FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2955908880> ?p ?o ?g. }

• W2955908880 endingPage "109226" @default.
• W2955908880 startingPage "109226" @default.
• W2955908880 abstract "Lake Van, the largest soda lake in the world, is a key area where climatic changes are recorded by well-preserved sedimentary successions. In spite of the existence of such sequences, the ancient lake levels are still under debate. Here, we present U/Th ages of tufa layers exposed along the northern margin of the lake near the town of Adilcevaz. Tufa are interpreted to form during humid and temperate climate conditions in the contact zone between the highly alkaline lake water – rich in bicarbonate and carbonate ions – and calcium-rich groundwater. These contact zones most likely appear near shore. Thus, U/Th ages and altitude of the tufa present minimum ancient lakestands. The tufas obtained in our study are dated between 112.7 and 19.3 ka. They are interpreted to record two transgressional intervals, the first starting at 1701 meters above sea level (masl) altitude at 112.7 ka reaching 1706 masl at 72.5 ka (based on three U/Th ages). The second transgression starts at the present Lake Van level of 1646 masl at 30.1 ka, reaching 1725 masl at 19.3 ka (based on 15 U/Th ages). Comparison with climate proxies reveals that the first transgression was caused by intensified precipitation accompanied by warming, while the second transgression was triggered mainly by warming that initiated melting of glaciers. The lake-level fluctuations described here are almost in line with the ones gathered from dated lake terraces but contradict lake-level reconstruction based on pore water salinity." @default.
• W2955908880 created "2019-07-12" @default.
• W2955908880 creator A5029414958 @default.
• W2955908880 creator A5058163430 @default.
• W2955908880 creator A5065791255 @default.
• W2955908880 creator A5074719835 @default.
• W2955908880 date "2019-11-01" @default.
• W2955908880 modified "2023-10-17" @default.
• W2955908880 title "Giant tufas of Lake Van record lake-level fluctuations and climatic changes in eastern Anatolia,Turkey" @default.
• W2955908880 cites W179100328 @default.
• W2955908880 cites W1959306637 @default.
• W2955908880 cites W1966146362 @default.
• W2955908880 cites W1979990331 @default.
• W2955908880 cites W1988791083 @default.
• W2955908880 cites W1991129415 @default.
• W2955908880 cites W1993033806 @default.
• W2955908880 cites W1993214984 @default.
• W2955908880 cites W1993887876 @default.
• W2955908880 cites W1995126499 @default.
• W2955908880 cites W2006849549 @default.
• W2955908880 cites W2015271100 @default.
• W2955908880 cites W2016670503 @default.
• W2955908880 cites W2016849684 @default.
• W2955908880 cites W2018135129 @default.
• W2955908880 cites W2022823282 @default.
• W2955908880 cites W2025736403 @default.
• W2955908880 cites W2026976482 @default.
• W2955908880 cites W2038947148 @default.
• W2955908880 cites W2047954492 @default.
• W2955908880 cites W2054365407 @default.
• W2955908880 cites W2055668923 @default.
• W2955908880 cites W2059474755 @default.
• W2955908880 cites W2065707934 @default.
• W2955908880 cites W2070519521 @default.
• W2955908880 cites W2071728384 @default.
• W2955908880 cites W2076525298 @default.
• W2955908880 cites W2078916267 @default.
• W2955908880 cites W2088834878 @default.
• W2955908880 cites W2095211591 @default.
• W2955908880 cites W2098518349 @default.
• W2955908880 cites W2136649657 @default.
• W2955908880 cites W2149562748 @default.
• W2955908880 cites W2150037729 @default.
• W2955908880 cites W2156703776 @default.
• W2955908880 cites W2166580640 @default.
• W2955908880 cites W2288854701 @default.
• W2955908880 cites W38519004 @default.
• W2955908880 cites W626177037 @default.
• W2955908880 doi "https://doi.org/10.1016/j.palaeo.2019.05.048" @default.
• W2955908880 hasPublicationYear "2019" @default.
• W2955908880 type Work @default.
• W2955908880 sameAs 2955908880 @default.
• W2955908880 citedByCount "4" @default.
• W2955908880 countsByYear W29559088802021 @default.
• W2955908880 countsByYear W29559088802022 @default.
• W2955908880 crossrefType "journal-article" @default.
• W2955908880 hasAuthorship W2955908880A5029414958 @default.
• W2955908880 hasAuthorship W2955908880A5058163430 @default.
• W2955908880 hasAuthorship W2955908880A5065791255 @default.
• W2955908880 hasAuthorship W2955908880A5074719835 @default.
• W2955908880 hasConcept C100970517 @default.
• W2955908880 hasConcept C109007969 @default.
• W2955908880 hasConcept C111368507 @default.
• W2955908880 hasConcept C127313418 @default.
• W2955908880 hasConcept C1284942 @default.
• W2955908880 hasConcept C146596784 @default.
• W2955908880 hasConcept C151730666 @default.
• W2955908880 hasConcept C152382732 @default.
• W2955908880 hasConcept C187320778 @default.
• W2955908880 hasConcept C191897082 @default.
• W2955908880 hasConcept C192562407 @default.
• W2955908880 hasConcept C205649164 @default.
• W2955908880 hasConcept C2524010 @default.
• W2955908880 hasConcept C2780659211 @default.
• W2955908880 hasConcept C33923547 @default.
• W2955908880 hasConcept C58640448 @default.
• W2955908880 hasConcept C6350597 @default.
• W2955908880 hasConcept C74501621 @default.
• W2955908880 hasConcept C76886044 @default.
• W2955908880 hasConcept C77271252 @default.
• W2955908880 hasConceptScore W2955908880C100970517 @default.
• W2955908880 hasConceptScore W2955908880C109007969 @default.
• W2955908880 hasConceptScore W2955908880C111368507 @default.
• W2955908880 hasConceptScore W2955908880C127313418 @default.
• W2955908880 hasConceptScore W2955908880C1284942 @default.
• W2955908880 hasConceptScore W2955908880C146596784 @default.
• W2955908880 hasConceptScore W2955908880C151730666 @default.
• W2955908880 hasConceptScore W2955908880C152382732 @default.
• W2955908880 hasConceptScore W2955908880C187320778 @default.
• W2955908880 hasConceptScore W2955908880C191897082 @default.
• W2955908880 hasConceptScore W2955908880C192562407 @default.
• W2955908880 hasConceptScore W2955908880C205649164 @default.
• W2955908880 hasConceptScore W2955908880C2524010 @default.
• W2955908880 hasConceptScore W2955908880C2780659211 @default.
• W2955908880 hasConceptScore W2955908880C33923547 @default.
• W2955908880 hasConceptScore W2955908880C58640448 @default.
• W2955908880 hasConceptScore W2955908880C6350597 @default.
• W2955908880 hasConceptScore W2955908880C74501621 @default.

• next