Nipponosaurus

History of study

The holotype (UHR 6590, University of Hokkaidō Registration) was discovered in November 1934 during the construction of a hospital for the Kawakami colliery of the Mitsui Mining Company on Karafuto Prefecture (now Sinegorsk, Sakhalin, Russia). It was disarticulated when discovered. N. sachalinensis was named and described in 1936 by Professor Takumi Nagao of the Imperial University of Hokkaido. The generic name refers to Nippon, the Japanese name of Japan; it was the first dinosaur named based on a find made on Japanese territory – though South Sakhalin was annexed by the Soviet Union in 1945. The specific name refers to Sakhalin.

Although being relatively complete at the time of discovery, the specimen was missing much of the skull and limbs. A second expedition was organised in the summer of 1937, in which limb material pertaining to the holotype was recovered. The next year, Nagao authored a second article on the species describing these additional remains.

Nipponosaurus was described as a member of the Trachodontidae; however Trachodon is now considered an invalid nomen dubium. The family is now known as the Hadrosauridae. Among its relatives, Nagao thought it was possibly closest to the taxa Cheneosaurus and Tetragonosaurus, even suggesting that his species might later prove to be congeneric with one of them.

For the remainder of the 20th century, the taxon was scarcely mentioned. after this it was rarely assigned past the Lambeosaurinae. A humerus from a pit near Hashima Island, Japan was assigned to Nipponosaurus, variously referred to as Trachodon, in 1967. No further studies have acknowledged the specimen, and the referral has been ignored, with the species still considered to be represented by a single specimen. Later in 1989, a study noted that features of its metacarpals could indicate a basal position within the Hadrosauridae. Near the turn of the century, in 1994, a review of Japanese dinosaurs noted the incomplete nature of many Asian hadrosaurs could mean some of them, including Nipponosaurus, may in fact be representatives of the same species.

More extensive research has been conducted in the 21st century. In 2004, the species was redescribed, with focus on its growth stage. They concluded it was a valid taxon, and that the holotype was immature. More recently, a 2017 study provided further descriptions of the specimen, and conducted a microscopic examination on sections of the left femur, a rib, and an isolated chevron, which re-affirmed the age of the holotype.

Description

The immature holotype specimen measures roughly 4 m in length. When it was originally described, it was considered to be an adult, because of its co-ossified sacral vertebra. Future authors doubted this, merely citing its small size. In the 2004 redescription, it was examined more closely and several characteristics were found that identified it as an juvenile individual. Later, in 2017, another team re-evaluated the specimen, and determined through investigating the fossils at a microscopic level (in a process called histology) that this was correct, although they doubted the significance of some of the characters identified in the former study.

Though the quality of bone preservation is generally poor, the holotype skeleton is estimated to be 60% complete. It consists of a left maxilla and dentary, parietal, various isolated skull elements, thirteen cervical vertebrae, six dorsal vertebrae, two sacral vertebrae, a series of 35 caudal vertebrae, a left scapula, lower portions of both humeri, most elements of the lower forelimbs, an ischium, left ilium, and most of the hindlimbs.

Classification

Some authors have deemed the species a nomen dubium, questioning its supposed diagnostic characteristics, especially in light of its presumed immature status. The validity of the taxon has therefore been controversial. The 2004 redescription denied this, proposing three diagnostic characters. Later, a 2017 study once again questioned the validity of the proposed diagnostic characters; however, upon a re-examination of the specimen, three new ones were put forward.

A cladistic analysis in 2004 placed Nipponosaurus sachalinensis very close to the well-known North American Hypacrosaurus altispinus within the Lambeosaurinae. They suggested it might be congeneric with the species, but because of the incomplete nature of the holotype and the questionable monophyly of the genus Hypacrosaurus, they refrained from reassigning it. The left cladogram was recovered in the 2004 study, and the right cladogram was recovered by the 2007 study:

More recently, another analysis, accounting for characters that vary through ontogeny, instead found it to be closely related to the European taxa Arenysaurus and Blasisaurus, outside of Lambeosaurini, unlike the earlier studies. Its position outside of the clade containing Parasaurolophini and Lambeosaurini was supported by the absence of two synapomorphies of the group in its teeth. Four characters united it with Arenysaurus and Blasisaurus; the end margin of the coronoid process overlapping with the back portion of the dental battery (which was suggested to perhaps reflect a difference in feeding habits from other taxa), a short edentulous slope, and two characters of the jugal. The following cladogram was recovered in their analysis:

Palaeoecology

The specimen was collected from Upper Yezo Group, which was known as the Upper Ammonites Bed at the time of the original description. Because the area where it was discovered no longer belongs to Japan, follow up research has become difficult. Additionally, field notes from the time of discovery have been lost. This has made determining the age of the horizon problematic. However, Nagao noted fossil molluscs now called Parapuzosia japonica and Sphenoceramus schmidti were also found at the locality, and these are known to hail from the lower Campanian. An age from the upper Santonian or lower Campanian is therefore likely.

Based on the sediments it was preserved in, the Nipponosaurus specimen is thought to have been buried in a marine setting. However, this would not have been far from the shore, as indicated by the relatively complete nature of the specimen and the presence of fossilised terrestrial plants found alongside it. This indicates the species may have lived primarily on low-lying plains near the coast, a lifestyle consistent with some of its North American relatives.

References

References

1. Nagao, Takumi. (1936). "''Nipponosaurus sachalinensis'' – A new genus and species of trachodont dinosaur from Japanese Saghalien". Journal of the Faculty of Science, Hokkaido Imperial University. Ser. 4, Geology and Mineralogy.
2. Takasaki, Ryuji. (2017). "Reanalysis of the phylogenetic status of ''Nipponosaurus sachalinensis'' (Ornithopoda: Dinosauria) from the Late Cretaceous of Southern Sakhalin". Historical Biology.
3. (2004). "''Nippponosaurus sachalinensis'' (Dinosauria; Ornithopoda): anatomy and systematic position within Hadrosauridae". Journal of Vertebrate Paleontology.
4. (1994). "Dinosaurs and sedimentary environments in the Japanese Cretaceous: a contribution to dinosaur facies in Asia based on molluscan palaeontology and stratigraphy". Cretaceous Research.
5. Nagao, Takumi. (1938). "On the limb-bones of ''Nipponosaurus sachalinensis'' Nagao, a Japanese hadrosaurian dinosaur.". 日本動物学彙報.
6. Creisler, B.S. (2007). Deciphering duckbills. in: K. Carpenter (ed.), ''Horns and Beaks: Ceratopsian and Ornithopod Dinosaurs''. Indiana University Press: Bloomington and Indianapolis, 185–210. {{ISBN. 0-253-34817-X
7. Dodson, Peter. (1975). "Taxonomic implications of relative growth in lambeosaurine dinosaurs". Systematic Zoology.
8. Rozhdestvensky, A. K.. (1968). "Hadrosaurs of Kazakhstan.". Upper Paleozoic and Mesozoic Amphibians and Reptiles. Moscow: Akademia Nauk SSSR.
9. Matsuo, Hidekuni. (1967). "A Cretaceous ''Salvinia'' from the Hashima-Is.(Gunkan-Jima), outside Nagasaki Harbour, West Kyushu, Japan". Transactions and Proceedings of the Paleontological Society of Japan..