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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/3789.rdf" xlink:actuate="onRequest">CTD data, bottle nutrients, and chlorophyll-a from phytoplankton taxa from R/V Pelican PE08-54, PE09-12, PE10-01 in the Northwest Florida shelf off Panama City FL. from 2008-2009 (BenDiM project)</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Kamykowski, D. (2012) CTD data, bottle nutrients, and chlorophyll-a from phytoplankton taxa from R/V Pelican PE08-54, PE09-12, PE10-01 in the Northwest Florida shelf off Panama City FL. from 2008-2009 (BenDiM project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). Version Date 2012-11-21 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/3789 [access date]</gco:CharacterString>
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        <gco:CharacterString>CTD data, bottle nutrients, and the contribution to total Chlorophyl-a by phytoplankton taxa Dataset Description: &amp;lt;p&amp;gt;CTD data, bottle nutrients, and the contribution to total Chlorophyl-a by phytoplankton taxa.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;At each hydrographic station, The R/V Pelican&amp;amp;rsquo;s SeaBird CTD provided  profiles for light attenuation, pressure, temperature, salinity,  dissolved oxygen, chlorophyll fluorescence and turbidity during the  first downcast. Beam-t measurements obtained from the CTD  transmissometer were used to approximate potential PAR attenuation based  on the sequential application of the percent transmission through  successive 1 m layers of the water column. A Secchi disc was attached to  the top of the CTD (2009).&amp;amp;nbsp;&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;A SeaBird Rosette on the CTD was configured with eleven 5 L Niskin  bottles that were triggered during the first upcast near the sediment  interface and then at 2 m intervals (~9 bottles) as well as mid-depth in  the remaining water column to the surface (1 bottle) and at the surface  (1 bottle).&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;The seawater collected by the Rosette was used for nitrate-nitrite  (NO3- + NO2-) analyses and HPLC pigment determinations. In May 2008,  phosphate (PO4) and silicate (SiO4) were also measured.&amp;amp;nbsp; For nutrient  samples, 10 ml of the filtered seawater were frozen immediately after  collection and returned to NCSU for laboratory analyses. In the  laboratory, these samples were thawed and analyzed against a standard of  natural seawater with low nitrate concentrations. NO3- + NO2-&amp;amp;nbsp; were  determined colorimetrically at NCSU using an automated QuAAtro  Continuous-Flow Analysis system. Precision of the NO3- + NO2- analysis  was 0.1 &amp;amp;micro;M with a detection limit of 1.4 &amp;amp;micro;M.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;For High-Performance Liquid Chromatography (HPLC) analysis,  approximately 1000 ml of water from selected sample depths were filtered  through a 2.5 cm diameter GF-F filters under a low pressure vacuum  (&amp;amp;lt; 200 mmHg). The filters were frozen with liquid nitrogen and stored  for 6-9 months. In the laboratory of Dr. J. L. Pinckney (USC), excess  water was removed and the filters for HPLC analysis were analyzed in the  dark on a Shimadzu dual LC10-AT vp and Controller SCL-10A vs binary  gradient pump. Pigments on the filters were extracted after they were  allowed to incubate for 18-24 hours in an acetone solution. The  supernatant separated from the filter was extracted and inserted into  smaller amber vials. The HPLC analysis was run with solvent A of 80%  methanol and 20% ammonium acetate and a solvent B of 80% methanol and  20% acetone. Spectra measurements between 380-700 nm were taken every 2  seconds and peaks were identified based on retention time. CHEMTAX, a  matrix factorization program, was used to optimize the contribution of  the selected groups to total Chl a. The taxonomic groups,  dinoflagellates (both gyroxanthin and peridinin types), and diatoms in  May 2008, plus chlorophytes, cyanobacteria, cryptophytes, chrysophytes,  and prymnesiophytes in Oct. 2008 and 2009, were selected according to  the 'hierarchical guide to interpreting pigment data'.&amp;amp;nbsp; Initial pigment  ratios were selected from the literature and regional studies. The  initial pigment ratio was optimized using multiple randomly generated  starting points as seed values.&amp;amp;nbsp; Output ratios from the previous runs  were used as input values for successive runs. Values are reported here  as absolute chlorophyll units.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/55111.rdf" xlink:title="OCE-0726271" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0726271 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0726271</gmx:Anchor>
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	Name: cruise_id
	Units: text
	Description: &lt;p&gt;cruise identification, official name in R2R catalog (&lt;a href=&quot;http://www.rvdata.us/&quot;&gt;http://www.rvdata.us/&lt;/a&gt;)&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30902.rdf
	Name: taxon
	Units: text
	Description: &lt;p&gt;plankton taxonomic name&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30903.rdf
	Name: station
	Units: integer
	Description: &lt;p&gt;station number&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30904.rdf
	Name: date
	Units: mm/dd/yyyy
	Description: &lt;p&gt;date of transect, gmt&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30905.rdf
	Name: time
	Units: HHMM
	Description: &lt;p&gt;time of transect, gmt&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30906.rdf
	Name: lat
	Units: decimal degrees
