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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 | TOC measurements:\n \nThe procedures used to set up each experiment (inoculum filtration and\ndilution with 0.2 um filtrate) removed the majority of particulate organic\ncarbon such that changes in bacterioplankton carbon production and DOC removal\nwere mainly a function of the growth of the inoculum. Ideally, samples\ncollected for organic carbon would be filtered in order to directly assess DOC\nremoval separate from bacterioplankton carbon production over the course of\nthe incubations. However, sample handling during filtration can result in\ncontamination that obscures changes in DOC on the scale of a few micro-molar\nC. To avoid contamination, seawater samples from the incubation experiments\nwere not filtered. Therefore, measured values of organic carbon include both\nDOC and bacterioplankton carbon and are considered total organic carbon (TOC).\n \nTOC samples were collected into 60 mL high-density polyethylene bottles\n(Sargasso Sea and South Pacific Subtropical Gyre) or in combusted 40 mL glass\nEPA vials with Teflon coated silicone septa (Santa Barbara Channel). All TOC\nsamples were frozen at -20 C until analysis. Samples were analyzed via high\ntemperature combustion method on a modified Shimadzu TOC-V or Shimadzu TOC-L\nusing the standardization and referencing approaches described in Carlson et\nal. 2010.\n \nBacterioplankton abundance measurement \\u2013 Samples for bacterioplankton\nabundance were analyzed by epifluorescence microscopy with 0, 6-diamidino\n-2-phenyl dihydrochloride (5ug/mL, DAPI, SIGMA-Aldrich, St. Louis, MO, USA)\naccording to Porter and Feig 1980, or by Flow Cytometry (FCM) on an LSR II\nwith SYBR Green I according to Nelson et al. 2011. See Parsons et al. 2014 and\nNelson et al. 2011 regarding sample preparation and instrument settings for\nepifluorescence microscopy and FCM analyses, respectively. DAPI direct counts\nand FCM analysis enumerate total prokaryotic abundance. We were not able to\ndifferentiate between bacterial and archaeal domains and refer to the combined\ncell densities as bacterioplankton abundance (Glockner et al. 1999).\n \nWater sources:\n \nExperiment OA11 was conducted on board a research cruise R/V Kilo Moana\nKM1416. The Sargasso Sea experiments were conducted at the Bermuda Institute\nfor Ocean Sciences (BIOS) with water was collected via the R/V Atlantic\nExplorer. The Santa Barbara Channel experiments were conducted with water\ncollected near-shore via a pier near the UCSB campus.\n \nExperimental design:\n \nAt all three study sites, experiments consisted of 0.2 um-filtered (0.2 um\nGSWP, Millipore, Billerica, MA) seawater or 0.2 um-filtered phytoplankton\nexudate that was inoculated with natural bacterial communities. The inoculum\nof natural bacterial communities consisted of either unfiltered whole seawater\n(Sargasso Sea and South Pacific Subtropical Gyre experiments) or 1.2 um\nfiltrate (Santa Barbara Channel experiments; 1.2 um RAWP, Millipore,\nBillerica, MA). Particulate organic carbon concentration in oligotrophic gyres\nis low (1-3 umol L-1) so to avoid filtration artifacts such as reduced\nbacterial production (unpublished data) and contamination of DOC due to\nhandling, the inoculum was not pre-filtered for the experiments conducted in\noligotrophic waters. Because particulate organic carbon concentration can be\nmuch greater in coastal upwelling systems it was necessary to remove large\nparticles and organisms from the inoculum. Inoculum was added at 25 \\u2013 30%\nof final volume, effectively diluting grazer concentrations and grazing\npressure. All filters were pre-rinsed with ~2 L of deionized distilled water\nand sample water prior to use in order to remove organic contaminants from the\nfilters.\n \nFour types of DOC treatments were used and are described in the data as\n\\\"doc_additions\\\":\n \n1\\. None: unamended seawater, which provided naturally occurring DOC. \n 2. CNP: Naturally occurring DOC amended with glucose (~10 uM C) plus NH4 Cl\n(1uM) and K2HPO4 (0.1uM) (CNP) \n 3. Species name + \\\" exudate\\\": phytoplankton exudate \n 4. Species name + \\\" lysate\\\": naturally occurring DOC amended with\nphytoplankton lysate (~10 uM C L-1; labeled by phytoplankton species used).\n \nThe various treatments were generated by inoculating the 0.2 um pre-filtered\nseawater or exudate with the microbial community; this solution was then\ndivided into two polycarbonate (PC) containers to adjust\\u00a0pCO2.