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            <gco:CharacterString>Cite this dataset as: Troccoli, L., Diaz-Ramos, R., Subero-Pino, S., Muller-Karger, F., Astor, Y., Varela, R., Rueda-Roa, D., Klein, E. (2019) Time-Series of Phytoplankton Taxonomy and Density collected by the CARIACO Ocean Time-Series Project from November 1995 to January 2017. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 1) Version Date 2019-08-14 [if applicable, indicate subset used]. doi:10.1575/1912/bco-dmo.3095.1 [access date]</gco:CharacterString>
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        <gco:CharacterString>CARIACO time series Phytoplankton taxonomy from samples collected during CTD/Niskin casts Dataset Description: &amp;lt;p&amp;gt;The CARIACO Ocean Time-Series Program (formerly known as CArbon Retention In A Colored Ocean) started on November 1995 (CAR-001) and ended on January 2017 (CAR-232). Monthly cruises were conducted to the CARIACO station (10.50° N, 64.67° W) onboard the R/V Hermano Ginés of the Fundación La Salle de Ciencias Naturales de Venezuela. The program studied the relationship between surface primary production, physical forcing variables like the wind, and the settling flux of particulate carbon in the Cariaco Basin. This depression, located on the continental shelf of Venezuela, shows marked seasonal and interannual variation in hydrographic properties and primary production (carbon fixation rates by photosynthesis of planktonic algae).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;One of the monthly measurements taken by the program was water sampling at different depths for phytoplankton taxonomy (occurrence and density). Those water samples were collected with Niskin bottles during the first CTD Cast of the morning at 1, 7, 25, 35, 75, and 100 m depth. Phytoplankton taxonomy and density was determined at each depth at the level of species or genera. Values of zero are real and denote that a specific species was not found at that cruise/depth.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Web page of the CARIACO Ocean Time-Series Program: http://imars.usf.edu/cariaco&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;A complete list of publications from the CARIACO Ocean Time-Series project can be found at: http://imars.usf.edu/view/biblio/803738/year&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;These data were also funded by the following awards:&amp;lt;br /&amp;gt;
- 23914: Ley Orgánica de Ciencia, Tecnología e Innovación, LOCTI (Estación de Investigaciones Marinas), Venezuela.&amp;lt;br /&amp;gt;
- 2011000353: Inter-American Institute for Global Change Research, IAI (IAI-CRN3094).&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Water was collected with a SeaBird rosette equipped with 12 (8 liter) teflon-coated Niskin bottles (bottle springs were also teflon-coated) at different depths. Water samples for phytoplankton taxonomy analysis were usually collected during the first CTD/Niskin Cast of the morning for the following depths: 1, 7, 25, 35, 75, and 100 m.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;The determination of microalgal taxonomy and abundance was carried out at the Laboratory of Phytoplankton of the Instituto Oceanográfico de Venezuela, Universidad de Oriente (Cumana, Venezuela), according to the Utermöhl sedimentation method that is described by Edler and Elbrächter (2010). Phytoplankton species were identified according to the works of Cupp (1943), Hasle et al. (1997), Berard-Thierrault et al. (1999) and Tenenbaum (2006).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54693.rdf" xlink:title="OCE-9401537" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9401537 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9401537</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54756.rdf" xlink:title="OCE-9729697" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9729697 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9729697</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54791.rdf" xlink:title="OCE-0326268" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0326268 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0326268</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54802.rdf" xlink:title="OCE-9216626" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9216626 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9216626</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54828.rdf" xlink:title="OCE-9711318" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9711318 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9711318</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54833.rdf" xlink:title="NAS5-97128" xlink:actuate="onRequest">Funding