About: The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic.

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About: The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic. Goto Sponge NotDistinct Permalink

An Entity of Type : http://linked.opendata.cz/ontology/domain/vavai/Vysledek, within Data Space : linked.opendata.cz associated with source document(s)

Attributes	Values
rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	The common marine trace fossil Chondrites occurs in thin layers in laminated micrites which fill deep submarine cavities in peri-reefal biocalcarenites and calcirudites of the Tithonian-Berriasian Stramberg limestone. The cavity fills display several generations which originated during long periods of time. Periodic colonization of this very stressful environment by the Chondrites trace maker was possible probably owing to episodic deposition of more oxygenated and more nutritious sediment at a certain stage of development of the cavities related to increased tectonic activity during the Berrisian. In more bioturbated laminate ?palaeophycus also occurs. The occurence of Chondrites in fillings of deep cavities represents new evidence for adaptation of its trace maker to stressful environments. The common marine trace fossil Chondrites occurs in thin layers in laminated micrites which fill deep submarine cavities in peri-reefal biocalcarenites and calcirudites of the Tithonian-Berriasian Stramberg limestone. The cavity fills display several generations which originated during long periods of time. Periodic colonization of this very stressful environment by the Chondrites trace maker was possible probably owing to episodic deposition of more oxygenated and more nutritious sediment at a certain stage of development of the cavities related to increased tectonic activity during the Berrisian. In more bioturbated laminate ?palaeophycus also occurs. The occurence of Chondrites in fillings of deep cavities represents new evidence for adaptation of its trace maker to stressful environments. (en)
Title	The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic. The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic. (en)
skos:prefLabel	The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic. The Trace Fossil Chondrites in Uppermost Jurasic-Lower Cretaceous Deep Cavity Fills from the Western Carpathians, Czech Republic. (en)
skos:notation	RIV/67985831:_____/03:09033078!RIV/2004/AV0/A09004/N
http://linked.open.../vavai/riv/strany	1;7
http://linked.open...avai/riv/aktivita	P Z
http://linked.open...avai/riv/aktivity	P(GA205/00/0118), Z(AV0Z3013912)
http://linked.open...iv/cisloPeriodika	3
http://linked.open...vai/riv/dodaniDat	2004
http://linked.open...aciTvurceVysledku	Houša, Václav Mikuláš, Radek
http://linked.open.../riv/druhVysledku	J - Článek v odborném periodiku
http://linked.open...iv/duvernostUdaju	S - Úplné a pravdivé údaje nepodléhající ochraně podle zvláštních právních předpisů
http://linked.open...titaPredkladatele	Geologický ústav AV ČR, v. v. i.
http://linked.open...dnocenehoVysledku	631234
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/03:09033078
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	jurassic; Cretaceous; trace fossils (en)
http://linked.open.../riv/klicoveSlovo	Cretaceous jurassic trace fossils
http://linked.open...odStatuVydavatele	SK - Slovenská republika
http://linked.open...ontrolniKodProRIV	[857FA8077737]
http://linked.open...i/riv/nazevZdroje	Geologica Carpathica
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	2 (xsd:int)
http://linked.open...cetTvurcuVysledku	3 (xsd:int)
http://linked.open...ocetUcastnikuAkce	0 (xsd:int)
http://linked.open...nichUcastnikuAkce	0 (xsd:int)
http://linked.open...vavai/riv/projekt	Facies architecture of the turbidite system of Moravice formation, Nízký Jeseník culm basin, based on sedimentology and ichnofacies analysis
http://linked.open...UplatneniVysledku	2003
http://linked.open...v/svazekPeriodika	54
http://linked.open...iv/tvurceVysledku	Mikuláš, Radek Uchman, A. Houša, Václav
http://linked.open...n/vavai/riv/zamer	Vývoj litosféry a přírodního prostředí od nejstarší geologické minulosti do současnosti
issn	1335-0552
number of pages	7 (xsd:int)

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