The age of the Sarmatian–Pannonian transition in the Transylvanian Basin (Central Paratethys)

Vasiliev, Iuliana; Leeuw, Arjan de; Filipescu, Sorin; Krijgsman, Wout; Kuiper, Klaudia F.; Stoica, Marius; Briceag, Andrei

doi:10.1016/j.palaeo.2010.07.015

Cited by 54 publications

(40 citation statements)

References 41 publications

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“…8), at about 2.3 m from the top of Section A (sample M10, Fig. 4), just below the ash layers of the Bazna Tuff (Vancea 1960; not "Oarba Tuff" as considered by Vasiliev et al 2010). Our boundary can be very clearly traced between the boundaries of Vancea (1960) and Sütő & Szegő (2008).…”

Section: -Glomospira Charoidesmentioning

confidence: 72%

“…Among the ostracods, Loxoconcha Considering the radio-isotopic age of the ash layer from the lower part of Section A (11.62 Ma) and the magnetostratigraphic calibration of the top of the section (Vasiliev et al 2010), we have a good age approximation for the Sarmatian-Pannonian biostratigraphic boundary, that is close to 11.3 Ma. This is approximately 300 kyr younger than the age of the Sarmatian-Pannonian boundary traced by Piller et al (2007) and about 100 kyr younger than the boundary traced by Lirer et al (2009).…”

Section: -Glomospira Charoidesmentioning

confidence: 86%

“…The newly established restrictive conditions produced very distinctive changes of biota (e.g. marine foraminifera replaced by brackish ostracods) about 11.3 Myr ago (Vasiliev et al 2010). This biotic boundary seems to be younger compared to other Central Paratethyan basins (e.g.…”

Section: Discussionmentioning

confidence: 99%

“…Preliminary results on magnetostratigraphy, radiometric dating, and biostratigraphy were presented by Vasiliev et al (2006), Filipescu et al (2009), and De . An integrated study was published by Vasiliev et al (2010). Our purpose is to present in detail the micropaleontological record for …”

Section: Introductionmentioning

confidence: 99%

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Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania)

Filipescu¹,

Wanek²,

Miclea³

et al. 2011

Geologica Carpathica

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Abstract:The Sarmatian-Pannonian transition has been investigated in Section A of Oarba de Mure in the central Transylvanian Basin. Micropaleontological assemblages are diagnostic for different environmental settings and demonstrate a clear zonation, which was used to reconstruct the genetic units. Five stratigraphic sequences were described and subdivided based on the microfossil assemblages. Transgressive intervals were documented by five-chambered and biserial planktonic foraminifera, normal regressions by assemblages with abundant mysid, dasyclads, diatoms, and benthic rotaliid foraminifera, while the forced regressions are characterized by reworking. The Sarmatian-Pannonian boundary (11.3 Ma) is clearly documented by microfossils and is calibrated with radiometric and magnetostratigraphic data. A new interpretation for the interbasinal correlation is proposed by synchronizing the top of the Central Paratethyan Sarmatian with the top of the Eastern Paratethyan Bessarabian.

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Section: -Glomospira Charoidesmentioning

confidence: 72%

Section: -Glomospira Charoidesmentioning

confidence: 86%

Section: Discussionmentioning

confidence: 99%

Section: Introductionmentioning

confidence: 99%

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Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania)

Filipescu¹,

Wanek²,

Miclea³

et al. 2011

Geologica Carpathica

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“…The Transylvanian Ba sin, one of the ma jor bas ins of the Cen tral Paratethys, pre serves char ac ter is tic strati graphic features but faces the same bio-and chronostratigraphic dif fi culties in cor re la tion with the stan dard zones and stages. Re cent at tempts to im prove the cor re la tion cri te ria for the Mio cene of the Transylvanian Ba sin, with im pli ca tions for the Paratethyan stra tig ra phy, were car ried out by Krézsek and Filipescu (2005), Filipescu and Silye (2008), Beldean et al (2010), Krézsek et al (2010), Vasiliev et al (2010), Filipescu et al (2011), and de Leeuw et al (2013).…”

Section: Introductionmentioning

confidence: 99%

Palaeoenvironmental changes in the Transylvanian Basin during the Early Miocene revealed by the foraminifera assemblages

Székely

Beldean

Bindiu

et al. 2015

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. Palaeoenvironmental changes in the Transylvanian Ba sin dur ing the Early Mio cene re vealed by the foraminifera as sem blages. Geo log i cal Quar terly, 60 (1): 167-180, doi: 10.7306/gq.1245The evo lu tion of the Transylvanian Ba sin dur ing the Early Mio cene has been re con structed from the suc ces sion of palaeoenvironments in ferred from sedimentological trends and the suc ces sion of spe cific foraminiferal as sem blages from Lower Mio cene Tihãu sec tion in the north west ern Transylvanian Ba sin. Plank tonic foraminifera sug gest a Burdigalian age and re cord sea level changes, cli ma tic and pro duc tiv ity events. Ben thic foraminifera of fer data on the palaeoenvironmental evo lu tion, with a large-scale progradational (coars en ing up) sed i men tary suc ces sion in flu enced by re gional tec ton ics. The suc ces sion of depositional events in cludes: (1) transgressive coarse grained de pos its with typ i cal Med i ter ra nean as semblages of bi valves in beach en vi ron ments; (2) a glauconitic fa cies which can be as so ci ated with the max i mum flood ing surface of the trans gres sion; (3) sed i men ta tion con tin ued on a nar row shelf in flu enced by del tas dur ing the highstand; (4) the in flu ence of re gional tec ton ics and sub se quent fill ing with turbidites as so ci ated with fan del tas.

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Latest Pannonian and Quaternary evolution at the transition between Eastern Alps and Pannonian Basin: new insights from geophysical, sedimentological and geochronological data

Zámolyi¹,

Salcher

Draganits

et al. 2016

Int J Earth Sci (Geol Rundsch)

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The age of the Sarmatian–Pannonian transition in the Transylvanian Basin (Central Paratethys)

Cited by 54 publications

References 41 publications

Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania)

Micropaleontological response to the changing paleoenvironment across the Sarmatian-Pannonian boundary in the Transylvanian Basin (Miocene, Oarba de Mureş section, Romania)

Palaeoenvironmental changes in the Transylvanian Basin during the Early Miocene revealed by the foraminifera assemblages

Latest Pannonian and Quaternary evolution at the transition between Eastern Alps and Pannonian Basin: new insights from geophysical, sedimentological and geochronological data

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