Reanalysis of the Atmospheric Radiocarbon Calibration Record from Lake Suigetsu, Japan
Open accessAbstract
ABSTRACT Terrestrial plant macrofossils from the sedimentary record of Lake Suigetsu, Japan, provide the only quasi-continuous direct atmospheric record of radiocarbon (14C) covering the last 50 ka cal BP (Bronk Ramsey et al. 2012). Since then, new high precision data have become available on U-Th dated speleothems from Hulu Cave China, covering the same time range (Cheng et al. 2018). In addition, an updated varve-based chronology has also been published for the 2006 core from Lake Suigetsu (SG06) based on extended microscopic analysis of the sediments and improved algorithms for interpolation (Schlolaut et al. 2018). Here we reanalyze the radiocarbon dataset from Suigetsu based on the new varve counting information and the constraints imposed by the speleothem data. This enables the new information on the calendar age scale of the Suigetsu dataset to be used in the construction of the consensus IntCal calibration curve. Comparison of the speleothem and plant macrofossil records provides insight into the mechanisms underlying the incorporation of carbon into different types of record and the relative strengths of different types of archive for calibration purposes.
AI snapshot
Written from the paper’s full text.
TL;DR
This paper reworks the Lake Suigetsu plant macrofossil radiocarbon record using a revised varve chronology and Hulu Cave speleothem constraints, then incorporates it into IntCal20. It finds close overall agreement but identifies two intervals where varve-based sedimentation rates may be too high, and suggests Suigetsu preserves more high-frequency atmospheric ¹⁴C variation than Hulu.
Key findings
- The reanalysis used 639 radiocarbon dates from the SG93 and SG06 cores, corresponding to 593 distinct depths over 1397.4–4040.75 cm; one date, SUERC-28223, was excluded because its error was large and it was reported as >42,700 BP.
- The updated SG06 2018 varve chronology extended the record by roughly 10 ka to 4041 cm composite depth; above that boundary, about half of years on average lacked countable seasonal layers and were interpolated with the Varve Interpolation Program.
- Offsets between Suigetsu and reservoir-corrected Hulu data were negligible: 21±19 yr for k=0.1, 12±17 yr for k=0.2, 5±16 yr for k=0.3, 8±19 yr with 100 yr extra error, and -1±32 yr with 200 yr extra error.
- Two intervals could not be supported by the varve uncertainty range: about 1730–1820 cm composite depth (~15–18 kvyr BP) with an age difference of ~300 years, and about 2700–2880 cm (~29.3–32.6 kvyr BP) with ~700 years; Suigetsu splines also showed more high-frequency signal than Hulu, and deconvolution of Hulu with a 420-year linear ramp accentuated features seen in Suigetsu.
Methods
- Data: 639 Lake Suigetsu ¹⁴C dates from the SG93 and SG06 cores, with 593 distinct depths, plus the Hulu Cave record of ~500 ¹⁴C determinations from three speleothems spanning 10.6–54 ka cal BP.
- Analysis: an OxCal Poisson-process P_Sequence model was run against the Hulu timescale with k=0.2, with sensitivity tests at k=0.1 and k=0.3 and additional relative uncertainties of 100 and 200 years; a Hulu-only curve was built using an errors-in-variables Bayesian spline with 400 knots, 250,000 MCMC iterations, half discarded as burn-in, and dead carbon fraction allowed to vary by ±50 years.
- Integration: marginal posterior calendar ages and a correlation matrix for Suigetsu depths were used as priors in the IntCal20 curve construction.
Limitations
- Stated in the paper: varve chronologies carry significant cumulative uncertainty; macrofossil availability can be limiting; μXRF counts were excluded because thin varves may be underrepresented in low-sedimentation intervals, though the affected locations are uncertain; the two offset intervals lack independent proof and their explanation remains theoretical; Suigetsu’s high-frequency signal could be noise or real; and Hulu’s dead carbon or reservoir effect is uncertain.
- Evident from the text: the final IntCal20 curve mutes some of Suigetsu’s high-frequency structure, and testing those signals depends on other records such as Cariaco and floating tree-ring sequences; the correlated calendar-age uncertainty across Suigetsu levels also complicates interpretation.
Model-written summary. Check it against the paper before relying on it.
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Cites
Statistics
Claims the paper makes
5 of 33 cited sources checked · 3 supported · 0 flagged · accuracy not yet measured
- Premisecitation
The revised Suigetsu dataset is part of the IntCal20 calibration curve.
“The revised Suigetsu dataset is included within the IntCal20 calibration curve, as described by Heaton et al. (2020 in this issue).”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Heaton et al. 2020 source
- Premisecitation
The Suigetsu record contains many substantial terrestrial plant macrofossils that three laboratories have radiocarbon dated.
“Furthermore, the record contains large numbers of substantial terrestrial plant macrofossils, radiocarbon dated by three different laboratories (Kitagawa and van der Plicht 1998;Bronk Ramsey et al. 2012).”
Quote in the paperNot a substantial claim1 of 2 sources checked- cites Kitagawa and van der Plicht 1998 source
The paper reports more than 250 terrestrial macrofossils from Lake Suigetsu sediments that were radiocarbon dated (p. 2). It says those measurements were made at the Groningen AMS facility; it does not support the claim that three different laboratories dated them. (LLM, conf=0.88)
Experimental — accuracy not yet measured - cites Bronk Ramsey et al. 2012 source
- Rests on an assumption: The plant macrofossils sampled from Lake Suigetsu are from non-aquatic species and therefore record atmospheric 14C.
- Interpretationcitation
Much available marine data, including U-Th dated corals, share the offset pattern seen here, despite scatter from diagenesis.
“However, it is clear that much of the available marine data, including the U-Th dated corals, share the pattern seen here, even though there is some scatter due to diagenesis.This is evident in the placement of the IntCal09 (Reimer et al. 2009) curve relative to IntCal13.”
Quote in the paperSubstantial claim1 of 1 sources checked- cites Reimer et al. 2009 source
The Introduction and IntCal09 Curve Construction sections say that IntCal09 incorporates marine records, including independently dated corals, and the Data Set Selection Criteria section discusses screening corals for diagenesis. The paper presents the IntCal09 curve, but it does not compare its placement with IntCal13 or establish that the marine data share the citing paper’s observed pattern. (LLM, conf=0.84)
Experimental — accuracy not yet measured
- Findingown data
Many dates in the preliminary model had significantly low agreement indices.
“In practice there were many dates with significantly low agreement indices, so we also tested the impact of increasing the relative uncertainty in the radiocarbon dates between the Hulu and Suigetsu datasets by both 100 and 200 years.”
Quote in the paperSubstantial claim - Findingown data
The method yields a correlation coefficient matrix for all distinct levels.
“Secondly, a correlation coefficient matrix for all distinct levels has been generated; given the nature of the underlying varve chronology there is a considerable degree of correlation between closely spaced dates (implying that calendar age shifts to one require others nearby to be similarly shifted).”
