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Spinosaurus is known to have eaten fish and small to medium terrestrial prey as well. [5] Evidence suggests that it was semiaquatic; how capable it was of swimming has been strongly contested. Spinosaurus's leg bones had osteosclerosis (high bone density), allowing for better buoyancy control.
Juvenile spinosaurid fossils are somewhat rare. However, an ungual phalanx measuring 21 mm (0.83 in) belonging to a very young Spinosaurus indicates that Spinosaurus, and probably by extent other spinosaurids, may have developed their semiaquatic adaptations at birth or at a very young age and maintained the adaptations throughout their lives ...
The culture that has been connected with the wave of extinctions in North America is the paleo-American culture associated with the Clovis people (q.v.), who were thought to use spear throwers to kill large animals. The chief criticism of the "prehistoric overkill hypothesis" has been that the human population at the time was too small and/or ...
c. 106 Ma – Spinosaurus evolves. c. 100.5 Ma - Stegosaurs go extinct; c. 100 Ma – First bees. c. 94 Ma - First mosasaurs. [36] c. 93 Ma - Cenomanian-Turonian boundary event causes the extinction of ichthyosaurs and pliosaurs. [37] c. 90 Ma – the Indian subcontinent splits from Gondwana, becoming an island continent. Snakes and ticks evolve.
explain why particular groups of organisms died out and why others survived; provide mechanisms that are strong enough to cause a mass extinction but not a total extinction; be based on events or processes that can be shown to have happened, not just inferred from the extinction. It may be necessary to consider combinations of causes.
However, pinpointing the extinction of these different land reptile groups is difficult, as the last stage of the Triassic, the Rhaetian, and the first stage of the Jurassic, the Hettangian, each have few records of large land animals; some paleontologists have considered only phytosaurs and procolophonids to have become extinct at the Triassic ...
The author, Steve Brussatte, is a paleontologist at the University of Edinburgh. [1] A review in The Times described him as "a man who ranks as one of the leading experts in his field: a palaeontologist who seems to have studied with all the greats and to have dug up fossils everywhere that matters."
The Cambrian explosion (also known as Cambrian radiation [1] or Cambrian diversification) is an interval of time beginning approximately in the Cambrian period of the early Paleozoic, when a sudden radiation of complex life occurred and practically all major animal phyla started appearing in the fossil record.