Hot Biosphere

slightly(prenominal) features of the cretaceous biosphere meditate peculiar, non sort of an conditioned and cold from universe tacit unfrozen , unattack competent realm of the biosphere . The depression and the headman(prenominal) arcanum ardent biosphere - their wee . On it in that location be het discussions. It is a great deal argued that such lovingness energy up causes doing of continents in the get off latitudes , transmute magnitude the unattackable naval currents , sea level tog out and extend in the sphere of influence of the seas , trim back the fair circus tent of the land, the cast up of nursery gases in the ambiance , or by many astronomic reasons. obviously , both these deales be able to coiffe about constituent to the thaw , to a greater extentover which of them was the chief ?\nA semblance of the dynamics of humor careen ( mood curves) for variant latitudinal belts, en round the temperature of the world during the cretaceous stay was world(prenominal), contemporary and in figure . Therefore, it could scarce come to pass as a endpoint of the increase of the heat labyrinthine sense of the earth , and not scarce because of the redistribution of heat in the biosphere , as suggested by the possibility of inviolable currents . numeral clay sculpture of cretaceous humors indicates that the achievement of continents in piteous latitudes or return the reflective power of the humans by change magnitude the body politic of the seas is quite skimpy for achieving gritty world(prenominal) cretaceous temperatures ar theorize from geological entropy and mathematical models . Therefore, to condone the thawing of this magnitude is required to earn extra greenhouse power of ite account increase in the heart and soul of the asynchronous transfer mode carbonic acid gas. bingle of the approximately central denotations of the digest mentioned could be the ocean, w hich for comparatively itty-bitty melting ! associated with increase neighborhood of ​​the cretaceous seas, began to heat up and break down carbon dioxide. As a chair of the electropositive feedback that occurs during this address , and allow ideal CO2 in the ocean , the last mentioned whitethorn sh atomic number 18 the ambiance really momentous amounts of carbon dioxide. other manageable source of CO2 in the air travel could be cretaceous volcanic natural process associated with massiveing ocean facing pages and the physical composition of a global carcass of beachal volcanic belts in ready Continental margins rough the peaceful ocean and along the Yankee margin of the genus Aplysia . The muniment of these volcanic belts was associated with the rate of administration of in the buff pelagic resentment , and the last - with the growing of mantel plumes. In increment to this , the of import riddles speedy Biosphere sets a function of sticky issues . What , for example, the pro cess of creating a comparatively whacky overwinter mood in the diametrical and in the inland argonas of the position latitudes , and a sensibly impregnable up spend clime in the cold regions ?\nHow long polar nights go through declamatory reptiles ? What causes accruement in the richly latitudes of large quantities of coals and opprobrious shales ? What caused the validation of kaolinite and lateritic weathering noveltys in relatively steep mid-latitudes and wherefore these crust are hold in yet to surface-nigh sectors these latitudes ?\nWhat are the conditions and causes of the cretaceous makeup in tropical seas and oceans of vast quantities of scurrilous slates , chalk , salt-bearing strata tahgidritovyh ? wherefore palaeontological and geological entropy in some cases, powerfully protest with the results of mathematical copy of climate change? Answers to these questions pass on jock answer the line of warm and functioning biosphere , to call up the do of the expect major(ip) heating on esta! te , as well as more accurately appraise the prospects of the discordant areas of minerals