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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/543286.rdf" xlink:actuate="onRequest">Physical and chemical metadata for microbiological samples from R/V New Horizon cruises GoCAL1, GoCAL2, GoCAL3 in the Guaymas Basin, Gulf of California from 2004-2005 (Guaymas plumes project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Dick, G. J. (2021) Physical and chemical metadata for microbiological samples from R/V New Horizon cruises GoCAL1, GoCAL2, GoCAL3 in the Guaymas Basin, Gulf of California from 2004-2005 (Guaymas plumes project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2014-12-19 [if applicable, indicate subset used]. doi:10.26008/1912/bco-dmo.543286.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>Physical and chemical metadata for microbiological samples from Guaymas Basin plumes. Dataset Description: &amp;lt;p&amp;gt;Physical and chemical metadata (sal, Mn, O2, temp, etc.) for microbiological samples from Guyamas Basin plumes.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;&amp;lt;em&amp;gt;The following publications are associated with this data:&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
Anantharaman, K.A., M.B. Duhaime, J.A. Breier, K. Wendt, B.M. Toner, and G.J. Dick (2014). Sulfur oxidation genes in diverse deep-sea viruses. Science 344: 757-760. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1126/science.1252229&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1126/science.1252229 &amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Li, M., B.M. Toner, B.J. Baker, J.A. Breier, C.S. Sheik, and G.J. Dick (2014). Microbial iron uptake as a mechanism for dispersing iron from deep-sea hydrothermal vents. Nature Communications 5: 3192. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1038/ncomms4192&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1038/ncomms4192&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Li, M., S. Jain, B.J. Baker, C. Taylor, and G.J. Dick (2014). Novel hydrocarbon monooxygenase genes in the metatranscriptome of a natural deep-sea hydrocarbon plume. Environmental Microbiology 16: 60-71. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1111/1462-2920.12182&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1111/1462-2920.12182&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Sheik, C.S. 2, S. Jain, and G.J. Dick (2014). Metabolic flexibility of enigmatic SAR324 revealed through metagenomics and metatranscriptomics. Environmental Microbiology 16: 304-317. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1111/1462-2920.12165&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1111/1462-2920.12165&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Baker, B.J., C.S. Sheik, C.A. Taylor, S. Jain, A. Bhasi, J.D. Cavalcoli, and G.J. Dick (2013). Community transcriptomic assembly reveals microbes that contribute to deep-sea carbon and nitrogen cycling. The ISME Journal 7: 1962-1973. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1038/ismej.2013.85&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1038/ismej.2013.85&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Dick, G.J., K. Anantharaman, B.J. Baker, M. Li, D.C. Reed, and C.S. Sheik (2013). Hydrothermal vent plume microbiology: ecological and biogeographic linkages to seafloor and water column habitats. Frontiers in Microbiology 4: 124. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.3389/fmicb.2013.00124&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.3389/fmicb.2013.00124 &amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Anantharaman, K., J.A. Breier, C.S. Sheik, and G.J. Dick (2013). Evidence for hydrogen oxidation and metabolic plasticity in widespread deep-sea bacteria. Proceedings of the National Academy of Sciences 110: 330-335. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1073/pnas.1215340110&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1073/pnas.1215340110&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Baker, B.J., R.A. Lesniewski, and G.J. Dick. Genome-enabled transcriptomics reveals archaeal populations that drive nitrification in a deep-sea hydrothermal plume (2012). The ISME Journal 6: 2269-2279. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1038/ismej.2012.64&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1038/ismej.2012.64&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Lesniewski, R.A., S. Jain, P.D. Schloss, K. Anantharaman,and G.J. Dick (2012). The metatranscriptome of a deep-sea hydrothermal plume is dominated by water column methanotrophs and chemolithotrophs. The ISME Journal 6: 2257-2268. doi:&amp;lt;a href=&amp;quot;http://dx.doi.org/10.1038/ismej.2012.63&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;10.1038/ismej.2012.63&amp;lt;/a&amp;gt;&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Hydrothermal plumes were detected by turbidity anomalies as measured by an air-calibrated transmissometer (WetLabs) on a CTD rosette (Sea-Bird). Water samples were collected in 10-L niskin bottles by CTD Rosette (Sea-Bird).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Samples were transferred from niskin bottles to acidwashed 50 mL polypropylene tubes. Samples for dissolved Mn (dMn) were filtered through 0.2 um acid-washed nucleopore polycarbonate filters within 1 h of collection. Filtrate (dMn) and unfiltered total Mn samples (tMn) were stabilized by acidification acidification with Optima grade nitric acid to a pH of &amp;amp;lt;2 and stored at 4 degrees C until analysis. All shipboard manipulations were performed in a laminar flow hood with clean techniques. Mn concentrations were determined on a Thermoquest Finnigan Element 2 double focusing, single collector, magnetic sector inductively coupled plasma mass spectrometer (ICP-MS) at the SIO unified laboratory analytical facility. ICP-MS was done at low resolution following instrument and induction parameters described previously (Field et al., 1999). Samples were diluted 1:50 in 2% nitric acid in quartz-distilled (QD) water prior to analysis. A calibration curve was prepared as described previously (Rodushkin and Ruth, 1998) using matrix-matched external standards made with 2% natural seawater stripped of metals by precipitation with Optima ammonium hydroxide. Indium (1 ppb) was used as an internal standard in all standards and samples. Standard additions (Willard et al., 1965) were used to rule out a matrix effect. To confirm analytical accuracy, reference waters CASS-4 and NASS-5 (Verplank et al., 2001) were included in the analysis as samples. Our experimentally determined average Mn concentration for CASS was 56 ± 10 nM (reported to be 51 nM) and for NASS-5 it was16 ± 8 nM (reported to be 17 nM). Six samples from station 1 were collected, processed and analyzed in duplicate. The average standard deviation was 8 nM, which includes variation due to both sampling and analytical error.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/542708.rdf" xlink:title="OCE-1029242" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1029242 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1029242</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/544200.rdf" xlink:title="GBMF2609" xlink:actuate="onRequest">Funding provided by Gordon and Betty Moore Foundation (GBMF) Award Number: GBMF2609 Award URL: http://www.moore.org/grants/list/GBMF2609</gmx:Anchor>
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