FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1997565617> ?p ?o ?g. }

• W1997565617 endingPage "242" @default.
• W1997565617 startingPage "239" @default.
• W1997565617 abstract "Research Article| March 01, 2009 A new look at old carbon in active margin sediments Nicholas J. Drenzek; Nicholas J. Drenzek * 11Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA *E-mail: ndrenzek@whoi.edu. Search for other works by this author on: GSW Google Scholar Konrad A. Hughen; Konrad A. Hughen 11Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Daniel B. Montluçon; Daniel B. Montluçon 11Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar John R. Southon; John R. Southon 22Deparment of Earth System Science, University of California–Irvine, Irvine, California 92697, USA Search for other works by this author on: GSW Google Scholar Guaciara M. dos Santos; Guaciara M. dos Santos 22Deparment of Earth System Science, University of California–Irvine, Irvine, California 92697, USA Search for other works by this author on: GSW Google Scholar Ellen R.M. Druffel; Ellen R.M. Druffel 22Deparment of Earth System Science, University of California–Irvine, Irvine, California 92697, USA Search for other works by this author on: GSW Google Scholar Liviu Giosan; Liviu Giosan 33Department of Geology and Geophysics, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Timothy I. Eglinton Timothy I. Eglinton 11Department of Marine Chemistry and Geochemistry, Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543, USA Search for other works by this author on: GSW Google Scholar Geology (2009) 37 (3): 239–242. https://doi.org/10.1130/G25351A.1 Article history received: 11 Jul 2008 rev-recd: 23 Oct 2008 accepted: 26 Oct 2008 first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation Nicholas J. Drenzek, Konrad A. Hughen, Daniel B. Montluçon, John R. Southon, Guaciara M. dos Santos, Ellen R.M. Druffel, Liviu Giosan, Timothy I. Eglinton; A new look at old carbon in active margin sediments. Geology 2009;; 37 (3): 239–242. doi: https://doi.org/10.1130/G25351A.1 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 SocietyGeology Search Advanced Search Abstract Recent studies suggest that as much as half of the organic carbon (OC) undergoing burial in the sediments of tectonically active continental margins may be the product of fossil shale weathering. These estimates rely on the assumption that vascular plant detritus spends little time sequestered in intermediate reservoirs such as soils, freshwater sediments, and river deltas, and thus only minimally contributes to the extraneously old 14C ages of total organic matter often observed on adjacent shelves. Here we test this paradigm by measuring the Δ14C and δ13C values of individual higher plant wax fatty acids as well as the δ13C values of extractable alkanes isolated from the Eel River margin (California). The isotopic signatures of the long chain fatty acids indicate that vascular plant material has been sequestered for several thousand years before deposition. A coupled molecular isotope mass balance used to reassess the sedimentary carbon budget indicates that the fossil component is less abundant than previously estimated, with pre-aged terrestrial material instead composing a considerable proportion of all organic matter. If these findings are characteristic of other continental margins proximal to small mountainous rivers, then the importance of petrogenic OC burial in marine sediments may need to be reevaluated. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W1997565617 created "2016-06-24" @default.
• W1997565617 creator A5002414024 @default.
• W1997565617 creator A5019862798 @default.
• W1997565617 creator A5023501632 @default.
• W1997565617 creator A5029547508 @default.
• W1997565617 creator A5034149386 @default.
• W1997565617 creator A5043939464 @default.
• W1997565617 creator A5072255354 @default.
• W1997565617 creator A5089327434 @default.
• W1997565617 date "2009-03-01" @default.
• W1997565617 modified "2023-10-03" @default.
• W1997565617 title "A new look at old carbon in active margin sediments" @default.
• W1997565617 cites W1569224549 @default.
• W1997565617 cites W1623136437 @default.
• W1997565617 cites W1675507387 @default.
• W1997565617 cites W1927080046 @default.
• W1997565617 cites W1937838860 @default.
• W1997565617 cites W1964199180 @default.
• W1997565617 cites W1973714196 @default.
• W1997565617 cites W1985053863 @default.
• W1997565617 cites W1987263719 @default.
• W1997565617 cites W1988624166 @default.
• W1997565617 cites W1990162765 @default.
