DOI: 10.1016/j.gloplacha.2012.10.001
论文题名: The isolation of the Pannonian basin (Central Paratethys): New constraints from magnetostratigraphy and biostratigraphy
作者: ter Borgh M. ; Vasiliev I. ; Stoica M. ; Knežević S. ; Matenco L. ; Krijgsman W. ; Rundić L. ; Cloetingh S.
刊名: Global and Planetary Change
ISSN: 0921-8350
出版年: 2013
卷: 103, 期: 1 起始页码: 99
结束页码: 118
语种: 英语
英文关键词: Back-arc basins
; Basin connectivity
; Central paratethys
; Pannonian basin
; Transylvanian basin
; Vienna basin
Scopus关键词: Back-arc basin
; Basin connectivity
; Central Paratethys
; Pannonian basin
; Transylvanian basin
; Vienna Basin
; Sea level
; Biostratigraphy
; backarc basin
; basin evolution
; basin fill
; biostratigraphy
; eustacy
; inland sea
; inselberg
; magnetostratigraphy
; mollusc
; ostracod
; paleoenvironment
; paleogeography
; Paratethys
; sediment transport
; tectonic evolution
; uplift
; sea level
; Carpathians
; Fruska Gora
; Pannonian Basin
; Romania
; Serbia
; Transylvanian Basin
; Vienna Basin
; Mollusca
; Ostracoda
; Paratethys
英文摘要: In this paper we establish when and how the Pannonian basin and associated Central Paratethys basins were isolated from the remainder of the Paratethys, a system of back-arc basins and inland seas that once extended over a large part of Europe. The isolation, which occurred at the beginning of the Late Miocene, is marked by a paleoenvironmental change from marine to fresh water conditions that caused the regional Sarmatian- Pannonian Extinction Event. It also had significant paleogeographical implications for the basin fill and for sedimentary transport across the Carpathian Mountains. The exact age of and cause for the isolation are still subject to debate. Here, we use magnetostratigraphic dating coupled to ostracod and mollusc biostratigraphy to establish the isolation age of the Pannonian basin. We dated the isolation of the Pannonian basin at 11.63±0.04 Ma in a section on the northern flank of the Fruška Gora inselberg (northern Serbia). This age is in line with recent results from the Vienna basin but predates the isolation of the Transylvanian by 0.33 Myr, suggesting that isolation took place in two steps. We conclude that the uplift of the Carpathian Mountains caused the isolation but that eustatic sea level fluctuations may have had a minor influence as well. © 2012 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84878217469&doi=10.1016%2fj.gloplacha.2012.10.001&partnerID=40&md5=1f87c4f8eb00cac6bc432455a3c44e56
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11256
Appears in Collections: 全球变化的国际研究计划
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作者单位: Netherlands Research Centre for Integrated Solid Earth Science (ISES), Utrecht University, Faculty of Geosciences, Budapestlaan 4, 3584CD, Utrecht, Netherlands
Recommended Citation:
ter Borgh M.,Vasiliev I.,Stoica M.,et al. The isolation of the Pannonian basin (Central Paratethys): New constraints from magnetostratigraphy and biostratigraphy[J]. Global and Planetary Change,2013-01-01,103(1).