Two recent articles on fossil platanistoid dolphins from New Zealand are:

Tanaka Y, Fordyce RE 2015. A new Oligo-Miocene dolphin from New Zealand: 
Otekaikea huata expands diversity of the early Platanistoidea. Palaeontologia 
electronica 18.2.23A: 1-71.  The New Zealand fossil dolphin Otekaikea huata  
(latest Oligocene to earliest Miocene, in the range 22.28 to 24.61 Ma) is here 
identified as an early new species in the clade Platanistoidea, which includes 
the endangered Ganges River dolphin (Platanista gangetica). Otekaikea huata is 
known only from the holotype, which comprises a partial skeleton from the 
marine Otekaike Limestone of the Hakataramea Valley, South Island. Otekaikea 
huata has multiple procumbent tusks passing back to otherwise near-homodont and 
polydont teeth, and an elevated face for the nasofacial muscles implicated in 
production of echolocation sounds. The skull vertex is asymmetrical and 
strongly left-skewed. Phylogenetic analyses based on morphological features 
place Otekaikea huata  in the clade Platanistoidea. The new species adds to the 
diversity of the superfamily Platanistoidea near the Oligocene-Miocene boundary.

The pdf is freely available here:
http://palaeo-electronica.org/content/2015/1161-fossil-platanistoid-dolphin


Tanaka Y, Fordyce RE 2015. Historically significant late Oligocene dolphin 
Microcetus hectori Benham 1935: a new species of Waipatia (Platanistoidea). 
Journal of the Royal Society of New Zealand: 10.1080/03036758.2015.1016046.  
The late Oligocene dolphin Microcetus hectori Benham 1935 (Otekaike Limestone, 
Duntroonian, around 25.2 million years ago) is documented, involving 
redescription of the teeth, and new description of the formerly undescribed 
skull. A separate recent phylogenetic analysis that included skull features 
indicates that M. hectori belongs in the genus Waipatia, rather than with 
Microcetus ambiguus. Waipatia hectori is readily distinguished from the older 
Waipatia maerewhenua by features that include: more robust zygomatic process of 
the squamosal; larger foramen spinosum; long and slender postorbital process; 
more inflated cheek-teeth. The two species of Waipatia form a basal clade in 
the Platanistoidea, elucidating the relationships of the hitherto monotypic 
late Oligocene genus Waipatia.

The pdf is available here
http://www.tandfonline.com/doi/full/10.1080/03036758.2015.1016046
(We have asked that the journal post a new version with less pixelated graphics)

or from Yoshi Tanaka  [email protected]
or from Ewan Fordyce  [email protected]


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