Data Table | Table Structure |
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Object Name: | Fiordland-SL-sedimentcores.csv | Size: | 784 byte | Authentication: | ceb06d26d4a7b60f99be370e7802f487
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
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Field Delimiter: | , |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | coreLocation | coreCountry | siteName | latitudeDD | longitudeDD | coreLength | coreSections | waterDepth | dateCored | seismicLine1 | seismicLine2 |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| coreLocation
| coreCountry
| siteName
| latitudeDD
| longitudeDD
| coreLength
| coreSections
| waterDepth
| dateCored
| seismicLine1
| seismicLine2
| Definition: | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location in Fiordland where the sediment core was obtained. | The country name where the sediment core was conducted. | The site name given to the area where the sediment core was obtained. | The latitude taken on board the RV Polaris II at the sediment coring site. | The longitude taken on board the RV Polaris II at the sediment coring site. | The total length of the sediment core obtained on board the RV Polaris II. The total length is a sum of the length of all individual core sections. | The total number of core sections obtained on board the RV Polaris II. | The water depth at the coring site as measured on board the RV Polaris II sounding equipment. | The calendar date (yyyy-mm-dd) the sediment core was obtained. | The name of the seismic line (Boomer and Chirp) used to identify the sediment coring site. | The name of the second seismic line (Boomer and Chirp) used to identify the sediment coring site. | Storage Type: | string
| string
| string
| string
| string
| string
| float
| float
| float
| float
| float
| dateTime
| string
| string
| Measurement Type: | nominal | nominal | nominal | nominal | nominal | nominal | ratio | ratio | ratio | ratio | ratio | dateTime | nominal | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Definition | The location in Fiordland where the sediment core was obtained. |
| Definition | The country name where the sediment core was conducted. |
| Definition | The site name given to the area where the sediment core was obtained. |
| Unit | decimal degrees WGS84 | Type | real |
| Unit | decimal degrees WGS84 | Type | real |
| | | | Format | YYYY-MM-DD | Precision | |
| Definition | The name of the seismic line (Boomer and Chirp) used to identify the sediment coring site. |
| Definition | The name of the second seismic line (Boomer and Chirp) used to identify the sediment coring site. |
| Missing Value Code: | | | | | | | | | | | | | | Code | none | Expl | None indicates only a single seismic line (pair of Boomer and Chirp lines) was used to identify the sediment coring site. |
| Accuracy Report: | | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-c14-ages.csv | Size: | 1946 byte | Authentication: | 92aa0c6af816c9b0951745eb1248c192
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | sampleDepth | sampleMaterial | chemicalPretreatment | datePreProcessed | labID | c14SampleCode | CRA | CRAerror | medCalAge | lowerError | upperError | fractionDated | delta13 | delta13Error | delta13Source |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| sampleDepth
| sampleMaterial
| chemicalPretreatment
| datePreProcessed
| labID
| c14SampleCode
| CRA
| CRAerror
| medCalAge
| lowerError
| upperError
| fractionDated
| delta13
| delta13Error
| delta13Source
| Definition: | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location of the oldest end of the sample as measured from the top of the core. | Type of material taken from the sediment core subsample (at the respective sampleDepth) for submission to AMS lab for radiocarbon age dating. | The method of chemical pretreatment used on the sampleMaterial prior to sending the sampleMaterial to the lab. ABA indicates an acid-base-acid rinse with HCl and NaOH, then rinsed twice with DI water and dried. | The calendar date (yyyy-mm-dd) the sampleMaterial was pre-processed. | An identifier assigned to the AMS laboratory where the sampleMaterial was submitted for radiocarbon age dating. NOSAMS indicates the National Ocean Science AMS Lab, Woods Hole, USA. NZA indicates the Rafter Radiocarbon Lab, Lower Hutt, New Zealand. | A sample code used by the AMS lab to identify the sample. OU indicates Otago University. | The conventional radiocarbon age of the sample as provided by the lab. | The error on the CRA as provided by the AMS lab. | The medican probability calibrated age of the sample calculated using Calib7.0 according to the Sh13 and Mar13 (delta R of 50) curves as appropriate. | The 2sigma lower error resulting from the calibration calculation using Calib7.0. | The 2sigma upper error resulting from the calibration calculation using Calib 7.0 | Notes from the AMS lab regarding the fraction of actual material dated. | The delta13 value provided by the AMS lab results. | Error range on the delta13 value provided by the AMS lab results. | The delta13 source reported by the AMS lab results. | Storage Type: | string
