http://lod.bco-dmo.org/id/dataset/719067
eng; USA
utf8
dataset
Highest level of data collection, from a common set of sensors or instrumentation, usually within the same research project
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
2017-11-13
ISO 19115-2 Geographic Information - Metadata - Part 2: Extensions for Imagery and Gridded Data
ISO 19115-2:2009(E)
Shotgun Metaproteomics of Bering Strait surface water and Chukchi Sea bottom water.
2017-11-13
publication
2017-11-13
revision
BCO-DMO Linked Data URI
2017-11-13
creation
http://lod.bco-dmo.org/id/dataset/719067
William S. Noble
University of Washington
principalInvestigator
Brook L. Nunn
University of Washington
principalInvestigator
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
publisher
Cite this dataset as: Nunn, B. L., Noble, W. S. (2017) Shotgun Metaproteomics of Bering Strait surface water and Chukchi Sea bottom water. Biological and Chemical Oceanography Data Management Office (BCO-DMO). Version Date 2017-11-13 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/719067 [access date]
Dataset Description: <p><strong>Location:&nbsp;&nbsp;</strong>Water samples were collected in August of 2013 from the Bering Strait (BSt) chlorophyll maximum layer (7 m depth, 65°43.44″ N, 168°57.42″ W) and from the more northern Chukchi Sea (CS) bottom waters (55.5 m depth, 72°47.624″ N, 16°53.89″ W) using a 24-bottle CTD (conductivity, temperature, and depth) rosette (10 L General Oceanics Niskin X). The measurement of integrated water column chlorophyll was 226.88 mg/m2 at station BSt and 2.64 mg/m2 at station CS.</p>
<p>Water was collected on ship, filtered, and bacterial fractions were lysed, digested and analyzed using proteomic mass spectrometry.</p>
<p>Cruise = BEST Cruise 2013</p>
<p>Data are available for download at the EBI PRIDE Archive. Project number = PXD006472.</p>
<pre>
Homepage: <a href="http://www.ebi.ac.uk/pride/archive" target="_blank">http://www.ebi.ac.uk/pride/archive</a>
Project URL: <a href="http://www.ebi.ac.uk/pride/archive/projects/PXD006472" target="_blank">http://www.ebi.ac.uk/pride/archive/projects/PXD006472</a>
Data URL: <a href="http://www.ebi.ac.uk/pride/archive/projects/PXD006472/files" target="_blank">http://www.ebi.ac.uk/pride/archive/projects/PXD006472/files</a></pre>
<p>Data are published in&nbsp;May, D.H., Timmins-Schiffman, E., Mikan, M.P., Harvey, H.R., Borenstein, E., Nunn, B.L., Noble, W.S. (2016) An alignment-free "metapeptide" strategy for metaproteomic characterization of microbiome samples using shotgun metagenomic sequencing. Journal of Proteome Research 15, 2697-2705. DOI:&nbsp;<a href="http://pubs.acs.org/doi/abs/10.1021/acs.jproteome.6b00239" target="_blank">10.1021/acs.jproteome.6b00239</a></p> Methods and Sampling: <p>Water samples were collected in August of 2013 from the Bering Strait (BSt) chlorophyll maximum layer (7 m depth, 65°43.44″ N, 168°57.42″ W) and from the more northern Chukchi Sea (CS) bottom waters (55.5 m depth, 72°47.624″ N, 16°53.89″ W) using a 24-bottle CTD (conductivity, temperature, and depth) rosette (10 L General Oceanics Niskin X). The measurement of integrated water column chlorophyll was 226.88 mg/m2 at station BSt and 2.64 mg/m2 at station CS. As our previous work has shown, to examine bacterial contributions, it is essential to remove the very high background contribution from algal inhabitants.(23) Also, oceanic marine bacteria are typically smaller than bacteria in gut biomes or freshwater systems, with the majority passing a 1.0 μm filter.(24, 25) Accordingly, a 15 L water sample was prefiltered through two high-volume cartridges (10 μm and then 1 μm) to remove larger eukaryotes, and the filtrate comprising the bacterial microbiome was then collected on a glass fiber filter (GF/F) with nominal pore size of 0.7 μm. Filters were flash frozen and stored at −80 °C until extraction. Filters were sliced, and</p>
