Difference between revisions of "Category:Chronologies Working Group"
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=== Radiocarbon === | === Radiocarbon === | ||
− | The following came from P. Reimer by way of T. Guilderson. | + | The following came from P. Reimer by way of T. Guilderson. |
==== Data standardization and reporting ==== | ==== Data standardization and reporting ==== | ||
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* F14C (13C and background correction applied)<ref> This is slightly different than Stuiver and Polach who have "D14C" as the optional parameter. </ref>: | * F14C (13C and background correction applied)<ref> This is slightly different than Stuiver and Polach who have "D14C" as the optional parameter. </ref>: | ||
− | We suggest the inclusion of the background and d13C corrected Fraction modern (F14C) as it is the primary reported value. In the past there has been some inconsistencies in the literature/laboratories with regards to fraction modern. By using/requesting F14C you will be explicitly requesting 13C and background corrected Fraction Modern (aka F14C, as per Reimer et al.[2004]) as intended by Stuiver and Polach (1977). | + | We suggest the inclusion of the background and d13C corrected Fraction modern (F14C) as it is the primary reported value. In the past there has been some inconsistencies in the literature/laboratories with regards to fraction modern. By using/requesting F14C you will be explicitly requesting 13C and background corrected Fraction Modern (aka F14C, as per Reimer et al.[2004]) as intended by Stuiver and Polach (1977). |
* Correction applied to radiocarbon date prior to, or during conversion to calibrated age: | * Correction applied to radiocarbon date prior to, or during conversion to calibrated age: | ||
** marine reservoir effect: | ** marine reservoir effect: | ||
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* Calibration or conversion to calibrated ages: | * Calibration or conversion to calibrated ages: | ||
As of present, the international radiocarbon community recommends the use of the INTCAL13 (aka Marine 13<ref>P. J. Reimer et al., 2013. INTCAL13 and MARINE13 Radiocarbon age calibration curves, 0-50,000 years CAL BP. Radiocarbon, 55, 1869-1887.</ref>) and SHCAL13 <ref>A. G. Hogg, et al., 2013. SHCal13 Southern Hemisphere calibration, 0-50,000 years cal BP. Radiocarbon 55, 1889-1903.</ref> data products. | As of present, the international radiocarbon community recommends the use of the INTCAL13 (aka Marine 13<ref>P. J. Reimer et al., 2013. INTCAL13 and MARINE13 Radiocarbon age calibration curves, 0-50,000 years CAL BP. Radiocarbon, 55, 1869-1887.</ref>) and SHCAL13 <ref>A. G. Hogg, et al., 2013. SHCal13 Southern Hemisphere calibration, 0-50,000 years cal BP. Radiocarbon 55, 1889-1903.</ref> data products. | ||
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* Calibration of post-bomb (post 1954/1957) samples should also include the calibration data-set utilized, description/reference of any corrections applied, and the software/algorithm utilized to convert the F14C data to years AD. | * Calibration of post-bomb (post 1954/1957) samples should also include the calibration data-set utilized, description/reference of any corrections applied, and the software/algorithm utilized to convert the F14C data to years AD. | ||
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=== Ice layers === | === Ice layers === | ||
Role of flow models. | Role of flow models. | ||
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+ | == Age-modeling software == | ||
+ | |||
+ | |||
+ | Nick/Liz: please provide guidelines on how age modeling software should be reported. | ||
+ | Content: | ||
+ | * method (e.g. Bacon, OxCal, BChron, BAM) | ||
+ | * version | ||
+ | * parameters | ||
+ | |||
+ | Form: what does this look like in JSON? | ||
== Polls == | == Polls == |
Revision as of 21:24, 15 September 2016
Contents
Overview
In the Linked Earth context, a working group (WG) is a self-organized coalition of knowledgeable experts, whose activities are governed herewith. This page is dedicated to the discussion of data and metadata standards for chronologies, and aims to formulate a set of recommendations for such a standard.
This WG needs to work closely with other WGs, as constraints will vary by archive. Nevertheless, some aspects are common enough that it is worth pursuing some general recommendations, and devise ad hoc adjustments for individual archives if need be. It is recommended that every WG coordinator join this WG to keep track of discussions.
Members of 'Chronologies Working Group'
This working group has 18 members.
Specific tasks
We recommend that discussions focus on the following techniques, and explore potential commonalities.
For each chronology type, we recommend:
- structuring discussions around what scientific questions one would want to ask of the data
- listing essential, recommended, and optional information for:
- the age models themselves
- the chronological measurements (ChronData tables, in LiDP/LinkedEarth parlance)
- their uncertainties, and what those numbers correspond to (e.g. 1-sigma or 2-sigma?)
- provide an ideal chronology table, so the community knows what to report and how to report it.
