Radiocarbon Dating of “Old” Charcoal Using a Wet Oxidation, Stepped-Combustion Procedure
Open accessAbstract
We present results that validate a new wet oxidation, stepped-combustion procedure for dating “old” charcoal samples. An acid–base–wet oxidation (ABOX) pretreatment procedure has been developed that is used in place of the conventional acid-base-acid (ABA) pretreatment. Combustions and graphitizations are performed in a vacuum line that is insulated from the atmosphere by a second backing vacuum to eliminate the risk of atmospheric leakage into the line at any stage of the procedure. Combustions are performed at 3 temperatures (330 °, 630 ° and 850 °) with a graphite target produced from the CO2 evolved during each combustion step. In this way, the removal of any contamination can be monitored, and a high degree of confidence can be placed on the final age. The pretreatment, combustion, graphitization, and measurement blank for the procedure, based on the analysis of a “radiocarbon-dead” graphite, is 0.5 ± 0.5 μg C (1σ, n=14), equivalent to 0.04 ± 0.02 pMC or an “age” of approximately 60 ka for a 1 mg graphite target. Analyses of a “radiocarbon-dead” natural charcoal after ABOX pretreatment and stepped combustion suggest that the total blank (including contamination not removed by pretreatment) may be higher than for graphite, ranging up to 0.10 ± 0.02 pMC. Additional experiments confirm good agreement with accepted values for the international low-14C “New Kauri” standard (0.16–0.25 pMC). They also confirm excellent reproducibility, with 3 separate dates on different aliquots of a charcoal sample from Ngarrabullgan Cave (Queensland, Australia) ranging from 35.2 to 35.5 ka 14C BP. It is also demonstrated that the ABOX pretreatment, in conjunction with the new vacuum line described here, is able to remove contamination not removed by the conventional ABA pretreatment, suggesting that the technique can be used to produce reliable 14C dates on charcoal up to at least 50 ka.
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Claims the paper makes
7 of 20 cited sources checked · 1 supported · 1 flagged · accuracy not yet measured
- Premisecitation
Previous studies have demonstrated that the major source of introduced contamination in combustion of samples for 14C analysis comes from the copper oxide used during combustion.
“Previous studies have demonstrated that the major source of introduced contamination in the com- bustion of samples for 14C analysis comes from the copper oxide used during combustion (Vogel et al. 1987;Vandeputte et al. 1998).”
Quote in the paperSubstantial claim1 of 2 sources checked- cites Vogel et al. 1987 source
In “Contamination During Combustion” (page not provided), replacing copper oxide with ultra-pure oxygen produced indistinguishable results, and changing the amount of copper oxide did not change measured ¹⁴C. The paper instead identifies the Vycor combustion tube as the likely source and reports lower background when Pyrex tubes were used. (LLM, conf=0.90)
Checked by a reasoning model — may be wrong.
Experimental — accuracy not yet measured - cites Vandeputte et al. 1998
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
It has been demonstrated that ABA pretreatment does not remove all contaminants.
“However, in some cases it has been demonstrated that the ABA pretreatment does not remove all contaminants (e.g.Gillespie et al. 1992; Gillespie 1.997)”
Quote in the paperSubstantial claim1 of 2 sources checked- cites Gillespie et al. 1992 source
- cites Gillespie 1.997
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
Work by Cachier et al. (1989) has shown that treatment at 330 °C will remove organic contaminants with minimal removal of black carbon from aerosol samples.
“Work by Cachier et al. (1989) has shown that this treatment will remove organic contaminants with minimal removal of black carbon from aerosol samples.”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Cachier et al. (1989) source
Section 3.4 says precombustion removes organic matter while seeking to minimize soot-carbon loss. It specifies 340 °C for two hours—not 330 °C—and estimates a 24% loss of refractory carbon under those conditions, so the claim’s temperature and unqualified description of minimal loss are not supported. (LLM, conf=0.86)
Experimental — accuracy not yet measured
- Findingown data
The ABOX pretreatment, in conjunction with the new vacuum line, is able to remove contamination not removed by conventional ABA pretreatment.
“It is also demonstrated that the ABOX pretreatment, in conjunction with the new vacuum line described here, is able to remove contamination not removed by the conventional ABA pretreatment”
Quote in the paperSubstantial claim - Findingown data
Analyses of a radiocarbon-dead natural charcoal after ABOX pretreatment and stepped combustion suggest that the total blank, including contamination not removed by pretreatment, may be higher than for graphite, ranging up to 0.10 ± 0.02 pMC.
“Analyses of a”
Quote in the paperSubstantial claim
- Findingreasoning
For samples subjected only to acid-base pretreatment, minor contamination is introduced during the initial steps, most likely from adsorption of atmospheric CO2 by the alkaline solution.
“For the samples that were subjected only to an acid-base pretreatment, it is evident that minor contamination is introduced to the sample during these initial steps, most likely from adsorption of atmospheric CO2 by the alkaline solution.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Findingown data
All five Ngarrabullgan samples show a significant shift to older ages from the 330 degrees C to the 630 degrees C step.
“All 5 samples show a significant shift to older ages from the 330 °C to 630 °C step (Table 1 and Fig- ure 6).”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Findingown data
The weighted mean 14C ages of the untreated and ABA pretreated samples across all combustion steps (41.6 and 46.3 ka) are significantly younger at the 2 sigma level than the corresponding weighted mean age of the ABOX pretreated sample (51.3 ka).
“The weighted mean 14C age (equivalent to the age that would have been obtained from complete combustion) of the untreated and ABA pretreated samples for all combustion steps (41.6 and 46.3 ka) are significantly younger at the 26 level than the cone- sponding weighted mean age for the ABOX pretreated sample (51.3 ka).”
Quote in the paperSubstantial claim - Findingown data
Four Ceylon graphite samples that received ABOX treatment before subsampling gave values statistically indistinguishable from the ten samples that received no pretreatment before combustion.
“The values obtained from these 4 samples are statistically indistinguishable from the 10 samples that were not subjected to any pre- treatment prior to combustion.”
Quote in the paperSubstantial claim - Findingcitation
A sample previously analyzed from this deposit after ABOX pretreatment without stepped combustion also returned an age at the upper extreme of the dated sample population (OZC-733, 35.5 ± 0.6 ka).
“A sample previously analyzed from this deposit subjected to the ABOX pretreatment (without stepped combustion) also returned an age at the upper extreme of the dated sample population (OZC-733, 35.5 ± 0.6 ka; Roberts et al. 1994)”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Roberts et al. 1994 source
- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Findingown data
For the homogenized Ngarrabullgan Cave charcoal, the three combustion steps across five pretreatments returned 14C ages from 30.9 to 35.5 ka BP (2.12-1.21 pMC).
“The 3 com- bustion steps for the 5 pretreatments returned 14C ages from 30.9 to 35.5 ka 14C BP (2.12-1.21pMC, Table 1).”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Findingcitation
Pretreated OREC samples were partly susceptible to oxidation during the 330 °C step, probably due to catalysis of the oxidation reaction by residual chromium ions on the sample surface.
“In practice it was found that pretreated OREC samples were partly susceptible to oxidation during this step, probably due to catalysis of the oxidation reaction by residual chromium ions on the sample surface (Mull et a1.1998).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Mull et al. 1998
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Findingown data
There is no obvious correlation between sample weight and measured 14C activity.
“There is, however, no obvious correlation between sample weight and the measured 14C activity (Figure 4)”
Quote in the paperSubstantial claim - Findingown data
The 14C ages of the untreated (50.4 ka) and ABA (52.2 ka) 850 degrees C fractions are younger than the same fraction of the ABOX pretreated sample (55.6 ka).
“The 14C ages of the untreated (50.4 ka) and ABA (52.2 ka) 850 °C fractions are younger than the same fraction of the ABOX pretreated sample (55.6 ka”
Quote in the paperSubstantial claim - Findingcitation
This age is at the upper end of the range of 19 dates on charcoal from this level of the deposit, which range from 28.8 to 34.6 14C ka BP.
“This age is at the upper end of the range of 19 dates on charcoal from this level of the deposit (David et al. 1997), which range from 28.8 to 34.614C ka BR”
Quote in the paperSubstantial claim0 of 1 sources checked- cites David et al. 1997 source
- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Interpretationreasoning
The technique can be used to produce reliable 14C dates on charcoal up to at least 50 ka.
“suggesting that the technique can be used to produce reliable 14C dates on charcoal up to at least 50 ka.”
Quote in the paperSubstantial claim- Rests on an assumption: Oxidation removes less resistant phases first, working progressively from the outside to the interior of the particles.
- Interpretationown data
The stepped-combustion procedure can ensure that blanks are sufficiently low to enable reliable 14C age determinations in the 40-50 ka time range.
“and that the stepped-combustion procedure can ensure that blanks are suf- ficiently low to enable reliable 14C age determinations in the 40-50 ka time range.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- Premisecitation
Bird and Grocke (1997) demonstrated that oxidation for 72 h under the above conditions will remove all organic carbon from the sample, leaving a residue of oxidation resistant elemental carbon (OREC).
