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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 |
attribute | NC_GLOBAL | acquisition_description | String | Sample collection: \n Pteropods were collected from upper ocean water down to a maximum depth of\n200 m from various locations across the Scotia Sea using a combination of\nvertically and obliquely towed Bongo nets and MOCNESS nets during the JR177\nresearch cruise. Oblique tows were carried out at speeds of less than 1 knot.\n \nExperimental conditions: \n A fraction of the captured specimens was preserved immediately in 70%\nethanol to act as controls for comparison with those exposed to raised pCO2\nconditions. A further fraction of specimens was incubated at various levels of\npCO2 to test the effect on shell dissolution. Two liter bottles containing\nfiltered sea water (0.7 um filters) were bubbled with air/CO2 mixtures of 500\nppm, 750 ppm, and 1200 ppm, until the required xCO2 was reached. An average of\n30 live pteropod of Limacina helicina ant. were incubated in each experimental\ncontainer and maintained for 4, 8, and 14 days before extraction and immediate\npreservation in 70% ethanol. The majority of specimens were juvenile stages of\nLimacina helicina ant., but the incubations were also carried out on adult\nstages of both Limacina helicina ant. and Clio pyramidata f. ant.\n \nOmega was assessed from measurements of DIC (dissolved inorganic carbon) and\ntotal alkalinity (TA) at the start and end of each incubation experiment. DIC\nand TA were measured using VINDTA instrument (Versatile INstrument for the\nDetermination of Titration Alkalinity, Marianda, Kiel, Germany) following the\nStandard Operating Procedures for oceanic CO2 measurements (Dickson et al.\n2007) with a Certified Reference Material (CRM) analysed in duplicate at the\nbeginning and end of each sample analysis day. Other carbonate chemistry\nparameters (total pH and Omega-aragonite) were calculated from all discrete\nsamples using\\u00a0 DIC, TA, temperature, salinity, pressure and macronutrient\nconcentrations using the CO2SYS programme (Lewis and Wallace 1998) with\nthermodynamic dissociation constants for K1 and K2 by Mehrbach et al. (1973)\nrefitted by Dickson & Millero (1987).\n \nShell dehydration: \n Dehydration was undertaken using 2,2-Dimethoxypropane (DMP; chemical\nformula: (CH3)2C(OCH3)2), and 1,1,1,3,3,3-hexamethyldisilazane (HMDS; chemical\nformula: (CH3)3SiNHSi(CH3)3). Before starting dehydration with DMP, the shells\nwere transferred to 50% methanol for two 5 min washes then transferred to 85%\nmethanol (10 min). Complete tissue dehydration was accomplished by immersion\nin DMP: two changes at 15-20 min each. It was important not to let the shells\nair dry at this stage, so they were transferred to a 1:1 mixture of DMP and\nHMDS for about 10 min, followed by 100% HMDS for 20\\u201325 min twice. The\nHMDS was subsequently allowed to evaporate allowing the shells to dry\ncompletely (Figure 2 of Bednarsek et al., 2012). The moderate vapor pressure\nand very low surface tension of HMDS allowed the shells to dry without\ndistortion or loss of shell integrity.\n \nSEM: \n Scanning Electron Microscopy (SEM) was done using a JEOL JSM 5900LV fitted\nwith a tungsten filament at an acceleration voltage of 15 kV and a working\ndistance of about 10 mm. Analysis of SEM photos enabled observation of the\nshell surface and identification of shell dissolution. Refer to Bednarsek et\nal. (2012) for more information on dissolution types. |
attribute | NC_GLOBAL | awards_0_award_nid | String | 54896 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1041106 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1041106 |
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 | David L. Garrison |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 50534 |
attribute | NC_GLOBAL | awards_1_award_nid | String | 489479 |
attribute | NC_GLOBAL | awards_1_award_number | String | NE/H017267/1 |
attribute | NC_GLOBAL | awards_1_data_url | String | http://gtr.rcuk.ac.uk/project/098910A1-90B5-48DD-8EDA-E546F7FD36EC |
