The trace fossil chondrites in uppermost Jurassic-lower cretaceous deep cavity fills from the Western Carpathians (Czech Republic)

2003
journal article
article
dc.abstract.enThe 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 Berriasian. In more bioturbated laminae ?Palaeophycus also occurs. The occurrence of Chondrites in fillings of deep cavities represents new evidence for adaptation of its trace maker to stressful environments.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.contributor.authorUchman, Alfred - 132472 pl
dc.contributor.authorMikuláš, Radekpl
dc.contributor.authorHouša, Václavpl
dc.date.accession2018-10-22pl
dc.date.accessioned2018-10-25T13:26:19Z
dc.date.available2018-10-25T13:26:19Z
dc.date.issued2003pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 186-187pl
dc.description.number3pl
dc.description.physical181-187pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume54pl
dc.identifier.eissn1336-8052pl
dc.identifier.issn1335-0552pl
dc.identifier.projectROD UJ / OPpl
dc.identifier.urihttps://ruj.uj.edu.pl/xmlui/handle/item/58715
dc.identifier.weblinkhttp://www.geologicacarpathica.com/browse-journal/volumes/54-3/article-156/pl
dc.languageengpl
dc.language.containerengpl
dc.rightsUznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 4.0 Międzynarodowa*
dc.rights.licenceCC-BY-NC-ND
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/legalcode*
dc.share.typeotwarte czasopismo
dc.subject.enJurassicpl
dc.subject.enCretaceouspl
dc.subject.enWestern Carpathianspl
dc.subject.enCzech Republicpl
dc.subject.enperi-reefal cavitiespl
dc.subject.encryptobiontspl
dc.subject.entrace fossilspl
dc.subject.enChondritespl
dc.subject.enPalaeophycuspl
dc.subtypeArticlepl
dc.titleThe trace fossil chondrites in uppermost Jurassic-lower cretaceous deep cavity fills from the Western Carpathians (Czech Republic)pl
dc.title.journalGeologica Carpathicapl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
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 Berriasian. In more bioturbated laminae ?Palaeophycus also occurs. The occurrence of Chondrites in fillings of deep cavities represents new evidence for adaptation of its trace maker to stressful environments.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.contributor.authorpl
Uchman, Alfred - 132472
dc.contributor.authorpl
Mikuláš, Radek
dc.contributor.authorpl
Houša, Václav
dc.date.accessionpl
2018-10-22
dc.date.accessioned
2018-10-25T13:26:19Z
dc.date.available
2018-10-25T13:26:19Z
dc.date.issuedpl
2003
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 186-187
dc.description.numberpl
3
dc.description.physicalpl
181-187
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
54
dc.identifier.eissnpl
1336-8052
dc.identifier.issnpl
1335-0552
dc.identifier.projectpl
ROD UJ / OP
dc.identifier.uri
https://ruj.uj.edu.pl/xmlui/handle/item/58715
dc.identifier.weblinkpl
http://www.geologicacarpathica.com/browse-journal/volumes/54-3/article-156/
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Uznanie autorstwa - Użycie niekomercyjne - Bez utworów zależnych 4.0 Międzynarodowa
dc.rights.licence
CC-BY-NC-ND
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-nd/4.0/legalcode
dc.share.type
otwarte czasopismo
dc.subject.enpl
Jurassic
dc.subject.enpl
Cretaceous
dc.subject.enpl
Western Carpathians
dc.subject.enpl
Czech Republic
dc.subject.enpl
peri-reefal cavities
dc.subject.enpl
cryptobionts
dc.subject.enpl
trace fossils
dc.subject.enpl
Chondrites
dc.subject.enpl
Palaeophycus
dc.subtypepl
Article
dc.titlepl
The trace fossil chondrites in uppermost Jurassic-lower cretaceous deep cavity fills from the Western Carpathians (Czech Republic)
dc.title.journalpl
Geologica Carpathica
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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