DOI: 10.1016/j.gloplacha.2015.12.013
论文题名: Application of the authigenic 10Be/9Be dating method to Late Miocene-Pliocene sequences in the northern Danube Basin (Pannonian Basin System): Confirmation of heterochronous evolution of sedimentary environments
作者: Šujan M. ; Braucher R. ; Kováč M. ; Bourlès D.L. ; Rybár S. ; Guillou V. ; Hudáčková N.
刊名: Global and Planetary Change
ISSN: 0921-8181
出版年: 2016
卷: 137 起始页码: 35
结束页码: 53
语种: 英语
英文关键词: Atmospheric beryllium-10
; Cosmogenic nuclide
; Lake Pannon
; Late Miocene
; Paleoenvironments
; Pliocene
Scopus关键词: Banks (bodies of water)
; Beryllium
; Deposition
; Floods
; Geochronology
; Lakes
; Sedimentology
; Structural geology
; Cosmogenic nuclides
; Deltaic sedimentation
; Depositional system
; Late Miocene
; Paleoenvironments
; Pleistocene sediments
; Pliocene
; Sedimentary environment
; Rivers
; beryllium isotope
; cosmogenic radionuclide
; dating method
; deltaic sedimentation
; depositional environment
; floodplain
; geochronology
; lacustrine deposit
; Miocene
; paleoenvironment
; Pliocene
; sedimentary basin
; sequence stratigraphy
; Alps
; Carpathians
; Danube Basin
; Eastern Alps
; Pannonian Basin
; Vienna Basin
; Western Carpathians
; Mammalia
英文摘要: Authigenic 10Be/9Be dating method was applied to lacustrine, deltaic and alluvial sequences of the northern Danube Basin (Pannonian Basin System), to bridge the insufficiency of geochronological data for the Late Miocene to Pliocene period. The measurements of 51 samples (both lacustrine and floodplain), ranging from 11.6 to 0.95Ma are consistent with the existing magnetostratigraphic and biostratigraphic data standing mainly on the evolution degree of endemic mollusk fauna, mammals and dinocysts. This agreement confirms our assumption that the incoming beryllium fluxes remained constant over the studied time period and thus that the two initial 10Be/9Be ratios determined in actual Holocene/Late Pleistocene sediments (lacustrine and floodplain) are valid for these environments. The obtained ages indicate gradual progradation of the deltaic depositional systems across the Danube Basin with a clear time-transgressional character, replacing basin floor and shelfal environments. Deltaic sedimentation occurred firstly in the north at foothills of the Western Carpathians from 11.0. Ma, and changed to the alluvial environment after 10.5 Ma. At the same time (~ 10.5 Ma), the paleo-Danube deltaic system draining the Eastern Alps entered the study area from the Vienna Basin situated on the West. Later, the deltaic systems were merged in the central part of the basin and reached its southeastern margin at ~ 9.4 Ma. Regression of the Lake Pannon from the southernmost part of the study area is evidenced after 8.7 Ma. Alluvial deposition of meandering rivers lasting until 6.0-5.0 Ma followed and was interrupted by the early Pliocene basin inversion. Sedimentation of braided streams took place during the late Pliocene and Pleistocene, reflecting uplift of mountains surrounding the basin margins. This study documents the powerful potential of the authigenic 10Be/9Be dating method and its reliability in a basin with complicated tectonic and sedimentary history. It demonstrates that this method can effectively be applied to lacustrine and floodplain deposits and to samples from outcrops as well as boreholes. © 2015 Elsevier B.V. URL: https://www.scopus.com/inward/record.uri?eid=2-s2.0-84951972194&doi=10.1016%2fj.gloplacha.2015.12.013&partnerID=40&md5=566c6ab3ee9abb0ac427232cc5d3993f
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/11720
Appears in Collections: 全球变化的国际研究计划 气候变化与战略
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作者单位: Department of Geology and Paleontology, Faculty of Natural Sciences, Comenius University in Bratislava, Slovakia
Recommended Citation:
Šujan M.,Braucher R.,Kováč M.,et al. Application of the authigenic 10Be/9Be dating method to Late Miocene-Pliocene sequences in the northern Danube Basin (Pannonian Basin System): Confirmation of heterochronous evolution of sedimentary environments[J]. Global and Planetary Change,2016-01-01,137.