FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2579030943> ?p ?o ?g. }

• W2579030943 endingPage "159" @default.
• W2579030943 startingPage "143" @default.
• W2579030943 abstract "The Subantarctic Zone (SAZ) plays a crucial role in global carbon cycling as a significant sink for atmospheric CO 2 . In the Australian sector, the SAZ exports large quantities of organic carbon from the surface ocean, despite lower algal biomass accumulation in surface waters than other Southern Ocean sectors. We present the first analysis of diatom and coccolithophore assemblages and seasonality, as well as the first annual quantification of bulk organic components of captured material at the base of the mixed layer (500 m depth) in the SAZ. Sediment traps were moored in the SAZ southwest of Tasmania as part of the long-term SAZ Project for one year (September 2003 to September 2004). Annual mass flux at 500 m and 2000 m was composed mainly of calcium carbonate, while biogenic silica made up on average <10% of material captured in the traps. Organic carbon flux was estimated at 1.1 g m −2 y −1 at 500 m, close to the estimated global mean carbon flux. Low diatom fluxes and high fluxes of coccoliths were consistent with low biogenic silica and high calcium carbonate fluxes, respectively. Diatoms and coccoliths were identified to species level. Diatom and coccolithophore sinking assemblages reflected some seasonal ecological succession. A theoretical scheme of diatom succession in live assemblages is compared to successional patterns presented in sediment traps. This study provides a unique, direct measurement of the biogeochemical fluxes and their main biological carbon vectors just below the winter mixed layer depth at which effective sequestration of carbon occurs. Comparison of these results with previous sediment trap deployments at the same site at deeper depths (i.e. 1000, 2000 and 3800 m) documents the changes particle fluxes experience in the lower “twilight zone” where biological processes and remineralisation of carbon reduce the efficiency of carbon sequestration. • Organic carbon flux was at 1.1 g m −2 y −1 at 500 m, close to the estimated global value. • Annual total mass flux was carbonate-dominated, reflecting high coccolithophore abundance. • Sediment trap assemblages were consistent with live diatom and coccolithophore communities. • Diatom and coccolithophore sinking assemblages reflected some seasonal ecological succession." @default.
• W2579030943 created "2017-01-26" @default.
• W2579030943 creator A5011063307 @default.
• W2579030943 creator A5031900731 @default.
• W2579030943 creator A5048027882 @default.
• W2579030943 creator A5048530627 @default.
• W2579030943 creator A5077795508 @default.
• W2579030943 creator A5082449571 @default.
• W2579030943 date "2017-03-01" @default.
• W2579030943 modified "2023-10-17" @default.
• W2579030943 title "Biogeochemical flux and phytoplankton succession: A year-long sediment trap record in the Australian sector of the Subantarctic Zone" @default.
• W2579030943 cites W1483305579 @default.
• W2579030943 cites W1502819700 @default.
• W2579030943 cites W1610088203 @default.
• W2579030943 cites W1636679337 @default.
• W2579030943 cites W1637244524 @default.
• W2579030943 cites W1649447126 @default.
• W2579030943 cites W1673314509 @default.
• W2579030943 cites W1871116690 @default.
• W2579030943 cites W1963675853 @default.
• W2579030943 cites W1968911577 @default.
• W2579030943 cites W1972704645 @default.
• W2579030943 cites W1974006045 @default.
• W2579030943 cites W1974153247 @default.
• W2579030943 cites W1975337812 @default.
• W2579030943 cites W1976160439 @default.
• W2579030943 cites W1976365567 @default.
• W2579030943 cites W1977741114 @default.
• W2579030943 cites W1977936220 @default.
• W2579030943 cites W1979302457 @default.
• W2579030943 cites W1979837403 @default.
• W2579030943 cites W1980637674 @default.
• W2579030943 cites W1983557286 @default.
• W2579030943 cites W1985707658 @default.
• W2579030943 cites W1988780671 @default.
• W2579030943 cites W1989327580 @default.
• W2579030943 cites W1989812709 @default.
• W2579030943 cites W1994808750 @default.
• W2579030943 cites W1995212325 @default.
• W2579030943 cites W1995372369 @default.
• W2579030943 cites W1995881129 @default.
• W2579030943 cites W2004359105 @default.
• W2579030943 cites W2006243920 @default.
• W2579030943 cites W2010587901 @default.
• W2579030943 cites W2011567753 @default.
• W2579030943 cites W2013045497 @default.
• W2579030943 cites W2013995291 @default.
• W2579030943 cites W2025507953 @default.
• W2579030943 cites W2031452471 @default.
• W2579030943 cites W2032682305 @default.
• W2579030943 cites W2034502216 @default.
• W2579030943 cites W2037971121 @default.
• W2579030943 cites W2041330813 @default.
• W2579030943 cites W2042893503 @default.
• W2579030943 cites W2044882040 @default.
• W2579030943 cites W2047352962 @default.
• W2579030943 cites W2047353257 @default.
• W2579030943 cites W2047461817 @default.
• W2579030943 cites W2049760601 @default.
• W2579030943 cites W2052202767 @default.
• W2579030943 cites W2058486476 @default.
• W2579030943 cites W2059316363 @default.
• W2579030943 cites W2061945692 @default.
• W2579030943 cites W2064899591 @default.
• W2579030943 cites W2066122888 @default.
• W2579030943 cites W2068449011 @default.
• W2579030943 cites W2069327439 @default.
• W2579030943 cites W2070707145 @default.
• W2579030943 cites W2072586896 @default.
• W2579030943 cites W2072609849 @default.
• W2579030943 cites W2073307266 @default.
• W2579030943 cites W2074084276 @default.
• W2579030943 cites W2075039156 @default.
• W2579030943 cites W2077812889 @default.
• W2579030943 cites W2077997882 @default.
• W2579030943 cites W2080922516 @default.
• W2579030943 cites W2081698385 @default.
• W2579030943 cites W2083848042 @default.
• W2579030943 cites W2085497384 @default.
• W2579030943 cites W2088104338 @default.
• W2579030943 cites W2088636794 @default.
• W2579030943 cites W2089056406 @default.
• W2579030943 cites W2098530244 @default.
• W2579030943 cites W2099924544 @default.
• W2579030943 cites W2105441522 @default.
• W2579030943 cites W2127531128 @default.
• W2579030943 cites W2144095328 @default.
• W2579030943 cites W2145259215 @default.
• W2579030943 cites W2155345800 @default.
• W2579030943 cites W2159840832 @default.
• W2579030943 cites W2284608533 @default.
• W2579030943 cites W2288751275 @default.
• W2579030943 cites W2297958963 @default.
• W2579030943 cites W2315911124 @default.
• W2579030943 cites W2411374435 @default.
• W2579030943 cites W2556425461 @default.
• W2579030943 cites W26651782 @default.
• W2579030943 cites W2707410288 @default.

• next