Ichnology of the Cambrian Ociesęki Sandstone Formation (Holy Cross Mountains, Poland)

2016
journal article
article
25
dc.abstract.enQuartz arenites and wackes with intercalations of silty shales of the Ociesęki Formation were analysed in small outcrops and one core. The succession contains about forty-three ichnogenera and seventy-four ichnospe- cies, among which thirty-three ichnogenera and fifty-three ichnospecies are described by present author. The formation belongs to the Schmidtiellus-Holmia Superzone and to the Protolenus-Issafeniella Zone. Most strata are totally bioturbated. The diverse and numerous trace fossils represent the Cruziana ichnofacies in the lower part of the formation and the Skolithos ichnofacies in the upper part. A few possibly new ichnospecies of different ichnogenera have been described in open nomenclature. Sedimentary structures and trace fossil assemblages indicate that the older part of this formation was deposited on the upper offshore to lower shoreface, while its younger part was deposited on the lower to middle shoreface, where storm episodes were the main factor controlling sedimentation and the activity of benthos. The trace fossil associations studied are similar to those from the lower Cambrian in many places around the world. The ichnoassociations from the Polish part of the East European Platform and from Sweden, which represent the Baltica palaeocontinent, display the closest similarity.pl
dc.affiliationWydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznychpl
dc.contributor.authorStachacz, Michał - 142881 pl
dc.date.accessioned2016-12-20T10:33:03Z
dc.date.available2016-12-20T10:33:03Z
dc.date.issued2016pl
dc.date.openaccess0
dc.description.accesstimew momencie opublikowania
dc.description.additionalBibliogr. s. 320-326pl
dc.description.number3pl
dc.description.physical291-328pl
dc.description.versionostateczna wersja wydawcy
dc.description.volume86pl
dc.identifier.doi10.14241/asgp.2016.007pl
dc.identifier.eissn2300-8512pl
dc.identifier.issn0208-9068pl
dc.identifier.projectROD UJ / Ppl
dc.identifier.urihttp://ruj.uj.edu.pl/xmlui/handle/item/34234
dc.languageengpl
dc.language.containerengpl
dc.rightsUdzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa*
dc.rights.licenceInna otwarta licencja
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl*
dc.share.typeotwarte czasopismo
dc.subject.enCambrianpl
dc.subject.entrace fossilspl
dc.subject.enshallow-water marine depositionpl
dc.subject.enHoly Cross Mountainspl
dc.subtypeArticlepl
dc.titleIchnology of the Cambrian Ociesęki Sandstone Formation (Holy Cross Mountains, Poland)pl
dc.title.journalAnnales Societatis Geologorum Poloniaepl
dc.typeJournalArticlepl
dspace.entity.typePublication
dc.abstract.enpl
Quartz arenites and wackes with intercalations of silty shales of the Ociesęki Formation were analysed in small outcrops and one core. The succession contains about forty-three ichnogenera and seventy-four ichnospe- cies, among which thirty-three ichnogenera and fifty-three ichnospecies are described by present author. The formation belongs to the Schmidtiellus-Holmia Superzone and to the Protolenus-Issafeniella Zone. Most strata are totally bioturbated. The diverse and numerous trace fossils represent the Cruziana ichnofacies in the lower part of the formation and the Skolithos ichnofacies in the upper part. A few possibly new ichnospecies of different ichnogenera have been described in open nomenclature. Sedimentary structures and trace fossil assemblages indicate that the older part of this formation was deposited on the upper offshore to lower shoreface, while its younger part was deposited on the lower to middle shoreface, where storm episodes were the main factor controlling sedimentation and the activity of benthos. The trace fossil associations studied are similar to those from the lower Cambrian in many places around the world. The ichnoassociations from the Polish part of the East European Platform and from Sweden, which represent the Baltica palaeocontinent, display the closest similarity.
dc.affiliationpl
Wydział Biologii i Nauk o Ziemi : Instytut Nauk Geologicznych
dc.contributor.authorpl
Stachacz, Michał - 142881
dc.date.accessioned
2016-12-20T10:33:03Z
dc.date.available
2016-12-20T10:33:03Z
dc.date.issuedpl
2016
dc.date.openaccess
0
dc.description.accesstime
w momencie opublikowania
dc.description.additionalpl
Bibliogr. s. 320-326
dc.description.numberpl
3
dc.description.physicalpl
291-328
dc.description.version
ostateczna wersja wydawcy
dc.description.volumepl
86
dc.identifier.doipl
10.14241/asgp.2016.007
dc.identifier.eissnpl
2300-8512
dc.identifier.issnpl
0208-9068
dc.identifier.projectpl
ROD UJ / P
dc.identifier.uri
http://ruj.uj.edu.pl/xmlui/handle/item/34234
dc.languagepl
eng
dc.language.containerpl
eng
dc.rights*
Udzielam licencji. Uznanie autorstwa - Użycie niekomercyjne - Na tych samych warunkach 4.0 Międzynarodowa
dc.rights.licence
Inna otwarta licencja
dc.rights.uri*
http://creativecommons.org/licenses/by-nc-sa/4.0/legalcode.pl
dc.share.type
otwarte czasopismo
dc.subject.enpl
Cambrian
dc.subject.enpl
trace fossils
dc.subject.enpl
shallow-water marine deposition
dc.subject.enpl
Holy Cross Mountains
dc.subtypepl
Article
dc.titlepl
Ichnology of the Cambrian Ociesęki Sandstone Formation (Holy Cross Mountains, Poland)
dc.title.journalpl
Annales Societatis Geologorum Poloniae
dc.typepl
JournalArticle
dspace.entity.type
Publication
Affiliations

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