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            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/dataset/781137.rdf" xlink:actuate="onRequest">Metagenomic data from samples collected on cruise Chikyu-331 in the Okinawa Trough, Japan from September to October 2010</gmx:Anchor>
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        <gco:CharacterString>Metagenomic data Dataset Description: &amp;lt;p&amp;gt;Next-generation sequencing data across a hydrothermal gradient; Okinawa Backarc Basin IODP 331 – subvent biosphere.&amp;amp;nbsp;The purpose these metagenomic data was to capture a distinct changeover of microbial assemblages between the mesophilic horizons above 10 mbsf and the hottest (55C) hydrothermal clay horizon. In this section of the dynamic Iheya North Hydrothermal system, the temperature gradient was estimated to be ~3C/m. These metagenomes provide functional evidence to this model, demonstrating that molecular signals represent a responsive microbial community to the increasingly demanding environmental conditions.&amp;lt;/p&amp;gt; Methods and Sampling: &amp;lt;p&amp;gt;Sampling of cores was done in accordance with IODP protocols.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;All C0014 samples were cored on 16 September 2010 via via HPCS (hydraulic piston coring system).&amp;lt;br /&amp;gt;
All C0015 samples were cored on 18 September 2010 via HPCS.&amp;lt;br /&amp;gt;
All C0017 samples were cored on 27 September 2010 via HPCS.&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Core sections were kept frozen (-80°C) until DNA extractions. A MoBio® Power Soil kit was used to extract environmental DNA. Metagenomic data was produced from whole genome amplified environmental DNA (REPLI-g Mini Kit, Qiagen).&amp;lt;/p&amp;gt;

&amp;lt;p&amp;gt;Sequencing was performed at the Penn State Genomics Core Facility – University Park, PA using the Illumina® HiSeq 2500 (NSF-MRI award DBI-1229046 (Axtell et al., 2012)). The sequencing facility prepared DNA libraries using Nextera XT Library Preparation Kits prior to sequencing. Together, the samples were run on one-half of a sequencing plate. This sequencing run was run using rapid-run model that averages up to 300 million single reads, or 600 million paired reads of ~150 nucleotides per rapid-run.&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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(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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The U.S. National Science Foundation (NSF) 
Japan's Ministry of Education, Culture, Sports, Science and Technology (MEXT) 
The European Consortium for Ocean Research Drilling (ECORD)

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                            <gmx:Anchor xlink:href="http://lod.bco-dmo.org/id/project/714230.rdf" xlink:title="Project Name" xlink:actuate="onRequest">An In-Depth analysis of the subvent biosphere within Okinawa Backarc Basin (IODP 331, Iheya North Hydrothermal Field) sediments</gmx:Anchor>
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                            <gco:CharacterString>&lt;p&gt;The Iheya North Hydrothermal Field in the Okinawa Backarc Basin represents an ideal environment in which to investigate the biotic temperature fringe of microbial life at depth because of its subsurface hydrothermal activity within its continental margin-type sediment profile. Geographically, the Okinawa Backarc Basin is situated along a continental margin, which is a sediment profile type commonly sampled and studied across the seafloor (e.g. Peru Margin, Costa Rica Margin, Cascadia Margin). The hydrothermal network within the subsurface here supplies an additional temperature obstacle to microbial life existing in the sediments. In particular, the sediment profile at Site C0014 exhibits a transition from hemipelagic ooze with pumiceous volcaniclastic sediments and low temperature (4°C) to a hydrothermally altered sequence of clays within the top ~10 mbsf of sediment. Temperature measurements indicate a gradient of approximately 3°C/m, which is roughly an order of magnitude greater than continental margin sites (e.g. Cascadia Margin, IODP 311 and Costa Rica Margin, IODP 344), but is more gradual than intense, centimeter-scale gradients from other hot, surface sediments. We have focused on the application of culture-independent, molecular methods to understand taxonomic and functional characteristics through this hydrothermal gradient. Confidence in DNA recovery suggests a microbial biosphere extent of approximately 15 mbsf (55°C).&lt;/p&gt;
&lt;p&gt;Results from both 16S rRNA gene surveys and metagenomics analyses suggest a temperature-dependent stratigraphy of taxonomic and functional adaptations between the shallowest and deepest sample horizons. Cosmopolitan marine subsurface bacterial and archaeal taxa are present throughout the top 10 mbsf, whereas, hyperthermophilic heterotrophic as well as thermophilic anaerobic methanotrophic archaea appear in varying local abundances in deeper, hydrothermal clay horizons. &quot;An In-Depth analysis of the subvent biosphere within Okinawa Backarc Basin (IODP 331, Iheya North Hydrothermal Field) sediments&quot; encompasses datasets funded through C-DEBI to investigate the microbial communities in IODP 331 Iheya North Hydrothermal Field sediments. Site C0014 at this field site is 500 m away from the active vent and experiences a 3C/m temperature gradient with depth. In the research grant &quot;Investigating the active microbial populations in near hydrothermal vent sediments&quot; and the Research Exchange grant &quot;Learning new RNA extraction techniques&quot;, we used an RNA-based approach to explore the active microbial community. Upon analysis, the RNA dataset does not appear to reflect the same information as the phylogenetic signals coming from both the 16S rRNA gene as well as the metagenomes. The data indicate significant background noise from the RNA extraction process rather than from an indigenous representation of the subsurface biosphere.&lt;/p&gt;
&lt;p&gt;The graduate fellowship &quot;An in-depth analysis of the subvent biosphere within the Okinawa backarc basin Iheya North hydrothermal field&quot; provided an opportunity to bring together metagenomic, 16S rRNA gene amplicon (DNA), and 16S rRNA amplicon datasets from IODP 331 Iheya North Hydrothermal Field sediments to understand the biogeography of this subvent biosphere.&lt;/p&gt;
&lt;p&gt;For more information, refer to the following C-DEBI grants/projects.&lt;br /&gt;
An in-depth analysis of the subvent biosphere within the Okinawa backarc basin Iheya North hydrothermal field:&lt;br /&gt;
&lt;a href=&quot;https://www.darkenergybiosphere.org/award/an-in-depth-analysis-of-the-subvent-biosphere-within-the-okinawa-backarc-basin-iheya-north-hydrothermal-field/&quot; target=&quot;_blank&quot;&gt;https://www.darkenergybiosphere.org/award/an-in-depth-analysis-of-the-subvent-biosphere-within-the-okinawa-backarc-basin-iheya-north-hydrothermal-field/&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Investigating the active microbial populations in near hydrothermal vent sediments: &lt;a href=&quot;https://www.darkenergybiosphere.org/award/investigating-the-active-microbial-populations-in-near-hydrothermal-vent-sediments/&quot; target=&quot;_blank&quot;&gt;https://www.darkenergybiosphere.org/award/investigating-the-active-microbial-populations-in-near-hydrothermal-vent-sediments/&lt;/a&gt;&lt;/p&gt;
&lt;p&gt;Learn new RNA extraction techniques: &lt;a href=&quot;https://www.darkenergybiosphere.org/award/learn-new-rna-extraction-techniques/&quot; target=&quot;_blank&quot;&gt;https://www.darkenergybiosphere.org/award/learn-new-rna-extraction-techniques/&lt;/a&gt;&lt;br /&gt;
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