English (United Kingdom)

https://curated-unify.zendy.io/wp-json/zendy-region/v1/featured_content/oa?rat=en

https://curated-unify.zendy.io/wp-json/zendy-region/v1/highlighted_journal/

Global: Zendy Plus annual

Presents the access of premium content as premium feature

Premium Content

Presents the keyphrase highlighting as premium feature

Keyphrase Highlighting

Presents the summarisation as premium feature

Summarisation

Insights

Presents the pdf analysis as premium feature

PDF Analysis

Presents the zaia usage as premium feature

ZAIA

Global: Zendy Tools annual

Global: Zendy Free Plan

Global: Zendy Tools monthly

Global: Zendy Plus monthly

The biostratigraphy of Calasparra Section is well-estabished with an ammonoid biozonation and ranges from Lower to Upper Ladinian. The continuous presence of Pseudofurnishius murcianus van den Boogaard, a characteristic conodont species of the Sephardic realm, along the section makes it one of the most important sections in the Iberian Peninsula for the study of the species. The first apparition of P. murcianus in the section corresponds with the first of Eoprotrachyceras curionii taxon, which is the principal marker for the base of the Ladinian stage in the GSSP of the Anisian-Ladinian boundary, and the age of the youngest conodonts, based on ammonoids (Epigonus Zone) is Lower Ladinian (upper Fassanian). This is similar to the range of P. murcianus in the Saharonim Formation in Israel, where its earliest appearance is also Early Fassanian (Curionii zone) age.La bioestratigrafía de la Sección de Calasparra está bien establecida mediante biozonación de ammonoideos, con una edad que va desde el Ladiniense inferior hasta el Longobardiense. La presencia continua de Pseudofurnishius murcianus van den Boogaard, una especie de conodontos característica del Dominio Sephardí, a lo largo de la sección la hace una de las más importantes de la Península Ibérica para el estudio de la especie. La primera aparición de P. murcianus en la sección se corresponde con el taxón Eoprotachyceras curionii, que es el principal marcador para la base del piso Ladiniense en el GSSP del límite Anisiense-Ladiniense, mientras que la edad de los conodontos más recientes, basada en ammonites (Epigonus Zone) es Ladiniense Inferior (Fassaniense superior) Este rango es similar al de P. murcianus en la Formación Saharonim en Israel, de edad Fassaniense inferior (Zona Curionii)

journal of iberian geology

Discussion about the stratigraphic range of "Pseudofurnishius murcianus" van den Boogaard (Conodonta) in the Iberian Peninsula, from the Calasparra section (Murcia, Spain)