attribute | NC_GLOBAL | awards_1_funder_name | String | United Kingdom Natural Environmental Research Council |
attribute | NC_GLOBAL | awards_1_funding_acronym | String | NERC |
attribute | NC_GLOBAL | awards_1_funding_source_nid | String | 363 |
attribute | NC_GLOBAL | awards_2_award_nid | String | 489482 |
attribute | NC_GLOBAL | awards_2_award_number | String | MEST-CT-2004-514159 |
attribute | NC_GLOBAL | awards_2_funder_name | String | European Commission Marie Curie Actions Program |
attribute | NC_GLOBAL | awards_2_funding_acronym | String | EC - Marie Curie Actions |
attribute | NC_GLOBAL | awards_2_funding_source_nid | String | 489481 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Pteropod shell dissolution \n Lead PI: Geraint Tarling \n Co-PIs: Dorothee C.E. Bakker & Sophie Fielding \n Contact: Nina Bednarsek (NOAA) \n Version: 03 Feb 2014 |
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 | 2014-02-03T21:24:03Z |
attribute | NC_GLOBAL | date_modified | String | 2019-11-21T17:45:15Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.489471.1 |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/489471 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Bongo Net |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Specimens were collected by vertically integrating the upper 200 m using a vertical Bongo (mesh size 200 um with an opening of 0.5 m2) and a towed Bongo net (2 nets, with 300 um and 600 um mesh sizes). |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 489534 |
attribute | NC_GLOBAL | instruments_0_description | String | A Bongo Net consists of paired plankton nets, typically with a 60 cm diameter mouth opening and varying mesh sizes, 10 to 1000 micron. The Bongo Frame was designed by the National Marine Fisheries Service for use in the MARMAP program. It consists of two cylindrical collars connected with a yoke so that replicate samples are collected at the same time. Variations in models are designed for either vertical hauls (OI-2500 = NMFS Pairovet-Style, MARMAP Bongo, CalVET) or both oblique and vertical hauls (Aquatic Research). The OI-1200 has an opening and closing mechanism that allows discrete \"known-depth\" sampling. This model is large enough to filter water at the rate of 47.5 m3/minute when towing at a speed of two knots. More information: Ocean Instruments, Aquatic Research, Sea-Gear |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/NETT0009/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Bongo Net |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 410 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Bongo Net |
attribute | NC_GLOBAL | instruments_1_acronym | String | MOCNESS |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | Pteropods were collected using a combination of vertically and obliquely towed Bongo nets and MOCNESS nets |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 489535 |
attribute | NC_GLOBAL | instruments_1_description | String | The Multiple Opening/Closing Net and Environmental Sensing System or MOCNESS is a family of net systems based on the Tucker Trawl principle. There are currently 8 different sizes of MOCNESS in existence which are designed for capture of different size ranges of zooplankton and micro-nekton Each system is designated according to the size of the net mouth opening and in two cases, the number of nets it carries. The original MOCNESS (Wiebe et al, 1976) was a redesigned and improved version of a system described by Frost and McCrone (1974).(from MOCNESS manual) This designation is used when the specific type of MOCNESS (number and size of nets) was not specified by the contributing investigator. |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/NETT0097/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | MOCNESS |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 511 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | MOCNESS |
