本文關(guān)鍵詞：蘭州盆地中始新世至早中新世磁性地層與古環(huán)境演化，，由筆耕文化傳播整理發(fā)布。

早漸新世蘭州盆地的巨犀及南坡坪動物群組合特征與環(huán)境意義

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摘要

在蘭州盆地漸新統(tǒng)韓家井組新發(fā)現(xiàn)的巨犀化石,屬于南坡坪動物群,該動物群主要由大小兩類動物組成.小型哺乳動物主要為梳趾鼠Ctenodactylidae等草原嚙齒類,大型林棲哺乳動物主要由巨犀Paraceratherium、副狶Paraentelodon等組成.動物群23個(gè)屬種類型中,森林型占~40%,草原型占~60%.與同期南北兩側(cè)的臨夏椒子溝動物群和黨河叮當(dāng)溝動物群相比較,明顯具有過渡區(qū)特點(diǎn).以哺乳動物化石證據(jù)推測,漸新世中國干旱帶南界很可能從蘭州盆地附近通過.
        

引文

安成邦,陳發(fā)虎.2009.中東亞干旱區(qū)全新世氣候變化的西風(fēng)模式——以湖泊研究為例.湖泊科學(xué),21:329–334
    鄧濤,王曉鳴,倪喜軍,劉麗萍,梁忠.2004.臨夏盆地的新生代地層及其哺乳動物化石證據(jù).古脊椎動物學(xué)報(bào),42:45–66
    鄧濤.2004.臨夏盆地晚新生代哺乳動物群演替與青藏高原隆升背景.第四紀(jì)研究,24:413–420
    方小敏,徐先海,宋春暉,韓文霞,孟慶泉,鳥居雅之.2007.臨夏盆地新生代沉積物高分辨率巖石磁學(xué)記錄與亞洲內(nèi)陸干旱化過程及原因.第四紀(jì)研究,27:989–1000
    符淙斌,安芷生.2002.我國北方干旱化研究-面向國家需求的全球變化科學(xué)問題.地學(xué)前緣,9:271–275
    葛肖虹,任收麥,馬立祥,吳光大,劉永江,袁四化.2006.青藏高原多期次隆升的環(huán)境效應(yīng).地學(xué)前緣,13:118–130
    耿寶印,陶君容,頡光普.2001.蘭州盆地早第三紀(jì)植物及古氣候意義.植物分類學(xué)報(bào),39:105–115
    黃學(xué)詩.1982.內(nèi)蒙古阿左旗烏蘭塔塔爾地區(qū)漸新世地層剖面及動物群初步觀察.古脊椎動物與古人類,20:337–349
    黃學(xué)詩.1993.內(nèi)蒙古烏蘭塔塔爾地區(qū)中漸新世的圓柱齒鼠科嚙齒類.古脊椎動物學(xué)報(bào),31:33–43
    李吉均,文世宣,張青松,王富葆,鄭本興,李炳元.1979.等青藏高原隆起的時(shí)間、幅度和形式的探討.中國科學(xué)B輯,6:608–618
    李吉均,周尚哲,趙志軍,張軍.2015.論青藏運(yùn)動主幕.中國科學(xué):地球科學(xué),45:1597–1608
    劉東生,鄭綿平,郭正堂.1998.亞洲季風(fēng)系統(tǒng)的起源和發(fā)展及其與兩極冰蓋和區(qū)域構(gòu)造運(yùn)動的時(shí)代耦合性.第四紀(jì)研究,3:194–204
    齊陶.1992.記云南巨兩棲犀屬一新種.古脊椎動物學(xué)報(bào),30:229–232+260
    強(qiáng)小科,安芷生,宋友桂,常宏,孫有斌,劉衛(wèi)國,敖紅,董吉寶,符超峰,吳楓,盧鳳艷,蔡演軍,周衛(wèi)健,曹軍驥,徐新文,艾莉.2010.晚漸新世以來中國黃土高原風(fēng)成紅粘土序列的發(fā)現(xiàn):亞洲內(nèi)陸干旱化起源的新記錄.中國科學(xué):地球科學(xué),40:1479–1488
    邱占祥.1962.記云南羅平的巨犀化石并論葛氏巨犀的性質(zhì).古脊椎動物與古人類,6:57–71
    邱占祥.1973.新疆準(zhǔn)噶爾盆地的巨犀化石.古脊椎動物學(xué)報(bào),11:182–191
    邱占祥,邱鑄鼎.1990.中國晚第三紀(jì)地方哺乳動物群的排序及其分期.地層學(xué)雜志,14:241–260
    邱占祥,王伴月,邱鑄鼎,頡光普,謝駿義,王曉鳴.1997.甘肅蘭州盆地咸水河組研究的新進(jìn)展.演化的實(shí)證——紀(jì)念楊鐘健教授百年誕辰論文集.北京:海洋出版社.177–192
    邱占祥,谷祖綱.1998.甘肅蘭州-第三紀(jì)中期哺乳動物化石地點(diǎn).古脊椎動物學(xué)報(bào),26:198–213
