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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/654429.rdf" xlink:actuate="onRequest">The eukaryotic (poly-A) metatranscriptome for Canterbury Basin from R/V JOIDES Resolution cruise JRES-317 in the Canterbury Basin from 2009-2010</gmx:Anchor>
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                <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/affiliation/653749.rdf" xlink:actuate="onRequest">Universite de Brest</gmx:Anchor>
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            <gco:CharacterString>Cite this dataset as: Edgcomb, V. P., Pachiadaki, M. G., Burgaud, G. (2016) The eukaryotic (poly-A) metatranscriptome for Canterbury Basin from R/V JOIDES Resolution cruise JRES-317 in the Canterbury Basin from 2009-2010. Biological and Chemical Oceanography Data Management Office (BCO-DMO). (Version 19 Aug 2016) Version Date 2016-08-19 [if applicable, indicate subset used]. http://lod.bco-dmo.org/id/dataset/654429 [access date]</gco:CharacterString>
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        <gco:CharacterString>The eukaryotic (poly-A) metatranscriptome for Canterbury Basin Dataset Description: &amp;lt;p&amp;gt;The eukaryotic (poly-A) metatranscriptome for Canterbury Basin; sampled from the&amp;amp;nbsp;eastern margin of the South Island of New Zealand&amp;amp;nbsp;on&amp;amp;nbsp;JOIDES Resolution IODP leg 317.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;During IODP leg 317 expedition (JOIDES&amp;amp;nbsp;Resolution),&amp;amp;nbsp;a sediment core was drilled at Site U1352&amp;amp;nbsp;in 344 m water&amp;amp;nbsp;depth. A total depth of 1927.5 mbsf was cored, spanning the Holocene to late Eocene periods. For this&amp;amp;nbsp;work, core sections were obtained&amp;amp;nbsp;from this site from 3.76 mbsf, 11.60 mbsf, 24.60 mbsf, 345.50 mbsf, and&amp;amp;nbsp;403.10 mbsf.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;RNA was extracted from 16 g of sediment from the Canterbury core samples using the RNA PowerSoil Total RNA Isolation Kit (MoBIO Laboratories, Carlsbad, CA) following a modified manufacturer's protocol. Modifications included: ten cycles of homogenization for 1-minute intervals with 1 minute rest between intervals using a FastPrep benchtop homogenizer (MP Biomedicals, Santa Ana, CA) set to 4.0 m/s and increasing the incubation time to 45 min following the addition of SR4 buffer. Trace DNA was removed by treatment with Turbo DNA-free (Life Technologies, Grand Island, NY) for 60 minutes at 37 degrees&amp;amp;nbsp;C. A final RNA purification step was performed using the MEGAclear kit (Life Technologies, USA). In order to avoid contamination, all manipulations were carried out in a dedicated PCR hood (AirClean Systems, USA) for RNA work. An extraction blank was also carried through the entire procedure to control for kit contamination and served as &amp;quot;negative control&amp;quot;. Removal of carry-over DNA in RNA extracts was confirmed by the absence of visible amplification of the V4 hypervariable region of SSU rDNA after 35 cycles of PCR using the RNA extracts as template with key-tagged bacterial primers (Flores et al., 2011). PCR conditions were: 95 degrees&amp;amp;nbsp;C for 2 minutes followed by 35 cycles of 95 degrees&amp;amp;nbsp;C for 15 seconds, 53 degrees&amp;amp;nbsp;C for 45 seconds and 68 degrees&amp;amp;nbsp;C for 45 seconds with a final incubation of 68 degrees&amp;amp;nbsp;C for 3 minutes. Total RNA was used as template for cDNA amplification using the Ovation 3’-DGE System (NuGEN, San Carlos, CA) to obtain an enriched eukaryotic metatranscriptome through selection of polyA transcripts. Double-stranded cDNA was purified using the DNA Clean &amp;amp;amp; Concentrator kit (Zymo Research) as described in the modified user guide (&amp;lt;a href=&amp;quot;https://www.biolynx.ca/pdf/admin/nu_threedgeuserguide.pdf&amp;quot; target=&amp;quot;_blank&amp;quot;&amp;gt;https://www.biolynx.ca/pdf/admin/nu_threedgeuserguide.pdf&amp;lt;/a&amp;gt;) provided by NuGEN. The quantity of amplified cDNA was evaluated using a fluorometer (Qubit 2.0, Life Technologies).&amp;lt;/p&amp;gt;</gco:CharacterString>
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        <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/award/554980.rdf" xlink:title="OCE-0939564" xlink:actuate="onRequest">Funding provided by NSF Division of Ocean Sciences (NSF OCE) Award Number: OCE-0939564 Award URL: https://www.nsf.gov/awardsearch/show-award?AWD_ID=0939564</gmx:Anchor>
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            <gmx:Anchor xlink:href="https://ror.org/03zbnzt98" xlink:actuate="onRequest">Woods Hole Oceanographic Institution</gmx:Anchor>
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(1) coordinate, integrate, support, and extend the research associated with four major programs—Juan de Fuca Ridge flank (JdF), South Pacific Gyre (SPG), North Pond (NP), and Dorado Outcrop (DO)—and other field sites;
(2) make substantial investments of resources to support field, laboratory, analytical, and modeling studies of the deep subseafloor ecosystems;
(3) facilitate and encourage synthesis and thematic understanding of submarine microbiological processes, through funding of scientific and technical activities, coordination and hosting of meetings and workshops, and support of (mostly junior) researchers and graduate students; and
(4) entrain, educate, inspire, and mentor an interdisciplinary community of researchers and educators, with an emphasis on undergraduate and graduate students and early-career scientists.
Note: Katrina Edwards was a former PI of C-DEBI; James Cowen is a former co-PI.
Data Management:
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                            <gco:CharacterString>&lt;p&gt;The deep sedimentary biosphere, extending hundreds of meters below the seafloor harbors unexpected diversity of Bacteria, Archaea and microbial eukaryotes. Far less is known about microbial eukaryotes in subsurface habitats, albeit several studies have indicated that fungi dominate microbial eukaryotic communities and fungal molecular signatures (of both yeasts and filamentous forms) have been detected in samples as deep as 1740mbsf. Here we compare and contrast fungal ribosomal RNA gene signatures and whole community metatranscriptomes present in sediment core samples from 6 and 95mbsf from Peru Margin site 1229A and from samples from 12 and 345 mbsf from Canterbury Basin site U1352. The metatranscriptome analyses reveal higher relative expression of amino acid and peptide transporters in the less nutrient rich Canterbury Basin sediments compared to the nutrient rich Peru Margin, and higher expression of motility genes in the Peru Margin samples. Higher expression of genes associated with metals transporters and antibiotic resistance and production was detected in Canterbury Basin sediments. A poly-A focused metatranscriptome produced for the Canterbury Basin sample from 345 mbsf provides further evidence for active fungal communities in the subsurface in the form of fungal-associated transcripts for metabolic and cellular processes, cell and membrane functions, and catalytic activities. Fungal communities at comparable depths at the two geographically separated locations appear dominated by distinct taxa. Differences in taxonomic composition and expression of genes associated with particular metabolic activities may be a function of sediment organic content as well as oceanic province. Microscopic analysis of Canterbury Basin sediment samples from 4 and 403 mbsf produced visualizations of septate fungal filaments, branching fungi, conidiogenesis and spores. These images provide another important line of evidence supporting the occurrence and activity of fungi in the deep subseafloor biosphere.&lt;/p&gt;
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