2012
DOI: 10.1007/s10347-012-0300-x
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Environmental changes close to the Lower–Middle Devonian boundary; the Basal Choteč Event in the Prague Basin (Czech Republic)

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Cited by 32 publications
(27 citation statements)
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“…In addition, the known ontogenetic data indicate that length proportions of most plates were constrained in different growth stages despite of allometry in other directions (e.g. Werdelin & Long 1986, Cloutier 2010. The length of the skull roof of A. rufus specimen Lc 125 based only on the size of the fragment of the C plate is at least 45 cm.…”
Section: Antineosteus Rufus Sp Nov Figures 3-6mentioning
confidence: 99%
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“…In addition, the known ontogenetic data indicate that length proportions of most plates were constrained in different growth stages despite of allometry in other directions (e.g. Werdelin & Long 1986, Cloutier 2010. The length of the skull roof of A. rufus specimen Lc 125 based only on the size of the fragment of the C plate is at least 45 cm.…”
Section: Antineosteus Rufus Sp Nov Figures 3-6mentioning
confidence: 99%
“…It comprises reddish and grey bioclastic (mainly crinoidal) and micritic, mostly well-bedded limestones with common stromatactis structures (e.g. Havlíček & Kukal 1990; for microfacies and some other characteristics see Dieken 1996, Koptíková 2011and Vodrážková et al 2013; the stromatactis structures were studied in detail by Kukal 1972, recently by Dieken 1996, Hladil 2005and Hladil et al 2006, its thickness is 20-30 m. Coarser detritus dominates both the lowest and uppermost parts of the sequence (Chlupáč et al 1979, Chlupáč 1998, Koptíková 2011. The sediments were deposited on the weathered and corroded surface of the Koněprusy Reef, represented by the Koně-prusy Limestone (e.g.…”
Section: Geological and Palaeontological Settingsmentioning
confidence: 99%
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“…The BCE represents a deepening episode with distinctive facies and faunal changes, which is placed in the time interval corresponding to the Polygnathus partitus and Polygnathus costatus biozones (Vodrážková et al, 2013). At the BCE turn- Keller, 2006).…”
Section: Basal Choteč Eventmentioning
confidence: 99%
“…Volcanic activity within this member is documented in the vicinity of Chýnice and Choteč (Fiala 1946, Svoboda & Prantl 1948. Further detailed information on their geology and faunas can be found in Svoboda & Prantl (1947-1951, Chlupáč (1959Chlupáč ( , 1998, Chlupáč et al (1998), andVodrážková et al (2012). The "Nad tratí" quarry section at Praha-Hlubočepy was selected as the lectostratotype of this lithostratigraphic unit (Chlupáč 1959(Chlupáč , 1981.…”
Section: Tøebotov Limestonementioning
confidence: 99%