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: 18禁影院亚洲专区| 亚洲区第一页| 国产农村1级毛片| 国禁国产you女视频网站| 高清免费毛片| 爱爱影院18禁免费| 亚洲天堂网视频| 18禁不卡免费网站| 欧洲一区二区三区无码| 久久精品91麻豆| 亚洲人成人无码www| 国产成人综合日韩精品无码不卡| 区国产精品搜索视频| 国产精品夜夜嗨视频免费视频| 国国产a国产片免费麻豆| 性69交片免费看| 一级毛片免费的| 亚洲AV无码精品无码久久蜜桃| 五月天福利视频| 一本大道视频精品人妻| 免费看a毛片| 日韩色图区| 天天色综网| 国产福利小视频在线播放观看| 国产乱人激情H在线观看| 亚洲不卡网| 欧美在线精品一区二区三区| 国产欧美在线| 精品精品国产高清A毛片| 无码AV日韩一二三区| 婷婷色中文| 国产aaaaa一级毛片| 色婷婷电影网| 日韩成人在线网站| 一区二区影院| 亚洲女同欧美在线| 国产综合网站| 欧美成人一级| 福利视频一区| 婷婷成人综合| 欧美激情视频二区| 日韩在线视频网站| 久久香蕉国产线| 67194成是人免费无码| 99999久久久久久亚洲| 亚洲美女一级毛片| 久久精品人人做人人爽| 国产微拍一区| AV无码一区二区三区四区| 久久久黄色片| 精品欧美一区二区三区在线| 丝袜亚洲综合| 亚洲无码37.| 国产欧美日韩视频怡春院| 美女无遮挡被啪啪到高潮免费| 精品视频91| 天天躁狠狠躁| 国产精品区网红主播在线观看| 波多野结衣的av一区二区三区| 毛片在线播放网址| 波多野结衣一区二区三视频| 综合五月天网| 九九香蕉视频| 精品久久蜜桃| 91在线播放免费不卡无毒| 国产亚洲男人的天堂在线观看 | 欧美一级黄色影院| 国产在线日本| 国产成人精品在线1区| 在线亚洲天堂| 欧美无专区| 中国黄色一级视频| 欧美五月婷婷| 国产欧美日韩一区二区视频在线| 2021国产精品自产拍在线| 直接黄91麻豆网站| 伊人久久大香线蕉影院| 日韩精品亚洲一区中文字幕| 亚洲人成网站在线观看播放不卡| 色哟哟国产成人精品| 萌白酱国产一区二区| 国产呦视频免费视频在线观看|