SciELO - Scientific Electronic Library Online

 
vol.75 número2Parientes fósiles de parásitos actuales de crustáceos, del Mesozoico de EuropaBiogeoquímica isotópica y desgaste dental en Mammuthus columbi: Análisis multiproxy y revisión para su reconstrucción paleodietética índice de autoresíndice de materiabúsqueda de artículos
Home Pagelista alfabética de revistas  

Servicios Personalizados

Revista

Articulo

Indicadores

Links relacionados

  • No hay artículos similaresSimilares en SciELO

Compartir


Boletín de la Sociedad Geológica Mexicana

versión impresa ISSN 1405-3322

Resumen

HUITRON-VARGAS, Gilberto  y  TORRES-MARTINEZ, Miguel A.. New records of columnar ossicles of crinoids from the Permian (early Cisuralian) of Chiapas, Mexico. Bol. Soc. Geol. Mex [online]. 2023, vol.75, n.2, A120423.  Epub 07-Jun-2024. ISSN 1405-3322.  https://doi.org/10.18268/bsgm2023v75n2a120423.

We described a new association of 10 morphospecies of crinoid columnar ossicles from eight different morphogenera. The biota includes Cylindrocauliscus fiski, Cyclocaudex cf. plenus, Cyclocaudex costatus, Preptopremnum cf. rugosum, Preptopremnum leave, Heterostelechus jeffordsi, Cycloscapus laevis, Cyclocaudiculus regularis, Nothrosterigma merum, and Cyclogrupera minor. The specimens were located in rocks from the Grupera Formation of Asselian-Sakmarian age (lower Permian). The lithostratigraphic unit belongs to the Carboniferous-Permian succession that outcrops in the Chicomuselo region in southeastern Mexico. It is recorded the first occurrence of C. costatus, P. rugosum, C. laevis, and N. merum for the Cisuralian of North America. Likewise, it highlights the first record of N. merum in Mexico, which along with P. rugosum are reported for the first time in the Cisuralian of North America. Despite controversy over the usefulness of crinoid ossicles as index fossils, it was possible relating the rocks of the locality studied to an approximate Asselian-Sakmarian age (early Cisuralian), previously suggested for the formation. Furthermore, the find of ossicles associated with other filtering marine invertebrates such as bryozoans and brachiopods, as well as preservation and lithological features of the rocks, allowed establishing that the depositional paleoenvironment was related to shallow water facies of high energy, well-illuminated, and with an important terrigenous supply. Regarding paleobiogeography, the distribution of crinoids was associated with the region’s geologic history, which was influenced by oceanic and continental changes that occurred during the formation of the Pangea supercontinent in the Late Pennsylvanian. This favored the emergence of generic and specific provincialisms in North America.

Palabras llave : Crinoid ossicles; Asselian - Sakmarian; Grupera Formation; paleoenvironment; paleobiogeography.

        · resumen en Español     · texto en Español