attribute | NC_GLOBAL | instruments_2_acronym | String | inorganic carbon and alkalinity analyser |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | DIC and TA were measured using VINDTA instrument (Versatile INstrument for the Determination of Titration Alkalinity, Marianda, Kiel, Germany) following the Standard Operating Procedures for oceanic CO2 measurements (Dickson et al. 2007). |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 489536 |
attribute | NC_GLOBAL | instruments_2_description | String | The Versatile INstrument for the Determination of Total inorganic carbon and titration Alkalinity (VINDTA) 3C is a laboratory alkalinity titration system combined with an extraction unit for coulometric titration, which simultaneously determines the alkalinity and dissolved inorganic carbon content of a sample. The sample transport is performed with peristaltic pumps and acid is added to the sample using a membrane pump. No pressurizing system is required and only one gas supply (nitrogen or dry and CO2-free air) is necessary. The system uses a Metrohm Titrino 719S, an ORION-Ross pH electrode and a Metrohm reference electrode. The burette, the pipette and the analysis cell have a water jacket around them. Precision is typically +/- 1 umol/kg for TA and/or DIC in open ocean water. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L22/current/TOOL0481/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | MARIANDA VINDTA 3C total inorganic carbon and titration alkalinity analyser |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 686 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | inorganic carbon and alkalinity analyser |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_description | String | SEM was done using a JEOL JSM 5900LV fitted with a tungsten filament at an acceleration voltage of 15 kV and a working distance of about 10 mm. |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 489537 |
attribute | NC_GLOBAL | instruments_3_description | String | Instruments that generate enlarged images of samples using the phenomena of reflection and absorption of electrons behaving as waves. |
attribute | NC_GLOBAL | instruments_3_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB07/ |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Microscope-Electron |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 709 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | Scanning Electron Microscope |
attribute | NC_GLOBAL | keywords | String | alk, alk_tot, alk_tot_stdev, altimetry, arg, bco, bco-dmo, bicarbonate, bicarbonate_stdev, biological, carbon, carbon dioxide, carbonate, carbonate_stdev, chemical, chemistry, co2, co3, concentration, data, dataset, deviation, dic, DIC_stdev, dioxide, diss, diss_rate1, diss_rate1_stdev, diss_rate2, diss_rate2_stdev, diss_rate3, diss_rate3_stdev, dmo, earth, Earth Science > Oceans > Ocean Chemistry > pH, Earth Science > Oceans > Ocean Chemistry > Phosphate, Earth Science > Oceans > Ocean Chemistry > Silicate, erddap, incubation, incubation_time, laboratory, management, mass, mass_concentration_of_phosphate_in_sea_water, mass_concentration_of_silicate_in_sea_water, non, non_diss, non_diss_stdev, ocean, oceanography, oceans, office, omega, omega_Arg, omega_Arg_stdev, pCO2, pCO2_stdev, pH_stdev, phosphate, po4, preliminary, rate1, rate2, rate3, reported, sal, satellite, scale, science, sea, sea_water_ph_reported_on_total_scale, seawater, silicate, species, standard, standard deviation, stdev, temperature, time, tot, total, treatment, water |
attribute | NC_GLOBAL | keywords_vocabulary | String | GCMD Science Keywords |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/489471/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/489471 |
attribute | NC_GLOBAL | param_mapping | String | {'489471': {}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/489471/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | British Antarctic Survey |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | BAS |
attribute | NC_GLOBAL | people_0_person_name | String | Geraint Tarling |
attribute | NC_GLOBAL | people_0_person_nid | String | 489466 |
attribute | NC_GLOBAL | people_0_role | String | Lead Principal Investigator |
attribute | NC_GLOBAL | people_0_role_type | String | originator |
