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Aragonian stratigraphy reconsidered, and a re-evaluation of the middle Miocene mammal biochronology in Europe

机译:重新考虑了阿拉贡地层,并对欧洲中新世中期哺乳动物的生物年代学进行了重新评估

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The recently collected fauna of Armantes 1A in Chron C5Br of the Armantes section necessitates reinterpretation of the previous bio- and magnetostratigraphical correlations between the Armantes and Vargas sections (Calatayud-Daroca Basin, Central Spain) [W. Krijgsman, M. Garces, C.G. Langereis, R. Daams, J. van Dam, A.J. van der Meulen, J. Agusti, L. Cabrera, A new chronology for the Middle to Late Miocene continental record in Spain, Earth Planet. Sci. Lett. 142 (1996) 367-380]. The long reversal in the Vargas section is now correlated to C5Br, instead of to C5Cr, on the basis of the biostratigraphical correlation of Armantes 1A to the faunas of Fuente Sierra 2 and 3 (in the Vargas section), which are situated in the basal part of the Middle Aragonian (MN5). This leads to the revised age of 16.0 Ma for the Early-Middle Aragonian (MN 4/5) boundary. Our age estimate of the MN5/6 boundary is maintained at ca. 13.75 Ma. The Vargas section is now considered to start in Chron C5Cn.2r and to end in C5Bn.1n. As a result of the revised correlation the duration of the time gap between the fossiliferous parts of Vargas and the younger Aragon section, previously estimated as ca. 1.5 Myr, is now reduced to less than 200,000 years. The tie points of the European mammal units (MN4-MN6) to the geomagnetic polarity time scale [F.F. Steininger, W.A. Berggren, D.V. Kent, R.L. Bernor, S. Sen, J. Agusti, Circum-Mediterranean Neogene (Miocene and Pliocene) marine-continental chronologic correlations of European mammal units, in: R.L Bernor, V. Fahlbusch, H.-W. Mittmann (Eds.), The Evolution of Western Eurasian Neogene Mammal Faunas, Columbia Univ. Press, New York, 1996. pp. 7-46] are evaluated. Our age estimates of the MN4/5 and MN5/6 boundaries are compatible with the new magnetostratigraphic calibration of middle Miocene mammal zones in the Swiss Molasse basin [O. Kempf, T. Bolliger, D. Kalin, B. Engesser, A. Matter, New magnetostratigraphic calibration of Early to Middle Miocene mammal biozones of the North Alpine foreland basin, in: J.-P. Aguilar, S. Legendre, J. Michaux (Eds.), Actes du Congres BiochroM'97, Mem. Trav. E.P.H.E. 21 (1997) 547-562].
机译:最近在阿曼特斯区Ch5 C5Br的阿曼特斯1A动物区系需要重新解释阿曼特斯和巴尔加斯地区(西班牙中部卡拉泰德-达罗卡盆地)之间以前的生物和地层学相关性。 Krijgsman,M.Garces,C.G. Langereis,R.Daams,J.van Dam,A.J。 van der Meulen,J。Agusti,L。Cabrera,西班牙中新世至中新世大陆记录的新年表,地球行星。科学来吧142(1996)367-380]。根据Armantes 1A与位于基底的Fuente Sierra 2和3的动物区系的生物地层相关性,现在Vargas区域中的长反转与C5Br相关,而不与C5Cr相关。中阿拉贡(MN5)的一部分。这导致阿拉贡早期至中部(MN 4/5)边界的修订年龄为16.0 Ma。我们对MN5 / 6边界的年龄估计保持在大约。 13.75毫安。现在认为Vargas部分从Chron C5Cn.2r开始,并以C5Bn.1n结尾。由于修正的相关性,瓦尔加斯的化石部分与较年轻的阿拉贡断层之间的时间间隔持续时间以前估计为。 1.5 Myr,现在减少到不到20万年。欧洲哺乳动物单位(MN4-MN6)与地磁极性时标的联系点[F.F. Steininger,W.A. Berggren,D.V. Kent,R.L. Bernor,S.Sen,J.Agusti,Circum-Mediterranean Neogene(中新世和上新世)欧洲哺乳动物单元的海陆年代学相关性,在:R.L Bernor,V.Fahlbusch,H.-W.米特曼(编辑),《西方欧亚新近纪哺乳动物动植物的进化》,哥伦比亚大学。出版社,纽约,1996年。第7-46页]。我们对MN4 / 5和MN5 / 6边界的年龄估算与瑞士Molasse盆地中中新世哺乳动物带的新地层学标定兼容[O. Kempf,T. Bolliger,D. Kalin,B.Engesser,A.Matter,北高山前陆盆地中新世早期至中新世哺乳动物生物带的新地层学标定,J.-P. Aguilar,S.Legendre,J.Michaux(编),Actes du Congres BiochroM'97,内存。出差E.P.H.E. 21(1997)547-562]。

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