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dc.contributor.author현정호-
dc.date.accessioned2019-11-20T02:51:38Z-
dc.date.available2019-11-20T02:51:38Z-
dc.date.issued2019-03-
dc.identifier.citationFRONTIERS IN MARINE SCIENCE , v. 6, Article no. UNSP 132en_US
dc.identifier.issn2296-7745-
dc.identifier.urihttps://www.frontiersin.org/articles/10.3389/fmars.2019.00132/full-
dc.identifier.urihttps://repository.hanyang.ac.kr/handle/20.500.11754/112529-
dc.description.abstractThe Scientific Committee on Oceanographic Research (SCOR) Working Group 144 Microbial Community Responses to Ocean Deoxygenation workshop held in Vancouver, B.C on July 2014 had the primary objective of initiating a process to standardize operating procedures for compatible process rate and multi-omic (DNA, RNA, protein, and metabolite) data collection in marine oxygen minimum zones and other oxygen depleted waters. Workshop attendees participated in practical sampling and experimental activities in Saanich Inlet, British Columbia, a seasonally anoxic fjord. Experiments were designed to compare and cross-calibrate in situ versus bottle sampling methods to determine effects on microbial community structure and potential activity when using different filter combinations, filtration methods, and sample volumes. Resulting biomass was preserved for small subunit ribosomal RNA (SSU or 16S rRNA) and SSU rRNA gene (rDNA) amplicon sequencing followed by downstream statistical and visual analyses. Results from these analyses showed that significant community shifts occurred between in situ versus on ship processed samples. For example, Bacteroidetes, Alphaproteobacteria, and Opisthokonta associated with on-ship filtration onto 0.4 mm filters increased fivefold compared to on-ship in-line 0.22 mm filters or 0.4 mm filters processed and preserved in situ. In contrast, Planctomycetes associated with 0.4 mm in situ filters increased fivefold compared to on-ship filtration onto 0.4 mm filters and on-ship in-line 0.22 mm filters. In addition, candidate divisions and Chloroflexi were primarily recovered when filtered onto 0.4 mm filters in situ. Results based on rRNA:rDNA ratios for microbial indicator groups revealed previously unrecognized roles of candidate divisions, Desulfarculales, and Desulfuromandales in sulfur cycling, carbon fixation and fermentation within anoxic basin waters. Taken together, filter size and in situ versus on-ship filtration had the largest impact on recovery of microbial groups with the potential to influence downstream metabolic reconstruction and process rate measurements. These observations highlight the need for establishing standardized and reproducible techniques that facilitate cross-scale comparisons and more accurately assess in situ activities of microbial communities.en_US
dc.description.sponsorshipThis work was performed under the auspices of the Scientific Committee on Oceanographic Research (SCOR), the United States Department of Energy (DOE) Joint Genome Institute, an Office of Science User Facility, supported by the Office of Science of the United States Department of Energy under Contract DE-AC02-05CH11231, the G. Unger Vetlesen and Ambrose Monell Foundations, the Tula Foundation-funded Centre for Microbial Diversity and Evolution, the Natural Sciences and Engineering Research Council of Canada, Genome British Columbia, the Canada Foundation for Innovation, and the Canadian Institute for Advanced Research through grants awarded to SH. McLane Research Laboratories and Connie Lovejoy contributed access to instrumentation for field work. Ship time support was provided by NSERC between 2007 and 2014 through grants awarded to SC, SH and Philippe Tortell MT-B was funded by Consejo Nacional de Ciencia y Tecnologia (CONACyT) and the Tula Foundation.en_US
dc.language.isoen_USen_US
dc.publisherFrontiers Media S.A.en_US
dc.subjectmicrobial ecologyen_US
dc.subjectoxygen minimum zoneen_US
dc.subjectstandards of practiceen_US
dc.subjectfiltration methodsen_US
dc.subjectamplicon sequencingen_US
dc.titleSampling and Processing Methods Impact Microbial Community Structure and Potential Activity in a Seasonally Anoxic Fjord: Saanich Inlet, British Columbiaen_US
dc.typeArticleen_US
dc.relation.no132-
dc.relation.volume6-
dc.identifier.doi10.3389/fmars.2019.00132-
dc.relation.page1-16-
dc.relation.journalFrontiers in Marine Science-
dc.contributor.googleauthorTorres-Beltran, Monica-
dc.contributor.googleauthorMueller, Andreas-
dc.contributor.googleauthorScofield, Melanie-
dc.contributor.googleauthorPachiadaki, Maria G.-
dc.contributor.googleauthorTaylor, Craig-
dc.contributor.googleauthorTyshchenko, Kateryna-
dc.contributor.googleauthorMichiels, Celine-
dc.contributor.googleauthorLam, Phyllis-
dc.contributor.googleauthorUlloa, Osvaldo-
dc.contributor.googleauthorJurgens, Klaus-
dc.contributor.googleauthorHyun, Jung-Ho-
dc.contributor.googleauthorEdgcomb, Virginia P.-
dc.contributor.googleauthorCrowe, Sean A.-
dc.contributor.googleauthorHallam, Steven J.-
dc.relation.code2019016898-
dc.sector.campusE-
dc.sector.daehakCOLLEGE OF SCIENCE AND CONVERGENCE TECHNOLOGY[E]-
dc.sector.departmentDEPARTMENT OF MARINE SCIENCE AND CONVERGENCE ENGINEERING-
dc.identifier.pidhyunjh-


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