Difference between revisions of "Category:Marine Sediment Working Group"
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| − | 'Additional' proxy data is widely measured along with the primary proxy data of interest (here, the primary data being the data discussed and interpreted in the manuscript. Often, this 'additional' data is not made publicly available, despite its potential utility for the community. For example, d13C is almost always measured along d18O in carbonates, many other trace element ratios are often measured alongside Mg/Ca in foraminifera, and multiple elements are measured by XRF core scanners. If it can be demonstrated that this 'additional' data has been measured accurately and precisely (i.e. by the reporting of standards), archiving this 'additional' data, along with the primary data, would allow its potential utility to be exploited. | + | 'Additional' proxy data is widely measured along with the primary proxy data of interest (here, the primary data being the data discussed and interpreted in the manuscript). Often, this 'additional' data is not made publicly available, despite its potential utility for the community. For example, d13C is almost always measured along d18O in carbonates, many other trace element ratios are often measured alongside Mg/Ca in foraminifera, and multiple elements are measured by XRF core scanners. If it can be demonstrated that this 'additional' data has been measured accurately and precisely (i.e. by the reporting of standards), archiving this 'additional' data, along with the primary data, would allow its potential utility to be exploited. |
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Revision as of 10:36, 26 June 2017
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 marine sedimentary archives (see this page for a definition of Marine Sediment Archive), and aims to formulate a set of recommendations for such a standard.
Members
The group currently has one coordinator, Julie Richey (USGS)
Members of 'Marine Sediment Working Group'
This working group has 16 members.
Specific tasks
We recommend that discussions focus on the following considerations, and explore potential commonalities.
For each observation type, we recommend:
- structuring discussions around what scientific questions one would want to ask of the data
- listing essential, recommended, and desired information for:
- the measurements themselves
- any inference made from the measurements (e.g. calibration to temperature)
- the underlying uncertainties, and what those numbers correspond to (e.g. 1-sigma or 2-sigma?)
- providing an ideal data table, so the community knows what to report and how to report it.
- providing separate recommendations for new and legacy datasets, and for how to label measured and inferred variable (e.g. Mg/Ca is measured, temperature is inferred)
- thinking about how the rest of the paleoscience community, or other (non)scientists may make use of the data you describe.
Marine sediments are a very ubiquitous archive on which many types of observations are made, and involving thousands of people around the world. It seems wise for this WG to rally around sub-groups start dedicated to data standards about the following sensors/observation types.
Previous standardization efforts
A discussion regarding paleoclimate data standards was started during the PMIP Ocean Workshop: Understanding changes since the Last Glacial Maximum (hereafter, PMIP_LGM) in Corvallis, OR in December 2013. Given the expertise of the working group members, the discussion focus on sedimentary archives. Meeting notes can be found here and summarized in the sections below.
The recommendations made at the workshop concerned new datasets only. It was recognized that different sets of standards would be necessary for legacy datasets.
Types of Data
There are three principle types of data that are relevant for the paleoceanography/paleoclimatology community:
Original data values
this would include raw values of all variables measured or otherwise determined on the substrate of interest, recorded against an unambiguous sample identifier (for instance, depth in the archive). This includes age control points (ACP) used to derive the age model of the paleo-time series, including radioisotopes (14C, excess 210Pb), and benthic stack comparison. All data that are reported for the first time in a scientific publication should be treated as original. The procedure of obtaining original data should be documented such as to allow full replication of the results. In the LinkedEarth Ontology, the original data values are referred as Category:MeasuredVariable_(L).
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Should the "unique sample identifier" identified at the PMIP_LGM workshop be:
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There were 7 votes since the poll was created on 23:13, 7 March 2017.
poll-id 36C56A4F3693990E0936AB6AC7F8F158
At the PMIP_LGM workshop, it was proposed that the unique sample identifier consists of the name, geographical coordinates, water depth of the sediment core in addition to the position of the analyses sediment segment in the core. Is this labelling:
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There were 7 votes since the poll was created on 23:27, 7 March 2017.
poll-id 14714BE25ABC4C1A7B14ED87FE6B20B1
Depth can be problematic as a unique identifier since there are several to calculate or report depth in a sample (i.e., top-depth, mid-depth, depth interval.) and IODP uses several depth scales.
In the case where depth is reported for sediment cores, should we report:
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poll-id 27DAE87F3370E83700CE16B6457F9284
Deborah Khider (talk) 15:29, 7 March 2017 (PST): I probably forgot ways of expressing depth, please add comments below.
Derived data values
this category refers to values of variables derived from other variables, derived or raw, original or compiled, reported against an unambiguous sample identifier and accompanied with a documentation of the derivation procedure such as to allow full replication of the result. This category includes algorithms of any kind relating depth to age that have been used to assign ages to values of raw or derived variables. In the LinkedEarth Ontology, derived data values are referred to as Category:InferredVariable_(L).
The derivation procedure is contained in the Category: CalibrationModel_(L).
