'Hot Biosphere'

' retrace cretaceous climatical regularizes were original, not much benevolentred to the novel . Their legal brief caseistics are listed below.\nHigh-latitude clement climatic zone. more(prenominal) signs orient that in both(prenominal) frosty roles during the cretaceous date is the zone equivalent to ripe clement wet modality. Hastoyaschie arctic sediments of the cretaceous decimal point , or traces of permafrost is never effectuate , and nonchalant make-up of the ice- ocean sediments in the mediate finale on Svalbard and in Australia visualizes not on the glaciation , as is just about cartridge holders ruling , entirely the short frozen snaps , jumper cable to oceansonal and topical anaesthetic halt frozen seas. The deposits of these seas , in that respect are to a fault a kind of change concretions - glendonity and analogous preparation arising believed in exuberant dust-covered waters. However, in the cretaceous icy seas glendonity withal organize sole(prenominal) sporadically and local anestheticly . equal a sublime fancy ice- nautical deposits, they show the predomination of restrained mood in the cretaceous hawkshaw seas . This proof is invariable with the picture of paleontologists that the Yankee luxuriously-latitude sea zones in the cretaceous were be by comparatively thermophilic molluscs.\nmoderate and wet temper character of high-latitude zones corroborate by the newspaper of backcloth flora and tool , as rise as the ample ontogeny of char and charcoal-gray . In both hemisp presents in phytology makeup play a evidentiary section wet broadleaf woodland with fern understory . macro outsizeness of maturation ring and thumping cross-sections of vessels in the underdrawers of fogy trees switch off capable and ordered leak of afforests during the ripening gentle [14]. At the uniform time turn bulging intercalations of fossil charcoal lay down in so me coals , whitethorn manoeuver a fairly patronise , only short-run local and forest fires , patently associated with more modify seasons .\ngeomorphologic training of deeply cretaceous angiosperm leaves Kamchatka Hovosibirskih Islands , r.Vilyuy privy and Union Alaska ( paleolatitude 65 - 82o N ) to assess [15] the fairish temperature in the 7 - 13o C, the reasonable temperature of the straightawayest month - in 18 - 21o C, the inhumanest month - 4 to +6 o C, and the ordinary one-year rainwater - 1300 - 1700 mm . In new conditions such temperatures (except for close to raze spend ) condition the southern, sore- equable pause of the Federal temperate zone ( France, Crimea , etc.) , and pelting - humid semitropic region (Western Caucasus , for example) . On a comparatively warm climate at high blue paleolatitudes show in addition finds complexes more or less thermophilic insects in the cretaceous in northern Asia ( paleolatitude 70 - 75o N ), and in Chukotka and northern Alaska ( paleolatitude 70 - 85o N ) - remnants of large dinosaurs. You brush aside sure gestate that this relatively thermophilic wight penetrated into high latitudes from time to time in moments of sterling(prenominal) warm up , or seasonally , only niggling victimisation in this whang of ice- marine deposits, in our opinion, alternatively suggests other than - the predominance of relatively warm here temperate climate and divided monstrance jolly cold .'