In recent decades, intensive research on non-avian dinosaurs has strongly suggested that these animals were restricted to terrestrial environments1. Historical proposals that some groups, such as sauropods and hadrosaurs, lived in aquatic environments2,3 were abandoned decades ago4,5,6. It has recently been argued that at least some of the spinosaurids—an unusual group of large-bodied theropods of the Cretaceous era—were semi-aquatic7,8, but this idea has been challenged on anatomical, biomechanical and taphonomic grounds, and remains controversial9,10,11. Here we present unambiguous evidence for an aquatic propulsive structure in a dinosaur, the giant theropod Spinosaurus aegyptiacus7,12. This dinosaur has a tail with an unexpected and unique shape that consists of extremely tall neural spines and elongate chevrons, which forms a large, flexible fin-like organ capable of extensive lateral excursion. Using a robotic flapping apparatus to measure undulatory forces in physical models of different tail shapes, we show that the tail shape of Spinosaurus produces greater thrust and efficiency in water than the tail shapes of terrestrial dinosaurs and that these measures of performance are more comparable to those of extant aquatic vertebrates that use vertically expanded tails to generate forward propulsion while swimming. These results are consistent with the suite of adaptations for an aquatic lifestyle and piscivorous diet that have previously been documented for Spinosaurus7,13,14. Although developed to a lesser degree, aquatic adaptations are also found in other members of the spinosaurid clade15,16, which had a near-global distribution and a stratigraphic range of more than 50 million years14, pointing to a substantial invasion of aquatic environments by dinosaurs.
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The authors declare that all data supporting the findings of this study are available in the paper and its Supplementary Information. Three-dimensional data are available on SketchFab: flesh model at https://sketchfab.com/3d-models/07b2b6bf4c464c09bd30daa629f266ff; scanned caudal vertebrae and chevrons at https://sketchfab.com/3d-models/chv-7-ca70592e5d07408980220d639bc1456f (Chv7), https://sketchfab.com/3d-models/chv-24-d917f541a7934492aaf0be7c5b97ad40 (Chv24), https://sketchfab.com/3d-models/ca-4-56e19d32f53043369ba23d5283279eef (Ca4), https://sketchfab.com/3d-models/ca-7-c2f551b61e294138954c4f2224bd3353 (Ca7), https://sketchfab.com/3d-models/ca-12-bb2f30fec9064645b2ff99be30f1ac92 (Ca12), https://sketchfab.com/3d-models/ca-16-3cd5f6713e1f43f5bf466471416f06c8 (Ca16), https://sketchfab.com/3d-models/ca-23-f34b71eaf4e54cb29a89a0f50730e70a (Ca23), https://sketchfab.com/3d-models/ca-24-4e21ecea81c8403484b9b7e3da7bd0d6 (Ca24), https://sketchfab.com/3d-models/ca-31-6d0748a851994d6d86b84803743b75a4 (Ca31) and https://sketchfab.com/3d-models/ca-41-34e5e6415f7d4fcea335e7120b9fe9b4 (Ca41).
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We thank M. Azroal, H. Azroal, M. Fouadassi and all other expedition members from the 2015, 2018 and 2019 seasons for assistance in the field; A. A. Ha for help in preparing the fossils; the Moroccan Ministry of Mines, Energy and Sustainable Development for providing fieldwork permits; F. Manucci for helpful discussions about the flesh reconstruction of Spinosaurus; and P. Fahn-Lai for coding assistance. This research was supported by a National Geographic Society grant to N.I. (CP-143R-170), a National Geographic Emerging Explorer Grant to N.I., contributions from the Board of Advisors of the University of Detroit Mercy to N.I., a Jurassic Foundation grant to M.F., a Paleontological Society grant to M.F., an Explorers Club grant to M.F., as well as financial support from the Lokschuppen Rosenheim, the Museo di Storia Naturale di Milano, J. Pfauntsch and A. Lania.
The authors declare no competing interests.
Peer review information Nature thanks Matthew C. Lamanna, John A. Nyakatura and the other, anonymous, reviewer(s) for their contribution to the peer review of this work.
