Everything about The Cretaceous totally explained
The
Cretaceous (
, usually abbreviated 'K' for its German translation "Kreide") is a
geological period, reaching from the end of the
Jurassic Period, (}} million years ago (Ma) to the beginning of the
Paleocene Period, }} Ma. It is the youngest geological period of the
Mesozoic, and at 80 million years long, the longest period of the
Phanerozoic. 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).
Dating
As with other older geologic periods, the rock beds that define the Cretaceous are well identified but the exact dates of the period's start and end are uncertain by a few million years. No great
extinction or burst of diversity separated the Cretaceous from the Jurassic. However, the end of the period is most sharply defined, being placed at an
iridium-rich layer found worldwide that's believed to be associated with the
Chicxulub impact crater in
Yucatan and the
Gulf of Mexico. This layer has been tightly dated at 65.5 Ma. This
bolide collision is probably responsible for the major, extensively-studied
Cretaceous–Tertiary extinction event.
Divisions
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:
Paleogeography
During the Cretaceous, the late
Paleozoic - early Mesozoic
supercontinent of
Pangaea completed its breakup into present day
continents, although their positions were substantially different at the time. As the
Atlantic Ocean widened, the convergent-margin
orogenies that had begun during the Jurassic continued in the
North American Cordillera, as the
Nevadan orogeny was followed by the
Sevier and
Laramide orogenies.
Though
Gondwana was still intact in the beginning of the Cretaceous, it broke up as
South America,
Antarctica and
Australia rifted away from
Africa (though
India and
Madagascar remained attached to each other); thus, the South Atlantic and
Indian Oceans were newly formed. Such active rifting lifted great undersea mountain chains along the welts, raising
eustatic sea levels worldwide. To the north of Africa the
Tethys Sea continued to narrow. Broad shallow seas advanced across central
North America (the
Western Interior Seaway) and Europe, then receded late in the period, leaving thick marine deposits sandwiched between
coal beds. At the peak of the Cretaceous
transgression, one-third of Earth's present land area was submerged.
The Cretaceous is justly famous for its
chalk; indeed, more chalk formed in the Cretaceous than in any other period in the
Phanerozoic.
Mid-ocean ridge activity — or rather, the circulation of seawater through the enlarged ridges — enriched the oceans in calcium; this made the oceans more saturated, as well as increased the bioavailability of the element for
calcareous nanoplankton. These widespread
carbonates and other
sedimentary deposits make the Cretaceous rock record especially fine. Famous
formations from North America include the rich marine fossils of
Kansas's Smoky Hill Chalk Member and the terrestrial fauna of the late Cretaceous
Hell Creek Formation. Other important Cretaceous exposures occur in
Europe (for example, the
Weald) and
China (the
Yixian Formation). In the area that's now India, massive lava beds called the
Deccan Traps were erupted in the very late Cretaceous and early Paleocene.
Climate
The
Berriasian epoch showed a cooling trend that had been seen in the last epoch of the Jurassic. There is evidence that snowfalls were common in the higher latitudes and the tropics became wetter than during the Triassic and Jurassic. Glaciation was however restricted to alpine
glaciers on some high-
latitude mountains, though seasonal snow may have existed further south.
After the end of the Berriasian, however, temperatures increased again, and these conditions were almost constant until the end of the period. This trend was due to intense
volcanic activity which produced large quantities of
carbon dioxide. The development of a number of
mantle plumes across the widening
mid-ocean ridges further pushed sea levels up, so that large areas of the continental crust were covered with shallow seas. The
Tethys Sea connecting the tropical oceans east to west also helped in warming the global climate. Warm-adapted
plant fossils are known from localities as far north as
Alaska and
Greenland, while
dinosaur fossils have been found within 15 degrees of the Cretaceous
south pole.
A very gentle
temperature gradient from the
equator to the poles meant weaker global winds, contributing to less
upwelling and more stagnant
oceans than today. This is evidenced by widespread black
shale deposition and frequent
anoxic events. Sediment cores show that tropical sea surface temperatures may have briefly been as warm as 42 °C (107 °F), 17 °C (31 °F) warmer than at present, and that they averaged around 37 °C (99 °F). Meanwhile deep ocean temperatures were as much as 15 to 20 °C (27 to 36 °F) higher than today's.
Life
Plants
Flowering plants (
angiosperms) spread during this period, although they didn't become predominant until the
Campanian stage near the end of the epoch. 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 leafy trees, including
figs,
planes and
magnolias, appeared in the Cretaceous. At the same time, some earlier Mesozoic
gymnosperms like
Conifers continued to thrive; pehuéns (Monkey Puzzle trees,
Araucaria) and other
conifers being notably plentiful and widespread, although other gymnosperm 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, akin to butterflies and moths, appeared. Aphids, grasshoppers, and gall wasps appeared.
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 didn't appear until the Miocene. The Cretaceous was also an important interval in the evolution of bioerosion, the production of borings and scrapings in rocks, hardgrounds and shells (Taylor and Wilson, 2003).
Extinction
There was a progressive decline in biodiversity during the Maastrichtian stage of the Cretaceous Period prior to the suggested ecological crisis induced by events at the K-T boundary. Furthermore, biodiversity required a substantial amount of time to recover from the K-T event, despite the probable existence of an abundance of vacant ecological niches.
Despite the severity of this boundary event, there was significant variability in the rate of extinction between and within different clades. Species which depended on photosynthesis declined or became extinct because of the reduction in solar energy reaching the earth's surface due to atmospheric particles blocking the sunlight. As is the case today, photosynthesizing organisms, such as phytoplankton and land plants, formed the primary part of the food chain in the late Cretaceous. Evidence suggests that herbivorous animals, which depended on plants and plankton as their food, died out as their food sources became scarce; consequently, top predators such as Tyrannosaurus rex also perished.
Coccolithophorids and molluscs, including ammonites, rudists, freshwater snails and mussels, as well as organisms whose food chain included these shell builders, became extinct or suffered heavy losses. For example, it's thought that ammonites were the principal food of mosasaurs, a group of giant marine reptiles that became extinct at the boundary.
Omnivores, insectivores and carrion-eaters survived the extinction event, perhaps because of the increased availability of their food sources. At the end of the Cretaceous there seem to have been no purely herbivorous or carnivorous mammals. Mammals and birds which survived the extinction fed on insects, larvae, worms, and snails, which in turn fed on dead plant and animal matter. Scientists theorise that these organisms survived the collapse of plant-based food chains because they fed on detritus.
In stream communities, few groups of animals became extinct. Stream communities rely less on food from living plants and more on detritus that washes in from land. This particular ecological niche buffered them from extinction. Similar, but more complex patterns have been found in the oceans. Extinction was more severe among animals living in the water column, than among animals living on or in the sea floor. Animals in the water column are almost entirely dependent on primary production from living phytoplankton, while animals living on or in the ocean floor feed on detritus or can switch to detritus feeding.
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