Quote in the paperSubstantial claim
- Findingown data
The method yields a marginal posterior U-Th age estimate for each radiocarbon date in the core.
“Firstly, a marginal posterior estimate for the U-Th age associated with each radiocarbon date within the core: this information has been summarized in the supplementary information of this paper using the mean and standard deviation (as used for the incorporation into IntCal) and the highest posterior density (hpd) ranges at 68.2 and 95.4% probabilities.”
Quote in the paperSubstantial claim - Findingown data
Only two significant core intervals could not be supported by the varve data: ~1730-1820 cm (~15-18 kvyr BP) and ~2700-2880 cm (~29.3-32.6 kvyr BP).
“This revealed that in only two significant core intervals could the U-Th adjusted chronology not be supported by the varve data: between ~1730 and ~1820 cm composite depth (~15 to 18 kvyr BP) and between ~2700 and ~2880 cm (~29.3 to 32.6 kvyr BP).”
Quote in the paperSubstantial claim - Findingown data
Within the 2-sigma uncertainty envelopes, the preliminary timescale estimates and the overall IntCal model output agree reasonably well.
“Here it can be seen that within the 2-σ uncertainty envelopes plotted, the two are in reasonable agreement.”
Quote in the paperNot a substantial claim - Findingreasoning
The final IntCal20 curve contains much of the Suigetsu high-frequency components, though somewhat muted.
“The final IntCal20 curve does contain much of the high-frequency components seen within the Suigetsu dataset, but somewhat muted; correctly we would argue, because there will undoubtedly be some noise as well as signal, and only testing against other datasets can distinguish between these.”
Quote in the paperSubstantial claim - Findingown data
The Suigetsu data appear to contain much more high-frequency signal than the Hulu data.
“What is clear from this is that the Suigetsu data appear to have much more high-frequency signal than the Hulu data.”
Quote in the paperNot a substantial claim - Premisecitation
From 10.6 to 54 ka cal BP, the Hulu Cave record contains about 500 14C determinations with independent calendar ages mainly from paired U-Th dates.
“Between 10.6 and 54 ka cal BP, the Hulu cave record consists of ~500 14 C determinations with corresponding, independent calendar age estimates obtained predominantly from paired U-Th dates.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Cheng et al. 2018 source
- Interpretationreasoning
The underlying varve chronology creates considerable correlation between closely spaced dates.
“Secondly, a correlation coefficient matrix for all distinct levels has been generated; given the nature of the underlying varve chronology there is a considerable degree of correlation between closely spaced dates (implying that calendar age shifts to one require others nearby to be similarly shifted).”
Quote in the paperSubstantial claim - Interpretationreasoning
Shared uncertainty in the Hulu Cave speleothems' reservoir age creates some correlation across the whole dataset.
“It should be noted that there is also some correlation across the dataset as a whole because of the shared uncertainty in the reservoir age of the Hulu Cave speleothems.”
Quote in the paperNot a substantial claim - Premisecitation
Lake Suigetsu's terrestrial plant macrofossils yield the sole quasi-continuous direct atmospheric 14C record spanning the last 50 ka cal BP.
“Terrestrial plant macrofossils from the sedimentary record of Lake Suigetsu, Japan, provide the only quasi-continuous direct atmospheric record of radiocarbon ( 14 C) covering the last 50 ka cal BP (Bronk Ramsey et al. 2012).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Bronk Ramsey et al. 2012 source
- Rests on an assumption: The plant macrofossils sampled from Lake Suigetsu are from non-aquatic species and therefore record atmospheric 14C.
- Premisecitation
U-Th dated speleothems from Hulu Cave, China, provide new high-precision data over the same time interval.
“Since then, new high precision data have become available on U-Th dated speleothems from Hulu Cave China, covering the same time range (Cheng et al. 2018).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Cheng et al. 2018 source
- Premisecitation
The dead carbon fraction in the three Hulu Cave speleothems is thought to be especially small and stable, based on their overlap with dendrochronologically dated trees and with each other.
“While, as described in the Introduction, all speleothems have a potentially time-varying dead carbon fraction, within the three Hulu cave speleothems this is believed to be particularly small and stable based on assessment of their overlap with dendrochronologically dated trees and one another.”
Quote in the paperSubstantial claim0 of 2 sources checked - Premisecitation
Above the 4041 cm depth, seasonal layers failed to form or were not preserved in about half the years on average.
“However, in on average 50% of the years above this point either seasonal layers did not form or were not preserved.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
- Premisecitation
Together, the Hulu speleothems provide a long, high-resolution 14C record with precise U-Th dates extending to 54 ka cal BP.
“Combined, these speleothems provide a long and high-resolution record of 14 C measurements together with equally high-resolution precise U-Th dates that extend back to 54 ka cal BP.”
Quote in the paperNot a substantial claim0 of 2 sources checked - Premisecitation
The indistinguishable layers in the 2018 chronology were interpolated with a new Varve Interpolation Program (VIP).
“These indistinguishable layers were interpolated using a new Varve Interpolation Program (VIP; Schlolaut et al. 2018).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
- Premisecitation
The VIP uses a different interpolation method that derives varve thickness frequency distributions from the incomplete count dataset.
“The use of the new program marks a major change to the previous 2012 varve chronology, as the new program uses an entirely different interpolation approach based on deriving varve thickness frequency distributions from the incomplete count dataset and using these for interpolation.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
- Interpretationown data
Increasing relative uncertainty has an effect similar to increasing the P_Sequence model's rigidity.
“In general, increasing the relative uncertainty has a similar effect to increasing the rigidity of the P_Sequence model.”
Quote in the paperNot a substantial claim - Premisereasoning
The 2018 varve chronology did not incorporate data from the independent μXRF counting method.
“Another major difference between the 2012 and 2018 varve chronologies is that data from a second, independent counting method using μXRF data (Marshall et al. 2012), were not incorporated in the 2018 varve chronology.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Marshall et al. 2012 source
- Premisecitation
A revised varve chronology for the SG06 core from Lake Suigetsu has been published, using extended microscopic sediment analysis and improved interpolation algorithms.
“In addition, an updated varve-based chronology has also been published for the 2006 core from Lake Suigetsu (SG06) based on extended microscopic analysis of the sediments and improved algorithms for interpolation (Schlolaut et al. 2018).”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
- Interpretationreasoning
The Suigetsu record alone would not be useful without age constraints from speleothem and coral data with direct U-Th ages.
“On the other hand, the Suigetsu record on its own would not be useful without the age constraints provided by the speleothem and coral data with their direct U-Th ages, so the high-frequency signals in the Suigetsu dataset can really only be tested against the high-resolution marine data from Cariaco (Hughen et al. 2004), and, where available, limited floating tree-ring sequences (for example, Tur”
Quote in the paperSubstantial claim - Interpretationreasoning
The combined datasets form a network of information that makes the calibration curve more robust.
“All of these different datasets together provide us with a network of information that makes the calibration curve more robust.”