| string
| string
| integer
| string
| string
| dateTime
| string
| string
| float
| float
| float
| float
| float
| string
| float
| float
| string
| Measurement Type: | nominal | nominal | nominal | ratio | nominal | nominal | dateTime | nominal | nominal | ratio | ratio | ratio | ratio | ratio | nominal | ratio | ratio | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Unit | centimeter | Type | integer |
| Definition | Type of material taken from the sediment core subsample (at the respective sampleDepth) for submission to AMS lab for radiocarbon age dating. |
| Definition | The method of chemical pretreatment used on the sampleMaterial prior to sending the sampleMaterial to the lab. ABA indicates an acid-base-acid rinse with HCl and NaOH, then rinsed twice with DI water and dried. |
| Format | YYYY-MM-DD | Precision | |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | NOSAMS | Definition | National Ocean Science AMS Lab, Woods Hole, USA | Source | |
| Code Definition | Code | NZA | Definition | Rafter Radiocarbon Lab, Lower Hutt, New Zealand | Source | |
|
|
| Definition | A sample code used by the AMS lab to identify the sample. OU indicates Otago University. |
| Unit | uncalibrated radiocarbon years before present | Type | integer |
| | Unit | med cal yr BP | Type | integer |
| | | Definition | Notes from the AMS lab regarding the fraction of actual material dated. |
| | | Definition | The delta13 source reported by the AMS lab results. |
| Missing Value Code: | | | | | | | Code | Unknown | Expl | Unknown indicates the pre-processing date for the radiocarbon sample is not known and could not be found at the time of 2022 data publication. |
| | | | | | | | Code | Unknown | Expl | Unknown indicates information not reported or not locatable at the time of 2022 data publication. |
| Code | 99999.0000 | Expl | 99999.000 indicates delta13 is unknown |
| Code | 99999.0 | Expl | 99999.000 indicates delta13Error is unknown |
| Code | Not reported | Expl | Not reported indicates the information was not reported or is not locatable at the time of the 2022 data publication. |
| Accuracy Report: | | | | | | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-diatom-counts.csv | Size: | 102781 byte | Authentication: | d7fe363a306ed071e9d8ebebb109561f
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | coreLocation | sampleDepth | diatomGenus | diatomSpecies | diatomValveCount | totalValvesCounted | valvePreservation | inferredEnvironment |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| coreLocation
| sampleDepth
| diatomGenus
| diatomSpecies
| diatomValveCount
| totalValvesCounted
| valvePreservation
| inferredEnvironment
| Definition: | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location in Fiordland where the sediment core was obtained. | The location of the oldest end of the sample as measured from the top of the core. | The scientific genus of the diatom identified. Identification sources for each species are cited in the Fiordand-SL-diatom-taxa-list.csv file. | The scientific species of the diatom. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. | The number of diatom valves of a species counted via light microscopy on a slide from the sampled depth. | The total number of diatom valves counted via light miscroscopy on a slide from the sampled depth. A minimum of 300 valves were counted whenever possible. | Qualitative indicator for the preservation of diatoms on the slide. | The environment inferred based upon the microfossil and diatom species assemblages from the sampled depth (marine, brackish-fresh or fresh). | Storage Type: | string
| string
| string
| string
| float
| string
| string
| float
| float
| string
| string
| Measurement Type: | nominal | nominal | nominal | nominal | ratio | nominal | nominal | ratio | ratio | nominal | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Definition | The location in Fiordland where the sediment core was obtained. |
| Unit | centimeter | Type | integer |
| Definition | The scientific genus of the diatom identified. Identification sources for each species are cited in the Fiordand-SL-diatom-taxa-list.csv file. |
| Definition | The scientific species of the diatom. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. |
| | | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | Good | Definition | diatom valves are well preserved | Source | |
| Code Definition | Code | Medium | Definition | diatom valves are preserved between well and poor | Source | |
| Code Definition | Code | Poor | Definition | diatom valves are poorly preserved | Source | |
| Code Definition | Code | Poor to Medium | Definition | diatom valves are preserved between poor and medium | Source | |
|
|
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | brackish-fresh | Definition | a brackish-fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | fresh | Definition | a fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | marine | Definition | a marine environment was inferred based on the diatom assemblages | Source | |
|
|
| Missing Value Code: | | | | | | | | Code | 0 | Expl | 0 indicates no valves of that species were counted on the slide. |
