{"id":2755,"date":"2016-09-22T00:00:00","date_gmt":"2016-09-21T16:00:00","guid":{"rendered":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/an-investigation-of-the-physiology-and-potential-role-of-components-of-the-deep-ocean-bacterial-community-of-the-ne-atlantic-by-enrichments-carried-out-under-minimal-environmental-change\/"},"modified":"2016-09-22T00:00:00","modified_gmt":"2016-09-21T16:00:00","slug":"an-investigation-of-the-physiology-and-potential-role-of-components-of-the-deep-ocean-bacterial-community-of-the-ne-atlantic-by-enrichments-carried-out-under-minimal-environmental-change","status":"publish","type":"post","link":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/an-investigation-of-the-physiology-and-potential-role-of-components-of-the-deep-ocean-bacterial-community-of-the-ne-atlantic-by-enrichments-carried-out-under-minimal-environmental-change\/","title":{"rendered":"An investigation of the physiology and potential role of components of the deep ocean bacterial community (of the NE Atlantic) by enrichments carried out under minimal environmental change"},"content":{"rendered":"<p>Samples of deep-ocean water (3170 m) taken from the Rockall Trough (North-East Atlantic) were incubated for one-month at atmospheric and in-situ pressure (31 MPa), at 4 &deg;C and in the absence and presence of added nutrients. Prokaryotic abundance (direct cell counts) increased by at least 28-fold in enrichments without added nutrients. However, the magnitude of increase in abundance was less for incubations carried out at in-situ pressure (131\u2013181-fold) than those incubations at surface pressure (163\u20131714-fold increase in abundance). Changes in the prokaryotic community profile as a result of one-month incubation were measured by means of Denaturing Gel Electrophoresis (DGGE) of extracted 16S rDNA. The profiles of post-incubation samples incubated at in-situ pressure were separated from all other profiles as were those of unpressurised samples with added nutrients. The behaviour (fitness) of individual community members (Operational Taxonomic Units: OTUs) was determined on the basis of change in relative DGGE band intensities between pre- and post-incubation samples. Of twenty-one OTUs examined, six were fitter when incubated in the presence of added nutrients and at in-situ pressure and one of these was advantaged when grown in the absence of added nutrients and at in-situ pressure. These represented autochthonous and active members of the deep-ocean prokaryotic community. In contrast, seven OTUs were disadvantaged when grown under in-situ pressure and were indicative surface-derived allochtonous microorganisms. A further two OTUs came to dominance in incubations with added nutrients (pressurised and unpressurised) and similar to the previous category were probably surface-derived microorganisms. A single OTU showed characteristics of piezophilic and oliogrophic behaviour and four OTUs were disadvantaged under all incubation conditions examined. The twenty-one DGGE bands were sequenced and the bacterial communities were dominated by Gamma proteobactria and to a lesser extent members of the Cytophaga\u2013Flavobacterium\u2013Bacteroides and &delta; groups of prokaryotes.<\/p>\n","protected":false},"excerpt":{"rendered":"<p>Samples of deep-ocean water (3170 m) taken from the Roc [&hellip;]<\/p>\n","protected":false},"author":1,"featured_media":0,"comment_status":"closed","ping_status":"open","sticky":false,"template":"","format":"standard","meta":{"_uag_custom_page_level_css":"","site-sidebar-layout":"default","site-content-layout":"","ast-site-content-layout":"default","site-content-style":"default","site-sidebar-style":"default","ast-global-header-display":"","ast-banner-title-visibility":"","ast-main-header-display":"","ast-hfb-above-header-display":"","ast-hfb-below-header-display":"","ast-hfb-mobile-header-display":"","site-post-title":"","ast-breadcrumbs-content":"","ast-featured-img":"","footer-sml-layout":"","ast-disable-related-posts":"","theme-transparent-header-meta":"","adv-header-id-meta":"","stick-header-meta":"","header-above-stick-meta":"","header-main-stick-meta":"","header-below-stick-meta":"","astra-migrate-meta-layouts":"default","ast-page-background-enabled":"default","ast-page-background-meta":{"desktop":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"ast-content-background-meta":{"desktop":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"tablet":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""},"mobile":{"background-color":"var(--ast-global-color-5)","background-image":"","background-repeat":"repeat","background-position":"center center","background-size":"auto","background-attachment":"scroll","background-type":"","background-media":"","overlay-type":"","overlay-color":"","overlay-opacity":"","overlay-gradient":""}},"footnotes":""},"categories":[15,14],"tags":[],"class_list":["post-2755","post","type-post","status-publish","format-standard","hentry","category-15","category-14"],"uagb_featured_image_src":{"full":false,"thumbnail":false,"medium":false,"medium_large":false,"large":false,"1536x1536":false,"2048x2048":false,"mailpoet_newsletter_max":false},"uagb_author_info":{"display_name":"administrator","author_link":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/author\/wayne\/"},"uagb_comment_info":0,"uagb_excerpt":"Samples of deep-ocean water (3170 m) taken from the Roc...","_links":{"self":[{"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/posts\/2755","targetHints":{"allow":["GET"]}}],"collection":[{"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/posts"}],"about":[{"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/types\/post"}],"author":[{"embeddable":true,"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/users\/1"}],"replies":[{"embeddable":true,"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/comments?post=2755"}],"version-history":[{"count":0,"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/posts\/2755\/revisions"}],"wp:attachment":[{"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/media?parent=2755"}],"wp:term":[{"taxonomy":"category","embeddable":true,"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/categories?post=2755"},{"taxonomy":"post_tag","embeddable":true,"href":"https:\/\/etdicwp2025.etdic.org.tw\/etdic\/wp-json\/wp\/v2\/tags?post=2755"}],"curies":[{"name":"wp","href":"https:\/\/api.w.org\/{rel}","templated":true}]}}