Quote in the paperNot a substantial claim - Interpretationcitation
The lower of the two intervals is suspicious because it nearly coincides with microfacies zone II.a2.
“In particular the lower of the two intervals is suspicious in this regard, since it almost coincides with microfacies zone II.a2 (Schlolaut et al. 2018).”
Quote in the paperNot a substantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
- Interpretationreasoning
This closeness is expected because Hulu data still influence SG06's calendar age within IntCal.
“This is to be expected, because, within IntCal, the Hulu data are still influencing the calendar age of SG06; this is not an argument for using a less rigid preliminary model, since that would effectively just down-weight the importance of the relative ages from the varve chronology.”
Quote in the paperSubstantial claim - Interpretationreasoning
The Suigetsu high-frequency signals can only be tested against high-resolution Cariaco marine data and limited floating tree-ring sequences.
“so the high-frequency signals in the Suigetsu dataset can really only be tested against the high-resolution marine data from Cariaco (Hughen et al. 2004), and, where available, limited floating tree-ring sequences (for example, Turney et al. 2016).”
Quote in the paperSubstantial claim0 of 2 sources checked - Interpretationown data
The Suigetsu data suggest the Hulu speleothem record may lack some high-frequency components of atmospheric radiocarbon variation.
“We would argue that the data from this series suggest that the speleothem record from Hulu (Cheng et al. 2018) may not contain all of the highfrequency components of the atmospheric variation in radiocarbon.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Cheng et al. 2018 source
- May combine two claims. 21
- Classified as probably not a substantial claim. 9
May combine two claims.
FindingcitationIn the younger sequence down to about 28 kvyr BP, offsets from the varve chronology were expected and resemble those for IntCal13.
“In the younger part of the sequence (down to about 28 kvyr BP in the varve chronology) the offsets were expected and are similar to those seen for IntCal13 (Reimer et al. 2013).”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites Reimer et al. 2013 source
Probably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductcitationThe Hulu-only atmospheric 14C estimate was produced with the same errors-in-variables Bayesian spline method used for the main IntCal20 curve.
“We created a Hulu-cave-only (Hulu-Cal) estimate of atmospheric 14 C using the same errors-in-variables Bayesian spline approach taken to create the main IntCal20 curve (see Heaton et al. 2020 in this issue).”
Quote in the paperNot a substantial claim1 of 1 sources checked- cites Heaton et al. 2020 source
- The authors state this as an assumption: The uncertainties on the U-Th based calendar ages for each Hulu 14C determination are independent of one another.
May combine two claims.
Findingown dataAll offset estimates are within error limits and consistent with no systematic offset between the Suigetsu and Hulu datasets.
“However, all are, within error limits, consistent with a zero systematic offset.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The uncertainties on the U-Th based calendar ages for each Hulu 14C determination are independent of one another.
May combine two claims.
Findingown dataThe 2012 and 2018 varve chronologies agree very well for most of the record, except between 1980 and 2375 cm composite depth.
“Despite these major changes, the 2012 and 2018 varve chronologies are in very good agreement for most of the record, with a notable exception between 1980 and 2375 cm composite depth.”
Quote in the paperSubstantial claimMay combine two claims.
Findingnone givenThe Suigetsu dataset's main distinguishing features are that it requires no dead carbon or reservoir effect and that its calendar age uncertainty is correlated.
“The main distinguishing features of this dataset are: i) that there is no dead carbon or reservoir effect required, and ii) the correlated nature of the calendar age uncertainty.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataIn the 1980-2375 cm interval, the 2018 chronology implies a higher sedimentation rate and younger ages than the 2012 chronology, although the 2012 chronology remains within the 2018 error estimate.
“In this interval the 2018 varve chronology suggests a higher sedimentation rate, i.e. younger ages, though the 2012 chronology is still within the error estimate of the 2018 chronology.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataAdding 100 or 200 years of relative uncertainty to the Hulu and Suigetsu radiocarbon dates changed model outputs slightly, especially below 15 kvyr BP, but all changes stayed within the model's 95% error limits.
“Although this did produce slightly different model outputs (particularly in the region <15 kvyr BP of the varve chronology), these were all well within the 95% error limits of the model (see Figure 2), so it was decided to use the unmodified data without any additional errors.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataThe models found a consistently negligible offset between the Suigetsu and reservoir-corrected Hulu datasets: 21±19 for k=0.1, 12±17 for k=0.2, 5±16 for k=0.3, 8±19 for k=0.2 with extra error 100, and -1±32 for k=0.2 with extra error 200.
“The models all showed a consistently negligible offset between the datasets: 21±19 for k=0.1, 12±17 for k=0.2, 5±16 for k=0.3, 8±19 for k=0.2 with an extra error of 100, and -1±32 for k=0.2 with an extra error of 200.”
Quote in the paperSubstantial claim- The authors state this as an assumption: The uncertainties on the U-Th based calendar ages for each Hulu 14C determination are independent of one another.
Classified as probably not a substantial claim. May combine two claims.
Findingown dataAt the Laschamp excursion (~41k cal BP), Suigetsu uncertainties become large, so the 20-35k cal BP period with smaller measurement uncertainty is more useful.
“At the Laschamp excursion (circa 41k cal BP) the uncertainties become large in the Suigetsu data, and so it is more useful to focus on the period where the measurement uncertainty is smaller (20-35k cal BP; see Figure 5).”
Quote in the paperSubstantial claimMay combine two claims.
FindingreasoningIn both intervals, final age-scale sedimentation rates are lower than the smallest rates within the varve model's uncertainty range, leaving age differences of ~300 years in the upper interval and ~700 years in the lower interval.
“In either case the sedimentation rates of the final age-scale are lower than the smallest sedimentation rates within the uncertainty range of the varve model, so that an age difference remains: in the upper interval ~300 years and in the lower interval ~700 years.”
Quote in the paperSubstantial claimMay combine two claims.
Findingown dataBetween 30 and 40 kvyr BP, the new Hulu data constrain offsets much better and shift SG06 significantly older, revealing both apparent under-counting and over-counting in the varve chronology.
“However, for the period between 30 and 40 kvyr BP the offsets are much better constrained by the new Hulu data.This shifts the SG06 data significantly older in this period with sections of both apparent under-counting and over-counting seen in the varve chronology.”
Quote in the paperSubstantial claimMay combine two claims.
FindingreasoningThe final age model lies slightly farther from the varve-only model and quite close to the preliminary Hulu-based model that would have been obtained with lower model rigidity.
“In general the final age model is pulled slightly further away from the varve-only model and is quite close to the preliminary model (against Hulu) that we would have obtained with a lower model rigidity (see Figure 1 above).”
Quote in the paperNot a substantial claimMay combine two claims.
PremisecitationThe 2018 varve chronology extends about 10 ka beyond the 2012 chronology, reaching a composite depth of 4041 cm.