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For marine sediment cores, should the calibration model be:
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There were 7 votes since the poll was created on 00:30, 8 March 2017.
poll-id 7C4AE17FE47EA87830F1BA07B51F59C9
Should the code used in the calibration of marine sedimentary records be:
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There were 8 votes since the poll was created on 00:30, 8 March 2017.
poll-id AB5F5404199B91D8313625A32343B5A2
Should the calibration Publication information be:
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There were 7 votes since the poll was created on 19:44, 8 March 2017.
poll-id 32117782905226D0ADDA2F1557EA3F92
Compilation of data values
this refers to raw values of all variables from published sources, gathered for the purpose of quantitative treatment, recorded against an unambiguous sample identifier and labelled with an unambiguous reference to the publication where such data were originally presented. Reporting of data compilations is required wherever these are used to derive patterns or variables from the data other than those reported in the original publication.
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Archived poll
Should compilation of previous work involving marine sediment records report:
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There were 8 votes since the poll was created on 00:31, 8 March 2017.
poll-id 54ACE3242CF87B5F02B413BD62B72E8D
New poll includes both option:
Should compilation of previous work involving marine sediment records report:
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There were 5 votes since the poll was created on 15:24, 29 March 2017.
poll-id 7FC73AF3379418CA402AD31E142E9BB5
LinkedEarth identifies each series using Property:HasVariableID_(L)
Archiving
The following recommendations were made at the PMIP_LGM workshop:
The data should be archived in easily accessible database administered by an editorial board. The database should included on on-line system for (1) the reporting of errors, (2) a community-driven quality flag system, and (3) the update of datasets as new data become available. Updates to a particular dataset should be assigned a version number with a link to the old and new references. The editorial board should also be tasked in identifying and archiving older datasets.
For versioning of datasets, see the proposed LinkedEarth standard here and use the Discussion page to comment.
'Additional' proxy data is widely measured along with the primary proxy data of interest (here, the primary data being the data discussed and interpreted in the manuscript). Often, this 'additional' data is not made publicly available, despite its potential utility for the community. For example, d13C is almost always measured along d18O in carbonates, many other trace element ratios are often measured alongside Mg/Ca in foraminifera, and multiple elements are measured by XRF core scanners. If it can be demonstrated that this 'additional' data has been measured accurately and precisely (i.e. by the reporting of standards), archiving this 'additional' data, along with the primary data, would allow its potential utility to be exploited.
Should any 'additional' proxy data measured along the primary data of interest be archived with the dataset?
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There were 4 votes since the poll was created on 17:19, 21 June 2017.
poll-id 50C99E5801C667F880C7B011C9E324F9
Marine Sediment Standards
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Collection Method: Gear Type | D | Some coring techniques are known to stretch/compress the cores (i.e. Marion Dufresne piston core) | Deborah Khider (talk) 16:17, 7 March 2017 (PST) |
| Collection method: Volume of sediment analyzed | D | May not be useful for all types of data measured on sediment cores. If deemed recommend or essential, insert comment/poll in appropriate section | Deborah Khider (talk) 16:17, 7 March 2017 (PST) |
| Collection method: Sampling methods | D | u-channel, syringe, slice | Deborah Khider (talk) 16:17, 7 March 2017 (PST) |
| Instrumentation | D | How were the MeasuredVariables measured? Desired for standard analytical techniques. Should be essential/recommended for new techniques | Deborah Khider (talk) 16:23, 7 March 2017 (PST) |
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For marine sediments, the gear type used for the collection of the archive should be:
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There were 5 votes since the poll was created on 18:00, 17 March 2017.
poll-id 7DC5CE9086A322329E11688B7BC1D130
For studies based on marine sediments, should the volume of sediment analyzed be:
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There were 5 votes since the poll was created on 18:00, 17 March 2017.
poll-id B7C3AB70BF578DC1DD84577B9927261C
For marine sediment studies, should the instrument used for standard analytical techniques be:
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There were 5 votes since the poll was created on 18:00, 17 March 2017.
poll-id 4ADE31D2B4F457D8E7F252760213ACF7
For marine sediment studies, should the instrument used in new protocols be:
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There were 4 votes since the poll was created on 18:00, 17 March 2017.
poll-id D90ACBF4A9DE1C00F457763F37E748C2
Geochemical Data
Bulk Sediment Geochemistry
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | Kau (talk) 13:34, 7 March 2017 (PST) |
| Property:Wgs84:Alt (L) (Depth) | R | Especially for deep-sea drilling sediments, water depths can be important to assess various biogeochemical properties and parameters of stable isotopic parameters | Kau (talk) 13:34, 7 March 2017 (PST) |
| Sample Pretreatment | R | Freeze-dried, ground in mortar and pestle, acid-washed, microwave digestion, pressed pellet, glass bead, sieved, scraped core surface and x-ray transparent film, thin sections [single or double-polished, thickness, epoxy type, mounting medium] | Julie (talk), 28 March 2017 following suggestion of Jason Addison |
| Analytical Method | E | ICP-MS, XRF, scanning XRF, wet chemistry spectrophotometry, INAA, micro-XRF, electron microprobe, HCNS elemental analyzer, carbonate coulometry | Julie (talk), 28 March 2017 following suggestion of Jason Addison |
| Measurement Parameter | E | i.e., Mg to U, Mo, opal, TOC, CaCO3, C/N, etc. | Julie (talk), 28 March 2017 following suggestion of Jason Addison |
| Units of measurement | E | wt%, ppm, x-ray intensities (counts per second) | Julie (talk), 28 March 2017 following suggestion of Jason Addison |
| Method Reference | R | Literature Reference for analytical method | Julie (talk), 28 March 2017 following suggestion of Jason Addison |
| Environmental Parameter | D | For instance, is the geochemical proxy sensitive to upwelling intensity, salinity, temperature, terrestrial input, etc. This is the Category:Interpretation_(L) field in the current LinkedEarth ontology. | Julie (talk), 28 March 2017 |
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For new datasets, when reporting bulk sediment measurements, should the sample pretreatment be:
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There were 3 votes since the poll was created on 18:45, 29 March 2017.
