Journal article

Allometry in Anisian (Middle Triassic) segminiplanate conodonts and its implications for conodont taxonomy


Authors listChen, YL; Neubauer, TA; Krystyn, L; Richoz, S

Publication year2016

Pages725-741

JournalPalaeontology

Volume number59

Issue number5

ISSN0031-0239

DOI Linkhttps://doi.org/10.1111/pala.12253

PublisherWiley


Abstract
Conodonts are a clade of chordates and are valuable indicator fossils for biostratigraphy. The segminiplanate (neogondolelliform) conodonts represent a major morphological group ranging from upper Carboniferous to Upper Triassic marine sediments. However, the morphological similarity of segminiplanate P1 elements generates problems for taxonomy, especially in the Permian and Triassic clades. This paper represents the first study of morphological variation in Triassic segminiplanate conodonts using a geometric morphometric approach. The laminar microstructures observed in conodont cross-sections indicate that, within our analysed specimens, smaller conodonts with fewer laminae are generally from an earlier ontogenetic stage while larger conodonts with more laminae are from a later stage of ontogeny. Using linear regressions between relative warp scores from both upper and lateral views and conodont length, we demonstrate strongly allometric growth patterns for the species Paragondolella bifurcata Budurov & Stefanov. Our results indicate that the species-group taxon Pg. praeszaboi bystrickyi (Kovacs et al.) is an early growth stage of Pg. bifurcata and thus synonymous. We suggest that the allometry of conodonts should be considered seriously, especially when there are numerous transitional morphologies between large-and small-sized conodonts. Reconstructing the ontogenetic series and using larger-sized conodonts within the numerous transitional morphologies in the population of a rock sample for the definition of new species are suggested for future studies.



Citation Styles

Harvard Citation styleChen, Y., Neubauer, T., Krystyn, L. and Richoz, S. (2016) Allometry in Anisian (Middle Triassic) segminiplanate conodonts and its implications for conodont taxonomy, Palaeontology, 59(5), pp. 725-741. https://doi.org/10.1111/pala.12253

APA Citation styleChen, Y., Neubauer, T., Krystyn, L., & Richoz, S. (2016). Allometry in Anisian (Middle Triassic) segminiplanate conodonts and its implications for conodont taxonomy. Palaeontology. 59(5), 725-741. https://doi.org/10.1111/pala.12253


Last updated on 2025-21-05 at 16:37