FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2013209996> ?p ?o ?g. }

• W2013209996 endingPage "5609" @default.
• W2013209996 startingPage "5593" @default.
• W2013209996 abstract "Amino acids and the bacterial biomarkers muramic acid and d-amino acids were quantified in the ultrafiltered dissolved, particulate and sedimentary organic matter (UDOM, POM and SOM) of the St. Lawrence system (Canada). The main objectives were to better describe the fate of terrigenous and marine organic matter (OM) in coastal zones and to quantify the bacterial contributions to OM composition and diagenesis. Regardless of their origin, the carbon (C) content of the particles substantially decreased with depth, especially near the water–sediment interface. Major diagenetic transformations of organic nitrogen (N) were revealed and important differences were observed between terrigenous and marine OM. Amino acid contents of particles decreased by 66–93% with depth and accounted for 12–30% of the particulate C losses in marine locations. These percentages were respectively 18–56% and 7–11% in the Saguenay Fjord where terrigenous input is important. A preferential removal of particulate N and amino acids with depth or during transport was measured, but only in marine locations and for N-rich particles. This leads to very low amino acid yields in deep marine POM. However, these yields then increased to a level up to three times higher after deposition on sediments, where SOM showed lower C:N ratios than deep POM. The associated increase of bacterial biomarker yields suggests an active in situ resynthesis of amino acids by benthic bacteria. The N content of the substrate most likely determines whether a preferential degradation or an enrichment of N and amino acid are observed. For N-poor OM, such as terrigenous or deep marine POM, the incorporation of exogenous N by attached bacteria can be measured, while the organic N is preferentially used or degraded in N-rich OM. Compared to the POM from the same water samples, the extracted UDOM was poor in N and amino acids and appeared to be mostly made of altered plant and bacterial fragments. Signs of in situ marine production of UDOM were observed in the most marine location. The POM entering the St. Lawrence Upper Estuary and the Saguenay Fjord appeared made of relatively fresh vascular plant OM mixed with highly altered bacterial debris from soils. In contrast, the POM samples from the more marine sites appeared mostly made of fresh planktonic and bacterial OM, although they were rapidly degraded during sinking. Based on biomarker yields, bacterial OM represented on average ∼20% of bulk C and approximately 40–70% of bulk N in POM and SOM, with the exception of deep marine POM exhibiting approximately two times lower bacterial contributions." @default.
• W2013209996 created "2016-06-24" @default.
• W2013209996 creator A5016470084 @default.
• W2013209996 creator A5044128150 @default.
• W2013209996 date "2010-10-01" @default.
• W2013209996 modified "2023-10-14" @default.
• W2013209996 title "Bacterial reworking of terrigenous and marine organic matter in estuarine water columns and sediments" @default.
• W2013209996 cites W1497204853 @default.
• W2013209996 cites W1615545896 @default.
• W2013209996 cites W1633546334 @default.
• W2013209996 cites W1934665271 @default.
• W2013209996 cites W1966028808 @default.
• W2013209996 cites W1967012853 @default.
• W2013209996 cites W1982860062 @default.
• W2013209996 cites W1985276039 @default.
• W2013209996 cites W1986923914 @default.
• W2013209996 cites W1986971437 @default.
• W2013209996 cites W1990733829 @default.
• W2013209996 cites W1990800053 @default.
• W2013209996 cites W1993328571 @default.
• W2013209996 cites W1994029344 @default.
• W2013209996 cites W1994551918 @default.
• W2013209996 cites W1994845524 @default.
• W2013209996 cites W1997667129 @default.
• W2013209996 cites W1999716014 @default.
• W2013209996 cites W2002232472 @default.
• W2013209996 cites W2003391958 @default.
• W2013209996 cites W2013091212 @default.
• W2013209996 cites W2016094557 @default.
• W2013209996 cites W2019721277 @default.
• W2013209996 cites W2020025535 @default.
• W2013209996 cites W2020873526 @default.
• W2013209996 cites W2024582683 @default.
• W2013209996 cites W2028347482 @default.
• W2013209996 cites W2028626507 @default.
• W2013209996 cites W2029389453 @default.
• W2013209996 cites W2037893214 @default.
• W2013209996 cites W2042895971 @default.
• W2013209996 cites W2043591550 @default.
• W2013209996 cites W2045598733 @default.
• W2013209996 cites W2048000262 @default.
• W2013209996 cites W2054160444 @default.
• W2013209996 cites W2058009447 @default.
• W2013209996 cites W2058641857 @default.
• W2013209996 cites W2059818368 @default.
• W2013209996 cites W2060026462 @default.
• W2013209996 cites W2064266307 @default.
• W2013209996 cites W2064891622 @default.
• W2013209996 cites W2069015237 @default.
• W2013209996 cites W2077871850 @default.
• W2013209996 cites W2082967831 @default.
• W2013209996 cites W2094690347 @default.
• W2013209996 cites W2095704344 @default.
• W2013209996 cites W2102504856 @default.
• W2013209996 cites W2102799963 @default.
• W2013209996 cites W2104372879 @default.
• W2013209996 cites W2106131153 @default.
• W2013209996 cites W2107602408 @default.
• W2013209996 cites W2113112355 @default.
• W2013209996 cites W2117642740 @default.
• W2013209996 cites W2128030331 @default.
• W2013209996 cites W2129156732 @default.
• W2013209996 cites W2130846455 @default.
• W2013209996 cites W2131650203 @default.
• W2013209996 cites W2135872201 @default.
• W2013209996 cites W2136335887 @default.
• W2013209996 cites W2151020563 @default.
• W2013209996 cites W2159113839 @default.
• W2013209996 cites W2160303883 @default.
• W2013209996 cites W2164358599 @default.
• W2013209996 cites W2165702243 @default.
• W2013209996 cites W2168262102 @default.
• W2013209996 cites W2168526533 @default.
• W2013209996 cites W2174725238 @default.
• W2013209996 cites W4206708139 @default.
• W2013209996 doi "https://doi.org/10.1016/j.gca.2010.06.037" @default.
• W2013209996 hasPublicationYear "2010" @default.
• W2013209996 type Work @default.
• W2013209996 sameAs 2013209996 @default.
• W2013209996 citedByCount "63" @default.
• W2013209996 countsByYear W20132099962012 @default.
• W2013209996 countsByYear W20132099962013 @default.
• W2013209996 countsByYear W20132099962014 @default.
• W2013209996 countsByYear W20132099962015 @default.
• W2013209996 countsByYear W20132099962016 @default.
• W2013209996 countsByYear W20132099962017 @default.
• W2013209996 countsByYear W20132099962018 @default.
• W2013209996 countsByYear W20132099962019 @default.
• W2013209996 countsByYear W20132099962020 @default.
• W2013209996 countsByYear W20132099962021 @default.
• W2013209996 countsByYear W20132099962022 @default.
• W2013209996 countsByYear W20132099962023 @default.
• W2013209996 crossrefType "journal-article" @default.
• W2013209996 hasAuthorship W2013209996A5016470084 @default.
• W2013209996 hasAuthorship W2013209996A5044128150 @default.
• W2013209996 hasConcept C107872376 @default.
• W2013209996 hasConcept C111368507 @default.
• W2013209996 hasConcept C127313418 @default.

• next