Is the Oxygen Isotopic Composition of Authigenic Mn-Carbonates a Bottom-Water Salinity Indicator or a Reflection of Early Burial Diagenetic Processes: Evidence from Recent Sapropelic Sediments of the Baltic Sea

Details Is the Oxygen Isotopic Composition of Authigenic Mn-Carbonates a Bottom-Water Salinity Indicator or a Reflection of Early Burial Diagenetic Processes: Evidence from Recent Sapropelic Sediments of the Baltic Sea Is the Oxygen Isotopic Composition of Authigenic Mn-Carbonates a Bottom-Water Salinity Indicator or a Reflection of Early Burial Diagenetic Processes: Evidence from Recent Sapropelic Sediments of the Baltic Sea

May 2001

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001eag..conf.3335n&link_type=article

Eleventh Annual V. M. Goldschmidt Conference, May 20-24, 2001, Hot Springs, Virginia, abstract no.3335

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