attribute | NC_GLOBAL | people_1_affiliation | String | University of East Anglia |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | UEA |
attribute | NC_GLOBAL | people_1_person_name | String | Dorothee C.E. Bakker |
attribute | NC_GLOBAL | people_1_person_nid | String | 50929 |
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 | British Antarctic Survey |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | BAS |
attribute | NC_GLOBAL | people_2_person_name | String | Sophie Fielding |
attribute | NC_GLOBAL | people_2_person_nid | String | 489467 |
attribute | NC_GLOBAL | people_2_role | String | Co-Principal Investigator |
attribute | NC_GLOBAL | people_2_role_type | String | originator |
attribute | NC_GLOBAL | people_3_affiliation | String | National Oceanic and Atmospheric Administration |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | NOAA-PMEL |
attribute | NC_GLOBAL | people_3_person_name | String | Nina Bednarsek |
attribute | NC_GLOBAL | people_3_person_nid | String | 489468 |
attribute | NC_GLOBAL | people_3_role | String | Contact |
attribute | NC_GLOBAL | people_3_role_type | String | related |
attribute | NC_GLOBAL | people_4_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_4_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_4_person_name | String | Shannon Rauch |
attribute | NC_GLOBAL | people_4_person_nid | String | 51498 |
attribute | NC_GLOBAL | people_4_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_4_role_type | String | related |
attribute | NC_GLOBAL | project | String | OA Nutrition and Coral Calcification |
attribute | NC_GLOBAL | projects_0_acronym | String | OA Nutrition and Coral Calcification |
attribute | NC_GLOBAL | projects_0_description | String | The project description is a modification of the original NSF award abstract.\nThis research project is part of the larger NSF funded CRI-OA collaborative research initiative and was funded as an Ocean Acidification-Category 1, 2010 award. Over the course of this century, all tropical coral reef ecosystems, whether fringing heavily populated coastlines or lining remote islands and atolls, face unprecedented threat from ocean acidification caused by rising levels of atmospheric CO2. In many laboratory experiments conducted to date, calcium carbonate production (calcification) by scleractinian (stony) corals showed an inverse correlation to seawater saturation state OMEGAar), whether OMEGAar was manipulated by acid or CO2 addition. Based on these data, it is predicted that coral calcification rates could decline by up to 80% of modern values by the end of this century. A growing body of new experimental data however, suggests that the coral calcification response to ocean acidification may be less straightforward and a lot more variable than previously recognized. In at least 10 recent experiments including our own, 8 different tropical and temperate species reared under nutritionally-replete but significantly elevated CO2 conditions (780-1200 ppm, OMEAGar ~1.5-2), continued to calcify at rates comparable to conspecifics reared under ambient CO2. These experimental results are consistent with initial field data collected on reefs in the eastern Pacific and southern Oman, where corals today live and accrete their skeletons under conditions equivalent to 2X and 3X pre-industrial CO2. On these high CO2, high nutrient reefs (where nitrate concentrations typically exceed 2.5 micro-molar), coral growth rates rival, and sometimes even exceed, those of conspecifics in low CO2, oligotrophic reef environments.