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Extended data figures and tables
a–f, Different stages of the excavation, which resulted in the removal of over 15 tons of rock using a range of tools, including picks, brushes, hammers and a jackhammer. a, 17 November 2013. b, 29 March 2015. c, 17 September 2018. d, 19 September 2018. e, 5 December 2018. f, 21 July 2019. g, h, Selected bones in situ. g, Largely complete proximal caudal vertebra (Ca4). h, Neural spine of a mid-distal caudal vertebra, fragmented by syndiagenetic cracks. Scale bars, 10 cm.
a, Largely complete distal caudal vertebra (Ca31), recovered in its entirety by digging a tunnel until the apex of the neural spine was reached. b, Semi-articulated mid-caudal vertebrae. c, Two haemal arches. d, Close association of middle caudal elements. Scale bars, 10 cm.
Detailed map of the site of discovery of FSAC-KK 11888, and fully revised skeletal reconstruction. Colours in the map and reconstruction correspond to different phases of excavation: the local discovery in 2007–2008 (red), our excavations during the 2015–2019 expeditions (green) and sieving in the debris area during the 2015–2019 expeditions (yellow). Both images are at the same scale. Scale bar, 1 m.
Photograph of the entire caudal series (numbered). Scale bar, 1 m.
Extended Data Fig. 5 Elements of FSAC-KK 11888 from 2008 (first excavation) and 2019 (most recent excavation), matched.
a–t, Evidence of the perfect match between elements collected by the local discoverer of the site in 2007–2008 (a, e, f, i, k, m, n, p, q, s) and elements excavated in situ or recovered from the site debris during the 2015–2019 excavations (b–d, g, h, j, l, o, r, t). a, b, Right and left metatarsal II. c, Left penultimate phalanx of the fourth pedal digit (IV-4) that came to light within the typical matrix in which bones of the FSAC-KK 11888 were embedded. d, e, Two possible splenial fragments reconnected. f–i, Phalanx IV-4 prepared and compared to the contralateral element of the right pes in dorsal view, and rearticulated with its ungual. j–m, Two complementary (broken) halves of the left squamosal and of a dorsal rib. n–p, s, t, Two key fragments from the debris, reconnecting the base and the shaft of a neural spine (possibly the 7th). q, r, The right astragalus (excavated in situ in July 2019) rearticulated to its tibia (from 2008). Arrows point to recomposed fractures.
Extended Data Fig. 6 Comparison of FSAC-KK 11888 caudal vertebrae to those destroyed in World War II.
Comparison between the caudal vertebrae of the neotype of S. aegyptiacus, with those of the two specimens (the holotype and a specimen known as ‘Spinosaurus B’, both of which are now lost) from the Bahariya Oasis (Egypt) described by E. Stromer12. a–d, Proximal caudal vertebra of the holotype (accession code BSP 1912 VIII 19) in distal (a) and right lateral (c) views; and of Ca4 of FSAC-KK 11888 in distal (b) and right lateral (d) views. e–j, Proximal caudal vertebra of Spinosaurus B in dorsal (e), right lateral (g) and proximal (i) views; Ca11 of FSAC-KK 11888 in dorsal (f), right lateral (h) and proximal (j) views. k–p, Middle caudal vertebra of Spinosaurus B in dorsal (k), left lateral (m) and distal (o) views; Ca21 of FSAC-KK 11888 in dorsal (l), left lateral (n) and distal (p) views. Scale bars = 10 cm.
a, b, Symmetrical pose in five views (a) and swimming pose (b).
This file contains Supplementary Text (Parts 1-9) and Figures (S1-S4) related to: Geological context; Description of new material; Evidence for single individual; Referral to Spinosaurus aegyptiacus; Photogrammetry; Whole body reconstruction; Body mass and centre of mass; Anatomical abbreviations; and References.
Raw thrust and efficiency data, including mean and standard error.
Body dimensions, body mass, body segment masses, and whole body centre of mass.
Excavation of Spinosaurus tail.
Photogrammetry of caudal vertebra.
Spinosaurus tail shape undulating in water flume from lateral perspective.
Spinosaurus tail shape undulating in water flume from ventral perspective.
Spinosaurus tail shape undulating in water flume from posterolateral perspective.
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Ibrahim, N., Maganuco, S., Dal Sasso, C. et al. Tail-propelled aquatic locomotion in a theropod dinosaur. Nature 581, 67–70 (2020). https://doi.org/10.1038/s41586-020-2190-3