PUCADELPHYDAE, de Muizon, 1998

Ladevèze, Sandrine, 2007, Petrosal bones of metatherian mammals from the Late Palaeocene of Itaboraí (Brazil), and a cladistic analysis of petrosal features in metatherians, Zoological Journal of the Linnean Society 150 (1), pp. 85-115 : 106

publication ID

https://doi.org/ 10.1111/j.1096-3642.2007.00282.x

DOI

https://doi.org/10.5281/zenodo.5489154

persistent identifier

https://treatment.plazi.org/id/03C13264-FFF0-FFCA-FEE1-27A6C343FADC

treatment provided by

Felipe

scientific name

PUCADELPHYDAE
status

 

PUCADELPHYDAE

This clade is supported by three unambiguous and two ambiguous synapomorphies.

The presence of a broad shelf of bone that surrounds the fenestra cochleae and makes a separation between it and the aqueductus cochleare is autapomorphic for pucadelphids (16 0> 1, RI = 1.000).

A vascular groove adjacent to the prootic sinus sulcus (36 0> 1, RI = 0.250) was observed on the mastoid part of petrosals of Pucadelphys , Andinodelphys , Type I, Type III, and the extant marsupials Monodelphis ( Wible, 2003) and Phascogale . This groove probably received a vein from the prootic sinus. The variability of this homoplastic character has not been tested on extant marsupials, because of the rarity of isolated petrosals.

The absence of a post-temporal sulcus on the squamosal surface of the petrosal for the diploetic vessels (37 0> 1, RI = 0.750) is a convergent apomorphy with the clade formed by Australidelphia, Caenolestes , and the Petrosal Types I, III, IV , and V.

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