Matches in SemOpenAlex for { <https://semopenalex.org/work/W2130514538> ?p ?o ?g. }
- W2130514538 endingPage "219" @default.
- W2130514538 startingPage "203" @default.
- W2130514538 abstract "The oxidation of organic matter in relation to porewater and solid-phase element chemistry was examined in mixed terrigenous-carbonate sediments in sheltered and exposed lagoons of Ningaloo Reef, Western Australia. Rates of O2 consumption and CO2 release were faster in the very fine sand (41–43% CaCO3 content) of the sheltered lagoon of Mangrove Bay (means = 10.5 mmolm−2day−1 O2 and 9.4mmolm−2day−1 CO2) than in the carbonate-rich (73% CaCO3) sand of the exposed back-reef lagoon of Ningaloo Reef (means = 2.1 mmolm−2 day−1 O2 and 3.5 mmolm−2 day−1 CO2). Rates of sulfate reduction (ΣSRR) were similarly faster in the Mangrove Bay sediments (6.1–25.3 mmolm−2day−1 S), sufficient to account for all of the organic matter mineralization. In Ningaloo reef sands, ΣSRR rates (1.0 mmol m−2 day−1 S) accounted for a significant fraction (57%) of total organic carbon oxidation. In Mangrove Bay, in contrast to previous measurements of sulfate reduction in tropical sediments, most (mean = 64%) of the reduced 35S was incorporated into the acid-volatile sulflde fraction with a buildup of iron sulfides. In contrast to most carbonate-bearing sediments, the production and accumulation of Fe sulfides (most evident in Mangrove Bay) increased pH to levels promoting carbonate precipitation. Higher decomposition rates in Mangrove Bay are attributed to restricted water circulation, a richer benthic community, and geomorphology conducive to greater input and retention of mangrove- and macroalgae-derived detritus. At both sites, the lack of a clear zonational sequence of porewater solutes, discrepancies between depth profiles of solutes and solid-phase elements, and high core-to-core variation in conservative element concentrations and in rates of bacterial activity, suggest non-steady state diagenesis. Non-steady state conditions may be fostered by a combination of factors, such as physical disturbances, temporal changes in rates and quality of organic sedimentation, and tidal advection." @default.
- W2130514538 created "2016-06-24" @default.
- W2130514538 creator A5022503288 @default.
- W2130514538 creator A5026721577 @default.
- W2130514538 creator A5032746776 @default.
- W2130514538 date "1996-10-01" @default.
- W2130514538 modified "2023-10-06" @default.
- W2130514538 title "Organic matter oxidation and sediment chemistry in mixed terrigenous-carbonate sands of Ningaloo Reef, Western Australia" @default.
- W2130514538 cites W1964215238 @default.
- W2130514538 cites W1964901884 @default.
- W2130514538 cites W1966265157 @default.
- W2130514538 cites W1972304614 @default.
- W2130514538 cites W1976805835 @default.
- W2130514538 cites W1978990622 @default.
- W2130514538 cites W1988349791 @default.
- W2130514538 cites W1989323664 @default.
- W2130514538 cites W1992364148 @default.
- W2130514538 cites W1994069627 @default.
- W2130514538 cites W1994614753 @default.
- W2130514538 cites W2004570116 @default.
- W2130514538 cites W2006113617 @default.
- W2130514538 cites W2007562615 @default.
- W2130514538 cites W2015104607 @default.
- W2130514538 cites W2021673628 @default.
- W2130514538 cites W2027326094 @default.
- W2130514538 cites W2029474731 @default.
- W2130514538 cites W2031304694 @default.
- W2130514538 cites W2031357690 @default.
- W2130514538 cites W2033942831 @default.
- W2130514538 cites W2035398133 @default.
- W2130514538 cites W2049508310 @default.
- W2130514538 cites W2053251028 @default.
- W2130514538 cites W2054645658 @default.
- W2130514538 cites W2056392157 @default.
- W2130514538 cites W2062740593 @default.
- W2130514538 cites W2063425499 @default.
- W2130514538 cites W2063704593 @default.
- W2130514538 cites W2065450971 @default.
- W2130514538 cites W2065538499 @default.
- W2130514538 cites W2069410810 @default.
- W2130514538 cites W2073678840 @default.
- W2130514538 cites W2077140170 @default.
- W2130514538 cites W2083311533 @default.
- W2130514538 cites W2090525362 @default.
- W2130514538 cites W2101606013 @default.
- W2130514538 cites W2125776675 @default.
- W2130514538 cites W2130490621 @default.
- W2130514538 cites W2323431606 @default.
- W2130514538 cites W2330059339 @default.
- W2130514538 doi "https://doi.org/10.1016/0304-4203(96)00037-0" @default.
- W2130514538 hasPublicationYear "1996" @default.
- W2130514538 type Work @default.
- W2130514538 sameAs 2130514538 @default.
- W2130514538 citedByCount "48" @default.
- W2130514538 countsByYear W21305145382012 @default.
- W2130514538 countsByYear W21305145382013 @default.
- W2130514538 countsByYear W21305145382014 @default.
- W2130514538 countsByYear W21305145382015 @default.
- W2130514538 countsByYear W21305145382016 @default.
- W2130514538 countsByYear W21305145382017 @default.
- W2130514538 countsByYear W21305145382018 @default.
- W2130514538 countsByYear W21305145382019 @default.
- W2130514538 countsByYear W21305145382020 @default.
- W2130514538 countsByYear W21305145382021 @default.
- W2130514538 countsByYear W21305145382022 @default.
- W2130514538 countsByYear W21305145382023 @default.
- W2130514538 crossrefType "journal-article" @default.
- W2130514538 hasAuthorship W2130514538A5022503288 @default.
- W2130514538 hasAuthorship W2130514538A5026721577 @default.
- W2130514538 hasAuthorship W2130514538A5032746776 @default.
- W2130514538 hasConcept C107872376 @default.
- W2130514538 hasConcept C111368507 @default.
- W2130514538 hasConcept C114793014 @default.
- W2130514538 hasConcept C115880899 @default.
- W2130514538 hasConcept C127313418 @default.
- W2130514538 hasConcept C158787203 @default.
- W2130514538 hasConcept C178790620 @default.
- W2130514538 hasConcept C185592680 @default.
- W2130514538 hasConcept C18903297 @default.
- W2130514538 hasConcept C199285206 @default.
- W2130514538 hasConcept C2780659211 @default.
- W2130514538 hasConcept C2816523 @default.
- W2130514538 hasConcept C48743137 @default.
- W2130514538 hasConcept C68874143 @default.
- W2130514538 hasConcept C77044568 @default.
- W2130514538 hasConcept C83042747 @default.
- W2130514538 hasConcept C86803240 @default.
- W2130514538 hasConceptScore W2130514538C107872376 @default.
- W2130514538 hasConceptScore W2130514538C111368507 @default.
- W2130514538 hasConceptScore W2130514538C114793014 @default.
- W2130514538 hasConceptScore W2130514538C115880899 @default.
- W2130514538 hasConceptScore W2130514538C127313418 @default.
- W2130514538 hasConceptScore W2130514538C158787203 @default.
- W2130514538 hasConceptScore W2130514538C178790620 @default.
- W2130514538 hasConceptScore W2130514538C185592680 @default.
- W2130514538 hasConceptScore W2130514538C18903297 @default.
- W2130514538 hasConceptScore W2130514538C199285206 @default.
- W2130514538 hasConceptScore W2130514538C2780659211 @default.