    邱占祥,王伴月,鄧濤.2004a.甘肅臨夏盆地的漸新世巨犀化石.古脊椎動物學(xué)報(bào),42:177–192
    邱占祥,王伴月,鄧濤.2004b.甘肅臨夏盆地牙溝的哺乳動物化石及有關(guān)地層問題.古脊椎動物學(xué)報(bào),42:261–268
    邱占祥,王伴月.2007.中國的巨犀化石.中國古生物志.總號第193冊,新丙種第29號.北京:科學(xué)出版社.1–444
    邱鑄鼎,李傳夔.2004.中國哺乳動物區(qū)系的演變與青藏高原的抬升.中國科學(xué)D輯:地球科學(xué),34:845–854
    孫柏年,閻德飛,解三平,叢培允,辛存林,云飛.2004.蘭州盆地古近系楊屬葉化石及古氣候指示意義.科學(xué)通報(bào),49:1283–1289
    孫秀玉,趙英娘,何卓生.1984.青海西寧-民和盆地漸新世至中新世孢粉組合.地質(zhì)論評,30:207–216,303
    童永生,鄭紹華,邱鑄鼎.1995.中國新生代哺乳動物分期.古脊椎動物學(xué)報(bào),33:290–314
    童永生,鄭紹華,邱鑄鼎.1996.中國新生代哺乳動物區(qū)系演變.古脊椎動物學(xué)報(bào),34:215–227
    拓守廷,劉志飛,趙泉鴻,成鑫榮.2006.漸新世初大冰期事件:南大西洋ODP1265站的記錄.地球科學(xué),31:151–158
    王伴月.1997.陸相漸新統(tǒng)劃分中的問題及新進(jìn)展.地層學(xué)雜志,21:81–90
    王伴月,邱占祥.2000.甘肅蘭州盆地咸水河組下紅泥巖中的小哺乳動物化石.古脊椎動物學(xué)報(bào),38:255–273
    王伴月.2001.會用“梳子”梳毛發(fā)的嚙齒動物——梳趾鼠.化石,3:8–10
    王伴月,邱占祥,王曉鳴,頡光普,謝駿義,Downs W,邱鑄鼎,鄧濤.2003.甘肅省黨河地區(qū)的新生代地層和青藏高原隆升.古脊椎動物學(xué)報(bào),41:66–75
    王伴月,邱占祥.2004.甘肅黨河下游地區(qū)早漸新世哺乳動物化石的發(fā)現(xiàn),42:130–143
    王大寧,孫秀玉,趙英娘,何卓生.1990.青海、新疆部分地區(qū)晚白堊世-第三紀(jì)孢粉植物群研究.北京:中國環(huán)境科學(xué)出版社.1–179
    王曉鳴,王伴月,邱占祥.2008.步林在甘肅黨河流域塔奔布魯克地區(qū)工作記錄——經(jīng)典脊椎動物化石與現(xiàn)代地層框架的解譯.古脊椎動物學(xué)報(bào),46:l–19
    吳珍漢,吳中海,胡道功,葉培盛,周春景.2007.青藏高原漸新世晚期隆升的地質(zhì)證據(jù).地質(zhì)學(xué)報(bào),81:577–587
    頡光普.2004.甘肅蘭州盆地的第三紀(jì)地層及哺乳動物群.地層學(xué)雜志,28:67–80
    頡光普,趙得思.2011.甘肅新生代氣候環(huán)境變化與哺乳動物群演替.第四紀(jì)研究,31:597–607
    姚妮妮,馬福軍,閆德飛.2010.甘肅蘭州盆地漸新世古氣候參數(shù)重建.甘肅地質(zhì),19:20–25
    姚妮妮,馬福軍,閆德飛.2011.共存分析法在蘭州盆地漸新世哺乳動物化石研究中的應(yīng)用.甘肅科學(xué)學(xué)報(bào),23:72–78
    袁復(fù)禮,杜恒儉.1984.中國新生代生物地層學(xué).北京:地質(zhì)出版社.1–376
    岳樂平,Heller F,邱占祥,張莉,頡光普,邱鑄鼎,張?jiān)葡?2000.蘭州盆地第三系磁性地層年代與古環(huán)境記錄.科學(xué)通報(bào),45:1998–2002
    張克信,王國燦,季軍良,駱滿生,寇曉虎,王岳明,徐亞東,陳奮寧,陳銳明,宋博文,張楗鈺,梁銀平.2010a.青藏高原古近紀(jì)-新近紀(jì)地層分區(qū)與序列及其對隆升的響應(yīng).中國科學(xué)D輯:地球科學(xué),40:1632–1654
    張克信,王國燦,駱滿生,季軍良,徐亞東,陳銳明,陳奮寧,宋博文,梁銀平,張楗鈺,楊永鋒.2010b.青藏高原新生代構(gòu)造巖相古地理演化及其對構(gòu)造隆升的響應(yīng).地球科學(xué),35:697–712
    張克信,王國燦,洪漢烈,徐亞東,王岸,曹凱,駱滿生,季軍良,肖國橋,林曉.2013.青藏高原新生代隆升研究現(xiàn)狀.地質(zhì)通報(bào),32:1–18
