About: Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin)

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About: Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) Goto Sponge NotDistinct Permalink

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rdf:type	skos:Concept http://linked.opendata.cz/ontology/domain/vavai/Vysledek
Description	The first attempt to reconstruct the sedimentary environments on a small Late Cretaceous (Upper Cenomanian - Lower Turonian) rocky island (Plaňany, Bohemian Cretaceous Basin) is presented. The shallow-water, highly variable coarse clastic to sandstone and limestone sedimentation prevailed in the Upper Cenomanian. An erosion event and following condensation interval with mineralization (glauconitization, phosphatization), deposition of the dark grey, Corg. enriched, and later the greenish glauconitic sediments were remarkable during the basal Lower Turonian (Whiteinella archaeocretacea Biozone). All the Lower Turonian strata are relatively fine-grained (claystones, siltstones, marlstones) and evidence the rapid deepening of the sea. During the Helvetoglobotruncana helvetica Biozone, the Plaňany island was deeply submerged and covered by light siltstones. The Early Turonian sea-level rise is well documented by changing microfaunal and macrofaunal (mainly sponge) populations. The first attempt to reconstruct the sedimentary environments on a small Late Cretaceous (Upper Cenomanian - Lower Turonian) rocky island (Plaňany, Bohemian Cretaceous Basin) is presented. The shallow-water, highly variable coarse clastic to sandstone and limestone sedimentation prevailed in the Upper Cenomanian. An erosion event and following condensation interval with mineralization (glauconitization, phosphatization), deposition of the dark grey, Corg. enriched, and later the greenish glauconitic sediments were remarkable during the basal Lower Turonian (Whiteinella archaeocretacea Biozone). All the Lower Turonian strata are relatively fine-grained (claystones, siltstones, marlstones) and evidence the rapid deepening of the sea. During the Helvetoglobotruncana helvetica Biozone, the Plaňany island was deeply submerged and covered by light siltstones. The Early Turonian sea-level rise is well documented by changing microfaunal and macrofaunal (mainly sponge) populations. (en)
Title	Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) (en)
skos:prefLabel	Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) (en)
skos:notation	RIV/67985831:_____/10:00348551!RIV11-AV0-67985831
http://linked.open...avai/riv/aktivita	I Z
http://linked.open...avai/riv/aktivity	I, Z(AV0Z30130516), Z(MZP0002579801)
http://linked.open...iv/cisloPeriodika	-
http://linked.open...vai/riv/dodaniDat	2011
http://linked.open...aciTvurceVysledku	Žítt, Jiří Svobodová, Marcela
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	277933
http://linked.open...ai/riv/idVysledku	RIV/67985831:_____/10:00348551
http://linked.open...riv/jazykVysledku	eng - angličtina
http://linked.open.../riv/klicovaSlova	Cretaceous island; weathering; geomorphology; sedimentary environments; biostratigraphy; Upper Cenomanian-Lower Turonian; Bohemian Cretaceous Basin (en)
http://linked.open.../riv/klicoveSlovo	geomorphology Bohemian Cretaceous Basin biostratigraphy weathering Cretaceous island Upper Cenomanian-Lower Turonian sedimentary environments
http://linked.open...odStatuVydavatele	CZ - Česká republika
http://linked.open...ontrolniKodProRIV	[2C42E90DF04A]
http://linked.open...i/riv/nazevZdroje	Journal of the National Museum
http://linked.open...in/vavai/riv/obor	DB
http://linked.open...ichTvurcuVysledku	2 (xsd:int)
http://linked.open...cetTvurcuVysledku	4 (xsd:int)
http://linked.open...UplatneniVysledku	2010
http://linked.open...v/svazekPeriodika	179
http://linked.open...iv/tvurceVysledku	Hradecká, L. Svobodová, Marcela Vodrážka, R. Žítt, Jiří
http://linked.open...n/vavai/riv/zamer	Zemský systém v průsečíku geologických procesů, vývoje života, klimatických a antropogenních vlivů Geosciences for the Society of the 21st Century: from regional research to geological hazards and global changes.
issn	1802-6842
number of pages	12 (xsd:int)
is http://linked.open...avai/riv/vysledek of	Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin) Palaeoenvironments and facies on a progressively flooded rocky island (Upper Cenomanian – Lower Turonian, Bohemian Cretaceous Basin)

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