FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W1904466915> ?p ?o ?g. }

• W1904466915 endingPage "300" @default.
• W1904466915 startingPage "287" @default.
• W1904466915 abstract "Abstract The isotopic, taxonomic, and nutrient dynamics of protist communities at the bottom of first‐year sea ice were studied for a wide range of ice conditions during the spring‐summer transition in the southeast Beaufort Sea. In bottom ice, total protist abundance ranged from 0.07 to 9.94 × 10 9 cells m –2 and chlorophyll a biomass ranged from 0.33 to 110 mg m –2 . Both variables were positively related to the concentrations of nitrate, silicic acid, and phosphate at the ice‐water interface, with r 2 values between 0.63 and 0.79. Results showed that the δ 13 C of sympagic (ice‐associated) particulate organic matter (POM) (–27.1 to –11.4‰) was mainly influenced by ice protist stocks and dissolved inorganic carbon availability. Flagellated cells maintained a low δ 13 C relative to diatoms. The δ 15 N of POM (3.9 to 9.4‰) could not be explained by any of the variables considered and showed considerable overlap with the pelagic δ 15 N‐POM (0.0 to 10.3‰). Detailed analyses of δ 13 C‐POM through size fractionation and settling experiments along with a short temporal study of the interaction between sympagic and pelagic communities confirmed or demonstrated that (1) the analysis of stable C isotopes is a valuable tool to trace the flow of ice‐derived matter, (2) sympagic POM contributes substantially to suspended pelagic biomass during release episodes, and (3) ice‐grown autotrophic flagellated cells have a strong potential to interact with the pelagic biota in the coastal Arctic Ocean. This study highlights the need to carefully evaluate stable isotope dynamics before assessing food web interactions or the fate of POM in seasonally ice‐covered waters." @default.
• W1904466915 created "2016-06-24" @default.
• W1904466915 creator A5027045277 @default.
• W1904466915 creator A5030032880 @default.
• W1904466915 creator A5057801751 @default.
• W1904466915 creator A5069562070 @default.
• W1904466915 creator A5087722620 @default.
• W1904466915 date "2013-01-01" @default.
• W1904466915 modified "2023-10-10" @default.
• W1904466915 title "The isotopic signature of particulate organic C and N in bottom ice: Key influencing factors and applications for tracing the fate of ice-algae in the Arctic Ocean" @default.
• W1904466915 cites W1488593324 @default.
• W1904466915 cites W1498931160 @default.
• W1904466915 cites W1510135386 @default.
• W1904466915 cites W1527493714 @default.
• W1904466915 cites W1742743498 @default.
• W1904466915 cites W1965731782 @default.
• W1904466915 cites W1966283669 @default.
• W1904466915 cites W1968202111 @default.
• W1904466915 cites W1974184821 @default.
• W1904466915 cites W1974389325 @default.
• W1904466915 cites W1977300523 @default.
• W1904466915 cites W1981497577 @default.
• W1904466915 cites W1985234919 @default.
• W1904466915 cites W1989626736 @default.
• W1904466915 cites W1990491823 @default.
• W1904466915 cites W1994592705 @default.
• W1904466915 cites W1995445718 @default.
• W1904466915 cites W1997228500 @default.
• W1904466915 cites W2018294845 @default.
• W1904466915 cites W2019159344 @default.
• W1904466915 cites W2021834438 @default.
• W1904466915 cites W2023616293 @default.
• W1904466915 cites W2027935460 @default.
• W1904466915 cites W2028602355 @default.
• W1904466915 cites W2037008939 @default.
• W1904466915 cites W2038595833 @default.
• W1904466915 cites W2040114325 @default.
• W1904466915 cites W2041373162 @default.
• W1904466915 cites W2042456369 @default.
• W1904466915 cites W2043671557 @default.
• W1904466915 cites W2049501678 @default.
• W1904466915 cites W2051337798 @default.
• W1904466915 cites W2055112516 @default.
• W1904466915 cites W2058782129 @default.
• W1904466915 cites W2062496768 @default.
• W1904466915 cites W2067081409 @default.
• W1904466915 cites W2078241235 @default.
• W1904466915 cites W2080561235 @default.
• W1904466915 cites W2082304151 @default.
• W1904466915 cites W2086606199 @default.
• W1904466915 cites W2087056583 @default.
• W1904466915 cites W2087818650 @default.
• W1904466915 cites W2088676399 @default.
• W1904466915 cites W2094249522 @default.
• W1904466915 cites W2099647185 @default.
• W1904466915 cites W2103030963 @default.
• W1904466915 cites W2107149568 @default.
• W1904466915 cites W2109736220 @default.
• W1904466915 cites W2115384265 @default.
• W1904466915 cites W2122653354 @default.
• W1904466915 cites W2129543789 @default.
• W1904466915 cites W2144210118 @default.
• W1904466915 cites W2154754282 @default.
• W1904466915 cites W2167364795 @default.
• W1904466915 cites W2168390752 @default.
• W1904466915 cites W2621678793 @default.
• W1904466915 cites W322753937 @default.
• W1904466915 cites W4236127842 @default.
• W1904466915 doi "https://doi.org/10.1029/2012jc008331" @default.
• W1904466915 hasPublicationYear "2013" @default.
• W1904466915 type Work @default.
• W1904466915 sameAs 1904466915 @default.
• W1904466915 citedByCount "46" @default.
• W1904466915 countsByYear W19044669152013 @default.
• W1904466915 countsByYear W19044669152014 @default.
• W1904466915 countsByYear W19044669152015 @default.
• W1904466915 countsByYear W19044669152016 @default.
• W1904466915 countsByYear W19044669152017 @default.
• W1904466915 countsByYear W19044669152018 @default.
• W1904466915 countsByYear W19044669152019 @default.
• W1904466915 countsByYear W19044669152020 @default.
• W1904466915 countsByYear W19044669152021 @default.
• W1904466915 countsByYear W19044669152022 @default.
• W1904466915 countsByYear W19044669152023 @default.
• W1904466915 crossrefType "journal-article" @default.
• W1904466915 hasAuthorship W1904466915A5027045277 @default.
• W1904466915 hasAuthorship W1904466915A5030032880 @default.
• W1904466915 hasAuthorship W1904466915A5057801751 @default.
• W1904466915 hasAuthorship W1904466915A5069562070 @default.
• W1904466915 hasAuthorship W1904466915A5087722620 @default.
• W1904466915 hasBestOaLocation W19044669151 @default.
• W1904466915 hasConcept C107872376 @default.
• W1904466915 hasConcept C111368507 @default.
• W1904466915 hasConcept C121332964 @default.
• W1904466915 hasConcept C127313418 @default.
• W1904466915 hasConcept C136894858 @default.
• W1904466915 hasConcept C142796444 @default.
• W1904466915 hasConcept C146458902 @default.

• next