“Compared to the 2012 varve chronology (SG06 2012 vyr BP chronology; Bronk Ramsey et al. 2012;Marshall et al. 2012) the 2018 iteration has been extended by approximately 10 ka to a composite depth of 4041 cm (correlation model ver.28 Feb. 2019).”
Quote in the paperSubstantial claim0 of 3 sources checkedMay combine two claims.
InterpretationreasoningThe marginal posterior dates for each Suigetsu SG06 level use all other calibration-curve data and give the best age estimate for SG06 sediments.
“These estimates make use of all of the other data included within the calibration curve, and so provide our best estimate of the age of the sediments within SG06.”
Quote in the paperSubstantial claimMay combine two claims.
Interpretationown dataExcept for the last case, SG06 dates were slightly older than corrected Hulu data, suggesting the Hulu reservoir or dead carbon fraction may be marginally overestimated.
“In all cases but the last, the SG06 dates were slightly older when compared to the corrected Hulu data suggesting, if anything, the Hulu reservoir (or dead carbon fraction) to be marginally over estimated.”
Quote in the paperNot a substantial claim- The authors state this as an assumption: The uncertainties on the U-Th based calendar ages for each Hulu 14C determination are independent of one another.
May combine two claims.
PremisecitationThe Lake Suigetsu sediment record is unusual because it spans the full radiocarbon technique range and contains varves throughout the interval lacking dendrochronological calibration data.
“More specifically, we look particularly at the lacustrine sediment record of Lake Suigetsu, central Japan (Nakagawa et al. 2012) which is unusual in covering the full range of the radiocarbon technique, with varves (albeit of variable quality) throughout the period for which we have no dendrochronogically based calibration datasets.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Nakagawa et al. 2012 source
May combine two claims.
PremisecitationThe Hulu Cave speleothem records have an unusually low dead carbon fraction or reservoir effect and cover the same pre-Holocene range.
“We also choose to focus on the unique series of speleothem records from Hulu Cave, China (Southon et al. 2012;Cheng et al. 2018) characterized by an unusually low dead carbon fraction or reservoir effect, and with coverage over the same range of the pre-Holocene period.”
Quote in the paperSubstantial claim0 of 2 sources checkedMay combine two claims.
InterpretationreasoningProperly modelling and including calendar age covariance in curve construction improves noise-signal separation and preserves more of the Suigetsu record's structure in IntCal20.
“Correctly modelling and including this calendar age covariance, also present within the Cariaco, Pakistan, and Iberian margin chronologies, into curve construction is important.It improves our ability to distinguish what is noise and what is signal by making it easier to identify common features when combining the full set of varied records; and means that more of the structure and shape of the Su”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
PremisecitationThe Hulu Cave 14C record comprises three speleothems: H82, MSD, and MSL.
“The Hulu cave 14 C record from Tang Shan, near Nanjing in Eastern China, consists of three speleothems (H82, Southon et al. 2012;MSD and MSL, Cheng et al. 2018).”
Quote in the paperNot a substantial claim0 of 2 sources checkedProbably not a substantial claim: may not pass S3 (load-bearing).
Study design and conductown dataThe preliminary model's sensitivity to the P_Sequence rigidity parameter k was tested at k=0.1 and k=0.3.
“However, the sensitivity of the model to different choices of this parameter was investigated (at k=0.1, which is less rigid, and k=0.3, which is more rigid).”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim.
PremisecitationThe 2018 Suigetsu varve chronology counts seasonal layers using thin-section microscopy.
“The 2018 Suigetsu varve chronology (SG06 2018 vyr BP chronology; Schlolaut et al. 2018) is based on the counts of seasonal layers using thin section microscopy.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
May combine two claims.
Interpretationown dataDeconvolution of the Hulu data accentuates some features seen in the Suigetsu data, suggesting the Suigetsu signals are at least not entirely noise.
“this is to retain as much of the authentic higher in Figure 6 where you can see that this does actually accentuate some features seen in the Suigetsu data, suggesting that the signals seen in Suigetsu are at least not entirely noise.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
InterpretationreasoningThe age-model offset might result from environmental conditions specific to microfacies zone II.a2 affecting varve formation.
“Since a microfacies zone indicates specific environmental conditions different from those of other microfacies zones, this offset in the age model might indeed be due to the effect of these environmental conditions on varve formation.”
Quote in the paperNot a substantial claimClassified as probably not a substantial claim. May combine two claims.
InterpretationcitationIf low sediment accumulation conditions also hindered varve formation, thin varves would be underrepresented, causing too high an interpolated sedimentation rate.
“This means that if environmental conditions which lead to low sediment accumulation were also unfavourable for varve formation, then thin varves are underrepresented.This in turn would lead to a problem in the interpolation (Schlolaut et al. 2018) resulting in too high an interpolated sedimentation rate.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
Probably not a substantial claim: may not pass S3 (load-bearing).
InterpretationreasoningThe atmospheric offset seen in Hulu may be more a reservoir effect than a dead carbon fraction.
“The implication of this is that the offset from the atmosphere seen in Hulu may be more of a reservoir effect than a dead carbon fraction.”
Quote in the paperNot a substantial claimMay combine two claims.
PremisecitationMicrofacies zone II.a2 has few seasonal layers, and a very high proportion of those layers are of low quality and poorly distinguishable.
“This interval is characterized by a low frequency of seasonal layers, with a very high proportion of the occurring layers being of low quality, i.e. poorly distinguishable.”
Quote in the paperSubstantial claim0 of 1 sources checked- cites Schlolaut et al. 2018 source
May combine two claims.
InterpretationreasoningThe Suigetsu dataset is direct, atmospheric, and unfiltered, and is closest in nature to the terrestrial samples many radiocarbon users date.
“In particular, it provides a direct atmospheric and unfiltered dataset, which is closest in nature to the types of terrestrial samples many users of radiocarbon will be using for chronological purposes.”
Quote in the paperSubstantial claimProbably not a substantial claim: may not pass S3 (load-bearing).
InterpretationreasoningIf the offsets stem from a varve-model error, systematic under-representation of small varve thicknesses could explain them because the varve model is interpolated.
“If these offsets are indeed due to an error in the varve model, then there are only a limited number of potential reasons for that.Since the varve model is interpolated, a systematic under-representation of, in this case, small varve thicknesses could be a reason.”
Quote in the paperNot a substantial claim
The paper relies on this without support.
There is no near-term prospect that dendrochronology will cover the full range of the radiocarbon dating technique.
“There is, however, no immediate prospect for this to cover the full range of the radiocarbon dating technique and so we must therefore fall back on other types of record for the older section of the curve, all of which have their strengths and limitations.”
The paper relies on this without support.
Varve chronologies carry significant cumulative uncertainties.
“Their disadvantages are that the varve chronologies have significant cumulative uncertainties, and finding enough substantial plant macrofossils can be a challenge.”
The paper relies on this without support.
The plant macrofossils sampled from Lake Suigetsu are from non-aquatic species and therefore record atmospheric 14C.
“these have the advantage of being atmospheric (since the plant species sampled are not aquatic)”
The paper relies on this without support.