poll-id C6EF3F00F2DDA8589269B3BE267B8FA1
For new datasets, when reporting bulk sediment measurements, should the analytical method be:
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There were 2 votes since the poll was created on 18:46, 29 March 2017.
poll-id 41D90357E253A3765871BDF6CC01CC6C
For new datasets, when reporting bulk sediment measurements, should the measurement parameter be:
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There was one vote since the poll was created on 18:46, 29 March 2017.
poll-id F6F0F777A698635D1E87AEFAF411355D
For new datasets, when reporting bulk sediment measurements, should the units of measurement be:
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There were 3 votes since the poll was created on 18:46, 29 March 2017.
poll-id 73B732C7ED8CD29BAF2795475570ECDF
For new datasets, when reporting bulk sediment measurements, should the method reference be:
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There were 3 votes since the poll was created on 18:47, 29 March 2017.
poll-id E8C01BE46009C3A955B1967F67702DAF
For new datasets, when reporting bulk sediment measurements, should the environmental parameter be:
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There were 2 votes since the poll was created on 18:47, 29 March 2017.
poll-id F9689133926C97F3942EDF3FCE1D491A
Foraminiferal Geochemistry
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For foraminiferal geochemistry work, should information about the taxonomy being followed on top of the genus/species information be:
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There were 4 votes since the poll was created on 00:25, 8 March 2017.
poll-id 0A5106C96F47C17DC1B065830CA5D1B6
Stable isotopes
In the following table, enter the metadata that you'd wish every member of the stable isotope community would enter to make their data reproducible. To add more lines, follow this guide. For a definition of Essential (E)/ Recommended (R)/ Desired (D), see this page.
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | Kau (talk) 13:34, 7 March 2017 (PST) |
| Property:Wgs84:Alt (L) (Depth) | R | Especially for deep-sea drilling sediments, water depths can be important to assess various biogeochemical properties and parameters of stable isotopic parameters | Kau (talk) 13:34, 7 March 2017 (PST) |
| Property:SensorGenus_(L) Property:SensorSpecies_(L) | E | Species information needed to infer which section of the water column is being recorded | Kau (talk) 13:34, 7 March 2017 (PST) |
| Cleaning Methodology(oxidative vs reductive) | R | Useful to correct for offsets, especially for compilation work although a quick plot can often help figure out the cleaning methodology | Kau (talk) 13:34, 7 March 2017 (PST) |
| Cleaning Methodology reference | D | The exact reference to the protocol used for cleaning. Added to differentiate between the actual methodology and the specific protocol. | Deborah Khider (talk) 11:05, 17 March 2017 (PDT) following a conversation with Jfehrenbacher |
| Sample Depth | E | Positional information needed to relate the samples back to the archive | Kau (talk) 13:34, 7 March 2017 (PST) |
| ChonDataTable | E for new datasets/ R for legacy datasets | The raw radiocarbon, tie points, 210Pb measurements should be made available so that age models can be updated in light of new calibration curves or new age modeling techniques | Kau (talk) 13:34, 7 March 2017 (PST) |
| Number of specimens utilized per sample | R | The number of foraminiferal tests used per sample can be used to understand the sampling uncertainity associated with the measurements based on the signal-to-noise ratio of the climate signal at the location (planktic foraminifera live for 2-4 weeks) | Kau (talk) 13:34, 7 March 2017 (PST) |
| Property:Standard (L) | E | The standard against which the measurements are reported (especially for d18O). VBDP vs VSMOW | Deborah Khider (talk) 13:41, 7 March 2017 (PST) |
| Analytical Precision | R | The machine precision based on reproducability of standards | Kau (talk) 13:49, 7 March 2017 (PST) |
| Size Fraction | R | Stable isotopes ratios have been shown to vary by size fraction in several studies | Deborah Khider (talk) 15:48, 7 March 2017 (PST) |
| Method of sediment disintegration and washing | D | Brought up at the PMIP_LGM meeting | Deborah Khider (talk) 16:19, 7 March 2017 (PST) |
| Correction applied/Equilibration offset | R | For instance, correction for offsets in benthic species (critical for compilation work) | Deborah Khider (talk) 16:27, 7 March 2017 (PST) |
| Seasonality | R | Necessary for compilation work especially as to not combine summer and winter ProxySensors | Deborah Khider (talk) 11:39, 8 March 2017 (PST) |
| Habitat Depth | R | Which part of the water column is being represented | Deborah Khider (talk) 11:39, 8 March 2017 (PST) |
To gather rapid feedback on whether the proposed metadata should be essential, recommended or optional, answer the polls below:
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For stable isotopes in foraminifera, should the location information (and water depth) be:
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There were 6 votes since the poll was created on 21:45, 7 March 2017.
