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Row Type | Variable Name | Attribute Name | Data Type | Value |
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attribute | NC_GLOBAL | access_formats | String | .htmlTable,.csv,.json,.mat,.nc,.tsv,.esriCsv,.geoJson |
attribute | NC_GLOBAL | acquisition_description | String | Acquisition methods are described in the following publication: Orcutt, B.N.\net al. 2005\n \nCore sectioning, porewater\\u00a0collection\\u00a0and analysis\n \nAt each sampling site, sediment sub-samples were collected for porewater\nanalyses and at selected depths for microbial rate assays (AOM, anaerobic\noxidation of methane oxidation; methanogenesis (MOG) from bicarbonate and\nacetate). Sediment was expelled from core liner using a hydraulic extruder\nunder anoxic conditions. The depth intervals for extrusion varied. At each\ndepth interval, a sub-sample was collected into a cut-off syringe for\ndissolved methane concentration quantification. Another 5 mL\\u00a0sub-\nsample\\u00a0was collected into pre-weighed and pre-combusted glass vial for\ndetermination of porosity (determined by the change in weight after drying at\n80 degrees celsius to a constant weight). The remaining material was used for\nporewater extraction. Sample fixation and\\u00a0analyses\\u00a0for dissolved\nconstituents followed the methods of Joye et al. (2010).\\u00a0\n \nMicrobial Activity Measurements\\u00a0\n \nTo determine AOM and MOG rates, 8 to 12 sub-samples (5 cm3) were collected\nfrom a core by manual insertion of a glass tube. For AOM, 100 uL of\ndissolved\\u00a014CH4\\u00a0tracer (about 2,000,000 DPM as gas) was injected\ninto each core. Samples were incubated for 36 to 48 hours at\\u00a0in\nsitu\\u00a0temperature.\\u00a0 Following incubation, samples were transferred to\n20 mL glass vials containing 2 mL of 2M NaOH (which served to arrest\nbiological activity and fix\\u00a014CO2\\u00a0as\\u00a014C-HCO3-).\\u00a0 Each\nvial was sealed with a\\u00a0teflon-lined screw cap, vortexed to mix the sample\nand base, and immediately frozen. Time zero samples were fixed immediately\nafter radiotracer injection. The specific activity of the tracer substrate\n(14CH4) was determined by injecting 50 uL directly into scintillation cocktail\n(Scintiverse BD) followed by liquid scintillation counting. The accumulation\nof 14C product (14CO2) was determined by acid digestion following the method\nof Joye et al. (2010).\\u00a0 The AOM rate was calculated using equation 1:\n \nAOM Rate = [CH4] x alphaCH4 /t x (a-14CO2/a-14CH4)\\u00a0\\u00a0\n\\u00a0\\u00a0\\u00a0 \\u00a0\\u00a0\\u00a0 \\u00a0(Eq. 1)\n \nHere, the AOM Rate is expressed as nmol CH4 oxidized per cm3 sediment per day\n(nmol\\u00a0cm-3 d-1), [CH4] is the methane concentration (uM), alphaCH4 is the\nisotope fractionation factor for AOM (1.06; (ALPERIN and REEBURGH, 1988)), t\nis the incubation time (d), a-14CO2 is the activity of the product pool, and\na-14CH4 is the activity of the substrate pool. If methane concentration was\nnot available, the turnover time of the 14CH4 tracer is presented.\n \nRates of bicarbonate-based-methanogenesis and acetoclastic methanogenesis were\ndetermined by incubating samples in gas-tight, closed-tube vessels without\nheadspace, to prevent the loss of gaseous 14CH4 product during sample\nmanipulation. These sample tubes were sealed using custom-designed plungers\n(black Hungate stoppers with the lip removed containing a plastic\n\\u201ctail\\u201d that was run through the stopper) were inserted at the base\nof the tube; the sediment was then pushed via the plunger to the top of the\ntube until a small amount protruded through the tube opening. A butyl rubber\nsepta\\u00a0was\\u00a0then eased into the tube opening to displace sediment in\ncontact with the atmosphere and close the tube, which was then sealed\nwith\\u00a0a open-top\\u00a0screw cap.