<p>&nbsp;</p>
<p>GF/F filters with the bacterial fraction were placed in 1.5 mL tubes with 100 μL of 0.5 mm glass beads, 100 μL of 6 M urea, and 500 μL of nanopure water. Filters were shaken on a bead beater for 1 min and then placed in ice for 5 min. This process was repeated 10 times to ensure cell lysis and filter breakup. A needle was then heated by flame and used to create a &lt;0.5 mm hole at the bottom of the 1.5 mL sample tube. The sample tubes were then placed atop an open 1.5 mL tube and centrifuged (3000g, 10 min). This process was completed to isolate protein lysate from extracted particles and glass beads. Protein concentrations were determined using BCA colormetric assay; 100 μg of total protein was used for digestion. Each 100 μg protein sample received 300 ng of purified human ApoA1 to monitor protein digesion. Samples were reduced, alkylated, enzymatically digested with trypsin, and desalted. Prior to MS injections, 50 fmol of the Pierce Peptide Retention Time Standard (ThermoFisher Scientific) was added to each autosample vial at 50 fmol per 2 μg of total protein.</p>
<p>Peptides were separated using an inline NanoAquity HPLC with a 4 cm precolumn (5 μm; 200A; Magic C18) and 30 cm Reprosil-Pur Basic 3 μm C18 analytical column (Dr. Maisch GmbH, Germany). Peptides were eluted using a 2–30% ACN, 0.1% formic acid nonlinear gradient in 120 min at 300 nL/min. LC-MS/MS was performed with a Q-Exactive-HF (ThermoScientific) on technical triplicates for each sample. The instrument was operated in Top 20 data-dependent acquisition mode, collecting data on 400–1600 m/z range with a 5 s dynamic exclusion.</p>
Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1233589 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1233589
onGoing
William S. Noble
University of Washington
Department of Genome Sciences Foege Building S113, 3720 15th Ave NE
Seattle
WA
98195
USA
wnoble@uw.edu
pointOfContact
Brook L. Nunn
University of Washington
206-616-9023
Department of Genome Sciences, Foege Building S113 3720 15th Ave NE
Seattle
WA
98195
USA
brookh@uw.edu
pointOfContact
asNeeded
Unknown
Repository
Project
Experiment_ID
Project_URL
10L General Oceanics Niskin X
Thermo Scientific Q-Exactive-HF
theme
None, User defined
No BCO-DMO term
project
experiment id
external_link
featureType
BCO-DMO Standard Parameters
CTD - profiler
Mass Spectrometer
instrument
BCO-DMO Standard Instruments
otherRestrictions
otherRestrictions
Access Constraints: none. Use Constraints: Please follow guidelines at: http://www.bco-dmo.org/terms-use Distribution liability: Under no circumstances shall BCO-DMO be liable for any direct, incidental, special, consequential, indirect, or punitive damages that result from the use of, or the inability to use, the materials in this data submission. If you are dissatisfied with any materials in this data submission your sole and exclusive remedy is to discontinue use.