poll-id 45FF02339429C6C462C391EC3CEE963C
For stable isotopes in foraminifera, should the sensor genus/species information be:
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There were 5 votes since the poll was created on 21:45, 7 March 2017.
poll-id F4DAE98FBB4889111B360750A225B6C6
For stable isotopes in foraminifera, should the depth (position of the measurement in the archive) information be:
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There were 6 votes since the poll was created on 21:45, 7 March 2017.
poll-id 9C0329A43D83FE74AB4BBFAF34E3676B
For stable isotopes in foraminifera, should the ChonMeasurementTable information be:
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There were 4 votes since the poll was created on 21:45, 7 March 2017.
poll-id 9E1154CAC198A5C2E9756598EC5FB134
For stable isotopes in foraminifera, should the numbers of specimens utilized be:
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There were 4 votes since the poll was created on 21:45, 7 March 2017.
poll-id E46F4CC0B5B309E1DD2E2019C99AD8E2
For stable isotopes in foraminifera, should the property standard reported be:
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There were 4 votes since the poll was created on 21:52, 7 March 2017.
poll-id 2F10B4A70435835B8464A443435D56CF
For stable isotopes in foraminifera, should the analytical precision reported be:
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There were 4 votes since the poll was created on 21:52, 7 March 2017.
poll-id E198E4FAF1A9E8358CE0BBA841C3BA4F
For stable isotopes in foraminifera, should size fraction be:
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There were 4 votes since the poll was created on 23:48, 7 March 2017.
poll-id 8ED5D3D55F5D5E0D577F05470CA3D485
For stable isotopes in foraminifera, should the method of sediment disintegration be:
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There were 4 votes since the poll was created on 19:37, 8 March 2017.
poll-id C03DF076795FD835C666874277A553FB
For stable isotopes in foraminifera, should the applied correction/equilibrium offset be:
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There were 4 votes since the poll was created on 19:38, 8 March 2017.
poll-id 4597E75365B81B5AB6E810309E50C28D
For stable isotopes in foraminifera, should the seasonality be:
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There were 5 votes since the poll was created on 19:38, 8 March 2017.
poll-id AE66893582EBBE5745D27A2288FAAB06
For stable isotopes in foraminifera, should the habitat depth be:
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There were 5 votes since the poll was created on 19:38, 8 March 2017.
poll-id E463DF6713337347458F54AECA2080C7
Trace Metals
From Jfehrenbacher:
"The properties described under Mg/Ca can be used for the other trace elements."
Additional information may be required for other trace elements (for example, for B/Ca were the samples cleaned in a hood with a B-free HEPA filter).
Mg/Ca
In the following table, enter the metadata that you'd wish every member of the Mg/Ca community would enter to make their data reproducible. To add more lines, follow this guide. For a definition of Essential (E)/ Recommended (R)/ Desired (D), see this page.
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | Deborah Khider (talk) 12:37, 17 February 2017 (PST) |
| Property:Wgs84:Alt (L) (Depth) | E | Water depth can be useful to get an idea of dissolution in the core. Especially for deep-sea drilling sediments, water depths can be important to assess various biogeochemical properties and parameters of stable isotopic parameters | Kau (talk) 13:39, 7 March 2017 (PST) |
| Property:SensorGenus_(L) Property:SensorSpecies_(L) | E | Species information needed to infer which section of the water column is being recorded | Deborah Khider (talk) 12:37, 17 February 2017 (PST) |
| Cleaning Methodology (oxidative vs reductive) | E for new datasets/ R or D for legacy datasets. | Useful to correct for offsets, especially for compilation work although a quick plot can often help figure out the cleaning methodology | Deborah Khider (talk) 12:37, 17 February 2017 (PST) Changed by Deborah Khider (talk) 11:22, 17 March 2017 (PDT) after a discussion with Jfehrenbacher |
| Cleaning methodology reference | D or R for both legacy and new datasets | The reference describing the specific protocol being followed (i.e., Barker et al., Martin and Lea...). Allows to differentiate between the general method being followed and the actual protocol | Deborah Khider (talk) 11:22, 17 March 2017 (PDT) after a discussion with Jfehrenbacher |
| Sample Depth | E | Positional information needed to relate the samples back to the archive | Deborah Khider (talk) 12:37, 17 February 2017 (PST) |
| ChonDataTable | E for new datasets/ R for legacy datasets | The raw radiocarbon, tie points, 210Pb measurements should be made available so that age models can be updated in light of new calibration curves or new age modeling techniques | Deborah Khider (talk) 12:37, 17 February 2017 (PST) |