    張鵬.2015.蘭州盆地中始新世至早中新世磁性地層與古環(huán)境演化.博士學(xué)位論文.西安:中國科學(xué)院地球環(huán)境研究所.1–117
    張仲石,郭正堂.2005.根據(jù)地質(zhì)記錄恢復(fù)漸新世和中新世不同時(shí)期環(huán)境空間特征及其意義.第四紀(jì)研究,25:523–530
    朱宗浩.1985.柴達(dá)木盆地第三紀(jì)孢粉學(xué)研究.北京:石油工業(yè)出版社.1–297
    An Z S.2014.Late Cenozoic Climate Change in Asia:Loess,Monsoon and Monsoon-arid Environment Evolution.Dordrecht:Springer.1–587
    Burchfiel B C,Zhang P Z,Wang Y P,Zhang W P,Song F M,Deng Q D,Molnar P,Royden L.1991.Geology of the Haiyuan fault zone,Ningxia-Hui Autonomous Region,China,and its relation to the evolution of the Northeastern Margin of the Tibetan Plateau.Tectonics,10:1091–1110
    David B Rowley,Brian S Currie.2006.Paleo-altimetry of the late Eocene to Miocene Lunpola basin,central Tibet.Nature,439:677–681
    Deng T,Downs W.2002.Evolution of Chinese Neogene Rhinocerotidae and its response to climatic variations.Acta Geol Sin,76:139–145
    Deng T,Qiu Z X,Wang B Y,Wang X M,Hou S K,2013.Late Cenozoic biostratigraphy of the Linxia Basin,northwestern China.In:Wang X M,Flynn L J,Fortelius M,eds.Fossil Mammals of Asia:Neogene Biostratigraphy and Chronology.New York:Columbia University Press.243–273
    Fang,X M,Garzione C,Voo R V D,Li J J,Fan M J.2003.Flexural subsidence by 29 Ma on the NE edge of Tibet from the magnetostratigraphy of Linxia Basin,China.Earth Planet Sci Lett,210:545–560
    Foster-Cooper C.1915.New genera and species of mammals from the Miocene deposits of Baluchistan:Preliminary notice.Ann Mag Nat Hist(Ser 8),16:404–410
    Li J J.1995.Uplift of Qinghai-Xizang(Tibet)Plateau and Global Change.Lanzhou:Lanzhou University Press.1–207
    Lucas S G,Sobus J C.1989.The systematic of indricotheres.In:Prothero D R,Schoch R M,eds.The Evolution of Perissodactyls.New York:Oxford University Press.358–378
    Metivier F,Gaudemer Y,Tapponnier P,Meyer B.1998.Northeastward growth of the Tibet Plateau deduced from balanced reconstruction of two deposional areas:The Qaidam and Hexi Corridor basins,China.Tectonics,17:823–842