Collaborative Research: Linking geochemistry and proteomics to reveal the impact of bacteria on protein cycling in the ocean
https://osprey.bco-dmo.org/project/675324
Collaborative Research: Linking geochemistry and proteomics to reveal the impact of bacteria on protein cycling in the ocean
<p><em>Text from NSF</em><em> award abstract:</em></p>
<p>Although proteins represent the primary source of new organic nitrogen in the ocean, the identification of individual proteins and mechanisms modulating their preservation has faced analytical and computational challenges in deciphering the vast suite of possible sequences and degradation by-products. Recent efforts to link geochemical cycling, biomedical proteomics and bioinformatics has demonstrated that only a small subset of the suite of proteins produced by marine diatoms appear to survive the degradation process, and those that do are largely protected by physical and enthalpic barriers to microbial attack. Although these discoveries help to explain the survival of individual proteins, they also generate multiple questions regarding bacteria as the dominant recyclers of organic nitrogen and carbon and needs for specific approaches to characterize modified protein products. Bacteria dominate the water column and sedimentary systems in both numbers and diversity, yet their relative contribution to the preserved proteomic pool appears low.</p>
<p>In this project, researchers at Old Dominion Universityand the University of Washington will join forces to decipher the bacterial role in protein recycling and their potential contribution. By integrating high mass accuracy tandem mass spectrometry-based proteomics with stable isotope-based geochemical analysis, they hope to identify those bacterial proteins initially synthesized during organic matter recycling. Three research objectives drive this investigation: (1) to determine the potential contribution of bacteria proteins to marine organic matter; (2) to identify those protein(s) synthesized by heterotrophic marine bacteria during initial stages of organic matter degradation; (3) to determine if glycan (carbohydrate) modifications represent an important component of preserved, yet unidentified, peptides seen in our analysis of oceanic particles and sediments.</p>
<p>Broader Impacts: This project will provide multiple opportunities for interdisciplinary student training in marine chemistry and proteomics as well as address the goal of disseminating results and tools to a broad audience. In the more traditional role, this project will expand the career for a female principal investigator in marine proteomics, support both graduate and undergraduate students at ODU which include opportunities for minority enrichment and provide training for a postdoctoral fellow at UW. On the broader level, the ODU PI participates in high school outreach programs for high achieving students in the local school which provides for summer internships and enrichment programs.</p>
<p><strong>Relevant Links:</strong></p>
<p>Old Dominion University: <a href="http://mogel.cbl.umces.edu/" target="_blank">Marine Organic Geochemistry and Ecology Laboratory (MOGEL) Lab Website</a><br />
Bering Sea Ecosystem Study: <a href="https://www.eol.ucar.edu/projects/best/" target="_blank">Data Archive</a><br />
Environmental Proteomics: <a href="http://www.environmentalproteomics.org/bacterial-degradation-of-proteins.html" target="_blank">Bacteria Recyclers in the Ocean</a><br />
Environmental Proteomics: <a href="http://www.environmentalproteomics.org/proteomics-at-subzero-temperatures.html" target="_blank">Proteomics of Colwellia psychretheca at subzero temperatures </a></p>
Bacterial Recyclers
largerWorkCitation
project
eng; USA
biota
oceans
2017-11-13
0
BCO-DMO catalogue of parameters from Shotgun Metaproteomics of Bering Strait surface water and Chukchi Sea bottom water.
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
http://lod.bco-dmo.org/id/dataset-parameter/719792.rdf
Name: Repository
Units: unitless
Description: <p>Name of database where data are currently served</p>
http://lod.bco-dmo.org/id/dataset-parameter/719793.rdf
Name: Project
Units: unitless
Description: <p>Unique project identifier for the database where data are currently served</p>
http://lod.bco-dmo.org/id/dataset-parameter/719795.rdf
Name: Experiment_ID
Units: unitless
Description: <p>unknown</p>
http://lod.bco-dmo.org/id/dataset-parameter/719796.rdf
Name: Project_URL
Units: unitless
Description: <p>Link to project page where data are currently served.</p>
GB/NERC/BODC > British Oceanographic Data Centre, Natural Environment Research Council, United Kingdom
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
210
https://datadocs.bco-dmo.org/file/3YY3gQnSR0qEjv/Metaproteomics_PRIDE_2192_May.csv
Metaproteomics_PRIDE_2192_May.csv