“Bird and Grocke (1997) have demonstrated that oxidation for 72 h under the above conditions will remove all organic carbon from the sample, leaving a resi- due of”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Bird and Grocke (1997) source
- Interpretationown data
The results of this study show that these criteria can be met for charcoal, enabling the production of reliable 14C dates in the >40 ka BP range, using a wet oxidation pretreatment protocol and a stepped-combustion procedure.
“The results of this study show that these criteria can be met for charcoal, enabling the production of reliable 14C dates in the >40 ka BP range, using a wet oxidation pretreatment protocol to ensure removal of contaminants, and a stepped-combustion procedure to verify decontamination of the sample.”
Quote in the paperSubstantial claim- The authors state this as an assumption: For a 14C date to be considered reliable at 50 ka, the combined blank from natural contamination and laboratory handling should be equivalent to a 14C age of at least 55 ka.
- Interpretationown data
The New Kauri standard results indicate that the pretreatment procedure does not introduce contaminants.
“The results for the 14C New Kauri standard indicate that the pretreatment procedure does not introduce contaminants.”
Quote in the paperSubstantial claim - Interpretationown data
Diffusion of modern carbon into the silica tubes during combustion does not contribute significantly to the 14C background.
“indicate that diffusion of modern carbon into the tubes during combustion does not contribute significantly to the 14C background.”
Quote in the paperSubstantial claim - Interpretationown data
This study demonstrated that ABOX pretreatment is a reliable technique for removing contaminants from charcoal.
“This study has demonstrated that the ABOX pretreatment is a reliable technique for removing contaminants from charcoal”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- Premisecitation
The Coulter Pedoderm is overlain by alluvial fan gravels stratigraphically equivalent to a valley-fill deposit in an adjacent valley dated by optically stimulated luminescence to greater than 50 ka.
“The unit is overlain by alluvial fan gravels stratigraphically equivalent to a valley-fill deposit in an adjacent valley dated by optically stimulated luminescence (OSL) to greater than 50 ka (T T Barrows and R G Roberts, unpublished data).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites T T Barrows and R G Roberts, unpublished data
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
- Premisecitation
The large difference in ages between the short and long chronologies is unlikely to be explained by disparities resulting from the use of two independent dating techniques, 14C and luminescence, representing two different time clocks.
“The large difference in ages between the short and the long chronologies is unlikely to be explained by any disparities resulting from the use of 2 independent dating techniques-14C and luminescencerepresenting 2 different time”
Quote in the paperSubstantial claim0 of 1 sources checked- cites David et al. 1997 source
- Interpretationown data
For relatively uncontaminated charcoals, the 850 degrees C fraction of step combustion alone can produce a reliable age.
“The results for the step-combusted, untreated sample further suggest that for relatively uncontaminated charcoals, the 850 °C fraction of the step combustion alone can produce a reliable age.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Interpretationreasoning
Producing multiple targets by stepped combustion provides an additional indicator of the reliability of age determinations in the 40-50 ka time range.
“The production of multiple targets by stepped combustion provides an additional indicator of the reliability of age determinations in this time range.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- Interpretationreasoning
The major contribution to reducing the overall blank for charcoal samples in this study comes from the use of stepped combustion, with oxygen as the oxidant at 330 degrees C.
“This suggests that the major contribution to reducing the overall blank for charcoal samples in this study comes from the use of stepped combustion, with oxygen employed as the oxidant at 330 °C.”
Quote in the paperSubstantial claim - Interpretationnone given
The contamination introduced during acid-base pretreatment is removed during the subsequent acid oxidation step of the full ABOX procedure.
“However, this contamination is removed during the subsequent acid oxidation step of the full ABOX procedure.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Interpretationown data
The blank for the ABOX/stepped-combustion procedure applied to charcoal from oxidizing surficial environments may be higher than for a crystalline graphite such as Ceylon graphite.
“The results also suggest that the blank for the ABOXlstepped-combustion procedure applied to charcoal from oxidizing surficial environments may be higher than for a crystalline graphite such as the Ceylon graphite.”
Quote in the paperSubstantial claim - Interpretationreasoning
The ABOX/stepped-combustion procedure consistently removes contaminants that conventional pretreatments do not remove.
“again suggesting that the ABOX/ stepped-combustion procedure consistently removes contaminants not removed by conventional pretreatments.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
- Premisenone given
The problem of ensuring complete removal of contaminants becomes increasingly severe as the age of the sample increases.
“the problem of ensuring the com- plete removal of contaminants becomes increasingly severe as the age of the sample increases.”
Quote in the paperNot a substantial claim - Study design and conductnone given
The Ceylon graphite analyses serve as the combustion, graphitization, and measurement blank for the procedure.
“The analyses of Ceylon graphite (generally 3 tar- gets per analysis) represent the combustion, graphitization, and measurement blank for the proce- dure.”
Quote in the paperSubstantial claim - Interpretationown data
The Black Mountain sample results suggest that both ABOX pretreatment and stepped combustion are required to reduce blanks to a level low enough to allow reliable finite dates on charcoal in the 40-50 ka time range.
“The results for the Black Mountain sample suggest that both the ABOX pretreatment and stepped combustion are required to reduce blanks to a level low enough to allow the measurement of reliable finite dates on charcoal in the 40-50 ka time range.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- May combine two claims. 29
- The quote only partly states this claim. 1
- Classified as probably not a substantial claim. 21
May combine two claims.
Findingown dataThe Ceylon graphite blank is at least an order of magnitude lower than 0.7% modern carbon, equivalent to 40 ka, and is 2-10 times lower than commonly reported procedural blanks.
“This blank is at least an order of magnitude lower than the 0.7% modern carbon that would be equivalent to an age of 40 ka, and is 2-10 times lower than commonly reported procedural blanks (Kitagawa et al. 1993;Vogel et al. 1987;Gagnon and Jones 1993).”
Quote in the paperSubstantial claim3 of 3 sources checked- cites Kitagawa et al. 1993 source
The “14C Background (or Blank) Levels” section (page not provided) reports a procedural background of 0.112 ± 0.057 percent modern carbon, so the paper supplies an example of a blank for comparison. It measures targets made from Yubari Mine coal, not a Ceylon graphite blank, and does not establish either the claimed order-of-magnitude difference from 0.7% or the 2–10-fold comparison. (LLM, conf=0.85)
Experimental — accuracy not yet measured - cites Vogel et al. 1987 source
The Contamination During Graphitization section reports anthracite backgrounds of 0.59 ± 0.24% modern, reduced to 0.44 ± 0.13% modern, providing a procedural-background comparison. It does not state the citing paper’s blank value, the 2–10-fold comparison, or that 0.7% modern is equivalent to 40 ka. (LLM, conf=0.82)
Experimental — accuracy not yet measured - cites Gagnon and Jones 1993 source
The Results report procedural blank values of 0.256% modern carbon for carbonate and 0.762% for organic carbon; the Conclusions equate the latter with about 39 ka, close to the cited 0.7% and 40 ka benchmark. The paper does not report a Ceylon graphite blank or establish that it is an order of magnitude below 0.7% modern carbon or 2–10 times below those procedural blanks. (LLM, conf=0.86)
Experimental — accuracy not yet measured
May combine two claims.
Findingown dataNew Kauri standard results range from 0.16 ± 0.06 pMC to 0.25 ± 0.06 pMC (48-51.7 ka), are internally consistent, and are comparable within error to the accepted range for this standard (0.12-0.21 pMC).
“the results for this standard, which range from 0.16 ± 0.06 pMC to 0.25 ± 0.06 pMC (48-51.7 ka), are internally consistent and comparable within error to the accepted range of values for this standard (0.12-0.21 pMC; Hogg et al. 1995).”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Hogg et al. 1995 source
The Laboratory Analysis section gives the same 0.12–0.21 pMC range for the new kauri standard, but proposes applying it provisionally until unresolved measurement problems are addressed; it does not call it an accepted range. The cited paper does not report the citing authors’ 0.16–0.25 pMC results, which are presented as their own findings. (LLM, conf=0.86)
Experimental — accuracy not yet measured
The quote only partly states this claim.
Findingown dataAdditional experiments confirm good agreement with accepted values for the international low-14C New Kauri standard (0.16-0.25 pMC).
“Additional experiments confirm good agreement with accepted values for the international low-14C”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThe pretreatment, combustion, graphitization, and measurement blank for the procedure, based on analysis of a radiocarbon-dead graphite, is 0.5 ± 0.5 μg C (16, n=14), equivalent to 0.04 ± 0.02 pMC or an age of approximately 60 ka for a 1 mg graphite target.
“The pretreatment, combustion, graphitization, and measurement blank for the procedure, based on the analysis of a”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThree separate dates on different aliquots of a charcoal sample from Ngarrabullgan Cave (Queensland, Australia) range from 35.2 to 35.5 ka 14C BP, confirming excellent reproducibility.
