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.2022 May 3;12(1):7207.
doi: 10.1038/s41598-022-11063-5.

New therizinosaurid dinosaur from the marine Osoushinai Formation (Upper Cretaceous, Japan) provides insight for function and evolution of therizinosaur claws

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New therizinosaurid dinosaur from the marine Osoushinai Formation (Upper Cretaceous, Japan) provides insight for function and evolution of therizinosaur claws

Yoshitsugu Kobayashi et al. Sci Rep..

Abstract

The record of therizinosaurs is rich in Asian countries such as Mongolia and China. Fragmentary therizinosaur specimens have been reported from the Lower and Upper Cretaceous deposits in Japan. One of these specimens, from the lower Campanian Osoushinai Formation in Nakagawa Town of Hokkaido Prefecture, was previously identified as a maniraptoran theropod dinosaur, possibly therizinosaur, but its taxonomic status remained unresolved. This study re-examines the specimen and provides a more detailed description and attempts to resolve its taxonomic status. Our study demonstrates that it is a new taxon, Paralitherizinosaurus japonicus gen. et sp. nov., because it shows a unique combination of characters in the metacarpal I and unguals. Our phylogenetic analysis places this new taxon within an unresolved clade of Therizinosauridae in the strict consensus tree. The 50% majority-rule consensus tree shows better resolution within Therizinosauridae, showing an unresolved monophyletic clade of Paralitherizinosaurus, Therizinosaurus, Suzhousaurus, and the Bissekty form. Geometric morphometric analysis suggests that Paralitherizinosaurus unguals most closely resemble Therizinosaurus unguals in being slender and has weak flexor tubercles. This study also shows an evolutionary trend in ungual shape, which associates a decrease in mechanical advantage, development of flexor tubercle, and hypothesized output (product of mechanical advantage and development of flexor tubercle) in derived therizinosaurs, supporting the hook-and-pull function of claws to bring vegetation to its mouth. Paralitherizinosaurus is the youngest therizinosaur from Japan and the first recovered from the marine deposits in Asia. This suggests a long temporal existence of therizinosaurs at the eastern edge of the Asian continent and adaptation of therizinosaurs to coastal environments.

© 2022. The Author(s).

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Conflict of interest statement

The authors declare no competing interests.

Figures

Figure 1
Figure 1
Map of Japan, showing the location of Nakagawa Town and other dinosaur localities (a). Two other names in red are locations of other therizinosaur materials. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/). A photo of the concretion containing materials ofParalitherizinosaurusjaponicus gen. et sp. nov. before preparation (b). Dark parts in the concretion are exposed bones ofParalitherizinosaurus, showing that all elements were preserved in this block. See Murakami et al. for stratigraphic column of the Oshoushinai Formation and the horizon of the specimen. Manual unguals and silhouette ofParalitherizinosaurus japonicus, showing recovered skeletal elements in white (c) (Courtesy of Genya Masukawa). Life reconstruction ofParalitherizinosaurus japonicus (d) (Courtesy of Masato Hattori).
Figure 2
Figure 2
A partial vertebra ofParalitherizinosauruss japonicus gen. et sp. nov. in anterior (a) and right lateral (b) views. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/).
Figure 3
Figure 3
Right metacarpal I ofParalitherizinosauruss japonicus gen. et sp. nov. in anterior (a), posterior (b), lateral (c), medial (d), proximal (e), and distal (f) views. (a′) to (f′) are corresponding images in black and white with labels. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/).
Figure 4
Figure 4
Right manual unguals ofParalitherizinosauruss japonicus gen. et sp. nov. Ungual of digit I in lateral (a) and medial (b) view. Ungual of digit II in proximal (c), lateral (d), medial (e), dorsal (f), and ventral (g) views. Ungual of digit III in proximal (h), lateral (i), medial (j), dorsal (k), and ventral (l) views. (a′) to (l′) are corresponding images in black and white with labels. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/).
Figure 5
Figure 5
Comparisons of manual unguals in digits I-III of therizinosaurs. An image at the lower left corner is a photo of the proximoventral end ofTherizinosaurus ungual in oblique view. Not to scale. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/).
Figure 6
Figure 6
Strict consensus tree (a) and 50% majority-rule consensus tree (b) of Therizinosauria in this study. This figure was created by using Adobe Illustrator 24.2.1 (https://www.adobe.com/).
Figure 7
Figure 7
(a) Scatter plot showing the PC1 and PC2 values obtained from the geometric morphometric analysis. The grey dots on the thin plate spline represent the “average” positions of the landmarks and the black dots represent the positions after deformation. (b) Regression plot of PC2 values obtained from the geometric morphometric analysis and the mechanical advantage of the therizinosauroid unguals. Boxplots showing the (c) mechanical advantages, (d) development of flexor tubercle, and (e) hypothesized output force among therizinosauroids. The red star represents Paralitherizinosaurus japonicus in all plots. Abbreviations: Ae: Alxasaurus elesitaiensis, B_A: Bissekty taxon A, B_B: Bissekty taxon B, Eb: Erliansaurus bellamanus, Pj: Paralitherizinosaurus japonicus, Fu: Falcarius utahensis, Jy: Jianchangosaurus yixianensis, Ls: Lingyuanosaurus sihedangensis, Mg: Martharaptor greenriverensis, Ng: Nothronychus graffami, Tc: Therizinosaurus cheloniformis. This figure was created by using Adobe Photoshop 21.2.0 and Adobe Illustrator 24.2.1 (https://www.adobe.com/).
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