    Miao Y F,Wu F L,Herrmann M,Yan X L,Meng Q Q,2013.Late early Oligocene East Asian summer monsoon in the NE Tibetan Plateau:Evidence from a palynological record from the Lanzhou Basin,China.J Asian Earth Sci,75:46–57
    Prothero D R,Gurin C,Manning E.1989.The history of the Rhinocerotoidea.In:Prothero D R,Schoch RM,eds.The Evolution of Perissodactyls.New York:Oxford University Press.321–340
    Ramstein G,Fluteau F,Besse J,Joussaume S.1997.Effect of orogeny,plate motion and land-sea distribution on Eurasian climate change over the past 30 million years.Nature,386:788–795
    Sun J M,Zhu R X,An Z S.2005.Tectonic uplift in the northern Tibetan Plateau since 13.7 Ma ago inferred from molasse deposits along the Altyn Tagh Fault.Earth Planet Sci Lett,235:641–653
    Sun J M,Ye J,Wu W Y,Ni X J,Bi S D,Zhang Z Q,Liu W M,Meng J.2010.Late Oligocene-Miocene mid-latitude aridification and wind patterns in the Asian interior.Geology,38:515–518
    Sun J M,Xu Q H,Liu W M,Zhang Z Q,Xue L,Zhao P.2014.Palynological evidence for the latest Oligocene-Early Miocene paleoelevation estimate in the Lunpola Basin,central Tibet.Palaeogeogr Paleoclimatol Paleoecol,399:21–30
    Tapponnier P,Xu Z Q,Roger F,Meyer B,Arnaud N,Wittlinger G,Yang.2001.Geology-Oblique stepwise rise and growth of the Tibet Plateau.Science,294:1671–1677
    Wang X M,Downs W,Xie J Y,Xie G P.2001.Didymoconus(Mammalia:Didymoconidae)from Lanzhou Basin,China and its Stratigraphic and Ecological Significance.U.S.A.J Vertebr Paleontol,21:555–564
    Wang X M,Wang B Y,Qiu Z X,Xie G.P,Xie J Y,Will D,Qiu Z D,Deng T.2003.Danghe area(weatern Gansu,China)biostratigraphy and implications for deposional history and tectonics of northern Tibetan Plateau.Earth Planet Sci Lett,208:253–269
    Zachos J C,Lohmann K C,Walker J C,Wise S W.1993.Abrupt climate change and transient climates during the Paleogene:A Marine Perspective.J Geol,101:191–213

  本文關(guān)鍵詞：蘭州盆地中始新世至早中新世磁性地層與古環(huán)境演化，由筆耕文化傳播整理發(fā)布。