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Paleobiogeographic Evolution and Distribution of Carcharodontosauridae (Dinosauria, Theropoda) During the Middle Cretaceous of North Africa

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Paleobiogeographic Evolution and Distribution of Carcharodontosauridae (Dinosauria, Theropoda) During the Middle Cretaceous of North Africa Edinburgh Research Explorer Paleobiogeographic evolution and distribution of Carcharodontosauridae (Dinosauria, Theropoda) during the middle Cretaceous of North Africa Citation for published version: Candeiro, CRDA, Brusatte, S, Vidal, L & Pereira, PVLGDC 2018, 'Paleobiogeographic evolution and distribution of Carcharodontosauridae (Dinosauria, Theropoda) during the middle Cretaceous of North Africa', Papéis Avulsos de Zoologia, vol. 58, pp. 29. https://doi.org/10.11606/1807-0205/2018.58.29 Digital Object Identifier (DOI): 10.11606/1807-0205/2018.58.29 Link: Link to publication record in Edinburgh Research Explorer Document Version: Publisher's PDF, also known as Version of record Published In: Papéis Avulsos de Zoologia Publisher Rights Statement: This work is licensed under a Creative Commons Attribution 4.0 International License. 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Oct. 2021 Paleobiogeographic evolution and distribution of Carcharodontosauridae (Dinosauria, Theropoda) during the middle Cretaceous of North Africa Carlos Roberto dos Anjos Candeiro¹⁴; Stephen Louis Brusatte²; Luciano Vidal¹⁵ & Paulo Victor Luiz Gomes da Costa Pereira³ ¹ Universidade Federal de Goiás (UFG), Laboratório de Paleontologia e Evolução (LABPALEOEVO), Curso de Geologia. Aparecida de Goiânia, GO, Brasil. ² University of Edinburgh, Grant Institute, School of GeoSciences. Edinburgh, Scotland, UK. ORCID: 0000-0001-7525-7319. E-mail: [email protected] ³ Universidade Federal do Rio de Janeiro (UFRJ), Instituto de Geociências (IGEO), Departamento de Geologia, Laboratório de Macrofósseis. Rio de Janeiro, RJ, Brasil. ORCID: 0000-0001-5946-3251. E-mail: [email protected] ⁴ ORCID: 0000-0002-8128-4660. E-mail: [email protected] ⁵ ORCID: 0000-0001-9034-6985. E-mail: [email protected] Abstract. Over the last few decades, the systematics and evolution of carcharodontosaurids, a group of large predatory dino- saurs, from North Africa have been better understood mainly due the discovery of new species. We review this record here and discuss its importance for understanding the evolution and ecology of these dinosaurs. North Africa has one of the best records of carcharodontosaurid species. These species show dietary specializations and paleogeographic distributions similar to other top predatory theropods such as Abelisauridae and Spinosauridae. However, carcharodontosaurids have a wider distribution than other large theropods. The middle Cretaceous of North Africa was characterized by the niche overlap between large pred- ators. This evidence increases our understanding of the evolution of Carcharodontosauridae in a highly competitive region, a conjuncture rarely reported for large top predators. Key-Words. Carcharodontosauridae; Gondwana; Middle Cretaceous; North Africa; Overlap. INTRODUCTION During the Early Cretaceous (late Aptian- Cenomanian), carcharodontosaurids were di- Several species of predatory dinosaurs are verse and widespread in South American and grouped in the family Carcharodontosauridae, Africa, particularly the northern parts of Africa a subgroup of basal tetanuran allosauroid that are now covered by the Sahara Desert. These theropods closely related to the well-known Gondwanan carcharodontosaurids occupied the Allosaurus (Brusatte & Sereno, 2008; Benson same areas as two other groups of large thero- et al., 2010; Carrano et al., 2012). Some of these pods, the sail-backed spinosauroids and the short- species are among the largest theropods to ever faced and small-armed abelisauroids. Indeed, live, with Carcharodontosaurus, Giganotosaurus, fossils of these three groups are often found to- and Acrocanthosaurus approaching the famous gether (e.g., Medeiros & Schultz, 2002; Brusatte Tyrannosaurus rex in size (ca. 12 meters in to- & Sereno, 2007; Sereno & Brusatte, 2008). The tal body length, 3+ tons in mass: Benson et al., diversity of carcharodontosaurids begins to de- 2014). Carcharodontosauridae had its main evo- crease sometime during or after the Cenomanian, lutionary radiation during the Early Cretaceous and no unequivocal fossils of the group have yet in Gondwana, but also has been recorded in been found in the post-Cenomanian deposits of some areas of Laurasia (e.g., Acrocanthosaurus, Gondwana. It appears, therefore, as if