\\u00a0 The rubber materials used in these\nassays were boiled in 1N NaOH for 1 hour, followed by several rinses in\nboiling milliQ, to leach potentially toxic substances. \\u00a0 \\u00a0\n \nA volume of radiotracer solution (100 uL of 14C-HCO3- tracer (~1 x\n107\\u00a0dpm\\u00a0in slightly alkaline milliQ\\u00a0water) or 1,2-14C-CH3COO-\ntracer (~5 x 107\\u00a0dpm\\u00a0in slightly alkaline milliQ\\u00a0water)) was\ninjected into each sample. Samples were incubated as described above and then\n2 ml of 2N NaOH was injected through the top stopper into each sample to\nterminate biological activity (time zero samples were fixed prior to tracer\ninjection).\\u00a0 Samples were mixed to evenly distribute NaOH through the\nsample.\\u00a0 Production of 14CH4 was quantified by stripping methane from the\ntubes with an air carrier, converting the 14CH4 to 14CO2 in a combustion\nfurnace, and subsequent trapping of the 14CO2 in NaOH as carbonate (CRAGG et\nal., 1990; CRILL and MARTENS, 1986).\\u00a0\\u00a0Activity\\u00a0of 14CO2 was\nmeasured subsequently by liquid scintillation counting.\\u00a0\n \nThe rates of Bi-MOG and Ac-MOG rates were calculated using equations 2 and 3,\nrespectively:\n \nBi-MOG Rate = [HCO3-] x alphaHCO3/t x\\u00a0 (a-14CH4/a-H14CO3-) \\u00a0 \\u00a0\n(Eq. 2)\n \nAc-MOG Rate = [CH3COO-] x alphaCH3COO-/t\\u00a0 x\\u00a0 (a-14CH4/a-14CH314COO-)\n\\u00a0 \\u00a0 (Eq. 3)\n \nBoth rates are expressed as nmol HCO3- or CH3COO-, respectively, reduced cm-3\nd-1, alphaHCO3\\u00a0and alphaCH3COO- are the isotope fractionation factors for\nMOG (assumed to be 1.06). [HCO3-] and [CH3COO-] are the\\u00a0pore\\u00a0water\nbicarbonate (mM) and acetate (uM) concentrations, respectively, t is\nincubation time (d), a-14CH4 is the activity of the product pool, and a-H14CO3\nand a-14CH314COO are the activities of the substrate pools. If samples for\nsubstrate concentration determination were not available, the substrate\nturnover constant instead of the rate is presented.\n \nFor water column methane oxidation rate assays, triplicate 20 mL of live water\n(in addition to one 20 mL sample which was killed with ethanol (750 uL of pure\nEtOH) before tracer addition) were transferred from the CTD into serum vials.\nSamples were amended with 2 x 10^6 DPM of 3H-labeled-methane tracer and\nincubated for 24 to 72 hours (linearity of activity was tested and confirmed).\nAfter incubation, samples were fixed with ethanol, as above, and a sub-sample\nto determine total sample activity (3H-methane + 3H-water) was collected.\nNext, the sample was purged with nitrogen to remove the 3H-methane tracer and\na sub-sample was amended with scintillation fluid and counted on a shipboard\nscintillation counter to determine the activity of tracer in the product of\n3H-methane oxidation, 3H-water. The methane oxidation rate was calculated as:\n \nMOX Rate = [methane concentration in nM] x alphaCH4/t\\u00a0 x\\u00a0 (a-3H-\nH2O/a-3H-CH4-) \\u00a0 \\u00a0 (Eq. 3) |
attribute | NC_GLOBAL | awards_0_award_nid | String | 651766 |
attribute | NC_GLOBAL | awards_0_award_number | String | PLR-1023444 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward?AWD_ID=1023444 |
attribute | NC_GLOBAL | awards_0_funder_name | String | NSF Division of Polar Programs |
attribute | NC_GLOBAL | awards_0_funding_acronym | String | NSF PLR |
attribute | NC_GLOBAL | awards_0_funding_source_nid | String | 490497 |
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 | Arctic Sediment Data \n S. Joye and V. Samarkin, PIs \n Version 4 October 2016 |
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 | 2016-10-04T21:16:40Z |
attribute | NC_GLOBAL | date_modified | String | 2019-04-22T21:24:55Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.660527.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | 172.361 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 78.942 |
attribute | NC_GLOBAL | geospatial_lat_min | double | 74.44 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | 172.361 |
attribute | NC_GLOBAL | geospatial_lon_min | double | 125.243 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/660527 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | CTD |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Used to collect water column samples |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 660538 |
