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Lituitid cephalopods from the upper Darriwilian and basal Sandbian (Middle-Upper Ordovician) of Estonia

Identifikátory výsledku

  • Kód výsledku v IS VaVaI

    <a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00216208%3A11310%2F20%3A10423812" target="_blank" >RIV/00216208:11310/20:10423812 - isvavai.cz</a>

  • Nalezeny alternativní kódy

    RIV/67985831:_____/20:00541391

  • Výsledek na webu

    <a href="https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=q8EfCNF4NJ" target="_blank" >https://verso.is.cuni.cz/pub/verso.fpl?fname=obd_publikace_handle&handle=q8EfCNF4NJ</a>

  • DOI - Digital Object Identifier

    <a href="http://dx.doi.org/10.1080/11035897.2020.1762723" target="_blank" >10.1080/11035897.2020.1762723</a>

Alternativní jazyky

  • Jazyk výsledku

    angličtina

  • Název v původním jazyce

    Lituitid cephalopods from the upper Darriwilian and basal Sandbian (Middle-Upper Ordovician) of Estonia

  • Popis výsledku v původním jazyce

    Cephalopods of the order Lituitida Starobogatov, 1983 from the late Darriwilian and early Sandbian strata of Estonia are revised herein. During that time, the lituitids reached their peak abundance and were among the key components of cephalopod faunas on Baltica, as well as in other mid- and low-latitude palaeogeographic locations. The Estonian lituitids mostly come from localities representing more off-shore environments with deeper-water sedimentation in the Middle Ordovician. This supports previous assumptions that lituitids preferred pelagic environments and were capable of long-distance migration. In the studied lituitid collection, two genera were identified -LituitesBertrand, 1763 andAncistrocerasBoll, 1857. Three species -Ancistroceras ristnensissp. nov.,Ancistroceras vahikuelaensissp. nov. andLituites nehatuensissp. nov. - were newly established. However, species determinations were often hindered by high intraspecific variability and fragmentary preservation. Investigation of cameral deposits using median sections showed that: connecting rings in chambers with deposits are commonly broken or missing; oriented fragments of connecting rings are present, sometimes overgrown by primary deposits; several generations of primary deposits can be developed; simultaneous presence of both broken and intact connecting rings in the same specimen is usual. These observations elucidate the formation of cameral deposits in lituitids. Currently, this process is explained either by passive deposition from cameral fluids, or active secretion by cameral mantle. The evidence collected herein from Estonian lituitids reveals, however, that both modes of formation might have occurred successively during the lituitid ontogeny and that a gradual, life-time destruction of connecting rings was possibly involved.

  • Název v anglickém jazyce

    Lituitid cephalopods from the upper Darriwilian and basal Sandbian (Middle-Upper Ordovician) of Estonia

  • Popis výsledku anglicky

    Cephalopods of the order Lituitida Starobogatov, 1983 from the late Darriwilian and early Sandbian strata of Estonia are revised herein. During that time, the lituitids reached their peak abundance and were among the key components of cephalopod faunas on Baltica, as well as in other mid- and low-latitude palaeogeographic locations. The Estonian lituitids mostly come from localities representing more off-shore environments with deeper-water sedimentation in the Middle Ordovician. This supports previous assumptions that lituitids preferred pelagic environments and were capable of long-distance migration. In the studied lituitid collection, two genera were identified -LituitesBertrand, 1763 andAncistrocerasBoll, 1857. Three species -Ancistroceras ristnensissp. nov.,Ancistroceras vahikuelaensissp. nov. andLituites nehatuensissp. nov. - were newly established. However, species determinations were often hindered by high intraspecific variability and fragmentary preservation. Investigation of cameral deposits using median sections showed that: connecting rings in chambers with deposits are commonly broken or missing; oriented fragments of connecting rings are present, sometimes overgrown by primary deposits; several generations of primary deposits can be developed; simultaneous presence of both broken and intact connecting rings in the same specimen is usual. These observations elucidate the formation of cameral deposits in lituitids. Currently, this process is explained either by passive deposition from cameral fluids, or active secretion by cameral mantle. The evidence collected herein from Estonian lituitids reveals, however, that both modes of formation might have occurred successively during the lituitid ontogeny and that a gradual, life-time destruction of connecting rings was possibly involved.

Klasifikace

  • Druh

    J<sub>imp</sub> - Článek v periodiku v databázi Web of Science

  • CEP obor

  • OECD FORD obor

    10505 - Geology

Návaznosti výsledku

  • Projekt

  • Návaznosti

    S - Specificky vyzkum na vysokych skolach<br>I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace

Ostatní

  • Rok uplatnění

    2020

  • Kód důvěrnosti údajů

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

Údaje specifické pro druh výsledku

  • Název periodika

    GFF

  • ISSN

    1103-5897

  • e-ISSN

  • Svazek periodika

    142

  • Číslo periodika v rámci svazku

    4

  • Stát vydavatele periodika

    SE - Švédské království

  • Počet stran výsledku

    30

  • Strana od-do

    267-296

  • Kód UT WoS článku

    000547129000001

  • EID výsledku v databázi Scopus

    2-s2.0-85087612097