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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 | Tables and Figures referenced in the acquisition description are found in the\npaper Frank et al., 2015\n \nOnce on board ship,\\u00a0tubeworms\\u00a0and other macrofauna were removed from\nthe samples and the large pieces were broken into more manageable fragments\n(~10-20 cm3) with a flame-sterilized chisel and sledgehammer, with the user\nwearing sterile nitrile gloves. Samples were quickly transferred to 0.2 um-\nfiltered anaerobic (nitrogen-sparged) seawater. Samples were further broken\ndown into smaller sizes while in anaerobic water, and subsamples from the\ninterior of the fragments were immediately transferred to gastight jars\n(Freund Container Inc.) filled with sterile anaerobic seawater containing 2 mM\nsodium sulfide at pH 6, and stored at 4 degrees celsius for incubations and\nanalyses. The sterile sulfidic seawater in the gastight\njars\\u00a0were\\u00a0refreshed periodically during storage at 4 degrees\ncelsius. The majority of the rate experiments (80%) were set up immediately on\nthe ship using freshly collected samples. In parallel, subsamples (~1 cm3)\nfrom each flange were preserved aboard ship in glutaraldehyde (2.5% in\nphosphate buffered saline, PBS, pH 7.0), then prepared for electron microscopy\nvia ethanol dehydration and critical point drying before being sputtered with\na thin layer of gold-palladium to improve image resolution. Samples were\nimaged with a Zeiss model EVO Scanning Electron Microscope (SEM).\\u00a0\n \nPrior to incubation, each flange subsample was pulverized by hand for about\none hour to minimize fine-scale geological and microbial heterogeneity and\nfacilitate more accurate experimental replication (akin to slurry experiments\nin sediments; Fossing & J\\u00f8rgensen 1989; Weber & J\\u00f8rgensen 2002;\nJ\\u00f8rgensen\\u00a0et al.\\u00a01992). Specifically, each subsample was\npulverized with a flame-sterilized sledgehammer in sterile seawater actively\nbubbled with nitrogen within an anaerobic chamber. For each independent\ntreatment, aliquots of 7.5 mL flange slurry (approx. 29 g wet weight and 20 g\ndry weight) were transferred into Balch tubes in an anaerobic chamber, and\nsupplemented with 15 mL of sterile artificial seawater media designed to mimic\nthe geochemical conditions within a hydrothermal flange (400 mM NaCl, 25 mM\nKCl, 30 mM CaCl2, 2.3 mM NaHCO3, 14 mM NaSO42-, 1 mM H2S, and 50 uM dissolved\norganic carbon - consisting of equimolar proportions 10 uM of pyruvate,\ncitrate, formate, acetate, lactate) under a pure nitrogen headspace.\\u00a0\n \nConcentrations of sulfide, sulfate and dissolved organic carbon (DOC) were\nvaried independently to investigate concentration dependent effects on the\nrates of SR. The range of experimental conditions tested was determined from\npreviously published concentration profiles of aqueous species modeled as\nfunctions of temperature and position within the Grotto vent structure (Tivey,\n2004). Concentrations were varied by orders of magnitude within the modeled\nranges to simulate conditions representative of different mixing regimes\nbetween seawater and vent fluid (Table 1). The range of DOC (which we\napproximate as a mix of pyruvate, citrate, formate, acetate, lactate \\u2013\nmost of which have been identified to varying degrees within vent fluid and\nare known carbon sources for heterotrophic SR in culture) concentrations\ntested were based on the average DOC concentrations measured within diffuse\nfluids at the Main Endeavor Field (Lang\\u00a0et al., 2006; Lang\\u00a0et\nal.,\\u00a02010). Hydrogen sulfide was present as H2S (pKa\\u00a0in seawater of\n6.60) across all the conditions tested (Amend & Shock, 2001). Incubations were\ncarried out at pH 4 (to simulate the pH of end-member Grotto vent fluid and\nthe average calculated pH of\\u00a0mixed fluids in highly reduced zones within\nthe flange; Tivey 2004) as well as pH 6 (representative of the calculated pH\nin fluid mixing zones; Tivey 2004). All the results are presented and\ndiscussed in the context of the initial measured media conditions.\\u00a0\n \nSufficient\\u00a035SO42-\\u00a0was added to achieve 15 uCi of activity. Samples\nwere incubated anaerobically for 1, 3 or 7 days at ambient seawater (4 degrees\ncelsius), thermophilic (50 degrees celsius) and hyperthermophilic (90 degrees\ncelsius) temperatures. The range of temperatures considered was representative\nof different thermal regimes associated with the surface, outer layer and\nmiddle regions of hydrothermal chimneys (Tivey 2004; Kormas\\u00a0et\nal.