\nThe investigators propose that a coral's energetic status, tightly coupled to the availability of inorganic nutrients and/or food, is a key factor in the calcification response to CO2-induced ocean acidification. Their hypothesis, if confirmed by the proposed laboratory investigations, implies that predicted changes in coastal and open ocean nutrient concentrations over the course of this century, driven by both climate impacts on ocean stratification and by increased human activity in coastal regions, could play a critical role in exacerbating and in some areas, modulating the coral reef response to ocean acidification. This research program builds on the investigators initial results and observations. The planned laboratory experiments will test the hypothesis that: (1) The coral calcification response to ocean acidification is linked to the energetic status of the coral host. The relative contribution of symbiont photosynthesis and heterotrophic feeding to a coral's energetic status varies amongst species. Enhancing the energetic status of corals reared under high CO2, either by stimulating photosynthesis with inorganic nutrients or by direct heterotrophic feeding of the host lowers the sensitivity of calcification to decreased seawater OMEGAar; (2) A species-specific threshold CO2 level exists over which enhanced energetic status can no longer compensate for decreased OMEGAar of the external seawater. Similarly, we will test the hypothesis that a nutrient threshold exists over which nutrients become detrimental for calcification even under high CO2 conditions; and (3) Temperature-induced reduction of algal symbionts is one stressor that can reduce the energetic reserve of the coral host and exacerbate the calcification response to ocean acidification.\nThe investigator's initial findings highlight the critical importance of energetic status in the coral calcification response to ocean acidification. Verification of these findings in the laboratory, and identification of nutrient and CO2 thresholds for a range of species will have immediate, direct impact on predictions of reef resilience in a high CO2 world. The research project brings together a diverse group of expertise in coral biogeochemistry, chemical oceanography, molecular biology and coral reproductive ecology to focus on a problem that has enormous societal, economic and conservation relevance. |
attribute | NC_GLOBAL | projects_0_end_date | String | 2013-09 |
attribute | NC_GLOBAL | projects_0_geolocation | String | global; experimental |
attribute | NC_GLOBAL | projects_0_name | String | An Investigation of the Role of Nutrition in the Coral Calcification Response to Ocean Acidification |
attribute | NC_GLOBAL | projects_0_project_nid | String | 2183 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2010-10 |
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 | species |
attribute | NC_GLOBAL | summary | String | This dataset contains data from a study of pteropod shell dissolution on individuals exposed to CO2-enriched seawater. The data include the amount of dissolution as well as the physical and chemical parameters on which carbonate chemistry parameters were calculated. |
attribute | NC_GLOBAL | title | String | [pteropod shell dissolution] - Pteropod shell dissolution in natural and high-CO2 environments from samples collected on RRS James Clark Ross cruise JR177 in the Scotia Sea, Southern Ocean from 2007-2008 (An Investigation of the Role of Nutrition in the Coral Calcification Response to Ocean Acidification) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | treatment | String | ||
attribute | treatment | bcodmo_name | String | treatment |
attribute | treatment | description | String | Type of experimental treatment. |
attribute | treatment | long_name | String | Treatment |
attribute | treatment | units | String | dimensionless |
variable | incubation_time | byte | ||
attribute | incubation_time | _FillValue | byte | 127 |
attribute | incubation_time | actual_range | byte | 4, 14 |
attribute | incubation_time | bcodmo_name | String | incubation time |
attribute | incubation_time | description | String | Number of days incubated. |
attribute | incubation_time | long_name | String | Incubation Time |
attribute | incubation_time | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/AZDRZZ01/ |
attribute | incubation_time | units | String | days |
variable | N | byte | ||
attribute | N | _FillValue | byte | 127 |
attribute | N | actual_range | byte | 9, 11 |
attribute | N | bcodmo_name | String | number |
attribute | N | description | String | Number of samples in the treatment. |
attribute | N | long_name | String | N |
attribute | N | units | String | dimensionless |
variable | species | String | ||
