Dzik, J. 2006. The Famennian „Golden Age” of conodonts and ammonoids in the Polish part of the Variscan sea. Palaeontologia Polonica 63, 1-359.

Abstract. The stratigraphically complete and extremely fossiliferous geological sections in the Holy Cross Mountains and Sudetes, Poland, cover the whole history of the Famennian tropical high-diversity pelagic ecosystem. Apparatus reconstruction of 142 conodont species allowed paleobiological interpretation of the faunal succession. Three families, nine genera and 39 species are newly proposed. 76 species of goniatites, with one genus and five species new, and 70 species of clymenias were also identified. Like in all other equatorial localities, a significant (but not catastrophic) decline of diversity marks the beginning of the Famennian. The local pelagic fauna developed mostly as a result of successive reappearances of lineages earlier occurring in the area but temporally removed from it by environmental factors. During the whole Famennian, 101 immigrations of conodont lineages are documented. In 31 of the lineages persisting in the area a more or less complete record of their phyletic evolution is represented; they cover about half (46%) of the summarized ranges of all the lineages. About half of them are suitable for stratophenetic studies. The fossil record of the ammonoids is much more punctuated, but it is estimated that 110 lineages was represented there, only 14 of them possibly evolving phyletically in the area (single case was stratophenetically proven). At the transition between goniatites and clymenias, a succession within the plexus of closely related sympatric species is observed, but the exact phyletic change is not recorded and probably all the first clymenias are immigrants from the east. At least two profound rebuildings of the fauna within the Famennian are observed, but only the terminal Devonian Hangenberg event was of truly dramatic nature. The newly acquired evidence supports the earlier notion thate it is more difficult to trace evolution stratophenetically in the equatorial regions than in high latitudes.