\\u00a02006; Schrenk\\u00a0et al. 2003). Negative controls consisted of\nsamples amended with 28 mM molybdate to inhibit SR (Newport & Nedwell, 1988;\nSaleh\\u00a0et al., 1964). Three biological replicates were run for each\ntreatment, and two biological replicates for each control.\\u00a0\n \nUpon completion, reactions were quenched with the injection of 5 mL 25% zinc\nacetate, at pH 8 (i.e. 20-fold excess Zn), and all samples were frozen at -20\ndegrees celsius for further analysis. 80% of incubations were performed\nshipboard with freshly collected samples and the remaining 20% of incubations\nwere completed within one year of collection.\\u00a0\n \nTo determine SR rates, samples were thawed and the supernatant was removed and\nfiltered through a 0.2 um syringe filter. The homogenized flange that remained\nin the tube was washed three times with deionized water to remove any\nremaining sulfate. One gram (wet weight) of flange material was added to 10 mL\nof a 1:1 ethanol to water solution in the chromium distillation apparatus, and\nthen degassed with nitrogen for 15 minutes to drive the environment anoxic.\nHydrogen sulfide gas was evolved after the anaerobic addition of 8 mL of 12 N\nHCl and 10 mL of 1 M reduced chromium chloride, followed by 3 hours of\nheating. The resulting hydrogen sulfide gas was carried via nitrogen gas\nthrough a condenser to remove\\u00a0HCl,\\u00a0and was then trapped as zinc\nsulfide in a 25% zinc acetate solution. To moderate potential artifacts of hot\ndistillation methods including elevated rates in control samples, experiments\nwere analyzed in triplicate, on different days and with different glassware to\nminimize cross-contamination, and any activity observed in \\u201ccontrol\\u201d\nsamples was deleted from the treatments. The radioactivity of the resulting\nsulfide (Zn35S) and the remaining sulfate from the supernatant\n(35SO42-)\\u00a0were\\u00a0measured via liquid scintillation counter in Ultima\nGold scintillation cocktail (ThermoFisher Inc., Waltham, MA).\\u00a0\n \nOnce on board ship,\\u00a0tubeworms\\u00a0and other macrofauna were removed from\nthe samples and the large pieces were broken into more manageable fragments\n(~10-20 cm3) with a flame-sterilized chisel and sledgehammer, with the user\nwearing sterile nitrile gloves. Samples were quickly transferred to 0.2 um-\nfiltered anaerobic (nitrogen-sparged) seawater. Samples were further broken\ndown into smaller sizes while in anaerobic water, and subsamples from the\ninterior of the fragments were immediately transferred to gastight jars\n(Freund Container Inc.) filled with sterile anaerobic seawater containing 2 mM\nsodium sulfide at pH 6, and stored at 4 degrees celsius for incubations and\nanalyses. The sterile sulfidic seawater in the gastight\njars\\u00a0were\\u00a0refreshed periodically during storage at 4 degrees\ncelsius. The majority of the rate experiments (80%) were set up immediately on\nthe ship using freshly collected samples. In parallel, subsamples (~1 cm3)\nfrom each flange were preserved aboard ship in glutaraldehyde (2.5% in\nphosphate buffered saline, PBS, pH 7.0), then prepared for electron microscopy\nvia ethanol dehydration and critical point drying before being sputtered with\na thin layer of gold-palladium to improve image resolution. Samples were\nimaged with a Zeiss model EVO Scanning Electron Microscope (SEM).\\u00a0\n \nPrior to incubation, each flange subsample was pulverized by hand for about\none hour to minimize fine-scale geological and microbial heterogeneity and\nfacilitate more accurate experimental replication (akin to slurry experiments\nin sediments; Fossing & J\\u00f8rgensen 1989; Weber & J\\u00f8rgensen 2002;\nJ\\u00f8rgensen et al. 1992). Specifically, each subsample was pulverized with\na flame-sterilized sledgehammer in sterile seawater actively bubbled with\nnitrogen within an anaerobic chamber. For each independent treatment, aliquots\nof 7.5 mL flange slurry (approx. 29 g wet weight and 20 g dry weight) were\ntransferred into Balch tubes in an anaerobic chamber, and supplemented with 15\nmL of sterile artificial seawater media designed to mimic the geochemical\nconditions within a hydrothermal flange (400 mM NaCl, 25 mM KCl, 30 mM CaCl2,\n2.3 mM NaHCO3, 14 mM NaSO42-, 1 mM H2S, and 50 uM dissolved organic carbon -\nconsisting of equimolar proportions 10 uM of pyruvate, citrate, formate,\nacetate, lactate) under a pure nitrogen headspace.