999精品在线视频,手机成人午夜在线视频,久久不卡国产精品无码,中日无码在线观看,成人av手机在线观看,日韩精品亚洲一区中文字幕,亚洲av无码人妻,四虎国产在线观看 ?

Folded Mountains and Seas:The Life Epic of the Qinghai-Xizang Plateau

2025-08-07 00:00:00
中國新書(英文版) 2025年3期

isaresearcheratthe the hasa Ph.D. in stratigraphy paleontology from Peking University.In recent years, hehasfocused onthe evolution Cenozoic fishes on the Qinghai-Xizang Plateau.

The author follows a personal scientific expedition the Qinghai-Xizang Plateau integrates the arduous scientific expedition process,the desolate magnificent plateau wonders,the colorful customs, exciting fossil discoveries in this book.Added by the exquisite self-painted paleontological illustrations, the book tells the evolution legend various creatures such as the ichthyosaurs, climbing perch,ancient rhinoceros, three-toed horses on the Qinghai-Xizang Plateau over the past 2O0 million years,presenting the epic life on the plateau.

FoldedMountainsSeas: TheLife Epic the QinghaiXizangPlateau

Wu Feixiang

China Science Technology

Press

January 2025

88.00 (CNY)

a giant jigsaw puzzle,with tectonic plates sliding undulating atop the searing,molten mantle. Drifting apart colliding again,they ceaselesslyreshapethedistribution l sea,remolding the face our planet.The mirrored coastlines across distant oceans, the colossal mountain ranges crisscrossingcontinentsall bearwitnesstotheirrelentless craftsmanship.

Around 3o0 million years ago, Gondwana beganto fracture.As a“porcelain platedropped from a height\"the supercontinent fragmented into lmasses varying sizes,drifting apart in differentdirectionsatdivergent speeds.Driven by mantle plume upwellingoceanicplate subduction (Note:some scholars posit that meteorite impacts may havealso contributed to the initial momentum),the Qiangtang Lhasa terranesatGondwana's northern margin,along with the lndiansubcontinent,raced northwardtoward Eurasia.Their collisionsultimately reshaped Asia's geography climate on acontinentalscale.Theripple effects these tectonic upheavals spread farwidewithinEarth's interconnected systems,reaching NorthAmericaAfrica.

This was an epic journey epochs, withcontinentalfragments travelingfromthesouthern hemisphere to the northern hemisphereoverhundreds millions years.Throughevershiftingenvironments,these lmassessailed like\"arks\" carryingpassengers from Earth's distantrealmstowhatwould

Chiculte

ago),shortlyaftertheextinction non-avian dinosaurs,the Indian subcontinentmettheEurasian continent (theLhasa terrane) near 14° north latitude.(ln 2021,some scientistsproposedan“IndiaAsia two-stage collision model\" suggesting thisinitial contact involved the Tethyan Himalayan terrane,a fragment rifted from the Indian subcontinent, colliding first withthe Asian continent.) As the continentsconverged collided, theyeventuallyforgedEarth's most majestic mountain system, the Himalayas, catalyzed the rise the Qinghai-Xizang Plateau, the\"Ro theWorld.\"This upheaval ultimately shaped China's fundamental geographical pattern: \"easternwaterswestern mountains\"Against the backdrop global cooling,thetwin forces marine regression mountainbuildingintensifiedaridityin CentralAsia'sGobideserts,while transforming the Yangtze River basin fromwindswept ssinto themisty,river-veined lscapes Jiangnan.

Life,ever-adapting to its environment,could not remain untouched by such monumental changes.The collision continent: marked not just the birth new mountains but also the opening biological corridors ripe With evolutionary opportunity. Scientists have discovered that faunal exchanges began almost immediatelywhen Indiafirst contactedEurasia.Over30million years later,despite the eastwest mountain barriers already spanning the Qinghai-Xizang Plateau,massive mammals like the Paraceratherium (giant rhinoceros) still migrated freely acrossitsnorthern southern reaches.Until the Early Miocene (around 20 million years ago), when the plateau began to take shape,hornless rhinos still roamed the dense forests along northern Xizang's lakes.Even when the plateau reached a state similar to its current appearance, the highls in the periglacial environment were not completely \"isolated isls\"Some animals traversed itsdeep valleys,

mountain passesalongitsedges. Mostdramatically,duringthe Pleistocene Ice Ages,frigid climates united theplateau with the Arctic. Cold-adapted species like the woolly rhinoceros theancestors Arctic foxesemerged from Xizang to colonize the polar circle, becoming legends biogeography.

The Qinghai-Xizang Plateau isten hailed asa“natural laboratory\" forundersting life's evolution. Inthishuge“laboratory\"the shifting seas continents, the connection lmasses, the risemountainsall serveas unique\"catalysts,driving biological succession dispersal. On the scale geological time, theplateau'stransformation,from oceanto l,from lowl to high-altituderealm,wasdramatic rapid,makingthetheater life here all the more spectacular.Next, let us journey across hundreds millionsyears retrace this extraordinary odyssey life.

主站蜘蛛池模板: 亚洲午夜久久久精品电影院| 国产精品专区第1页| 久久精品一品道久久精品 | 免费一级无码在线网站| 一区二区三区四区精品视频 | 亚洲欧美激情小说另类| 久久黄色一级片| 欧美日韩资源| 人人妻人人澡人人爽欧美一区| 欧美精品v欧洲精品| 国产香蕉97碰碰视频VA碰碰看| 伊人天堂网| 精品久久久久久成人AV| 91精品啪在线观看国产| 日本免费高清一区| 亚洲香蕉在线| 国产99精品视频| AV网站中文| 九色在线视频导航91| 99热这里只有精品国产99| 欧美色伊人| 99热最新网址| 成人蜜桃网| 亚洲日韩精品伊甸| 深夜福利视频一区二区| 无码专区在线观看| 91黄色在线观看| 久久99精品久久久久久不卡| h视频在线播放| 91无码网站| 最新国产麻豆aⅴ精品无| 99久久精品国产麻豆婷婷| 亚洲码在线中文在线观看| 特级毛片8级毛片免费观看| 高清码无在线看| 激情在线网| 亚洲一级毛片| 免费观看精品视频999| 69国产精品视频免费| 91视频青青草| 无码啪啪精品天堂浪潮av| 免费看一级毛片波多结衣| 99热6这里只有精品| 国产玖玖视频| 女人一级毛片| 四虎在线观看视频高清无码| 欧美色视频日本| 亚洲精品大秀视频| 欧美97欧美综合色伦图 | 视频二区亚洲精品| 久久综合丝袜日本网| 国产99在线| 亚洲成在线观看 | 国产高清又黄又嫩的免费视频网站| 亚洲黄色高清| 为你提供最新久久精品久久综合| 久久综合结合久久狠狠狠97色| 98超碰在线观看| 国产一区二区影院| 婷婷综合在线观看丁香| yjizz国产在线视频网| 国产欧美精品一区二区| 国产正在播放| 亚洲毛片一级带毛片基地| 亚洲h视频在线| 亚洲精品中文字幕无乱码| 欧美亚洲国产视频| 999在线免费视频| 福利在线不卡一区| 一级全免费视频播放| 亚洲精品视频免费看| 国产人前露出系列视频| 日本高清免费不卡视频| 五月婷婷综合色| 成人欧美日韩| 5555国产在线观看| 欧美综合成人| 美女一级免费毛片| 伊人成人在线| 久久黄色免费电影| jizz在线观看| 国产精品第页|