georefid:2010-093223SEDIS Publication Catalogue

ana.macario@awi.de

http://sedis.iodp.org/pub-catalogue/informationpointOfContact2011-07-06T00:00:00Zhttp://sedis.iodp.org/pub-catalogue/index.php?id=10.2110/palo.2010.p10-032r2010-01-01publicationgeorefid:2010-093223doi:10.2110/palo.2010.p10-032rHeindel, KatrinUniversity of Bremen, Center of Marine Environmental Sciences, Bremen, Federal Republic of GermanyauthorBirgel, DanielauthorPeckmann, JoernauthorKuhnert, HenningauthorWestphal, HildegardauthorSociety for Sedimentary Geology, Tulsa, OK, United StatespublisherdocumentHardcopyPalaios25 (10)618-635During IODP Expedition 310 (Tahiti Sea Level), drowned Pleistocene-Holocene barrier-reef terraces were drilled on the slope of the volcanic island. The deglacial reef succession typically consists of a coral framework encrusted by coralline algae and later by microbialites; the latter make up < or =80% of the rock volume. Lipid biomarkers were analyzed in order to identify organisms involved in reef-microbialite formation at Tahiti, as the genesis of deglacial microbialites and the conditions favoring their formation are not fully understood. Sterols plus saturated and monounsaturated short-chain fatty acids predominantly derived from both marine primary producers (algae) and bacteria comprise 44 wt% of all lipids on average, whereas long-chain fatty acids and long-chain alcohols derived from higher land plants represent an average of only 24 wt%. Bacterially derived mono-O-alkyl glycerol ethers (MAGEs) and branched fatty acids (10-Me-C (sub 16:0) ; iso- and anteiso-C (sub 15:0) and -C (sub 17:0) ) are exceptionally abundant in the microbial carbonates (average, 19 wt%) and represent biomarkers of intermediate-to-high specificity for sulfate-reducing bacteria. Both are relatively enriched in (super 13) C compared to eukaryotic lipids. No lipid biomarkers indicative of cyanobacteria were preserved in the microbialites. The abundances of Al, Si, Fe, Mn, Ba, pyroxene, plagioclase, and magnetite reflect strong terrigenous influx with Tahitian basalt as the major source. Chemical weathering of the basalt most likely elevated nutrient levels in the reefs and this fertilization led to an increase in primary production and organic matter formation, boosting heterotrophic sulfate reduction. Based on the observed biomarker patterns, sulfate-reducing bacteria were apparently involved in the formation of microbialites in the coral reefs off Tahiti during the last deglaciation.completedSedimentary petrologyIsotope geochemistrybacteriabiomarkersC-13/C-12carboncarbonate rocksCenozoicchemical compositionEast PacificExpedition 310French PolynesiaHoloceneICP mass spectraIntegrated Ocean Drilling ProgramIODP Site M0005IODP Site M0009IODP Site M0015IODP Site M0016IODP Site M0017IODP Site M0018IODP Site M0021IODP Site M0023isotope ratiosisotopeslimestonelipidsmass spectramicrobialiteO-18/O-16Oceaniaorganic compoundsoxygenPacific OceanpaleoclimatologypaleoecologypaleoenvironmentPleistocenePolynesiaproductivityQuaternaryreef environmentsedimentary rocksSociety IslandsSouth PacificSoutheast Pacificspectrastable isotopesTahitiTahiti Sea Level ExpeditionX-ray diffraction dataurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0005urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0009urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0015urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0016urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0017urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0018urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0021urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignurn:org.iodp:exp:310:site:M0023urnlargerWorkCitationstudyurn:org.iodp:exp:310urnlargerWorkCitationcampaignEnglishgeoscientificInformation-149.3600-149.2400-17.4600-17.2900