carcharo- Concavenator, Shaochilong, Kelmayisaurus). This dontosaurids went extinct in Gondwana by the cosmopolitan distribution differs from the more Turonian, replaced by other large predatory di- limited distribution of some other large thero- nosaurs such as megaraptorids and abelisaurids pods, particularly tyrannosaurids, which were re- (Novas et al., 2013). They apparently persisted lon- stricted to the North America and Asia (e.g., Holtz, ger in Laurasia, as the Chinese Shaochilong dates 2004; Brusatte et al., 2010a). During the early to to the Turonian (Brusatte et al., 2009), but some- middle part of the Cretaceous, carcharodontosau- time during the early-middle Late Cretaceous they rids were among the most important large-bod- were replaced as apex predators in North America ied predatory dinosaurs globally, and were apex and Asia by tyrannosauroids (Brusatte et al., 2009, predators in many terrestrial ecosystems. 2010a; Zanno & Makovicky, 2013). Pap. Avulsos Zool., 2018; v.58: e20185829 ISSN On-Line: 1807-0205 http://doi.org/10.11606/1807-0205/2018.58.29 ISSN Printed: 0031-1049 ISNI: 0000-0004-0384-1825 www.revistas.usp.br/paz www.scielo.br/paz Pap. Avulsos Zool., 2018; v.58: e20185829 Candeiro, C.R.A. et al.: Evolution of Carcharodontosauridae from North Africa 2/8 Some of the best records of large carcharodon- According to the large-scale basal theropod phylogenet- tosaurids come from the Lower Cretaceous rocks of ic analysis of Carrano et al. (2012), carcharodontosaurids Egypt, Niger, Morocco and Tunisia, in North Africa. This are diagnosed by several characters, including a short or region underwent a complex paleogeographic history absent anterior ramus of the maxilla, hyposphenes in the during the time that carcharodontosaurids thrived, as dorsal vertebrae that are comprised of parallel sheets, it was completely severed from Europe by the middle tall neural spines in the dorsal vertebrae, and a peg-and- Cretaceous and was fragmented by high sea levels. socket articulation between the ilium and ischium. In this review we discuss the evolution and paleo- The name-bearing taxon for Carcharodontosauridae biogeography of carcharodontosaurids from the middle is the genus Carcharodontosaurus, which means “a liz- Cretaceous of North Africa, with the aim of understand- ard with shark tooth – Carcharodon”. This genus was ing the distribution and ecological role of these large named by Stromer (1931) based on a disarticulated theropods. We focus on the fossil record of the formal- skeleton found in the Cenomanian of Egypt. In naming ly described species. As considerable new material of this dinosaur, Stromer was inspired by similarities be- carcharodontosaurids has been discovered in North tween its dentition and teeth of the great Cenozoic shark Africa in recent years, this review is an attempt to summa- Carcharodon. Carcharodontosaurid teeth are relative- rize our understanding of this group as it currently stands. ly wide, laterally compressed, finely serrated, and have wrinkles on the enamel surface (e.g., Sereno et al., 1996; Brusatte et al., 2007; Hendrickx & Mateus, 2014). Characteristics In general, the North African carcharodontosau- rids were mid-to-large theropods, with estimated total Carcharodontosaurids are a subgroup of body lengths ranging from an estimate 6-8 meters in Allosauroidea, “a major clade of basal tetanuran thero- Eocarcharia (Sereno & Brusatte, 2008) to ~12 meters in pods that also includes Allosauridae (Allosaurus and Carcharodontosaurus (Sereno et al., 1996) and perhaps kin), Metriacanthosauridae (= Sinraptoridae, includ- Sauroniops (Cau et al., 2012). They and other carcharodon- ing Sinraptor and close relatives), and Neovenatoridae tosaurids had many distinctive features of the anatomy, (Neovenator and most likely the megaraptorans)” including sculptured facial bones (particularly the max- (Benson et al., 2010; Carrano et al. 2012 and references illa), thickened and fused bones of the skull roof, exten- therein) (Fig. 1). Allosauroids are mid-to-large size thero- sively fused braincases, and a heavily pneumatized post- pods diagnosed by several characters, including a large cranial skeleton (e.g., Stromer, 1931; Stovall & Langston, promaxillary fenestra in the maxilla, pneumatic nasals, 1950; Coria & Salgado, 1995; Sereno et al., 1996; Coria & lateral crests on the nasals, a large knob on the supraoc- Currie, 2002, 2006; Novas et al., 2005; Brusatte & Sereno, cipital, and L-shaped chevrons in the middle part of the 2007, 2008; Sereno & Brusatte, 2008; Brusatte et al., 2009, tail (Carrano et al., 2012). 2010b; Ortega et al., 2010; Eddy
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