{"refrec":{"BRefID":342291,"RR":"<b>Vasiliev, I.; Stoica, M.; Grothe, A.; Lazarev, S.; Palcu, D.V.; Van Baak, C.G.C.; Leeuw, A.; Sangiorgi, F.; Reichart, G.-J.; Davies, G.R.; Krijgsman, W.</b> (2021). Hydrological changes in restricted basins: Insights from strontium isotopes on late Miocene‐Pliocene connectivity of the Eastern Paratethys (Dacian Basin, Romania). <i>Geochem. Geophys. Geosyst. 22(7)</i>. <a href=\"https://dx.doi.org/10.1029/2020gc009369\" target=\"_blank\">https://dx.doi.org/10.1029/2020gc009369</a>","BEntID":338926,"PublicFlag":1,"CheckedFlag":0,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Geochem. Geophys. Geosyst. 22(7)</i>. <a href=\"https://dx.doi.org/10.1029/2020gc009369\" target=\"_blank\">https://dx.doi.org/10.1029/2020gc009369</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":0,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Vasiliev, I.; Stoica, M.; Grothe, A.; Lazarev, S.; Palcu, D.V.; Van Baak, C.G.C.; Leeuw, A.; Sangiorgi, F.; Reichart, G.-J.; Davies, G.R.; Krijgsman, W.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Vasiliev, I. <i>et al.</i>","Englishabstract":"The Dacian Basin was uniquely situated to record late Miocene hydrological    changes that influenced depositional environments and faunal dispersal    patterns in Central Eurasia's mega-lake Paratethys. Differences between the    high strontium isotope ratio (<sup>87</sup>Sr/<sup>86</sup>Sr) of the    waters from Lake Pannon and local Carpathian rivers and low <sup>87</sup>    Sr/<sup>86</sup>Sr of the Eastern Paratethys (Black Sea ‒ Caspian Sea)    allow a thorough investigation of connectivity and water fluxes in the    transient Dacian Basin. We present a detailed <sup>87</sup>Sr/<sup>86</sup>    Sr record for the Dacian Basin, which provides an exceptional record of    basin connectivity from the latest Tortonian (ca. 7.7 Ma) until the early    Pleistocene (ca. 1.8 Ma). Data show that a late Tortonian transgression    (7.6–7.4 Ma) started with an incursion of Eastern Paratethys waters into    the Dacian Basin, after which local rivers became the dominant source for    the mostly freshwater environments of the early Messinian. The regional    Maeotian-Pontian transitional interval (6.3–5.9 Ma) records a second    incursion of Eastern Paratethys waters, but this time with an additional    marine (Mediterranean) influx coinciding with a short-lived salinity    incursion. During the Messinian Salinity Crisis of the Mediterranean, the    Dacian Basin progressively connected with the Eastern Paratethys (5.9–5.5    Ma), after which it became restricted during the peak Mediterranean    lowstand (5.5 Ma) and filled with Lake Pannon and local river water    (5.5–5.3 Ma). During the Plio-Pleistocene, the Dacian Basin reconnectedwith the, at that time isolated, Black Sea, which shows similar    <sup>87</sup>Sr/<sup>86</sup>Sr as in the Last Glacial Maximum.","AbstractOtherLang":null,"BibLvlCode":"AS","StandardTitle":"Hydrological changes in restricted basins: Insights from strontium isotopes on late Miocene‐Pliocene connectivity of the Eastern Paratethys (Dacian Basin, Romania)","OrigTitleLangCode":"en","OrigTitleLangCodeExtended":"eng","OrigTitleLangID":15,"DateLastModified":{"date":"2026-05-28 01:31:38.128893","timezone_type":1,"timezone":"+02:00"},"UserAccessRight":null,"UserAccID":null,"AuthorKeywords":"strontium isotopes; marine influx; connectivity; transgression; Dacian Basin; ostracods","OtherDescriptors":null,"Notes":null,"AnaPub":2021,"MonPub":null,"DateUpdate":"2021-08-12","DateCreate":"2021-08-12","SecASFANote":null,"ConfID":null,"PeerRev":1,"VlizCoreFlag":1,"WoScode":"WOS:000678953500022","VABBcode":null,"OpenAcc":1,"DOI":"10.1029/2020gc009369"},"refs":null,"anarec":{"AnaID":342291,"PubliDate":2021,"Pagination":null,"XtraPublOfAnaID":null,"ISBN":null,"Volume":"22","Issue":"7","BRefMon":null,"BRefMonRR":null,"BRefXtra":null,"BRefXtraRR":null,"SerBRefID":100768,"SerRR":"Geochemistry, Geophysics, Geosystems. 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