| Number of specimens utilized per sample | R | The number of foraminiferal tests used per sample can be used to understand the sampling uncertainity associated with the measurements based on the signal-to-noise ratio of the climate signal at the location (planktic foraminifera live for 2-4 weeks) | Kau (talk) 13:17, 7 March 2017 (PST) |
| Analytical Precision | D | Uncertainty in the measurements | Deborah Khider (talk) 13:51, 7 March 2017 (PST) |
| Size fraction | R | Mg/Ca and other trace element ratios have been shown to vary with specimens size | Deborah Khider (talk) 15:49, 7 March 2017 (PST) |
| Method of sediment disintegration and washing | D | Brought up at the PMIP_LGM workshop | Deborah Khider (talk) 16:20, 7 March 2017 (PST) |
| Correction applied/Equilibrium offset | R | For instance, correction for offsets for cleaning methodologies (critical for compilation work) | Deborah Khider (talk) 16:27, 7 March 2017 (PST) |
| Seasonality | R | Necessary for compilation work especially as to not combine summer and winter ProxySensors | Deborah Khider (talk) 11:39, 8 March 2017 (PST) |
| Habitat Depth | R | Which part of the water column is being represented | Deborah Khider (talk) 11:39, 8 March 2017 (PST) |
| Contamination indicators | R | Ancillary trace element data to asses contamination (e.g. Al/Ca, Mn/Ca, Fe/Ca) | William Gray (talk) 17:12, 17 March 2017 (GMT) |
| Property:Standard (L) | D | The value of any certified reference material analysed by the lab (e.g. ECRM 752-1) | William Gray (talk) 17:24, 17 March 2017 (GMT) |
| "Raw" Mg/Ca data | E | It is essential the Mg/Ca data are available - not just derived temperature values | William Gray (talk) 18:12, 20 March 2017 (GMT) |
To gather rapid feedback on whether the proposed metadata should be essential, recommended or optional, answer the polls below:
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For Mg/Ca in foraminifera, should the location information (especially in relation to water depth) be:
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There were 5 votes since the poll was created on 21:26, 7 March 2017.
poll-id 30B1E1BEA2083F7429E59527F2DBF8A8
For Mg/Ca in foraminifera, should the sensor genus/species information be:
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There were 5 votes since the poll was created on 21:26, 7 March 2017.
poll-id 036FE79A6C27842348B489B982D516D8
Should the cleaning methodology be considered:
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There were 7 votes since the poll was created on 20:07, 7 November 2016.
poll-id 5D88039254CA2FE4746A7A2515CDDBCA
More specific polls on cleaning methodology (see table above):
For new datasets, should the cleaning methodology for for foraminifera trace elements (oxidative vs reductive) be:
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There were 4 votes since the poll was created on 18:20, 17 March 2017.
poll-id 59DE784ACBD8E8A6B0FBFF57193A9B38
For legacy datasets, should the cleaning methodology for for foraminifera trace elements (oxidative vs reductive) be:
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There were 4 votes since the poll was created on 18:21, 17 March 2017.
poll-id 71165B5A66BC5CE5CE3BB5950E0F520D
Should the cleaning methodology reference (i.e. the specific protocol) for for foraminifera trace elements be:
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There were 4 votes since the poll was created on 18:21, 17 March 2017.
poll-id 21D6862F3CFB88611ED5780BED262E57
For Mg/Ca in foraminifera, should the depth (position of the measurement in the archive) information be:
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There were 5 votes since the poll was created on 21:26, 7 March 2017.
poll-id 5E204D0FB2EBB8A0B8A78A229261EC4E
For Mg/Ca in foraminifera, should the ChonMeasurementTable information be:
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There were 5 votes since the poll was created on 21:26, 7 March 2017.
poll-id 40ECF6DB8C722909F39479BD19C3F2CD
For Mg/Ca in foraminifera, should the numbers of specimens utilized be:
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There were 4 votes since the poll was created on 21:46, 7 March 2017.
poll-id 9D1700879FA581737C1F779C8C0BAB9E
For Mg/Ca in foraminifera, should the analytical precision reported be:
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There were 4 votes since the poll was created on 23:49, 7 March 2017.
poll-id E59628A325A1D182243A5EAF06D70679
For Mg/Ca in foraminifera, should the size fraction be:
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There were 4 votes since the poll was created on 23:49, 7 March 2017.
poll-id 775A08139E4A98D799AA31AA05C7D200
For Mg/Ca in foraminifera, should the method of sediment disintegration be:
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There were 4 votes since the poll was created on 19:39, 8 March 2017.
poll-id 5CEF1475190DAD116F1B4CBC88281438
This question is unclear - what does equilibrium refer to for Mg/Ca?