| | | | Accuracy Report: | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | Coverage: | | | | | | | | | | | | Methods: | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-diatom-percent.csv | Size: | 85606 byte | Authentication: | 3c009631736400022eb2077c177bcb33
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | coreLocation | sampleDepth | diatomGenus | diatomSpecies | diatomValvePercent | inferredEnvironment |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| coreLocation
| sampleDepth
| diatomGenus
| diatomSpecies
| diatomValvePercent
| inferredEnvironment
| Definition: | RV Polaris II cruise ID following the format ##PLO## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location in Fiordland where the sediment core was obtained. | The location of the oldest end of the sample as measured from the top of the core. | The scientific genus of the diatom identified. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. | The scientific species of the diatom. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. | The relative abundance of a diatom species calculated from diatomValveCount reported in the Fiordland-SL-diatom-count.csv file. | The environment inferred based upon the microfossil and diatom species assemblages from the sampled depth (marine, brackish-fresh or fresh). | Storage Type: | string
| string
| string
| string
| float
| string
| string
| float
| string
| Measurement Type: | nominal | nominal | nominal | nominal | ratio | nominal | nominal | ratio | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PLO## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Definition | The location in Fiordland where the sediment core was obtained. |
| Unit | centimeter | Type | integer |
| Definition | The scientific genus of the diatom identified. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. |
| Definition | The scientific species of the diatom. Identification sources for each species are cited in the Fiordand-SLC-diatom-taxa-list.csv file. |
| | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | brackish-fresh | Definition | a brackish-fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | fresh | Definition | a fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | marine | Definition | a marine environment was inferred based on the diatom assemblages | Source | |
|
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| Missing Value Code: | | | | | | | | Code | 0 | Expl | 0 indicates no valves of that species were counted on the slide. |
| | Accuracy Report: | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | Coverage: | | | | | | | | | | Methods: | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-microfossil-counts.csv | Size: | 6864 byte | Authentication: | 9734d66c288f8a346bc4456a1177367c
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | coreLocation | sampleDepth | generalSurveyMicrofossil | generalSurveyCount | generalSurveyTotal | inferredEnvironment |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| coreLocation
| sampleDepth
| generalSurveyMicrofossil
| generalSurveyCount
| generalSurveyTotal
| inferredEnvironment
| Definition: | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location in Fiordland where the sediment core was obtained. | The location of the oldest end of the sample as measured from the top of the core. | The microfossil observed via light microscopy on a slide from the sampled depth (sponge spicules, ascidian spicules, foraminifera, ostracods, silicoflagellates, diatoms). | The number of microfossils of a certain type counted via light microscopy on a slide from the sampled depth. | The total number of microfossils counted via light miscroscopy on a slide from the sampled depth. A minimum of 300 microfossils were counted whenever possible. | The environment inferred based upon the microfossil and diatom species assemblages from the sampled depth (marine, brackish-fresh or fresh). | Storage Type: | string
| string
| string
| string
| float
| string
| float
| float
| string
| Measurement Type: | nominal | nominal | nominal | nominal | ratio | nominal | ratio | ratio | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PL0## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Definition | The location in Fiordland where the sediment core was obtained. |
| Unit | centimeter | Type | integer |
| Definition | The microfossil observed via light microscopy on a slide from the sampled depth (sponge spicules, ascidian spicules, foraminifera, ostracods, silicoflagellates, diatoms). |
| | | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | brackish-fresh | Definition | a brackish-fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | fresh | Definition | a fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | marine | Definition | a marine environment was inferred based on the diatom assemblages | Source | |
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| Missing Value Code: | | | | | | | | | | Accuracy Report: | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | Coverage: | | | | | | | | | | Methods: | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-microfossil-percent.csv | Size: | 6136 byte | Authentication: | 854318b5ceb2bd389429caf9be3a19cd
