ICP OES (Agilent Technologies 700 series axial)
A spectrometer is an optical instrument used to measure properties of light over a specific portion of the electromagnetic spectrum.
URL | https://www.bco-dmo.org/dataset/626741 |
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Download URL | https://www.bco-dmo.org/dataset/626741/data/download |
Media Type | text/tab-separated-values |
Created | November 20, 2015 |
Modified | August 19, 2016 |
State | Final no updates expected |
Brief Description | Elemental composition for 16S rRNA gene amplicon and metagenomic sequences |
Analyses performed on “Mobio” IODP samples previously frozen at -80C. Reactive Fe and Mn were extracted using the citrate-dithionite method and measured on an ICP OES (Agilent Technologies 700 series axial). Analysis for TC, TN, and TS were determined using PE 2400 CN(S) analyzer. Analysis for TIC was determined by CM5014 CO2 coulometer with a CM5130 Acidification module.
BCO-DMO Processing:
– Added cruise_id, lat and lon columns
ICP OES (Agilent Technologies 700 series axial)
A spectrometer is an optical instrument used to measure properties of light over a specific portion of the electromagnetic spectrum.
PE 2400 CN(S) analyzer
Instruments that quantify carbon, nitrogen and sometimes other elements by combusting the sample at very high temperature and assaying the resulting gaseous oxides. Usually used for samples including organic material.
CM5014 CO2 coulometer with a CM5130 Acidification module.
latitude, in decimal degrees, North is positive, negative denotes South; Reported in some datasets as degrees, minutes
longitude, in decimal degrees, East is positive, negative denotes West; Reported in some datsets as degrees, minutes
unique sample identification or number; any combination of alpha numeric characters; precise definition is file dependent
unique sample identification or number; any combination of alpha numeric characters; precise definition is file dependent
Observation/sample depth below the sea surface. Units often reported as: meters, feet.
When used in a JGOFS/GLOBEC dataset the depth is a best estimate; usually but not always calculated from pressure; calculated either from CTD pressure using Fofonoff and Millard (1982; UNESCO Tech Paper #44) algorithm adjusted for 1980 equation of state for seawater (EOS80) or simply equivalent to nominal depth as recorded during sampling if CTD pressure was unavailable.
Calcium Carbonate, in sediments as percent; or CaCO3 from water samples reported in various units; CAUTION measured in sediment and water column samples
Iron (Fe). Concentrations may be reported in parts per million, nanomoles per liter, or other units. Refer to dataset metadata for units.
reactive iron standard deviation of duplicate extractions and analyses
Manganese (Mn). Concentrations may be reported in parts per million, nanomoles per liter, or other units. Refer to dataset metadata for units.
standard deviation of duplicate extractions and analyses for reactive manganese
Name | Affiliation | Contact |
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Jennifer B. Glass | Georgia Institute of Technology (Georgia Tech) | ✓ |
James McManus | Georgia Institute of Technology (Georgia Tech) | ✓ |
Nancy Copley | University of Akron (UAkron) | |
Beth N. Orcutt | University of Akron (UAkron) | |
Nancy Copley | Woods Hole Oceanographic Institution (WHOI BCO-DMO) |
Project Title | Functional gene diversity and expression in methane-hydrate bearing deep subsurface sediments |
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Acronym | Methane-Hydrate Sediment Omics |
URL | https://www.bco-dmo.org/project/626690 |
Created | November 19, 2015 |
Modified | November 19, 2015 |
Methane is a critical component of the deep subsurface. In shallow marine sediments, anaerobic oxidation of methane (AOM) is coupled to sulfate reduction. However, relatively little is known about which microbial metabolisms are active in deeply buried sediment containing methane hydrates, particularly with regard to alternative electron acceptors that could fuel deep AOM. We propose to determine which microbial population(s) and functional genes are active in the deep biosphere beneath Hydrate Ridge offshore Oregon by sequencing metagenomes and metatranscriptomes from samples drilled on ODP Leg 204 and archived for future molecular analysis. We will analyze gene diversity and expression in six geochemically distinct zones from 2 to 139 meters below the seafloor with the goal of evaluating the relationship between geochemical conditions (i.e. sulfate, iron and manganese availability) and microbial metabolic activity.
Related References:
Tréhu, A.M, Bohrmann, G., Rack, F.R., Torres, M.E., et al., 2003. Proc. ODP, Init. Repts., 204: College Station, TX (Ocean Drilling Program).doi:10.2973/odp.proc.ir.204.2003
Shipboard Scientific Party, 2003. Site 1244. In Tréhu, A.M, Bohrmann, G., Rack, F.R., Torres, M.E., et al., Proc. ODP, Init. Repts., 204: College Station, TX (Ocean Drilling Program), 1–132. doi:10.2973/odp.proc.ir.204.103.2003
Tréhu, A.M., Bohrmann, G., Torres, M.E., and Colwell, F.S. (Eds.), 2006. Proc. ODP, Sci. Results, 204: College Station, TX (Ocean Drilling Program). doi:10.2973/odp.proc.sr.204.2006
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This work was supported by a C-DEBI Research Grant.
Name | Affiliation | Role |
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Jennifer B. Glass | Georgia Institute of Technology (Georgia Tech) | Principal Investigator |
Cecilia Batmalle Kretz | Georgia Institute of Technology (Georgia Tech) | Co-Principal Investigator |
James McManus | University of Akron (UAkron) | Scientist |