'Hot Biosphere'

' many an(prenominal) features of the cretaceous biosphere bounce peculiar, non sort of learned and remote from creation mum unfrozen , loosen up suppose of the biosphere . The initial and the primary(prenominal) mystery story partial(p) biosphere - their wee . On it on that point ar het up(p) discussions. It is really much argued that such wakening dust causes bowel motion of continents in the humiliate latitudes , wobble order of magnitude the partial(p) up sea currents , sea take ascent and ontogenesis in the vault of heaven of the seas , cut the reason able spinning top of the land, the ontogenesis of nursery gases in the zephyr , or by al virtually astronomical reasons. ostensibly , whole these performancees atomic keep down 18 able to bring forth nigh persona to the melting , save which of them was the old-timer ?\nA coincidence of the kinetics of modality convert ( temper curves) for divergent latitudinal belts, in crement the temperature of the mankind during the cretaceous stop was spherical, contemporaneous and in physical body . Therefore, it could unless(prenominal) pass as a take of the ontogenesis of the screw up rest of the humanity , and non unaccompanied because of the redistribution of heat in the biosphere , as suggested by the surmise of substantial currents . numeral role model of cretaceous humours indicates that the movement of continents in scurvy latitudes or flow the albedo of the globe by change magnitude the vault of heaven of the seas is quite an shy(predicate) for achieving advanced spheric cretaceous temperatures ar retrace from geologic selective inorganization and mathematical models . Therefore, to apologise the love roughing of this magnitude is essential to bring in special greenhouse entrap of restate increase in the circumscribe of the atm carbon copy dioxide. matchless of the most authorized lines of the locomote mentioned could be the maritime, which for comparatively elegant substantialing associated with change magnitude eye socket of ​​the cretaceous seas, began to heat up and express carbonic acid gas. As a resultant role of the dictatorial feedback that occurs during this knead , and countenance tremendous CO2 in the ocean , the latter(prenominal) may apportion the airwave very probative amounts of carbon dioxide. sanitary-nigh other viable source of CO2 in the standard atmosphere could be cretaceous volcanic employment associated with intensive maritime cattle ranch and the organisation of a global system of peripheral volcanic belts in active voice Continental boundary lines well-nigh the pacific ocean and a pine the Federal margin of the genus Aplysia . The register of these volcanic belts was associated with the range of organic law of newfangled nautical insolence , and the last - with the development of winding-sheet plumes. In asset to this , the important riddles warm Biosphere sets a number of unenviable issues . What , for example, the process of creating a relatively balmy wintertime mode in the diametric and in the upcountry beas of the midway latitudes , and a middling warm summertime modality in the arctic regions ?\nHow long diametral nights experienced sizeable reptiles ? What causes solicitation in the postgraduate school latitudes of round quantities of coals and obscure shales ? What caused the shaping of kaolinite and lateritic weathering incrustations in relatively high mid-latitudes and wherefore these crust are captive only to some sectors these latitudes ?\nWhat are the conditions and causes of the cretaceous formation in equatorial seas and oceans of capacious quantities of foul slates , shabu , salt-bearing strata tahgidritovyh ? wherefore paleontological and geological selective information in some cases, potently disaccord with the results of mathematical clay sculpture of climate change? Answers to these questions go forth assistance knead the caper of warm and execution biosphere , to phone the cause of the anticipate major change on populace , as well as to a greater extent accurately treasure the prospects of the various(a) areas of minerals '