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
Simple Delimited: |
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Table Column Descriptions |
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| | | cruiseID | cruiseCoreID | paperCoreID | coreLocation | sampleDepth | generalSurveyMicrofossil | generalSurveyPercent | inferredEnvironment |
---|
Column Name: | cruiseID
| cruiseCoreID
| paperCoreID
| coreLocation
| sampleDepth
| generalSurveyMicrofossil
| generalSurveyPercent
| inferredEnvironment
| Definition: | RV Polaris II cruise ID following the format ##PLO## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). | The location in Fiordland where the sediment core was obtained. | The location of the oldest end of the sample as measured from the top of the core. | The microfossil observed via light microscopy on a slide from the sampled depth (sponge spicules, ascidian spicules, foraminifera, ostracods, silicoflagellates, diatoms). | The relative abundance of a type of microfossil calculated from generalSurveyCount reported in the Fiordland-SL-microfossil-counts.csv file. | The environment inferred based upon the microfossil and diatom species assemblages from the sampled depth (marine, brackish-fresh or fresh). | Storage Type: | string
| string
| string
| string
| float
| string
| float
| string
| Measurement Type: | nominal | nominal | nominal | nominal | ratio | nominal | ratio | nominal | Measurement Values Domain: | Definition | RV Polaris II cruise ID following the format ##PLO## in which the first two digits are the final two numbers in the calendar year in which the cruise occurred. (example: 13PL018 took place in the year 2013.) |
| Definition | The sediment core ID assigned to the core in the field on the research cruise following the format ##P## in which the first two digits represent the core's collection in sequence on the cruise and the second digits represent the core section number (if multiple core sections were obtained). |
| Definition | The shorthand sediment core ID used in the paper by Dlabola et al 2015 following the format ##P## in which the first two digits represent the final two digits of the cruiseID and the final two digits represent the cruiseCoreID. (Example: 27P13 was collected on board the 12PL027 cruise and was the 13th core collected on that cruise). |
| Definition | The location in Fiordland where the sediment core was obtained. |
| Unit | centimeter | Type | integer |
| Definition | The microfossil observed via light microscopy on a slide from the sampled depth (sponge spicules, ascidian spicules, foraminifera, ostracods, silicoflagellates, diatoms). |
| | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | brackish-fresh | Definition | a brackish-fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | fresh | Definition | a fresh environment was inferred based on the diatom assemblages | Source | |
| Code Definition | Code | marine | Definition | a marine environment was inferred based on the diatom assemblages | Source | |
|
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| Missing Value Code: | | | | | | | Code | 0 | Expl | 0 indicates no microfossils of that type were counted on the slide. |
| | Accuracy Report: | | | | | | | | | Accuracy Assessment: | | | | | | | | | Coverage: | | | | | | | | | Methods: | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-SLC-NZc14.csv | Size: | 16895 byte | Authentication: | 9624a28b2a21833815f2eac1258c5505
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
Simple Delimited: |
Field Delimiter: | , |
Quote Character: | " |
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Table Column Descriptions |
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| | | calibratedSampleAge | c14LowerError2sigma | c14UpperError2sigma | sillDepth | relativeSeaLevel | depthError | depthErrorDirection | seaLevelIndicator | sampleType | depositionalEnvironment | sampleLocation | sampleCountry | sampleAgeMethod | sampleAgeCode | ageCalibrationMethod | dataSource |
---|
Column Name: | calibratedSampleAge
| c14LowerError2sigma
| c14UpperError2sigma
| sillDepth
| relativeSeaLevel
| depthError
| depthErrorDirection
| seaLevelIndicator
| sampleType
| depositionalEnvironment
| sampleLocation
| sampleCountry
| sampleAgeMethod
| sampleAgeCode
| ageCalibrationMethod
| dataSource
