Skip navigation

Zastosuj identyfikator do podlinkowania lub zacytowania tej pozycji: http://hdl.handle.net/20.500.12128/12676
Pełny rekord metadanych
DC poleWartośćJęzyk
dc.contributor.authorZatoń, Michał-
dc.contributor.authorKremer, Barbara-
dc.contributor.authorMarynowski, Leszek-
dc.contributor.authorWilson, Mark A.-
dc.contributor.authorKrawczyński, Wojciech-
dc.date.accessioned2020-02-18T12:14:21Z-
dc.date.available2020-02-18T12:14:21Z-
dc.date.issued2011-
dc.identifier.citation"Facies" Vol. 58, iss. 1 (2012), s. 57-77pl_PL
dc.identifier.issn1612-4820-
dc.identifier.issn0172-9179-
dc.identifier.urihttp://hdl.handle.net/20.500.12128/12676-
dc.description.abstractOncoids from two localities (Ogrodzieniec and Blanowice) of the Polish Jura, southern Poland, have been investigated with respect to their genesis and paleoecology. These oncoids occur within Middle Jurassic (Bathonian) deposits. Those from Ogrodzieniec are large, elliptical, and embedded within a presumably condensed carbonate bed. Those from Blanowice, on the contrary, are significantly smaller, irregular to box-like in shape, and occur within the ore-bearing clays. The oncoids fromboth localities consist of a distinct carbonate core and laminated cortex that is significantly thicker and better preserved in the Ogrodzieniec oncoids. SEM and optical microscopic investigation of the oncoid cortices revealed the presence of carbonate and silicate layers withweb-like structures similar to those occurring in recent cyanobacterial microbialites. Thus, the oncoid cortices investigated may have formed in a photic zone environment with the aid of coccoid and filamentous cyanobacteria. Oxic conditions prevailed during oncoid cortex formation within the siliciclastic setting, which is manifested by low total organic carbon content, high pristane/phytane (Pr/Ph) ratio, and significant predomination of the C31 homohopanes. On the cortices’ surfaces, as well as between particular laminae, various encrusting organisms have been found. The encrusters, dominated by serpulids and bryozoans, are cryptic species that inhabited the undersides and recesses of the oncoids. Their presence on both the upper and lower surfaces of the oncoids indicates that the oncoids were episodically overturned on the seafloor. The much better developed cortex lamination and much higher diversity and abundance of encrusters in the Ogrodzieniec oncoids may point to better trophic conditions prevailing in a shallower marine environment characterized by transparent waters, as opposed to a deeper siliciclastic environment with less transparent waters and probably worse trophic conditio.pl_PL
dc.language.isoenpl_PL
dc.rightsUznanie autorstwa-Użycie niekomercyjne 3.0 Polska*
dc.rights.urihttp://creativecommons.org/licenses/by-nc/3.0/pl/*
dc.subjectOncoidspl_PL
dc.subjectCyanobacteriapl_PL
dc.titleMiddle Jurassic (Bathonian) encrusted oncoids from the Polish Jura, southern Polandpl_PL
dc.typeinfo:eu-repo/semantics/articlepl_PL
dc.identifier.doi10.1007/s10347-011-0273-1-
Pojawia się w kolekcji:Artykuły (WNP)

Pliki tej pozycji:
Plik Opis RozmiarFormat 
Zaton_Middle_Jurassic_(Bathonian)_encrusted.pdf2,27 MBAdobe PDFPrzejrzyj / Otwórz
Pokaż prosty rekord


Uznanie autorstwa - użycie niekomercyjne 3.0 Polska Creative Commons Creative Commons