Primary data file for dataset ID 719067
download
https://osprey.bco-dmo.org/dataset/719067/data/download
download
onLine
dataset
<p>Water samples were collected in August of 2013 from the Bering Strait (BSt) chlorophyll maximum layer (7 m depth, 65°43.44″ N, 168°57.42″ W) and from the more northern Chukchi Sea (CS) bottom waters (55.5 m depth, 72°47.624″ N, 16°53.89″ W) using a 24-bottle CTD (conductivity, temperature, and depth) rosette (10 L General Oceanics Niskin X). The measurement of integrated water column chlorophyll was 226.88 mg/m2 at station BSt and 2.64 mg/m2 at station CS. As our previous work has shown, to examine bacterial contributions, it is essential to remove the very high background contribution from algal inhabitants.(23) Also, oceanic marine bacteria are typically smaller than bacteria in gut biomes or freshwater systems, with the majority passing a 1.0 μm filter.(24, 25) Accordingly, a 15 L water sample was prefiltered through two high-volume cartridges (10 μm and then 1 μm) to remove larger eukaryotes, and the filtrate comprising the bacterial microbiome was then collected on a glass fiber filter (GF/F) with nominal pore size of 0.7 μm. Filters were flash frozen and stored at −80 °C until extraction. Filters were sliced, and</p>
<p>&nbsp;</p>
<p>GF/F filters with the bacterial fraction were placed in 1.5 mL tubes with 100 μL of 0.5 mm glass beads, 100 μL of 6 M urea, and 500 μL of nanopure water. Filters were shaken on a bead beater for 1 min and then placed in ice for 5 min. This process was repeated 10 times to ensure cell lysis and filter breakup. A needle was then heated by flame and used to create a &lt;0.5 mm hole at the bottom of the 1.5 mL sample tube. The sample tubes were then placed atop an open 1.5 mL tube and centrifuged (3000g, 10 min). This process was completed to isolate protein lysate from extracted particles and glass beads. Protein concentrations were determined using BCA colormetric assay; 100 μg of total protein was used for digestion. Each 100 μg protein sample received 300 ng of purified human ApoA1 to monitor protein digesion. Samples were reduced, alkylated, enzymatically digested with trypsin, and desalted. Prior to MS injections, 50 fmol of the Pierce Peptide Retention Time Standard (ThermoFisher Scientific) was added to each autosample vial at 50 fmol per 2 μg of total protein.</p>
<p>Peptides were separated using an inline NanoAquity HPLC with a 4 cm precolumn (5 μm; 200A; Magic C18) and 30 cm Reprosil-Pur Basic 3 μm C18 analytical column (Dr. Maisch GmbH, Germany). Peptides were eluted using a 2–30% ACN, 0.1% formic acid nonlinear gradient in 120 min at 300 nL/min. LC-MS/MS was performed with a Q-Exactive-HF (ThermoScientific) on technical triplicates for each sample. The instrument was operated in Top 20 data-dependent acquisition mode, collecting data on 400–1600 m/z range with a 5 s dynamic exclusion.</p>
Specified by the Principal Investigator(s)
<p>All computation was performed on a Univa Grid Engine cluster with 1.90 GHz AMD Opteron processors. The MOCAT pipeline was used to assemble a metagenome and predict genes as follows. Trimmed and filtered reads from both BSt and CS samples were aligned to the human hg19 reference using SOAPaligner v2.21, and aligned reads were removed. The remaining reads were assembled into contigs and scaftigs with SOAPdenovo v1.06. The assembly was revised, correcting for indels and chimeric regions, with SOAPdenovo v1.06 and BWA v0.7.5a-r16. Genes were predicted using Prodigal v2.60. We used three well-established gene fragment prediction tools to predict gene fragments directly from shotgun metagenomic sequencing reads from each sample: MetaGeneAnnotator (in multiple species mode), FragGeneScan version 1.2.0 (illumina_10 model parameters), and Orphelia (with Net300 prediction model). Separate metapeptide databases were constructed from the BSt and CS sequencing runs, from either predicted gene fragments or raw read sequences. When starting from raw read sequences, each read was translated in all six reading frames, and reading frames containing a stop codon were discarded. The results described in section 3 were obtained by starting with predicted gene fragments from MetaGeneAnnotator. Whether starting from gene fragments or raw read sequences, amino acid sequences from each nucleotide sequence were trimmed to the first and last tryptic cleavage site (or discarded if fewer than two sites), and the remaining ends were discarded. This was done in order to remove partial tryptic peptide sequences that are unlikely to be detected by LC-MS/MS of a trypsinized metaproteome. The resulting candidate sequences were discarded if they were less than 10 amino acids long, if they contained no tryptic peptides with seven or more amino acids, or if the minimum Phred quality