• W1997565617 cites W1991413173 @default.
• W1997565617 cites W1995363061 @default.
• W1997565617 cites W1996813892 @default.
• W1997565617 cites W2008410509 @default.
• W1997565617 cites W2015298615 @default.
• W1997565617 cites W2020661576 @default.
• W1997565617 cites W2020873526 @default.
• W1997565617 cites W2027232936 @default.
• W1997565617 cites W2029333538 @default.
• W1997565617 cites W2036872876 @default.
• W1997565617 cites W2038281478 @default.
• W1997565617 cites W2040140061 @default.
• W1997565617 cites W2044487919 @default.
• W1997565617 cites W2044611122 @default.
• W1997565617 cites W2056864037 @default.
• W1997565617 cites W2058371571 @default.
• W1997565617 cites W2062097675 @default.
• W1997565617 cites W2062885842 @default.
• W1997565617 cites W2071390384 @default.
• W1997565617 cites W2073770054 @default.
• W1997565617 cites W2073876136 @default.
• W1997565617 cites W2076024570 @default.
• W1997565617 cites W2082416161 @default.
• W1997565617 cites W2095347466 @default.
• W1997565617 cites W2100286653 @default.
• W1997565617 cites W2107664788 @default.
• W1997565617 cites W2108934364 @default.
• W1997565617 cites W2112836917 @default.
• W1997565617 cites W2138082266 @default.
• W1997565617 cites W2138239189 @default.
• W1997565617 cites W2158727851 @default.
• W1997565617 cites W2164868142 @default.
• W1997565617 doi "https://doi.org/10.1130/g25351a.1" @default.
• W1997565617 hasPublicationYear "2009" @default.
• W1997565617 type Work @default.
• W1997565617 sameAs 1997565617 @default.
• W1997565617 citedByCount "78" @default.
• W1997565617 countsByYear W19975656172012 @default.
• W1997565617 countsByYear W19975656172013 @default.
• W1997565617 countsByYear W19975656172014 @default.
• W1997565617 countsByYear W19975656172015 @default.
• W1997565617 countsByYear W19975656172016 @default.
• W1997565617 countsByYear W19975656172017 @default.
• W1997565617 countsByYear W19975656172018 @default.
• W1997565617 countsByYear W19975656172019 @default.
• W1997565617 countsByYear W19975656172020 @default.
• W1997565617 countsByYear W19975656172021 @default.
• W1997565617 countsByYear W19975656172022 @default.
• W1997565617 countsByYear W19975656172023 @default.
• W1997565617 crossrefType "journal-article" @default.
• W1997565617 hasAuthorship W1997565617A5002414024 @default.
• W1997565617 hasAuthorship W1997565617A5019862798 @default.
• W1997565617 hasAuthorship W1997565617A5023501632 @default.
• W1997565617 hasAuthorship W1997565617A5029547508 @default.
• W1997565617 hasAuthorship W1997565617A5034149386 @default.
• W1997565617 hasAuthorship W1997565617A5043939464 @default.
• W1997565617 hasAuthorship W1997565617A5072255354 @default.
• W1997565617 hasAuthorship W1997565617A5089327434 @default.
• W1997565617 hasBestOaLocation W19975656172 @default.
• W1997565617 hasConcept C111368507 @default.
• W1997565617 hasConcept C127313418 @default.
• W1997565617 hasConcept C161191863 @default.
• W1997565617 hasConcept C17744445 @default.
• W1997565617 hasConcept C199539241 @default.
• W1997565617 hasConcept C2780510313 @default.
• W1997565617 hasConcept C28115305 @default.
• W1997565617 hasConcept C41008148 @default.
• W1997565617 hasConceptScore W1997565617C111368507 @default.
• W1997565617 hasConceptScore W1997565617C127313418 @default.
• W1997565617 hasConceptScore W1997565617C161191863 @default.
• W1997565617 hasConceptScore W1997565617C17744445 @default.
• W1997565617 hasConceptScore W1997565617C199539241 @default.
• W1997565617 hasConceptScore W1997565617C2780510313 @default.
• W1997565617 hasConceptScore W1997565617C28115305 @default.

• next