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TitreNew conodont faunal assemblages from the Anisian of British Columbia and their use in local stratigraphic correlation
AuteurGolding, M; Orchard, M J
SourceGeological Society of America, Abstracts With Programs 2014.
LiensOnline - En ligne
Année2014
Séries alt.Secteur des sciences de la Terre, Contribution externe 20140180
ÉditeurGeological Society of America
RéunionGeological Society of America, Annual Meeting; Vancouver; CA; Octobre 19-22, 2014
Documentpublication en série
Lang.anglais
Mediapapier; en ligne
Formatspdf
ProvinceColombie-Britannique
SNRC93I; 93J; 93K; 93L; 93M; 93N; 93O; 93P; 94; 103I; 103P; 104A; 104G; 104H; 104I; 104J; 104K; 104M/01; 104M/07; 104M/08; 104M/09; 104M/10; 104M/10; 104M/11; 104M/13; 104M/14; 104M/15; 104M/16; 104N; 104O; 104P
Lat/Long OENS-136.0000 -120.0000 60.0000 54.0000
Sujetsconodontes; fossiles; biostratigraphie; taxonomie; assemblages fossiles; stratigraphie paléontologique; géochronologie; paléontologie; stratigraphie
ProgrammeBassin de Sverdrup de l'ouest de l'Arctique, GEM2 : La géocartographie de l'énergie et des minéraux
Résumé(disponible en anglais seulement)
Conodonts and ammonoids are the two most useful and widely used taxonomic groups for biostratigraphy in the marine Triassic of North America. Both groups have a well-established zonation throughout the Triassic. However, during the Anisian stage (Middle Triassic) in North America, the resolution of the current conodont zonation is not as precise as that of the ammonoids. Although ammonoids are often abundant in some outcrop sections, conodonts are far more ubiquitous, and the lack of resolution in their zonation during this stage affects the precision and accuracy of correlation between sections. This lack of precision is particularly problematic when attempting to correlate between outcrop sections and subsurface drill core, as ammonoids are virtually absent in the latter.
The lack of resolution in the conodont zonation is due in part to the broad taxonomic concepts that have previously been applied to conodont species from the Anisian of North America; the majority of specimens recovered from rocks of this age have been assigned to one of only six species belonging to either Neogondolella or Paragondolella. This has led to the obscuring of morphological variability, some of which is now thought to be stratigraphically significant.
Examination of new and existing collections from outcrop sections and subsurface drill core in northeastern British Columbia has allowed the recognition of 10 new species of conodonts belonging to Neogondolella, as well as 19 new morphotypes of species of Neogondolella and Paragondolella. This represents a dramatic increase in taxa from the six species that have commonly been recognized in the past. These new species and morphotypes allow the delineation of eleven new, informal conodont faunal assemblages that enable correlation between outcrop sections and subsurface drill core across British Columbia. These assemblages have not yet been formalized as biozones, pending further work on existing material to constrain their stratigraphical and geographical extent. At present, these assemblages appear to be applicable at a local scale, and further work on Anisian faunas from the Canadian Arctic and Nevada is underway to determine if they can be recognised at a regional scale as well.
Résumé(Résumé en langage clair et simple, non publié)
Un étalonnage comparatif préliminaire des successions de conodontes et d'ammonoïdés du Trias moyen marin en Amérique du Nord est présenté. Bien que les ammonoïdés puissent être abondants dans les affleurements rocheux, les conodontes, plus omniprésents, permettent d'établir des corrélations entre les affleurements rocheux et les carottes prélevées sous la surface, ce qui est essentiel dans le cadre des études paléogéographiques. Les révisions taxinomiques actuellement en cours sont au c'ur de l'amélioration de l'utilisation des conodontes : les taxons nouvellement identifiés permettent de délimiter onze nouveaux assemblages qui promettent d'être largement utilisés.
GEOSCAN ID295135