| Definition: | The median probability calibrated radiocarbon age from the literature data. Raw radiocarbon ages from literature were calibrated using Calib7.0 using the calibration curve indicated in ageCalibrationMethod. | The 2sigma lower error resulting from the calibration calculation using Calib7.0 or directly from the literature data. | The 2sigma upper error resulting from the calibration calculation using Calib7.0 or directly from the literature data. | If applicable, the depth of the sill in meters below sea level used to constrain paleosea level in the literature data from marine ingression basins or isolated lake basins. | Relative sea level in meters as reported in the literature data. | The error on the relativeSeaLevel. | If depthError is available, the direction of the depthError where + indicates the error applies only above sea level and +/- indicates the error applies both above and below sea level. | The type of proxy or indicator used to constrain paleosea level. | The source type of material sample used in the literature data to study paleosea level. | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. | The location where the literature data sample was obtained. | The country name where the literature study was conducted. | The absolute age dating method used to obtain the calibratedSampleAge. C14 indicates radiocarbon age dating and U-Th indicates uranium-thorium age dating. | The code associated with the age in the literature data. | The calibration method used for calibrating conventional radiocarbon ages reported in the literature to the calibratedSampleAge reported here. | The reference for the source data following Author Surname yyyy format. (Example: Bard 2010) | Storage Type: | float
| float
| float
| float
| float
| float
| string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| Measurement Type: | ratio | ratio | ratio | ratio | ratio | ratio | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | Measurement Values Domain: | Unit | med cal yr BP | Type | integer |
| | | Unit | meters below sea level | Type | real |
| | | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | +/- | Definition | +/- indicates the error applies both above and below sea level. | Source | |
| Code Definition | Code | + | Definition | + indicates the error applies only above sea level | Source | |
|
|
| Definition | The type of proxy or indicator used to constrain paleosea level. |
| Definition | The source type of material sample used in the literature data to study paleosea level. |
| Definition | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. |
| Definition | The location where the literature data sample was obtained. |
| Definition | The country name where the literature study was conducted. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | C14 | Definition | radicarbon age dating | Source | |
| Code Definition | Code | UTh | Definition | uranium-thorium age dating | Source | |
|
|
| Definition | The code associated with the age in the literature data. |
| Definition | The calibration method used for calibrating conventional radiocarbon ages reported in the literature to the calibratedSampleAge reported here. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | Dlabola et al 2015 | Definition | Dlabola. E.K., Wilson, G.S., Gorman, A.R., Riesselman, C.R., and Moy, C.M. 2015. A post-glacial sea-level curve from Fiordland, New Zealand. Global and Planetary Change, 131, 101-114. https://doi.org/10.1016/j.gloplacha.2015.05.010 | Source | |
| Code Definition | Code | Gibb 1986 | Definition | Gibb, J.G., 1986. A New Zealand regional Holocene eustatic sea-level curve and its application to determination of vertical tectonic movements. Bull. Roy. Soc. NZ 24, 377–395. | Source | |
| Code Definition | Code | Pickrill et al 1992 | Definition | Pickrill, R.A., Fenner, J.M., McGlone, M.S., 1992. Late Quaternary evolution o environment in Preservation Inlet, New Zealand. Quat. Res. 38, 331–346 | Source | |
|
|
| Missing Value Code: | | Code | -9999 | Expl | -9999 indicates the 2sigma lower error was not provided in the literature data. |
| Code | -9999 | Expl | -9999 indicates the 2sigma upper error was not provided in the literature data. |
| Code | 9999 | Expl | 9999 indicates that a sill level is not applicable to the data. |
| | Code | 9999 | Expl | 9999 indicates the depthError is not known or not reported in the literature data. |
| Code | None | Expl | None indicates no depthError and thus no depthErrorDirection was available or not reported in the literature data. |
| | | Code | Not reported | Expl | Not reported indicates the literature data does not specify the depositional environment. |
| | | | Code | Unknown | Expl | Unknown indicates the sampleAgeCode is not known or was not located for the 2022 data publication. |
| Code | Unknown | Expl | Unknown indicates the calibration method is unknown or not locatable for the 2022 data publication. |
| | Accuracy Report: | | | | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SLClitdata-globalc14.csv | Size: | 7171 byte | Authentication: | dc0002140fe8b739ade52ecb316bdbb2
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
Simple Delimited: |
Field Delimiter: | , |
Quote Character: | " |
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Table Column Descriptions |
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| | | calibratedSampleAge | c14LowerError2sigma | c14UpperError2sigma | sillDepthmbsl | relativeSeaLevel | depthError | depthErrorDirection | seaLevelIndicator | sampleType | depositionalEnvironment | sampleLocation | sampleCountry | sampleAgeMethod | sampleAgeCode | ageCalibrationMethod | dataSource |
---|
Column Name: | calibratedSampleAge
| c14LowerError2sigma
| c14UpperError2sigma
| sillDepthmbsl
| relativeSeaLevel
| depthError
| depthErrorDirection
| seaLevelIndicator