\\u00a0pCO2\nlevels were adjusted via chemical additions (Sargasso Sea experiment) or by\nbubbling with CO2-mixed air (Santa Barbara Channel and South Pacific\nSubtropical Gyre experiments). Adjusted seawater incubations were then\ntransferred into new PC carboys and CNP or lysate was added, if appropriate. A\nvery small volume of lysate (1.2 mL to 11.5 L of experimental volume) or CNP\n(12 mL to 10 L of experimental water for the Sargasso Sea experiment; 0.28 mL\nto 10 L of experimental volume for the Santa Barbara Channel experiment) was\nadded to minimize perturbing the carbonate chemistry. All experiments were\nconducted in duplicate, at in situ temperatures, and in the dark to eliminate\nphotoautotrophic production. All PC bottles had been acid-washed (5 % or 10 %\nHCL) and rinsed with deionized distilled water and sample water before use. \n \\u00a0 |
attribute | NC_GLOBAL | awards_0_award_nid | String | 55209 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1041038 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward?AWD_ID=1041038&HistoricalAwards=false |
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 | Donald L. Rice |
attribute | NC_GLOBAL | awards_0_program_manager_nid | String | 51467 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Bacterial use of DOC as a function of pCO2 \n Uta Passow, PI \n version 28 Nov 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 | 2013-11-25T16:22:02Z |
attribute | NC_GLOBAL | date_modified | String | 2019-09-04T18:22:42Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.665253 |
attribute | NC_GLOBAL | Easternmost_Easting | double | -64.6353 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 34.4216 |
attribute | NC_GLOBAL | geospatial_lat_min | double | -17.4502 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | -64.6353 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -149.8727 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/472032 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | Shimadzu TOC-V |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Samples were analyzed via high-temperature combustion method on a modified Shimadzu TOC-V or Shimadzu TOC-L using the standardization and referencing approaches described in Carlson et al. 2010. |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 665756 |
attribute | NC_GLOBAL | instruments_0_description | String | A Shimadzu TOC-V Analyzer measures DOC by high temperature combustion method. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | http://onto.nerc.ac.uk/CAST/124 |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | Shimadzu TOC-V Analyzer |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 603 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | modified Shimadzu TOC-L |
attribute | NC_GLOBAL | instruments_1_acronym | String | Flow Cytometer |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | Flow Cytometry (FCM) on an LSR II with SYBR Green I according to Nelson et al. 2011. |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 665758 |
attribute | NC_GLOBAL | instruments_1_description | String | Flow cytometers (FC or FCM) are automated instruments that quantitate properties of single cells, one cell at a time. They can measure cell size, cell granularity, the amounts of cell components such as total DNA, newly synthesized DNA, gene expression as the amount messenger RNA for a particular gene, amounts of specific surface receptors, amounts of intracellular proteins, or transient signalling events in living cells.\n(from: http://www.bio.umass.edu/micro/immunology/facs542/facswhat.htm) |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB37/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Flow Cytometer |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 660 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Flow Cytometry (FCM) |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | Samples for bacterioplankton abundance were analyzed by epifluorescence microscopy with 0, 6-diamidino -2-phenyl dihydrochloride (5µg mL-1, DAPI, SIGMA-Aldrich, St. Louis, MO, USA) according to Porter and Feig 1980. |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 665757 |
attribute | NC_GLOBAL | instruments_2_description | String | Instruments that generate enlarged images of samples using the phenomena of fluorescence and phosphorescence instead of, or in addition to, reflection and absorption of visible light. Includes conventional and inverted instruments. |
attribute | NC_GLOBAL | instruments_2_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB06/ |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | Microscope-Fluorescence |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 695 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | Epifluorescence microscopy |
