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Grid DAP Data | Sub- set | Table DAP Data | Make A Graph | W M S | Source Data Files | Acces- sible | Title | Sum- mary | FGDC, ISO, Metadata | Back- ground Info | RSS | E | Institution | Dataset ID |
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data | graph | files | public | [VAHINE nitrogen] - Dissolved and sinking particulate organic nitrogen data from a large volume mesocosm experiment in the Noumea Lagoon, New Caledonia, measured from January to February 2013 (Quantifying nitrogen fixation along unique geochemical gradients in the southwest Pacific Ocean) | I M | background | BCO-DMO | bcodmo_dataset_739646 |
Row Type | Variable Name | Attribute Name | Data Type | Value |
---|---|---|---|---|
attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv |
attribute | NC_GLOBAL | acquisition_description | String | Sampling and analytical procedures: The concentration of total nitrogen (TN) for samples was determined by persulfate oxidation (Solorzano and Sharp, 1980) with adaptations (Knapp et al., 2005), and the resulting NO3- was measured by chemiluminescence (Braman and Hendrix, 1989). DON concentration was determined by subtracting the concentrations of PNsusp, NH4+, and NO3-+NO2- (reported in Berthelot et al., 2015, Biogeosciences) from the measured TN concentration of each sample with a propagated error of +/- 0.5 \u03bcM. The d15N of the resulting NO3- was measured using the denitrifier method (Casciotti et al., 2002; McIlvin and Casciotti, 2011; Sigman et al., 2001). The d15N of PNsink was measured using a Thermo Scientific Flash 2000 Elemental Analyzer coupled with a Delta Plus Thermo Scientific mass spectrometer. The average standard deviation for individual DON concentration measurements was +/- 0.3 \u00b5M. DON concentration was determined by subtracting the concentrations of PNsusp, NH4+, and NO3-+NO2- (reported in Berthelot et al., 2015, Biogeosciences) from the measured TN concentration of each sample with a propagated error of +/- 0.5 \u03bcM. The d15N of TN was determined via persulfate oxidation of TN to NO3- (Knapp et al., 2005) and subsequent analysis of NO3- d15N by the denitrifier method, with a propagated error for DON d15N calculated using a Monte Carlo method (Press et al., 1992) of +/- 0.6\u2030. Samples were calibrated with IAEA N3 and USGS 34 NO3- d15N isotopic reference materials as described in McIlvin and Casciotti, 2011. The d15N of PNsink was measured using a Thermo Scientific Flash 2000 Elemental Analyzer coupled with a Delta Plus Thermo Scientific mass spectrometer. The average standard deviation for standards was +/- 0.06\u2030. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 710561 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1537314 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1537314 |
attribute | NC_GLOBAL | awards_0_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_0_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_0_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_0_program_manager | String | Henrietta N Edmonds |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 51517 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | VAHINE nitrogen PI: Angela Knapp Data version 1: 2018-07-10 |
attribute | NC_GLOBAL | Conventions | String | COARDS, CF-1.6, ACDD-1.3 |
attribute | NC_GLOBAL | creator_email | String | info at bco-dmo.org |
attribute | NC_GLOBAL | creator_name | String | BCO-DMO |
attribute | NC_GLOBAL | creator_type | String | institution |
attribute | NC_GLOBAL | creator_url | String | https://www.bco-dmo.org/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2018-07-10T19:07:01Z |
attribute | NC_GLOBAL | date_modified | String | 2018-07-12T18:56:18Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.739646.1 |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/739646 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | IR Mass Spec |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | DON d15N was measured on a Thermo Delta V isotope ratio mass spectrometer. |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 739696 |
attribute | NC_GLOBAL | instruments_0_description | String | The Isotope-ratio Mass Spectrometer is a particular type of mass spectrometer used to measure the relative abundance of isotopes in a given sample (e.g. VG Prism II Isotope Ratio Mass-Spectrometer). |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB16/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Isotope-ratio Mass Spectrometer |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 469 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Thermo Delta V isotope ratio mass spectrometer |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | DON concentration was measured on a Thermo Scientific 42i chemiluminescent NOx box. |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 739695 |