attribute | NC_GLOBAL | instruments_0_description | String | The Conductivity, Temperature, Depth (CTD) unit is an integrated instrument package designed to measure the conductivity, temperature, and pressure (depth) of the water column. The instrument is lowered via cable through the water column and permits scientists observe the physical properties in real time via a conducting cable connecting the CTD to a deck unit and computer on the ship. The CTD is often configured with additional optional sensors including fluorometers, transmissometers and/or radiometers. It is often combined with a Rosette of water sampling bottles (e.g. Niskin, GO-FLO) for collecting discrete water samples during the cast. This instrument designation is used when specific make and model are not known. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/130/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | CTD profiler |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 417 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | CTD |
attribute | NC_GLOBAL | instruments_1_acronym | String | Multi Corer |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | Core used in sampling |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 660536 |
attribute | NC_GLOBAL | instruments_1_description | String | The Multi Corer is a benthic coring device used to collect multiple, simultaneous, undisturbed sediment/water samples from the seafloor. Multiple coring tubes with varying sampling capacity depending on tube dimensions are mounted in a frame designed to sample the deep ocean seafloor. For more information, see Barnett et al. (1984) in Oceanologica Acta, 7, pp. 399-408. |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/51/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Multi Corer |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 532 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Multiple core |
attribute | NC_GLOBAL | instruments_2_acronym | String | LSC |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | Used to determine activity of tracer substrate |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 660537 |
attribute | NC_GLOBAL | instruments_2_description | String | Liquid scintillation counting is an analytical technique which is defined by the incorporation of the radiolabeled analyte into uniform distribution with a liquid chemical medium capable of converting the kinetic energy of nuclear emissions into light energy. Although the liquid scintillation counter is a sophisticated laboratory counting system used the quantify the activity of particulate emitting (ß and a) radioactive samples, it can also detect the auger electrons emitted from 51Cr and 125I samples. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB21/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Liquid Scintillation Counter |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 624 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | Liquid scintillation counter |
attribute | NC_GLOBAL | keywords | String | aom, AOM_rate, bco, bco-dmo, biological, carbonate, ch3, ch4, chemical, co3, collection, collection_type, coo, data, dataset, depth, dmo, erddap, h14, latitude, longitude, management, mog, month, oceanography, office, preliminary, rate, sample, sample_ID, sed, sed_CH4, sediment, sediment_depth, srr, station, turnover, turnover_14_CH3COO_MOG, turnover_H14_CO3_MOG, turnover_SRR, type, year |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/660527/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/660527 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 78.942 |
attribute | NC_GLOBAL | param_mapping | String | {'660527': {'lat': 'master - latitude', 'sediment_depth': 'flag - depth', 'lon': 'master - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/660527/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | University of Georgia |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | UGA |
attribute | NC_GLOBAL | people_0_person_name | String | Samantha B. Joye |
attribute | NC_GLOBAL | people_0_person_nid | String | 51421 |
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 | University of Georgia |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | UGA |
