Ammonoids and nautiloids from the earliest Spathian Paris Biota and other early Spathian localities in southeastern Idaho, USA

Affiliation auteurs!!!! Error affiliation !!!!
TitreAmmonoids and nautiloids from the earliest Spathian Paris Biota and other early Spathian localities in southeastern Idaho, USA
Type de publicationJournal Article
Year of Publication2019
AuteursBrayard A, Jenks JF, Bylund KG, Escarguel G, Fara E, Goudemand N, Gueriau P, Jenks JF, Krumenacker L.J, Olivier N, Stephen DA, Thomazo C, Thoury M, Vennin E, Team PBiota
JournalGEOBIOS
Volume54
Pagination13-36
Date PublishedJUN
Type of ArticleArticle
ISSN0016-6995
Mots-clésAmmonoidea, Biostratigraphy, Early Triassic, Nautiloidea, Panthalassa, Sonoma Foreland Basin
Résumé

Intensive sampling of three earliest Spathian sites represented by the Lower Shale unit and coeval beds within the Bear Lake vicinity and neighboring areas, southeastern Idaho, yielded several new ammonoid and nautiloid assemblages. These new occurrences overall indicate that the lower boundary of the Tirolites beds, classically used as a regional marker for the base of the early Spathian, and therefore the regional Smithian/Spathian boundary, must be shifted downward into the Lower Shale unit and coeval beds. Regarding ammonoids, one new genus (Caribouceras) and two new species (Caribouceras slugense and Albanites americanus) are described. In addition, the regional temporal distribution of Bajarunia, Tirolites, Columbites, and Coscaites is refined, based on a fourth sampled site containing a newly reported occurrence of the early Spathian Columbites fauna in coeval beds of the Middle Shale unit. As a complement to ammonoids, changes observed in nautiloid dominance are also shown to facilitate correlation with high-latitude basins such as Siberia during this short time interval, and they also highlight the major successive environmental fluctuations that took place during the late Smithian early Spathian transition. (C) 2019 Elsevier Masson SAS. All rights reserved.

DOI10.1016/j.geobios.2019.04.007