Hypuronector, COLBERT & OLSEN, 2001

COLBERT, EDWIN H. & OLSEN, PAUL E., 2001, A New and Unusual Aquatic Reptile from the Lockatong Formation of New Jersey (Late Triassic, Newark Supergroup), American Museum Novitates 3334, pp. 1-24 : 9-11

publication ID

https://doi.org/ 10.1206/0003-0082(2001)334<0001:ANAUAR>2.0.CO;2

persistent identifier

https://treatment.plazi.org/id/038B87DE-FF8E-FFAA-0876-BC1BFECF6073

treatment provided by

Carolina

scientific name

Hypuronector
status

gen. nov.

Hypuronector , new genus

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TYPE AND ONLY SPECIES: Hypuronector limnaios , new species

ETYMOLOGY: From the Greek ηψπo (hypo), deep; υpo (uro), tail; νeĸTop, (nektor), the swimmer, meaning the ‘‘deep tailed swimmer’’, the new reptile’s informal name for more than 20 years. Name suggested by Donald Baird.

DIAGNOSIS: Small (<18 cm) drepanosaurid with uniquely deep tail consisting of extremely elongated chevrons or hemal spines and proximally high neural spines; the longest hemal spine being equivalent in length to 11 articulated caudal vertebrae. Limbs long and slender; humerus equal to femur in length, radius and ulna about two­thirds length of humerus and longer than tibia and fibula. Differs from Megalancosaurus in having notochordal centra and a distally edentulous lower jaw and lacking the peculiarly enlarged anterior dorsal neural spines. Differs from Dolabrosaurus and Megalancosaurus in lacking the distally expanded tips of the neural spines. Differs from Megalancosaurus in having amphicoelous rath­ er than procoelous vertebrae. Differs from Drepanosaurus in showing greater fusion of the ribs to the centra, lacking the extreme enlargement of the ungual phalanx digit II of the manus and the greatly broadened ulna, and lacking the ‘‘spine’’ on the tip of the tail. Differs from both Drepanosaurus and Megalancosaurus in lacking massively enlarged neural spines in the shoulder region and the fenestrate or bifurcate proximal chevrons.

Hypuronector limnaios , new species

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HOLOTYPE: AMNH 7759 About AMNH , a partially articulated skeleton lacking the skull (fig. 6). Most vertebrae, present including 11 presacrals, two possible sacrals and 38 caudals in close articulation, numerous ribs, shoulder girdle, forelimbs, pelvis, both femora, left tibia and fibula, distal ends of right tibia and fibula. Both pedes and manus incomplete. The holotype was prepared by the air abrasive technique.

ETYMOLOGY: Greek λιμναιoơ (limnaios), of the lake, referring to the lacustrine environment in which the animal lived.

REFERRED MATERIAL: From the Granton Quarry: AMNH, 1721, anterior thoracic region including pectoral girdle; AMNH 7205, 5 presacral ribs, fragments of a pelvis, and 13 anterior caudal vertebrae; AMNH 7755, 3 cervical vertebrae, AMNH 1998, 7 caudal vertebrae; AMNH 2080, a dentary with 7 teeth; AMNH 2076, vertebrae; NJSM 19701, partial mostly articulated posterior trunk and anterior tail; NJSM 19702, proximal caudal vertebra and chevron. From Weehawken: YPM 8641, proximal caudal vertebra and chevron; YPM 56385, limb bone; YPM 56386, distal end of humerus; YPM 56387, caudal vertebrae with chevron and?humerus; YPM 56388, left mandible; YPM 56389, caudal vertebra and partial chevron; YPM 56390, three associated caudal vertebrae with chevrons; YPM 56391, obliquely preserved caudal vertebra and partial chevron; YPM 56392, isolated sacral vertebra; YPM 56393, isolated forelimb. All of the Granton material has been prepared by air abrasion or left unprepared, while all of the Weehawken material has been negatively prepared with hydrochloric acid.

HORIZON AND LOCALITY: Lockatong Formation of the Newark basin portion of the Newark Supergroup , Late Triassic. The ho­ lotype is from the Granton Quarry , North Bergen , New Jersey,? Ewing Creek Member , cycle ‘‘G7’’. Other referred specimens from the Granton Quarry are also from the Ewing Creek Member. Those from Weehawken , New Jersey, are from cycle W­5 of the Nursery Member .

DIAGNOSIS: As for genus, which has only one known species.

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