attribute | NC_GLOBAL | people_1_person_name | String | Vladimir Samarkin |
attribute | NC_GLOBAL | people_1_person_nid | String | 641543 |
attribute | NC_GLOBAL | people_1_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_1_role_type | String | originator |
attribute | NC_GLOBAL | people_2_affiliation | String | University of Georgia |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | UGA |
attribute | NC_GLOBAL | people_2_person_name | String | Samantha B. Joye |
attribute | NC_GLOBAL | people_2_person_nid | String | 51421 |
attribute | NC_GLOBAL | people_2_role | String | Contact |
attribute | NC_GLOBAL | people_2_role_type | String | related |
attribute | NC_GLOBAL | people_3_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_3_person_name | String | Hannah Ake |
attribute | NC_GLOBAL | people_3_person_nid | String | 650173 |
attribute | NC_GLOBAL | people_3_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_3_role_type | String | related |
attribute | NC_GLOBAL | project | String | ESAS Water Column Methane |
attribute | NC_GLOBAL | projects_0_acronym | String | ESAS Water Column Methane |
attribute | NC_GLOBAL | projects_0_description | String | We propose to study methane (CH4) release over the East Siberian Arctic shelf (ESAS), the largest (~10% of the world ocean shelf area) and the shallowest shelf (mean depth |
attribute | NC_GLOBAL | projects_0_end_date | String | 2015-08 |
attribute | NC_GLOBAL | projects_0_geolocation | String | East Siberian Arctic Shelf |
attribute | NC_GLOBAL | projects_0_name | String | The East Siberian Arctic Shelf as a Source of Atmospheric Methane: First Approach to Quantitative Assessment |
attribute | NC_GLOBAL | projects_0_project_nid | String | 651769 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2010-09 |
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 | Southernmost_Northing | double | 74.44 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | subsetVariables | String | year,month,collection_type |
attribute | NC_GLOBAL | summary | String | Sediment geochemical and microbial activity data collected on R/V Oden along the East Siberian Arctic Shelf from 2014 (ESAS Water Column Methane project) |
attribute | NC_GLOBAL | title | String | [Multi-core Arctic sediment data] - Sediment geochemical and microbial activity data collected on R/V Oden along the East Siberian Arctic Shelf from 2014 (ESAS Water Column Methane project) (The East Siberian Arctic Shelf as a Source of Atmospheric Methane: First Approach to Quantitative Assessment) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | 125.243 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | year | short | ||
attribute | year | _FillValue | short | 32767 |
attribute | year | actual_range | short | 2014, 2014 |
attribute | year | bcodmo_name | String | year |
attribute | year | description | String | Year of sampling; YYYY |
attribute | year | long_name | String | Year |
attribute | year | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/YEARXXXX/ |
attribute | year | units | String | unitless |
variable | month | byte | ||
attribute | month | _FillValue | byte | 127 |
attribute | month | actual_range | byte | 7, 7 |
attribute | month | bcodmo_name | String | month |
attribute | month | description | String | Month of sampling; mm |
attribute | month | long_name | String | Month |
attribute | month | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/MNTHXXXX/ |
attribute | month | units | String | unitless |
variable | collection_type | String | ||
attribute | collection_type | bcodmo_name | String | sampling_method |
attribute | collection_type | description | String | Method used to collect samples |
attribute | collection_type | long_name | String | Collection Type |
attribute | collection_type | units | String | unitless |
variable | station | byte | ||
attribute | station | _FillValue | byte | 127 |
attribute | station | actual_range | byte | 1, 63 |
attribute | station | bcodmo_name | String | station |
attribute | station | description | String | Station where sampling occurred |
attribute | station | long_name | String | Station |
