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1 March 2013 Reinvestigation of the Basicranium of Haldanodon Exspectatus (Mammaliaformes, Docodonta)
Irina Ruf, Zhe-Xi Luo, Thomas Martin
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Abstract

The docodont Haldanodon exspectatus, a mammaliaform from the Late Jurassic of Portugal, is a crucial taxon for studying higher-level relationships of mammaliaforms and their morphological evolution. Based on high-resolution computed tomography scanning of three specimens of Haldanodon, we developed a new reconstruction of the basicranium including the petrosal and the inner ear. Our study confirms that Haldanodon and other basal mammaliaforms, such as Morganucodon and Sinoconodon, are similar in the main characteristics of their external anatomy of the petrosal. However, Haldanodon shows several derived features that support a phylogenetic position of docodonts more derived than Morganucodon and Sinoconodon: (1) elongated and curved cochlear canal (nearly 180°), (2) single lateral flange foramen of petrosal, (3) absence of anterior paroccipital process, and (4) squamosal constriction. The bony labyrinth reveals a secondary crus commune, which is regarded to be a plesiomorphic feature of the mammaliaform groundplan. The cochlear canal shows an apical inflation connected to a distinct sulcus and a separate notch in the internal acoustic meatus, supporting the existence of a lagenar nerve and macula as in monotremes. Haldanodon is unique among Mesozoic mammaliaforms in having a hypertrophied paroccipital region that is excavated into large tympanic pneumatic recesses, which are connected with the extensive porous and probably also pneumatic internal structures of the surrounding bones. The curved cochlear canal and the pneumatized middle ear region support the hypothesis that Haldanodon had more effective low-frequency hearing as an adaptation to a fossorial mode of life.

© 2013 by the Society of Vertebrate Paleontology
Irina Ruf, Zhe-Xi Luo, and Thomas Martin "Reinvestigation of the Basicranium of Haldanodon Exspectatus (Mammaliaformes, Docodonta)," Journal of Vertebrate Paleontology 33(2), 382-400, (1 March 2013). https://doi.org/10.1080/02724634.2013.722575
Received: 20 March 2012; Accepted: 1 August 2012; Published: 1 March 2013
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