attribute | NC_GLOBAL | instruments_1_description | String | The chemiluminescence method for gas analysis of oxides of nitrogen relies on the measurement of light produced by the gas-phase titration of nitric oxide and ozone. A chemiluminescence analyzer can measure the concentration of NO/NO2/NOX. One example is the Teledyne Model T200: http://www.teledyne-api.com/products/T200.asp |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Chemiluminescence NOx Analyzer |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 542895 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Thermo Scientific 42i chemiluminescent NOx |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | The d15N of PNsink was measured using a Thermo Scientific Flash 2000 Elemental Analyzer coupled with a Delta Plus Thermo Scientific mass spectrometer. |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 739697 |
attribute | NC_GLOBAL | instruments_2_description | String | Instruments that quantify carbon, nitrogen and sometimes other elements by combusting the sample at very high temperature and assaying the resulting gaseous oxides. Usually used for samples including organic material. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB01/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Elemental Analyzer |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 546339 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | Thermo Scientific Flash 2000 Elemental Analyzer |
attribute | NC_GLOBAL | keywords | String | bco, bco-dmo, biological, chemical, d15, data, dataset, date, dmo, don, dond15, erddap, M1_d15NPNsink, M1_DON, M1_DONd15N, M2_d15NPNsink, M2_DON, M2_DONd15N, M3_d15NPNsink, M3_DON, M3_DONd15N, management, npnsink, oceanography, office, preliminary, sampling, time |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/739646/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/739646 |
attribute | NC_GLOBAL | param_mapping | String | {'739646': {}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/739646/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | Florida State University |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | FSU |
attribute | NC_GLOBAL | people_0_person_name | String | Angela N. Knapp |
attribute | NC_GLOBAL | people_0_person_nid | String | 555499 |
attribute | NC_GLOBAL | people_0_role | String | Principal Investigator |
attribute | NC_GLOBAL | people_0_role_type | String | originator |
attribute | NC_GLOBAL | people_1_affiliation | String | Florida State University |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | FSU |
attribute | NC_GLOBAL | people_1_person_name | String | Angela N. Knapp |
attribute | NC_GLOBAL | people_1_person_nid | String | 555499 |
attribute | NC_GLOBAL | people_1_role | String | Contact |
attribute | NC_GLOBAL | people_1_role_type | String | related |
attribute | NC_GLOBAL | people_2_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_2_person_name | String | Amber York |
attribute | NC_GLOBAL | people_2_person_nid | String | 643627 |
attribute | NC_GLOBAL | people_2_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_2_role_type | String | related |
attribute | NC_GLOBAL | project | String | SW Pac N2 fixation |
attribute | NC_GLOBAL | projects_0_acronym | String | SW Pac N2 fixation |
attribute | NC_GLOBAL | projects_0_description | String | NSF Award Abstract: The availability of nitrogen in the surface ocean plays a critical role regulating rates of primary productivity in the ocean, and thus through modification of the carbon cycle, nitrogen has the capacity to influence climate. The dominant source of biologically available nitrogen to the ocean is through a process known as di-nitrogen (N2) fixation, which involves the reduction of N2 gas dissolved in seawater to ammonium by microbes referred to as diazotrophs. While significant progress has been made identifying a diversity of marine diazotrophs in recent years using molecular tools, quantifying global rates of N2 fixation, and identifying which ocean basin supports the highest fluxes, has remained a vexing question. This research will quantify rates of N2 fixation as well as its importance for supporting production in the southwest Pacific Ocean. Results from this research will shed light on the sensitivities of N2 fixation (temperature, iron concentrations) as well as the extent