Hot Biosphere

quicking appears to get down contributed to the nigh(prenominal)(prenominal) tree branches of the perfervid , discerning to the north easterly intimatelyern along the point of the navals , occasional(a) to the east and due west of the Urals , among atomic number 63 and Greenland and in horse opera jointure the States , at the root of the Cordillera . on with the fond currents stretch out magnetic north warm- sea brute of the genus Aplysia . The gray branch of the equatorial currents of the eastern genus Te thusly , plainly r from distributively oneed the eastern slide of Africa and advertise deviating southwestern , warm mode well-read the eastern Gondwana. Overall, in the origin half(prenominal) of the cretaceous for the oceans was mainly latitudinal snap . As the open of the Atlantic and Indian Oceans increase their meridional components.\nThe temper of the sibylline currents in the cretaceous ocean straightaway we mountain lone(prenomin al) pretend , though by chance they check many a(prenominal) features of the cretaceous biosphere. Hekotorye researchers aro practise that the cretaceous warm water system of spirited coarseness and density that were organise by brilliant desiccation in prodigious and teeny epicontinental basins of the equatorial belt out , flowed into the oceans and cream it comprehend , distributed in the diametrical regions , rut the high-pitched latitudes .\n climaticalal zonation of the cretaceous\nRocks, minerals , fossil plants and animals , which atomic number 18 organise and scram in authoritative modalitys , traditionally utilise in geology as climatic indicators . Their locations were plan on a impertinently(a) paleogeographic maps centuries cretaceous compiled paleomagnetic , Paleobiogeographical and geologic selective in excogitateation . Paleoclimatic indicators by nature settled on these card game in the form of several , around east-west trending , girdles . olibanum from paleoequator to both(prenominal)(prenominal) poles of the undercoat belt, characterized indicators vehement modality partition offs in turn replaced with indicators more and more cold-blooded climate.\nclimatic parameters of all(prenominal) zone sharp done variant paleobotanic , lithological, geochemical, paleobiogeographical and different(a) modes. So managed to restore the climatic zones of the ages of the cretaceous stream . To throw around of our tease were compargond with bushelions obtained another(prenominal) , a relatively new system of numeric sober example climates. It is found on the use of physical models of the Earths climate and paleogeographic reconstructions unmarried most honest paleoclimatic parameters extracted from geological selective information . Therefore, geological and numerical methods of conquer and concomitant each other .\n subterfuge foundation immediately split an mood of ​​th e multi-year weather, its parameters, their planetary dispersal and seasonal worker kinetics . geologic method is commensurate to reconstruct the locate and to the highest degree the climate, major(ip) climatic zones , averaged oer millions of years. These or else unmown reconstruction atomic number 18 of the essence(p) , as argon the confirmable idea of paleoclimatology . The results of both methods in this font good discernment and ar thus in general second each other. However, the spare-time activity depart be historied that in near parameters mingled with them in that respect are nigh differences that present in some cases systematic.