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The storm surge recorded in a thin section

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Limestone and sandstone beds deposited by storms are called tempestites, and exhibit much variation in thickness, grain size and internal structures, depending on the proximity and on the intensity of the storm waves. In this paper, diagnostic features of storm beds observed in thin sections, was presented. Characteristic features are investigated on the basis of detailed study in the Upper Devonian carbonates in the western part of the Holy Cross Mountains (Poland).
The paper describes a new species of blind trilobite from the lower Fammenian of Concours−le−Haut at Causses−et−Veyran, Montagne Noire (France). Trimerocephalus (Trifoliops) nigritus subgen. et sp. nov. is assigned to a new subgenus together with Tr. (Trif.) trifolius (Osmólska, 1958). This grouping is supported by the results of phylogenetic analysis of thirteen species attributed to the Fammenian genus Trimerocephalus McCoy, 1849; of 16 previously known species attributed to this genus, only 12 were represented by data of quality sufficient to be included in the analysis, using 23 morphological characters. The Frasnian phacopine Acuticryphops acuticeps (Kayser, 1889) is used as the outgroup. The three most parsimonious trees have a length of 51 steps and a consistency index of 0.82. The new subgenus Trifoliops forms a clade together with Trimerocephalus? steinachensis (Richter and Richter, 1926), supported by an exclusive synapomorphy: widening of the cephalic antero−lateral border. Tr.? steinachensis seems to be more closely related to Tr. (Trif.) trifolius (sharing two synapomorphies) and may represent a more derived taxon (possibly deserving a separate subgeneric status). The remanig Trimerocephalus species are not formally assigned to subgeneric taxa, pending further studies (their relationships are shown in cladograms). The results do not confirm the classification suggested by Chlupač (1966) for Trimerocephalus.
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A double-spired brachiopod Biernatella polonica gen. et sp.n. is described for the first time from the Upper Devonian of Southern Poland. A new family Biernatellidae has been established for it within the Dayioidea.
Organic remains of tentaculitids have been recovered during palynological research on archival samples from the Dobrzyca 2 borehole (Western Pomerania). Until now tentaculitids are widely known from their abundant mineralised shells. As organic remains, on the other hand, they have only been known since 2004. The present discovery is currently the second one of this kind found in Upper Devonian strata. The shape and morphology of some recognized tentaculitid organic remains are similar to embryonic and juvenile forms of dacryoconarids belonging to orders Nowakiida and Stylionida. Based on palynomorphs, the age of the two samples investigated has been established as Frasnian, RB and RD local miospore zones.
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