of spatial and temporal coupling of nitrogen sources and sinks in the ocean. The work will be carried out by an early career scientist, and involve mentoring of young women, middle school girls and minorities, training of undergraduate and graduate researchers, and international collaborations. Identifying the spatial distribution of the largest di-nitrogen (N2) fixation fluxes to the ocean remains a critical goal of chemical oceanography. The spatial distribution can inform our understanding of the environmental sensitivities of N2 fixation and the capacity for the dominant marine nitrogen (N) source and sink processes to respond to each other and thus influence the global carbon cycle and climate. In addition to temperature, two factors are at the heart of the current debate over what influences the spatial distribution of N2 fixation in the ocean: 1) the presence of adequate iron to meet the needs of N2 fixing microbes, and, 2) the absolute concentrations as well as ratios of surface ocean nitrate and phosphate concentrations that are low relative to the "Redfield" ratio, which are thought to favor N2 fixing microbes. This project will test the effects of gradients in atmospheric dust deposition on N2 fixation rates when surface waters have relatively constant but favorable nitrate to phosphate concentrations. The work will be carried out in the southwest Pacific, a region highlighted by new modeling work for its unique geochemical characteristics that are expected to favor significant N2 fixation fluxes. Nitrate+nitrite d15N as well as total dissolved nitrogen (TDN) concentration and d15N will be measured in water column samples collected on a French cruise and sediment traps were deployed to capture the sinking particulate N flux. The results will be compared with published work to evaluate which ocean regions support the largest N2 fixation fluxes. More information: This project was part of the Oligotrophy to UlTra-oligotrophy PACific Experiment (OUTPACE) cruise in the Southwest Pacific between New Caledonia (166°28' E; 22°14' S) and Tahiti (149°36' W; 17°34' S) 0-2000 m * OUTPACE cruise (doi: https://dx.doi.org/10.17600/15000900) * OUTPACE website: https://outpace.mio.univ-amu.fr/?lang=en |
attribute | NC_GLOBAL | projects_0_end_date | String | 2018-07 |
attribute | NC_GLOBAL | projects_0_geolocation | String | Southwest Pacific Ocean between New Caledonia and Tahiti along ~18 deg S |
attribute | NC_GLOBAL | projects_0_name | String | Quantifying nitrogen fixation along unique geochemical gradients in the southwest Pacific Ocean |
attribute | NC_GLOBAL | projects_0_project_nid | String | 710562 |
attribute | NC_GLOBAL | projects_0_project_website | String | http://scope.soest.hawaii.edu/data/lava/lava.html |
attribute | NC_GLOBAL | projects_0_start_date | String | 2015-08 |
attribute | NC_GLOBAL | publisher_name | String | Biological and Chemical Oceanographic Data Management Office (BCO-DMO) |
attribute | NC_GLOBAL | publisher_type | String | institution |
attribute | NC_GLOBAL | sourceUrl | String | (local files) |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | summary | String | This dataset includes water column dissolved organic nitrogen (DON) concentration and d15N data, as well as sinking particulate nitrogen d15N (\u201cPNsink d15N\u201d) data. These samples were collected inside triplicate (\u201cM1\u201d, \u201cM2\u201d, and \u201cM3\u201d) large volume (i.e., 2.3 m diameter, 15 m deep) mesocosm experiments deployed in a lagoon off of Noumea, New Caledonia. DON samples were collected at 6 m depth daily by a Teflon pump and PVC tubing. PNsink d15N samples were collected daily by SCUBA divers who removed a screw-top plastic bottle from the bottom of the plastic mesocosm. \u201cSwimmers\u201d were removed from the PNsink d15N samples prior to analysis.\r\n\r\nThese measurements were made as part of project \VAriability of vertical and tropHIc transfer of diazotroph derived N in the south wEst Pacific\ (VAHINE) to study the fate of fixed nitrogen in the oceanic pelagic food web and its potential impact on carbon export. The field campaign of VAHINE took place in the South West Pacific (New Caledonia) in January and February of 2013 and involved 16 scientists from France, Israel, Germany and the USA. |
attribute | NC_GLOBAL | title | String | [VAHINE nitrogen] - Dissolved and sinking particulate organic nitrogen data from a large volume mesocosm experiment in the Noumea Lagoon, New Caledonia, measured from January to February 2013 (Quantifying nitrogen fixation along unique geochemical gradients in the southwest Pacific Ocean) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | Sampling_Date | String | ||
