Summary of East Gondwanan conodont data through the Ireviken Event at Boree Creek

Result code in IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F60460709%3A41330%2F21%3A85413" target="_blank" >RIV/60460709:41330/21:85413 - isvavai.cz</a>
Result on the web
<a href="https://link.springer.com/article/10.1007/s12583-021-1310-9?utm_source=xmol&utm_medium=affiliate&utm_content=meta&utm_campaign=DDCN_1_GL01_metadata" target="_blank" >https://link.springer.com/article/10.1007/s12583-021-1310-9?utm_source=xmol&utm_medium=affiliate&utm_content=meta&utm_campaign=DDCN_1_GL01_metadata</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1007/s12583-021-1310-9" target="_blank" >10.1007/s12583-021-1310-9</a>

Result language
angličtina
Original language name
Summary of East Gondwanan conodont data through the Ireviken Event at Boree Creek
Original language description
The Ireviken Event was the first Middle Paleozoic event consisting of synchronised faunal, isotopic and facies change to be recognised. An analysis of the conodont faunas throughout the Boree Creek/Borenore Limestone succession in the central western region of the Tasman fold belt of New South Wales (Australia) revealing all five conodont zones that comprise the event is presented. While some zonal boundaries are precise, allowing direct comparison of stratigraphic intervals on other paleo-continents, some can only be approximated. Conodont data from pre-Ireviken Event strata, in contrast, only permit the identification of a broad Telychian chronology. The identification of Wenlock post-Ireviken Event conodont zones is incomplete due to lithological variability, namely the presence of tuffaceous beds near the top of the formation and an unconformity between the Boree Creek and overlying Borenore Limestone. The Boree Creek Formation contains the only example of the Ireviken Event discovered t
Czech name
—
Czech description
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Type
J<sub>imp</sub> - Article in a specialist periodical, which is included in the Web of Science database
CEP classification
—
OECD FORD branch
10506 - Paleontology

Project
<a href="/en/project/GA17-18120S" target="_blank" >GA17-18120S: Ca and O Isotope Constraints on the Origin of C Isotope Anomalies: Testing the Model of Global ‘Carbonate Hypersaturation’ of Silurian Seawater</a><br>
Continuities
P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Publication year
2021
Confidentiality
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

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