attribute | NC_GLOBAL | instruments_3_acronym | String | Shimadzu TOC-L |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_description | String | Samples were analyzed via high-temperature combustion method on a modified Shimadzu TOC-V or Shimadzu TOC-L using the standardization and referencing approaches described in Carlson et al. 2010. |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 665755 |
attribute | NC_GLOBAL | instruments_3_description | String | A Shimadzu TOC-L Analyzer measures DOC by high temperature combustion method.\n\nDeveloped by Shimadzu, the 680 degree C combustion catalytic oxidation method is now used worldwide. One of its most important features is the capacity to efficiently oxidize hard-to-decompose organic compounds, including insoluble and macromolecular organic compounds. The 680 degree C combustion catalytic oxidation method has been adopted for the TOC-L series.\n\nhttp://www.shimadzu.com/an/toc/lab/toc-l2.html |
attribute | NC_GLOBAL | instruments_3_instrument_external_identifier | String | http://onto.nerc.ac.uk/CAST/124.html |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Shimadzu TOC-L Analyzer |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 527277 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | modified Shimazdu TOC-L |
attribute | NC_GLOBAL | keywords | String | abun, addition, average, bact, bact_abun_x10e6_avg, bact_abun_x10e6_stderr, bact_abun_x10e6_stdev, bco, bco-dmo, biological, bottle, bottle_number, carbon, carbon dioxide, chemical, co2, commerce, data, dataset, date, days, department, deviation, dioxide, dmo, doc, doc_addition, erddap, experiment, latitude, longitude, management, number, oceanography, office, point, preliminary, site, standard, standard deviation, stderr, stdev, target, target_pCO2, time, time_days, time_point, toc, toc_avg, toc_stderr, toc_stdev, x10e6 |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/472032/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/472032 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 34.4216 |
attribute | NC_GLOBAL | param_mapping | String | {'472032': {'latitude': 'flag - latitude', 'longitude': 'flag - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/472032/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | University of California-Santa Barbara |
attribute | NC_GLOBAL | people_0_affiliation_acronym | String | UCSB-MSI |
attribute | NC_GLOBAL | people_0_person_name | String | Dr Uta Passow |
attribute | NC_GLOBAL | people_0_person_nid | String | 51317 |
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 Barbara |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | UCSB-MSI |
attribute | NC_GLOBAL | people_1_person_name | String | Mark A. Brzezinski |
attribute | NC_GLOBAL | people_1_person_nid | String | 50663 |
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 California-Santa Barbara |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | UCSB-MSI |
attribute | NC_GLOBAL | people_2_person_name | String | Craig Carlson |
attribute | NC_GLOBAL | people_2_person_nid | String | 50575 |
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 | University of California-Santa Barbara |
attribute | NC_GLOBAL | people_3_affiliation_acronym | String | UCSB-MSI |
attribute | NC_GLOBAL | people_3_person_name | String | Ms Anna James |
attribute | NC_GLOBAL | people_3_person_nid | String | 471722 |
attribute | NC_GLOBAL | people_3_role | String | Student |
attribute | NC_GLOBAL | people_3_role_type | String | related |
attribute | NC_GLOBAL | people_4_affiliation | String | University of California-Santa Barbara |
attribute | NC_GLOBAL | people_4_affiliation_acronym | String | UCSB-MSI |
attribute | NC_GLOBAL | people_4_person_name | String | Dr Uta Passow |
attribute | NC_GLOBAL | people_4_person_nid | String | 51317 |
attribute | NC_GLOBAL | people_4_role | String | Contact |
attribute | NC_GLOBAL | people_4_role_type | String | related |
attribute | NC_GLOBAL | people_5_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_5_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_5_person_name | String | Stephen R. Gegg |
attribute | NC_GLOBAL | people_5_person_nid | String | 50910 |
attribute | NC_GLOBAL | people_5_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_5_role_type | String | related |
attribute | NC_GLOBAL | people_6_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_6_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_6_person_name | String | Amber York |
attribute | NC_GLOBAL | people_6_person_nid | String | 643627 |
attribute | NC_GLOBAL | people_6_role | String | BCO-DMO Data Manager |