\\u00a0\n \nConcentrations of sulfide, sulfate and dissolved organic carbon (DOC) were\nvaried independently to investigate concentration dependent effects on the\nrates of SR. The range of experimental conditions tested was determined from\npreviously published concentration profiles of aqueous species modeled as\nfunctions of temperature and position within the Grotto vent structure (Tivey,\n2004). Concentrations were varied by orders of magnitude within the modeled\nranges to simulate conditions representative of different mixing regimes\nbetween seawater and vent fluid (Table 1). The range of DOC (which we\napproximate as a mix of pyruvate, citrate, formate, acetate, lactate \\u2013\nmost of which have been identified to varying degrees within vent fluid and\nare known carbon sources for heterotrophic SR in culture) concentrations\ntested were based on the average DOC concentrations measured within diffuse\nfluids at the Main Endeavor Field (Lang et al., 2006; Lang et al., 2010).\nHydrogen sulfide was present as H2S (pKa in seawater of 6.60) across all the\nconditions tested (Amend & Shock, 2001). Incubations were carried out at pH 4\n(to simulate the pH of end-member Grotto vent fluid and the average calculated\npH of mixed fluids in highly reduced zones within the flange; Tivey 2004) as\nwell as pH 6 (representative of the calculated pH in fluid mixing zones; Tivey\n2004). All the results are presented and discussed in the context of the\ninitial measured media conditions.\\u00a0\n \nSufficient 35SO42- was added to achieve 15 uCi of activity. Samples were\nincubated anaerobically for 1, 3 or 7 days at ambient seawater (4 degrees\ncelsius), thermophilic (50 degrees celsius) and hyperthermophilic (90 degrees\ncelsius) temperatures. The range of temperatures considered was representative\nof different thermal regimes associated with the surface, outer layer and\nmiddle regions of hydrothermal chimneys (Tivey 2004; Kormas et al. 2006;\nSchrenk et al. 2003). Negative controls consisted of samples amended with 28\nmM molybdate to inhibit SR (Newport & Nedwell, 1988; Saleh et al., 1964).\nThree biological replicates were run for each treatment, and two biological\nreplicates for each control.\\u00a0\n \nUpon completion, reactions were quenched with the injection of 5 mL 25% zinc\nacetate, at pH 8 (i.e. 20-fold excess Zn), and all samples were frozen at -20\ndegrees celsius for further analysis. 80% of incubations were performed\nshipboard with freshly collected samples and the remaining 20% of incubations\nwere completed within one year of collection.\\u00a0\n \nTo determine SR rates, samples were thawed and the supernatant was removed and\nfiltered through a 0.2 um syringe filter. The homogenized flange that remained\nin the tube was washed three times with deionized water to remove any\nremaining sulfate. One gram (wet weight) of flange material was added to 10 mL\nof a 1:1 ethanol to water solution in the chromium distillation apparatus, and\nthen degassed with nitrogen for 15 minutes to drive the environment anoxic.\nHydrogen sulfide gas was evolved after the anaerobic addition of 8 mL of 12 N\nHCl and 10 mL of 1 M reduced chromium chloride, followed by 3 hours of\nheating. The resulting hydrogen sulfide gas was carried via nitrogen gas\nthrough a condenser to remove\\u00a0HCl,\\u00a0and was then trapped as zinc\nsulfide in a 25% zinc acetate solution. To moderate potential artifacts of hot\ndistillation methods including elevated rates in control samples, experiments\nwere analyzed in triplicate, on different days and with different glassware to\nminimize cross-contamination, and any activity observed in \\u201ccontrol\\u201d\nsamples was deleted from the treatments. The radioactivity of the resulting\nsulfide (Zn35S) and the remaining sulfate from the supernatant\n(35SO42-)\\u00a0were\\u00a0measured via liquid scintillation counter in Ultima\nGold scintillation cocktail (ThermoFisher Inc., Waltham, MA).\\u00a0 |
attribute | NC_GLOBAL | awards_0_award_nid | String | 554913 |
attribute | NC_GLOBAL | awards_0_award_number | String | OCE-1061934 |
attribute | NC_GLOBAL | awards_0_data_url | String | http://www.nsf.gov/awardsearch/showAward.do?AwardNumber=1061934 |
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 | 626305 |
attribute | NC_GLOBAL | awards_1_award_number | String | OCE-0838107 |
attribute | NC_GLOBAL | awards_1_data_url | String | http://www.nsf.gov/awardsearch/showAward?AWD_ID=0838107 |
attribute | NC_GLOBAL | awards_1_funder_name | String | NSF Division of Ocean Sciences |
attribute | NC_GLOBAL | awards_1_funding_acronym | String | NSF OCE |
attribute | NC_GLOBAL | awards_1_funding_source_nid | String | 355 |
