FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2090317838> ?p ?o ?g. }

• W2090317838 endingPage "59" @default.
• W2090317838 startingPage "43" @default.
• W2090317838 abstract "Three major depositional basins (the Gdansk, Bornholm and Eastern Gotland basins) of the Baltic Proper, which together account for >50% of the depositional areas in the entire Baltic Sea, have accumulated increased amounts of sediment and organic carbon during the last 50 years, as is shown in 210Pb-dated sediment cores. The shallow Arkona Basin has had constant accumulation rates and rate increases of bulk sediment, organic carbon and aluminium in the Bornholm Basin are parallel and are interpreted to reflect increased material input from land or from erosion of shallow-water areas. In the Gdansk and Eastern Gotland basins, the accumulation rates of mineral matter have risen at lower rates than those of organic carbon and point to preferential enrichment of organic matter. At increasing rates of burial, the material in the Gdansk and Eastern Gotland basins appears to have been depleted in phosphorus relative to nitrogen and organic carbon. Using C:N:P ratios from a sediment trap mooring in the Gotland Basin and from fluffy layer material in the Pomeranian Bight as characteristic ratios for sedimenting material, we find evidence for significant increases in the ratios of C to P in sediments younger than 15–25 years in cores from the Eastern Gotland basin, coincident with H2S build-up in deep waters. Paired oxygen and phosphorus concentration data from the sub-halocline water column of the Gotland Basin covering the time since 1970 suggest that the phosphate reflux is fed from two sources: At the transition from oxic to anoxic conditions, iron-bound phosphate is suddenly liberated at the sediment–water interface and results in a concentration jump of approximately 2 μmol dm−3 phosphate in deep water. During anoxic periods with H2S in bottom waters, phosphate diffuses out of the sediment and adds to the dissolved phosphate pool. Our data imply that the sediment contributed approximately 14,000 t a−1 of phosphorus to the water column of the deep Gotland Basin since the early 1970s. Compared to total P input to the Baltic Sea (1993: 39,000 t), the reflux of P from anoxic sediments in the Gotland Basin thus is a major source of P for the Baltic Sea. On time scales of years and decades, the reflux of phosphorus from the sediments may be the reason for discrepancies between the ratios of nitrogen and phosphorus in the Baltic Sea and for a lack of effects of declining phosphate discharge into this large ecosystem." @default.
• W2090317838 created "2016-06-24" @default.
• W2090317838 creator A5020494833 @default.
• W2090317838 creator A5051754193 @default.
• W2090317838 creator A5067063183 @default.
• W2090317838 creator A5076718578 @default.
• W2090317838 creator A5077106608 @default.
• W2090317838 creator A5077894990 @default.
• W2090317838 date "2000-06-01" @default.
• W2090317838 modified "2023-10-18" @default.
• W2090317838 title "Changes in the C, N, P burial rates in some Baltic Sea sediments over the last 150 years—relevance to P regeneration rates and the phosphorus cycle" @default.
• W2090317838 cites W1609313813 @default.
• W2090317838 cites W1969576448 @default.
• W2090317838 cites W1992773737 @default.
• W2090317838 cites W2013730878 @default.
• W2090317838 cites W2020900764 @default.
• W2090317838 cites W2026198658 @default.
• W2090317838 cites W2033359010 @default.
• W2090317838 cites W2034148763 @default.
• W2090317838 cites W2036832435 @default.
• W2090317838 cites W2042707470 @default.
• W2090317838 cites W2043018364 @default.
• W2090317838 cites W2076585433 @default.
• W2090317838 cites W2078586738 @default.
• W2090317838 cites W2138546463 @default.
• W2090317838 cites W2153161933 @default.
• W2090317838 cites W2170957430 @default.
• W2090317838 cites W2319348843 @default.
• W2090317838 cites W276944000 @default.
• W2090317838 cites W284352328 @default.
