scholarly journals A unique predator in a unique ecosystem: modelling the apex predator within a Late Cretaceous crocodyliform‐dominated fauna from Brazil

2020 ◽  
Vol 237 (2) ◽  
pp. 323-333
Author(s):  
Felipe C. Montefeltro ◽  
Stephan Lautenschlager ◽  
Pedro L. Godoy ◽  
Gabriel S. Ferreira ◽  
Richard J. Butler
2021 ◽  
Vol 8 (9) ◽  
pp. 210923
Author(s):  
Kohei Tanaka ◽  
Otabek Ulugbek Ogli Anvarov ◽  
Darla K. Zelenitsky ◽  
Akhmadjon Shayakubovich Ahmedshaev ◽  
Yoshitsugu Kobayashi

Carcharodontosauria is a group of medium to large-sized predatory theropods, distributed worldwide during the Cretaceous. These theropods were probably the apex predators of Asiamerica in the early Late Cretaceous prior to the ascent of tyrannosaurids, although few Laurasian species are known from this time due to a poor rock record. Here, we describe Ulughbegsaurus uzbekistanensis gen. et sp. nov. from the early Late Cretaceous (Turonian) of Central Asia, which represents the first record of a Late Cretaceous carcharodontosaurian from the region. This new taxon is represented by a large, isolated maxilla from the Bissekty Formation of the Kyzylkum Desert, the Republic of Uzbekistan, a formation yielding a rich and diverse assemblage of dinosaurs and other vertebrates from fragmentary remains. Comparison of the maxilla with that of other allosauroids indicates Ulughbegsaurus was 7.5–8 m in body length and greater than 1000 kg in body mass, suggesting it was the previously unrecognized apex predator of the Bissekty ecosystem while smaller known tryannosauroids and dromaeosaurids were probable mesopredators. The discovery of Ulughbegsaurus records the geologically latest stratigraphic co-occurrence of carcharodontosaurid and tyrannosauroid dinosaurs from Laurasia, and evidence indicates carcharodontosaurians remained the dominant predators relative to tyrannosauroids, at least in Asia, as late as the Turonian.


2019 ◽  
Vol 138 (1) ◽  
pp. 1-15
Author(s):  
Luca Samperi ◽  
Kamaldeen Omosanya ◽  
Giorgio Minelli ◽  
Ståle Johansen

2020 ◽  
Vol 24 (1) ◽  
pp. 72
Author(s):  
Akihiro Misaki ◽  
Yoshihiko Okazaki ◽  
Yoshiaki Mizuno ◽  
Takeshi Matsunaga
Keyword(s):  

Palaeobotany ◽  
2013 ◽  
Vol 4 ◽  
pp. 116-147 ◽  
Author(s):  
S. V. Shczepetov ◽  
A. B. Herman

Results of comprehensive study of the Kholokhovchan floral assemblage collection is summarized. These plant fossils were collected in 1978 by E. L. Lebedev from volcanogenic deposits in Penzhina and Oklan rivers interfluve, North-Eastern Russia. This assemblage was previously known as a list of Lebedev’s preliminary identifi cations only. He had suggested that the Kholokhovchan assemblage is correlative to the latest Albian — early Turonian Grebenka flora from the Anadyr River middle reaches. However, our study demonstrates that the Kholokhovchan assemblage is most similar to the presumably the Turonian-Coniacian Arman flora of the Okhotsk-Chukotka volcanogenic belt and, therefore, should be dated as the Turonian-Coniacian or Turonian.


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