Refining the late Silurian sea‑level history of the Prague Syncline—a case study based on the Přídolí GSSP (Czech Republic)
The result's identifiers
Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00025798%3A_____%2F18%3A00000125" target="_blank" >RIV/00025798:_____/18:00000125 - isvavai.cz</a>
Alternative codes found
RIV/67985831:_____/18:00496845 RIV/00023272:_____/18:10134042
Result on the web
<a href="https://link.springer.com/article/10.1007/s10347-018-0542-3" target="_blank" >https://link.springer.com/article/10.1007/s10347-018-0542-3</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s10347-018-0542-3" target="_blank" >10.1007/s10347-018-0542-3</a>
Alternative languages
Result language
angličtina
Original language name
Refining the late Silurian sea‑level history of the Prague Syncline—a case study based on the Přídolí GSSP (Czech Republic)
Original language description
A 50-m-thick section in the Požáry quarry, Prague Syncline (Czech Republic) spanning the upper Silurian (uppermost Ludlow and Přídolí) to the lowermost Devonian (Lochkovian) has been studied using sedimentological and physical stratigraphical (gamma-ray spectrometry) methods combined with conodont biostratigraphy. Conodont data demonstrate the presence of local conodont biozones: “Ozarkodina” crispa (uppermost Ludlow)—Zieglerodina zellmeri (base of Přídolí)—Zieglerodina ivochlupaci—Delotaxis detorta—“Ozarkodina” eosteinhornensis s.s.—Zieglerodina klonkensis—Icriodus hesperius-optima (lowermost Lochkovian). The studied section represents a transgressive–regressive facies succession characterized by a transition from distal calciturbidites deposited in a distally steepened carbonate platform during transgression and sea-level highstand (crispa to lower ivochlupaci zones) to mixed calciturbidites/coarse-grained bioclastic limestones (falling-stage systems tract, upper ivochlupaci to lower klonkensis zones). The upper part of the succession consists of bioclastic limestones corresponding to a subtidal setting between storm-wave and fair-weather wave base (lowstand systems tract in upper klonkensis and hesperius-optima zones). This interpretation corresponds to the late Silurian global sea-level pattern as recorded in other regions. Thus the depositional system is interpreted as mostly driven by eustasy with short-lived periods of influence from local tectonics.
Czech name
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Czech description
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Classification
Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
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OECD FORD branch
10505 - Geology
Result continuities
Project
<a href="/en/project/GA17-06700S" target="_blank" >GA17-06700S: Přídolí Series in the Prague Synform - proposal for chronostratigraphic subdivision</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)
Others
Publication year
2018
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Data specific for result type
Name of the periodical
Facies
ISSN
0172-9179
e-ISSN
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Volume of the periodical
64
Issue of the periodical within the volume
4:30
Country of publishing house
DE - GERMANY
Number of pages
16
Pages from-to
nestránkováno
UT code for WoS article
000446583400001
EID of the result in the Scopus database
2-s2.0-85054160978