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

Kód výsledku v 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>

Výsledek na webu

<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>

Jazyk výsledku

angličtina

Název v původním jazyce

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

Popis výsledku v původním jazyce

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

Název v anglickém jazyce

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

Popis výsledku anglicky

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

Druh

J_imp - Článek v periodiku v databázi Web of Science

CEP obor

—

OECD FORD obor

10506 - Paleontology

Projekt

<a href="/cs/project/GA17-18120S" target="_blank" >GA17-18120S: Mechanismus vzniku izotopových anomalií C vyplývající ze studia izotopů Ca a O: Test modelu globální „karbonátové hypersaturace“ silurské mořské vody</a><br>

Návaznosti

P - Projekt vyzkumu a vyvoje financovany z verejnych zdroju (s odkazem do CEP)

Rok uplatnění

2021

Kód důvěrnosti údajů

S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů

Název periodika

Journal of Earth Science

ISSN

1674-487X

e-ISSN

1867-111X

Svazek periodika

32

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

CZ - Česká republika

Počet stran výsledku

12

Strana od-do

512-523

Kód UT WoS článku

000658321900005

EID výsledku v databázi Scopus

2-s2.0-85107187905