Cretaceous Period

Cretaceous period

Cretaceous is the name given to a period of time in Earth's history (i.e., Cretaceous Period) from 145.6 to 65 million years ago. Also, all the rocks that formed during that time have the same proper name of Cretaceous (i.e., they are referred to as the Cretaceous System). Said differently, the Cretaceous System is the rock record of events that occurred—and organisms that lived—during a span of geological time that is called Cretaceous Period. Cretaceous was the third and final period of the Mesozoic Era .

Cretaceous is a name derived from the Latin word for chalk, creta. Chalk is a common type of sedimentary rock formed during this interval of Earth history. The term Cretaceous was first used in 1822 by d'Omalius d'Halloy (1707–1789), a Belgian geologist who was engaged in pioneering efforts at geological mapping of parts of France. He mapped the Terrain Cretac (Cretaceous System) within the Paris Basin and later in Belgium. D'Halloy's strata were easily correlated with chalks mapped earlier, but not formally named, by William Smith (1769–1839) on his revolutionary 1815 geological map. Other geologists of the day rapidly correlated the Cretaceous System with chalks they found in northern France, Holland, Denmark, northern Germany, Poland, and Sweden. Since their recognition and definition during the nineteenth century, Cretaceous strata have been mapped on all the world's continents.

During Cretaceous, the breakup of the supercontinent of Pangaea became nearly complete. The Atlantic Ocean opened sufficiently so that a substantial body of water existed between North America and Europe and South America and Africa were widely separated. While the Atlantic was opening, the Pacific Ocean continued to close rapidly and an episode of major tectonic change occurred as a result in western North and South America. Specifically, a major subduction zone developed along the western coast of the Americas and substantial tectonic uplift and volcanic activity occurred along this western margin.

During most of Cretaceous, global sea levels were at some of their highest elevations in the last 500 million years of Earth history. Much of the low-lying areas of the world's continents were covered by shallow seas , also known as epicontinental seas. During part of Late Cretaceous, sea level was so high (approximately 275 m above present level) that an epicontinental sea (i.e., Western Interior Seaway) connected the Gulf of Mexico with the Arctic Ocean through the center of North America. (The Rocky Mountains were not formed at this time, and thus this area was rather low-lying and flat).

Cretaceous was a time of elevated global temperatures and there were essentially no polar or high-altitude glaciers . This contributed to elevated sea levels as did the vast development of volcanic activity along Earth's mid-ocean ridges . Such volcanic activity and accompanying swelling of these undersea ridges displaced a considerable volume of seawater (strongly exacerbating sea-level rise). Also, there was rapid sea-floor spreading during Cretaceous. Further, effusive volcanism from mantle hot spots caused flood basalts to erupt on land, the most noteworthy of these produced the massive Deccan Traps of India.

Cretaceous life in the oceans was very plentiful, with numerous species of fish, sharks, rays, ammonites, turtles, mosasaurs, plesiosaurs, and other creatures plying ocean waters. Numerous massive reef systems developed, including one rimming the Gulf of Mexico during Early Cretaceous, which was dominated by a specialized type of large clams called rudists. Large oysters were common at this time. The main plankon, the golden-brown alga, produced massive amounts of calcareous platelets that settled to the sea floor along with abundant foraminifers thus forming an ooze that eventually became the famous Cretaceous chalk (as seen at the White Cliffs of Dover, England, and many other areas).

Cretaceous life on land was dominated by the reptiles, which dwelt for the most part in heavily vegetated terrains. Lush Cretaceous cycad-ginko-conifer forests and swamps are well preserved in vast tracts of coal and lignite deposits of this age. Late Cretaceous was the time of development of flowing plants and co-evolution of a very diverse insect population. Land animals such as snakes, lizards, crocodiles, dinosaurs, pterosaurs, birds, and small mammals were common. Among the dinosaurs, Cretaceous ecosystems saw the rise of many diverse types, which were indigenous to the rapidly separating continental land masses. The rising groups of dinosaurs during this time included pachycephalosarus, ceratopsians, iguanodonts, hadrosaurs, coelurosaurs, and carnosaurs (e.g., tyrannosaurids).

The end of Cretaceous came abruptly with global ecosystem collapse and mass extinction. The end-Cretaceous catastrophe resulted in rapid death of nearly 50% of all living species of organisms. Known since the nineteenth century as an inexplicable sudden mass death marker, the Cretaceous-Tertiary (K-T) boundary has attracted considerable interest from researchers in recent years because the boundary clay layer contains a substantial enrichment in certain chemical elements (e.g., iridium), which are much more common in asteroids and comets than on Earth. Discovery in the 1980s of a 180-km diameter impact crater in the state of Yucatan, Mexico, which has the same age as the K-T boundary, indicates a strong connection between the mass death and cosmic impact at this time in Earth history. Subsequent studies have shown that impact of a 10-km diameter asteroid at Yucatan could have resulted in such a global ecosystem collapse and accompanying mass death. The impact crater is known as Chicxulub, which is a Mayan word meaning "tail of the Devil."

See also Chronostratigraphy; K-T event; Impact crater; Mesozoic Era; Stratigraphy; Supercontinents