|
|
SCF in Lower Palaeozoic sediments of the Barrandian area
Kovář, Vojtěch ; Fatka, Oldřich (advisor) ; Brocke, Rainer (referee)
1 Abstract In recent years, the term small carbonaceous fossils (SCFs) has been established to accomodate fragile organic-walled fossils of micro- to mesoscopic size that are usually extracted by means of the 'low-manipulation HF extraction' method. This method has so far only been utilized by several authors and no reports have been published on the usage of the method on samples from the Barrandian area. To test the applicability of the method, samples from the Barrandian area were processed. The samples came from eleven localities representing six stratigraphic units (Paseky Shale, Jince Formation, Letná Formation, Kosov Formation, Daleje Shale and Roblín Member). All the units have been studied before by 'standard' methods of palynological processing. Various previously unreported fossils are described, including wiwaxiid sclerites, putative chaetognath remains and acritarch clusters. Furthermore, it is discovered, that the 'low-manipulation HF extraction' can also be used for extraction of originally calcareous fossils. The pilot study provides a further proof that the 'low-manipulation HF extraction' is a useful tool with the potential to significantly expand our knowledge of fossil assemblages. Key words: Small carbonaceous fossils, Cambrian, Ordovician, Devonian, Barrandian area
|
|
| |
|
|
Review of phyllocarid crustacenas of the Barrandian area
Šilinger, Matěj ; Fatka, Oldřich (advisor) ; Budil, Petr (referee)
The thesis summarizes the actual knowledge about classification and stratigraphic distribution of phyllocarid crustaceans in Ordovician to Devonian sediments of the Barrandian area. The thesis includes revision of systematic position and classification of individual taxa, mainly on the basis of data and observations published outside of the Czech Republic. The photographic documentation of selected specimens housed in institutional collections is newly provided.
|
|
|
SCF in Lower Palaeozoic sediments of the Barrandian area
Kovář, Vojtěch ; Fatka, Oldřich (advisor) ; Brocke, Rainer (referee)
1 Abstract In recent years, the term small carbonaceous fossils (SCFs) has been established to accomodate fragile organic-walled fossils of micro- to mesoscopic size that are usually extracted by means of the 'low-manipulation HF extraction' method. This method has so far only been utilized by several authors and no reports have been published on the usage of the method on samples from the Barrandian area. To test the applicability of the method, samples from the Barrandian area were processed. The samples came from eleven localities representing six stratigraphic units (Paseky Shale, Jince Formation, Letná Formation, Kosov Formation, Daleje Shale and Roblín Member). All the units have been studied before by 'standard' methods of palynological processing. Various previously unreported fossils are described, including wiwaxiid sclerites, putative chaetognath remains and acritarch clusters. Furthermore, it is discovered, that the 'low-manipulation HF extraction' can also be used for extraction of originally calcareous fossils. The pilot study provides a further proof that the 'low-manipulation HF extraction' is a useful tool with the potential to significantly expand our knowledge of fossil assemblages. Key words: Small carbonaceous fossils, Cambrian, Ordovician, Devonian, Barrandian area
|
|
|
Vertebrates of the Lower Palaeozoic from the Barrandian area (Bohemian Massif) and their comparison with faunas of adjacent areas
Vaškaninová, Valéria ; Kraft, Petr (advisor) ; Přikryl, Tomáš (referee) ; Trinajstic, Kate (referee)
This thesis deals with early vertebrate fossil remains from the Lower Palaeozoic strata of the Barrandian area (Bohemian Massif). It is presented as a compilation of four papers that were published or submitted in scientific peer-reviewed journals with impact factor. All included papers are focused on the most abundant and diverse vertebrate fauna from the Barrandian area - the placoderms. Placodermi are early vertebrates characterized by articulated head and trunk shields composed of dermal bony plates. In the Barrandian area, they occur exclusively in the Devonian of the Prague Basin. The main objectives of the thesis are modern taxonomic revisions of the placoderm taxa from the Prague Basin as well as discussions about trends in their abundance, diversity, and distribution in space and time, taphonomy, and the evolutionary and phylogenetic implications of their morphology. Two characteristic placoderm associations were distinguished. In the Lochkovian and Pragian, members of the group Acanthothoraci dominate the placoderm record. Acanthothoracid placoderms are among the most basal jawed vertebrates and thus a detailed study of their morphology has a great potential to illuminate the relationships and evolutionary patterns among the stem jawed vertebrates. They are most abundant in the...
|
|
| |
|
|
Placodermi of the Prague Basin (Lower Palaeozoic of the Barrandian area)
Kašpar Vaškaninová, Valéria ; Kraft, Petr (advisor) ; Zajíc, Jaroslav (referee)
Placoderms are restricted to the Devonian in the Prague Basin, occuring on localities dated from the Lochkovian to the Givetian. Černá rokle near Kosoř with the Radotin Limestone is the richest placoderm bearing locality. A revision of specimens from collections of the National Museum in Pra- gue confirms occurences of three species of two genera belonging to the pla- coderm order Acanthothoraci: Radotina kosorensis Gross, 1950; Radotina tesselata Gross, 1958 and Kosoraspis peckai Gross, 1959. Genus Holopeta- lichthys was accepted as valid and a diagnosis of H. primus (Barrande, 1872) was amended. Its assignment to higher taxonomic units remains uncertain. Four morphological types of undeterminable specimens classified in the order Arthrodira are defined. Some previously unpublished morphological structures are figured and described: the median dorsal plate of the thoracic armour of R. kosorensis and its relation to the head shield, the cranial cavities and trunk shield plates of R. tesselata, a well preserved neurocranium and scales of K. peckai, the trunk shield and vertebral column of H. primus and large dermal plates of each Arthrodiran morphotype. The placoderm diversity in the Prague Basin was lower compared to ne- ighbouring areas at the beginning of the Devonian (Lochkovian and Pra- gian). Only...
|
|
| |
|
| |
guest ::
