BCO-DMO ERDDAP
Accessing BCO-DMO data |
log in
Brought to you by BCO-DMO |
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 | Sample Collection \n Samples were collected on two separate research cruises aboard the R/V Kilo\nMoana in August 2014 and May 2015. Sampling was conducted at the Hawaii Ocean\nTime Series Station ALOHA (A Long-Term Oligotrophic Habitat Assessment;\n22\\u00b0 45'N, 158\\u00b0 00'W) and the Bermuda Atlantic Time Series Site\n(BATS; 31\\u00b0 40'N, 64\\u00b0 10'W) in the Central North Atlantic.\n \nSurface water was sampled via the vessel's underway sampling system. The\nintake pipe is situated on the forward starboard hull section of the vessel\napproximately 7.5 m below the waterline. The laboratory seawater tap was\nallowed to flush for 2 hours prior to each sampling. Seawater was pre-filtered\nthrough 53 \\u00b5m Nitex mesh, and pumped through a 0.2 \\u00b5m\npolyethersulfone (PES) cartridge filter (Shelco Filters, Micro Vantage, water\ngrade, 9.75\\\" DOE, polycarbonate housing) prior to introduction to the\nultrafiltration system. Large volume subsurface water samples were collected\nusing successive casts of a rosette equipped with 24 x 12 L Niskin bottles.\n \nTangential-Flow Ultrafiltration \n The main UF system was constructed using a modified design of the system\ndescribed in Roland et al. (2009), and expanded on by Walker et al. (2011).\nBriefly, the system was comprised of four-spiral wound PES UF membranes,\nhaving a nominal molecular weight cut off of 2.5 kD (GE Osmonics GH2540F30,\n40-inch long, 2.5-inch diameter). The membranes were mounted in stainless\nsteel housings, plumbed in parallel to a 100 L fluorinated HDPE reservoir,\nwith flow driven by a 1.5 HP stainless steel centrifugal pump (Goulds Pumps,\nStainless steel centrifugal pump, NPE series 1 x 1-1/4 -6, close coupled to a\n1-1/2 horsepower, 3500 RPM, 60 Hz, 3 phase, Open Drip Proof Motor; 5.75 Inch\nImpeller Diameter, Standard Viton Mechanical Seals). All other system plumbing\ncomponents contacting seawater were composed of polytetrafluoroethylene (PTFE)\nor stainless steel.\n \nThe system was run continuously at a membrane pressure of 40-50 psi, resulting\nin permeation flow rates of 1-2 L/min, depending primarily on the temperature\nof the feed seawater. Sample water was fed into the system using peristaltic\npumps and platinum cured silicone tubing at a flow rate matched to the system\npermeation rates to ensure a constant system volume of approximately 100 L.\n \nSeawater samples of 3000-4000 L were concentrated to a final retentate volume\nof 15-20 L, drained from the system into acid washed PC carboys and\nrefrigerated (less than 12 hours at 2C) until the next phase of processing.\nSamples requiring storage for longer than 12 hours were frozen and stored at\n-20\\u00b0C. The UF system was then reconfigured to a smaller volume system,\nconsisting of a single membrane having a smaller nominal molecular weight\ncutoff (GE Osmonics GE2540F30, 40-inch long, 2.5-inch diameter, 1 kD MWCO),\nand a 2.5 L PES reservoir for further volume reduction and subsequent salt\nremoval (diafiltration). Using this smaller system, samples were reduced to\n2-3 L under lower pressure (25 psi, permeation rate = 250 mL/min). Samples\nwere then diafiltered using 40 L of 18.2 M\\u03a9 Milli-Q (ultrapure) water,\nadding water to the sample retentate reservoir at the same rate of membrane\npermeation. Reduced and diafiltered samples were stored in acid washed PC\nbottles at -20\\u00b0C for transport. In the laboratory, samples were further\nconcentrated by rotary evaporation using pre-combusted glassware (450 \\u00b0C,\n5 h). A molecular sieve and a liquid nitrogen trap were placed between the\nvacuum pump and rotovap chamber to ensure no contamination of isolated\nmaterial by back streaming of hydrocarbons or other contaminants. After\nreduction to 50-100 mL, samples were dried to powder via centrifugal\nevaporation in PTFE centrifuge tubes. Dry material was homogenized with an\nethanol cleaned agate mortar and pestle, transferred to pre-combusted glass\nvials, and stored in a desiccation cabinet until subsequent analyses.\n \nSolid Phase Extraction \n Solid phase extraction was conducted using PPL sorbent (Agilent Bondesil\nPPL, 125 \\u00b5m particle size, part # 5982-0026) following the general\nrecommendations of Dittmar et al. (2008) and Green et al. (2014), including\nloading rates, seawater to sorbent ratios, and elution volumes and rates.