FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4311138021> ?p ?o ?g. }

• W4311138021 endingPage "104539" @default.
• W4311138021 startingPage "104539" @default.
• W4311138021 abstract "The percentage of C37:4 alkenone relative to total C37 alkenones (C37:4%) in northern high-latitude ocean waters and surface sediments, which can be up to 77%, has been recently found to correlate strongly with annual mean sea ice coverage. Genomic data and culture experiments suggest these high percentage of C37:4 alkenones may be mainly attributed to the production by Group 2i Isochrysidales, because the cosmopolitan Isochrysidales, Emiliania huxleyi (recently renamed to Gephyrocapsa huxleyi) typically does not produce significant amount of C37:4 alkenone in laboratory cultures. However, the presence of significant amounts of C38 methyl alkenones in high-latitude ocean sediments and suspended particulate samples suggests possible contributions from G. huxleyi as well. Here we performed the first culture experiments on G. huxleyi strain NIES3366 from the Chukchi Sea. This strain was isolated from the coldest and highest latitude ocean waters known for G. huxleyi strains so far. NIES1312 from the Bering Sea was also cultured under identical conditions for comparison. We show that, in f/2 growth media, NIES3366 was capable of producing unusually large amounts of C37:4 alkenone reaching 12.8% at 12 °C and up to 20% between 6 °C and 9 °C. In comparison, NIES1312 only produced 3.6% C37:4 at 12 °C. Our results suggest that Arctic strains of G. huxleyi may have also contribute to the inventory of the high-C37:4 alkenone profile in northern high-latitude oceans. Importantly, however, when NIES3366 was grown in 10 times lower nutrient (f/20) at 12 °C, the C37:4% decreased by ∼ 50% (to 6%), indicating a strong impact of nutrients on the production of C37:4 alkenone. In contrast, salinity levels had a negligible impact on the percentage of C37:4 for both strains, indicating an absence of a physiological effect of salinity. We also demonstrate that at low temperatures, tetra-unsaturated alkenones must be included for calculating unsaturation indices to achieve strong linear correlation with temperatures for NIES3366, a feature contrary to other G. huxleyi strains isolated from mid- and low- latitude oceans. Our findings provide a refined mechanistic explanation for the application of alkenone C37:4% as a quantitative sea ice proxy in high-latitude oceans." @default.
• W4311138021 created "2022-12-23" @default.
• W4311138021 creator A5052005893 @default.
• W4311138021 creator A5084347331 @default.
• W4311138021 creator A5089852706 @default.
• W4311138021 date "2023-03-01" @default.
• W4311138021 modified "2023-10-14" @default.
• W4311138021 title "Unusually high production of C37:4 alkenone by an Arctic Gephyrocapsa huxleyi strain grown under nutrient-replete conditions" @default.
• W4311138021 cites W1505094049 @default.
• W4311138021 cites W1524215045 @default.
• W4311138021 cites W1582736910 @default.
• W4311138021 cites W1602868930 @default.
• W4311138021 cites W1638007290 @default.
• W4311138021 cites W1658032313 @default.
• W4311138021 cites W1810959483 @default.
• W4311138021 cites W1983186777 @default.
• W4311138021 cites W1991795942 @default.
• W4311138021 cites W1996736897 @default.
• W4311138021 cites W2014646959 @default.
• W4311138021 cites W2016269445 @default.
• W4311138021 cites W2019920563 @default.
• W4311138021 cites W2032482799 @default.
• W4311138021 cites W2053251742 @default.
• W4311138021 cites W2083392509 @default.
• W4311138021 cites W2084682724 @default.
• W4311138021 cites W2086155711 @default.
• W4311138021 cites W2091232642 @default.
• W4311138021 cites W2091284813 @default.
• W4311138021 cites W2115280287 @default.
• W4311138021 cites W2116367889 @default.
• W4311138021 cites W2130748065 @default.
• W4311138021 cites W2131805843 @default.
• W4311138021 cites W2138348889 @default.
• W4311138021 cites W2140677888 @default.
• W4311138021 cites W2142487983 @default.
• W4311138021 cites W2142573446 @default.
• W4311138021 cites W2148618833 @default.
• W4311138021 cites W2156739270 @default.
• W4311138021 cites W2165158548 @default.
• W4311138021 cites W2172478393 @default.
• W4311138021 cites W2284181245 @default.
• W4311138021 cites W2298295142 @default.
• W4311138021 cites W2370662695 @default.
• W4311138021 cites W2726007953 @default.
• W4311138021 cites W2792554943 @default.
• W4311138021 cites W2807585016 @default.
• W4311138021 cites W2885012396 @default.
• W4311138021 cites W2903074401 @default.
• W4311138021 cites W2905666875 @default.
• W4311138021 cites W2953976140 @default.
• W4311138021 cites W2973563149 @default.
• W4311138021 cites W2974442572 @default.
• W4311138021 cites W2974659188 @default.
• W4311138021 cites W3040902116 @default.
• W4311138021 cites W3043108592 @default.
• W4311138021 cites W3047185420 @default.
• W4311138021 cites W3197023342 @default.
• W4311138021 cites W3211436343 @default.
• W4311138021 cites W4224879840 @default.
• W4311138021 cites W4306742456 @default.
• W4311138021 doi "https://doi.org/10.1016/j.orggeochem.2022.104539" @default.
• W4311138021 hasPublicationYear "2023" @default.
• W4311138021 type Work @default.
• W4311138021 citedByCount "2" @default.
• W4311138021 countsByYear W43111380212023 @default.
• W4311138021 crossrefType "journal-article" @default.
• W4311138021 hasAuthorship W4311138021A5052005893 @default.
• W4311138021 hasAuthorship W4311138021A5084347331 @default.
• W4311138021 hasAuthorship W4311138021A5089852706 @default.
• W4311138021 hasConcept C111368507 @default.
• W4311138021 hasConcept C122523270 @default.
• W4311138021 hasConcept C127313418 @default.
• W4311138021 hasConcept C13280743 @default.
• W4311138021 hasConcept C134097258 @default.
• W4311138021 hasConcept C142796444 @default.
• W4311138021 hasConcept C18903297 @default.
• W4311138021 hasConcept C2777066016 @default.
• W4311138021 hasConcept C2777339954 @default.
• W4311138021 hasConcept C2780892065 @default.
• W4311138021 hasConcept C518008717 @default.
• W4311138021 hasConcept C86803240 @default.
• W4311138021 hasConceptScore W4311138021C111368507 @default.
• W4311138021 hasConceptScore W4311138021C122523270 @default.
• W4311138021 hasConceptScore W4311138021C127313418 @default.
• W4311138021 hasConceptScore W4311138021C13280743 @default.
• W4311138021 hasConceptScore W4311138021C134097258 @default.
• W4311138021 hasConceptScore W4311138021C142796444 @default.
• W4311138021 hasConceptScore W4311138021C18903297 @default.
• W4311138021 hasConceptScore W4311138021C2777066016 @default.
• W4311138021 hasConceptScore W4311138021C2777339954 @default.
• W4311138021 hasConceptScore W4311138021C2780892065 @default.
• W4311138021 hasConceptScore W4311138021C518008717 @default.
• W4311138021 hasConceptScore W4311138021C86803240 @default.
• W4311138021 hasFunder F4320306076 @default.
• W4311138021 hasLocation W43111380211 @default.
• W4311138021 hasOpenAccess W4311138021 @default.
• W4311138021 hasPrimaryLocation W43111380211 @default.
• W4311138021 hasRelatedWork W1524215045 @default.

• next