FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2068694429> ?p ?o ?g. }

• W2068694429 endingPage "166" @default.
• W2068694429 startingPage "157" @default.
• W2068694429 abstract "Geochemical and petrographical analyses were done in 26 surficial sediment samples from Mejillones Bay (northern Chile) to investigate the processes that participate in the preservation of sedimentary organic matter. Annual variability of chlorophyll-a and DIC δ13C measured in surface waters of three different parts of Mejillones Bay did not show any significant spatial variability in biological productivity. On the other hand, bottom dissolved oxygen showed strong changes associated with water depth and season. Surface sediment composition was statistically analyzed displaying organic facies, which are in agreement with the principal zones of bottom oxygenation (annual mean condition) identified in this bay. In the oxic coastal zone (> 1 ml l− 1) the total carbon (TC), total nitrogen (TN), total organic carbon (TOC), hydrogen index (HI) and oxygen index (OI) were 1.3%, 0.1%, 0.4%, 355.8 mg HC/g TOC and 237.6 mg CO2/g TOC, respectively. These results and the presence of almost exclusively dispersed amorphous organic matter suggest an environment where most metabolizable organic matter is degraded within the water-column and/or in the sediment water interface. In the microxic hemipelagic zone (< 0.1 ml l− 1), located deeper than 65 m, the TC, TN, TOC, HI and OI were 10.5%, 1.0%, 6.6%, 529.7 mg HC/g TOC and 103.1 mg CO2/g TOC, respectively. These values and the presence of abundant agglomerated amorphous organic matter suggest a better preservation of metabolizable and non-metabolizable compounds. We can conclude that biological productivity and dissolved oxygen exert a similar influence on the sedimentary organic matter, but the characteristics and quantity of organic material preserved in bottom sediments of this bay are controlled, principally, by the availability of dissolved oxygen at the sediment–water interface. According to this conclusion, we suggest that the sedimentary record of Mejillones Bay must be interpreted in paleoceanographic terms primarily in relation to the temporal variability of dissolved oxygen, more than biological productivity. The OI seems to be a good proxy of paleoxygenation in this coastal system." @default.
• W2068694429 created "2016-06-24" @default.
• W2068694429 creator A5039091058 @default.
• W2068694429 creator A5051276311 @default.
• W2068694429 creator A5057740350 @default.
• W2068694429 creator A5064979036 @default.
• W2068694429 date "2009-09-01" @default.
• W2068694429 modified "2023-10-10" @default.
• W2068694429 title "Interplay between sedimentary organic matter and dissolved oxygen availability in a coastal zone of the Humboldt Current System; Mejillones Bay, northern Chile" @default.
• W2068694429 cites W1498526448 @default.
• W2068694429 cites W1553347294 @default.
• W2068694429 cites W1970347133 @default.
• W2068694429 cites W1973691303 @default.
• W2068694429 cites W1975669272 @default.
• W2068694429 cites W1988490427 @default.
• W2068694429 cites W1997338331 @default.
• W2068694429 cites W2000208071 @default.
• W2068694429 cites W2002078974 @default.
• W2068694429 cites W2004361138 @default.
• W2068694429 cites W2009657375 @default.
• W2068694429 cites W2014088934 @default.
• W2068694429 cites W2015588081 @default.
• W2068694429 cites W2016822223 @default.
• W2068694429 cites W2017529503 @default.
• W2068694429 cites W2022965257 @default.
• W2068694429 cites W2025666086 @default.
• W2068694429 cites W2039391119 @default.
• W2068694429 cites W2041559800 @default.
• W2068694429 cites W2042899316 @default.
• W2068694429 cites W2045066120 @default.
• W2068694429 cites W2045414140 @default.
• W2068694429 cites W2050130572 @default.
• W2068694429 cites W2050670879 @default.
• W2068694429 cites W2054968094 @default.
• W2068694429 cites W2058772564 @default.
• W2068694429 cites W2059109340 @default.
• W2068694429 cites W2065620784 @default.
• W2068694429 cites W2065673834 @default.
• W2068694429 cites W2070606963 @default.
• W2068694429 cites W2081893898 @default.
• W2068694429 cites W2097106372 @default.
• W2068694429 cites W2097724472 @default.
• W2068694429 cites W2129355929 @default.
• W2068694429 cites W2146003002 @default.
• W2068694429 cites W2155842996 @default.
• W2068694429 cites W2162316927 @default.
• W2068694429 cites W2490512164 @default.
• W2068694429 doi "https://doi.org/10.1016/j.margeo.2009.07.004" @default.
• W2068694429 hasPublicationYear "2009" @default.
• W2068694429 type Work @default.
• W2068694429 sameAs 2068694429 @default.
• W2068694429 citedByCount "16" @default.
• W2068694429 countsByYear W20686944292012 @default.
• W2068694429 countsByYear W20686944292014 @default.
• W2068694429 countsByYear W20686944292015 @default.
• W2068694429 countsByYear W20686944292019 @default.
• W2068694429 countsByYear W20686944292021 @default.
• W2068694429 countsByYear W20686944292022 @default.
• W2068694429 countsByYear W20686944292023 @default.
• W2068694429 crossrefType "journal-article" @default.
• W2068694429 hasAuthorship W2068694429A5039091058 @default.
• W2068694429 hasAuthorship W2068694429A5051276311 @default.
• W2068694429 hasAuthorship W2068694429A5057740350 @default.
• W2068694429 hasAuthorship W2068694429A5064979036 @default.
• W2068694429 hasConcept C107872376 @default.
• W2068694429 hasConcept C111368507 @default.
• W2068694429 hasConcept C114793014 @default.
• W2068694429 hasConcept C115880899 @default.
• W2068694429 hasConcept C122846477 @default.
• W2068694429 hasConcept C127313418 @default.
• W2068694429 hasConcept C139719470 @default.
• W2068694429 hasConcept C149348798 @default.
• W2068694429 hasConcept C158787203 @default.
• W2068694429 hasConcept C162324750 @default.
• W2068694429 hasConcept C185592680 @default.
• W2068694429 hasConcept C18903297 @default.
• W2068694429 hasConcept C204983608 @default.
• W2068694429 hasConcept C2780134711 @default.
• W2068694429 hasConcept C2780173749 @default.
• W2068694429 hasConcept C2780275952 @default.
• W2068694429 hasConcept C2816523 @default.
• W2068694429 hasConcept C36574619 @default.
• W2068694429 hasConcept C39432304 @default.
• W2068694429 hasConcept C48743137 @default.
• W2068694429 hasConcept C86803240 @default.
• W2068694429 hasConceptScore W2068694429C107872376 @default.
• W2068694429 hasConceptScore W2068694429C111368507 @default.
• W2068694429 hasConceptScore W2068694429C114793014 @default.
• W2068694429 hasConceptScore W2068694429C115880899 @default.
• W2068694429 hasConceptScore W2068694429C122846477 @default.
• W2068694429 hasConceptScore W2068694429C127313418 @default.
• W2068694429 hasConceptScore W2068694429C139719470 @default.
• W2068694429 hasConceptScore W2068694429C149348798 @default.
• W2068694429 hasConceptScore W2068694429C158787203 @default.
• W2068694429 hasConceptScore W2068694429C162324750 @default.
• W2068694429 hasConceptScore W2068694429C185592680 @default.
• W2068694429 hasConceptScore W2068694429C18903297 @default.
• W2068694429 hasConceptScore W2068694429C204983608 @default.

• next