attribute | species | bcodmo_name | String | species |
attribute | species | description | String | Name of the species of study. |
attribute | species | long_name | String | Species |
attribute | species | units | String | dimensionless |
variable | sal | float | ||
attribute | sal | _FillValue | float | NaN |
attribute | sal | actual_range | float | 33.82, 33.86 |
attribute | sal | bcodmo_name | String | sal |
attribute | sal | description | String | Salinity. |
attribute | sal | long_name | String | Sal |
attribute | sal | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PSALST01/ |
attribute | sal | units | String | dimensionless |
variable | temp | byte | ||
attribute | temp | _FillValue | byte | 127 |
attribute | temp | actual_range | byte | 3, 4 |
attribute | temp | bcodmo_name | String | temperature |
attribute | temp | description | String | Water temperature. |
attribute | temp | long_name | String | Temperature |
attribute | temp | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/TEMPP901/ |
attribute | temp | units | String | degrees Celsius |
variable | phosphate | float | ||
attribute | phosphate | _FillValue | float | NaN |
attribute | phosphate | actual_range | float | 1.15, 1.8 |
attribute | phosphate | bcodmo_name | String | unknown |
attribute | phosphate | description | String | Phosphate concentration. |
attribute | phosphate | long_name | String | Mass Concentration Of Phosphate In Sea Water |
attribute | phosphate | units | String | micromoles per kilogram (umol/kg) |
variable | silicate | float | ||
attribute | silicate | _FillValue | float | NaN |
attribute | silicate | actual_range | float | 8.0, 12.5 |
attribute | silicate | bcodmo_name | String | SiOH_4 |
attribute | silicate | description | String | Silicate concentration. |
attribute | silicate | long_name | String | Mass Concentration Of Silicate In Sea Water |
attribute | silicate | units | String | micromoles per kilogram (umol/kg) |
variable | alk_tot | float | ||
attribute | alk_tot | _FillValue | float | NaN |
attribute | alk_tot | actual_range | float | 2290.6, 2360.3 |
attribute | alk_tot | bcodmo_name | String | TALK |
attribute | alk_tot | description | String | Total alkalinity. |
attribute | alk_tot | long_name | String | Alk Tot |
attribute | alk_tot | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/MDMAP014/ |
attribute | alk_tot | units | String | micromoles per kilogram (umol/kg) |
variable | alk_tot_stdev | float | ||
attribute | alk_tot_stdev | _FillValue | float | NaN |
attribute | alk_tot_stdev | actual_range | float | 1.3, 8.9 |
attribute | alk_tot_stdev | bcodmo_name | String | standard deviation |
attribute | alk_tot_stdev | description | String | Standard deviation of alk_tot. |
attribute | alk_tot_stdev | long_name | String | Alk Tot Stdev |
attribute | alk_tot_stdev | units | String | micromoles per kilogram (umol/kg) |
variable | DIC | float | ||
attribute | DIC | _FillValue | float | NaN |
attribute | DIC | actual_range | float | 2123.0, 2298.3 |
attribute | DIC | bcodmo_name | String | DIC |
attribute | DIC | description | String | Total dissolved inorganic carbon. |
attribute | DIC | long_name | String | DIC |
attribute | DIC | units | String | micromoles per kilogram (umol/kg) |
variable | DIC_stdev | float | ||
attribute | DIC_stdev | _FillValue | float | NaN |
attribute | DIC_stdev | actual_range | float | 0.0, 61.9 |
attribute | DIC_stdev | bcodmo_name | String | standard deviation |
attribute | DIC_stdev | description | String | Standard deviation of C_tot. |
attribute | DIC_stdev | long_name | String | DIC Stdev |
attribute | DIC_stdev | units | String | micromoles per kilogram (umol/kg) |
variable | pH | float | ||
attribute | pH | _FillValue | float | NaN |
attribute | pH | actual_range | float | 7.7, 8.13 |
attribute | pH | bcodmo_name | String | pH |
attribute | pH | colorBarMaximum | double | 9.0 |
attribute | pH | colorBarMinimum | double | 7.0 |
attribute | pH | description | String | pH of the water. |
attribute | pH | long_name | String | Sea Water Ph Reported On Total Scale |
attribute | pH | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PHXXZZXX/ |