attribute | NC_GLOBAL | people_6_role_type | String | related |
attribute | NC_GLOBAL | project | String | OA - Effects of High CO2 |
attribute | NC_GLOBAL | projects_0_acronym | String | OA - Effects of High CO2 |
attribute | NC_GLOBAL | projects_0_description | String | From the NSF Award Abstract\nCoastal waters are already experiencing episodic exposure to carbonate conditions that were not expected until the end of the century making understanding the response to these episodic events as important as understanding the long-term mean response. Among the most striking examples are those associated with coastal upwelling along the west coast of the US, where the pH of surface waters may drop to 7.6 and pCO2 can reach 1100 uatm. Upwelling systems are responsible for a significant fraction of global carbon export making them prime targets for investigations on how ocean acidification is already affecting the biological pump today.\nIn this study, researchers at the University of California at Santa Barbara will investigate the potential effects of ocean acidification on the strength of the biological pump under the transient increases in CO2 experienced due to upwelling. Increases in CO2 are expected to alter the path and processing of carbon through marine food webs thereby strengthening the biological pump. Increases in inorganic carbon without proportional increases in nutrients result in carbon over-consumption by phytoplankton. How carbon over-consumption affects the strength of the biological pump will depend on the fate of the extra carbon that is either incorporated into phytoplankton cells forming particulate organic matter (POM), or is excreted as dissolved organic matter (DOM). Results from mesocosm experiments demonstrate that the mechanisms controlling the partitioning of fixed carbon between the particulate and dissolved phases, and the processing of those materials, are obscured when both processes operate simultaneously under natural or semi-natural conditions. Here, POM and DOM production and the heterotrophic processing of these materials will be separated experimentally across a range of CO2 concentrations by conducting basic laboratory culture experiments. In this way the mechanisms whereby elevated CO2 alters the flow of carbon along these paths can be elucidated and better understood for use in mechanistic forecasting models.\nBroader Impacts- The need to understand the effects of ocean acidification for the future of society is clear. In addition to research education, both formal and informal, will be important for informing the public. Within this project 1-2 graduate students and 2-3 minority students will be recruited as interns from the CAMP program (California Alliance for Minority Participation). Within the 'Ocean to Classrooms' program run by outreach personnel from UCSB's Marine Science Institute an educational unit for K-12 students will be developed. Advice and support is also given to the Education Coordinator of NOAA, Channel Islands National Marine Sanctuary for the development of an education unit on ocean acidification.\n\nPUBLICATIONS PRODUCED AS A RESULT OF THIS RESEARCH\nArnosti C, Grossart H-P, Muehling M, Joint I, Passow U. \"Dynamics of extracellular enzyme activities in seawater under changed atmsopheric pCO2: A mesocosm investigation.,\" Aquatic Microbial Ecology, v.64, 2011, p. 285.\nPassow U. \"The Abiotic Formation of TEP under Ocean Acidification Scenarios.,\" Marine Chemistry, v.128-129, 2011, p. 72.\nPassow, Uta; Carlson, Craig A.. \"The biological pump in a high CO2 world,\" MARINE ECOLOGY PROGRESS SERIES, v.470, 2012, p. 249-271.\nGaerdes, Astrid; Ramaye, Yannic; Grossart, Hans-Peter; Passow, Uta; Ullrich, Matthias S.. \"Effects of Marinobacter adhaerens HP15 on polymer exudation by Thalassiosira weissflogii at different N:P ratios,\" MARINE ECOLOGY PROGRESS SERIES, v.461, 2012, p. 1-14.\nPhilip Boyd, Tatiana Rynearson, Evelyn Armstrong, Feixue Fu, Kendra Hayashi, Zhangi Hu, David Hutchins, Raphe Kudela, Elena Litchman, Margaret Mulholland, Uta Passow, Robert Strzepek, Kerry Whittaker, Elizabeth Yu, Mridul Thomas. \"Marine Phytoplankton Temperature versus Growth Responses from Polar to Tropical Waters - Outcome of a Scientific Community-Wide Study,\" PLOS One 8, v.8, 2013, p. e63091.\nArnosti, C., B. M. Fuchs, R. Amann, and U. Passow. \"Contrasting extracellular enzyme activities of particle-associated bacteria from distinct provinces of the North Atlantic Ocean,\" Frontiers in Microbiology, v.3, 2012, p. 1.\nKoch, B.P., Kattner, G., Witt, M., Passow, U., 2014. Molecular insights into the microbial formation of marine dissolved organic matter: recalcitrant or labile? Biogeosciences Discuss. 11 (2), 3065-3111.\nTaucher, J., Brzezinski, M., Carlson, C., James, A., Jones, J., Passow, U., Riebesell, U., submitted. Effects of warming and elevated pCO2 on carbon uptake and partitioning of the marine diatoms Thalassiosira weissflogii and Dactyliosolen fragilissimus. Limnology and Oceanography |