| sampleType
| depositionalEnvironment
| sampleLocation
| sampleCountry
| sampleAgeMethod
| sampleAgeCode
| ageCalibrationMethod
| dataSource
| Definition: | The median probability calibrated radiocarbon age from the literature data. Raw radiocarbon ages from literature were calibrated using Calib7.0 using the calibration curve indicated in ageCalibrationMethod. | The 2sigma lower error resulting from the calibration calculation using Calib7.0 or directly from the literature data. | The 2sigma upper error resulting from the calibration calculation using Calib7.0 or directly from the literature data. | If applicable, the depth of the sill in meters below sea level used to constrain paleosea level in the literature data from marine ingression basins or isolated lake basins. | Relative sea level in meters as reported in the literature data. | The error on the relativeSeaLevel. | If depthError is available, the direction of the depthError where + indicates the error applies only above sea level and +/- indicates the error applies both above and below sea level. | The type of proxy or indicator used to constrain paleosea level. | The source type of material sample used in the literature data to study paleosea level. | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. | The location where the literature data sample was obtained. | The country name where the literature study was conducted. | The absolute age dating method used to obtain the calibratedSampleAge. C14 indicates radiocarbon age dating and U-Th indicates uranium-thorium age dating. | The code associated with the age in the literature data. | The calibration method used for calibrating conventional radiocarbon ages reported in the literature to the calibratedSampleAge reported here. | The reference for the source data following Author Surname yyyy format. (Example: Bard 2010) | Storage Type: | float
| float
| float
| float
| float
| float
| string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| Measurement Type: | ratio | ratio | ratio | ratio | ratio | ratio | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | Measurement Values Domain: | | | | | | | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | + | Definition | + indicates the error applies only above sea level | Source | |
| Code Definition | Code | +/- | Definition | +/- indicates the error applies both above and below sea level. | Source | |
|
|
| Definition | The type of proxy or indicator used to constrain paleosea level. |
| Definition | The source type of material sample used in the literature data to study paleosea level. |
| Definition | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. |
| Definition | The location where the literature data sample was obtained. |
| Definition | The country name where the literature study was conducted. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | C14 | Definition | radiocarbon age dating | Source | |
| Code Definition | Code | UTh | Definition | uranium-thorium age dating | Source | |
|
|
| Definition | The code associated with the age in the literature data. |
| Definition | The calibration method used for calibrating conventional radiocarbon ages reported in the literature to the calibratedSampleAge reported here. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | Dallimore et al 2010 | Definition | Dallimore, A., Enkin, R.J., Pienitz, R., Southon, J.R., Baker, J., Wright, C.A., Pedersen, T.F., Calvert, S.E., Ivanochko, T., Thomson, R.E., 2008. Postglacial evolution of a Pacific coastal fjord in British Columbia, Canada: interactions of sea-level change, crustal response, and environmental fluctuations — results from MONA core MD02-2494. Can. J. Earth Sci. 45 (11), 1345–1362. | Source | |
| Code Definition | Code | Guilderson 2000 | Definition | Guilderson, T.P., Burckle, L., Hemming, S., Peltier, W.R., 2000. Late Pleistocene sea level variations derived from the Argentine Shelf. Geochem. Geophys. Geosyst. 1 (12) (2000GC000098) | Source | |
| Code Definition | Code | McHugh et al 2008 | Definition | McHugh, C.M.G., Gurung, D., Giosan, L., Ryan, W.B.F., Mart, Y., Sancar, U., Burckle, L., Çagatay, M.N., 2008. The last reconnection of the Marmara Sea (Turkey) to the World Ocean: a paleoceanographic and paleoclimatic perspective. Mar. Geol. 255 (1-2), 64–82. | Source | |
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|
| Missing Value Code: | | Code | -9999 | Expl | -9999 indicates the 2sigma lower error was not provided in the literature data. |
| Code | -9999 | Expl | -9999 indicates the 2sigma upper error was not provided in the literature data. |
| Code | 9999 | Expl | 9999 indicates that a sill level is not applicable to the data. |
| | Code | 9999 | Expl | 9999 indicates the depthError is not known or not reported in the literature data. |
| Code | None | Expl | None indicates no depthError and thus no depthErrorDirection was available or not reported in the literature data. |
| | | Code | Not reported | Expl | Not reported indicates the literature data does not specify the depositional environment. |