\nBetween 300 and 500 g of sorbent was used for each extraction, depending on\nsample volume and DOC concentration, with average loading of 4.2 \\u00b1 1.5 L\nUF permeate per g sorbent representing 1.9 \\u00b1 0.6 mg DOC per g sorbent or\na DOC to sorbent mass ratio of 1:600 \\u00b1 200. This is in line with both the\nrecommendations of Dittmar et al. (2008) (maximum loading = 10 L seawater per\ng sorbent) and Li et al. (2016) (DOC to sorbent ratio = 1:800). Permeate from\nthe UF system was fed through PTFE tubing to a pair of 200 L HDPE barrels. The\npermeate water was then acidified in 200 L batches to pH 2 by adding 400 mL of\n6 M HCl (Fisher Chemical, ACS Plus grade). Batch samples were mixed\ncontinuously during collection, acidification, and loading using a peristaltic\npump and platinum cured Si and PTFE tubing positioned at the surface and\nbottom of each barrel. Acidified batches of seawater permeate were then pumped\nthrough the SPE sorbent. SPE flow rates were matched to UF permeation rates\n(1-2 L/min), such that a pair of 200 L barrels allowed one barrel to be filled\nwhile the contents of the other was passed through the sorbent.\n \nThree custom SPE column configurations were used to contain the sorbent\nmaterial. The column configuration was modified several times for ease of use\non subsequent cruises. First, an open, gravity fed, large (49 mm ID x 1000 mm\nlength, 1875 mL volume) glass chromatography column with 40 \\u00b5m fritted\ndisk and PTFE stopcock (Kimble-Chase, Kontes) was used. Next, we tested a\ncustom built high-pressure SS housing (10 cm ID x 3.5 cm bed height), and\nfinally a parallel combination of 2 medium-pressure glass chromatography\ncolumns (Kimble-Chase, Kontes, Chromaflex LC, 4.8 mm ID x 30 cm, 543 mL\nvolume). While all designs proved to be functionally equivalent, the latter\nparallel combination of 2 medium-pressure glass columns ultimately provided\nthe best configuration in order to maximize flow rates while simultaneously\noptimizing the ratio of sorbent bed height to loading speed. Further, the\ncommercial availability and ease of use associated with this configuration\nmade it our preferred design.\n \nFollowing sample loading, the SPE sorbent was desalted with 6 L of pH 2\nultrapure water at a low flow rate (250-300 mL/min). After desalting, the SPE\nsorbent was transferred to a glass chromatography column (75 mm ID x 300 mm\nlength, 40 \\u00b5m fritted disk, PTFE stopcock) with ultrapure water rinses to\nensure quantitative transfer. Isolated organic material was then eluted from\nthe sorbent with five to six 500 mL additions of methanol. The eluted methanol\nsolution was stored in pre-combusted amber glass bottles at -20\\u00b0C for\ntransport. Similar to UF samples, the methanol-eluted solutions were first\nreduced by rotary evaporation to 50-100 mL. Samples were then dried to powder\nvia centrifugal evaporation in PTFE centrifuge tubes. Dry material was\nhomogenized with an ethanol cleaned agate mortar and pestle, transferred to\npre-combusted glass vials, and stored in a desiccation cabinet until elemental\nand isotopic analyses.\n \nAmino Acid Enantiomeric Analysis \n AA enantiomers were analyzed by gas chromatography-mass spectrometry (GC-MS;\nAgilent 7890A + 5975B) using a chiral column (Altech Chirasi-L-Val, 50 m\nlength, 0.25 mm internal diameter, 0.16 \\u03bcm film thickness). 1 \\u03bcL of\nsample was injected through a splitless inlet at 200\\u00b0C, using helium\ncarrier (0.9 mL/min). Individual amino acids were separated using a 4-ramp,\n57.5 min temperature program: 45\\u00b0C start;\\u00a0 2\\u00b0C/min to\n75\\u00b0C;\\u00a0 4\\u00b0C/min to 110\\u00b0C;\\u00a0 1\\u00b0C/min to\n125\\u00b0C;\\u00a0 4\\u00b0C/min to a final temperature of 200\\u00b0C.\nQuantification was based on retention times for authentic D and L standards of\neach AA, coupled with ion peak areas obtained using single-ion monitoring,\nbased on the following characteristic ion fragments (m/z): Alanine (Ala), 140;\nvaline (Val), 168.1; threonine (Thr), 153; glycine (Gly), 126; isoleucine and\nleucine (Ile and Leu), 182.1; serine (Ser), 138; proline (Pro), 166.1;\naspartic acid (Asp), 184; glutamic acid (Glu), 180; and phenylalanine (Phe),\n190.1. Total amino acid yields, and relative abundance were quantified using\nmixed L-AA standards in a linear four-point calibration curve ranging from\n1-1000 \\u03bcmol/AA. For each AA, peak areas for both enantiomers were\nconverted to molar quantities using the calibration curve for the\ncorresponding ion fragment. Molar percentage abundance (Mol%) for each AA\nmeasured was calculated using the sum of the D and L enantiomers. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 701743 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1358041 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1358041 |