Correction to changes in seawater Mg/Ca ratio over time Deborah Khider (talk) 17:04, 31 March 2017 (PDT)
For Mg/Ca in foraminifera, should the applied correction/equilibrium offset be:
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There were 3 votes since the poll was created on 19:39, 8 March 2017.
poll-id B2D384EDF4B84E02B35DD8B24FDF2109
For Mg/Ca in foraminifera, should the seasonality be:
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There were 4 votes since the poll was created on 19:39, 8 March 2017.
poll-id C43DEA2CB3276A48B899AC1C0AF4204A
For Mg/Ca in foraminifera, should the habitat depth be:
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There were 4 votes since the poll was created on 19:39, 8 March 2017.
poll-id BB59D36FDAEE93B0CE37426CD39AA9A2
For Mg/Ca in foraminifera, should contamination indicators (Al/Ca, Mn/Ca, Fe/Ca) be:
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There were 4 votes since the poll was created on 17:05, 17 March 2017.
poll-id A8E7999FB8F8C9C39260BE14FD789CA5
Boron isotopes
In the following table, enter the metadata that you'd wish every member of the stable isotope community would enter to make their data reproducible. To add more lines, follow this guide. For a definition of Essential (E)/ Recommended (R)/ Desired (D), see this page.
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Property:Wgs84:Alt (L) (Depth) | R/E | Water depth is Recommended for planktonic foraminifera and Essential for benthic foraminferal data | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Property:SensorGenus_(L) Property:SensorSpecies_(L) | E | Planktonic species show different relationships to d11B of borate and infuanal benthic species show offsets from seawater values | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Sample Depth | E | Positional information needed to relate the samples back to the archive | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| ChonDataTable | E for new datasets/ R for legacy datasets | The raw radiocarbon, tie points, 210Pb measurements should be made available so that age models can be updated in light of new calibration curves or new age modeling techniques | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Analytical Method | E | The analytical method used for seperation (e.g. Amberlite columns, micro sublimation ) and analysis (MC-ICP-MS, NTIMS) | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Sample size | R | ng of Boron analysed | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Property:Standard (L) | E | The values for certified reference materials, both boric acids and carbonates (e.g. JCP, JCT, AE121) | William Gray (talk) 17:29, 17 March 2017 (GMT) |
| Analytical precision | E | Precision based on reproducibility of standards, may be a function of sample size | William Gray (talk) 17:29, 17 March 2017 (GMT) |
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For boron isotopes on foraminifera, should the location of the archive be:
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There were 0 votes since the poll was created on 19:58, 25 April 2017.
poll-id 51C2D4D8F4E9FC1E5F00861065FA5A0D
For boron isotopes on planktonic foraminifera, should the water depth be:
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There were 0 votes since the poll was created on 19:59, 25 April 2017.
poll-id D7D75AB7A3001683AAC4BB7559BC9CA1
For boron isotopes on benthic foraminifera, should the water depth be:
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There were 0 votes since the poll was created on 19:59, 25 April 2017.
poll-id 12B59751B18C5A1FAC746485C5993D99
For boron isotopes on foraminifera, should the Genus/Species information be:
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There were 0 votes since the poll was created on 19:59, 25 April 2017.
poll-id 4431718A25DAEF0AEAF3C1E7BA6D1A35
For boron isotopes on foraminifera, should the sample depth on the archive be:
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There were 0 votes since the poll was created on 20:00, 25 April 2017.
poll-id D5A19651D0D370C83105D106D7965706
For boron isotopes on foraminifera in new datasets, should the chronology information be:
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There were 0 votes since the poll was created on 20:00, 25 April 2017.
poll-id BA771CAECE8982231574D9C7054DFDFC
For boron isotopes on foraminifera in legacy datasets, should the chronology information be:
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There were 0 votes since the poll was created on 20:00, 25 April 2017.
poll-id 71B136DCD22640624C57F068DDFB1670
For boron isotopes on foraminifera, should the method used for separation be:
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There were 0 votes since the poll was created on 20:01, 25 April 2017.
poll-id BF2A9AB62F43755E631C835376405484
For boron isotopes on foraminifera, should the analysis method (MC-ICP-MS, NTIMS) be:
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There were 0 votes since the poll was created on 20:01, 25 April 2017.
poll-id 288ABF119E994D9C8CA831FBCC8A33BA
For boron isotopes on foraminifera, should the sample size (ng of Boron analyzed) be:
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There were 0 votes since the poll was created on 20:01, 25 April 2017.
poll-id F7700EE6F4C30E62948EA361846D1852
For boron isotopes on foraminifera, should the standard value for certified reference materials be:
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There were 0 votes since the poll was created on 20:02, 25 April 2017.
poll-id A1FD054307064E197CCB057FD8E2FAAA
For boron isotopes on foraminifera, should the analytical precision be:
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There were 0 votes since the poll was created on 20:02, 25 April 2017.
