IDEAN   23403
INSTITUTO DE ESTUDIOS ANDINOS "DON PABLO GROEBER"
Unidad Ejecutora - UE
congresos y reuniones científicas
Título:
Allometric growth pattern in the genus Ptychomya from the Lower Cretaceous of the Neuquén Basin, west-central Argentina
Autor/es:
MILLA CARMONA, P.S., LAZO D.G. & SOTO, I.
Lugar:
Mendoza
Reunión:
Congreso; 4th International Palaeontological Congress; 2014
Resumen:
Ptychomya koeneni Behrendsen is a frequently recorded heterodont bivalve in Lower Cretaceous
marine rocks of the Neuquén Basin, especially in the Agrio Formation. It shows a characteristic
divaricate ornamentation, which makes it easy to be identified. The sole published study to
date on its taxonomy has established the existence of six varieties of subspecific rank. However,
a recent unpublished study by the authors based on newly collected specimens from the Agrio
Formation and type specimens of the mentioned varieties from the Burke Museum of Natural
History & Culture (Seattle, USA) found out that there is a wide morphological gap between one
of the varieties, namely P. koeneni coihuicoensis, and the rest of them, suggesting that they could be
two distinct groups. The aim of this work was to compare the allometric growth patterns of P. k.
coihuicoensis and the P. koeneni cluster in order to determine if they share a common ontogeny. Two
aspects of external morphology of the shell were quantified (general outline and ornamentation) for
specimens of each group at different shell sizes (i.e. growth stages) using geometric morphometrics.
Allometric curves were statistically compared through regressions with categorical predictors for
each morphological variable. Results showed that while some morphological variables seemed to
share a common allometric curve, there are other variables that differ in their growth attributes
(i.e. regression curves have a statistically different origin and/or slope). Shape trajectories of P. k.
coihuicoensis and the P. koeneni cluster differed along the ontogeny in the multivariate morphospace,
meaning that the overall growth pattern was different between these two groups. This evidence
supports the hypothesis that P. k. coihuicoensis is a distinct group separated from the rest of the P.
koeneni varieties, and points out the need for a taxonomical reevaluation of the genus Ptychomya in
the Lower Cretaceous of the Neuquén Basin.