- provide separate recommendations for new and legacy datasets
While it is recognized that most real-word chronologies are of mixed types (e.g. a Holocene lake sediment chronology may blend radiocarbon dates, 210Pb dates, and volcanic ash markers), it is critical to first define guidelines for how to report pure chronologies. Once the foundations are sound, they will be easier to compose together.
Tie-point chronologies
Radiocarbon
The following came from P. Reimer by way of T. Guilderson.
Data standardization and reporting
Key references: Stuiver & Polach [1977] [1] and Reimer et al., [2004] [2]
Sample Information (metadata):
Sample ID, type/matrix, location (lat, lon, masl/mbsl altitude/depth, depth/height in section/core and referenced), etc.
Radiocarbon Data Table
- Chemical pretreatment/preparation (oxidation, chemical leach (%), a/b/a, soxhlet, ultrafiltration, none, etc)
- Method: GPC, LSC, AMS, etc
- Laboratory ID# (eg. OS####; CAMS####; QUB####)
- delta-13C ratio actual/estimated (PDB/V-PDB) [3]
- Conventional radiocarbon age as years BP and one-sigma standard deviation [4]
- F14C (13C and background correction applied)[5]:
We suggest the inclusion of the background and d13C corrected Fraction modern (F14C) as it is the primary reported value. In the past there has been some inconsistencies in the literature/laboratories with regards to fraction modern. By using/requesting F14C you will be explicitly requesting 13C and background corrected Fraction Modern (aka F14C, as per Reimer et al.[2004]) as intended by Stuiver and Polach (1977).
- Correction applied to radiocarbon date prior to, or during conversion to calibrated age:
- marine reservoir effect:
- Marine reservoir age, ± one-sigma sd (or square root of the variance) uncertainty, reference/source
- DELTA_R value, ± one-sigma sd (or square root of the variance) uncertainty, reference/source
- marine reservoir effect:
- hard/soft water effect: value, ± one-sigma sd (or square root of var) uncertainty, reference/source
- other corrections: value (14C years), ± one-sigma sd (or square root of var), reference/source
- Calibration or conversion to calibrated ages:
As of present, the international radiocarbon community recommends the use of the INTCAL13 (aka Marine 13[6]) and SHCAL13 [7] data products.
- Calibration of post-bomb (post 1954/1957) samples should also include the calibration data-set utilized, description/reference of any corrections applied, and the software/algorithm utilized to convert the F14C data to years AD.
Lead
no known existing standard/template
U-series
Layer-counted chronologies
Comboul et al[8] argue that it is critical to report uncertainties in layer-counted chronologies, and that these can be expressed in terms of an undercounting and overcounting rate. However, there needs to be agreement about how to measure and report this rate for various archives.
Varves
Growth rings
Trees, corals, speleothems
Ice layers
Role of flow models.
Age-modeling software
Nick/Liz: please provide guidelines on how age modeling software should be reported.
Content:
- method (e.g. Bacon, OxCal, BChron, BAM)
- version
- parameters
Form: what does this look like in JSON?
Polls
Here are polls that the group might want to consider:
For NEW DATASETS: (this is a dummy poll; please update)
You are not entitled to view results of this poll.
For LEGACY DATASETS:
You are not entitled to view results of this poll.
References
- ↑ Minze Stuiver and H. A. Polach, 1977. Discussion: Reporting of 14C Data. Radiocarbon 19, 3, 355-363.
- ↑ Paula J. Reimer, T. A. Brown, and R. W. Reimer, 2004. Discussion: Reporting and calibration of post-bomb 14C Data. Radiocarbon, 46, 3, 1299-1304.
- ↑ Note, the AMS measured 13C has low precision (a few per mil, compared to IRMS). Most AMS labs do NOT report the machine measured 13C value because it is frequently misused. This should be estimated as per SP77 or an IRMS-based value/estimate.
- ↑ Note, that by definition, conventional radiocarbon age is the Libby based age. Most AMS laboratories report 1-sigma sd of the analysis or the 1-sigma sd reproducibility for similar aged/sized material.
- ↑ This is slightly different than Stuiver and Polach who have "D14C" as the optional parameter.
- ↑ P. J. Reimer et al., 2013. INTCAL13 and MARINE13 Radiocarbon age calibration curves, 0-50,000 years CAL BP. Radiocarbon, 55, 1869-1887.
- ↑ A. G. Hogg, et al., 2013. SHCal13 Southern Hemisphere calibration, 0-50,000 years cal BP. Radiocarbon 55, 1889-1903.
- ↑ Comboul, M., J. Emile-Geay, M. N. Evans, N. Mirnateghi, K. M. Cobb, and D. M. Thompson (2014), A probabilistic model of chronological errors in layer-counted climate proxies: applications to annually banded coral archives, Climate of the Past, 10(2), 825–841, doi:10.5194/cp-10-825-2014
Pages in category "Chronologies Working Group"
This category contains only the following page.