B. Papp szerk.: Studia Botanica Hungarica 35. 2004 (Budapest, 2004)

Erdei, B.; Bruch, A. A.: A climate analysis of Late Oligocene (Egerian) macrofloras from Hungary

CLIMATE ANALYSIS OF LATE OLIGOCENE (EGERIAN) MACROFLORAS 7 brackish and limnic sediments of the Eger Formation overlying conformably the Kiscell Clay (Early Oligocène). According to NAGYMAROSY (pers. comm. in KVACEK and HABLY 1991) in Eger-Wind the lower part of the Egerian is exposed and the sequence covers the upper part of the NP24 zone and the Globorotalia opima opima foraminifera zone to the lower part of the NP25 zone. However, BÁLDI et al. (1999) suppose that NP24 nannozone may correlate with the Upper Kiscellian only as well as they note that the separation of the NP24 and NP25 Fig. 2. Stratigraphy of the Hungarian Oligocène (after Báldi 1998).