FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2000673314> ?p ?o ?g. }

• W2000673314 endingPage "70" @default.
• W2000673314 startingPage "57" @default.
• W2000673314 abstract "MEPS Marine Ecology Progress Series Contact the journal Facebook Twitter RSS Mailing List Subscribe to our mailing list via Mailchimp HomeLatest VolumeAbout the JournalEditorsTheme Sections MEPS 478:57-70 (2013) - DOI: https://doi.org/10.3354/meps10040 Denitrification, anammox and nitrate reduction in sediments of the southern Great Barrier Reef lagoon Dirk V. Erler*,1, Lindsay A. Trott2, Daniel M. Alongi2, Bradley D. Eyre1 1Centre for Coastal Biogeochemistry, School of Environmental Science and Management, Southern Cross University, Lismore NSW 2480, Australia. 2Australian Institute of Marine Science, PMB 3, Townsville MC QLD 4810, Australia *Email: dirk.erler@scu.edu.au ABSTRACT: We provide the first reported estimates of anammox activity in tropical continental shelf sediments (southern section of the Great Barrier Reef lagoon; GBRL). The measured contribution of anammox to total N2 production was up to 70% but restricted to only 1 of the 4 (2 inshore and 2 offshore) sites assayed. Sediment characteristics (contents of total organic carbon [TOC] and manganese [Mn], C:N ratio) at this site appeared to favour anammox activity and the estimated maximum rate was 4.9 µmol m-2 h-1. Anammox bacteria may be a significant contributor to N2 production along the coastal zone of the GBRL. The availability of labile (low C:N) TOC seemed to drive denitrification to completion in the offshore sediments. However, rates of NO3- reduction to NH4+ at the offshore sites were comparable to or higher than denitrification rates. It was unclear whether dissimilatory or assimilatory processes were responsible for the observed reduction of NO3- to NH4+ at the offshore sites. At the 2 inshore sites, NO3- reduction to NH4+ was a larger sink for NO3- than denitrification. Anammox does exist in the tropical continental shelf sediments of the GBRL and should be studied further to determine its role in larger scale N cycling. The roles of assimilatory and dissimilatory nitrate reduction to ammonium also need to be assessed within the GBRL. KEY WORDS: Great Barrier Reef · Anammox · Dissimilatory/assimilatory nitrate reduction to ammonia · Denitrification Full text in pdf format PreviousNextCite this article as: Erler DV, Trott LA, Alongi DM, Eyre BD (2013) Denitrification, anammox and nitrate reduction in sediments of the southern Great Barrier Reef lagoon. Mar Ecol Prog Ser 478:57-70. https://doi.org/10.3354/meps10040 Export citation RSS - Facebook - Tweet - linkedIn Cited by Published in MEPS Vol. 478. Online publication date: March 25, 2013 Print ISSN: 0171-8630; Online ISSN: 1616-1599 Copyright © 2013 Inter-Research." @default.
• W2000673314 created "2016-06-24" @default.
• W2000673314 creator A5011735601 @default.
• W2000673314 creator A5026721577 @default.
• W2000673314 creator A5042240513 @default.
• W2000673314 creator A5077040357 @default.
• W2000673314 date "2013-03-25" @default.
• W2000673314 modified "2023-10-14" @default.
• W2000673314 title "Denitrification, anammox and nitrate reduction in sediments of the southern Great Barrier Reef lagoon" @default.
• W2000673314 cites W1544386505 @default.
• W2000673314 cites W1967904323 @default.
• W2000673314 cites W1982267887 @default.
• W2000673314 cites W1989048534 @default.
• W2000673314 cites W1991465668 @default.
• W2000673314 cites W1998652560 @default.
• W2000673314 cites W2000793063 @default.
• W2000673314 cites W2009815697 @default.
• W2000673314 cites W2012358502 @default.
• W2000673314 cites W2024349221 @default.
• W2000673314 cites W2027318176 @default.
• W2000673314 cites W2031571844 @default.
• W2000673314 cites W2035518975 @default.
• W2000673314 cites W2048342577 @default.
• W2000673314 cites W2054178484 @default.
