The Early Carboniferous biogeotraphic position of the Balkan Penninsula

首次对巴尔干半岛的半岛的晚维森期和Serpukhovian期（早石炭世晚期）菊石组合进行定量分析，最好的代表是塞尔维亚Druzetic-Milivojevici的动物群。它将被测试，如果这些组合属于北华力西或南华力西-北冈瓦纳领域，或者如果他们是无关紧要的。对菊石动物群的重新调查和分析，与牙形石和其他微体化石的研究平行，将为华力西褶皱带的重建和造山带的时间确定提供重要数据。

For the first time, a quantitative analysis of the Late Viséan and Serpukhovian (late Early Carboniferous) ammonoid assemblages of the Balkan Peninsula, best represented by the faunas from Druzetic-Milivojevici in Serbia, will be achieved. It will be tested if these assemblages belong to the North Variscan or South Variscan-North Gondwanan Realm, or if they are indifferent. Re-investigation and analyses of the ammonoid faunas, parallel to studies of conodonts and other microfossils, will reveal important data for the reconstruction of the Variscan Fold Belt and timing of the orogeny.