“They also confirm excellent reproducibility, with 3 separate dates on different aliquots of a charcoal sample from Ngarrabullgan Cave (Queen- sland, Australia) ranging from 35.2 to 35.5 ka 14C BP.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataFor ABOX-pretreated Ngarrabullgan samples, consistent and reproducible ages can be obtained from the 850 degrees C fraction, and possibly from the 630 degrees C fraction, but not from the 330 degrees C fraction.
“For ABOX-pretreated samples, the results indicate that consistent, reproducible ages can be obtained from the 850 °C fraction, and possibly from the 630 °C fraction, but not from the 330 °C fraction (Figure 6).”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
May combine two claims.
Findingown dataCalculated blanks above 1 microgram came from the first two Ceylon graphites prepared on the combustion line, and calculated blanks for all later analyses were consistently lower.
“It should also be noted that calculated blanks in excess of 1 µg were from the first 2 Ceylon graphites prepared using the combustion line, and calculated blanks for all subsequent analyses have been consistently lower.”
Quote in the paperNot a substantial claimMay combine two claims.
Findingown dataABOX pretreatment alone does not remove all contamination, because the lower temperature fractions of the step-combusted ABOX pretreated sample have younger 14C ages (37.7 and 51.3 ka) than the 850 degrees C fraction (55.9 ka).
“The ABOX pretreatment alone does not remove all contamination, as the lower temperature fractions of the step-combusted ABOX pretreated sample have younger 14C ages ( 37.7 and 51.3 ka) than the 850 °C fraction (55.9 ka).”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataNo ABA-treated Ngarrabullgan sample was analyzed because the untreated and ABOX-treated results indicate that the sample is virtually uncontaminated.
“No ABA-treated sample was ana- lyzed, as the results from the untreated and ABOX-treated samples indicate that the Ngarrabullgan sample is virtually uncontaminated.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
May combine two claims.
Findingown dataNeither stepped combustion of an unpretreated sample nor ABA pretreatment followed by stepped combustion is sufficient to remove all contaminants.
“Neither the stepped combustion of an unpretreated sample nor an ABA pretreatment with stepped combustion is sufficient to remove all contaminants.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThe Ceylon graphite samples spanned graphite weights from 0.1 to 2.2 mg; the corresponding modern carbon varied from about 0.1 to 1.7 micrograms, with an average of approximately 0.5 ± 0.5 micrograms (1 sigma, n = 14, equivalent to about 60 ka for a 1 mg graphite target).
“The samples spanned a range of graphite weights from 0.1 to 2.2 mg, and the corresponding amount of modern carbon that would account for the observed pMC varies between about 0.1 and 1.7 µg, giving an average of approximately 0.5 ± 0.5 µg (16, n=14, equivalent to -60 ka for a 1 mg graphite target).”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataCeylon graphite combusted for 1 and 5 hours gave 14C ages of 60.7 and 62.4 ka BP (0.05 and 0.04 pMC, respectively), which are statistically indistinguishable.
“The resulting 14C ages of 60.7 and 62.4 ka BP (0.05 and 0.04 pMC, respectively) are statistically indistinguishable”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataAll 14 Ceylon graphite measurements are consistent with a mean of 0.04 pMC (chi-square nu = 1.2), and the standard deviation of the data set is 0.02 pMC.
“All 14 measurements are consistent with the mean value of 0.04 pMC (x2v =1.2) and the stan- dard deviation of the data set is 0.02 pMC (Figure 3).”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Findingown dataIn the case of untreated graphite, very little CO2 was produced in the 330 °C or 630 °C combustion steps, so the 3 targets were made from 3 combustions at 850 °C.
“In the case of untreated graphite, very little CO2 was produced in the 330 °C or 630 °C combustion steps, so the 3 targets were made from 3 combustions at 850 °C (850 I, II, III; Table 1).”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing), S4 (based).
Findingnone givenThe precombustion of the Fe powder does not appear to affect its catalytic action during the conversion of CO2 to graphite.
“The precombustion of the Fe powder does not appear to affect its catalytic action during the conversion of CO2 to graphite.”
Quote in the paperNot a substantial claimMay combine two claims.
Study design and conductreasoningCombustions are performed at 330 °C, 630 °C and 850 °C, with a graphite target produced from the CO2 evolved during each combustion step, allowing removal of contamination to be monitored and a high degree of confidence to be placed on the final age.
“Combustions are performed at 3 temperatures (330 °C, 630 °C and 850 °C) with a graphite target produced from the CO2 evolved during each combustion step.In this way, the removal of any contamination can be monitored, and a high degree of confidence can be placed on the final age.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing), S4 (based). May combine two claims.
Study design and conductnone givenCombustions and graphitizations are performed in a vacuum line insulated from the atmosphere by a second backing vacuum, which eliminates the risk of atmospheric leakage into the line at any stage.
“Combustions and graphitizations are performed in a vacuum line that is insu- lated from the atmosphere by a second backing vacuum to eliminate the risk of atmospheric leakage into the line at any stage of the procedure.”
Quote in the paperNot a substantial claimMay combine two claims.
PremisecitationThe proportion of OREC left after oxidation for 72 h depends on the nature of the charcoal and can range widely from 20 to 80%.
“The proportion of OREC left after oxidation for 72 h depends on the nature of the charcoal and can range widely from 20 to 80%.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Bird and Grocke (1997) source
May combine two claims.
Interpretationnone givenThe Black Mountain charcoal represents a worst case because it is overlain by a vegetated soil profile and has been exposed to infiltrating waters and their organic compounds since sediment deposition and subsequent pedogenesis.
“This sample represents a worst case in that it is overlain by a vegetated soil profile and has been exposed to infiltrating waters and the organic compounds carried by those waters since deposition of the sediments and subsequent pedogenesis.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
PremisecitationA substantial body of dates have been published for the Ngarrabullgan Cave unit, with 19 14C determinations spanning 28.8-34.6 14C ka BP.
“A substantial body of dates have been published for this unit, with 19 14C determinations spanning 28.8-34.614Cka BP (David et al. 1997).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites David et al. 1997 source
Probably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone givenAn additional step in the graphitization procedure is preoxidation of approximately 0.5 to 1.0 mg iron powder to remove carbonaceous contaminants present in the Fe powder or introduced during sample loading.
“An additional step used in our procedure is a preoxidation of approximately 0.5 to 1.0 mg iron pow- der (Merck; 10 µm) to remove carbonaceous contaminants present in the Fe powder, or introduced during the sample loading procedure.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
PremisecitationLuminescence techniques suggested that humans may have arrived in Australia at 54-60 ka BP (the long chronology).
“whereas the advent of luminescence techniques in the 1980s suggested that humans may have arrived at 54-60 ka BP (the”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Roberts et al. 1994 source
Probably not a substantial claim: may not pass S3 (load-bearing), S4 (based).
Premisenone givenCharcoal from Ngarrabullgan Cave has been substantially protected from interaction with infiltrating waters.
“which has been substantially protected from interaction with infiltrating waters (discussed below).”
Quote in the paperNot a substantial claimMay combine two claims.
InterpretationreasoningStepped combustion removes contaminants present in the copper oxide and/or introduced during sample loading, and also removes contamination from samples that ABOX pretreatment did not remove.
“The stepped combustion removes contaminants present in the copper oxide and/or introduced during sample loading, and also removes contamination from samples not removed by the ABOX pretreatment.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S2 (checkable), S4 (based).
Study design and conductnone givenFor a 14C date to be considered reliable, the removal of all contamination must be verifiable.
“and the removal of all contamination must be verifiable.”
Quote in the paperNot a substantial claimMay combine two claims.
Interpretationown dataAlthough total combustion can produce reliable ages on charcoal, the effective limit of the 14C technique will be considerably younger for samples analyzed by total combustion.
“It therefore seems that although total combustion can produce reliable ages on charcoal, the effective limit of the 14C technique will be considerably younger for samples that are analyzed by total combustion.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Interpretationown dataThe few 14C atoms observed may already have been present in the Ceylon graphite itself or may have been added during target pressing.
“suggesting that the few '4C atoms observed may already be present in the Ceylon graphite itself or were possibly added during target pressing.”
Quote in the paperNot a substantial claimMay combine two claims.
PremisereasoningDetecting sample contamination and verifying the reliability of the ages produced also become more difficult as the age of the sample increases.
“Detecting sample contamination and verifying the reliability of the ages produced also become more difficult as the age of the sample increases.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
Interpretationnone givenOther procedures used in this study, including preoxidation of iron powder, molecular sieves, storage in vacuo, and a vacuum-backed extraction line, may also contribute to overall blank reduction, but more importantly guard against random contamination of individual samples.
“The other procedures used in this study, including preoxidation of the iron powder, use of molecular sieves, storage of samples in vacuo and the use of a vacuum-backed extraction line, may also con- tribute to overall blank reduction, but more importantly, guard against random contamination of individual samples.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductnone givenThe completeness of the graphitization for the 850 °C fraction can be checked by measuring the total pressure and CO2 pressure at the end of the reaction period.
