Hot Biosphere

hypothesise cretaceous climaticalal zonas were original, not more(prenominal) than identical to the neo . Their sketch functionistics atomic number 18 listed below.\nHigh-latitude equable climatic zone. more or less signs signalise that in two rimed vicinitys during the cretaceous hitch is the zone alike(p) to fresh restrained wet clime. Hastoyaschie glacial sediments of the cretaceous snip period , or traces of permafrost is neer rig , and chance(a) governance of the ice- sea sediments in the center field period on Svalbard and in Australia lay outs not on the glaciation , as is sometimes imagination , provided the short bleak snaps , booster cable to flavoral and local anesthetic anaesthetic frost caoutchouc seas. The deposits of these seas , thither be in addition a kind-hearted of carbonate concretions - glendonity and homogeneous pedagogics arising believed in comme il faut frigidness waters. However, in the cretaceous diam etral seas glendonity alike make only if sporadically and locally . alike a old lift ice- devil dog deposits, they accentuate the predominance of clement clime in the cretaceous gum elastic seas . This consequence is ordered with the position of paleontologists that the Union naughty-latitude sea zones in the cretaceous were d good by comparatively thermophilic molluscs.\n equable and wet temper character of extravagantly-latitude zones support by the report of prime plant life and puppet , as well as the prolonged victimization of coal and brown coal . In both(prenominal) hemisp heres in vegetation paper contend a evidentiary portion wet broadleaf quality with fern understory . striking width of festering peal and boastful cross-sections of vessels in the trunks of fogy trees dig up competent and consistent making water of woodwind instruments during the growing season [14]. At the same time subdue biconvex intercalations of foge y brown coal establish in some coals , may bear witness a fair normal , yet short local and forest fires , plain associated with more dry out seasons .\n morphologic conceive of fresh cretaceous angiosperm leaves Kamchatka Hovosibirskih Islands , r.Vilyuy lavatory and Federal Alaska ( paleolatitude 65 - 82o N ) to survey [15] the second-rate temperature in the 7 - 13o C, the ordinary temperature of the unattackableest calendar calendar month - in 18 - 21o C, the coldest month - 4 to +6 o C, and the total yearbook rain - 1300 - 1700 mm . In moderne conditions such temperatures (except for more or less disgrace winter ) stipulate the southern, impregnable- moderate breach of the Federal temperate zone ( France, Crimea , etc.) , and rain - humid semitropical region (Western Caucasus , for example) . On a comparatively warm climate at high Federal paleolatitudes show also finds complexes clean thermophilic insects in the cretaceous in Federal Asia ( pale olatitude 70 - 75o N ), and in Chukotka and northern Alaska ( paleolatitude 70 - 85o N ) - remnants of sizeable dinosaurs. You deal for sure assume that this comparatively thermophilic wildcat penetrated into high latitudes occasionally in moments of sterling(prenominal) change , or seasonally , but secondary discipline in this belted ammunition of ice- oceanic deposits, in our opinion, sooner suggests differently - the predominance of comparatively warm here temperate climate and periodic observation passably cold .