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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/883989.rdf" xlink:actuate="onRequest">Thorium-234 data from SalpPOOP cruise on the R/V Tangaroa to the Chatham Rise (subtropical and subantarctic waters) in October and November 2018</gmx:Anchor>
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        <gco:CharacterString>Methods and Sampling: &amp;lt;p&amp;gt;This dataset represents water column Thorium-234 data from the SalpPOOP, Tangaroa Cruise 1810 (aka&amp;amp;nbsp;SalpPOOP cruise). Salinity and density were measured using a CTD.&amp;amp;nbsp; 4-liter (L) samples for total water-column 234Th activity were collected using CTD bottles at approximately 12 depths from the surface to approximately 300 meters.&amp;amp;nbsp; Samples were acidified with nitric acid to a pH &amp;amp;lt; 2,&amp;amp;nbsp;and a Th-230 tracer spike was added.&amp;amp;nbsp; Samples were shaken and allowed to equilibrate for 4 to 9 hours.&amp;amp;nbsp; Samples were then re-basified with ammonium hydroxide to a pH of 8-9, shaken, and allowed to equilibrate for more than 8 hours.&amp;amp;nbsp; Samples were then vacuum filtered at high vacuum pressure through a quartz (QMA) filter.&amp;amp;nbsp; Filters were mounted in RISO planchets and counted on a RISO low-level beta multi-counter at Palmer Station, Antarctica.&amp;amp;nbsp; Following a background count &amp;amp;gt; 6 months later, samples were dissolved in 8M nitric acid / 10% hydrogen peroxide solution and a Th-229 tracer spike was added.&amp;amp;nbsp; Samples were then analyzed on an ICP-MS to quantify the Th-229:Th-230 ratio, which was used to calculate the initial precipitation and filtration yield of Th-234.&amp;amp;nbsp; Protocols from Pike et al. (2005) were followed.&amp;amp;nbsp;&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;For additional sampling details see Decima et al. (in review, Nat. Comm.).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/754877.rdf" xlink:title="OCE-1756465" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1756465 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1756465</gmx:Anchor>
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Salps are unique open-ocean animals that range in size from a few millimeters to greater than twenty centimeters, have a gelatinous (jelly-like) body, and can form long chains of many connected individuals. These oceanic organisms act as oceanic vacuum cleaners, having incredibly high feeding rates on phytoplankton and, unusual for consumers of their size, smaller bacteria-sized prey. This rapid feeding and the salps' tendency to form dense blooms, allows them move substantial amounts of prey carbon from the surface into the deep ocean, leading to carbon dioxide removal from the atmosphere. However, salps are often considered a trophic dead-end, rather than a link, in the food web due to the assumption that they themselves are not consumed, since their gelatinous bodies are less nutritious than co-occurring crustacean prey. Along with this, salp populations are hypothesized to be increasing due to climate change. This proposal addresses these questions: 1) Do salps compete primarily with crustaceans (as in the prevailing paradigm) or are they competitors of single-celled protists, which are the dominant grazers of small phytoplankton? 2) Do salp blooms increase the efficiency of food-web pathways from tiny phytoplankton to fisheries production in nutrient-poor ocean regions?&lt;/p&gt;
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