attribute | NC_GLOBAL | projects_0_end_date | String | 2014-09 |
attribute | NC_GLOBAL | projects_0_geolocation | String | Passow Lab, Marine Science Institute, University of California Santa Barbara |
attribute | NC_GLOBAL | projects_0_name | String | Will high CO2 conditions affect production, partitioning and fate of organic matter? |
attribute | NC_GLOBAL | projects_0_project_nid | String | 2284 |
attribute | NC_GLOBAL | projects_0_project_website | String | http://www.msi.ucsb.edu/people/research-scientists/uta-passow |
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 | Southernmost_Northing | double | -17.4502 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | summary | String | Factors that affect the removal of organic carbon by heterotrophic bacterioplankton can impact the rate and magnitude of organic carbon loss in the ocean through the conversion of a portion of consumed organic carbon to CO2. Through enhanced rates of consumption, surface bacterioplankton communities can also reduce the amount of dissolved organic carbon (DOC) available for export from the surface ocean. The present study investigated the direct effects of elevated pCO2 on bacterioplankton removal of several forms of DOC ranging from glucose to complex phytoplankton exudate and lysate, and naturally occurring DOC. Elevated pCO2 (1000 \\u2013 1500 ppm) enhanced both the rate and magnitude of organic carbon removal by bacterioplankton communities compared to low (pre-industrial and ambient) pCO2 (250 \\u2013 ~400 ppm). The increased removal was largely due to enhanced respiration, rather than enhanced production of bacterioplankton biomass. |
attribute | NC_GLOBAL | title | String | [Data Set 3A: Utilization of dissolved organic carbon by a natural bacterial community as a function of pCO2] - 3A: Removal of organic carbon by natural bacterioplankton communities as a function of pCO2 from laboratory experiments between 2012 and 2016 (Will high CO2 conditions affect production, partitioning and fate of organic matter?) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -149.8727 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | experiment | String | ||
attribute | experiment | bcodmo_name | String | exp_id |
attribute | experiment | description | String | Experiment identifier |
attribute | experiment | long_name | String | Experiment |
attribute | experiment | units | String | unitless |
variable | site | String | ||
attribute | site | bcodmo_name | String | site |
attribute | site | description | String | Site the water for the experiment came from |
attribute | site | long_name | String | Site |
attribute | site | units | String | unitless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | -17.4502, 34.4216 |
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 where water samples were collected; north is positive. |
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 | -149.8727, -64.6353 |
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 where water samples were collected; west is negative. |
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 | bottle_number | String | ||
attribute | bottle_number | bcodmo_name | String | bottle |
attribute | bottle_number | description | String | Bottle identifier |
attribute | bottle_number | long_name | String | Bottle Number |
attribute | bottle_number | units | String | unitless |
variable | doc_addition | String | ||
attribute | doc_addition | bcodmo_name | String | treatment |
attribute | doc_addition | description | String | Dissolved organic carbon additions. See Aquisition Description section for an explaination of values. |
attribute | doc_addition | long_name | String | Doc Addition |
attribute | doc_addition | units | String | unitless |
variable | target_pCO2 | short | ||
attribute | target_pCO2 | _FillValue | short | 32767 |
attribute | target_pCO2 | actual_range | short | 250, 1500 |
attribute | target_pCO2 | bcodmo_name | String | pCO2 |
attribute | target_pCO2 | description | String | Target pCO2 level |
attribute | target_pCO2 | long_name | String | Target P CO2 |
attribute | target_pCO2 | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/PCO2C101/ |
attribute | target_pCO2 | units | String | parts per million (ppm) |
variable | time_point | String | ||
attribute | time_point | bcodmo_name | String | time_point |