“The completeness of the graphitization for the 850 °C (C) fraction can then be checked by measuring the total pressure, and CO2 pressure at the end of the reaction period.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S4 (based). May combine two claims.
Premisenone givenThe so-called radiocarbon barrier and the difficulty of ensuring that ages are reliable at <1% modern carbon levels has limited research in many disciplines.
“The so-called”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S4 (based).
Premisenone givenSignificant contamination of samples from atmospheric leakage into the extraction line can potentially occur during combustion of the sample to CO2 or during graphitization.
“Significant contamination of samples from atmospheric leakage into the extraction line can poten- tially occur during the combustion of the sample to C02, or during graphitization.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
PremisecitationEarly 14C determinations suggested that humans first arrived in Australia about 40 ka BP (the short chronology).
“Early 14C determinations suggested that humans first arrived about 40 ka BP (the”
Quote in the paperSubstantial claim0 of 2 sources checked- cites Allen and Holdaway 1995 source
- cites O'Connell and Allen 1998
Couldn’t be matched to a paper in Crossref, so it can’t be checked.
May combine two claims.
Study design and conductreasoningA graphite target is generally made from the CO2 produced during each combustion step (330 °C, 630 °C, and 850 °C), so that contaminants remaining after pretreatment are expected to be combusted in the 330 °C step and the reliability of the 14C age can be assessed by the coherence of results from the 630 °C and 850 °C steps.
“A graphite target is generally made from the CO2 produced during each combustion step (i.e., 330 °C, 630 °C, and 850 °C).In this way it is expected that any contaminants remaining after the sample pretreatment will be combusted in the 330 °C step, and that the reliability of the 14C age can be assessed by the coherence of the results from the 630 °C and 850 °C steps.”
Quote in the paperSubstantial claim- Rests on an assumption: Oxidation removes less resistant phases first, working progressively from the outside to the interior of the particles.
Probably not a substantial claim: may not pass S3 (load-bearing).
PremisereasoningThe 14C-dead charcoal from the Coulter Pedoderm is likely to be at least of last interglacial age.
“The unit is thought to have undergone pedogenesis during a period of climatic stability similar to the present, and is likely to be at least of last interglacial age.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
PremisereasoningMany laboratories will only quote 14C ages to about 40 ka BP, with ages greater than this generally considered infinite or indistinguishable from procedural blanks.
“In practice this means that many laboratories will only quote 14C ages to about 40 ka BP (thousands of '4C years Before Present), with ages greater than this generally considered to be”
Quote in the paperSubstantial claimClassified as probably not a substantial claim. May combine two claims.
Study design and conductnone givenAll pretreatment steps are carried out in either a laminar flow cabinet, a HEPA-filtered clean lab, or capped vials, with all vessels and implements precleaned by combustion or by washing with hot dichromate/sulfuric acid solution.
“All pretreatment steps are carried out in either a laminated flow cabinet, a HEPA-filtered clean lab, or capped vials, with all vessels and implements precleaned either by combustion overnight at 550 °C (Pyrex®) or 850 °C (quartz), or by washing with a hot solution of O.1 M K2Cr2O7 in a 2M solution of H2SO4.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing). May combine two claims.
InterpretationreasoningIn the AB-treated samples, there is a suggestion that ages become younger for the 850 degrees C fraction, possibly owing to formation of Na2CO3, which has a decarbonation temperature of 851 degrees C.
“However, in the case of the AB-treated samples, there is a suggestion that the ages become younger for the 850 °C fraction, possibly owing to formation of Na2CO3, which has a decarbonation temperature of 851 °C.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
- The authors state this as an assumption: The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
Classified as probably not a substantial claim.
PremisereasoningThe production of reliable 14C dates on old archaeological charcoal samples can assist in resolving the discrepancy between the short and long chronologies.
“The production of reliable 14C dates on old archaeological charcoal samples can assist in this respect.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S2 (checkable).
Premisenone givenResolution of the discrepancy between the short and long chronologies is important for a refined understanding of early human migration and colonization of Australia and the ecological effects accompanying human colonization.
“Resolution of this discrepancy is important for a refined understanding of early human migration and colonization of the continent as well as of the ecological effects accompanying human colonization.”
Quote in the paperNot a substantial claimMay combine two claims.
Premiseown dataThe buried paleosol has been subject to infiltrating waters carrying organic compounds from the vegetated surface, and interactions between the charcoal and groundwater are evidenced by fine gypsum crystals deposited on the surface of some fragments.
“The buried paleosol has been subject to infiltrating waters carrying organic compounds from the vegetated surface.Interactions between the charcoal and groundwater are evidenced by fine gypsum crystals deposited on the surface of some fragments.”
Quote in the paperNot a substantial claimProbably not a substantial claim: may not pass S4 (based).
Study design and conductnone givenFor a 14C date to be considered reliable, the ages must be reproducible within the stated error bounds.
“In addition, the ages must be reproducible within the stated error bounds”
Quote in the paperNot a substantial claim
The paper relies on this without support.
Oxidation removes less resistant phases first, working progressively from the outside to the interior of the particles.
“This is because oxi- dation can be expected to remove less resistant phases first, and work progressively from the outside to the interior of the particles.”
The authors state this as an assumption.
For a 14C date to be considered reliable at 50 ka, the combined blank from natural contamination and laboratory handling should be equivalent to a 14C age of at least 55 ka.
“We believe that for a 14C date to be considered reliable at 50 ka, for example, the combined blank from natural contamination and laboratory handling should be equivalent to a 14C age of at least 55 ka.”
The paper relies on this without support.
The 330 °C combustion step removes contaminants introduced during loading or adsorbed onto the sample surface.
“This step serves to remove contaminants that may have been introduced during the loading procedure or that are adsorbed onto the sample surface.”
The authors state this as an assumption.
The delta 13C values for ANU sucrose and charcoal are -11 per mil and -25 per mil, respectively, and a fractionation correction of 14 per mil (equivalent to 110 years) applies to each charcoal sample.
“Although the 613C value has not been mea- sured, it has been assumed that ANU sucrose and charcoal have values of -11%o and -25%, respec- tively, and hence a fractionation correction of 14% (equivalent to 110 yr) has been applied to each of the charcoal samples.”
The authors state this as an assumption.
The true blank for natural charcoal lies between the average value for the ABOX pretreated 850 degrees C fraction of Black Mountain charcoal and the Ceylon graphite blank (0.07 ± 0.05 pMC).
“A conservative approach to assigning a blank value to analyses of natural charcoals would be to assume that the true blank lies between the average value obtained for the ABOX pre- treated 850 °C fraction of the Black Mountain charcoal and the blank obtained for the Ceylon graph- ite (i.e., 0.07 ± 0.05 pMC).”
Claims other papers make about this one
Each is checked against this paper’s own text: does it say what the citing paper says it does?
Sedimentology analysis and reconstruction of sedimentation conditions of the Tonto Group [Grand Canyon] reveals that deposits of different stratigraphic sub-divisions were formed simultaneously in different litho-dynamical zones of the Cambrian paleobasin.
“Sedimentology analysis and reconstruction of sedimentation conditions of the Tonto Group [Grand Canyon] reveals that deposits of different stratigraphic sub-divisions were formed simultaneously in different litho-dynamical zones of the Cambrian paleobasin.”
From The Search for Solutions to Mysterious Anomalies in the Geologic Column (2019) · cites this paper as [34]
Split into 2 atoms — 0 confirmed, 0 partially supported, 0 disputed, 0 misattributed, 2 unverifiable. Expand the claim to see per-atom verdicts.
Experimental — accuracy not yet measured[34] showed that sediments formed simultaneously by size and density in moving waters spontaneously in the disastrous Bijou Flood in Colorado of 1965.
“[34] showed that sediments formed simultaneously by size and density in moving waters spontaneously in the disastrous Bijou Flood in Colorado of 1965.”
From The Search for Solutions to Mysterious Anomalies in the Geologic Column (2019) · cites this paper as [34]
The Samples and Pretreatment sections discuss charcoal used for radiocarbon dating and laboratory removal of mineral impurities. Searches for the 1965 Bijou Flood and for sediment sorting by size and density found no passage in our copy addressing either claim. (LLM, conf=0.77)
Experimental — accuracy not yet measured
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Self-citationBeyond the radiocarbon limit in Australian archaeology and Quaternary research
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Self-citationAMS Dating of a Late Quaternary Tephra at Graham's Terrace, New Zealand
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Radiocarbon Age Assessment of a New, Near Background Iaea <sup>14</sup>C Quality Assurance Material
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Research works printed but not linked: 1
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Cited by
Sorted by citations
Human occupation of northern Australia by 65,000 years ago
Clarkson, C., Jacobs, Z., Marwick, B., Fullagar, R., Wallis, L., Smith, M., Roberts, R. G., Hayes, E., Lowe, K., Carah, X., et al. (2017) · Nature · doi:10.1038/nature22968 · Cited by 1,185 · see citing works
“3 The three ANUA- charcoal samples were given a more aggressive acid–base wet- oxidation (ABOx) pretreatment regime, together with stepped combustion (SC) to remove contaminants at the lower-temperature steps (Bird et al., 1999a).”