attribute | NC_GLOBAL | awards_1_program_manager | String | Kandace S Binkley |
attribute | NC_GLOBAL | awards_1_program_manager_nid | String | 51512 |
attribute | NC_GLOBAL | awards_2_award_nid | String | 626308 |
attribute | NC_GLOBAL | awards_2_award_number | String | NNX09AB78G |
attribute | NC_GLOBAL | awards_2_funder_name | String | NASA Astrobiology Science & Technology for Exploring Planets |
attribute | NC_GLOBAL | awards_2_funding_acronym | String | NASA-ASTEP |
attribute | NC_GLOBAL | awards_2_funding_source_nid | String | 626307 |
attribute | NC_GLOBAL | awards_3_award_nid | String | 626309 |
attribute | NC_GLOBAL | awards_3_award_number | String | NNX07AV51G |
attribute | NC_GLOBAL | awards_3_funder_name | String | NASA Astrobiology Science & Technology for Exploring Planets |
attribute | NC_GLOBAL | awards_3_funding_acronym | String | NASA-ASTEP |
attribute | NC_GLOBAL | awards_3_funding_source_nid | String | 626307 |
attribute | NC_GLOBAL | cdm_data_type | String | Other |
attribute | NC_GLOBAL | comment | String | Sulfate Reduction Rates \n P. Girguis, PI \n Version 13 October 2016 |
attribute | NC_GLOBAL | Conventions | String | COARDS, CF-1.6, ACDD-1.3 |
attribute | NC_GLOBAL | creator_email | String | info at bco-dmo.org |
attribute | NC_GLOBAL | creator_name | String | BCO-DMO |
attribute | NC_GLOBAL | creator_type | String | institution |
attribute | NC_GLOBAL | creator_url | String | https://www.bco-dmo.org/ |
attribute | NC_GLOBAL | data_source | String | extract_data_as_tsv version 2.3 19 Dec 2019 |
attribute | NC_GLOBAL | date_created | String | 2016-10-13T21:40:27Z |
attribute | NC_GLOBAL | date_modified | String | 2019-04-22T18:17:30Z |
attribute | NC_GLOBAL | defaultDataQuery | String | &time<now |
attribute | NC_GLOBAL | doi | String | 10.1575/1912/bco-dmo.661557.1 |
attribute | NC_GLOBAL | Easternmost_Easting | double | -129.1 |
attribute | NC_GLOBAL | geospatial_lat_max | double | 47.95 |
attribute | NC_GLOBAL | geospatial_lat_min | double | 47.95 |
attribute | NC_GLOBAL | geospatial_lat_units | String | degrees_north |
attribute | NC_GLOBAL | geospatial_lon_max | double | -129.1 |
attribute | NC_GLOBAL | geospatial_lon_min | double | -129.1 |
attribute | NC_GLOBAL | geospatial_lon_units | String | degrees_east |
attribute | NC_GLOBAL | infoUrl | String | https://www.bco-dmo.org/dataset/661557 |
attribute | NC_GLOBAL | institution | String | BCO-DMO |
attribute | NC_GLOBAL | instruments_0_acronym | String | in-situ incubator |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_description | String | Used aboard ship and in lab |
attribute | NC_GLOBAL | instruments_0_dataset_instrument_nid | String | 661748 |
attribute | NC_GLOBAL | instruments_0_description | String | A device on shipboard or in the laboratory that holds water samples under controlled conditions of temperature and possibly illumination. |
attribute | NC_GLOBAL | instruments_0_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/82/ |
attribute | NC_GLOBAL | instruments_0_instrument_name | String | In-situ incubator |
attribute | NC_GLOBAL | instruments_0_instrument_nid | String | 494 |
attribute | NC_GLOBAL | instruments_0_supplied_name | String | Incubator |
attribute | NC_GLOBAL | instruments_1_acronym | String | LSC |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_description | String | Used to quantify activity |
attribute | NC_GLOBAL | instruments_1_dataset_instrument_nid | String | 661807 |
attribute | NC_GLOBAL | instruments_1_description | String | Liquid scintillation counting is an analytical technique which is defined by the incorporation of the radiolabeled analyte into uniform distribution with a liquid chemical medium capable of converting the kinetic energy of nuclear emissions into light energy. Although the liquid scintillation counter is a sophisticated laboratory counting system used the quantify the activity of particulate emitting (ß and a) radioactive samples, it can also detect the auger electrons emitted from 51Cr and 125I samples. |
attribute | NC_GLOBAL | instruments_1_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB21/ |
attribute | NC_GLOBAL | instruments_1_instrument_name | String | Liquid Scintillation Counter |
attribute | NC_GLOBAL | instruments_1_instrument_nid | String | 624 |
attribute | NC_GLOBAL | instruments_1_supplied_name | String | Liquid scintillation counter |
attribute | NC_GLOBAL | instruments_2_acronym | String | pH Sensor |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_description | String | pH sensor |
