Matches in SemOpenAlex for { <https://semopenalex.org/work/W2053516099> ?p ?o ?g. }
- W2053516099 endingPage "256" @default.
- W2053516099 startingPage "241" @default.
- W2053516099 abstract "Dissolved organic carbon (DOC), stable carbon isotopic (delta(13)C) compositions of DOC and particulate organic carbon (POC), and elemental C/N ratios of POC were measured for samples collected from the lower Mississippi and Atchafalaya rivers and adjacent coastal waters in the northern Gulf of Mexico during the low flow season in June 2000 and high flow season in April 2001. These isotopic and C/N results combined with DOC measurements were used to assess the sources and transport of terrestrial organic matter from the Mississippi and Atchafalaya rivers to the coastal region in the northern Gulf of Mexico. delta(13)C values of both POC (-23.8parts per thousand to -26.8parts per thousand) and DOC (-25.0parts per thousand to -29.0parts per thousand) carried by the two rivers were more depleted than the values measured for the samples collected in the offshore waters. Strong seasonal variations in delta(13)C distributions were observed for both POC and DOC in the surface waters of the region. Fresh water discharge and horizontal mixing played important roles in the distribution and transport of terrestrial POC and DOC offshore. Our results indicate that both POC and DOC exhibited non-conservative behavior during the mixing especially in the mid-salinity range. Based on a simple two end-member mixing model, the comparison of the measured DOC-delta(13)C with the calculated conservative isotopic mixing curve indicated that there was a significant in situ production of marine-derived DOC in the mid- to high-salinity waters consistent with our in situ chlorophyll-a measurements. Our DOC-delta(13)C data suggest that a removal of terrestrial DOC mainly occurred in the high-salinity (>25) waters during the mixing. Our study indicates that the mid- to high- (10-30) salinity range was the most dynamic zone for organic carbon transport and cycling in the Mississippi River estuary. Variability in isotopic and elemental compositions along with variability in DOC and POC concentrations suggest that autochthonous production, bacterial utilization, and photo-oxidation could all play important roles in regulating and removing terrestrial DOC in the northern Gulf of Mexico and further study of these individual processes is warranted. (C) 2004 Elsevier B.V. All rights reserved." @default.
- W2053516099 created "2016-06-24" @default.
- W2053516099 creator A5015998530 @default.
- W2053516099 creator A5026956124 @default.
- W2053516099 creator A5049495080 @default.
- W2053516099 date "2004-10-01" @default.
- W2053516099 modified "2023-09-27" @default.
- W2053516099 title "Sources and transport of dissolved and particulate organic carbon in the Mississippi River estuary and adjacent coastal waters of the northern Gulf of Mexico" @default.
- W2053516099 cites W1977105134 @default.
- W2053516099 cites W1979327430 @default.
- W2053516099 cites W1984424164 @default.
- W2053516099 cites W1985053863 @default.
- W2053516099 cites W1992307572 @default.
- W2053516099 cites W1997382336 @default.
- W2053516099 cites W1999711018 @default.
- W2053516099 cites W1999832358 @default.
- W2053516099 cites W2002238879 @default.
- W2053516099 cites W2002371864 @default.
- W2053516099 cites W2005963968 @default.
- W2053516099 cites W2008410509 @default.
- W2053516099 cites W2009560431 @default.
- W2053516099 cites W2010395522 @default.
- W2053516099 cites W2011332052 @default.
- W2053516099 cites W2015175583 @default.
- W2053516099 cites W2022198731 @default.
- W2053516099 cites W2037317208 @default.
- W2053516099 cites W2038504962 @default.
- W2053516099 cites W2040021345 @default.
- W2053516099 cites W2040110576 @default.
- W2053516099 cites W2040140061 @default.
- W2053516099 cites W2044197201 @default.
- W2053516099 cites W2045054463 @default.
- W2053516099 cites W2045733825 @default.
- W2053516099 cites W2045839452 @default.
- W2053516099 cites W2047369246 @default.
- W2053516099 cites W2053173497 @default.
- W2053516099 cites W2054160444 @default.
- W2053516099 cites W2054248197 @default.
- W2053516099 cites W2061539198 @default.
- W2053516099 cites W2063732589 @default.
- W2053516099 cites W2071612694 @default.
- W2053516099 cites W2071835205 @default.
- W2053516099 cites W2075484456 @default.
- W2053516099 cites W2091355073 @default.
- W2053516099 cites W2093197746 @default.
- W2053516099 cites W2113135961 @default.
- W2053516099 cites W2135166067 @default.
- W2053516099 cites W2136774340 @default.
- W2053516099 cites W2145790592 @default.
- W2053516099 cites W2148649599 @default.
- W2053516099 cites W2312479243 @default.
- W2053516099 cites W2328467696 @default.
- W2053516099 cites W2489851730 @default.
- W2053516099 doi "https://doi.org/10.1016/j.marchem.2004.02.014" @default.
- W2053516099 hasPublicationYear "2004" @default.
- W2053516099 type Work @default.
- W2053516099 sameAs 2053516099 @default.
- W2053516099 citedByCount "122" @default.
- W2053516099 countsByYear W20535160992012 @default.
- W2053516099 countsByYear W20535160992013 @default.
- W2053516099 countsByYear W20535160992014 @default.
- W2053516099 countsByYear W20535160992015 @default.
- W2053516099 countsByYear W20535160992016 @default.
- W2053516099 countsByYear W20535160992017 @default.
- W2053516099 countsByYear W20535160992018 @default.
- W2053516099 countsByYear W20535160992019 @default.
- W2053516099 countsByYear W20535160992020 @default.
- W2053516099 countsByYear W20535160992021 @default.
- W2053516099 countsByYear W20535160992022 @default.
- W2053516099 countsByYear W20535160992023 @default.
- W2053516099 crossrefType "journal-article" @default.
- W2053516099 hasAuthorship W2053516099A5015998530 @default.
- W2053516099 hasAuthorship W2053516099A5026956124 @default.
- W2053516099 hasAuthorship W2053516099A5049495080 @default.
- W2053516099 hasConcept C107872376 @default.
- W2053516099 hasConcept C111368507 @default.
- W2053516099 hasConcept C127313418 @default.
- W2053516099 hasConcept C142796444 @default.
- W2053516099 hasConcept C158787203 @default.
- W2053516099 hasConcept C185592680 @default.
- W2053516099 hasConcept C187320778 @default.
- W2053516099 hasConcept C18903297 @default.
- W2053516099 hasConcept C24245907 @default.
- W2053516099 hasConcept C2778810354 @default.
- W2053516099 hasConcept C2780892065 @default.
- W2053516099 hasConcept C2993636123 @default.
- W2053516099 hasConcept C36574619 @default.
- W2053516099 hasConcept C39432304 @default.
- W2053516099 hasConcept C76886044 @default.
- W2053516099 hasConcept C86803240 @default.
- W2053516099 hasConcept C88160329 @default.
- W2053516099 hasConceptScore W2053516099C107872376 @default.
- W2053516099 hasConceptScore W2053516099C111368507 @default.
- W2053516099 hasConceptScore W2053516099C127313418 @default.
- W2053516099 hasConceptScore W2053516099C142796444 @default.
- W2053516099 hasConceptScore W2053516099C158787203 @default.
- W2053516099 hasConceptScore W2053516099C185592680 @default.
- W2053516099 hasConceptScore W2053516099C187320778 @default.