2016
DOI: 10.14430/arctic4599
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Dating and Digging Stratified Archaeology in Circumpolar North America: A View from Nunalleq, Southwestern Alaska

Abstract: ABSTRACT. Through the case study of the Thule-era village site of Nunalleq (GDN-248), this paper presents 14 C dating results and perspectives on the issues associated with radiocarbon dating stratified archaeological sites in circumpolar North America. The objective was to investigate relative variation in the 14 C age of ecofacts with the aim of establishing a hierarchy of dating suitability for Nunalleq that could more widely inform 14 C sample selection on archaeological sites across the North American su… Show more

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Cited by 16 publications
(22 citation statements)
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“…Arneborg et al, 1999;Barrett & Richards, 2004;Craig, Bondioli, Fattore, Higham, & Hedges, 2013;Raghavan et al, 2014), local deviations, termed the delta (Δ) R, in the offset between atmospheric 14 C concentrations and the marine radiocarbon reservoir remain a major source of uncertainty that must be included in the calibration of 14 C ages from human and marine faunal skeletal remains (Bronk Ramsey, 2008;Stuiver, 1986). A discussion of ongoing research on this topic is beyond the scope of this paper, but readers are encouraged to see Dyke et al (2018), Krus, Jensen, Hamilton, and Sayle (2019), and Ledger, Forbes, Masson-MacLean, and Knecht (2016) for an Arctic perspective on this issue. In the following section, we elaborate on some of the issues associated with equifinality, and present recently developed areas of research that have potential applications in Arctic archaeology.…”
Section: Challenges and Future Prospects Of Stable Isotope Studies Ofmentioning
confidence: 99%
“…Arneborg et al, 1999;Barrett & Richards, 2004;Craig, Bondioli, Fattore, Higham, & Hedges, 2013;Raghavan et al, 2014), local deviations, termed the delta (Δ) R, in the offset between atmospheric 14 C concentrations and the marine radiocarbon reservoir remain a major source of uncertainty that must be included in the calibration of 14 C ages from human and marine faunal skeletal remains (Bronk Ramsey, 2008;Stuiver, 1986). A discussion of ongoing research on this topic is beyond the scope of this paper, but readers are encouraged to see Dyke et al (2018), Krus, Jensen, Hamilton, and Sayle (2019), and Ledger, Forbes, Masson-MacLean, and Knecht (2016) for an Arctic perspective on this issue. In the following section, we elaborate on some of the issues associated with equifinality, and present recently developed areas of research that have potential applications in Arctic archaeology.…”
Section: Challenges and Future Prospects Of Stable Isotope Studies Ofmentioning
confidence: 99%
“…In 2015, further radiocarbon analyses (15 in total) were undertaken to examine inter-context 14 C age variation of a suite of ecofacts from the terminal occupation levels of Phase II. The results indicated that caribou ( Rangifer tarandus ) bone collagen and seeds from edible berries ( Rubus chamaemorus and Empetrum nigrum ) provided the most consistent age estimates (Ledger et al 2016). The work also confirmed previous observations regarding the MRE associated with bone collagen of marine organisms (e.g., Dumond and Griffin 2002), noted inconsistencies in the ages of grass artifacts, and highlighted wood at the site as being probable driftwood (Ledger et al 2016).…”
Section: Introductionmentioning
confidence: 99%
“…The results indicated that caribou ( Rangifer tarandus ) bone collagen and seeds from edible berries ( Rubus chamaemorus and Empetrum nigrum ) provided the most consistent age estimates (Ledger et al 2016). The work also confirmed previous observations regarding the MRE associated with bone collagen of marine organisms (e.g., Dumond and Griffin 2002), noted inconsistencies in the ages of grass artifacts, and highlighted wood at the site as being probable driftwood (Ledger et al 2016). Assays undertaken on wood, grass, and indeterminable plant remains have therefore been excluded from the current study.…”
Section: Introductionmentioning
confidence: 99%
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