• W2090317838 doi "https://doi.org/10.1016/s0025-3227(00)00015-3" @default.
• W2090317838 hasPublicationYear "2000" @default.
• W2090317838 type Work @default.
• W2090317838 sameAs 2090317838 @default.
• W2090317838 citedByCount "172" @default.
• W2090317838 countsByYear W20903178382012 @default.
• W2090317838 countsByYear W20903178382013 @default.
• W2090317838 countsByYear W20903178382014 @default.
• W2090317838 countsByYear W20903178382015 @default.
• W2090317838 countsByYear W20903178382016 @default.
• W2090317838 countsByYear W20903178382017 @default.
• W2090317838 countsByYear W20903178382018 @default.
• W2090317838 countsByYear W20903178382019 @default.
• W2090317838 countsByYear W20903178382020 @default.
• W2090317838 countsByYear W20903178382021 @default.
• W2090317838 countsByYear W20903178382022 @default.
• W2090317838 countsByYear W20903178382023 @default.
• W2090317838 crossrefType "journal-article" @default.
• W2090317838 hasAuthorship W2090317838A5020494833 @default.
• W2090317838 hasAuthorship W2090317838A5051754193 @default.
• W2090317838 hasAuthorship W2090317838A5067063183 @default.
• W2090317838 hasAuthorship W2090317838A5076718578 @default.
• W2090317838 hasAuthorship W2090317838A5077106608 @default.
• W2090317838 hasAuthorship W2090317838A5077894990 @default.
• W2090317838 hasConcept C111368507 @default.
• W2090317838 hasConcept C127313418 @default.
• W2090317838 hasConcept C151730666 @default.
• W2090317838 hasConcept C171056886 @default.
• W2090317838 hasConcept C178790620 @default.
• W2090317838 hasConcept C185592680 @default.
• W2090317838 hasConcept C2816523 @default.
• W2090317838 hasConcept C2986433049 @default.
• W2090317838 hasConcept C510538283 @default.
• W2090317838 hasConcept C86803240 @default.
• W2090317838 hasConcept C95444343 @default.
• W2090317838 hasConceptScore W2090317838C111368507 @default.
• W2090317838 hasConceptScore W2090317838C127313418 @default.
• W2090317838 hasConceptScore W2090317838C151730666 @default.
• W2090317838 hasConceptScore W2090317838C171056886 @default.
• W2090317838 hasConceptScore W2090317838C178790620 @default.
• W2090317838 hasConceptScore W2090317838C185592680 @default.
• W2090317838 hasConceptScore W2090317838C2816523 @default.
• W2090317838 hasConceptScore W2090317838C2986433049 @default.
• W2090317838 hasConceptScore W2090317838C510538283 @default.
• W2090317838 hasConceptScore W2090317838C86803240 @default.
• W2090317838 hasConceptScore W2090317838C95444343 @default.
• W2090317838 hasIssue "1-2" @default.
• W2090317838 hasLocation W20903178381 @default.
• W2090317838 hasOpenAccess W2090317838 @default.
• W2090317838 hasPrimaryLocation W20903178381 @default.
• W2090317838 hasRelatedWork W1969776835 @default.
• W2090317838 hasRelatedWork W2047147828 @default.
• W2090317838 hasRelatedWork W2065269418 @default.
• W2090317838 hasRelatedWork W2080739914 @default.
• W2090317838 hasRelatedWork W2121036537 @default.
• W2090317838 hasRelatedWork W2367909481 @default.
• W2090317838 hasRelatedWork W2389981343 @default.
• W2090317838 hasRelatedWork W274727775 @default.
• W2090317838 hasRelatedWork W3131339940 @default.
• W2090317838 hasRelatedWork W4256416663 @default.
• W2090317838 hasVolume "167" @default.
• W2090317838 isParatext "false" @default.
• W2090317838 isRetracted "false" @default.
• W2090317838 magId "2090317838" @default.
• W2090317838 workType "article" @default.