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 | Amino Acid Enantiomeric Ratios (D/L) \n PI: Matthew McCarthy (UC Santa Cruz) \n Co-PI: Thomas Guilderson (UC Santa Cruz) \n Version date: 13 May 2020 |
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 | dataset_current_state | String | Final and no updates |
attribute | NC_GLOBAL | date_created | String | 2020-05-13T19:42:12Z |
attribute | NC_GLOBAL | date_modified | String | 2020-05-20T15:39:28Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.26008/1912/bco-dmo.811458.1 |
attribute | NC_GLOBAL | geospatial_vertical_max | double | 2500.0 |
attribute | NC_GLOBAL | geospatial_vertical_min | double | 7.5 |
attribute | NC_GLOBAL | geospatial_vertical_positive | String | down |
attribute | NC_GLOBAL | geospatial_vertical_units | String | m |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/811458 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 811469 |
attribute | NC_GLOBAL | instruments_0_description | String | A Niskin bottle (a next generation water sampler based on the Nansen bottle) is a cylindrical, non-metallic water collection device with stoppers at both ends. The bottles can be attached individually on a hydrowire or deployed in 12, 24, or 36 bottle Rosette systems mounted on a frame and combined with a CTD. Niskin bottles are used to collect discrete water samples for a range of measurements including pigments, nutrients, plankton, etc. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0412/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Niskin bottle |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 413 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | rosette equipped with 24 x 12 L Niskin bottles |
attribute | NC_GLOBAL | instruments_1_acronym | String | Pump-Ship Intake |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 811468 |
attribute | NC_GLOBAL | instruments_1_description | String | The 'Pump-underway ship intake' system indicates that samples are from the ship's clean water intake pump. This is essentially a surface water sample from a source of uncontaminated near-surface (commonly 3 to 7 m) seawater that can be pumped continuously to shipboard laboratories on research vessels. There is typically a temperature sensor near the intake (known as the hull temperature) to provide measurements that are as close as possible to the ambient water temperature. The flow from the supply is typically directed through continuously logged sensors such as a thermosalinograph and a fluorometer. Water samples are often collected from the underway supply that may also be referred to as the non-toxic supply. Ideally the data contributor has specified the depth in the ship's hull at which the pump is mounted. |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/31/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Pump - Surface Underway Ship Intake |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 534 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | underway sampling system |
attribute | NC_GLOBAL | instruments_2_acronym | String | Gas Chromatograph |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 811475 |
attribute | NC_GLOBAL | instruments_2_description | String | Instrument separating gases, volatile substances, or substances dissolved in a volatile solvent by transporting an inert gas through a column packed with a sorbent to a detector for assay. (from SeaDataNet, BODC) |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB02/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Gas Chromatograph |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 661 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | GC-MS; Agilent 7890A + 5975B |
attribute | NC_GLOBAL | instruments_3_acronym | String | Mass Spec |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 811476 |
attribute | NC_GLOBAL | instruments_3_description | String | General term for instruments used to measure the mass-to-charge ratio of ions; generally used to find the composition of a sample by generating a mass spectrum representing the masses of sample components. |
attribute | NC_GLOBAL | instruments_3_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB16/ |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Mass Spectrometer |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 685 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | GC-MS; Agilent 7890A + 5975B |