poll-id 58DCB21DFC17DC41F39672A9C30DF58F
Organic Geochemistry
Alkenones
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | Julie (talk), 22 March 2017 |
| Property:Wgs84:Alt (L) (Depth) | E | Water depth can be useful to get an idea of diagenesis in the core. Especially for deep-sea drilling sediments, water depths can be important to assess various biogeochemical properties | Julie (talk), 22 March 2017 |
| Sample Depth | E | Positional information needed to relate the samples back to the archive | Julie (talk), 22 March 2017 |
| ChonDataTable | E for new datasets/ R for legacy datasets | The raw radiocarbon, tie points, 210Pb measurements should be made available so that age models can be updated in light of new calibration curves or new age modeling techniques | Julie (talk), 22 March 2017 |
| Uk’37 index | E | Unsaturation index of C37 alkenones | Julie (talk), 22 March 2017 |
| Analytical Precision | E | Based on replicate injections of samples or standards | Julie (talk), 22 March 2017 |
| Method of sediment extraction | D | i.e. ,microwave, ASE | Julie (talk), 22 March 2017 |
| "Raw" Peak Areas | D | Peak areas of C37:2 and C37:3 (and possibly C37:4 and C38 alkneones) | Julie (talk), 22 March 2017 |
| SST | R | Sea surface temperature derived from Uk’37 index | Julie (talk), 22 March 2017 |
| SST Calibration used | R | Method of converting Uk’37 to SST | Julie (talk), 22 March 2017 |
| Alkenone Concentration | D | Calculated concentration of alkenone | Julie (talk), 22 March 2017 |
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For alkenones measurements in marine sediments, should the location information of the archive be:
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There were 0 votes since the poll was created on 20:04, 25 April 2017.
poll-id DF940799B6686B75F7B4573E930C64CC
For alkenones measurements in marine sediments, should the water depth be:
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There were 0 votes since the poll was created on 20:04, 25 April 2017.
poll-id 8DE5245B764997049DF2F94511C04985
For alkenones measurements in marine sediments, should the sample depth in the archive be:
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There were 0 votes since the poll was created on 20:05, 25 April 2017.
poll-id ABFB9B4242D9644CF787CE6051B6B9FB
For alkenones measurements in marine sediments for new datasets, should chronology information be:
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poll-id 46660C26E21B486ED7F9A8FBF09749E0
For alkenones measurements in marine sediments for legacy datasets, should chronology information be:
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There were 0 votes since the poll was created on 20:05, 25 April 2017.
poll-id 18F23A346BBCD43B2BF3E160F4ED3B1B
For alkenones measurements in marine sediments, should the uk'37/uk37 index be:
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There were 0 votes since the poll was created on 20:06, 25 April 2017.
poll-id B67E652EC6EB9097DFE6D78410A2750C
For alkenones measurements in marine sediments, should the analytical precision be:
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There were 0 votes since the poll was created on 20:06, 25 April 2017.
poll-id 81B40B29AD3B6B210EEE8A65957CAAA6
For alkenones measurements in marine sediments, should the method of sediment extraction be:
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There were 0 votes since the poll was created on 20:06, 25 April 2017.
poll-id 4E65BE21D1C7EE9C8ED2CB9EA26319D6
For alkenones measurements in marine sediments, should the "raw" peak areas be:
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There was one vote since the poll was created on 20:07, 25 April 2017.
poll-id 3F41CF33B2EE7F0D34E3B4DB22ED9097
For alkenones measurements in marine sediments, should the inferred SST be:
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There were 0 votes since the poll was created on 20:07, 25 April 2017.
poll-id 031F3FC1A1F4F65D7A680877D3075737
For alkenones measurements in marine sediments, should the calibration info used to transform the index into SST be:
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poll-id A04763298B49AC91D4028EB052315C8E
For alkenones measurements in marine sediments, should the alkenone concentration be:
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There were 0 votes since the poll was created on 20:07, 25 April 2017.
poll-id 0840D3E04C22EBFED5ED02868C85A3AC
GDGTs
| Metadata | Essential (E)/ Recommended (R) / Desired (D) | Reason | Added by (optional) |
|---|---|---|---|
| Category: Location_(L) (Lat, Lon) | E | Location is a must | Julie (talk), 22 March 2017 |
| Property:Wgs84:Alt (L) (Depth) | E | Water depth can be useful to get an idea of diagenesis in the core. Especially for deep-sea drilling sediments, water depths can be important to assess various biogeochemical properties | Julie (talk), 22 March 2017 |
| Sample Depth | E | Positional information needed to relate the samples back to the archive | Julie (talk), 22 March 2017 |
| ChonDataTable | E for new datasets/ R for legacy datasets | The raw radiocarbon, tie points, 210Pb measurements should be made available so that age models can be updated in light of new calibration curves or new age modeling techniques | Julie (talk), 22 March 2017 |
| GDGT index | E | One or more GDGT-based index must be provided (e.g., TEX86, BIT, MBT, CBT, RI, etc.) | Julie (talk), 22 March 2017 |
| Were core lipids or IPLs analyzed | E | Were the GDGTs measured on Intact Polar lipids or core lipids? | Julie (talk), 22 March 2017 |
| Analytical Precision | D | Usually based on replicate injections of a sample | Julie (talk), 22 March 2017 |
| Method of sediment extraction | D | i.e. ,microwave, ASE | Julie (talk), 22 March 2017 |
| "Raw" Peak Areas | R | As other indices are developed, this allows new information to be calculated from archived data | Julie (talk), 22 March 2017 |
| Definition of the index used | E | The definitions of indices can change over time. If raw peak areas are not provided, then the equation used for the calculated index needs to be provided | Julie (talk), 22 March 2017 |
| Derived Parameter | R | Environmental parameter that GDGT index is calibrated to (e.g., SST, MAT, pH, etc.) | Julie (talk), 22 March 2017 |
| Calibration used for conversion of GDGT index to environmental parameter | R | Which calibration was used to convert TEX86 to SST, for example | Julie (talk), 22 March 2017 |
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Should raw peak areas (as opposed to just TEX86 index) be:
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There were 4 votes since the poll was created on 19:20, 21 November 2016.