Thin varves may be systematically underrepresented in intervals with low sedimentation rate in the μXRF count because of a methodological limit.
“The main reason for this exclusion was that, due to a methodological limit, thin varves may be systematically underrepresented in intervals with a low sedimentation rate in the μXRF count.”
The authors state this as an assumption.
The uncertainties on the U-Th based calendar ages for each Hulu 14C determination are independent of one another.
“The uncertainties on the U-Th based calendar ages for each 14 C determination were considered independent from one another.”
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?
An updated timescale for Lake Suigetsu was modeled using both the new varve chronology and a 14C wiggle-match to the extended Hulu Cave record.
“An updated timescale was modeled (Bronk Ramsey et al. 2020 in this issue) using both the new varve chronology and a 14 C wiggle-match to the extended Hulu Cave record (Cheng et al. 2018).”
From The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP) (2020) · cites this paper as Bronk Ramsey et al. 2020 in this issue
Cites
IntCal13 and Marine13 radiocarbon age calibration curves 0–50,000 years cal BP
Reimer, P. J., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Ramsey, C. B., Buck, C. E., Cheng, H., Edwards, R. L., Friedrich, M., et al. (2013) · Radiocarbon · doi:10.2458/azu_js_rc.55.16947 · Cited by 14,591 · see citing works
Self-citationIntCal13とMarine13放射性炭素年代較正曲線0-50,000年cal BP
Reimer, P. J., Bard, É., Bayliss, A., Warren, B. J., Blackwell, P. G., Bronk, R., Buck Caitlin, E., Cheng, H., Lawrence, E. R., Michael, F., et al. (2013) · Radiocarbon · Cited by 5,676 · see citing works
Self-citationIntCal09 and Marine09 radiocarbon age calibration curves, 0–50,000 years cal BP
Reimer, P. J., Baillie, M. G. L., Bard, E., Bayliss, A., Beck, J. W., Blackwell, P. G., Bronk Ramsey, C., Buck, C. E., Burr, G. S., Edwards, R. L., et al. (2009) · Radiocarbon · doi:10.1017/s0033822200034202 · Cited by 4,290 · see citing works
Self-citationDeposition models for chronological records
Ramsey, C. B. (2008) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2007.01.019 · Cited by 1,772 · see citing works
Self-citation<sup>14</sup> C Activity and Global Carbon Cycle Changes over the Past 50,000 Years
Hughen, K., Lehman, S., Southon, J., Overpeck, J., Marchal, O., Herring, C., & Turnbull, J. (2004) · Science · doi:10.1126/science.1090300 · Cited by 492 · see citing works
Kitagawa, H., & van der Plicht, J. (1998) · Science · doi:10.1126/science.279.5354.1187 · Cited by 414 · see citing works
Bard, É., Arnold, M., Hamelin, B., Tisnérat‐Laborde, N., & Cabioch, G. (1998) · Radiocarbon · doi:10.1017/s0033822200019135 · Cited by 360 · see citing works
A complete terrestrial radiocarbon record for 11.2 to 52.8 kyr B.P
Bronk Ramsey, C., Staff, R. A., Bryant, C. L., Brock, F., Kitagawa, H., van der Plicht, J., Schlolaut, G., Marshall, M. H., Brauer, A., Lamb, H. F., et al. (2012) · Science · doi:10.1126/science.1226660 · Cited by 250 · see citing works
Self-citationA high-resolution record of atmospheric 14C based on Hulu Cave speleothem H82
Southon, J., Noronha, A. L., Cheng, H., Edwards, R. L., & Wang, Y. (2012) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2011.11.022 · Cited by 175 · see citing works
Atmospheric <sup>14</sup> C/ <sup>12</sup> C changes during the last glacial period from Hulu Cave
Cheng, H., Edwards, R. L., Southon, J., Matsumoto, K., Feinberg, J. M., Sinha, A., Zhou, W., Li, H., Li, X., Xu, Y., et al. (2018) · Science · doi:10.1126/science.aau0747 · Cited by 135 · see citing works
Nakagawa, T., Gotanda, K., Haraguchi, T., Danhara, T., Yonenobu, H., Brauer, A., Yokoyama, Y., Tada, R., Takemura, K., Staff, R. A., et al. (2012) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2010.12.013 · Cited by 133 · see citing works
Self-citationHeaton, T. J., Blaauw, M., Blackwell, P. G., Bronk Ramsey, C., Reimer, P. J., & Scott, E. M. (2020) · Radiocarbon · doi:10.1017/rdc.2020.46 · Cited by 124 · see citing works
Self-citationMarshall, M., Schlolaut, G., Nakagawa, T., Lamb, H., Brauer, A., Staff, R., Ramsey, C. B., Tarasov, P., Gotanda, K., Haraguchi, T., et al. (2012) · Quaternary Geochronology · doi:10.1016/j.quageo.2012.06.002 · Cited by 64 · see citing works
Self-citationTurney, C. S. M., Palmer, J., Bronk Ramsey, C., Adolphi, F., Muscheler, R., Hughen, K. A., Staff, R. A., Jones, R. T., Thomas, Z. A., Fogwill, C. J., et al. (2016) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2016.02.005 · Cited by 47 · see citing works
Self-citationSchlolaut, G., Staff, R. A., Brauer, A., Lamb, H. F., Marshall, M. H., Bronk Ramsey, C., & Nakagawa, T. (2018) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2018.09.021 · Cited by 32 · see citing works
Self-citationIntegration of the Old and New Lake Suigetsu (Japan) Terrestrial Radiocarbon Calibration Data Sets
Staff, R. A., Schlolaut, G., Ramsey, C. B., Brock, F., Bryant, C., Kitagawa, H., van der Plicht, J., Marshall, M., Brauer, A., Lamb, H. F., et al. (2013) · Radiocarbon · doi:10.2458/azu_js_rc.v55i2.16339 · Cited by 25 · see citing works
Self-citation
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The IntCal20 Northern Hemisphere Radiocarbon Age Calibration Curve (0–55 cal kBP)
Reimer, P. J., Austin, W. E. N., Bard, E., Bayliss, A., Blackwell, P. G., Bronk Ramsey, C., Butzin, M., Cheng, H., Edwards, R. L., Friedrich, M., et al. (2020) · Radiocarbon · doi:10.1017/rdc.2020.41 · Cited by 7,900 · see citing works
“An updated timescale was modeled (Bronk Ramsey et al. 2020 in this issue) using both the new varve chronology and a 14 C wiggle-match to the extended Hulu Cave record (Cheng et al. 2018).”