provided by National Aeronautics &amp; Space Administration (NASA) Award Number: NAS5-97128</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54835.rdf" xlink:title="OCE-9415790" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9415790 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9415790</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54840.rdf" xlink:title="OCE-9729284" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-9729284 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=9729284</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54868.rdf" xlink:title="NAG5-6448" xlink:actuate="onRequest">Funding provided by National Aeronautics &amp; Space Administration (NASA) Award Number: NAG5-6448</gmx:Anchor>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54895.rdf" xlink:title="OCE-0963028" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0963028 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0963028</gmx:Anchor>
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                            <gco:CharacterString>Program description text taken from Chapter 1: Introduction from the Global Intercomparability in a Changing Ocean: An International Time-Series Methods Workshop report published following the workshop held November 28-30, 2012 at the Bermuda Institute of Ocean Sciences. The full report is available from the workshop Web site hosted by US OCB: http://www.whoi.edu/website/TS-workshop/home
Decades of research have demonstrated that the ocean varies across a range of time scales, with anthropogenic forcing contributing an added layer of complexity. In a growing effort to distinguish between natural and human-induced earth system variability, sustained ocean time-series measurements have taken on a renewed importance. Shipboard biogeochemical time-series represent one of the most valuable tools scientists have to characterize and quantify ocean carbon fluxes and biogeochemical processes and their links to changing climate (Karl, 2010; Chavez et al., 2011; Church et al., 2013). They provide the oceanographic community with the long, temporally resolved datasets needed to characterize ocean climate, biogeochemistry, and ecosystem change.
The temporal scale of shifts in marine ecosystem variations in response to climate change are on the order of several decades.  The long-term, consistent and comprehensive monitoring programs conducted by time-series sites are essential to understand large-scale atmosphere-ocean interactions that occur on interannual to decadal time scales.  Ocean time-series represent one of the most valuable tools scientists have to characterize and quantify ocean carbon fluxes and biogeochemical processes and their links to changing climate.
Launched in the late 1980s, the US JGOFS (Joint Global Ocean Flux Study; http://usjgofs.whoi.edu) research program initiated two time-series measurement programs at Hawaii and Bermuda (HOT and BATS, respectively) to measure key oceanographic measurements in oligotrophic waters. Begun in 1995 as part of the US JGOFS Synthesis and Modeling Project, the CARIACO Ocean Time-Series (formerly known as the CArbon Retention In A Colored Ocean) Program has studied the relationship between surface primary production, physical forcing variables like the wind, and the settling flux of particulate carbon in the Cariaco Basin.
The objective of these time-series effort is to provide well-sampled seasonal resolution of biogeochemical variability at a limited number of ocean observatories, provide support and background measurements for process-oriented research, as well as test and validate observations for biogeochemical models. Since their creation, the BATS, CARIACO and HOT time-series site data have been available for use by a large community of researchers.
 
Data from those three US funded, ship-based, time-series sites can be accessed at each site directly or by selecting the site name from the Projects section below.
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                            <gco:CharacterString>&lt;p&gt;Since 1995, the CARIACO Ocean Time-Series (formerly known as the CArbon Retention In A Colored Ocean) Program has studied the relationship between surface primary production, physical forcing variables like the wind, and the settling flux of particulate carbon in the Cariaco Basin. This depression, located on the continental shelf of Venezuela (Map), shows marked seasonal and interannual variation in hydrographic properties and primary production (carbon fixation rates by photosynthesis of planktonic algae).&lt;/p&gt;
