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TitleNew conodont faunal assemblages from the Anisian of British Columbia and their use in local stratigraphic correlation
AuthorGolding, M; Orchard, M J
SourceGeological Society of America, Abstracts With Programs 2014.
LinksOnline - En ligne
Year2014
Alt SeriesEarth Sciences Sector, Contribution Series 20140180
PublisherGeological Society of America
MeetingGeological Society of America, Annual Meeting; Vancouver; CA; October 19-22, 2014
Documentserial
Lang.English
Mediapaper; on-line
File formatpdf
ProvinceBritish Columbia
NTS93I; 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
Areanortheastern British Columbia
Lat/Long WENS-136.0000 -120.0000 60.0000 54.0000
Subjectsgeochronology; paleontology; stratigraphy; conodonts; fossils; biostratigraphy; taxonomy; fossil assemblages; biochronology
ProgramWestern Arctic Sverdrup Basin, GEM2: Geo-mapping for Energy and Minerals
AbstractConodonts 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.
Summary(Plain Language Summary, not published)
Preliminary intercalibration of the successions of conodonts and ammonoids in the marine Middle Triassic of North America is presented. Although ammonoids may be abundant in outcrop sections, the more ubiquitous conodonts enable correlation between outcrop and subsurface drill core, vital in basin analysis. Central to the enhancement of the conodont tool are taxonomic revisions currently underway: newly identified taxa allow the delineation of eleven new faunal assemblages that show the promise of broad application.
GEOSCAN ID295135