MethodSelf-citationHeaton, T. J., Blaauw, M., Blackwell, P. G., Bronk Ramsey, C., Reimer, P. J., & Scott, E. M. (2020) · Radiocarbon · doi:10.1017/rdc.2020.46 · Cited by 124 · see citing works
Self-citationRadiocarbon: A key tracer for studying Earth’s dynamo, climate system, carbon cycle, and Sun
Heaton, T., Bard, É., Ramsey, C. B., Martin Butzin, A., Köhler, P., Muscheler, R., Reimer, P. J., & Wacker, L. (2021) · Science · doi:10.1126/science.abd7096 · Cited by 116 · see citing works
Self-citationComposition and consequences of the IntCal20 radiocarbon calibration curve
Reimer, P. J. (2020) · Quaternary Research · doi:10.1017/qua.2020.42 · Cited by 94 · see citing works
“In addition, the Lake Suigetsu varved sediment record, which contains terrestrial macrofossils, has been revised and extended (Schlolaut et al., 2018), and the calendar age has been modelled with the Hulu cave timescale (Bronk Ramsey et al., 2020).”
MethodA 51,000-year-old engraved bone reveals Neanderthals’ capacity for symbolic behaviour
Leder, D., Hermann, R., Hüls, M., et al. (2021) · Nature Ecology & Evolution · doi:10.1038/s41559-021-01487-z · Cited by 74 · see citing works
Graves, C. A., Benson, L., Aldridge, J., Austin, W. E. N., Molin, F. D., Fonseca, V. G., Hicks, N., Hynes, C., Kröger, S., Lamb, P. D., et al. (2022) · Frontiers in Marine Science · doi:10.3389/fmars.2022.926215 · Cited by 52 · see citing works
“Classical age-depth models can be constructed in software such as CLAM (Blaauw, 2010), but more commonly Bayesian statistical packages such as OxCal (Ramsey, 1995; Ramsey, 2009), and BACON (Blaauw and Christen, 2011), are applied to create models that fully account for uncertainties al lowing for the calculat ion of s…”
MethodUpdated Cariaco Basin<sup>14</sup>C Calibration Dataset from 0–60 cal kyr BP
Hughen, K. A., & Heaton, T. J. (2020) · Radiocarbon · doi:10.1017/rdc.2020.53 · Cited by 50 · see citing works
Self-citationSimon, Q., Thouveny, N., Bourlès, D. L., Valet, J., & Bassinot, F. (2020) · Earth and Planetary Science Letters · doi:10.1016/j.epsl.2020.116547 · Cited by 48 · see citing works
“Such feature is also coherent with the structure of the atmospheric 14C variation observed over the Laschamp interval in high-resolution records (Staff et al., 2019; Bronk Ramsey et al., 2020).”
BackgroundSarnthein, M., Küssner, K., Grootes, P. M., Ausín, B., Eglinton, T. I., Muglia, J., Muscheler, R., & Schlolaut, G. (2020) · Climate of the past · doi:10.5194/cp-16-2547-2020 · Cited by 39 · see citing works
Self-citationEVOLUTION OF RADIOCARBON CALIBRATION
Reimer, P. J. (2021) · Radiocarbon · doi:10.1017/rdc.2021.62 · Cited by 32 · see citing works
Testing and Improving the IntCal20 Calibration Curve with Independent Records
Muscheler, R., Adolphi, F., Heaton, T. J., Bronk Ramsey, C., Svensson, A., van der Plicht, J., & Reimer, P. J. (2020) · Radiocarbon · doi:10.1017/rdc.2020.54 · Cited by 30 · see citing works
Self-citationMcLean, D., Albert, P. G., Suzuki, T., Nakagawa, T., Kimura, J., Chang, Q., Miyabuchi, Y., Manning, C., MacLeod, A., Blockley, S. P. E., et al. (2020) · Geochemistry Geophysics Geosystems · doi:10.1029/2019gc008874 · Cited by 26 · see citing works
Self-citationGlacial-to-deglacial reservoir and ventilation ages on the southwest Iberian continental margin
Ausín, B., Sarnthein, M., & Haghipour, N. (2021) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2021.106818 · Cited by 23 · see citing works
Bard, É., & Heaton, T. (2021) · Climate of the past · doi:10.5194/cp-17-1701-2021 · Cited by 20 · see citing works
“Reimer, P.J., Bard, E., Bayliss, A., Beck, J.W., Blackwell, P.G., Bronk Ramsey, C., Buck, C.E., Cheng, H., Edwards, R.L., Friedrich, M., Grootes, P.M., Guilderson, T.P., Haflidason, H., 880 Hajdas, I., Hatté, C., Heaton, T.J., Hoffmann, D.L., Hogg, A.G., Hughen, K.A., Kaiser, K.F., Kromer, B., Manning, S.W., Niu, M.,…”
MethodInfluentialSelf-citationBard, E., & Heaton, T. J. (2021) · Climate of the past · doi:10.5194/cp-2020-164-cc2 · Cited by 16 · see citing works
Self-citationReimer, P. J. (2020) · Radiocarbon · doi:10.1017/rdc.2020.99 · Cited by 13 · see citing works
“I am confident that the IntCal Working Group will continue to work together to provide the user community with ever improving calibration curves under the capable leadership of Christopher Bronk Ramsey.”
MethodVineberg, S. O., Albert, P. G., McLean, D., et al. (2024) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2024.109021 · Cited by 12 · see citing works
Self-citationLIQUID SCINTILLATION COUNTING (LSC)—PAST, PRESENT, AND FUTURE
Hogg, A. G., & Cook, G. (2021) · Radiocarbon · doi:10.1017/rdc.2021.91 · Cited by 12 · see citing works
“Sequential analysis of ancient kauri tree-rings (e.g., Lorrey et al. 2018; Cooper et al. 2021) can provide much higher resolution 14C atmospheric data that any other available archives (e.g., Suigetsu Lake sediments, Bronk Ramsey et al. 2020) or Hulu Cave speleothem deposits (Cheng et al. 2018).”
BackgroundDEVELOPMENT OF THE INTCAL DATABASE
Ramsey, C. B., Adolphi, F., Austin, W. E. N., Bard, É., Bayliss, A., Blaauw, M., Cheng, H., Edwards, R. L., Friedrich, M., Heaton, T., et al. (2023) · Radiocarbon · doi:10.1017/rdc.2023.53 · Cited by 11 · see citing works
Self-citationAlbert, P. G., McLean, D., Buckland, H. M., Suzuki, T., Jones, G., Staff, R. A., Vineberg, S. O., Kitaba, I., Yamada, K., Moriwaki, H., et al. (2023) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2023.108376 · Cited by 11 · see citing works
Self-citationControls on luminescence signals in lake sediment cores: A study from Lake Suigetsu, Japan
Rex, C. L., Staff, R. A., Sanderson, D. C. W., et al. (2022) · Quaternary Geochronology · doi:10.1016/j.quageo.2022.101319 · Cited by 10 · see citing works
“…dataset consisting of over 800 measurements (Staff et al., 2011; Bronk Ramsey et al., 2012) and tephra tie points (e.g., McLean et al., 2018; Albert et al., 2019) constitute the robust core chronology to 50,000 cal BP, which is aligned to the IntCal20 timescale (Bronk Ramsey et al., 2020).”
