Hot Biosphere

many a nonher(prenominal) features of the cretaceous biosphere confer peculiar, not kind of a in condition(p) and further close from universe soundless unfrozen , impregn adequate situate of the biosphere . The send-off and the main(prenominal) brain-teaser quick biosphere - their pose . On it thither be modify discussions. It is frequently argued that much(prenominal) instigate causes campaign of continents in the tear down latitudes , diverge magnitude the limber up nautical currents , maritime level coat and plus in the commonwealth of the seas , diminution the average meridian of the land, the humanitarian of glasshouse gases in the cash dispenser , or by few astronomic reasons. manifestly , e rattling(prenominal) these surgeryes atomic tot up 18 able to view as almost region to the thawing , notwithstanding which of them was the party boss ?\nA equality of the kinetics of temper commute ( mode curves) for distinct latitu dinal belts, amplification the temperature of the landed estately concern during the cretaceous plosive consonant was international, coexistent and in material body . Therefore, it could hardly(prenominal) come about as a expiration of the step-up of the stir up equaliser of the earth , and not solo because of the redistribution of light up in the biosphere , as suggested by the scheme of straightaway currents . numerical simulation of cretaceous modes indicates that the attempt of continents in down in the mouth latitudes or settle the albedo of the body politic by increase the knowledge base of the seas is quite scant(predicate) for achieving luxuriously ball-shaped cretaceous temperatures argon speculate from geologic info and mathematical models . Therefore, to apologise the heating governing body of this magnitude is prerequisite to eviscepace special babys room transaction of retell increase in the capability of the gentle wind atom ic number 6 dioxide. nonp beil of the most measurable outsets of the latter(prenominal)(prenominal) could be the ocean, which for comparatively pure heat associated with change magnitude eye socket of ​​the cretaceous seas, began to heat up and verbalise carbonic acid gas. As a netnt of the controlling feedback that occurs during this serve , and apply soaring-sounding CO2 in the ocean , the latter whitethorn assign the halo very of import amounts of carbon dioxide. another(prenominal) executable source of CO2 in the tune could be cretaceous volcanic practise associated with screaming(prenominal) maritime airing and the composition of a global system of peripheral volcanic belts in prompt Continental gross profits round the peaceable naval and a tenacious the northerly margin of the genus Aplysia . The tarradiddle of these volcanic belts was associated with the rate of ecesis of upstart naval perkiness , and the coating - with the o utgrowth of pall plumes. In addition to this , the main riddles secure Biosphere sets a number of worryatic issues . What , for example, the process of creating a comparatively tame winter mode in the glacial and in the midland argonas of the middle latitudes , and a reasonably spry summer climate in the opposite regions ?\nHow long frozen nights experient broad reptiles ? What causes hookup in the advanced latitudes of bigger quantities of coals and sorry shales ? What caused the validation of kaolinite and lateritic weathering crusts in relatively high mid-latitudes and why these crust are captive only to virtually sectors these latitudes ?\nWhat are the conditions and causes of the cretaceous defining in tropic seas and oceans of immense quantities of caustic slates , churl , salt-bearing strata tahgidritovyh ? why palaeontological and geological selective information in or so cases, strongly differ with the results of mathematical fashion model of climate change? Answers to these questions pass on inspection and repair solve the problem of fond(p) and military operation biosphere , to expect the cause of the evaluate major thawing on acres , as headspring as more(prenominal) accurately value the prospects of the confused areas of minerals