Diminutive epibionts on crinoid stems from the Lower/Middle Devonian boundary in the Barrandian, Czech Republic
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F49777513%3A23420%2F22%3A43966762" target="_blank" >RIV/49777513:23420/22:43966762 - isvavai.cz</a>
Result on the web
<a href="http://hdl.handle.net/11025/51539" target="_blank" >http://hdl.handle.net/11025/51539</a>
DOI - Digital Object Identifier
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Alternative languages
Result language
angličtina
Original language name
Diminutive epibionts on crinoid stems from the Lower/Middle Devonian boundary in the Barrandian, Czech Republic
Original language description
Diminutive crinoid holdfasts and cemented tests of the foraminifers Psammosphaera and Toly pammina were observed on coarse bioclasts in weathered limestones of the Daleje-Třebotov Formation. Specimens were obtained in 1984 by washing so called “white beds” at a temporary locality in Praha Barrandov. A few millimeter sized bioclasts with epibionts were freed from hard limestone beds of the Třebotov Limestone near the Lower/Middle Devonian boundary by long-term weathering. Many of the crinoid holdfasts attached to pluricolumnals provoked a stereomic response of the host crinoid. Also the growth orientation of the crinoid epibiont is not random and indicates some crinoid-epibiont to crinoid host interaction. Reaction of host stereome and non-random stem orientation offer direct evidence of epi biont larval settlement and subsequent growth on the stem of a living crinoid host. The extensive growth of the host stereome ended by partial to total engulfing of the epibiont holdfast. This indicates advancing and finally successful defence of the host crinoid against the epibiont. The holdfast gives evidence that the small host crinoids offered a somewhat higher tier for even smaller epibiont crinoids. However, other observed holdfasts indicate fixation of larva and growth over loose bioclasts lying on a sea bed. Location of foraminifer test on bioclasts confims that foraminifers cemented and grew on loose echinodermal and brachiopod remains and preferred crevices and similar protected sites with concave profiles. This is clear evidence that diverse bioclasts (brachiopod shells, pelmatozoan ossicles) provided the hard substrate suitable for epibiont life on a sea bed.
Czech name
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Czech description
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Classification
Type
J<sub>ost</sub> - Miscellaneous article in a specialist periodical
CEP classification
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OECD FORD branch
10506 - Paleontology
Result continuities
Project
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Continuities
S - Specificky vyzkum na vysokych skolach
Others
Publication year
2022
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Folia Musei rerum naturalium Bohemiae occidentalis - Geologica et Paleobiologica
ISSN
1805-2371
e-ISSN
1805-286X
Volume of the periodical
56
Issue of the periodical within the volume
1-2
Country of publishing house
CZ - CZECH REPUBLIC
Number of pages
16
Pages from-to
27-42
UT code for WoS article
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EID of the result in the Scopus database
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