BackgroundSelf-citationBard, E., & Heaton, T. J. (2021) · Climate of the past · doi:10.5194/cp-2020-164-cc1 · Cited by 10 · see citing works
Self-citationStable isotope evidence of human diet in Mediterranean context during the Last Glacial Maximum
Drucker, D. G., Naito, Y. I., Coromina, N., et al. (2021) · Journal of Human Evolution · doi:10.1016/j.jhevol.2021.102967 · Cited by 9 · see citing works
Comment on cp-2020-164, Bernhard Weninger, 23rd Feb 2021
Bard, E., & Heaton, T. J. (2021) · Climate of the past · doi:10.5194/cp-2020-164-cc4 · Cited by 8 · see citing works
Self-citationReliable radiocarbon dating of fossil pollen grains: It is truly possible
Omori, T., Yamada, K., Kitaba, I., et al. (2023) · Quaternary Geochronology · doi:10.1016/j.quageo.2023.101456 · Cited by 8 · see citing works
Self-citationIntermittent non-axial dipolar-field dominance of twin Laschamp excursions
Hyodo, M., Nakagawa, T., Matsushita, H., Kitaba, I., Yamada, K., Tanabe, S., Bradák, B., Miki, M., McLean, D., Staff, R. A., et al. (2022) · Communications Earth & Environment · doi:10.1038/s43247-022-00401-0 · Cited by 8 · see citing works
Self-citationStaff, R. A., Sanderson, D. C. W., Rex, C. L., et al. (2024) · Quaternary Geochronology · doi:10.1016/j.quageo.2024.101588 · Cited by 8 · see citing works
Self-citationTauseef, M., Ray, E., Paul, D., et al. (2021) · Quaternary International · doi:10.1016/j.quaint.2021.12.014 · Cited by 8 · see citing works
Late Glacial development of lakes and wetland vegetation in a dune area in Central Poland
Lewandowska, A. M., Milecka, K., & Niedzielski, P. (2023) · Acta Palaeobotanica · doi:10.35535/acpa-2023-0001 · Cited by 7 · see citing works
Muschitiello, F., & Aquino‐López, M. A. (2024) · Climate of the past · doi:10.5194/cp-20-1415-2024 · Cited by 6 · see citing works
Hogg, A. G., Lorrey, A. M., TURNEY, C. S. M., Palmer, J., Boswijk, G., & Fenwick, P. (2021) · Quaternary Geochronology · doi:10.1016/j.quageo.2021.101251 · Cited by 6 · see citing works
Rex, C. L., Tyler, J. J., Nagaya, K., et al. (2023) · Quaternary Science Advances · doi:10.1016/j.qsa.2023.100145 · Cited by 5 · see citing works
Self-citationNEW RADIOCARBON DATES FOR THE MIDDLE CHALCOLITHIC PERIOD OF THE CENTRAL ZAGROS, IRAN
Bahranipoor, H. (2023) · Radiocarbon · doi:10.1017/rdc.2023.41 · Cited by 4 · see citing works
Atmospheric radiocarbon levels were highly variable during the last deglaciation
Talamo, S., Friedrich, M., Adolphi, F., Kromer, B., Heaton, T., Cercatillo, S., Muscheler, R., Paleček, D., Pelloni, E., Tassoni, L., et al. (2023) · Communications Earth & Environment · doi:10.1038/s43247-023-00929-9 · Cited by 4 · see citing works
Self-citationKarasiewicz, M. T., Hrynowiecka, A., Weckwerth, P., et al. (2023) · Earth Surface Processes and Landforms · doi:10.1002/esp.5719 · Cited by 4 · see citing works
Radiocarbon calibration: The next generation
Staff, R. A., & Liu, R. (2021) · Science China Earth Sciences · doi:10.1007/s11430-020-9722-x · Cited by 4 · see citing works
Self-citationSarnthein, M., & Blaser, P. (2025) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2025.109181 · Cited by 4 · see citing works
“In turn, Suigetsu age control is based on U/Th-based model ages of Bronk Ramsey et al., 2020 (details of age derivation in Sarnthein et al., 2020 and 2023) (Figs.”
InfluentialVineberg, S. O., Albert, P. G., McLean, D., et al. (2025) · Journal of Volcanology and Geothermal Research · doi:10.1016/j.jvolgeores.2025.108436 · Cited by 3 · see citing works
Self-citationViva, S., Lubritto, C., Cantini, F., et al. (2022) · Archaeological and Anthropological Sciences · doi:10.1007/s12520-022-01515-4 · Cited by 3 · see citing works
Francke, A., Tyler, J. J., Staff, R. A., McLean, D., Nowinski, V., Saito-Kato, M., Tibby, J., Ikehara, M., Yokoyama, Y., Gotanda, K., et al. (2025) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2025.109566 · Cited by 3 · see citing works
Self-citationYang, J., Zhang, G., Zhao, Y., Wei, H., Liu, S., Li, S., Xu, J., Zhang, Y., & Wang, N. (2025) · Journal of Ocean University of China · doi:10.1007/s11802-025-6071-0 · Cited by 2 · see citing works
“The δ 18 O sw values during 12−6.5 kyr (average 0.42‰) were (Bronk et al ., 2020; Heaton et al ., 2020). higher than those during 6.5−1.5 kyr (average 0.15‰).”
InfluentialWIGGLE MATCHING WITH CORRELATIONS
Muzikar, P., & Heaton, T. (2022) · Radiocarbon · doi:10.1017/rdc.2021.106 · Cited by 2 · see citing works
“The calendar ages of the macrofossils from Lake Suigetsu (Bronk Ramsey et al. 2020) also possess covariance, as do the foraminifera from ocean sediments (Bard et al. 2013; Hughen and Heaton 2020) which are linked to the Hulu Cave timescale by the tying of global abrupt palaeoclimatic events (Heaton…”
BackgroundSelf-citationMuschitiello, F. (2021) · doi:10.5194/cp-2021-116 · Cited by 2 · see citing works
Bard, E., & Heaton, T. J. (2021) · Climate of the past · doi:10.5194/cp-2020-164-cc6 · Cited by 3 · see citing works
Self-citationZhang, G., Zhao, Y., Yang, J., Liu, S., Zhang, Z., Guo, X., Cao, G., Yang, L., Li, S., & Zou, L. (2025) · Deep Sea Research Part I Oceanographic Research Papers · doi:10.1016/j.dsr.2025.104553 · Cited by 1 · see citing works
Holocene Land‐Use and Climate Forcing of Ombrotrophic Peatland Dynamics in Northwest Estonia
Roberts, H., Andrews, L., Słowiński, M., et al. (2025) · Journal of Geophysical Research Biogeosciences · doi:10.1029/2025jg009140 · Cited by 1 · see citing works
“Calibrated dates were used to develop an absolute chronology for the whole MUS core using Bayesian age‐depth modeling in OxCal (version 4.4.4; Bronk Ramsey et al., 2020).”