score over the length of the sequence was less than 30. Finally, metapeptide candidates meeting all the above criteria were discarded if they were represented by fewer than two reads. A FASTA database was constructed from the remaining metapeptides. For purposes of comparison, we also made use of a metagenome-derived database of translated genes from the metagenome described above and the NCBI nonredundant database of protein sequences from large environmental sequencing projects (‘env_nr’, downloaded from ftp://ftp.ncbi.nlm.nih.gov/blast/db/FASTA/env_nr.gz on December 1, 2015). All database searches were performed using Comet version 2015.01 rev. 2, using a concatenated decoy database in which peptide sequences were reversed but C-terminal amino acids were left in place. Search parameters included a static modification for cysteine carbamidomethylation (57.021464) and a variable modification for methionine oxidation (15.9949). Enzyme specificity was trypsin, with one missed cleavage allowed. Parent ion mass tolerance was set to 10 ppm around five isotopic peaks, and fragment ion binning was 0.02, with offset 0.0. Peptide-spectrum matches (PSMs) from all technical replicates were combined into a single data set. As described previously, after each unique peptide was associated with its top-scoring spectrum, irrespective of charge state, we used the widely used target–decoy search strategy of estimating the false discovery rate (FDR) associated with a given set of accepted peptides. In this context, the FDR is defined as the proportion of the accepted peptides that are not responsible for generating observed spectra. We then empirically examined the trade-off between FDR and the number of accepted peptides, since in practice the mass spectrometrist is typically interested in accepting as many peptides as possible while maintaining an acceptable FDR. Note that this trade-off is similar to the distinction between precision (1 – FDR) and recall or sensitivity. Results of searches of individual samples against multiple databases were integrated as follows. PSMs from searches against all databases were combined into a single tab-delimited file of features for input to Percolator. For each database, a new binary feature was added to the combined feature file indicating whether the PSM was derived from a search against that database. Percolator was then used to analyze the combined set, thereby computing a discriminant score for each PSM. For each scan with multiple PSMs (from multiple databases), all but the highest-scoring PSM were removed. Peptide-level FDR was then calculated as described above.</p>
<p>May, D.H., Timmins-Schiffman, E., Mikan, M.P., Harvey, H.R., Borenstein, E., Nunn, B.L., Noble, W.S. (2016) An alignment-free "metapeptide" strategy for metaproteomic characterization of microbiome samples using shotgun metagenomic sequencing. Journal of Proteome Research 15, 2697-2705.</p>
Specified by the Principal Investigator(s)
asNeeded
7.x-1.1
Biological and Chemical Oceanography Data Management Office (BCO-DMO)
Unavailable
508-289-2009
WHOI MS#36
Woods Hole
MA
02543
USA
info@bco-dmo.org
http://www.bco-dmo.org
Monday - Friday 8:00am - 5:00pm
For questions regarding this resource, please contact BCO-DMO via the email address provided.
pointOfContact
10L General Oceanics Niskin X
10L General Oceanics Niskin X
PI Supplied Instrument Name: 10L General Oceanics Niskin X Instrument Name: CTD - profiler Instrument Short Name: Instrument Description: The Conductivity, Temperature, Depth (CTD) unit is an integrated instrument package designed to measure the conductivity, temperature, and pressure (depth) of the water column. The instrument is lowered via cable through the water column. It permits scientists to observe the physical properties in real-time via a conducting cable, which is typically connected to a CTD to a deck unit and computer on a ship. The CTD is often configured with additional optional sensors including fluorometers, transmissometers and/or radiometers. It is often combined with a Rosette of water sampling bottles (e.g. Niskin, GO-FLO) for collecting discrete water samples during the cast.
This term applies to profiling CTDs. For fixed CTDs, see https://www.bco-dmo.org/instrument/869934. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/130/
Thermo Scientific Q-Exactive-HF
Thermo Scientific Q-Exactive-HF
PI Supplied Instrument Name: Thermo Scientific Q-Exactive-HF Instrument Name: Mass Spectrometer Instrument Short Name:Mass Spec Instrument Description: General term for instruments used to measure the mass-to-charge ratio of ions; generally used to find the composition of a sample by generating a mass spectrum representing the masses of sample components. Community Standard Description: http://vocab.nerc.ac.uk/collection/L05/current/LAB16/