BackgroundMethodBrock, F., Higham, T., Ditchfield, P. W., & Ramsey, C. B. (2010) · Radiocarbon · doi:10.1017/s0033822200045069 · Cited by 931 · see citing works
“This method removes contaminants more efficiently than a standard ABA pretreatment and has been shown to yield significantly older dates for some samples (Turney et al. 2001; Bird et al. 2003; Santos et al. 2003; Higham et al. 2009a,b; Brock and Higham 2009).”
MethodThe timing and spatiotemporal patterning of Neanderthal disappearance
Higham, T., Douka, K., Wood, R. E., Ramsey, C. B., Brock, F., Basell, L., Camps, M., Valbuena, Á. A., Preysler, J. B., Ruíz, C. B., et al. (2014) · Nature · doi:10.1038/nature13621 · Cited by 898 · see citing works
Symbolic use of marine shells and mineral pigments by Iberian Neandertals
Zilhão, J., Angelucci, D. E., Badal-García, E., d’Errico, F., Daniel, F., Dayet, L., Douka, K., Higham, T. F. G., Martínez-Sánchez, M. J., Montes-Bernárdez, R., et al. (2010) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.0914088107 · Cited by 681 · see citing works
Archaeology and age of a new hominin from Flores in eastern Indonesia
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“These tuffaceous silts were derived from volcanic eruptions and occur elsewhere in the cave, providing a useful stratigraphic marker horizon that is bracketed by ages of 13 and 11 calibrated kyr ( Supplementary Table 1a ) from associated charcoal, using acid-base wet oxidation, stepped-combustion (ABOX-SC) 14 C (ref”
MethodSelf-citationBarker, G., Barton, H. J., Bird, M. I., Daly, P., Datan, I., Dykes, A. P., Farr, L., Gilbertson, D. D., Harrisson, B., Hunt, C. O., et al. (2006) · Journal of Human Evolution · doi:10.1016/j.jhevol.2006.08.011 · Cited by 438 · see citing works
Self-citationDating the colonization of Sahul (Pleistocene Australia–New Guinea): a review of recent research
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Early Human Occupation at Devil's Lair, Southwestern Australia 50,000 Years Ago
TURNEY, C. S. M., Bird, M. I., Fifield, L. K., Roberts, R. G., Smith, M. A., Dortch, C. E., Grün, R., Lawson, E. M., Ayliffe, L. K., Miller, G. H., et al. (2001) · Quaternary Research · doi:10.1006/qres.2000.2195 · Cited by 353 · see citing works
Self-citationRADIOCARBON DATING: REVOLUTIONS IN UNDERSTANDING*
Ramsey, C. B. (2008) · Archaeometry · doi:10.1111/j.1475-4754.2008.00394.x · Cited by 340 · see citing works
Revised stratigraphy and chronology for Homo floresiensis at Liang Bua in Indonesia
Sutikna, T., Tocheri, M. W., Morwood, M. J., Saptomo, E. W., Jatmiko, Awe, R. D., Wasisto, S., Westaway, K. E., Aubert, M., Li, B., et al. (2016) · Nature · doi:10.1038/nature17179 · Cited by 330 · see citing works
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Problems with radiocarbon dating the Middle to Upper Palaeolithic transition in Italy
Higham, T., Brock, F., Peresani, M., Broglio, A., Wood, R. E., & Douka, K. (2009) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2008.12.018 · Cited by 256 · see citing works
“Bird et al. (1999, 2003) suggested that the total methodological blank for the ABOx–SC method was 0.1 0.02 pMC, which is equivalent to c. 55 ka BP.”
InfluentialThe early Upper Paleolithic occupations at Üçağızlı Cave (Hatay, Turkey)
Kuhn, S. L., Stiner, M. C., Güleç, E., Özer, İ., Yılmaz, H., Baykara, İ., Açıkkol, A., Goldberg, P. S., Molina, K. M., Ünay, E., et al. (2008) · Journal of Human Evolution · doi:10.1016/j.jhevol.2008.07.014 · Cited by 257 · see citing works
“a Determinations marked ‘‘ABOX’’ were processed using the ‘‘ultra-clean’’ protocol (Bird et al., 1999).”
BackgroundHigham, T. (2011) · Antiquity · doi:10.1017/s0003598x00067570 · Cited by 251 · see citing works
When did <i>Homo sapiens</i> first reach Southeast Asia and Sahul?
O’Connell, J. F., Allen, J., Williams, M. A. J., Williams, A. N., Turney, C. S. M., Spooner, N. A., Kamminga, J., Brown, G., & Cooper, A. (2018) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1808385115 · Cited by 236 · see citing works
Self-citationHajdas, I., Ascough, P. L., Garnett, M. H., Fallon, S., Pearson, C. L., Quarta, G., Spalding, K. L., Yamaguchi, H., & Yoneda, M. (2021) · Nature Reviews Methods Primers · doi:10.1038/s43586-021-00058-7 · Cited by 244 · see citing works
Permanent human occupation of the central Tibetan Plateau in the early Holocene
Meyer, M. C., Aldenderfer, M. S., Wang, Z., Hoffmann, D. L., Dahl, J., Degering, D., Haas, R., & Schlütz, F. (2017) · Science · doi:10.1126/science.aag0357 · Cited by 227 · see citing works
O’Connell, J., & Allen, J. (2015) · Journal of Archaeological Science · doi:10.1016/j.jas.2015.02.020 · Cited by 228 · see citing works
“These include: 1) more frequent use of pretreatment methods that extend the applicability of radiocarbon dating back to ca. 50e55 ka (Bird et al., 1999); 2) widespread use of accelerator mass spectrometry (AMS) as a means of generating more precise estimates of radiocarbon content (but see Hogg et…”
BackgroundReinhardt, L., Jerolmack, D. J., Cardinale, B. J., Vanacker, V., & Wright, J. P. (2010) · Earth Surface Processes and Landforms · doi:10.1002/esp.1912 · Cited by 209 · see citing works
“New advances also allow the measurement of extremely low 14C concentrations, enabling the dating of organic material up to 60 kyrs old (Bird et al., 1999; Turney et al., 2001, 2006).”
BackgroundVolcanism and the Greenland ice-cores: the tephra record
Abbott, P. M., & Davies, S. M. (2012) · Earth-Science Reviews · doi:10.1016/j.earscirev.2012.09.001 · Cited by 209 · see citing works
Age estimates for hominin fossils and the onset of the Upper Palaeolithic at Denisova Cave
Douka, K., Slon, V., Jacobs, Z. L., Ramsey, C. B., Shunkov, M. V., Derevianko, A. P., Mafessoni, F., Kozlikin, M. B., Li, B., Grün, R., et al. (2019) · Nature · doi:10.1038/s41586-018-0870-z · Cited by 203 · see citing works
A complete pollen record of the last 230 ka from Lynch's Crater, north-eastern Australia
Kershaw, P., Bretherton, S. C., & van der Kaars, S. (2007) · Palaeogeography Palaeoclimatology Palaeoecology · doi:10.1016/j.palaeo.2007.02.015 · Cited by 176 · see citing works
From revolution to convention: the past, present and future of radiocarbon dating
Wood, R. E. (2015) · Journal of Archaeological Science · doi:10.1016/j.jas.2015.02.019 · Cited by 170 · see citing works
Nolte, S., Koppenaal, E. C., Esselink, P., Dijkema, K. S., Schuerch, M., de Groot, A. V., Bakker, J. P., & Temmerman, S. (2013) · Journal of Coastal Conservation · doi:10.1007/s11852-013-0238-3 · Cited by 160 · see citing works
“The longest time periods are covered by the 14C-method (300–60.000 year; Bird et al. 1999; Turney et al. 2001, 2006) and the OSL-method (up to 100.000 year; Huntley et al. 1985).”