attribute | NC_GLOBAL | instruments_2_dataset_instrument_nid | String | 661637 |
attribute | NC_GLOBAL | instruments_2_description | String | General term for an instrument that measures the pH or how acidic or basic a solution is. |
attribute | NC_GLOBAL | instruments_2_instrument_name | String | pH Sensor |
attribute | NC_GLOBAL | instruments_2_instrument_nid | String | 674 |
attribute | NC_GLOBAL | instruments_2_supplied_name | String | pH sensor |
attribute | NC_GLOBAL | instruments_3_acronym | String | Dissolved Oxygen Sensor |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_description | String | DOC was measured |
attribute | NC_GLOBAL | instruments_3_dataset_instrument_nid | String | 661638 |
attribute | NC_GLOBAL | instruments_3_description | String | An electronic device that measures the proportion of oxygen (O2) in the gas or liquid being analyzed |
attribute | NC_GLOBAL | instruments_3_instrument_name | String | Dissolved Oxygen Sensor |
attribute | NC_GLOBAL | instruments_3_instrument_nid | String | 705 |
attribute | NC_GLOBAL | instruments_3_supplied_name | String | DO sensor |
attribute | NC_GLOBAL | instruments_4_dataset_instrument_description | String | Tubeworm and macrofauna subsamples were imaged. |
attribute | NC_GLOBAL | instruments_4_dataset_instrument_nid | String | 661635 |
attribute | NC_GLOBAL | instruments_4_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_4_instrument_external_identifier | String | https://vocab.nerc.ac.uk/collection/L05/current/LAB07/ |
attribute | NC_GLOBAL | instruments_4_instrument_name | String | Microscope-Electron |
attribute | NC_GLOBAL | instruments_4_instrument_nid | String | 709 |
attribute | NC_GLOBAL | instruments_4_supplied_name | String | Zeiss model EVO Scanning Electron Microscope |
attribute | NC_GLOBAL | keywords | String | 3day, 7day, bco, bco-dmo, biological, chemical, chemistry, commerce, data, dataset, department, dmo, doc, earth, Earth Science > Oceans > Ocean Chemistry > pH, erddap, experiment, experiment_num, inhibited, inoculum, latitude, longitude, management, num, ocean, oceanography, oceans, office, preliminary, replicates, reported, scale, science, sea, sea_water_ph_reported_on_total_scale, seawater, srrate, SRrate_3day, SRrate_3day_replicates, SRrate_7day, SRrate_7day_replicates, SRrate_inhibited, SRrate_inhibited_replicates, sulfate, sulfide, temperature, total, water |
attribute | NC_GLOBAL | keywords_vocabulary | String | GCMD Science Keywords |
attribute | NC_GLOBAL | license | String | https://www.bco-dmo.org/dataset/661557/license |
attribute | NC_GLOBAL | metadata_source | String | https://www.bco-dmo.org/api/dataset/661557 |
attribute | NC_GLOBAL | Northernmost_Northing | double | 47.95 |
attribute | NC_GLOBAL | param_mapping | String | {'661557': {'lat': 'master - latitude', 'lon': 'master - longitude'}} |
attribute | NC_GLOBAL | parameter_source | String | https://www.bco-dmo.org/mapserver/dataset/661557/parameters |
attribute | NC_GLOBAL | people_0_affiliation | String | Harvard University |
attribute | NC_GLOBAL | people_0_person_name | String | Peter Girguis |
attribute | NC_GLOBAL | people_0_person_nid | String | 544586 |
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 Hawaii at Manoa |
attribute | NC_GLOBAL | people_1_affiliation_acronym | String | SOEST |
attribute | NC_GLOBAL | people_1_person_name | String | Kiana Frank |
attribute | NC_GLOBAL | people_1_person_nid | String | 626318 |
attribute | NC_GLOBAL | people_1_role | String | Contact |
attribute | NC_GLOBAL | people_1_role_type | String | related |
attribute | NC_GLOBAL | people_2_affiliation | String | Woods Hole Oceanographic Institution |
attribute | NC_GLOBAL | people_2_affiliation_acronym | String | WHOI BCO-DMO |
attribute | NC_GLOBAL | people_2_person_name | String | Hannah Ake |
attribute | NC_GLOBAL | people_2_person_nid | String | 650173 |
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 | North Pond Microbes,Middle Valley Vents |
attribute | NC_GLOBAL | projects_0_acronym | String | North Pond Microbes |
