Статья

Quaternary time scales for the Pontocaspian domain: Interbasinal connectivity and faunal evolution

Wout KrijgsmanDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsА. С. ТесаковGeological Institute of the Russian Academy of Sciences, Pyzhevsky 7, Moscow 119017, RussiaТ.А. YaninaLomonosov Moscow State University, Moscow 119991, RussiaSergei LazarevDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsGuzel DanukalovaRussian Academy of Sciences, Institute of Geology of the Ufimian Scientific Centre, K. Marx St. 16/2, Ufa 450077, RussiaChristiaan van BaakJordi Agustı́ICREA. Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Universitat Rovira i Virgili, Tarragona, SpainMehmet Cihat AlçiçekDepartment of Geology, Pamukkale University, Denizli 20070, TurkeyE. AliyevaDiksha BistaBRIDGE, School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol BS8 1SS, UKAngela A BruchSenckenberg Forschungsinstitut Senckenberganlage, Frankfurt 25 60325, GermanyYeşim BüyükmeriçDepartment of Geological Engineering, Bülent Ecevit University, Incivez/Zonguldak 67100, TurkeyMaia BukhsianidzeThe National Museum of Georgia, 3 Purtseladze St., 0107, Tbilisi, GeorgiaRachel FleckerBRIDGE, School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol BS8 1SS, UKP. D. FrolovGeological Institute of the Russian Academy of Sciences, Pyzhevsky 7, Moscow 119017, RussiaThomas M. HoyleDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsElisabeth L. JorissenDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsUwe KirscherEarth Dynamics Research Group, Department of Applied Geology, WASM, Curtin University, Perth, AustraliaSifan A. KoricheDepartment of Meteorology and Centre for Past Climate Change, University of Reading, UKS.B. KroonenbergDepartment of Applied Earth Sciences, Delft University of Technology, Delft 2600, The NetherlandsDavid LordkipanidzeThe National Museum of Georgia, 3 Purtseladze St., 0107, Tbilisi, GeorgiaOriol OmsDepartment of Applied Earth Sciences, Delft University of Technology, Delft 2600, The NetherlandsLea RauschDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsJoy SingarayerDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsMarius StoicaDepartment of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The NetherlandsSabrina van de VeldeDepartment of Applied Earth Sciences, Delft University of Technology, Delft 2600, The NetherlandsВ. В. ТитовRussian Academy of Sciences, Institute of Arid Zones, Chekhova 41, Rostov-on-Don 344006, RussiaFrank P. WesselinghNaturalis Biodiversity Center, P.O. Box 9517, Leiden 2300, The Netherlands

2018en

ABI

Аннотация

The Pontocaspian (Black Sea - Caspian Sea) region has a very dynamic history of basin development and biotic evolution. The region is the remnant of a once vast Paratethys Sea. It contains some of the best Eurasian geological records of tectonic, climatic and paleoenvironmental change. The Pliocene-Quaternary co-evolution of the Black Sea-Caspian Sea is dominated by major changes in water (lake and sea) levels resulting in a pulsating system of connected and isolated basins. Understanding the history of the region, including the drivers of lake level and faunal evolution, is hampered by indistinct stratigraphic nomenclature and contradicting time constraints for regional sedimentary successions. In this paper we review and update the late Pliocene to Quaternary stratigraphic framework of the Pontocaspian domain, focusing on the Black Sea Basin, Caspian Basin, Marmara Sea and the terrestrial environments surrounding these large, mostly endorheic lake-sea systems.

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Идентификаторы

DOI: 10.1016/j.earscirev.2018.10.013

Цитирования и источники

Цитирований: 2Использованных источников: 0

Показатели — AkademScholar