Cretaceous
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Cretaceous
The Cretaceous is usually separated into Early and Late Cretaceous Epochs. The faunal stages from youngest to oldest are listed below; time is referred to as early or late, and the corresponding rocks are referred to as lower or upper: Upper/Late Cretaceous
Maastrichtian (70.6 ± 0.6 – 65.8 ± 0.3 Mya)
Campanian (83.5 ± 0.7 – 70.6 ± 0.6 Mya)
Santonian (85.8 ± 0.7 – 83.5 ± 0.7 Mya)
Coniacian (89.3 ± 1.0 – 85.8 ± 0.7 Mya)
Turonian (93.5 ± 0.8 – 89.3 ± 1.0 Mya)
Cenomanian (99.6 ± 0.9 – 93.5 ± 0.8 Mya)
Lower/Early Cretaceous
Albian (112.0 ± 1.0 – 99.6 ± 0.9 Mya)
Aptian (125.0 ± 1.0 – 112.0 ± 1.0 Mya)
Barremian (130.0 ± 1.5 – 125.0 ± 1.0 Mya)
Hauterivian (136.4 ± 2.0 – 130.0 ± 1.5 Mya)
Valanginian (140.2 ± 3.0 – 136.4 ± 2.0 Mya)
Berriasian (145.5 ± 4.0 – 140.2 ± 3.0 Mya)
The Cretaceous Period is one of the major divisions of the geologic timescale, reaching from the end of the Jurassic Period (i.e. from 145.5 ± 4.0 million years ago (Mya)) to the beginning of the Paleocene epoch of the Tertiary Period (about 65.5 ± 0.3 Myaa). As the longest geological period, the Cretaceous constitutes nearly half of the Mesozoic. The end of the Cretaceous defines the boundary between the Mesozoic and Cenozoic eras.
The Cretaceous (from Latin creta meaning 'chalk') as a separate period was first defined by a Belgian geologist Jean d'Omalius d'Halloy in 1822, using strata in the Paris Basin and named for the extensive beds of chalk (calcium carbonate deposited by the shells of marine invertebrates, principally coccoliths), found in the upper Cretaceous of continental Europe and the British Isles (including the White Cliffs of Dover).
Plants
Monkey Puzzle Trees, flowering plants, also known as angiosperms, spread during this period, although they did not become predominant until near the end of the period (Campanian age). Their evolution was aided by the appearance of bees; in fact angiosperms and insects are a good example of coevolution. The first representatives of many modern trees, including figs, planes and magnolias, appeared in the Cretaceous. At the same time, some earlier Mesozoic gymnosperms, like Conifers continued to thrive, although other taxa like Bennettitales died out before the end of the period.
Terrestrial fauna
On land, mammals were a small and still relatively minor component of the fauna. The fauna was dominated by archosaurian reptiles, especially dinosaurs, which were at their most diverse. Pterosaurs were common in the early and middle Cretaceous, but as the Cretaceous proceeded they faced growing competition from the adaptive radiation of birds, and by the end of the period only two highly specialised families remained.
The Liaoning lagerstätte (Chaomidianzi formation) in China provides a glimpse of life in the Early Cretaceous, where preserved remains of numerous types of small dinosaurs, birds, and mammals have been found. The coelurosaur dinosaurs found there represent types of the group maniraptora, which is transitional between dinosaurs and birds, and are notable for the presence of hair-like feathers.
During the Cretaceous, insects began to diversify, and the oldest known ants, termites and some lepidopterans appeared. Aphids, grasshoppers, and gall wasps appeared. Numerous exceptionally preserved insects have been found in the Lower Cretaceous Siberian lagerstätte of Baissa.
Marine fauna
In the seas, rays, modern sharks and teleosts became common. Marine reptiles included ichthyosaurs in the early and middle of the Cretaceous, plesiosaurs throughout the entire period, and mosasaurs in the Late Cretaceous.
Baculites, a genus of straight-shelled form of ammonite, flourished in the seas. The Hesperornithiformes were flightless, marine diving birds that swam like grebes. Globotruncanid Foraminifera and echinoderms such as sea urchins and starfish (sea stars) thrived. The first radiation of the diatoms (generally siliceous, rather than calcareous) in the oceans occurred during the Cretaceous; freshwater diatoms did not appear until the Miocene. The Cretaceous was also an important interval in the evolution of bioerosion, the production of borings and scrapings in rocks and shells (Taylor and Wilson, 2003).
Extinction
In the extinction event that defines the end of the Cretaceous, a significant number of species (~50%) and known families (~25%) disappeared. Plants were nearly unscathed, while marine organisms were hit the hardest. These include a large number (~95%) of types of planktic foraminifers (excepting the Globigerinida), an even larger number of Coccolithophores, all the ammonite and belemnite cephalopods, and all reef-forming rudist molluscs and inoceramid clams), as well as all marine reptiles except turtles and crocodiles. Dinosaurs are the most famous victims of the Cretaceous extinction. Dinosaurs that were unique to the very end of the period (such as Tyrannosaurus rex, Triceratops, and Ankylosaurus) were wiped out. The last of the pterosaurs became extinct and the vast majority of birds did as well, including the Enantiornithes and Hesperornithiformes.
The intensive mid-Cretaceous insect extinction began during the Albian.
http://www.palaeos.com/Mesozoic/Cretaceous/Cretaceous.htm