FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2916133074> ?p ?o ?g. }

• W2916133074 endingPage "12" @default.
• W2916133074 startingPage "1" @default.
• W2916133074 abstract "Understanding the long-term environmental forcings driving Caspian Sea (CS) water levels is of utmost importance, not only owing to its large size, or to the surrounding developing economies but also to improve global climate models and forecasts. However, Late Quaternary CS level changes and their amplitude are mostly documented from incomplete coastal sediment records. Because of the CS idiosyncrasies, that behaves neither as a sea nor as a lake, the methods used to reconstruct water levels in the global ocean or in freshwater lakes do not always apply. Here, we propose a first step toward the use of dinoflagellate cysts records to reconstruct qualitative changes in water mass, focusing on new and published deep-water sedimentary sequences from the south and middle CS basins. Trends in water level changes are reconstructed on the relative proportions of dinocyst assemblages with different levels of brackishness. A higher highstand than previously seen is reconstructed post-Mangyshlak lowstand. A reverse water flow gradient from S to N, not previously detected, is identified at 8.5–8 to 4 cal ka BP. A major turnover in dinocyst assemblage is found at 4 cal ka BP. While the Volga River is the main source of water nowadays, we propose that the source of water to maintain the 8.5–8 to 4 cal ka BP highstand is the now-disconnected drainage basin of the Amu-Darya. The CS was at that time most likely strongly influenced by low latitude climates, with more precipitation over the Karakum and, perhaps, even indirect monsoonal influence." @default.
• W2916133074 created "2019-03-02" @default.
• W2916133074 creator A5047190823 @default.
• W2916133074 creator A5072537778 @default.
• W2916133074 creator A5089729582 @default.
• W2916133074 date "2019-04-01" @default.
• W2916133074 modified "2023-10-18" @default.
• W2916133074 title "Dinocyst records from deep cores reveal a reversed salinity gradient in the Caspian Sea at 8.5–4.0 cal ka BP" @default.
• W2916133074 cites W1676573182 @default.
• W2916133074 cites W1973895405 @default.
• W2916133074 cites W1979117038 @default.
• W2916133074 cites W1981724328 @default.
• W2916133074 cites W1989022780 @default.
• W2916133074 cites W1999888263 @default.
• W2916133074 cites W2001095317 @default.
• W2916133074 cites W2006037150 @default.
• W2916133074 cites W2014411114 @default.
• W2916133074 cites W2024133647 @default.
• W2916133074 cites W2024608698 @default.
• W2916133074 cites W2026290077 @default.
• W2916133074 cites W2027350044 @default.
• W2916133074 cites W2028207512 @default.
• W2916133074 cites W2030324173 @default.
• W2916133074 cites W2031333660 @default.
• W2916133074 cites W2031764603 @default.
• W2916133074 cites W2033242016 @default.
• W2916133074 cites W2034238372 @default.
• W2916133074 cites W2039003315 @default.
• W2916133074 cites W2044261516 @default.
• W2916133074 cites W2044636155 @default.
• W2916133074 cites W2045848830 @default.
• W2916133074 cites W2046387909 @default.
• W2916133074 cites W2046808001 @default.
• W2916133074 cites W2050818497 @default.
• W2916133074 cites W2053124740 @default.
• W2916133074 cites W2061624406 @default.
• W2916133074 cites W2061672521 @default.
• W2916133074 cites W2066133680 @default.
• W2916133074 cites W2075036169 @default.
• W2916133074 cites W2087590096 @default.
• W2916133074 cites W2088231369 @default.
• W2916133074 cites W2088633565 @default.
• W2916133074 cites W2091350276 @default.
• W2916133074 cites W2091876533 @default.
• W2916133074 cites W2095361963 @default.
• W2916133074 cites W2101522077 @default.
• W2916133074 cites W2108295243 @default.
• W2916133074 cites W2119239298 @default.
• W2916133074 cites W2121712014 @default.
• W2916133074 cites W2122188420 @default.
• W2916133074 cites W2124647012 @default.
• W2916133074 cites W2126612937 @default.
• W2916133074 cites W2136246993 @default.
• W2916133074 cites W2137022741 @default.
• W2916133074 cites W2141831833 @default.
• W2916133074 cites W2147984849 @default.
• W2916133074 cites W2162741979 @default.
• W2916133074 cites W2167425355 @default.
• W2916133074 cites W2273973443 @default.
• W2916133074 cites W2322962237 @default.
• W2916133074 cites W2463507092 @default.
• W2916133074 cites W2573000315 @default.
• W2916133074 cites W2573799245 @default.
• W2916133074 cites W2605479247 @default.
• W2916133074 cites W2624548826 @default.
• W2916133074 cites W275611125 @default.
• W2916133074 cites W2776900114 @default.
• W2916133074 cites W2803825341 @default.
• W2916133074 cites W2884062598 @default.
• W2916133074 cites W2900493612 @default.
• W2916133074 cites W2905571073 @default.
• W2916133074 cites W59526064 @default.
• W2916133074 doi "https://doi.org/10.1016/j.quascirev.2019.02.011" @default.
• W2916133074 hasPublicationYear "2019" @default.
• W2916133074 type Work @default.
• W2916133074 sameAs 2916133074 @default.
• W2916133074 citedByCount "9" @default.
• W2916133074 countsByYear W29161330742019 @default.
• W2916133074 countsByYear W29161330742020 @default.
• W2916133074 countsByYear W29161330742021 @default.
• W2916133074 countsByYear W29161330742022 @default.
• W2916133074 countsByYear W29161330742023 @default.
• W2916133074 crossrefType "journal-article" @default.
• W2916133074 hasAuthorship W2916133074A5047190823 @default.
• W2916133074 hasAuthorship W2916133074A5072537778 @default.
• W2916133074 hasAuthorship W2916133074A5089729582 @default.
• W2916133074 hasBestOaLocation W29161330741 @default.
• W2916133074 hasConcept C107054158 @default.
• W2916133074 hasConcept C109007969 @default.
• W2916133074 hasConcept C111368507 @default.
• W2916133074 hasConcept C127313418 @default.
• W2916133074 hasConcept C1284942 @default.
• W2916133074 hasConcept C129513315 @default.
• W2916133074 hasConcept C136996986 @default.
• W2916133074 hasConcept C140302290 @default.
• W2916133074 hasConcept C140345934 @default.
• W2916133074 hasConcept C151730666 @default.
• W2916133074 hasConcept C153294291 @default.

• next