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All cruises were conducted as part of the larger BATS program and sampled at least monthly with biweekly sampling between February and April. This sampling strategy has been successful in revealing the major temporal microbial and biogeochemical patterns at this site (Carlson and Ducklow, 1996;\u00a0Steinberg et al., 2001;\u00a0Morris et al., 2005;\u00a0Carlson et al., 2009;\u00a0Treusch et al., 2009;\u00a0Lomas et al., 2010). A broader assessment of the BATS biogeochemical data is presented in\u00a0Deep Sea Research II\u00a0in 1996 (volume 43, issues 2\u20133) and 2001 (volume 48, issues 8\u20139).</p>\n<p>Samples for virioplankton (0, 20, 40, 60, 80, 100, 140, 160, 200, 250 and 300\u2009m) and bacterioplankton (0, 10, 20, 40, 60, 80, 100, 120, 140, 160, 200, 250 and 300\u2009m) were collected at the BATS site from January 2000 to December 2009 via conductivity, temperature, depth profiling rosette equipped with 12\u2009l Niskin bottles. The 120\u2009m virioplankton sample was added after October 2007. Throughout the entire time-series, all virioplankton samples were fixed with 0.02\u2009um filtered formalin (1% final concentration), placed in 5\u2009ml cryovials and flash frozen in liquid nitrogen (Wen et al., 2004) until processing (within 12 weeks of collection). Samples for bacterioplankton abundance were fixed with 0.2\u2009um filtered gluteraldehyde (1% final concentration) and stored at either 4\u2009\u00b0C for 72\u2009h or flash frozen and subsequently stored at \u221280\u2009\u00b0C for up to 6 months until processing as described in\u00a0Steinberg et al (2001). Storage tests demonstrated no appreciable loss of virioplankton or bacterioplankton abundance when stored in liquid nitrogen for periods up to 6 months (unpublished data). Picophytoplankton samples were collected at the same depths through 250\u2009m from October 2001 to December 2009 (Casey et al., 2007). Samples for fluorescence\u00a0in situ\u00a0hybridization (FISH) of specific heterotrophic bacterioplankton lineages were collected from the upper 300\u2009m from January 2003 to December 2005 (Carlson et al., 2009).</p>\n<p>Biogeochemical and physical data collected at the BATS site are available at\u00a0<a href=\"http://bats.bios.edu\">http://bats.bios.edu</a>. The MLD was determined as the depth where potential density (sigma-t) of the water was equal to sea surface sigma-t\u00a0plus the equivalent in sigma-t\u00a0to a 0.2\u2009\u00b0C decrease in temperature (Sprintall and Tomczak, 1992). Contour plots were created in Ocean Data View (R Schlitzer,\u00a0<a href=\"http://odv.awi.de/\">http://odv.awi.de/</a>) with VG Gridding and linear mapping adjusted to the median of each data set. Statistics (Pearson's correlation and two-tailed Student's\u00a0t-test for unequal variances), ratios and percent contributions were determined using Microsoft Excel.</p>\n<p>Virioplankton abundance:<br />\nVirioplankton abundance was enumerated according to the methods of\u00a0Noble and Fuhrman (1998). Briefly, water samples were filtered on to 0.02\u2009um Anodisc aluminum oxide filters (Whatman, Kent, UK), stained with SYBR Green I (Molecular Probes Inc., Eugene, OR, USA), and enumerated via epifluorescence microscopy using an Olympus AX70 microscope (Olympus, Tokyo, Japan) equipped with a Toshiba CCD video camera (Irvine, CA, USA) and Pro-series Capture Kit version 4.5 (I-CUBE, Crofton, MD, USA). Ten images from each sample were processed with scripts written in Image Pro Plus (Media Cybernetics, Bethesda, MD, USA) for particles sized 0.01\u20130.27\u2009um2, using the clean borders function (cells touching the edge of the image or grid were omitted). We consider these estimates of viral abundance conservative because it is possible that some viral particles less than one pixel were omitted from the final count. We performed pairwise comparisons of automated versus manual enumeration of virioplankton abundance to determine