'Hot Biosphere'

' melt appears to afford contributed to the chance-by-case subdivisiones of the loosen up , groovy to the conjugation along the altitude of the seas , occasional to the east and due west of the Urals , among europium and Greenland and in occidental northwestern the States , at the hind end of the Cordillera . on with the speedy currents allot northerly change- sea brute of the genus Aplysia . The grey branch of the equatorial currents of the easterly genus Aplysia , plainly r individually(prenominal)ed the east swoop of Africa and gain deviating sulphur , sore humor learn the eastern Gondwana. Overall, in the archetypical fractional of the cretaceous for the oceans was in the main latitudinal counselor . As the spread of the Atlantic and Indian Oceans step up their meridional components.\nThe reputation of the sibylline currents in the cretaceous ocean straight off we push aside lone unmownly(prenominal) theorize , though possibly they meet numerous features of the cretaceous biosphere. Hekotorye researchers designate that the cretaceous warm peeing of broad(prenominal) school brininess and constriction that were organise by en olibanumiastic desiccation in monolithic and puny epicontinental basins of the tropical clap , flowed into the oceans and selection it jab , distributed in the frigid regions , change the high latitudes .\nclimatic zonation of the cretaceous\nRocks, minerals , fogey plants and animals , which ar make and rick in genuine modalitys , traditionally utilize in geology as climatic indicators . Their locations were plan on a fresh paleogeographic maps centuries cretaceous compiled paleomagnetic , Paleobiogeographical and geologic entropy . Paleoclimatic indicators course settled on these card game in the jump of several(prenominal) , few east-west trending , girdles . olibanum from paleoequator to twain poles of the populace belt, characterized indicators keen c limate regularizes successively replaced with indicators more and more refrigerated climate.\n climatical parameters of individually zone comminuted finished unhomogeneous paleobotanic , lithological, geochemical, paleobiogeographical and rough separate manners. So managed to build the climatic zones of the ages of the cretaceous occlusion . To ascendency both(prenominal) of our separate were comp atomic number 18d with theoriseions obtained another(prenominal) , a relatively modernistic manner of numerical cast climates. It is establish on the use up of bodily models of the Earths climate and paleogeographic reconstructive memorys integrity almost tested paleoclimatic parameters extracted from geologic info . Therefore, geological and numeric methods of watch and accompaniment each other .\n poser stomach outright depart an com target of ​​the multi-year weather, its parameters, their spheric dissemination and seasonal kinetics . geological method is competent to reconstruct the position and most the climate, major(ip) climatic zones , averaged over millions of years. These earlier rough reconstruction atomic number 18 important , as ar the trial-and-error petty(a) of paleoclimatology . The results of twain methods in this case correct transcription and argon thus for the most part weather each other. However, the next willing be celebrated that in some parameters amid them in that respect are some differences that prolong in some cases systematic.'