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- W2092786250 abstract "Other| June 01, 2002 Stable Carbon-Isotope Compositions of Compression Fossils from Lower Paleozoic Konservat-Lagerstätten STEVEN T. LO DUCA; STEVEN T. LO DUCA 1Department of Geography and Geology, Eastern Michigan University, Ypsilanti, MI 48197 Search for other works by this author on: GSW Google Scholar LISA M. PRATT LISA M. PRATT 2Department of Geological Sciences, Indiana University, Bloomington, IN 47405 Search for other works by this author on: GSW Google Scholar Author and Article Information STEVEN T. LO DUCA 1Department of Geography and Geology, Eastern Michigan University, Ypsilanti, MI 48197 LISA M. PRATT 2Department of Geological Sciences, Indiana University, Bloomington, IN 47405 Publisher: SEPM Society for Sedimentary Geology Accepted: 17 Dec 2001 First Online: 03 Mar 2017 Online ISSN: 1938-5323 Print ISSN: 0883-1351 Society for Sedimentary Geology PALAIOS (2002) 17 (3): 287–291. https://doi.org/10.1669/0883-1351(2002)017<0287:SCICOC>2.0.CO;2 Article history Accepted: 17 Dec 2001 First Online: 03 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation STEVEN T. LO DUCA, LISA M. PRATT; Stable Carbon-Isotope Compositions of Compression Fossils from Lower Paleozoic Konservat-Lagerstätten. PALAIOS 2002;; 17 (3): 287–291. doi: https://doi.org/10.1669/0883-1351(2002)017<0287:SCICOC>2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyPALAIOS Search Advanced Search Abstract Taxon-specific stable carbon-isotope ratios were determined for 7 graptolite (consumer) and 4 alga (primary producer) taxa preserved as thin organic compressions within North American Silurian Konservat-Lagerstätten. Values range from −26.6‰ for a graptolite from the Goat Island Formation, New York, to −32.3‰ for an alga from the Cape Phillips Formation, Arctic Canada. Co-occurring graptolite taxa display nearly identical δ13C compositions (within 0.2‰). Algal taxa co-occurring with graptolite taxa have δ13C compositions which are 1–2‰ more negative than those of associated graptolites. The observed isotopic offset between associated graptolites and macroalgae, both of which are common sources of organic matter in Paleozoic strata, holds implications for the interpretation of time-series δ13Corg curves, and suggests that stable carbon-isotope composition could serve as a chemosystematic tool for discerning the affinities of organic macrofossil problematica. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
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- W2092786250 title "Stable Carbon-Isotope Compositions of Compression Fossils from Lower Paleozoic Konservat-Lagerstatten" @default.
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