attribute | NC_GLOBAL | projects_0_description | String | Description from NSF award abstract:\nCurrent estimates suggest that the volume of ocean crust capable of sustaining life is comparable in magnitude to that of the oceans. To date, there is little understanding of the composition or functional capacity of microbial communities in the sub-seafloor, or their influence on the chemistry of the oceans and subsequent consequences for global biogeochemical cycles. This project focuses on understanding the relationship between microbial communities and fluid chemistry in young crustal fluids that are responsible for the transport of energy, nutrients, and organisms in the crust. Specifically, the PIs will couple microbial activity measurements, including autotrophic carbon, nitrogen and sulfur metabolisms as well as mineral oxide reduction, with quantitative assessments of functional gene expression and geochemical transformations in basement fluids. Through a comprehensive suite of in situ and shipboard analyses, this research will yield cross-disciplinary advances in our understanding of the microbial ecology and geochemistry of the sub-seafloor biosphere. The focus of the effort is at North Pond, an isolated sediment pond located on ridge flank oceanic crust 7-8 million years old on the western side of the Mid-Atlantic Ridge. North Pond is currently the target for drilling on IODP expedition 336, during which it will be instrumented with three sub-seafloor basement observatories.\nThe project will leverage this opportunity for targeted and distinct sampling at North Pond on two German-US research cruises to accomplish three main objectives:\n1. to determine if different basement fluid horizons across North Pond host distinct microbial communities and chemical milieus and the degree to which they change over a two-year post-drilling period.\n2. to quantify the extent of autotrophic metabolism via microbially-mediated transformations in carbon, nitrogen, and sulfur species in basement fluids at North Pond.\n3. to determine the extent of suspended particulate mineral oxides in basement fluids at North Pond and to characterize their role as oxidants for fluid-hosted microbial communities.\nSpecific outcomes include quantitative assessments of microbial activity and gene expression as well as geochemical transformations. The program builds on the integrative research goals for North Pond and will provide important data for guiding the development of that and future deep biosphere research programs. Results will increase understanding of microbial life and chemistry in young oceanic crust as well as provide new insights into controls on the distribution and activity of marine microbial communities throughout the worlds oceans.\nThere are no data about microbial communities in ubiquitous cold, oceanic crust, the emphasis of the proposed work. This is an interdisciplinary project at the interface of microbial ecology, chemistry, and deep-sea oceanography with direct links to international and national research and educational organizations. |
attribute | NC_GLOBAL | projects_0_end_date | String | 2015-05 |
attribute | NC_GLOBAL | projects_0_geolocation | String | North Pond, mid-Atlantic Ridge |
attribute | NC_GLOBAL | projects_0_name | String | Collaborative Research: Characterization of Microbial Transformations in Basement Fluids, from Genes to Geochemical Cycling |
attribute | NC_GLOBAL | projects_0_project_nid | String | 554914 |
attribute | NC_GLOBAL | projects_0_start_date | String | 2011-06 |
attribute | NC_GLOBAL | projects_1_acronym | String | Middle Valley Vents |
attribute | NC_GLOBAL | projects_1_description | String | This project characterizes rates of microbially mediated sulfate reduction from three distinct hydrothermal vents in the Middle Valley vent field along the Juan de Fuca Ridge, as well as assessments of bacterial and archaeal diversity, estimates of total biomass and the abundance of functional genes related to sulfate reduction, and in situ geochemistry. Maximum rates of sulfate reduction occurred at 90°C in all three deposits. Pyrosequencing and functional gene abundance data reveal differences in both biomass and community composition among sites, including differences in the abundance of known sulfate reducing bacteria. The abundance of sequences for Thermodesulfovibro-like organisms and higher sulfate reduction rates at elevated temperatures, suggests that Thermodesulfovibro-like organisms may play a role in sulfate reduction in warmer environments. The rates of sulfate reduction observed suggest that - within anaerobic niches of hydrothermal deposits - heterotrophic sulfate reduction may be quite common and might contribute substantially to secondary productivity, underscoring the potential role of this process in both sulfur and carbon cycling at vents.\nThis project was funded, in part, by a C-DEBI Graduate Student Fellowship. |
attribute | NC_GLOBAL | projects_1_geolocation | String | Middle Valley vent field along the Juan de Fuca Ridge |
attribute | NC_GLOBAL | projects_1_name | String | Characterizing the distribution and rates of microbial sulfate reduction at Middle Valley hydrothermal vents |
