2009
Bio-events in Early Badenian sedimentary sequence from Kralice nad Oslavou (Carpathian Foredeep, Czech Republic)
ZÁGORŠEK, Kamil; Katarina HOLCOVÁ; Slavomír NEHYBA; Šárka HLADILOVÁ; Andreas KROH et al.Základní údaje
Originální název
Bio-events in Early Badenian sedimentary sequence from Kralice nad Oslavou (Carpathian Foredeep, Czech Republic)
Autoři
Vydání
Acta Naturalia de „L Ateneo Parmense, Parma, 2009, 0004-654X
Další údaje
Jazyk
angličtina
Typ výsledku
Článek v odborném periodiku
Obor
10500 1.5. Earth and related environmental sciences
Stát vydavatele
Itálie
Utajení
není předmětem státního či obchodního tajemství
Označené pro přenos do RIV
Ano
Kód RIV
RIV/00216224:14310/09:00029977
Organizační jednotka
Přírodovědecká fakulta
Klíčová slova anglicky
Bryozoa; Foraminifera; Echinodermata; Mollusca; Middle Miocene; Carpathian Foredeep
Příznaky
Mezinárodní význam
Změněno: 6. 11. 2012 10:45, doc. RNDr. Nela Doláková, CSc.
V originále
Based on an analysis of the faunal composition, the palaeoenvironmental evolution of the section has been investigated. The sediments at the base of the section originate from a deeper marine basin and well oxygenated bottom waters. A first bryozoan event can be recorded in this interval. Above, foraminiferal evidence points to increased depth and decreased oxygen levels, coinciding with an abundance peak of molluscs and asteroids, but disappearance of bryozoans. In the upper half of the section, conditions changed considerably. Echinoderms and bryozoans exhibit high diversities in this interval. These drastic changes are related here to changes in basin geometry.
Česky
Based on an analysis of the faunal composition, the palaeoenvironmental evolution of the section has been investigated. The sediments at the base of the section originate from a deeper marine basin and well oxygenated bottom waters. A first bryozoan event can be recorded in this interval. Above, foraminiferal evidence points to increased depth and decreased oxygen levels, coinciding with an abundance peak of molluscs and asteroids, but disappearance of bryozoans. In the upper half of the section, conditions changed considerably. Echinoderms and bryozoans exhibit high diversities in this interval. These drastic changes are related here to changes in basin geometry.
Návaznosti
| GA205/09/0103, projekt VaV |
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