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首页> 外文期刊>Geodiversitas >A systematic study of the middle-late Miocene rodents and lagomorphs (Mammalia) of Fels??t??rk??ny 3/8 and 3/10 (Northern Hungary) with stratigraphical relations
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A systematic study of the middle-late Miocene rodents and lagomorphs (Mammalia) of Fels??t??rk??ny 3/8 and 3/10 (Northern Hungary) with stratigraphical relations

机译:具有地层关系的Fels ?? t ?? rk ?? ny 3/8和3/10(匈牙利北部)中新世中期啮齿类动物和哺乳动物形态(哺乳动物)的系统研究

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The present paper gives a systematic study of rodent and lagomorph remains together with the list of terrestrial molluscs recovered in the localities FT 3/8 and FT 3/10. Miocene nonmarine deposits and fossils had been known from the beginning of the 20th century in the surroundings of the village Fels??t??rk??ny, close to the town of Eger. An intensive sampling campaign was initiated by the first author in 2000. The collection was taken by screen-washing. Up to the present seven localities were studied. Among them, Fels??t??rk??ny 3/8 and 3/10 occur in the highest lithostratigraphic position. The faunas of FT 3/8 and 3/10 are unusual due to the association of Vallesian rodents (e.g., Myoxus vallesiensis, Microtocricetus molassicus, Megacricetodon minutus) and Sarmatian molluscs (e.g., Perforatella punctigera, Pirenella picta nympha). The coexistence of Collimys and Microtocricetus is rare among the European Early Vallesian faunas. Another special character of the fauna FT 3/10 is the high frequency (53%) of Collimys. The biostratigraphic comparisons suggest that the age of the studied faunas cannot be younger than the A-B mollusc zones of the Vienna Basin (Fig. 11; Papp 1951) and fits with the lower part of MN 9 or perhaps the uppermost MN 7/8. This late Sarmatian-Early Pannonian period is imperfectly documented in the Central European Neogene.
机译:本文提供了对啮齿动物和泻湖类动物遗骸的系统研究,以及在FT 3/8和FT 3/10地区回收的陆生软体动物清单。从20世纪初开始就在靠近埃格尔(Eger)镇的Fels ?? t ?? rk ?? ny村庄周围发现了中新世的非海洋沉积物和化石。第一作者于2000年发起了一次密集的采样运动。该采集是通过屏幕清洗进行的。到目前为止,已经研究了七个地区。其中,Fels ?? t ?? rk ?? ny 3/8和3/10出现在最高的岩石地层位置。 FT 3/8和3/10的动物区系很不常见,这是由于它们与瓦利兹啮齿动物有关(例如, Myoxus vallesiensis Microtocricetus molassicus Megacricetodon minutus )和Sarmatian软体动物(例如,小孔穿孔菌 Pirenella picta nympha )。 Collimys Microtocricetus 的共存在欧洲早期的瓦利西亚动物群中很少见。 FT 3/10动物区系的另一个特色是 Collimys 的高频率(53%)。生物地层学比较表明,研究动物区系的年龄不能比维也纳盆地的A-B软体动物区年轻(图11; Papp 1951),并且适合MN 9的下部或最高MN 7/8。在中欧新近纪中,这一晚期的萨尔玛蒂安-潘诺尼早期记录不完整。

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