attribute | time_point | description | String | Time point identifier in experiment |
attribute | time_point | long_name | String | Time Point |
attribute | time_point | units | String | unitless |
variable | time_days | float | ||
attribute | time_days | _FillValue | float | NaN |
attribute | time_days | actual_range | float | 0.0, 17.05 |
attribute | time_days | bcodmo_name | String | time_elapsed |
attribute | time_days | description | String | Elapsed time since start of experiment in days |
attribute | time_days | long_name | String | Time Days |
attribute | time_days | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/ELTMZZZZ/ |
attribute | time_days | units | String | unitless |
variable | date | String | ||
attribute | date | bcodmo_name | String | date |
attribute | date | description | String | Date of experiment in format YYYY-MM-DD |
attribute | date | long_name | String | Date |
attribute | date | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/ADATAA01/ |
attribute | date | units | String | unitless |
variable | bact_abun_x10e6_avg | float | ||
attribute | bact_abun_x10e6_avg | _FillValue | float | NaN |
attribute | bact_abun_x10e6_avg | actual_range | float | 0.0, 4.86 |
attribute | bact_abun_x10e6_avg | bcodmo_name | String | bact_abundance |
attribute | bact_abun_x10e6_avg | description | String | Bacterial abundance multiplied by 10^6 |
attribute | bact_abun_x10e6_avg | long_name | String | Bact Abun X10e6 Avg |
attribute | bact_abun_x10e6_avg | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P02/current/BNTX |
attribute | bact_abun_x10e6_avg | units | String | cells per milliliter |
variable | bact_abun_x10e6_stderr | float | ||
attribute | bact_abun_x10e6_stderr | _FillValue | float | NaN |
attribute | bact_abun_x10e6_stderr | actual_range | float | 0.0, 1.16 |
attribute | bact_abun_x10e6_stderr | bcodmo_name | String | bact_abundance |
attribute | bact_abun_x10e6_stderr | colorBarMaximum | double | 50.0 |
attribute | bact_abun_x10e6_stderr | colorBarMinimum | double | 0.0 |
attribute | bact_abun_x10e6_stderr | description | String | Standard error of bacterial abundance multiplied by 10^6 |
attribute | bact_abun_x10e6_stderr | long_name | String | Bact Abun X10e6 Stderr |
attribute | bact_abun_x10e6_stderr | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P02/current/BNTX |
attribute | bact_abun_x10e6_stderr | units | String | cells per milliliter |
variable | bact_abun_x10e6_stdev | float | ||
attribute | bact_abun_x10e6_stdev | _FillValue | float | NaN |
attribute | bact_abun_x10e6_stdev | actual_range | float | 0.0, 1.64 |
attribute | bact_abun_x10e6_stdev | bcodmo_name | String | bact_abundance |
attribute | bact_abun_x10e6_stdev | description | String | Standard deviation Bacterial abundance multiplied by 10^6 |
attribute | bact_abun_x10e6_stdev | long_name | String | Bact Abun X10e6 Stdev |
attribute | bact_abun_x10e6_stdev | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P02/current/BNTX |
attribute | bact_abun_x10e6_stdev | units | String | cells per milliliter |
variable | toc_avg | float | ||
attribute | toc_avg | _FillValue | float | NaN |
attribute | toc_avg | actual_range | float | 63.84, 398.62 |
attribute | toc_avg | bcodmo_name | String | TOC |
attribute | toc_avg | description | String | Total organic carbon |
attribute | toc_avg | long_name | String | Toc Avg |
attribute | toc_avg | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/CORGCOTX/ |
attribute | toc_avg | units | String | micromoles per liter (uM) |
variable | toc_stderr | float | ||
attribute | toc_stderr | _FillValue | float | NaN |
attribute | toc_stderr | actual_range | float | 0.0, 14.2 |
attribute | toc_stderr | bcodmo_name | String | TOC |
attribute | toc_stderr | colorBarMaximum | double | 50.0 |
attribute | toc_stderr | colorBarMinimum | double | 0.0 |
attribute | toc_stderr | description | String | Standard error of total organic carbon |
attribute | toc_stderr | long_name | String | Toc Stderr |
attribute | toc_stderr | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/CORGCOTX/ |
attribute | toc_stderr | units | String | micromoles per liter (uM) |
variable | toc_stdev | float | ||
attribute | toc_stdev | _FillValue | float | NaN |
attribute | toc_stdev | actual_range | float | 0.0, 20.08 |
attribute | toc_stdev | bcodmo_name | String | TOC |
attribute | toc_stdev | description | String | Standard deviation of total organic carbon |
attribute | toc_stdev | long_name | String | Toc Stdev |
attribute | toc_stdev | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/CORGCOTX/ |
attribute | toc_stdev | units | String | micromoles per liter (uM) |