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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/3459.rdf" xlink:actuate="onRequest">GoMX PIT from R/V Oceanus cruise OC468-02 in the Gulf of Mexico in 2010 (GoMX - DHOS Marine Snow and Sedimentation project)</gmx:Anchor>
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                <gmx:Anchor xlink:href="https://ror.org/02t274463" xlink:title="ROR ID" xlink:actuate="onRequest">University of California-Santa Barbara</gmx:Anchor>
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                <gmx:Anchor xlink:href="https://ror.org/0270vfa57" xlink:title="ROR ID" xlink:actuate="onRequest">University of Southern Mississippi</gmx:Anchor>
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				    <gco:CharacterString>02543</gco:CharacterString>
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            <gco:CharacterString>Cite this dataset as: Passow, U., Asper, V. L., Diercks, A. R. (2011) GoMX PIT from R/V Oceanus cruise OC468-02 in the Gulf of Mexico in 2010 (GoMX - DHOS Marine Snow and Sedimentation project). Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 11 April 2011) Version Date 2011-04-11 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/3459 [access date]</gco:CharacterString>
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        <gco:CharacterString>GoMX_PIT_Oceanus_8-2010 Dataset Description: &amp;lt;p&amp;gt;Results from floating particle interceptor traps (PIT) deployed August/ September for about 36 hours each at 8 stations in the Gulf of Mexico at 150 or 180 m&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
&amp;lt;strong&amp;gt;Note: These data are restricted. Contact PI for access information.&amp;lt;/strong&amp;gt;&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;&amp;lt;u&amp;gt;&amp;lt;strong&amp;gt;GoMX Aug/ Sep 2010: PIT traps&amp;lt;/strong&amp;gt;&amp;lt;/u&amp;gt;&amp;amp;nbsp;&amp;lt;br /&amp;gt;
&amp;lt;em&amp;gt;Methods&amp;lt;/em&amp;gt;&amp;lt;br /&amp;gt;
Eight (PIT 1 &amp;amp;amp; 2, 7, &amp;amp;amp; 8) to twelve (PIT 3, 4, 5, 6) columns were attached to a cross (2-3 in each of 4 directions) attached 30 m above the weight. Above the column a bungee cord connection that buffered the wave action connected to two large benthos floats and a bead of a series of small floats with a buoy at the surface. The traps, which were suspended at 150 m depth (PIT 1 to 6) or 185 m (PIT &amp;amp;gt; 6) and drifted freely, were deployed at the beginning of each main station and recovered at the end. Deployment time varied around 36 hours, except PIT 7 where it was 24 h. Each trap column was 62.5 cm high, with baffles in the 9 top cm and a diameter of 6.96 cm (area 37.94 cm&amp;lt;sup&amp;gt;2&amp;lt;/sup&amp;gt;).&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Gels in jars fitting tightly into the columns were added at the bottom of two columns to investigate size distribution and type of sinking particles. Prior to deployment the cup with the softened gel (softened by adding a layer of 50 ‰ FSW ≥ 2 days before deployment) was fitted into the bottom of the column and overlaid first with a layer of salt-enriched water and then with FSW. The other 6 to 10 columns were filled with FSW which was under laid with 300 mL of salt-enriched water using a tube connected to a sawed off pipette.&amp;lt;br /&amp;gt;
&amp;lt;br /&amp;gt;
Upon retrieval, water was drained above the gel cups, the cups removed and stored in the fridge. The upper 2/3 of the water in the other columns was also drained after particles wee allowed to settle and the lower third of all columns mixed and used for subsequent analysis of POC, PON, Isotopes. DNA content and oil signature is analyzed for selected samples only.&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/54941.rdf" xlink:title="OCE-1045330" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-1045330 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=1045330</gmx:Anchor>
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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/51317.rdf" xlink:actuate="onRequest">Uta Passow</gmx:Anchor>
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            <gmx:Anchor xlink:href="https://ror.org/02t274463" xlink:title="ROR ID" xlink:actuate="onRequest">University of California-Santa Barbara</gmx:Anchor>
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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/50598.rdf" xlink:actuate="onRequest">Vernon L. Asper</gmx:Anchor>
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            <gmx:Anchor xlink:href="https://ror.org/0270vfa57" xlink:title="ROR ID" xlink:actuate="onRequest">University of Southern Mississippi</gmx:Anchor>
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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/person/51318.rdf" xlink:actuate="onRequest">Arne R. Diercks</gmx:Anchor>
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GOM - Broader Impacts
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&lt;p&gt;Intellectual Merit&lt;br /&gt;
The  characteristics and the potential fate of these marine snow like  aggregates, which may potentially sink or float, be grazed, degraded or  remain suspended in the water for a long period of time, is unknown.  This accident is an opportunity to evaluate and expand our knowledge on  reactions of marine ecosystems to such large disturbances in general and  more specifically to study the role of aggregation and sedimentation in  the process. Marine snow formation and its sedimentation are an  essential component of elemental cycling.  It has been postulated that  sedimentation of material &quot;cleans&quot; the water column from particles.  Marine snow is also thought to be hotspots of microbial activity.  Potentially this oily marine snow could not only represent hotspots of  activity for oil degrading organisms, but may also function to isolate  oil into small volumes.  However, rapid sedimentation of such oil  aggregates may lead to anoxia at depths.  Scientifically we do not  understand the possible interactions between marine snow, marine  particles, oil and dispersant. &lt;/p&gt;
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