attribute | pH | units | String | dimensionless |
variable | pH_stdev | float | ||
attribute | pH_stdev | _FillValue | float | NaN |
attribute | pH_stdev | actual_range | float | 0.01, 0.13 |
attribute | pH_stdev | bcodmo_name | String | standard deviation |
attribute | pH_stdev | description | String | Standard deviation of pH. |
attribute | pH_stdev | long_name | String | P H Stdev |
attribute | pH_stdev | units | String | dimensionless |
variable | pCO2 | short | ||
attribute | pCO2 | _FillValue | short | 32767 |
attribute | pCO2 | actual_range | short | 318, 940 |
attribute | pCO2 | bcodmo_name | String | pCO2 |
attribute | pCO2 | description | String | Partial pressure of carbon dioxide at sea surface temperature. |
attribute | pCO2 | long_name | String | P CO2 |
attribute | pCO2 | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PCO2C101/ |
attribute | pCO2 | units | String | microatmospheres (uatm) |
variable | pCO2_stdev | byte | ||
attribute | pCO2_stdev | _FillValue | byte | 127 |
attribute | pCO2_stdev | actual_range | byte | 12, 111 |
attribute | pCO2_stdev | bcodmo_name | String | standard deviation |
attribute | pCO2_stdev | description | String | Standard deviation of pCO2. |
attribute | pCO2_stdev | long_name | String | P CO2 Stdev |
attribute | pCO2_stdev | units | String | microatmospheres (uatm) |
variable | bicarbonate | float | ||
attribute | bicarbonate | _FillValue | float | NaN |
attribute | bicarbonate | actual_range | float | 1983.1, 2192.7 |
attribute | bicarbonate | bcodmo_name | String | bicarbonate |
attribute | bicarbonate | description | String | Concentration of bicarbonate ion [HCO3]-. |
attribute | bicarbonate | long_name | String | Bicarbonate |
attribute | bicarbonate | units | String | micromoles per kilogram (umol/kg) |
variable | bicarbonate_stdev | float | ||
attribute | bicarbonate_stdev | _FillValue | float | NaN |
attribute | bicarbonate_stdev | actual_range | float | 4.4, 91.9 |
attribute | bicarbonate_stdev | bcodmo_name | String | standard deviation |
attribute | bicarbonate_stdev | description | String | Standard deviation of bicarbonate concentration. |
attribute | bicarbonate_stdev | long_name | String | Bicarbonate Stdev |
attribute | bicarbonate_stdev | units | String | micromoles per kilogram (umol/kg) |
variable | carbonate | float | ||
attribute | carbonate | _FillValue | float | NaN |
attribute | carbonate | actual_range | float | 51.6, 121.6 |
attribute | carbonate | bcodmo_name | String | carbonate |
attribute | carbonate | description | String | Concentration of carbonate ion [CO3]2-. |
attribute | carbonate | long_name | String | Carbonate |
attribute | carbonate | units | String | micromoles per kilogram (umol/kg) |
variable | carbonate_stdev | float | ||
attribute | carbonate_stdev | _FillValue | float | NaN |
attribute | carbonate_stdev | actual_range | float | 0.9, 39.6 |
attribute | carbonate_stdev | bcodmo_name | String | standard deviation |
attribute | carbonate_stdev | description | String | Standard deviation of carbonate concentration. |
attribute | carbonate_stdev | long_name | String | Carbonate Stdev |
attribute | carbonate_stdev | units | String | micromoles per kilogram (umol/kg) |
variable | omega_Arg | float | ||
attribute | omega_Arg | _FillValue | float | NaN |
attribute | omega_Arg | actual_range | float | 0.78, 1.82 |
attribute | omega_Arg | bcodmo_name | String | OM_ar |
attribute | omega_Arg | description | String | Aragonite saturation state. |
attribute | omega_Arg | long_name | String | Omega Arg |
attribute | omega_Arg | units | String | dimensionless |
variable | omega_Arg_stdev | float | ||
attribute | omega_Arg_stdev | _FillValue | float | NaN |
attribute | omega_Arg_stdev | actual_range | float | 0.02, 0.6 |
attribute | omega_Arg_stdev | bcodmo_name | String | standard deviation |
attribute | omega_Arg_stdev | description | String | Standard deviation of omega_Arg. |
attribute | omega_Arg_stdev | long_name | String | Omega Arg Stdev |
attribute | omega_Arg_stdev | units | String | dimensionless |
variable | non_diss | float | ||