attribute | NC_GLOBAL | keywords | String | acid, amino, amino_acid, bco, bco-dmo, biological, chemical, D_L_ratio, D_L_ratio_stdev, data, dataset, depth, deviation, dmo, erddap, management, mol, Mol_pcnt, Mol_pcnt_stdev, oceanography, office, pcnt, pcnt_D, pcnt_D_stdev, preliminary, ratio, sample, sample_type, season, standard, standard deviation, stdev, type, year |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/811458/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/811458 |
attribute | NC_GLOBAL | param_mapping | String | {'811458': {'depth': 'flag - depth'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/811458/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | University of California-Santa Cruz |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | UC Santa Cruz |
attribute | NC_GLOBAL | people_0_person_name | String | Matthew D. McCarthy |
attribute | NC_GLOBAL | people_0_person_nid | String | 557245 |
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 California-Santa Cruz |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | UC Santa Cruz |
attribute | NC_GLOBAL | people_1_person_name | String | Thomas Guilderson |
attribute | NC_GLOBAL | people_1_person_nid | String | 51494 |
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 | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_2_person_name | String | Shannon Rauch |
attribute | NC_GLOBAL | people_2_person_nid | String | 51498 |
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 | DON Microbial Nitrogen Pump |
attribute | NC_GLOBAL | projects_0_acronym | String | DON Microbial Nitrogen Pump |
attribute | NC_GLOBAL | projects_0_description | String | Dissolved organic nitrogen is one of the most important - but perhaps least understood - components of the modern ocean nitrogen cycle. While dissolved organic nitrogen represents a main active reservoir of fixed and seemingly biologically-available nitrogen, at the same time most of ocean's dissolved organic nitrogen pool is also apparently unavailable for use by organisms. Recently, the idea of the \"Microbial Carbon Pump\" has emerged, providing a renewed focus on microbes as primary agents for the formation of biologically-available dissolved material. However, the role that microbes play in transformation of biologically-available dissolved organic nitrogen is still lacking. In order to fill gaps in this knowledge, researchers from the University of California Santa Cruz will apply a series of new analytical approaches to test the role of microbial source and transformation in formation of the ocean's biologically-available dissolved organic nitrogen pool. Results from this study will address one of the major unknowns of both chemical oceanography and the ocean nitrogen cycle.\nBroader Impacts:\nThis proposal will provide oceanographers new tools to test ideas of microbial organic matter sequestration in a world where the oceans are rapidly changing. High school, undergraduate, graduate and post-doctoral education will be furthered through active participation in lab, field, and data synthesis activities. |
attribute | NC_GLOBAL | projects_0_end_date | String | 2017-03 |
attribute | NC_GLOBAL | projects_0_geolocation | String | North Pacific Subtropical Gyre (HOT station), North Atlantic Subtropical Gyre (BATS time series station), California Margin |
attribute | NC_GLOBAL | projects_0_name | String | The Microbial Nitrogen Pump: Coupling 14C and Compound-specific Amino Acids to Understand the Role of Microbial Transformations in the Refractory Ocean DON Pool |
attribute | NC_GLOBAL | projects_0_project_nid | String | 701744 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2014-04 |
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 | subsetVariables | String | location |
attribute | NC_GLOBAL | summary | String | Amino acid enantiomeric ratios (D/L) of high and low molecular weight (HMW,\nLMW) DOM collected from the North Pacific Subtropical Gyre and Central North\nAtlantic. These data were published in Broek et al. (2019) and Broek et al.\n(2017). |
attribute | NC_GLOBAL | title | String | [Amino Acid Enantiomeric Ratios] - Amino acid enantiomeric ratios (D/L) of high and low molecular weight (HMW, LMW) DOM collected from the North Pacific Subtropical Gyre and Central North Atlantic (The Microbial Nitrogen Pump: Coupling 14C and Compound-specific Amino Acids to Understand the Role of Microbial Transformations in the Refractory Ocean DON Pool) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.5 |
variable | location | String | ||
attribute | location | bcodmo_name | String | site |
attribute | location | description | String | Sample collection location. HOT = Hawaii Ocean Time Series station ALOHA (22° 45'N, 158° 00'W) in North Pacific Subtropical Gyre (NPSG); BATS = Hawaii Ocean Time Series station ALOHA (22° 45'N, 158° 00'W) in North Pacific Subtropical Gyre (NPSG) |
