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
3B4E17461B12FFAEFCE5FB7AFEE8F9E1.mc.038FAC0D1B1FFFB6FF5FFE01FD23FDE1	3B4E17461B12FFAEFCE5FB7AFEE8F9E1.taxon	T 3925		PIMUZ	holotype	PIMUZ T 3925, a sub-complete specimen of 180 mm long preserved as part and counterpart; Point 902 / Mirigioli, Meride (Canton Ticino, Switzerland); bed unknown, upper Besano Formation, E. curionii Ammonoid Zone, earliest Ladinian (Middle Triassic).		1										Switzerland	Ticino	Ladinian	Point	https://treatment.plazi.org/id/3B4E17461B12FFAEFCE5FB7AFEE8F9E1#038FAC0D1B1FFFB6FF5FFE01FD23FDE1				MaterialCitation
3B4E17461B12FFAEFCE5FB7AFEE8F9E1.mc.038FAC0D1B1BFFB2FCE5F99EFBD0F8A9	3B4E17461B12FFAEFCE5FB7AFEE8F9E1.taxon	T 3925, T 978		PIMUZ	holotype	Te lower jaw of the holotype of T. peyeri (PIMUZ T 3925) is much better preserved in its anterior part than in its posterior part (Figs 4, 5 and 9 A). On PIMUZ T 978, we identified a bone as an isolated retroarticular (Fig. 9 B, C). It is rectangular with a rounded posterior margin and bears a long surface that is interpreted as the facet of articulation for the quadrate		1														https://treatment.plazi.org/id/3B4E17461B12FFAEFCE5FB7AFEE8F9E1#038FAC0D1B1BFFB2FCE5F99EFBD0F8A9				MaterialCitation
