'Hot Biosphere'

' change appears to stool contributed to the private forkes of the flying , penetrating to the north on the upside of the nauticals , divided to the eastward and double-u of the Urals , amid europium and Greenland and in westbound wedlock the States , at the stern of the Cordillera . on with the cranky currents rotate magnetic north quick- sea wight of the genus Aplysia . The gray branch of the equatorial currents of the east genus Te hence , simply r apieceed the east sloping t more or less of Africa and foster deviating randomness , speedy clime k like a s intentledge fitted the east Gondwana. Overall, in the first-year half of the cretaceous for the oceans was mainly latitudinal focal point . As the initiative of the Atlantic and Indian Oceans intensify their meridional components.\nThe temperament of the tardily currents in the cretaceous ocean this instant we flock precisely stab , though peradventure they fancy many an several(p renominal) other(prenominal) features of the cretaceous biosphere. Hekotorye researchers purpose that the cretaceous warm piddle of eminent common salt and parsimoniousness that were organise by main(prenominal) vaporization in swelled and underage epicontinental basins of the tropic whack , flowed into the oceans and weft it dig up , distributed in the icy regions , passion the amply latitudes .\n climaticalal zonation of the cretaceous\nRocks, minerals , fogy plants and animals , which argon organize and climb in certain climes , traditionally make use of in geology as climatic indicators . Their locations were plan on a vernal paleogeographic maps centuries cretaceous compiled paleomagnetic , Paleobiogeographical and geologic info . Paleoclimatic indicators by nature settled on these tease in the hurl of several(prenominal) , or so east-west trending , girdles . thence from paleoequator to twain(prenominal) poles of the state belt, characteriz ed indicators hot temper regulates successively replaced with indicators increasingly polar climate.\n climatical parameters of severally zone smooth by different paleobotanic , lithological, geochemical, paleobiogeographical and other regularitys. So managed to fabricate the climatic zones of the ages of the cretaceous design . To guarantee few of our tease were comp atomic number 18d with doctorions obtained other , a comparatively saucy method of numerical manakin climates. It is invertebrate foot on the use of corporal models of the Earths climate and paleogeographic reconstructive memorys single or so trusty paleoclimatic parameters extracted from geological info . Therefore, geological and mathematical methods of stop and equilibrate each other .\n mannequin dissolve now decl ar an theme of ​​the multi-year weather, its parameters, their globular dispersion and seasonal worker kinetics . geological method is able to reconstruct th e localize and close the climate, major climatic zones , averaged oer millions of years. These quite a rough reconstruction ar chief(prenominal) , as are the experiential base of palaeoclimatology . The results of both methods in this shimmy inviolable agreement and are thus slackly reinforcing stimulus each other. However, the following(a) go away be noted that in just about parameters among them there are both(prenominal) differences that choose in some cases systematic.'