poll-id 661DF66A537B28E6EBFFACB0E845D584
For marine sediments and new datasets, should the TEX86 index be:
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There was one vote since the poll was created on 14:34, 4 April 2017.
poll-id 632CD032F4DA5988A4B72D81216F3BDC
For marine sediments and legacy datasets, should the TEX86 index be:
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There was one vote since the poll was created on 14:34, 4 April 2017.
poll-id 96EC1777FA8363F807C150D8C285D29A
For marine sediments and new datasets based on TEX86, should the depth information in the archive be:
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There was one vote since the poll was created on 14:34, 4 April 2017.
poll-id 7073F1FEA36F561671F82ECEF37167B1
For marine sediments and legacy datasets based on TEX86, should the depth information in the archive be:
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There was one vote since the poll was created on 14:35, 4 April 2017.
poll-id 7F8827867755C33A57D67DABAC9520AD
For marine sediments and new datasets based on TEX86, should the method of sediment extraction be:
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There were 0 votes since the poll was created on 14:36, 4 April 2017.
poll-id 2B8A9F8C864A58E5DA04F1888814A9D7
For marine sediments and legacy datasets based on TEX86, should the method of sediment extraction be:
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There were 0 votes since the poll was created on 14:36, 4 April 2017.
poll-id 49086E7F6FDFECE920B99A54D1561E6A
For marine sediments and new datasets based on TEX86, should the use of core lipids or IPLS be reported as:
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There were 0 votes since the poll was created on 18:52, 16 May 2017.
poll-id 6A8EB4257744013B3A78CE8DC54767AA
For marine sediments and legacy datasets based on TEX86, should the use of core lipids or IPLS be reported as:
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There were 0 votes since the poll was created on 18:52, 16 May 2017.
poll-id 4EC112392060033487DB5902E6187A3B
For polls regarding the analytical precision, see the Uncertainty Working Group page.
For TEX86 measurements on marine sediments, should the definition of the index used be:
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There were 0 votes since the poll was created on 20:10, 25 April 2017.
poll-id 58763F0A1AAD75C11B6F47384FC1062E
For TEX86 measurements on marine sediments, should the inferred variable name be:
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There were 0 votes since the poll was created on 20:10, 25 April 2017.
poll-id 2AD8FC1B45843E21CDAFED6C046B8376
For TEX86 measurements on marine sediments, should the calibration used be:
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There were 0 votes since the poll was created on 20:10, 25 April 2017.
poll-id 361DFA4F5B4AFB48AEE243473B94C67E
Compound specific isotopes
Physical Data
Grain Size
Micropaleontological Data
- Report raw counts if available. If not available, then at least report minimum number of specimens counted
- Minimum number of specimens counted
- Size fraction
If the data were used to infer temperature or sea ice concentration, then the method (MAT, WA-PLS, etc) and the training set should be mentioned/required metadata.
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For Micropaleontological Data , should raw counts be:
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There were 3 votes since the poll was created on 23:53, 7 March 2017.
poll-id 7A33C91948DB228ECA30F04A172545F2
For Micropaleontological Data , should the number of specimens counted be:
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There were 3 votes since the poll was created on 23:53, 7 March 2017.
poll-id C9A7C884503C82BD1523BC97FF29A258
For Micropaleontological Data, should size fraction be:
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There were 3 votes since the poll was created on 23:54, 7 March 2017.
poll-id 6DB2FF5E82BDB47B27497680D9290BEE
For Micropaleontological Data, should the seasonality be:
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There were 3 votes since the poll was created on 19:27, 8 March 2017.
poll-id 93117ECF8F1D6DB124852051416FE405
For Micropaleontological Data, should the habitat depth be:
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There were 3 votes since the poll was created on 19:27, 8 March 2017.
poll-id 6E4C094C8B33C461F680E659DE4F5A65
For micropaleontological data, if the data were used to infer temperature or sea ice concentration, should the method (MAT, WA-PLS, etc) be:
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There were 0 votes since the poll was created on 17:53, 12 April 2017.
poll-id BD29524BD109756133A6727B20D76388
For micropaleontological data, if the data were used to infer temperature or sea ice concentration, should the training set be:
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There were 0 votes since the poll was created on 17:53, 12 April 2017.
poll-id E0F11D0CC10510D9B53F1ACE8D868458
Pages in category "Marine Sediment Working Group"
This category contains only the following page.