MethodInfluentialZilhão, J., Anesin, D., Aubry, T., Badal, E., Cabanes, D., Kehl, M., Klasen, N., Lucena, A., Lerma, I. M., Martínez, S., et al. (2017) · Heliyon · doi:10.1016/j.heliyon.2017.e00435 · Cited by 159 · see citing works
O’Connor, S. (2007) · Antiquity · doi:10.1017/s0003598x00095569 · Cited by 151 · see citing works
The chronostratigraphy of the Haua Fteah cave (Cyrenaica, northeast Libya)
Douka, K., Jacobs, Z., Lane, C., Grün, R., Farr, L., Hunt, C., Inglis, R. H., Reynolds, T., Albert, P., Aubert, M., et al. (2014) · Journal of Human Evolution · doi:10.1016/j.jhevol.2013.10.001 · Cited by 145 · see citing works
“…few years that ABA does not efficiently decontaminate ‘old’ (>29e30 ka BP) charcoal samples when compared with a newmore rigorous protocol (ABOx-SC: Bird et al., 1999): at almost all Palaeolithic sites where the latter has been applied, the results are older and more consistent both with the…”
Direct dating of human fossils
Grün, R. (2006) · American Journal of Physical Anthropology · doi:10.1002/ajpa.20516 · Cited by 143 · see citing works
“It is obvious that radiocarbon, including the most advanced pretreatment techniques (Bird et al., 1999; Bronk Ramsey et al., 2004b) can only address chronological issues relating to relatively recent fossils, mainlyHomo sapiens, and perhaps the youngest Neanderthal and Homo erectus specimens as…”
BackgroundPollen analyses from a 50 000‐yr rodent midden series in the southern Atacama Desert (25° 30′ S)
Maldonado, A., Betancourt, J. L., Latorre, C., et al. (2005) · Journal of Quaternary Science · doi:10.1002/jqs.936 · Cited by 138 · see citing works
“The contamination problem can now be avoided, however, through (a) an invasive chemical pretreatment and stepped-combustion techniques to remove contaminants; (b) a modified extraction system that reduces the amount of atmospheric CO2 introduced into the sample during processing (Bird et al., 1999).”
BackgroundMarco, Y. C., Ntinou, M., & Badal, E. (2010) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2009.12.015 · Cited by 137 · see citing works
“The ABOX method eliminates a substantially larger percentage of recent contaminants and it can be used to produce reliable 14C dates on charcoal up to at least 50 ka (Bird et al., 1999: 127). recovered at the Higueral de Valleja Cave (4).”
MethodQuaternary Sea-Level Changes: A Global Perspective
Murray‐Wallace, C. V., & Woodroffe, C. D. (2014) · Research Online (University of Wollongong) · Cited by 136 · see citing works
A 14C chronology for the Middle to Upper Palaeolithic transition at Bacho Kiro Cave, Bulgaria
Fewlass, H., Talamo, S., Wacker, L., Kromer, B., Tuna, T., Fagault, Y., Bard, É., McPherron, S. P., Aldeias, V., Maria, R., et al. (2020) · Nature Ecology & Evolution · doi:10.1038/s41559-020-1136-3 · Cited by 132 · see citing works
Current issues in late Middle Palaeolithic chronology: New assessments from Northern Iberia
Maroto, J., Vaquero, M., Valbuena, Á. A., Preysler, J. B., Baquedano, E., Pardo, J. F. J., Julià, R., Montes, R., van der Plicht, J., del Río, P. R., et al. (2011) · Quaternary International · doi:10.1016/j.quaint.2011.07.007 · Cited by 131 · see citing works
“Bird et al. (1999) developed a more rigorous method, Acid-Base-Oxidation-Stepped-Combustion (ABOx-SC).”
78,000-year-old record of Middle and Later Stone Age innovation in an East African tropical forest
Shipton, C., Roberts, P., Archer, W., Armitage, S. J., Bita, C., Blinkhorn, J., Mustaphi, C. J. C., Crowther, A., Curtis, R., Errico, F. D., et al. (2018) · Nature Communications · doi:10.1038/s41467-018-04057-3 · Cited by 133 · see citing works
On the chronology of the Uluzzian
Douka, K., Higham, T., Wood, R. E., Boscato, P., Gambassini, P., Karkanas, P., Peresani, M., & Ronchitelli, A. M. (2014) · Journal of Human Evolution · doi:10.1016/j.jhevol.2013.12.007 · Cited by 128 · see citing works
“This chemical protocol has been shown to underestimate systematically the age of samples older than 30 ka BP when compared with more rigorous new methods, such as the ABOx-SC protocol (Bird et al., 1999; Santos et al., 2003; Higham et al., 2009; Douka et al., 2010b; Higham, 2011; Wood et al., 2012).”
MethodPigati, J. S., Quade, J., Wilson, J., et al. (2006) · Quaternary International · doi:10.1016/j.quaint.2006.12.006 · Cited by 129 · see citing works
Pinhasi, R., Higham, T., Golovanova, L. V., & Doronichev, V. B. (2011) · Proceedings of the National Academy of Sciences · doi:10.1073/pnas.1018938108 · Cited by 127 · see citing works
Radiocarbon dating and its applications in Quaternary studies
Hajdas, I. (2008) · E&amp;G Quaternary Science Journal · doi:10.3285/eg.57.1-2.1 · Cited by 130 · see citing works
Higham, T., Jacobi, R. M., Basell, L., Ramsey, C. B., Chiotti, L., & Nespoulet, R. (2011) · Journal of Human Evolution · doi:10.1016/j.jhevol.2011.06.005 · Cited by 124 · see citing works
“…and apply newer methods, including using an ultrafiltration protocol in our collagen extraction (Brown et al., 1988; Bronk Ramsey et al., 2004; Higham et al., 2006), as well as utilising more rigorous ABOx-SC preparation methods for dating charcoal (Bird et al., 1999; Higham et al., 2006, 2009).”
MethodTURNEY, C. S. M., Kershaw, P., Moss, P., Bird, M. I., Fifield, L. K., Cresswell, R. G., Santos, G. M., Tada, M., Hausladen, P. A., & Zhou, Y. (2001) · Journal of Quaternary Science · doi:10.1002/jqs.643 · Cited by 123 · see citing works
“…then sequentially pre-treated with HCl, HF, NaOH and HCl. Results from macroscopic charcoal have shown that consistent, reproducible ages can be obtained from the 850 °C combustion fraction, and that the lower temperature fractions may still contain younger contaminant carbon (Bird et al., 1999).”
BackgroundMethodSelf-citationCrann, C. A., Murseli, S., St‐Jean, G., Zhao, X., Clark, I. D., & Kieser, W. E. (2016) · Radiocarbon · doi:10.1017/rdc.2016.55 · Cited by 125 · see citing works
“Test protocols used by other labs for old charcoals: e.g. ABOx-SC (acid-base-wet oxidationstepped combustion; Bird et al. 1999; Brock et al. 2010); 7.”
MethodDouka, K., Bergman, C. A., Hedges, R. E. M., Wesselingh, F. P., & Higham, T. (2013) · PLoS ONE · doi:10.1371/journal.pone.0072931 · Cited by 120 · see citing works
X-ray microtomographic imaging of charcoal
Bird, M. I., Ascough, P. L., Young, I. M., Wood, C. V., & Scott, A. C. (2008) · Journal of Archaeological Science · doi:10.1016/j.jas.2008.04.018 · Cited by 118 · see citing works
Self-citationOstracod shell chemistry — overview
Holmes, J. A., & Chivas, A. R. (2002) · Geophysical monograph · doi:10.1029/131gm10 · Cited by 116 · see citing works
Rebollo, N. R., Weiner, S., Brock, F., Meignen, L., Goldberg, P. S., Belfer‐Cohen, A., Bar‐Yosef, O., & Boaretto, E. (2011) · Journal of Archaeological Science · doi:10.1016/j.jas.2011.05.010 · Cited by 113 · see citing works
Radiocarbon dating late Quaternary loess deposits using small terrestrial gastropod shells
Pigati, J. S., McGeehin, J. P., Muhs, D. R., & Bettis, E. A. (2013) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2013.05.013 · Cited by 110 · see citing works
“Significant strides have been made recently in designing and constructing ultra-low-blank 14C extraction systems which, when combined with aggressive new pretreatment procedures, can yield reliable 14C ages for charcoal of up to w50 ka or more (Bird et al., 1999; Pigati et al., 2007; Higham, 2011).”
BackgroundSample Preparation at the Jena 14 C Laboratory
Steinhof, A., Soppa, M. A., & Machts, H. (2017) · Radiocarbon · doi:10.1017/rdc.2017.50 · Cited by 107 · see citing works
“The different steps involved in charcoal purification are given in Table 2, and they are very similar to those of the acid–base–oxidation (ABOx) procedure described by Bird et al. (1999).”
MethodAt the end of the 14C time scale—the Middle to Upper Paleolithic record of western Eurasia
Jöris, O., & Street, M. (2008) · Journal of Human Evolution · doi:10.1016/j.jhevol.2008.04.002 · Cited by 104 · see citing works
Lowe, J. J., & WALKER, M. J. C. (2000) · Radiocarbon · doi:10.1017/s0033822200053054 · Cited by 105 · see citing works
Bird, M. I., TURNEY, C. S. M., Fifield, L. K., Jones, R., Ayliffe, L. K., Palmer, A., Cresswell, R., & Robertson, S. (2002) · Quaternary Science Reviews · doi:10.1016/s0277-3791(01)00058-0 · Cited by 104 · see citing works
“Bird et al. / Quaternary Science Reviews 21 (2002) 1061–1075 1062”
Self-citationDavid, B., Roberts, R. G., Magee, J., et al. (2007) · Journal of Quaternary Science · doi:10.1002/jqs.1136 · Cited by 104 · see citing works
“ABOX involves the sequential pretreatment of samples with HCl, HF, and NaOH followed by a K2Cr2O7/H2SO4 oxidation at 608C for up to 14 h (Bird et al., 1999).”