attribute | station | units | String | unitless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | 74.44, 78.942 |
attribute | latitude | axis | String | Y |
attribute | latitude | bcodmo_name | String | latitude |
attribute | latitude | colorBarMaximum | double | 90.0 |
attribute | latitude | colorBarMinimum | double | -90.0 |
attribute | latitude | description | String | Latitude |
attribute | latitude | ioos_category | String | Location |
attribute | latitude | long_name | String | Latitude |
attribute | latitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LATX/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | 125.243, 172.361 |
attribute | longitude | axis | String | X |
attribute | longitude | bcodmo_name | String | longitude |
attribute | longitude | colorBarMaximum | double | 180.0 |
attribute | longitude | colorBarMinimum | double | -180.0 |
attribute | longitude | description | String | Longitude |
attribute | longitude | ioos_category | String | Location |
attribute | longitude | long_name | String | Longitude |
attribute | longitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LONX/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | sample_ID | String | ||
attribute | sample_ID | bcodmo_name | String | sample |
attribute | sample_ID | description | String | PI issued sample ID number |
attribute | sample_ID | long_name | String | Sample ID |
attribute | sample_ID | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P02/current/ACYC/ |
attribute | sample_ID | units | String | unitless |
variable | sediment_depth | double | ||
attribute | sediment_depth | _FillValue | double | NaN |
attribute | sediment_depth | actual_range | double | -5.0, 52.5 |
attribute | sediment_depth | bcodmo_name | String | depth_core |
attribute | sediment_depth | description | String | Depth of sediment; negative depth values represent overlying water samples |
attribute | sediment_depth | long_name | String | Sediment Depth |
attribute | sediment_depth | units | String | centimeters |
variable | sed_CH4 | float | ||
attribute | sed_CH4 | _FillValue | float | NaN |
attribute | sed_CH4 | actual_range | float | 0.0, 53.52 |
attribute | sed_CH4 | bcodmo_name | String | unknown |
attribute | sed_CH4 | description | String | Methane concentration in sediment |
attribute | sed_CH4 | long_name | String | Sed CH4 |
attribute | sed_CH4 | units | String | microns (uM) |
variable | AOM_rate | float | ||
attribute | AOM_rate | _FillValue | float | NaN |
attribute | AOM_rate | actual_range | float | 0.05, 247.62 |
attribute | AOM_rate | bcodmo_name | String | unknown |
attribute | AOM_rate | description | String | Anaerobic Oxidation of Methane; CH4 oxidized in sediment per day; Rates were measured at stations 13 and 23 only. |
attribute | AOM_rate | long_name | String | AOM Rate |
attribute | AOM_rate | units | String | picomole per centimeter per day (pmol/cm/day) |
variable | turnover_14_CH3COO_MOG | String | ||
attribute | turnover_14_CH3COO_MOG | bcodmo_name | String | unknown |
attribute | turnover_14_CH3COO_MOG | description | String | 14-CH3COO methanogenesis turnover; Rates were measured at stations 13 and 23 only. |
attribute | turnover_14_CH3COO_MOG | long_name | String | Turnover 14 CH3 COO MOG |
attribute | turnover_14_CH3COO_MOG | units | String | percent |
variable | turnover_H14_CO3_MOG | String | ||
attribute | turnover_H14_CO3_MOG | bcodmo_name | String | unknown |
attribute | turnover_H14_CO3_MOG | description | String | H14-CO3 methanogenesis turnover; Rates were measured at stations 13 and 23 only. |
attribute | turnover_H14_CO3_MOG | long_name | String | Turnover H14 CO3 MOG |
attribute | turnover_H14_CO3_MOG | units | String | percent |
variable | turnover_SRR | float | ||
attribute | turnover_SRR | _FillValue | float | NaN |
attribute | turnover_SRR | actual_range | float | 0.002, 0.127 |
attribute | turnover_SRR | bcodmo_name | String | unknown |
attribute | turnover_SRR | description | String | Sulfate reduction methanogenesis turnover; Rates were measured at stations 13 and 23 only. |
attribute | turnover_SRR | long_name | String | Turnover SRR |
attribute | turnover_SRR | units | String | percent |