Matuku otagoense, Scofield & Worthy & Tennyson, 2010

Scofield, R. Paul, Worthy, Trevor H. & Tennyson, Alan J. D., 2010, A Heron (Aves: Ardeidae) from the Early Miocene St Bathans Fauna of Southern New Zealand, Records of the Australian Museum 62 (1), pp. 89-104 : 93-95

publication ID

https://doi.org/ 10.3853/j.0067-1975.62.2010.1542

publication LSID

lsid:zoobank.org:pub:D4EEDDE2-967C-401D-BB06-2859B7DD3B08

persistent identifier

https://treatment.plazi.org/id/90A23137-F402-46CB-AE7E-FB3CFBFF77EC

taxon LSID

lsid:zoobank.org:act:90A23137-F402-46CB-AE7E-FB3CFBFF77EC

treatment provided by

Felipe

scientific name

Matuku otagoense
status

sp. nov.

Matuku otagoense n.sp.

Holotype. NMNZ S.50003: Distal end, shaft and lateral proximal edge of left tarsometatarsus with fragmentary lateral cotyla and basal hypotarsus; the three trochlea are preserved but the distal foramen is obscured; the medial proximal end is missing. The bone was already fragmented in situ when discovered and has subsequently been repaired in the laboratory ( Figs 1 View Figure 1 , 2 View Figure 2 ). It was collected on 9 January 2007 during a University New South Wales, NSW, Australia / University of Adelaide , South Australia/ Canterbury Museum, Christchurch, NZ/Museum of New Zealand Te Papa Tongarewa, Wellington, NZ, expedition.

Diagnosis. As for genus.

Etymology otagoense, Latin , after Otago province in southern New Zealand, where the excavations take place; gender neuter, conforming to the gender of the generic name.

Type locality. Home Hills Station , Site HH 4, true left side Manuherikia River , Otago, New Zealand. 44° 54.472'S 169° 51.434'E. NZMS 260 H41/618843, New Zealand Fossil Record File Number H 41/f0095. The site was first exposed by river erosion between February 2005 and March 2006 GoogleMaps . Bones were recovered from the site in March 2006 and January 2007.

Stratigraphy/Age/Fauna. Bannockburn Formation, Manuherikia Group, Early Miocene (Altonian); 19–16 Ma; St Bathans Fauna. HH4 is a 5–15 cm thick clay-silt layer notable for the large number of shell fragments of the gastropod Glyptophysa . It is located 2.15–2.35 m above the top of an obvious oncolite layer and 25.63–25.83 m above base of Bannockburn Formation.

Measurements of holotype. See Table 3.

Paratypes. NMNZ S.51264. Distal end of tarsometatarsus, missing distal end of all three trochlea (HH1b Trench excavation, 15 January 2008) ; NMNZ S.50004. Cranial end of right coracoid, broken approximately half way down shaft (HH1a, 8 January 2007) ; NMNZ S.50852. Left quadrate missing entire proc. orbitalis (HH4, 8–16 January 2008) ; NMNZ S.50854. Left quadrate missing entire proc. orbitalis (HH1a, 15 January 2008) ; NMNZ S.50853. Axis with damage to caudal end of proc. caudalis (HH4, 8–16 January 2008) ; NMNZ S.51174. Tip of mandible including most of mandibular symphysis, but with damage to tip (HH1b trench excavation, 14 January 2008) .

Tarsometatarsus (NMNZ S.51264, not illustrated).

In its exterior appearance, this fragmentary element does not differ significantly in any way from NMNZ S.50003. The exceptional preservation of the distal foramen in this specimen, however, allows us to see a feature that can not be discerned in NMNZ S.50003. In NMNZ S.51264, the dorsal opening of the foramen does not open into the intertrochlear incision but is separated from it, by a thin lamella giving the foramen three openings, one dorsally, one opening to the incision and one plantarly. This feature appears to be a feature the fossil shares only with Syrigma and Botaurus amongst the ardeids examined.

Differential diagnosis of tarsometatarsi

NMNZ

Museum of New Zealand Te Papa Tongarewa

Kingdom

Animalia

Phylum

Chordata

Class

Aves

Order

Pelecaniformes

Family

Ardeidae

Genus

Matuku

Darwin Core Archive (for parent article) View in SIBiLS Plain XML RDF