Sulcatidens

The holotype specimen, QM F18010, of Sulcatidens was discovered from the 'Wayne's Wok' site at the Riversleigh World Heritage Area, in the Boodjamulla National Park of north-western Queensland. It consists of a partial maxilla retaining teeth. In addition, an incomplete maxilla was also referred to the species. It was described alongside other agamid material from Riversleigh by Covacevich et al. in 1990.{{cite journal |last1=Covacevich |first1=J. |last2=Couper |first2=P. |last3=Molnar |first3=R. E. |last4=Witten |first4=G. |last5=Young |first5=W. |title=Miocene dragons from Riversleigh: new data on the history of the family Agamidae (Reptilia: Squamata) in Australia |journal=Memoirs of the Queensland Museum |date=1990 |volume=29 |issue=2 |pages=339–360 [349] |url=https://www.biodiversitylibrary.org/page/40654465}}

The generic name is derived from the Latin word sulcare ("to furrow"), in reference to the notches in the middle of the posterior maxillary teeth. The specific name comes from the Latin quadratus ("to make square"), which refers to the square-like shape of the posterior maxillary teeth.

The teeth of Sulcatidens, and all other agamids, are described as acrodont, as they are attached to the apex of the jaw bone. The four posterior most maxillary teeth are roughly square in appearance and situated close to one another. When viewed occlusally, the teeth have a flattened labial surface. It differs from all other agamids in that the posterior most maxillary teeth have distal edges that are notched into the mesial edge of the preceding tooth.

Sulcatidens is known exclusively from the 'Wayne's Wok' site at Riversleigh, which dates to the Early Miocene.{{Cite journal|last1=Woodhead|first1=J.|last2=Hand|first2=S.J.|last3=Archer|first3=M.|last4=Graham|first4=I.|last5=Sniderman |first5=K.| last6=Arena|first6=D.A.|last7=Black|first7=K.H.|last8=Godthelp|first8=H.|last9=Creaser|first9=P.|last10=Price|first10=E.|year=2014|title=Developing a radiometrically-dated chronologic sequence for Neogene biotic change in Australia, from the Riversleigh World Heritage Area of Queensland.|journal=Gondwana Research|volume=29|issue=1|pages=153–167|doi=10.1016/j.gr.2014.10.004| url=https://www.researchgate.net/publication/267628392|hdl=1959.4/unsworks_36975|hdl-access=free}} At the time, Riversleigh was covered in a permanently wet and closed canopy rainforest environment.{{Cite journal|last1=Travouillon|first1=K.J.|last2=Legendre|first2=S.|last3=Archer|first3=M.|last4=Hand|first4=S.J.|year=2009|title=Palaeoecological analyses of Riversleigh's Oligo-Miocene sites: Implications for Oligo-Miocene climate change in Australia.|journal=Palaeogeography, Palaeoclimatology, Palaeoecology|volume=276|issue=1–4|pages=24–37|doi=10.1016/j.palaeo.2009.02.025|bibcode=2009PPP...276...24T | url=https://www.researchgate.net/publication/233918870}}

{{reflist}}

{{Extinct squamates|I.}}

{{Taxonbar|from=Q132225027}}

Category:Agamidae

Category:Agamid lizards of Australia

Category:Prehistoric lizard genera

Category:Fossil taxa described in 1990

{{Paleo-lizard-stub}}