• W2000673314 cites W2063529400 @default.
• W2000673314 cites W2080767659 @default.
• W2000673314 cites W2080944095 @default.
• W2000673314 cites W2094189933 @default.
• W2000673314 cites W2101148706 @default.
• W2000673314 cites W2103523209 @default.
• W2000673314 cites W2104229340 @default.
• W2000673314 cites W2106143747 @default.
• W2000673314 cites W2110701998 @default.
• W2000673314 cites W2119097801 @default.
• W2000673314 cites W2120777049 @default.
• W2000673314 cites W2122911960 @default.
• W2000673314 cites W2123136455 @default.
• W2000673314 cites W2138538269 @default.
• W2000673314 cites W2146538520 @default.
• W2000673314 cites W2151157461 @default.
• W2000673314 cites W2159502644 @default.
• W2000673314 cites W2162485441 @default.
• W2000673314 cites W2165798555 @default.
• W2000673314 cites W2171070596 @default.
• W2000673314 cites W2171761799 @default.
• W2000673314 cites W4229735386 @default.
• W2000673314 cites W4233853379 @default.
• W2000673314 cites W4238820525 @default.
• W2000673314 cites W4240130016 @default.
• W2000673314 cites W4242274296 @default.
• W2000673314 cites W4245689640 @default.
• W2000673314 doi "https://doi.org/10.3354/meps10040" @default.
• W2000673314 hasPublicationYear "2013" @default.
• W2000673314 type Work @default.
• W2000673314 sameAs 2000673314 @default.
• W2000673314 citedByCount "16" @default.
• W2000673314 countsByYear W20006733142012 @default.
• W2000673314 countsByYear W20006733142013 @default.
• W2000673314 countsByYear W20006733142014 @default.
• W2000673314 countsByYear W20006733142015 @default.
• W2000673314 countsByYear W20006733142016 @default.
• W2000673314 countsByYear W20006733142017 @default.
• W2000673314 countsByYear W20006733142018 @default.
• W2000673314 countsByYear W20006733142019 @default.
• W2000673314 countsByYear W20006733142020 @default.
• W2000673314 countsByYear W20006733142021 @default.
• W2000673314 crossrefType "journal-article" @default.
• W2000673314 hasAuthorship W2000673314A5011735601 @default.
• W2000673314 hasAuthorship W2000673314A5026721577 @default.
• W2000673314 hasAuthorship W2000673314A5042240513 @default.
• W2000673314 hasAuthorship W2000673314A5077040357 @default.
• W2000673314 hasBestOaLocation W20006733141 @default.
• W2000673314 hasConcept C107872376 @default.
• W2000673314 hasConcept C111368507 @default.
• W2000673314 hasConcept C127313418 @default.
• W2000673314 hasConcept C130309983 @default.
• W2000673314 hasConcept C151730666 @default.
• W2000673314 hasConcept C158787203 @default.
• W2000673314 hasConcept C178790620 @default.
• W2000673314 hasConcept C184751465 @default.
• W2000673314 hasConcept C185592680 @default.
• W2000673314 hasConcept C18903297 @default.
• W2000673314 hasConcept C197011783 @default.
• W2000673314 hasConcept C2776384668 @default.
• W2000673314 hasConcept C2816523 @default.
• W2000673314 hasConcept C39432304 @default.
• W2000673314 hasConcept C537208039 @default.
• W2000673314 hasConcept C54776530 @default.
• W2000673314 hasConcept C73593433 @default.
• W2000673314 hasConcept C77044568 @default.
• W2000673314 hasConcept C86803240 @default.
• W2000673314 hasConceptScore W2000673314C107872376 @default.
• W2000673314 hasConceptScore W2000673314C111368507 @default.
• W2000673314 hasConceptScore W2000673314C127313418 @default.
• W2000673314 hasConceptScore W2000673314C130309983 @default.
• W2000673314 hasConceptScore W2000673314C151730666 @default.
• W2000673314 hasConceptScore W2000673314C158787203 @default.
• W2000673314 hasConceptScore W2000673314C178790620 @default.

• next