MethodSelf-citationA new chronostratigraphic framework for the Upper Palaeolithic of Riparo Mochi (Italy)
Douka, K., Grimaldi, S., Boschian, G., Lucchese, A. D., & Higham, T. (2011) · Journal of Human Evolution · doi:10.1016/j.jhevol.2011.11.009 · Cited by 105 · see citing works
“This refined protocol developed by Bird et al. (1999) specifically targets older samples and involves an acidbase treatment (AB), an additional oxidation step with potassium dichromate in sulphuric acid (Ox) followed by stepped combustion (SC).”
MethodPini, R., Ravazzi, C., & Reimer, P. J. (2010) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2010.06.040 · Cited by 100 · see citing works
Prehistoric Foragers and Farmers in South-east Asia: Renewed Investigations at Niah Cave, Sarawak
Barker, G., Barton, H. J., Beavitt, P., Bird, M. I., Daly, P., Doherty, C., Gilbertson, D. D., Hunt, C. O., Krigbaum, J., Lewis, H., et al. (2002) · Proceedings of the Prehistoric Society · doi:10.1017/s0079497x00001481 · Cited by 101 · see citing works
“…just above the location of the Deep Skull at the junction between the red silts and the mudflow have yielded radiocarbon dates using the ABOX-SC technique (Bird et al. 1999) of 42,600±670 BP (Niah-310) and 41,800±620 BP (Niah - 311), dating the mudflow and providing an upper date for the skull.”
MethodSelf-citationRadiocarbon dating from 40 to 60kaBP at Border Cave, South Africa
Bird, M. I., Fifield, L. K., Santos, G. M., Beaumont, P. B., Zhou, Y., Tada, M., & Hausladen, P. A. (2003) · Quaternary Science Reviews · doi:10.1016/s0277-3791(03)00005-2 · Cited by 97 · see citing works
Self-citationHigham, T., Barton, H., TURNEY, C. S. M., et al. (2008) · Journal of Quaternary Science · doi:10.1002/jqs.1197 · Cited by 96 · see citing works
“Similarly at the Border Cave site in South Africa, ABOX-SC determinations provided a robust chronology back to 59 ka BP, in good agreement with independent chronologies obtained using other techniques (electron spin resonance and amino acid racemisation) (Bird et al., 2003).”
MethodResultInfluentialSelf-citationTesting the ABOx-SC method: Dating known-age charcoals associated with the Campanian Ignimbrite
Wood, R. E., Douka, K., Boscato, P., Haesaerts, P., Sinitsyn, A. A., & Higham, T. (2012) · Quaternary Geochronology · doi:10.1016/j.quageo.2012.02.003 · Cited by 94 · see citing works
Vasconcelos, P. M., Knesel, K. M., Cohen, B. E., et al. (2008) · Australian Journal of Earth Sciences · doi:10.1080/08120090802120120 · Cited by 94 · see citing works
“1999 ; Trumbore 2000 ), but many of the earlier 14 C dates in Australia were performed prior to the introduction of these washing procedures; therefore, the reliability of many of these results is difficult to assess.”
BackgroundResultRixhon, G., Briant, R. M., Cordier, S., Duval, M., Jones, A. F., & Scholz, D. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.08.016 · Cited by 92 · see citing works
“Significant progress has been made in recent years in providing more reliable radiocarbon ages on bone and charcoal from this older time period (e.g. Higham et al., 2006; Bird et al., 1999) and these pretreatments should be used for these materials.”
BackgroundStewart, B. A., Dewar, G., Morley, M. W., Inglis, R., Wheeler, M., Jacobs, Z. L., & Roberts, R. G. (2011) · Quaternary International · doi:10.1016/j.quaint.2011.11.028 · Cited by 89 · see citing works
“…on individual quartz grains (Jacobs et al., 2006a, b) and acid-base-wet oxidation stepped-combustion (ABOx-SC) pretreatment for 14C samples in excess of w25 ka (Bird et al., 1999; Brock et al., 2010), a robust preliminary chronology for Melikane is constructed despite taphonomic obstacles.”
BackgroundWood, R. E., Jacobs, Z. L., Vannieuwenhuyse, D., Balme, J., O’Connor, S., & Whitau, R. (2016) · PLoS ONE · doi:10.1371/journal.pone.0160123 · Cited by 85 · see citing works
Living in the Landscape: Essays in Honour of Graeme Barker
Boyle, K. V., Rabett, R., & Hunt, C. O. (2014) · Cited by 87 · see citing works
Allen, J., & O’Connell, J. F. (2003) · Australian Archaeology · doi:10.1080/03122417.2003.11681758 · Cited by 86 · see citing works
“…in the development of the acidbase-wet oxidation pretreatment with stepped combustion (ABOX-SC) used in conjunction with AMS radiocarbon dating (Bird et al. 1999), and secondly in refinements to calibration curves and the delineation of radiocarbon plateaux, like the one around 33-34 ka…”
InfluentialBrandt, S., Hildebrand, E., Vogelsang, R., Wolfhagen, J., & Wang, H. (2016) · Journal of Archaeological Science Reports · doi:10.1016/j.jasrep.2016.09.013 · Cited by 86 · see citing works
Újvári, G., Molnár, M., Novothny, Á., Páll‐Gergely, B., Kovács, J., & Várhegyi, A. (2014) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2014.06.009 · Cited by 86 · see citing works
A Comparison of Cellulose Extraction and ABA Pretreatment Methods for AMS14C Dating of Ancient Wood
Southon, J. R., & Magana, A. L. (2010) · Radiocarbon · doi:10.1017/s0033822200046452 · Cited by 83 · see citing works
“Gillespie (1990) used dilute Schutze reagent (10% KClO3 in 35% HNO3); the ABOX method (Bird et al. 1999; Santos et al. 2001; Pigati et al. 2007) employs acid-dichromate solution (0.”
BackgroundMethodInfluentialRadiocarbon chronology of Manot Cave, Israel and Upper Paleolithic dispersals
Alex, B., Barzilai, O., Hershkovitz, I., et al. (2017) · Science Advances · doi:10.1126/sciadv.1701450 · Cited by 82 · see citing works
Roberts, P., Perera, N., Wedage, O., Deraniyagala, S. U., Perera, J., Eregama, S. K., Petraglia, M. D., & Lee‐Thorp, J. A. (2017) · Journal of Human Evolution · doi:10.1016/j.jhevol.2017.01.015 · Cited by 82 · see citing works
“It is also worth noting that, as of yet, the Acid-BaseOxidation (ABOX) protocol (Bird et al., 1999) has not been applied to the 1980s or 2000s charcoal samples from Batadomba-lena, nor at other rainforest forager sites in Sri Lanka.”
Rebollo, N. R., Cohen-Ofri, I., Popovitz-Biro, R., Bar-Yosef, O., Meignen, L., Goldberg, P., Weiner, S., & Boaretto, E. (2008) · Radiocarbon · doi:10.1017/s0033822200033592 · Cited by 82 · see citing works
“Bird et al. (1999) introduced the use of wet oxidation as the last step of the chemical pretreatment in charcoal (ABOX).”
BackgroundRoberts, R. G., Westaway, K., Zhao, J., TURNEY, C. S. M., Bird, M. I., Rink, W. J., & Fifield, L. K. (2009) · Journal of Human Evolution · doi:10.1016/j.jhevol.2009.01.003 · Cited by 81 · see citing works
“…discussion, we have cited the ages associated with the highest temperature combustion step for the ABOX-prepared samples, as this is generally considered to yield the most reliable ages for ‘‘old’’ charcoal (Bird et al., 1999, 2002, 2003; Fifield et al., 2001; Turney et al., 2001; Bird, 2007).”
BackgroundMethodSelf-citationBoth half right:Updating the evidence for dating first human arrivals in Sahul
Allen, J., & O’Connell, J. F. (2014) · Australian Archaeology · doi:10.1080/03122417.2014.11682025 · Cited by 79 · see citing works
“The two samples with ABOX-SC pre-treatment were at the older end of the original range, suggesting that the Ngarrabullgan charcoal was largely uncontaminated; even so, ABOX-SC pre-treatment had refined these dates (Bird et al. 1999:139).”
BackgroundIs Classical Acid-Alkali-Acid Treatment Responsible for Contamination? An Alternative Proposition
Hatté, C., Morvan, J., Noury, C., et al. (2001) · Radiocarbon · doi:10.1017/s003382220003798x · Cited by 79 · see citing works
“The classical AAA treatment is presented in Hatté et al. (2001) and consists of: In an alternative protocol, the last acid step is replaced by an oxidation step, following the Bird et al. (1999) suggestion.”
BackgroundMethodRichter, D., Tostevin, G. B., Škrdla, P., & Davies, W. (2008) · Journal of Archaeological Science · doi:10.1016/j.jas.2008.10.017 · Cited by 78 · see citing works
“The ABOX treatment (Bird et al., 1999) was not possible for any of the samples presented here because of their small sizes.”
