<?xml version="1.0" encoding="UTF-8" ?><MD_Metadata xmlns="http://www.isotc211.org/2005/gmd" xmlns:gco="http://www.isotc211.org/2005/gco" xmlns:gml="http://www.opengis.net/gml" xmlns:xlink="http://www.w3.org/1999/xlink" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.isotc211.org/2005/gmd http://www.isotc211.org/2005/gmd/gmd.xsd"><fileIdentifier><gco:CharacterString>georefid:2006-060880</gco:CharacterString></fileIdentifier><parentIdentifier><gco:CharacterString>georefid:2006-060877</gco:CharacterString></parentIdentifier><contact><CI_ResponsibleParty><organisationName><gco:CharacterString>SEDIS Publication Catalogue</gco:CharacterString></organisationName><contactInfo><CI_Contact><address><CI_Address><electronicMailAddress><gco:CharacterString>ana.macario@awi.de</gco:CharacterString></electronicMailAddress></CI_Address></address><onlineResource><CI_OnlineResource><linkage><URL>http://sedis.iodp.org/pub-catalogue/</URL></linkage><function><CI_OnLineFunctionCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_OnLineFunctionCode_information">information</CI_OnLineFunctionCode></function></CI_OnlineResource></onlineResource></CI_Contact></contactInfo><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_pointOfContact">pointOfContact</CI_RoleCode></role></CI_ResponsibleParty></contact><dateStamp><gco:DateTime>2011-06-23T00:00:00Z</gco:DateTime></dateStamp><dataSetURI><gco:CharacterString>http://sedis.iodp.org/pub-catalogue/index.php?id=10.2973/odp.proc.sr.185.008.2003</gco:CharacterString></dataSetURI><identificationInfo><MD_DataIdentification><citation><CI_Citation><title><gco:CharacterString>Bacterial populations in deepwater low-sedimentation-rate marine sediments and evidence for subsurface bacterial manganese reduction (ODP Site 1149, Izu-Bonin Trench)</gco:CharacterString></title><date><CI_Date><date><gco:Date>2006-01-01</gco:Date></date><dateType><CI_DateTypeCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_DateTypeCode_publication">publication</CI_DateTypeCode></dateType></CI_Date></date><identifier><MD_Identifier><code><gco:CharacterString>georefid:2006-060880</gco:CharacterString></code></MD_Identifier></identifier><identifier><MD_Identifier><code><gco:CharacterString>doi:10.2973/odp.proc.sr.185.008.2003</gco:CharacterString></code></MD_Identifier></identifier><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Cragg, Barry A.</gco:CharacterString></individualName><organisationName><gco:CharacterString>University of Bristol, Department of Earth Sciences, Bristol, United Kingdom</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Wellsbury, Peter</gco:CharacterString></individualName><organisationName><gco:CharacterString>Boston University, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Murray, Richard W.</gco:CharacterString></individualName><organisationName><gco:CharacterString>Ocean Drilling Program, United States</gco:CharacterString></organisationName><role><CI_RoleCode codeList="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode" codeListValue="http://www.isotc211.org/2005/resources/Codelist/gmxCodelists.xml#CI_RoleCode_author">author</CI_RoleCode></role></CI_ResponsibleParty></citedResponsibleParty><citedResponsibleParty><CI_ResponsibleParty><individualName><gco:CharacterString>Parkes, R. 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(editor), Plank, Terry (editor), Escutia, Carlota (editor), Abrams, Lewis J., Alt, Jeffrey C., Armstrong, Robin N., Barr, Samantha, Bartolini, Annachiara, Cairns, Graeme, Fisk, Martin R., Guerin, Gilles, Haveman, Shelley A., Hirono, Tetsuro, Honnorez, Jose, Kelley, Katherine A., Larson, Roger L., Lozar, Francesca M., Murray, Richard W., Pletsch, Thomas K., Pockalny, Robert A., Rouxel, Olivier, Schmidt, Angelika, Smith, David C., Spivack, Arthur J., Staudigel, Hubert, Steiner, Maureen B., Valentine, Robert B., Proceedings of the Ocean Drilling Program; scientific results, Izu-Mariana Margin; covering Leg 185 of the drilling vessel JOIDES Resolution; Hong Kong, People's Republic of China, to Yokohama, Japan; Sites 801 and 1149; 12 April-14 June 1999</gco:CharacterString></name><issueIdentification><gco:CharacterString>185</gco:CharacterString></issueIdentification></CI_Series></series></CI_Citation></citation><abstract><gco:CharacterString>Bacterial distributions were determined at Site 1149 in the Izu-Bonin Trench, which is a deepwater (5818 m) low-sedimentation-rate area. This was the first Ocean Drilling Program (ODP) leg where contamination checks were conducted for microbiology. These demonstrated that the inner portion of cores, where the microbiological samples were taken, were free from any potential sampling contamination. Bacterial populations were present in all samples (deepest at 171.2 meters below seafloor [mbsf]). The highest numbers were near the surface (1.4 mbsf; 7.2X10 (super 6) cells/cm (super 3) ), but these declined rapidly within the upper 10 mbsf. Below this, numbers decreased at a more gradual rate to 7.2X10 (super 5) cells/cm (super 3) at 172 mbsf, a 10-fold reduction. This two-stage bacterial depth distribution has been observed at several other ODP sites (e.g., Amazon Fan and Santa Barbara Basin). Bacterial depth distributions at this site were well below those predicted by the general equation for global deep-sediment bacteria and predominantly below the lower 95% prediction limits. These low bacterial populations were thought to reflect the low sedimentation rates and low input of bioavailable organic matter that is characteristic for deepwater sites. Consistent with this trend is that there was only limited removal of pore water sulfate and, thus, bacterial sulfate reduction. Most of this removal was in the top approximately 5 mbsf, coinciding with the highest bacterial populations, the presence of small amounts of methane, and an increase in pore water manganese and ammonia. In the deeper sediments, however, there was still indirect evidence of continuing low bacterial activity, with increases in pore water ammonia, soluble manganese, bioavailable acetate, and decreasing sulfate. 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