InfluentialMcLean, D., Albert, P. G., Jones, G., et al. (2026) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2026.109837 · Cited by 1 · see citing works
Self-citationVinci, G., Fontana, A., Musina, G., et al. (2022) · Archaeometry · doi:10.1111/arcm.12833 · Cited by 1 · see citing works
Macchia, A., Montorsi, S., Salatino, G., et al. (2023) · Heritage · doi:10.3390/heritage6040188 · Cited by 1 · see citing works
14C plateau tuning – A misleading approach or trendsetting tool for marine paleoclimate studies?Preprint
Sarnthein, M., & Grootes, P. M. (2022) · doi:10.5194/cp-2021-173 · Cited by 1 · see citing works
Calibration of the radiocarbon (14C) record
Reimer, P. J., Blaauw, M., Heaton, T., & Hogg, A. G. (2023) · Elsevier eBooks · doi:10.1016/b978-0-323-99931-1.00043-x · Cited by 1 · see citing works
Self-citationRex, C. L., Staff, R. A., Leng, M. J., Toney, J. L., Pearson, E. J., Tyler, J. J., Swann, G. E. A., Lacey, J. H., Saito-Kato, M., & Nakagawa, T. (2023) · doi:10.31223/x56q3n · Cited by 1 · see citing works
Self-citationBard, E., & Heaton, T. (2021) · Climate of the past · doi:10.5194/cp-2020-164-rc1
Self-citationMuschitiello, F. (2021) · doi:10.5194/cp-2021-116-rc2
Muschitiello, F. (2021) · doi:10.5194/cp-2021-116-rc1
Muschitiello, F. (2021) · doi:10.5194/cp-2021-116-ec1
Muschitiello, F. (2022) · doi:10.5194/cp-2021-116-ac3
Muschitiello, F. (2022) · doi:10.5194/cp-2021-116-ac2
Muschitiello, F. (2022) · doi:10.5194/cp-2021-116-ac1
Bard, É., & Heaton, T. (2021) · Climate of the past · doi:10.5194/cp-2020-164-rc2
Self-citationMuschitiello, F. (2021) · doi:10.5194/cp-2021-116-rc3
Sarnthein, M., & Grootes, P. M. (2022) · doi:10.5194/cp-2021-173-rc1
Sarnthein, M., & Grootes, P. M. (2022) · doi:10.5194/cp-2021-173-cc1
Sarnthein, M., & Grootes, P. M. (2022) · doi:10.5194/cp-2021-173-rc2
Comment on cp-2021-173 _ Response to Review #2
Sarnthein, M. (2022) · doi:10.5194/cp-2021-173-ac3
Sarnthein, M., & Grootes, P. M. (2022) · doi:10.5194/cp-2021-173-cc2
Sarnthein, M. (2022) · doi:10.5194/cp-2021-173-ac1
Comment on cp-2021-173_Response to Review#1
Sarnthein, M. (2022) · doi:10.5194/cp-2021-173-ac2
Bard, É. (2021) · Climate of the past · doi:10.5194/cp-2020-164-ac1
Bard, É., & Heaton, T. (2021) · Climate of the past · doi:10.5194/cp-2020-164-cc3
Self-citationvan der Plicht, J. (2023) · Elsevier eBooks · doi:10.1016/b978-0-323-99931-1.00014-3
Sarnthein, M., Grootes, P. M., & Manfred Mudelsee, A. (2023) · Radiocarbon · doi:10.1017/rdc.2023.47
“In particular, the age tie points provided by these 14 C structures will reduce the problem of properly assigning cal. age estimates by interpolation over long 14 C plateau periods with varying climate and sedimentation conditions down to the scale of a 14 C Fluctuations of the Lake Suigetsu Atmospheric 14 C Record 20…”
InfluentialNowinski, V., Francke, A., Tibby, J., et al. (2025) · Quaternary Science Reviews · doi:10.1016/j.quascirev.2025.109624
Self-citationAzadi, A. (2025) · Parseh Journal of Archaeological Studies · doi:10.61882/pjas.8.30.7
Coeli, L., de Oliveira, F. S., Rodet, M. J., et al. (2026) · Revista Brasileira de Ciência do Solo · doi:10.36783/18069657rbcs20250055
- Authors
- Bronk Ramsey, C., Heaton, T. J., Schlolaut, G., Staff, R. A., Bryant, C. L., Brauer, A., Lamb, H. F., Marshall, M. H., & Nakagawa, T.
- Affiliations
- University of Sheffield (GB)
- Japan Agency for Marine-Earth Science and Technology (JP)
- Scottish Universities Environmental Research Centre (GB)
- GFZ Helmholtz Centre for Geosciences (DE)
- Aberystwyth University (GB)
- Ritsumeikan University (JP)
- ORCID
- Venue
- Radiocarbon
- Publisher
- Cambridge University Press (CUP)
- Published
- 2020-03-25
- Volume
- 62
- Issue
- 4
- Pages
- 989-999
- ISSN
- 0033-8222 (ISSN-L)
- 1945-5755
- OpenAlex
- W2994961501
- Cited by
- 77
- References
- 17
- Citations by year
- 2026: 2 · 2025: 9 · 2024: 3 · 2023: 13 · 2022: 19 · 2021: 23 · 2020: 8
- FWCI
- 9.02
- Type
- journal article
- Language
- en
- Open access
- bronze
- doi.org
- Locations
- Radiocarbon (publishedVersion)
- ENLIGHTEN (Jurnal Bimbingan dan Konseling Islam) (acceptedVersion, cc-by-sa)
- White Rose Research Online (University of Leeds, The University of Sheffield, University of York) (submittedVersion)
- Publication Database GFZ (GFZ German Research Centre for Geosciences) (submittedVersion)
- Funders
- Natural Environment Research Council (NE/F004400/1, NE/H007865/1, NE/D011604/1, NRCF010002, NE/F003056/1, NE/S011854/1, NE/D012996/1)
- Japan Society for the Promotion of Science (15H06905)
- Topics
- Physical Sciences › Earth and Planetary Sciences › Paleontology › Archaeology and ancient environmental studies
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
- Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Tree-ring climate responses
- Keywords
- atmospheric radiocarbon, radiocarbon calibration, Lake Suigetsu, varve chronology, Hulu Cave, paleoclimate archives
About these checks
Registry, retraction, Cites and statistics results are computed, not judged, with one exception: a printed reference that no index lists is read once by a model before it counts as a citation error. Claims are extracted by a model and kept only when their quote appears verbatim in the text; each cited source is then checked, with a model’s help, for whether it says what the claim relies on. Those verdicts can be wrong — read the claim’s quote and the cited source before relying on one.
Claims read under definition version 3 (extract-v3) on 2026-09-27.
Classified by jev-1.13-20260917 (gold-guideline-v0.2) on 2026-09-27.
Cited sources are checked by gpt-6-sol.
Statistics and arithmetic are recomputed, not judged.
Confidence bands are shown only for fields calibrated on our annotated test set. None is calibrated yet, so no band is shown.
What counts as a claim ›How we measure confidence ›How we check this ›
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