A new fossil dolphin Dilophodelphis fordycei provides insight into the evolution of supraorbital crests in Platanistoidea (Mammalia, Cetacea)

Author:

Boersma Alexandra T.12ORCID,McCurry Matthew R.1345,Pyenson Nicholas D.167ORCID

Affiliation:

1. Department of Paleobiology, National Museum of Natural History, Smithsonian Institution, PO Box 37012, Washington, DC 20013, USA

2. College of Extended Education, California State University Monterey Bay, Seaside, CA 93955, USA

3. Monash Biomedicine Discovery Institute and Centre for Human Anatomy Education, Department of Anatomy and Developmental Biology, Monash University Melbourne, Victoria 3800, Australia

4. School of Biological Sciences, Monash University, Melbourne, Victoria 3800, Australia

5. Geosciences, Museums Victoria, Melbourne, Victoria 3053, Australia

6. Department of Mammalogy, Burke Museum of Natural History and Culture, Seattle, WA 98195, USA

7. Department of Paleontology, Burke Museum of Natural History and Culture, Seattle, WA 98195, USA

Abstract

Many odontocete groups have developed enlarged facial crests, although these crests differ in topography, composition and function. The most elaborate crests occur in the South Asian river dolphin ( Platanista gangetica ), in which they rise dorsally as delicate, pneumatized wings anterior of the facial bones. Their position wrapping around the melon suggests their involvement in sound propagation for echolocation. To better understand the origin of crests in this lineage, we examined facial crests among fossil and living Platanistoidea, including a new taxon, Dilophodelphis fordycei , nov. gen. and sp., described herein, from the Early Miocene Astoria Formation of Oregon, USA. We measured the physical extent and thickness of platanistoid crests, categorized their relative position and used computed tomography scans to examine their internal morphology and relative bone density. Integrating these traits in a phylogenetic context, we determined that the onset of crest elaboration or enlargement and the evolution of crest pneumatization among the platanistoids were separate events, with crest enlargement beginning in the Oligocene. However, we find no evidence for pneumatization until possibly the Early Miocene, although certainly by the Middle Miocene. Such an evolutionary context, including data from the fossil record, should inform modelling efforts that seek to understand the diversity of sound generation morphology in Odontoceti.

Funder

National Museum of Natural History, Kellogg Fund

Publisher

The Royal Society

Subject

Multidisciplinary

Reference84 articles.

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