any discrepancies between the two approaches. Samples collected along a gradient from offshore (BATS;\u00a0n=92) to onshore waters of Bermuda (n=32) were highly correlated with automated counts being slightly greater than manual counts (slope=1.07,\u00a0r=0.99,\u00a0n=134). The lower estimates of viral abundance from manual counts may have resulted from image fading during enumeration and/or operator fatigue. We argue that for this study, the automated image analysis was the most reliable approach for viral particle enumeration. The coefficient of variation for the automated counts averaged 11% (n=1517).</p></div>","@type":"rdf:HTML"}],"http://ocean-data.org/schema/hasBriefDescription":[{"@value":"Virioplankton abundance at BATS site, 2000-2011","@language":"en-US"}],"http://purl.org/dc/terms/description":[{"@value":"<div><p>Virioplankton abundances were measured from samples collected from January 2000 to December 2011 as part of the larger BATS program aboard the R/V <em>Weatherbird II </em>or the R/V<em> Atlantic Explorer. </em>Supporting data provided by the BATS time-series program and are available at (<a href=\"http://bats.bbsr.edu/\">http://bats.bios.edu/)</a></p></div>","@type":"rdf:HTML"}],"http://www.w3.org/2000/01/rdf-schema#label":[{"@value":"MO - virioplankton abundance","@type":"xsd:string"}],"http://ocean-data.org/schema/hasProcessingDescription":[{"@value":"<div><p><strong>BCO-DMO Processing:</strong><br />\n- added conventional header with dataset name, PI name, version date, reference information<br />\n- renamed parameters to BCO-DMO standard<br />\n- converted longitudes to negative values to represent degrees West<br />\n- converted -999\u00a0to nd for 'no data'</p></div>","@type":"rdf:HTML"}],"http://purl.org/dc/terms/identifier":[{"@value":"543808","@type":"xsd:int"}],"http://purl.org/dc/terms/title":[{"@value":"MO - virioplankton abundance"}],"http://purl.org/dc/terms/date":[{"@value":"2014-12-23T13:13:37-05:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/created":[{"@value":"2014-12-23T13:13:37-05:00","@type":"xsd:dateTime"}],"http://purl.org/dc/terms/modified":[{"@value":"2025-03-18T21:53:52-04:00","@type":"xsd:dateTime"}],"http://rdfs.org/ns/void#inDataset":[{"@id":"http://www.bco-dmo.org/"}],"http://ocean-data.org/schema/namedGraph":[{"@value":"urn:bcodmo:dataset:543808","@type":"xsd:token"}],"http://ocean-data.org/schema/osprey_page":[{"@id":"https://osprey.bco-dmo.org/dataset/543808"}],"http://ocean-data.org/schema/identifier":[{"@id":"urn:bcodmo:osprey:v2:node:identifier:543808"}],"http://ocean-data.org/schema/datasetTitle":[{"@value":"Virioplankton abundance from multiple cruises at the Bermuda AtlanticTime Series Station (BATS), Western Sargasso Sea from 2000-2011 (Ocean Microbial Observatory project)","@language":"en-US"}],"http://ocean-data.org/schema/abstract":[{"@value":"Virioplankton abundances were measured from samples collected from January 2000 to December 2011 at the Bermuda Atlantic Time Series Station (BATS), Western Sargasso Sea, as part of the larger BATS program aboard the R/V Weatherbird II or the R/V Atlantic Explorer. Supporting data provided by the BATS time-series program and are available at (http://bats.bios.edu/).","@language":"en-US"}],"http://purl.org/dc/terms/rights":[{"@id":"https://creativecommons.org/licenses/by/4.0/"}],"http://ocean-data.org/schema/deprecated":[{"@value":"false","@type":"xsd:boolean"}],"http://ocean-data.org/schema/temporalExtent":[{"@id":"urn:bcodmo:dataset:543808:temporalExtent"}],"http://ocean-data.org/schema/spatialCoverage":[{"@id":"urn:bcodmo:dataset:543808:spatialCoverage"}],"http://purl.org/dc/terms/bibliographicCitation":[{"@value":"Carlson, C., Giovannoni, S. (2020) Virioplankton abundance from multiple cruises at the Bermuda AtlanticTime Series Station (BATS), Western Sargasso Sea from 2000-2011 (Ocean Microbial Observatory project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). 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