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: 免费无遮挡AV| 伊人大杳蕉中文无码| 国产黄网站在线观看| 国产中文一区二区苍井空| 一区二区影院| 国产精品va免费视频| 国产99免费视频| 在线欧美一区| 国产黑丝视频在线观看| 一级爱做片免费观看久久| 99精品欧美一区| 亚洲精品图区| 亚洲第一黄片大全| 国产精品久久久久久影院| 国产精品夜夜嗨视频免费视频| 久久无码av一区二区三区| 国产簧片免费在线播放| 亚洲国产无码有码| 欧洲日本亚洲中文字幕| 国内精自视频品线一二区| 国产成人精品男人的天堂下载| 亚洲熟女偷拍| 永久免费无码日韩视频| 亚洲综合久久一本伊一区| 男女性午夜福利网站| 亚洲最大看欧美片网站地址| 72种姿势欧美久久久大黄蕉| 青青草久久伊人| 六月婷婷综合| av天堂最新版在线| 亚洲精品国产精品乱码不卞| 亚洲欧美另类日本| 伊人久久精品无码麻豆精品| 国产特一级毛片| 婷婷五月在线| 成人夜夜嗨| 日韩 欧美 小说 综合网 另类| 国产免费久久精品99re丫丫一| аv天堂最新中文在线| 最新国产高清在线| 国产女人喷水视频| 亚洲成人www| 欧美亚洲国产一区| 国产精品流白浆在线观看| 97成人在线视频| 尤物成AV人片在线观看| 91精品国产福利| 久久精品娱乐亚洲领先| 欧美日韩精品一区二区在线线| 激情无码字幕综合| 国产成人做受免费视频| 国产网友愉拍精品视频| 日韩高清欧美| 久久久久九九精品影院| a毛片免费观看| 免费毛片a| 国产一在线观看| 亚洲国产日韩在线观看| 四虎国产精品永久一区| 在线视频精品一区| 97久久人人超碰国产精品| 热久久这里是精品6免费观看| 日韩黄色在线| 99色亚洲国产精品11p| 国产免费怡红院视频| 国产精彩视频在线观看| 怡红院美国分院一区二区| 九色综合伊人久久富二代| 国产在线观看第二页| 精品無碼一區在線觀看 | 99ri精品视频在线观看播放| 国产幂在线无码精品| 超碰91免费人妻| 久久青青草原亚洲av无码| 日韩av无码精品专区| 四虎影视库国产精品一区| 日本不卡在线| 精品国产自| 精品人妻一区无码视频| 亚卅精品无码久久毛片乌克兰| 亚洲精品国产乱码不卡| 日韩第九页|