attribute | Sampling_Date | bcodmo_name | String | date |
attribute | Sampling_Date | description | String | Sample date in format "dd-mmm-yyyy" |
attribute | Sampling_Date | long_name | String | Sampling Date |
attribute | Sampling_Date | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/ADATAA01/ |
attribute | Sampling_Date | source_name | String | Sampling_Date |
attribute | Sampling_Date | time_precision | String | 1970-01-01 |
attribute | Sampling_Date | units | String | unitless |
variable | M1_DON | float | ||
attribute | M1_DON | _FillValue | float | NaN |
attribute | M1_DON | actual_range | float | 5.1, 5.9 |
attribute | M1_DON | bcodmo_name | String | Dissolved Organic Nitrogen |
attribute | M1_DON | description | String | Dissolved organic nitrogen (replicate "M1") |
attribute | M1_DON | long_name | String | M1 DON |
attribute | M1_DON | units | String | micromolar (uM) |
variable | M1_DONd15N | float | ||
attribute | M1_DONd15N | _FillValue | float | NaN |
attribute | M1_DONd15N | actual_range | float | 3.2, 6.0 |
attribute | M1_DONd15N | bcodmo_name | String | N |
attribute | M1_DONd15N | description | String | Dissolved organic nitrogen isotopic composition (replicate "M1") |
attribute | M1_DONd15N | long_name | String | M1 DONd15 N |
attribute | M1_DONd15N | units | String | per mil (0/00) |
variable | M2_DON | float | ||
attribute | M2_DON | _FillValue | float | NaN |
attribute | M2_DON | actual_range | float | 3.6, 7.0 |
attribute | M2_DON | bcodmo_name | String | Dissolved Organic Nitrogen |
attribute | M2_DON | description | String | Dissolved organic nitrogen (replicate "M2") |
attribute | M2_DON | long_name | String | M2 DON |
attribute | M2_DON | units | String | micromolar (uM) |
variable | M2_DONd15N | float | ||
attribute | M2_DONd15N | _FillValue | float | NaN |
attribute | M2_DONd15N | actual_range | float | 4.1, 5.1 |
attribute | M2_DONd15N | bcodmo_name | String | N |
attribute | M2_DONd15N | description | String | Dissolved organic nitrogen isotopic composition (replicate "M2") |
attribute | M2_DONd15N | long_name | String | M2 DONd15 N |
attribute | M2_DONd15N | units | String | per mil (0/00) |
variable | M3_DON | float | ||
attribute | M3_DON | _FillValue | float | NaN |
attribute | M3_DON | actual_range | float | 4.9, 6.5 |
attribute | M3_DON | bcodmo_name | String | Dissolved Organic Nitrogen |
attribute | M3_DON | description | String | Dissolved organic nitrogen (replicate "M3") |
attribute | M3_DON | long_name | String | M3 DON |
attribute | M3_DON | units | String | micromolar (uM) |
variable | M3_DONd15N | float | ||
attribute | M3_DONd15N | _FillValue | float | NaN |
attribute | M3_DONd15N | actual_range | float | 4.0, 6.7 |
attribute | M3_DONd15N | bcodmo_name | String | N |
attribute | M3_DONd15N | description | String | Dissolved organic nitrogen isotopic composition (replicate "M3") |
attribute | M3_DONd15N | long_name | String | M3 DONd15 N |
attribute | M3_DONd15N | units | String | per mil (0/00) |
variable | M1_d15NPNsink | float | ||
attribute | M1_d15NPNsink | _FillValue | float | NaN |
attribute | M1_d15NPNsink | actual_range | float | 0.2, 5.8 |
attribute | M1_d15NPNsink | bcodmo_name | String | N |
attribute | M1_d15NPNsink | description | String | Sinking particulate nitrogen isotopic composition (replicate "M1") |
attribute | M1_d15NPNsink | long_name | String | M1 D15 NPNsink |
attribute | M1_d15NPNsink | units | String | per mil (0/00) |
variable | M2_d15NPNsink | float | ||
attribute | M2_d15NPNsink | _FillValue | float | NaN |
attribute | M2_d15NPNsink | actual_range | float | 0.1, 4.5 |
attribute | M2_d15NPNsink | bcodmo_name | String | N |
attribute | M2_d15NPNsink | description | String | Sinking particulate nitrogen isotopic composition (replicate "M2") |
attribute | M2_d15NPNsink | long_name | String | M2 D15 NPNsink |
attribute | M2_d15NPNsink | units | String | per mil (0/00) |
variable | M3_d15NPNsink | float | ||
attribute | M3_d15NPNsink | _FillValue | float | NaN |
attribute | M3_d15NPNsink | actual_range | float | 0.6, 6.4 |
attribute | M3_d15NPNsink | bcodmo_name | String | N |
attribute | M3_d15NPNsink | description | String | Sinking particulate nitrogen isotopic composition (replicate "M3") |
attribute | M3_d15NPNsink | long_name | String | M3 D15 NPNsink |
attribute | M3_d15NPNsink | units | String | per mil (0/00) |
The information in the table above is also available in other file formats (.csv, .htmlTable, .itx, .json, .jsonlCSV1, .jsonlCSV, .jsonlKVP, .mat, .nc, .nccsv, .tsv, .xhtml) via a RESTful web service.