attribute | NC_GLOBAL | projects_1_project_nid | String | 626603 |
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 | 47.95 |
attribute | NC_GLOBAL | standard_name_vocabulary | String | CF Standard Name Table v55 |
attribute | NC_GLOBAL | subsetVariables | String | latitude,longitude,SRrate_3day_replicates,SRrate_inhibited_replicates |
attribute | NC_GLOBAL | summary | String | Sulfate reduction rates at Main Endeavor grotto chimney from samples collected on RV Atlantis (AT18-08) during Jason II dives in the Juan de Fuca Ridge from July to August 2011 |
attribute | NC_GLOBAL | title | String | [Sulfate reduction rates] - Sulfate reduction rates at Main Endeavor grotto chimney from samples collected on RV Atlantis (AT18-08) during Jason II dives in the Juan de Fuca Ridge from July to August 2011 (Characterizing the distribution and rates of microbial sulfate reduction at Middle Valley hydrothermal vents) |
attribute | NC_GLOBAL | version | String | 1 |
attribute | NC_GLOBAL | Westernmost_Easting | double | -129.1 |
attribute | NC_GLOBAL | xml_source | String | osprey2erddap.update_xml() v1.3 |
variable | inoculum | String | ||
attribute | inoculum | bcodmo_name | String | incubation time |
attribute | inoculum | description | String | Fresh: incubation performed on shipboard with freshly collected samples; Stored: incubation completed within one year of collection. |
attribute | inoculum | long_name | String | Inoculum |
attribute | inoculum | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/AZDRZZ01/ |
attribute | inoculum | units | String | unitless |
variable | experiment_num | String | ||
attribute | experiment_num | bcodmo_name | String | exp_id |
attribute | experiment_num | description | String | PI issued experiment ID number |
attribute | experiment_num | long_name | String | Experiment Num |
attribute | experiment_num | units | String | unitless |
variable | latitude | double | ||
attribute | latitude | _CoordinateAxisType | String | Lat |
attribute | latitude | _FillValue | double | NaN |
attribute | latitude | actual_range | double | 47.95, 47.95 |
attribute | latitude | axis | String | Y |
attribute | latitude | bcodmo_name | String | latitude |
attribute | latitude | colorBarMaximum | double | 90.0 |
attribute | latitude | colorBarMinimum | double | -90.0 |
attribute | latitude | description | String | Latitude |
attribute | latitude | ioos_category | String | Location |
attribute | latitude | long_name | String | Latitude |
attribute | latitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LATX/ |
attribute | latitude | standard_name | String | latitude |
attribute | latitude | units | String | degrees_north |
variable | longitude | double | ||
attribute | longitude | _CoordinateAxisType | String | Lon |
attribute | longitude | _FillValue | double | NaN |
attribute | longitude | actual_range | double | -129.1, -129.1 |
attribute | longitude | axis | String | X |
attribute | longitude | bcodmo_name | String | longitude |
attribute | longitude | colorBarMaximum | double | 180.0 |
attribute | longitude | colorBarMinimum | double | -180.0 |
attribute | longitude | description | String | Longitude |
attribute | longitude | ioos_category | String | Location |
attribute | longitude | long_name | String | Longitude |
attribute | longitude | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P09/current/LONX/ |
attribute | longitude | standard_name | String | longitude |
attribute | longitude | units | String | degrees_east |
variable | sulfide | float | ||
attribute | sulfide | _FillValue | float | NaN |
attribute | sulfide | actual_range | float | 1.0E-9, 0.001 |
attribute | sulfide | bcodmo_name | String | sulfide |
attribute | sulfide | description | String | Independently varied concentration of sulfide |
attribute | sulfide | long_name | String | Sulfide |
attribute | sulfide | units | String | molar (M) |
variable | DOC | float | ||
attribute | DOC | _FillValue | float | NaN |
attribute | DOC | actual_range | float | 0.0, 50.0 |
attribute | DOC | bcodmo_name | String | DOC |
attribute | DOC | description | String | Independently varied dissolved oxygen concentration |
attribute | DOC | long_name | String | DOC |
attribute | DOC | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/CORGZZZX/ |
attribute | DOC | units | String | micromoles (uM) |
variable | sulfate | float | ||
attribute | sulfate | _FillValue | float | NaN |
attribute | sulfate | actual_range | float | 1.0E-5, 14.0 |
attribute | sulfate | bcodmo_name | String | SO4 |