	Description: &lt;p&gt;latitude; North is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30907.rdf
	Name: lon
	Units: decimal degrees
	Description: &lt;p&gt;longitude; East is positive&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30908.rdf
	Name: pres
	Units: decibars
	Description: &lt;p&gt;pressure&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30909.rdf
	Name: depth
	Units: meters
	Description: &lt;p&gt;depth &lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30910.rdf
	Name: temp
	Units: degrees Celsius
	Description: &lt;p&gt;seawater temperature&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30911.rdf
	Name: sal
	Units: dimensionless; salinity units
	Description: &lt;p&gt;salinity on Practical Salinity Scale&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30912.rdf
	Name: sigma_0
	Units: kg/m^3
	Description: &lt;p&gt;Potential density, Sigma-theta is denoted 'sigma_0', where the last digit, a zero, is used to represent the Greek letter theta. This altered density which takes into account adiabatic heating/cooling with changes in pressure is called the 'potential density'.&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30913.rdf
	Name: spar
	Units: micro-Einsteins/m2.s
	Description: &lt;p&gt;Surface Photosynthetically Available [Active] Radiation; surface irradiance&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30914.rdf
	Name: dpar
	Units: microEinsteins/m2.s
	Description: &lt;p&gt;PAR at depth&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30915.rdf
	Name: O2_sat_pcent
	Units: %
	Description: &lt;p&gt;percent oxygen saturation&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30916.rdf
	Name: O2
	Units: milliliters/liter
	Description: &lt;p&gt;dissolved oxygen&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30917.rdf
	Name: fluor
	Units: milligrams/meter^3
	Description: &lt;p&gt;fluorescence&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30918.rdf
	Name: beamt
	Units: 1/m^2
	Description: &lt;p&gt;attenuation (loss of light) of a narrow well collimated beam of light; beam attenuation due to particles&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30919.rdf
	Name: secchi
	Units: Formazin Turbidity Units (FTU)
	Description: &lt;p&gt;Turbidity as measured by a Secchi disk&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30920.rdf
	Name: NO3_NO2
	Units: micromoles/liter
	Description: &lt;p&gt;nitrates plus nitrites in phytoplankton sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30921.rdf
	Name: PO4
	Units: micromoles/liter
	Description: &lt;p&gt;phosphates&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30922.rdf
	Name: SiO4
	Units: micromoles/liter
	Description: &lt;p&gt;silicate&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30923.rdf
	Name: chl_a
	Units: micrograms chl a /liter
	Description: &lt;p&gt;total chlorophyll-a of the bottle sample&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/30924.rdf
	Name: chla_taxon
	Units: micrograms chl a /liter
	Description: &lt;p&gt;chlorophyll-a  contribution by the specific taxon&lt;/p&gt; 
http://lod.bco-dmo.org/id/dataset-parameter/34062.rdf
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&amp;lt;p&amp;gt;The seawater collected by the Rosette was used for nitrate-nitrite  (NO3- + NO2-) analyses and HPLC pigment determinations. In May 2008,  phosphate (PO4) and silicate (SiO4) were also measured.&amp;amp;nbsp; For nutrient  samples, 10 ml of the filtered seawater were frozen immediately after  collection and returned to NCSU for laboratory analyses. In the  laboratory, these samples were thawed and analyzed against a standard of  natural seawater with low nitrate concentrations. NO3- + NO2-&amp;amp;nbsp; were  determined colorimetrically at NCSU using an automated QuAAtro  Continuous-Flow Analysis system. Precision of the NO3- + NO2- analysis  was 0.1 &amp;amp;micro;M with a detection limit of 1.4 &amp;amp;micro;M.&amp;lt;/p&amp;gt;
&amp;lt;p&amp;gt;For High-Performance Liquid Chromatography (HPLC) analysis,  approximately 1000 ml of water from selected sample depths were filtered  through a 2.5 cm diameter GF-F filters under a low pressure vacuum  (&amp;amp;lt; 200 mmHg). The filters were frozen with liquid nitrogen and stored  for 6-9 months. In the laboratory of Dr. J. L. Pinckney (USC), excess  water was removed and the filters for HPLC analysis were analyzed in the  dark on a Shimadzu dual LC10-AT vp and Controller SCL-10A vs binary  gradient pump. Pigments on the filters were extracted after they were  allowed to incubate for 18-24 hours in an acetone solution. The  supernatant separated from the filter was extracted and inserted into  smaller amber vials. The HPLC analysis was run with solvent A of 80%  methanol and 20% ammonium acetate and a solvent B of 80% methanol and  20% acetone. Spectra measurements between 380-700 nm were taken every 2  seconds and peaks were identified based on retention time. CHEMTAX, a  matrix factorization program, was used to optimize the contribution of  the selected groups to total Chl a. The taxonomic groups,  dinoflagellates (both gyroxanthin and peridinin types), and diatoms in  May 2008, plus chlorophytes, cyanobacteria, cryptophytes, chrysophytes,  and prymnesiophytes in Oct. 2008 and 2009, were selected according to  the 'hierarchical guide to interpreting pigment data'.&amp;amp;nbsp; Initial pigment  ratios were selected from the literature and regional studies. The  initial pigment ratio was optimized using multiple randomly generated  starting points as seed values.&amp;amp;nbsp; Output ratios from the previous runs  were used as input values for successive runs. Values are reported here  as absolute chlorophyll units.&amp;lt;/p&amp;gt;</gco:CharacterString>
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