BackgroundInfluentialBalme, J. (2000) · Australian Archaeology · doi:10.1080/03122417.2000.11681674 · Cited by 76 · see citing works
Briant, R. M., & Bateman, M. D. (2009) · Journal of Quaternary Science · doi:10.1002/jqs.1258 · Cited by 72 · see citing works
“The ABOX-SC pre-treatment (Bird et al., 1999) seems to be effective in removing contamination from charcoal and may also be appropriate for plant macrofossil material (Hajdas et al.”
BackgroundMethodInfluentialSantos, G. M., Bird, M. I., Parenti, F., et al. (2003) · Quaternary Science Reviews · doi:10.1016/s0277-3791(03)00205-1 · Cited by 71 · see citing works
Self-citationMartínez‐Moreno, J., Torcal, R. M., & de la Torre, I. (2010) · Journal of Human Evolution · doi:10.1016/j.jhevol.2009.09.002 · Cited by 70 · see citing works
Gillespie, R. (2002) · Radiocarbon · doi:10.1017/s0033822200031830 · Cited by 70 · see citing works
“Phase 3—ABOX-SC chemistry with a 14C “event horizon” of 48–50,000 BP (Bird et al. 1999; Fifield et al. 2001; Turney et al. 2001).”
BackgroundBuang Merabak: Early Evidence For Human Occupation In The Bismarck Archipelago, Papua New Guinea
Leavesley, M., Bird, M. I., Fifield, L. K., Hausladen, P. A., Santos, G. M., & Tada, M. (2002) · Australian Archaeology · doi:10.1080/03122417.2002.11682070 · Cited by 68 · see citing works
Self-citationRoberts, R. G., & Jacobs, Z. L. (2008) · Research Online (University of Wollongong) · Cited by 64 · see citing works
Long, H., Shen, J., Wang, Y., et al. (2015) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2015.07.003 · Cited by 68 · see citing works
New isotope technologies in environmental physics
Povinec, P. P., Betti, M., Jull, A. J. T., et al. (2008) · Acta Physica Slovaca Reviews and Tutorials · doi:10.2478/v10155-010-0088-6 · Cited by 68 · see citing works
Douka, K., Higham, T., & Sinitsyn, A. A. (2010) · Quaternary Research · doi:10.1016/j.yqres.2010.01.002 · Cited by 68 · see citing works
Alon, D., Mintz, G., Cohen, I., et al. (2002) · Radiocarbon · doi:10.1017/s0033822200064638 · Cited by 68 · see citing works
“Another is to combust the organic material to be dated at different temperatures, choosing the appropriate fraction (McGeehin et al. 2001; Bird et al. 1999).”
BackgroundRadiocarbon dating, reservoir effects, and calibration
Jull, A. J. T., Burr, G. S., & Hodgins, G. W. L. (2012) · Quaternary International · doi:10.1016/j.quaint.2012.10.028 · Cited by 67 · see citing works
Caseldine, C. J., & TURNEY, C. S. M. (2009) · Journal of Quaternary Science · doi:10.1002/jqs.1337 · Cited by 70 · see citing works
“Despite the improvement in radiocarbon pre-treatment, measurement and calibration over recent decades (Bird et al., 1999; Hogg et al., 2002; Higham et al., 2006, 2009; Ramsey, 2008; Turney et al., 2008) and availability of new dating/ correlation techniques such as tephrochronology (Turney, 1998;…”
Self-citationDating Materials in Good Archaeological Contexts: The Next Challenge for Radiocarbon Analysis
Boaretto, E. (2009) · Radiocarbon · doi:10.1017/s0033822200033804 · Cited by 64 · see citing works
“Such charred materials should be stable enough to withstand the very harsh treatments involving alkali, acid, and wet oxidation (Bird et al. 1999) that are commonly applied for removing the contamination.”
BackgroundJull, A. J. T., Burr, G. S., Beck, J., et al. (2006) · Radioactivity in the environment · doi:10.1016/s1569-4860(05)08001-0 · Cited by 63 · see citing works
Climate, people and faunal succession on Java, Indonesia: evidence from Song Gupuh
Morwood, M. J., Sutikna, T., Saptomo, E. W., Westaway, K., Jatmiko, J., Due, R. A., Moore, M. W., Umar, D. Y. Y., Sulistyarto, P. H., Zhao, J., et al. (2008) · Journal of Archaeological Science · doi:10.1016/j.jas.2007.11.025 · Cited by 63 · see citing works
Self-citationHydropyrolysis: Implications for Radiocarbon Pretreatment and Characterization of Black Carbon
Ascough, P. L., Bird, M. I., Meredith, W., et al. (2010) · Radiocarbon · doi:10.1017/s0033822200046427 · Cited by 62 · see citing works
Self-citationWood, R. E., de Quirós, F. B., Maíllo‐Fernández, J., et al. (2016) · Quaternary International · doi:10.1016/j.quaint.2016.03.005 · Cited by 62 · see citing works
Small, D., Clark, C. D., Chiverrell, R. C., Smedley, R., Bateman, M. D., Duller, G. A. T., Ely, J. C., Fabel, D., Medialdea, A., & Moreton, S. G. (2016) · Earth-Science Reviews · doi:10.1016/j.earscirev.2016.11.007 · Cited by 61 · see citing works
“Following sampling material can be subject to various pre-treatments, which can influence the accuracy of the 14C age (e.g. Bird et al., 1999; Jacobi and Higham, 2008; Blockley et al., 2008).”
MethodBadino, F., Pini, R., Ravazzi, C., Margaritora, D., Arrighi, S., Bortolini, E., Figus, C., Giaccio, B., Lugli, F., Marciani, G., et al. (2019) · Quaternary International · doi:10.1016/j.quaint.2019.09.024 · Cited by 59 · see citing works
“…low levels of residual 14C activity induces lower precision (higher uncertainty) and accuracy (higher offset of the measured isotope ratio with respect to the actual one) of AMS measurements and makes samples much more vulnerable to contamination (e.g., Bird et al., 1999; Higham, 2011; Wood, 2015).”
BackgroundTURNEY, C. S. M., Fifield, L. K., Hogg, A. G., Palmer, J., Hughen, K. A., Baillie, M. G. L., Galbraith, R. F., Ogden, J., Lorrey, A. M., Tims, S. G., et al. (2010) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2010.08.017 · Cited by 61 · see citing works
Self-citationKadowaki, S., Omori, T., & Nishiaki, Y. A. (2015) · Journal of Human Evolution · doi:10.1016/j.jhevol.2015.02.017 · Cited by 61 · see citing works
Ice‐free conditions in Sweden during Marine Oxygen Isotope Stage 3?
Wohlfarth, B. (2010) · Boreas · doi:10.1111/j.1502-3885.2009.00137.x · Cited by 61 · see citing works
“2001 and references therein), the socalled ABOX method (a wet oxidation technique with stepped combustion of samples) is now being used (Bird et al. 1999). This procedure is regarded as providing reliable (14)C ages (Blockley et al. 2008). The most commonly used pretreatment method for ancient bones is the ‘Longin met…”
MethodShen, J. (2012) · Chinese Science Bulletin · doi:10.1007/s11434-012-5510-7 · Cited by 61 · see citing works
Alloway, B. V., Pribadi, A., Westgate, J. A., Bird, M. I., Fifield, L. K., Hogg, A. G., & Smith, I. E. M. (2004) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2004.08.014 · Cited by 61 · see citing works
Self-citationKadereit, A., Kind, C.-J., & Wagner, G. A. (2012) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2012.10.026 · Cited by 60 · see citing works
- Authors
- Bird, M. I., Ayliffe, L. K., Fifield, L. K., Turney, C. S. M., Cresswell, R. G., Barrows, T. T., & David, B.
- Affiliations
- Australian National University (AU)
- Venue
- Radiocarbon
- Publisher
- Cambridge University Press (CUP)
- Published
- 1999
- Volume
- 41
- Issue
- 2
- Pages
- 127-140
- ISSN
- 0033-8222 (ISSN-L)
- 1945-5755
- OpenAlex
- W1955935479
- Semantic Scholar
- 0b86b4d2ded1bc772aa8185d1d86f9fc14c36f78
- Cited by
- 320
- References
- 16
- Citations by year
- 2026: 6 · 2025: 9 · 2024: 8 · 2023: 8 · 2022: 4 · 2021: 10 · 2020: 13 · 2019: 15 · 2018: 19 · 2017: 17 · 2016: 18 · 2015: 14 · 2014: 19 · 2013: 18 · 2012: 15
- FWCI
- 5.36
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Radiocarbon (publishedVersion)
- UA Campus Repository (The University of Arizona) (acceptedVersion)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
- Social Sciences › Geography, Planning and Development › Pacific and Southeast Asian Studies
- Keywords
- charcoal dating, graphitization, pollutant removal
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