attribute | non_diss | _FillValue | float | NaN |
attribute | non_diss | actual_range | float | 0.04, 0.997 |
attribute | non_diss | bcodmo_name | String | unknown |
attribute | non_diss | description | String | Percentage of non-dissolving individuals as determined by SEM. |
attribute | non_diss | long_name | String | Non Diss |
attribute | non_diss | units | String | percentage (%) |
variable | non_diss_stdev | float | ||
attribute | non_diss_stdev | _FillValue | float | NaN |
attribute | non_diss_stdev | actual_range | float | 0.005, 0.15 |
attribute | non_diss_stdev | bcodmo_name | String | standard deviation |
attribute | non_diss_stdev | description | String | Standard deviation of non_diss. |
attribute | non_diss_stdev | long_name | String | Non Diss Stdev |
attribute | non_diss_stdev | units | String | percentage (%) |
variable | diss_rate1 | float | ||
attribute | diss_rate1 | _FillValue | float | NaN |
attribute | diss_rate1 | actual_range | float | 0.002, 0.8 |
attribute | diss_rate1 | bcodmo_name | String | unknown |
attribute | diss_rate1 | description | String | Type I dissolution rate as determined by SEM. Bednarsek et al. (2012) describe Type I dissolution as \"First indices of slightly increased porosity. Aragonite crystals within the upper-prismatic layer affected by dissolution - ‘cauliflower heads’ present.\" |
attribute | diss_rate1 | long_name | String | Diss Rate1 |
attribute | diss_rate1 | units | String | percentage (%) |
variable | diss_rate1_stdev | float | ||
attribute | diss_rate1_stdev | _FillValue | float | NaN |
attribute | diss_rate1_stdev | actual_range | float | 0.003, 0.15 |
attribute | diss_rate1_stdev | bcodmo_name | String | standard deviation |
attribute | diss_rate1_stdev | description | String | Standard deviation of diss_rate1. |
attribute | diss_rate1_stdev | long_name | String | Diss Rate1 Stdev |
attribute | diss_rate1_stdev | units | String | percentage (%) |
variable | diss_rate2 | float | ||
attribute | diss_rate2 | _FillValue | float | NaN |
attribute | diss_rate2 | actual_range | float | 0.0, 0.26 |
attribute | diss_rate2 | bcodmo_name | String | unknown |
attribute | diss_rate2 | description | String | Type II dissolution rate as determined by SEM. Bednarsek et al. (2012) describe Type II dissolution as \"Increased porosity. Dissolved patches more extensive and numerous. Prismatic layer partially or completely dissolved, crossed-lamellar layer exposed.\" |
attribute | diss_rate2 | long_name | String | Diss Rate2 |
attribute | diss_rate2 | units | String | percentage (%) |
variable | diss_rate2_stdev | float | ||
attribute | diss_rate2_stdev | _FillValue | float | NaN |
attribute | diss_rate2_stdev | actual_range | float | 0.0, 0.1 |
attribute | diss_rate2_stdev | bcodmo_name | String | standard deviation |
attribute | diss_rate2_stdev | description | String | Standard deviation of diss_rate2. |
attribute | diss_rate2_stdev | long_name | String | Diss Rate2 Stdev |
attribute | diss_rate2_stdev | units | String | percentage (%) |
variable | diss_rate3 | float | ||
attribute | diss_rate3 | _FillValue | float | NaN |
attribute | diss_rate3 | actual_range | float | 0.0, 0.31 |
attribute | diss_rate3 | bcodmo_name | String | unknown |
attribute | diss_rate3 | description | String | Type III dissolution rate as determined by SEM. Bednarsek et al. (2012) describe Type III dissolution as \"Less compact crystal structure with compromised shell integrity and extreme frailness. Dissolution within crossed-lamellar layer with crystals thicker and chunkier.\" |
attribute | diss_rate3 | long_name | String | Diss Rate3 |
attribute | diss_rate3 | units | String | percentage (%) |
variable | diss_rate3_stdev | float | ||
attribute | diss_rate3_stdev | _FillValue | float | NaN |
attribute | diss_rate3_stdev | actual_range | float | 0.0, 0.06 |
attribute | diss_rate3_stdev | bcodmo_name | String | standard deviation |
attribute | diss_rate3_stdev | description | String | Standard deviation of diss_rate3. |
attribute | diss_rate3_stdev | long_name | String | Diss Rate3 Stdev |
attribute | diss_rate3_stdev | units | String | percentage (%) |