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Fungal sporocarps having ostiole with setae were found in the upper Pliocene deposits from Mizerna (borehole Mizerna-Nowa), southern Poland. These remains morphologically correspond to the fossil-genus  Trichothyrites  Rosend., although the structure of the ostiolar collar with non-septate setae seems unique and is typical for sporocarps (catathecia) of some modern species of the genus  Lichenopeltella  Höhn. Other contemporary fungal genera with setose sporocarps differ considerably from  Lichenopeltella  in respect of their morphology. Taking this into consideration, a new fossil-species  Lichenopeltella mizerniana  G. Worobiec is proposed. Morphologically,  Lichenopeltella mizerniana  is similar both to some modern lichenicolous [ L. peltigericola  (D. Hawksw.) R. Sant.,  L. rangiferinae  Brackel, and  L. uncialicola  Brackel] and non-lichenicolous species [ L. ammophilae  (J.P. Ellis) P.M. Kirk &amp; Minter,  L. palustris  (J.P. Ellis) P.M. Kirk &amp; Minter] of this genus. The presence of  Lichenopeltella mizerniana  suggests that the Pliocene climate of the Mizerna locality was probably at least moderately humid.

Lichenopeltella mizerniana sp. nov. from the upper Pliocene of Mizerna (southern Poland)