attribute | sulfate | description | String | Independently varied concentration of sulfate |
attribute | sulfate | long_name | String | Sulfate |
attribute | sulfate | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/SPHTMAXX/ |
attribute | sulfate | units | String | millimoles (mM) |
variable | pH | byte | ||
attribute | pH | _FillValue | byte | 127 |
attribute | pH | actual_range | byte | 4, 6 |
attribute | pH | bcodmo_name | String | pH |
attribute | pH | colorBarMaximum | double | 9.0 |
attribute | pH | colorBarMinimum | double | 7.0 |
attribute | pH | description | String | pH of media added to incubations; Incubations were carried out at either pH 4 or 6; 4: simulates the pH of end-member Grotto vent fluid and the average calculated pH of mixed fluids in highly reduced zones within flange (Tivey 2004). 6: represents the calculated pH in fluid mixing zones (Tivey 2004). |
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 | pH |
variable | temperature | byte | ||
attribute | temperature | _FillValue | byte | 127 |
attribute | temperature | actual_range | byte | 4, 90 |
attribute | temperature | bcodmo_name | String | temperature |
attribute | temperature | description | String | Temperatures at which samples were incubated anaerobically for 1, 3, or 7 days. 4 C: ambient seawater; 50 C: thermophilic; 90 C: hyperthermophilic. |
attribute | temperature | long_name | String | Temperature |
attribute | temperature | units | String | celsius (C) |
variable | SRrate_3day | float | ||
attribute | SRrate_3day | _FillValue | float | NaN |
attribute | SRrate_3day | actual_range | float | 0.0, 1695.552 |
attribute | SRrate_3day | bcodmo_name | String | SO4 |
attribute | SRrate_3day | description | String | Sulfate reduction rate after 3 day incubation |
attribute | SRrate_3day | long_name | String | SRrate 3day |
attribute | SRrate_3day | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/SPHTMAXX/ |
attribute | SRrate_3day | units | String | nmol/gday |
variable | SRrate_3day_replicates | byte | ||
attribute | SRrate_3day_replicates | _FillValue | byte | 127 |
attribute | SRrate_3day_replicates | actual_range | byte | 3, 3 |
attribute | SRrate_3day_replicates | bcodmo_name | String | num_reps |
attribute | SRrate_3day_replicates | description | String | Number of replicates used for 3 day incubation |
attribute | SRrate_3day_replicates | long_name | String | SRrate 3day Replicates |
attribute | SRrate_3day_replicates | units | String | count |
variable | SRrate_7day | float | ||
attribute | SRrate_7day | _FillValue | float | NaN |
attribute | SRrate_7day | actual_range | float | 0.0, 1678.113 |
attribute | SRrate_7day | bcodmo_name | String | SO4 |
attribute | SRrate_7day | description | String | Sulfate reduction rate after 7 day incubation |
attribute | SRrate_7day | long_name | String | SRrate 7day |
attribute | SRrate_7day | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/SPHTMAXX/ |
attribute | SRrate_7day | units | String | nmol/gday |
variable | SRrate_7day_replicates | byte | ||
attribute | SRrate_7day_replicates | _FillValue | byte | 127 |
attribute | SRrate_7day_replicates | actual_range | byte | 0, 3 |
attribute | SRrate_7day_replicates | bcodmo_name | String | num_reps |
attribute | SRrate_7day_replicates | description | String | Number of replicates used for 7 day incubation |
attribute | SRrate_7day_replicates | long_name | String | SRrate 7day Replicates |
attribute | SRrate_7day_replicates | units | String | count |
variable | SRrate_inhibited | float | ||
attribute | SRrate_inhibited | _FillValue | float | NaN |
attribute | SRrate_inhibited | actual_range | float | 0.0, 9.19 |
attribute | SRrate_inhibited | bcodmo_name | String | SO4 |
attribute | SRrate_inhibited | description | String | Sulfate reduction rate molybdate inhibited controls |
attribute | SRrate_inhibited | long_name | String | SRrate Inhibited |
attribute | SRrate_inhibited | nerc_identifier | String | https://vocab.nerc.ac.uk/collection/P01/current/SPHTMAXX/ |
attribute | SRrate_inhibited | units | String | nmol/gday |
variable | SRrate_inhibited_replicates | byte | ||
attribute | SRrate_inhibited_replicates | _FillValue | byte | 127 |
attribute | SRrate_inhibited_replicates | actual_range | byte | 2, 2 |
attribute | SRrate_inhibited_replicates | bcodmo_name | String | num_reps |
attribute | SRrate_inhibited_replicates | description | String | Number of replicates used for molybdate inhibited controls |
attribute | SRrate_inhibited_replicates | long_name | String | SRrate Inhibited Replicates |
attribute | SRrate_inhibited_replicates | units | String | count |