occurrenceID	taxonID	catalogNumber	collectionCode	institutionCode	typeStatus	verbatimLabel	sex	individualCount	eventDate	recordedBy	recordNumber	decimalLatitude	decimalLongitude	minimumElevationInMeters	maximumElevationInMeters	minimumDepthInMeters	maximumDepthInMeters	country	stateProvince	municipality	locality	references	associatedOccurrences	associatedReferences	associatedSequences	basisOfRecord
03F9879B325DFF97FF03FDE5FC4D7B3C.mc.3B383CD0325DFF9EFCEEFF6BFBCF7E3B	03F9879B325DFF97FF03FDE5FC4D7B3C.taxon	R1148, R1629, R1632, R811, R604		NHMUK	holotype	The holotype NHMUK R 1148 includes specimens allocated with the registered numbers R 1629 and R 1632, which were collected from the same quarry. As evidence of association, some specimens, for example the metatarsals of the left pes (MtIII: NHMUK R 1148 and MtII: NHMUK R 1629) fit together perfectly (Fig. 11 A – H). Additional material assigned to registered numbers NHMUK R 811, R 811 a, b (including sacral and pelvic bones) as well as NHMUK R 604 (cervical, dorsal, and caudal vertebrae, some imperfectly preserved ribs, and some broken tooth fragments) were also collected from this quarry and are, if not part of the type series, commensurate, and show the same preservational characteristics and almost no duplication of elements. It must be noted, however, that an ischial shaft fragment of NHMUK R 1629 (Fig. 17) duplicates one of the two ischia associated with NHMUK R 811 (Fig. 31 B). This ischium fragment alone suggests that two commensurate and osteologically identical ornithopod skeletons must have been collected from a site that Dawson recorded as the same locality		1														https://treatment.plazi.org/id/03F9879B325DFF97FF03FDE5FC4D7B3C#3B383CD0325DFF9EFCEEFF6BFBCF7E3B				MaterialCitation
03F9879B3254FF90FC71F912FCC67A0A.mc.3B383CD03251FF92FF01FB7BFD0A7B1F	03F9879B3254FF90FC71F912FCC67A0A.taxon	R1148		NHMUK	holotype	The seventh / eighth (d 7 / 8) and ninth / tenth (d 9 / 10) dorsals (Fig. 23) have centra of a more rectangular outline and smaller, more rounded parapophyses (par) compared with previous examples. The parapophysis (par) can also be seen to commence its lateral migration along the transverse process. These centra have a narrow keel and have shallowly concave articular surfaces [and the seventh / eighth example (Fig. 23 A) is most similar to the dorsals of the holotype NHMUK R 1148: Fig. 12]. Judged by their shape these centra (particularly d 7 / 8) resemble ‘ keystones’ at the centre of the span of an arched dorsal series. Centrum (d 9 / 10 – Fig. 23 B) leans more posteriorly and has rather thicker and more prominent articular margins		1											Centre		Judged	https://treatment.plazi.org/id/03F9879B3254FF90FC71F912FCC67A0A#3B383CD03251FF92FF01FB7BFD0A7B1F				MaterialCitation
03F9879B3275FFB6FCF7FEFFFA857B8C.mc.3B383CD03275FFB6FC87FED5FB857C8F	03F9879B3275FFB6FCF7FEFFFA857B8C.taxon					This taxon is based upon a partial associated skeleton collected at Galve in the Province of Teruel in the Autonomous region of Aragon (Camarillas Formation: lower Barremian)		1											Aragon	Autonomous region	lower Barremian	https://treatment.plazi.org/id/03F9879B3275FFB6FCF7FEFFFA857B8C#3B383CD03275FFB6FC87FED5FB857C8F				MaterialCitation
03F9879B3275FFB6FF54FC7EFBE67C7D.mc.3B383CD03275FFB6FF19FBB4FD9579CF	03F9879B3275FFB6FF54FC7EFBE67C7D.taxon					This taxon is based upon a disarticulated partial skull and an isolated sternal plate of a comparatively small (∼ 4 m long) ornithopod collected from Kitadani Quarry, Fukui Prefecture, Japan. The geological age of the material is late Hauterivian−Barremian		1						4				Japan	Fukui	The	Kitadani Quarry	https://treatment.plazi.org/id/03F9879B3275FFB6FF54FC7EFBE67C7D#3B383CD03275FFB6FF19FBB4FD9579CF				MaterialCitation
03F9879B3274FFB4FCD2FD52FE637E67.mc.3B383CD03274FFB7FC9BFCE9FB667ED3	03F9879B3274FFB4FCD2FD52FE637E67.taxon					This taxon was recovered from the Lakota Formation (Barremian) of Lawrence County, South Dakota and comprises a major portion of an articulated skull of a large (∼ 8 m long) ornithopod		1						8					South Dakota	This	Lakota Formation	https://treatment.plazi.org/id/03F9879B3274FFB4FCD2FD52FE637E67#3B383CD03274FFB7FC9BFCE9FB667ED3				MaterialCitation
03F9879B320CFFCFFF75FDC9FC4B7884.mc.3B383CD0320CFFCFFEB8FD04FEA77E3D	03F9879B320CFFCFFF75FDC9FC4B7884.taxon					is represented by several partial skulls and postcranial material collected from the Mussentuchit Member of the Cedar Mountain Formation (lower Cenomanian) of eastern Utah, USA (Hunt et al., 2011). The material indicates a medium−large-sized ornithopod (∼ 7 – 8 m in length)		1						8				United States of America	Utah	lower Cenomanian	Mussentuchit Member	https://treatment.plazi.org/id/03F9879B320CFFCFFF75FDC9FC4B7884#3B383CD0320CFFCFFEB8FD04FEA77E3D				MaterialCitation