&lt;p&gt;This peculiar basin is anoxic below ~250 m, due its restricted circulation and high primary production &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Muller-Karger-2001&quot;&gt;(Muller-Karger et al., 2001)&lt;/a&gt;. CARIACO observations show annual primary production rates exceed 500 gC/m&lt;sup&gt;2&lt;/sup&gt;y, of which over 15-20% can be accounted for by events lasting one month or less. Such events are observed in other locations where time series observations are collected, and suggest that prior estimates of regional production based on limited sampling may have been underestimated. The annual primary production rates in the Cariaco Basin are comparable to rates estimated using time series observations for Monterey Bay (460 gC/m&lt;sup&gt;2&lt;/sup&gt;y; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Chavez&quot;&gt;Chavez, 1996&lt;/a&gt;), and higher than previous rates estimated for Georges Bank, the New York Shelf, and the Oregon Shelf (380, 300, and 190 gC/m&lt;sup&gt;2&lt;/sup&gt;y, respectively; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Walsh-1988&quot;&gt;Walsh, 1988&lt;/a&gt;).&lt;/p&gt;
&lt;p&gt;The Cariaco Basin has long been the center of attention of scientists trying to explain paleoclimate. Due to its high rates of sedimentation (30 to &amp;gt;100 cm/ky; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Peterson-2000&quot;&gt;Peterson et al., 2000&lt;/a&gt;) and excellent preservation, the varved sediments of the Cariaco Basin offer the opportunity to study high resolution paleoclimate and better understand the role of the tropics in global climate change ( &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Black&quot;&gt;Black et al., 1999;&lt;/a&gt; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Peterson-2000&quot;&gt;Peterson et al., 2000;&lt;/a&gt; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Haug-2001&quot;&gt;Haug et al., 2001;&lt;/a&gt; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Black-2004&quot;&gt;Black et al., 2004;&lt;/a&gt; &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Hughen-2004&quot;&gt;Hughen et al., 2004&lt;/a&gt; ).&lt;/p&gt;
&lt;p&gt;Now, the CARIACO program provides a link between the sediment record and processes near the surface of the ocean. Sediment traps maintained by the CARIACO program show that over 5% of autochtonous material reaches 275 m depth, and that nearly 2% reaches 1,400 m. The significance of this flux is that it represents a sink for carbon and that it helps explain the record of ancient climate stored at the bottom of the Cariaco Basin.&lt;/p&gt;
&lt;p&gt;Acknowledgements: This work was supported by the National Science Foundation (NSF), the National Aeronautics and Space Administration (NASA), and Venezuela's Fondo Nacional de Ciencia, Tecnología e Innovación (FONACIT). For more information please see this &lt;a href=&quot;http://www.imars.usf.edu/CAR/ar.html#Acknowledgments&quot;&gt;Acknowledgements&lt;/a&gt; link.&lt;/p&gt;</gco:CharacterString>
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            <gmi:type>
              <gmi:MI_OperationTypeCode codeList="https://data.noaa.gov/resources/iso19139/schema/resources/Codelist/gmxCodelists.xml#MI_OperationTypeCode" codeListValue="real"/>
            </gmi:type>
            <gmi:parentOperation gco:nilReason="inapplicable"/>
            <gmi:platform>
  <gmi:MI_Platform>
    <gmi:identifier>
      <gmd:MD_Identifier>
        <gmd:code>
          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54065.rdf"
           xlink:actuate="onRequest">B/O Hermano Gines</gmx:Anchor>
        </gmd:code>
      </gmd:MD_Identifier>
    </gmi:identifier>
    <gmi:description>
      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54065.rdf" xlink:title="B/O Hermano Gines" xlink:actuate="onRequest">vessel</gmx:Anchor>
    </gmi:description>
    <gmi:instrument gco:nilReason="unknown"/>
  </gmi:MI_Platform>
</gmi:platform>
            </gmi:MI_Operation>
      </gmi:operation><gmi:platform>
  <gmi:MI_Platform>
    <gmi:identifier>
      <gmd:MD_Identifier>
        <gmd:code>
          <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54065.rdf"
           xlink:actuate="onRequest">B/O Hermano Gines</gmx:Anchor>
        </gmd:code>
      </gmd:MD_Identifier>
    </gmi:identifier>
    <gmi:description>
      <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/platform/54065.rdf" xlink:title="B/O Hermano Gines" xlink:actuate="onRequest">vessel</gmx:Anchor>
    </gmi:description>
    <gmi:instrument gco:nilReason="unknown"/>
  </gmi:MI_Platform>
</gmi:platform>
          </gmi:MI_AcquisitionInformation>
  </gmi:acquisitionInformation>
</gmi:MI_Metadata>
