo sapiens sites in Wallacea. We suggest that the intensive early occupation at Laili represents a colonisation phase, which may have overwhelmed previous human dispersals in this part of the world.
“…2 mm using a scalpel, prior to reaction in HCl (1 M, 30 min, 70 o C), NaOH (1M, 30 min, 70 o C, solution changed until it remained colorless) and HCl (1 M, 30 min, 70 o C). Between each treatment, the sample was rinsed 3 times in ultrapure water, or until it remained colorless (Wood et al 2023). After freeze-drying the charcoal was combusted in a sealed quartz tube in the presence of CuO wire and Ag foil.…”
Section: Radiocarbon Datingmentioning
confidence: 99%
“…To assess the cleanliness of the charcoal, the %C was measured volumetrically during collection of the CO 2 gas. Except where the charring temperature is very low, charcoal normally contains >50 %C (Ascough et al 2011;Wood et al 2023). If much lower than this, substantial amounts of clay may be present in the dated sample, potentially affecting the date obtained.…”
Radiocarbon dates on charred plant remains are often used to define the chronology of archives such as lake cores and fluvial sequences. However, charcoal is often older than its depositional context because old-wood can be burnt and a range of transport and storage stages exist between the woodland and stream or lake bed (“inherited age”). In 1978, Blong and Gillespie dated four size fractions of charcoal found floating or saltating in the Macdonald River, Australia. They found larger fragments gave younger age estimates, raising the possibility that taphonomic modifications could help identify the youngest fragments. In 1978 each date required 1000s charcoal fragments. This study returns to a sample from the Macdonald River to date individual charcoal fragments and finds the inherited age may be more than 1700 years (mode 250 years) older than the collection date. Taphonomic factors, e.g., size, shape or fungal infestation cannot identify the youngest fragments. Only two fragments on short-lived materials correctly estimated the date of collection. In SE Australia, this study suggests that wood charcoal will overestimate the age of deposition, taphonomic modifications cannot be used to identify which are youngest, and multiple short-lived materials are required to accurately estimate the deposition age.
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