Hadimopanella oezgueli Gedik, 1977: a palaeoscolecidan sclerite useless for taxonomic purposes

Kód výsledku v IS VaVaI

<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F49777513%3A23420%2F14%3A43923359" target="_blank" >RIV/49777513:23420/14:43923359 - isvavai.cz</a>

Výsledek na webu

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DOI - Digital Object Identifier

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Jazyk výsledku

angličtina

Název v původním jazyce

Hadimopanella oezgueli Gedik, 1977: a palaeoscolecidan sclerite useless for taxonomic purposes

Popis výsledku v původním jazyce

A new assemblage of Hadimopanella oezgueli Gedik, 1977 is described from the middle Caesaraugustan (mid Cambrian) part of the Genestosa Member (Oville Formation) in the Cantabrian Mountains, northern Spain. Sclerites occur disarticulated and display distinct diagenetic processes, with authigenic chlorites occluding primary porosity and secondary fissures. Sclerite distribution was controlled by patchy development of epibenthic multispecies clumps on shell (both carbonate and clayey) substrates. A jointbiometric and statistical analysis in both dorsal and lateral views of disarticulated sclerites allows characterization of two distinct morphotypes. These are compared with other occurrences of H. oezgueli sclerites from other margins of Gondwana and theSiberian Platform, as a result of which, another morphotype is identified. Two main inferences can be drawn: (i) different ventral trunk-sided sclerites of a same scleritome comprise different sclerite morphotypes and (ii) one distinct s

Název v anglickém jazyce

Hadimopanella oezgueli Gedik, 1977: a palaeoscolecidan sclerite useless for taxonomic purposes

Popis výsledku anglicky

A new assemblage of Hadimopanella oezgueli Gedik, 1977 is described from the middle Caesaraugustan (mid Cambrian) part of the Genestosa Member (Oville Formation) in the Cantabrian Mountains, northern Spain. Sclerites occur disarticulated and display distinct diagenetic processes, with authigenic chlorites occluding primary porosity and secondary fissures. Sclerite distribution was controlled by patchy development of epibenthic multispecies clumps on shell (both carbonate and clayey) substrates. A jointbiometric and statistical analysis in both dorsal and lateral views of disarticulated sclerites allows characterization of two distinct morphotypes. These are compared with other occurrences of H. oezgueli sclerites from other margins of Gondwana and theSiberian Platform, as a result of which, another morphotype is identified. Two main inferences can be drawn: (i) different ventral trunk-sided sclerites of a same scleritome comprise different sclerite morphotypes and (ii) one distinct s

Druh

J_x - Nezařazeno - Článek v odborném periodiku (Jimp, Jsc a Jost)

CEP obor

DB - Geologie a mineralogie

OECD FORD obor

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Projekt

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Návaznosti

I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Rok uplatnění

2014

Kód důvěrnosti údajů

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

Název periodika

Palaeontologia Electronica

ISSN

1094-8074

e-ISSN

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Svazek periodika

17

Číslo periodika v rámci svazku

3

Stát vydavatele periodika

GB - Spojené království Velké Británie a Severního Irska

Počet stran výsledku

20

Strana od-do

1-20

Kód UT WoS článku

000345393600012

EID výsledku v databázi Scopus

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