| | | | Code | Unknown | Expl | Unknown indicates the sampleAgeCode is not known or was not located for the 2022 data publication. |
| Code | Unknown | Expl | Unknown indicates the calibration method is unknown or not locatable for the 2022 data publication. |
| | Accuracy Report: | | | | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-SLClitdata-coralUTh.csv | Size: | 26829 byte | Authentication: | 985527b5bb40b2046a479bb5bd644ed8
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
Simple Delimited: |
Field Delimiter: | , |
Quote Character: | " |
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Table Column Descriptions |
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| | | calibratedSampleAge | UThageError | UThErrorRange | relativeSeaLevel | depthError | depthErrorDirection | seaLevelIndicator | sampleType | depositionalEnvironment | sampleLocation | sampleCountry | sampleAgeMethod | sampleAgeCode | dataSource |
---|
Column Name: | calibratedSampleAge
| UThageError
| UThErrorRange
| relativeSeaLevel
| depthError
| depthErrorDirection
| seaLevelIndicator
| sampleType
| depositionalEnvironment
| sampleLocation
| sampleCountry
| sampleAgeMethod
| sampleAgeCode
| dataSource
| Definition: | The calibrated age reported from the literature data. | The depth error reported from the literature data. | The error range reported from the literature data. (2sigma or 1sigma) | Relative sea level in meters as reported in the literature data. | The error on the relativeSeaLevel as reported in the literature data. | If depthError is available, the direction of the depthError where + indicates the error applies only above sea level and +/- indicates the error applies both above and below sea level. | The type of proxy or indicator used to constrain paleosea level. | The source type of material sample used in the literature data to study paleosea level. | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. | The location where the literature data sample was obtained. | The country name where the literature study was conducted. | The absolute age dating method used to obtain the calibratedSampleAge. C14 indicates radiocarbon age dating and U-Th indicates uranium-thorium age dating. | The code associated with the age in the literature data. | The reference for the source data following Author Surname yyyy format. (Example: Bard 2010) | Storage Type: | float
| float
| string
| float
| float
| string
| string
| string
| string
| string
| string
| string
| string
| string
| Measurement Type: | ratio | ratio | nominal | ratio | ratio | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | Measurement Values Domain: | Unit | calibrated years before present | Type | integer |
| | Definition | The error range reported from the literature data. (2sigma or 1sigma) |
| | | Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | + | Definition | + indicates the error applies only above sea level | Source | |
| Code Definition | Code | +/- | Definition | +/- indicates the error applies both above and below sea level. | Source | |
|
|
| Definition | The type of proxy or indicator used to constrain paleosea level. |
| Definition | The source type of material sample used in the literature data to study paleosea level. |
| Definition | The depositional environment indicated by the seaLevelIndicator used to reconstruct paleosea level. |
| Definition | The location where the literature data sample was obtained. |
| Definition | The country name where the literature study was conducted. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | U-Th | Definition | uranium-thorium age dating | Source | |
| Code Definition | Code | C14 | Definition | radicarbon age dating | Source | |
|
|
| Definition | The code associated with the age in the literature data. |
| Allowed Values and DefinitionsEnumerated Domain | | Code Definition | Code | Bard 2010 | Definition | Bard, E., Hamelin, B., Delanghe-Sabatier, D., 2010. Deglacial meltwater pulse 1B and Younger Dryas sea levels revsited with boreholes at Tahiti. Science 327 (5970), 1235–1237. | Source | |
| Code Definition | Code | Deschamps et al 2012 | Definition | Deschamps, P., Durand, N., Bard, E., Hamelin, B., Camoin, G., Thomas, A.L., Henderson, G.M., Okuno, J., Yokoyama, Y., 2012. Ice-sheet collapse and sea-level rise at the Bølling warming 14,600 years ago. Nature 483 (7391), 559–564 | Source | |
| Code Definition | Code | Peltier and Fairbanks 2006 | Definition | Peltier, W.R., Fairbanks, R.G., 2006. Global glacial ice volume and Last Glacial Maximum duration from an extended Barbados sea level record. Quat. Sci. Rev. 25 (23-24), 3322–3337. | Source | |
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| Missing Value Code: | | | | | Code | -9999 | Expl | -9999 indicates the depthError was not reported in the literature data. |
| Code | None | Expl | None indicates no depthError and thus no depthErrorDirection was available or not reported in the literature data. |
| | | | | | | Code | Unknown | Expl | Unknown indicates the sampleAgeCode is not known or was not located for the 2022 data publication. |
| | Accuracy Report: | | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | | |
