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dc.contributor.authorMergl, Michal
dc.date.accessioned2022-01-10T11:00:27Z-
dc.date.available2022-01-10T11:00:27Z-
dc.date.issued2021
dc.identifier.citationMERGL, M. Dead or alive? Brachiopods and other shells as substrates for endo- and sclerobiont activity in the Early Devonian (Lochkovian) of the Barrandian (Czechia). Bulletin of Geosciences, 2021, roč. 96, č. 4, s. 401-429. ISSN: 1214-1119cs
dc.identifier.issn1214-1119
dc.identifier.uri2-s2.0-85117228968
dc.identifier.urihttp://hdl.handle.net/11025/46568
dc.format29 s.cs
dc.format.mimetypeapplication/pdf
dc.language.isoenen
dc.publisherCzech Geological Surveyen
dc.relation.ispartofseriesBulletin of Geosciencesen
dc.rights© Czech Geological Surveyen
dc.titleDead or alive? Brachiopods and other shells as substrates for endo- and sclerobiont activity in the Early Devonian (Lochkovian) of the Barrandian (Czechia)en
dc.typečlánekcs
dc.typearticleen
dc.rights.accessopenAccessen
dc.type.versionpublishedVersionen
dc.description.abstract-translatedTwelve encrusters and three endobiont trace fossils were distinguished on silicified brachiopod, coral and gastropod shells coming from the Kotýs Limestone (Lochkovian) of the Prague Basin, Bohemia. Encrusters preferred larger and costellate brachiopod shells with prominent convexity of valves. Locations and developments of coral encrustations produced by tabulate Aulopora sp., rugose Syringaxon sp., and an unnamed rugose coral indicate different strategies in selection of substrate. The auloporid preferred living host, articulated shells or intact valves, the rugose corals were less selective and colonised also dead and broken shells. Unlike encruster associations of middle and upper Devonian age in other areas (France, Poland, USA), in Bohemia, the encruster hosts were chiefly orthids (Parmorthina Havlíček, 1975; Isorthis Kozłowski, 1929; Dalejina Havlíček, 1953; Resserella Bancroft, 1928) and atrypids (Spinatrypa Stainbrook, 1951). Apart from corals, a microproblematicum Allonema Ulrich & Bassler, 1904, two pterobranchs, bryozoans, a hederellid, a craniid, a protorthid brachiopod, and a microconchid were observed on host shells together with small dendritic borings, cylindrical borings of Trypanites Mägdefrau, 1932, and a dendritic structure of unclear origin.en
dc.subject.translatedbioerosionen
dc.subject.translatedencrustersen
dc.subject.translatedBrachiopodaen
dc.subject.translatedAuloporaen
dc.subject.translatedAllonemaen
dc.subject.translatedLochkovianen
dc.identifier.doi10.3140/bull.geosci.1838
dc.type.statusPeer-revieweden
dc.identifier.document-number726720800002
dc.identifier.obd43933755
dc.project.IDGA18-05935S/Z minulosti do přítomnosti: fosilní versus recentní schránky mořských živočichů jako substrát pro kolonizaci a bioerozics
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