FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2904216967> ?p ?o ?g. }

• W2904216967 endingPage "219" @default.
• W2904216967 startingPage "203" @default.
• W2904216967 abstract "The Pannonian Basin of Croatia is the largest back-arc extensional basin on the European continent, located between the Alps, Carpathians and Dinarides. Syn-rift subsidence started at ~18 Ma and predated the onset of the Miocene Climate Optimum (MCO; 17–14.7 Ma). In this paper, we investigate the evolution of the fluvial-lacustrine palaeoenvironment just prior to the transgression of the Central Paratethys Sea. Studies are based on a 17-m-thick section of the Požega palaeolake in the Southern Pannonian Basin using palaeobiological (mollusks, ostracods, palynomorphs, fish otoliths), mineralogical and sedimentological data. Our results reveal fluctuating freshwater and brackish conditions and a pulsating water budget, which we relate to phases in which the basin was, alternatively, hydrologically open and closed. We infer that the alternating environmental conditions can be best-explained by dry and wet periods, respectively. Droughts produced stagnant conditions, algae overproduction and increased salinity levels, supporting the survival of sporadically invading brackish water species. The wet periods, on the other hand, led to lake highstand episodes, expansion of lake area, and to the widespread development of profundal facies. The lake basin eventually became overfilled and connected through outflowing rivers with the Central Paratethys sea. However, the absence of brackish-marine assemblages in the Požega palaeolake nevertheless indicates that there was no marine water inflow from the Central Paratethys at that time." @default.
• W2904216967 created "2018-12-22" @default.
• W2904216967 creator A5010567966 @default.
• W2904216967 creator A5026871427 @default.
• W2904216967 creator A5032273992 @default.
• W2904216967 creator A5038621324 @default.
• W2904216967 creator A5047673176 @default.
• W2904216967 creator A5090315181 @default.
• W2904216967 date "2019-02-01" @default.
• W2904216967 modified "2023-10-18" @default.
• W2904216967 title "Multiproxy reconstruction of the middle Miocene Požega palaeolake in the Southern Pannonian Basin (NE Croatia) prior to the Badenian transgression of the Central Paratethys Sea" @default.
• W2904216967 cites W1777507756 @default.
• W2904216967 cites W1789491862 @default.
• W2904216967 cites W1966440077 @default.
• W2904216967 cites W1969020655 @default.
• W2904216967 cites W1970576134 @default.
• W2904216967 cites W1975936840 @default.
• W2904216967 cites W1992316800 @default.
• W2904216967 cites W2014856287 @default.
• W2904216967 cites W2022616238 @default.
• W2904216967 cites W2035198811 @default.
• W2904216967 cites W2035397340 @default.
• W2904216967 cites W2039019170 @default.
• W2904216967 cites W2053852225 @default.
• W2904216967 cites W2061001640 @default.
• W2904216967 cites W2072986148 @default.
• W2904216967 cites W2077147039 @default.
• W2904216967 cites W2082485247 @default.
• W2904216967 cites W2087047379 @default.
• W2904216967 cites W2091048790 @default.
• W2904216967 cites W2098607383 @default.
• W2904216967 cites W2104541252 @default.
• W2904216967 cites W2108187370 @default.
• W2904216967 cites W2111926569 @default.
• W2904216967 cites W2113790692 @default.
• W2904216967 cites W2115575384 @default.
• W2904216967 cites W2118210343 @default.
• W2904216967 cites W2122579123 @default.
• W2904216967 cites W2122709257 @default.
• W2904216967 cites W2127845629 @default.
• W2904216967 cites W2140477756 @default.
• W2904216967 cites W2148038246 @default.
• W2904216967 cites W2151683625 @default.
• W2904216967 cites W2151914223 @default.
• W2904216967 cites W2166330017 @default.
• W2904216967 cites W2177714650 @default.
• W2904216967 cites W2201911031 @default.
• W2904216967 cites W2266966050 @default.
• W2904216967 cites W2319996752 @default.
• W2904216967 cites W2333205088 @default.
• W2904216967 cites W2339834576 @default.
• W2904216967 cites W2522181992 @default.
• W2904216967 cites W2568893007 @default.
• W2904216967 cites W2569183133 @default.
• W2904216967 cites W2590379789 @default.
• W2904216967 cites W2593482517 @default.
• W2904216967 cites W2618498834 @default.
• W2904216967 cites W2788200810 @default.
• W2904216967 cites W2792974011 @default.
• W2904216967 cites W2800300550 @default.
• W2904216967 cites W2898368518 @default.
• W2904216967 cites W4306293736 @default.
• W2904216967 doi "https://doi.org/10.1016/j.palaeo.2018.12.003" @default.
• W2904216967 hasPublicationYear "2019" @default.
• W2904216967 type Work @default.
• W2904216967 sameAs 2904216967 @default.
• W2904216967 citedByCount "14" @default.
• W2904216967 countsByYear W29042169672019 @default.
• W2904216967 countsByYear W29042169672020 @default.
• W2904216967 countsByYear W29042169672021 @default.
• W2904216967 countsByYear W29042169672022 @default.
• W2904216967 countsByYear W29042169672023 @default.
• W2904216967 crossrefType "journal-article" @default.
• W2904216967 hasAuthorship W2904216967A5010567966 @default.
• W2904216967 hasAuthorship W2904216967A5026871427 @default.
• W2904216967 hasAuthorship W2904216967A5032273992 @default.
• W2904216967 hasAuthorship W2904216967A5038621324 @default.
• W2904216967 hasAuthorship W2904216967A5047673176 @default.
• W2904216967 hasAuthorship W2904216967A5090315181 @default.
• W2904216967 hasConcept C109007969 @default.
• W2904216967 hasConcept C111368507 @default.
• W2904216967 hasConcept C112959462 @default.
• W2904216967 hasConcept C118178180 @default.
• W2904216967 hasConcept C127313418 @default.
• W2904216967 hasConcept C129513315 @default.
• W2904216967 hasConcept C146588470 @default.
• W2904216967 hasConcept C151730666 @default.
• W2904216967 hasConcept C2779421809 @default.
• W2904216967 hasConcept C77271252 @default.
• W2904216967 hasConceptScore W2904216967C109007969 @default.
• W2904216967 hasConceptScore W2904216967C111368507 @default.
• W2904216967 hasConceptScore W2904216967C112959462 @default.
• W2904216967 hasConceptScore W2904216967C118178180 @default.
• W2904216967 hasConceptScore W2904216967C127313418 @default.
• W2904216967 hasConceptScore W2904216967C129513315 @default.
• W2904216967 hasConceptScore W2904216967C146588470 @default.
• W2904216967 hasConceptScore W2904216967C151730666 @default.
• W2904216967 hasConceptScore W2904216967C2779421809 @default.

• next