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Data Table | Table Structure |
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Object Name: | Fiordland-SL-diatom-taxa-list.csv | Size: | 14018 byte | Authentication: | 74b7e8414a5b0b7a6190fdee3cc88a6f
Calculated By MD5 | Text Format: |
Number of Header Lines: | 1 |
Record Delimiter: | \r\n |
Orientation: | column |
Simple Delimited: |
Field Delimiter: | , |
Quote Character: | " |
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Table Column Descriptions |
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| | | AlgaeBaselink | scientificClass | scientificOrder | scientificFamily | scientificGenus | scientificSpecies | scientificNameAuthorship | identificationReference | taxonomicStatus | IDreferencePlate | environmentalAssociation | thesisAppendixAPlate | Comments |
---|
Column Name: | AlgaeBaselink
| scientificClass
| scientificOrder
| scientificFamily
| scientificGenus
| scientificSpecies
| scientificNameAuthorship
| identificationReference
| taxonomicStatus
| IDreferencePlate
| environmentalAssociation
| thesisAppendixAPlate
| Comments
| Definition: | URL to the diatom species in www.algaebase.org | The scientific class to which the diatom species belongs based on AlgaeBase. | The scientific order to which the diatom species belongs based on AlgaeBase. | The scientific family to which the diatom species belongs based on AlgaeBase. | The scientific genus to which the diatom species belongs based on AlgaeBase. | The scientific species to which the diatom species belongs based on AlgaeBase. | The authorship information for the scientificName formatted according to the identificationReference. | A citation for the identification source reference used. | Indication of the species verification status, whether accepted or synonymous with another accepted species. | The plate and figure numbers from the identificationReference. | The diatom species associated environment (marine, freshwater or brackish-fresh) as listed on AlgaeBase. | The Plate number for the diatom species from Dlabola 2015 thesis. | Explanatory or supplemental comments regarding species identirications or taxonomic status. | Storage Type: | string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| string
| Measurement Type: | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | nominal | Measurement Values Domain: | Definition | URL to the diatom species in www.algaebase.org |
| Definition | The scientific class to which the diatom species belongs based on AlgaeBase. |
| Definition | The scientific order to which the diatom species belongs based on AlgaeBase. |
| Definition | The scientific family to which the diatom species belongs based on AlgaeBase. |
| Definition | The scientific genus to which the diatom species belongs based on AlgaeBase. |
| Definition | The scientific species to which the diatom species belongs based on AlgaeBase. |
| Definition | The authorship information for the scientificName formatted according to the identificationReference. |
| Definition | A citation for the identification source reference used. |
| Definition | Indication of the species verification status, whether accepted or synonymous with another accepted species. |
| Definition | The plate and figure numbers from the identificationReference. |
| Definition | The diatom species associated environment (marine, freshwater or brackish-fresh) as listed on AlgaeBase. |
| Definition | The Plate number for the diatom species from Dlabola 2015 thesis. |
| Definition | Explanatory or supplemental comments regarding species identirications or taxonomic status. |
| Missing Value Code: | Code | None | Expl | The diatom species was not found on AlgaeBase as of 2022 data publication. |
| Code | Unknown | Expl | The diatom class was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | Unknown | Expl | The diatom order was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | Unknown | Expl | The diatom family was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| | | Code | Unknown | Expl | The diatom authorshipName was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | Unknown | Expl | The diatom identificationReference was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | Unknown | Expl | The diatom taxonomicStatus was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | Unknown | Expl | The diatom IDreferencePlate was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. |
| Code | unknown | Expl | Unknown indicates the diatom environmentalAssociation was not reported in the original Dlabola 2015 thesis or Dlabola et al 2015 publication and could not be recovered for the 2022 data publication. | Code | none | Expl | None indicates the association was cosmopolitan or not listed in the identificationReference or AlgaeBase. |
| Code | none | Expl | There is no plate figure in the Dlabola 2015 thesis. |
| Code | none | Expl | comments not applicable |
| Accuracy Report: | | | | | | | | | | | | | | Accuracy Assessment: | | | | | | | | | | | | | | Coverage: | | | | | | | | | | | | | | Methods: | | | | | | | | | | | | | |
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