New developments in the Upper Pliocene-Pleistocene stratigraphic units of the Dacian Basin (Eastern Paratethys), Romania

被引:29
|
作者
Andreescu, Ion
Codrea, Vlad [1 ]
Lubenescu, Victoria
Munteanu, Tudor [2 ]
Petculescu, Alexandru [3 ]
Stiuca, Emil [3 ]
Terzea, Elena
机构
[1] Univ Babes Bolyai, Fac Biol & Geol, Cluj Napoca 400084, Romania
[2] Natl Inst Hydrol & Water Management, Bucharest 013686, Romania
[3] Inst Speol E Racovitza, Bucharest, Romania
关键词
D O I
10.1016/j.quaint.2012.02.009
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
As a result of multidisciplinary investigations carried out, in the last two decades, the knowledge of the Pliocene and Quaternary stratigraphy from Dacian Basin has increased considerably. New lithostratigraphic units were revealed, for example: Trajkovo Fm (Romanian), Vladeni Fm, Vanatori Fm (Pleistocene), and other units have been reassessed: Izvoarele Fm, Tulucesti Fm (Romanian). A new biozonation based on molluscan fauna from the Late Pliocene (NSM11, NSM12) and Pleistocene (QM1-QM9) deposits made possible a more accurate subdivision and cronostratigraphical assignments and correlations. Many localities with Romanian mammal associations (Lupoaia, Dranic, Podari, Tetoiu, Leu etc.) were reviewed, adding new taxa in the faunal list, with implications for accurately establishing host deposit ages. These studies, together with bio-magnetostratigraphic investigations led to revision of the Romanian Stage boundaries and subdivisions (Pelendavian, Valahian) and to outline several new Pleistocene chronostratigraphic units: the Argedavian, Dinogetian, Ilfovian stages and Milcovian, Uzunian, Netindavian, Musaisian substages. Finally, one major achievement consisted in the Pliocene/Pleistocene boundary relocation in the Dacian Basin, in agreement with its new position at similar to 2.6 Ma in the Mediterranean realm. (c) 2012 Elsevier Ltd and INQUA. All rights reserved.
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页码:15 / 29
页数:15
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