attribute | location | long_name | String | Location |
attribute | location | units | String | unitless |
variable | year | short | ||
attribute | year | _FillValue | short | 32767 |
attribute | year | actual_range | short | 2014, 2015 |
attribute | year | bcodmo_name | String | year |
attribute | year | description | String | Year of sample collection; format: 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 | season | String | ||
attribute | season | bcodmo_name | String | season |
attribute | season | description | String | Season of sample collection |
attribute | season | long_name | String | Season |
attribute | season | units | String | unitless |
variable | sample_type | String | ||
attribute | sample_type | bcodmo_name | String | sample_type |
attribute | sample_type | description | String | DOM Fraction |
attribute | sample_type | long_name | String | Sample Type |
attribute | sample_type | units | String | unitless |
variable | depth | double | ||
attribute | depth | _CoordinateAxisType | String | Height |
attribute | depth | _CoordinateZisPositive | String | down |
attribute | depth | _FillValue | double | NaN |
attribute | depth | actual_range | double | 7.5, 2500.0 |
attribute | depth | axis | String | Z |
attribute | depth | bcodmo_name | String | depth |
attribute | depth | colorBarMaximum | double | 8000.0 |
attribute | depth | colorBarMinimum | double | -8000.0 |
attribute | depth | colorBarPalette | String | TopographyDepth |
attribute | depth | description | String | Sample depth |
attribute | depth | ioos_category | String | Location |
attribute | depth | long_name | String | Depth |
attribute | depth | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/DEPH/ |
attribute | depth | positive | String | down |
attribute | depth | standard_name | String | depth |
attribute | depth | units | String | m |
variable | amino_acid | String | ||
attribute | amino_acid | bcodmo_name | String | amino_acid |
attribute | amino_acid | description | String | Amino acid |
attribute | amino_acid | long_name | String | Amino Acid |
attribute | amino_acid | units | String | unitless |
variable | Mol_pcnt | float | ||
attribute | Mol_pcnt | _FillValue | float | NaN |
attribute | Mol_pcnt | actual_range | float | 1.6, 38.6 |
attribute | Mol_pcnt | bcodmo_name | String | amino_conc |
attribute | Mol_pcnt | description | String | Relative amino acid molar abundance |
attribute | Mol_pcnt | long_name | String | Mol Pcnt |
attribute | Mol_pcnt | units | String | unitless (percent) |
variable | Mol_pcnt_stdev | float | ||
attribute | Mol_pcnt_stdev | _FillValue | float | NaN |
attribute | Mol_pcnt_stdev | actual_range | float | 0.2, 3.9 |
attribute | Mol_pcnt_stdev | bcodmo_name | String | amino_conc |
attribute | Mol_pcnt_stdev | description | String | Standard deviation of Mol_pcnt |
attribute | Mol_pcnt_stdev | long_name | String | Mol Pcnt Stdev |
attribute | Mol_pcnt_stdev | units | String | unitless (percent) |
variable | pcnt_D | float | ||
attribute | pcnt_D | _FillValue | float | NaN |
attribute | pcnt_D | actual_range | float | 1.3, 44.3 |
attribute | pcnt_D | bcodmo_name | String | amino_conc |
attribute | pcnt_D | description | String | Relative amount of D-amino acid enantiomer |
attribute | pcnt_D | long_name | String | PCNT D |
attribute | pcnt_D | units | String | unitless (percent) |
variable | pcnt_D_stdev | float | ||
attribute | pcnt_D_stdev | _FillValue | float | NaN |
attribute | pcnt_D_stdev | actual_range | float | 0.3, 1.4 |
attribute | pcnt_D_stdev | bcodmo_name | String | amino_conc |
attribute | pcnt_D_stdev | description | String | Standard deviation of pcnt_D |
attribute | pcnt_D_stdev | long_name | String | Pcnt D Stdev |
attribute | pcnt_D_stdev | units | String | unitless (percent) |
variable | D_L_ratio | float | ||
attribute | D_L_ratio | _FillValue | float | NaN |
attribute | D_L_ratio | actual_range | float | 0.01, 0.79 |
attribute | D_L_ratio | bcodmo_name | String | amino_conc |
attribute | D_L_ratio | description | String | Ratio of D-AA to L-AA abundance |
attribute | D_L_ratio | long_name | String | D L Ratio |
attribute | D_L_ratio | units | String | unitless |
variable | D_L_ratio_stdev | float | ||
attribute | D_L_ratio_stdev | _FillValue | float | NaN |
attribute | D_L_ratio_stdev | actual_range | float | 0.003, 0.014 |
attribute | D_L_ratio_stdev | bcodmo_name | String | amino_conc |
attribute | D_L_ratio_stdev | description | String | Standard deviation of D_L_ratio |
attribute | D_L_ratio_stdev | long_name | String | D L Ratio Stdev |
attribute | D_L_ratio_stdev | units | String | unitless |