地球科学进展 ›› 2008, Vol. 23 ›› Issue (6): 651 -658. doi: 10.11867/j.issn.1001-8166.2008.06.0651

研究简报 上一篇    

浙东中新世 Betula mioluminifera Hu et Chaney 的发现及古气候重建
李明涛 1,2,孙柏年 1,2*1,任文秀 1,李相传 1,戴静 1   
  1. 1.兰州大学资源环境学院,甘肃 兰州 730000;2.现代古生物学与地层学国家重点实验室,中国科学院南京地质与古生物研究所,江苏 南京 210008
  • 收稿日期:2007-12-08 修回日期:2008-04-29 出版日期:2008-06-10
  • 通讯作者: 孙柏年(1955-),男,山东沂水人,教授,博导,主要从事古生物地层学的研究. E-mail:bnsun@lzu.edu.cn
  • 基金资助:

    国家自然科学基金项目“滇西腾冲—陇川新近纪植物化石角质层及古气候指示作用”(编号:40772012);现代古生物学与地层学国家重点实验室(中国科学院南京地质古生物研究所)基金项目“浙江宁海新近纪某些植物化石角质层研究”(编号:063101)资助.

Discovery of Betula mioluminifera Hu et Chaney from the Miocene in Eastern Zhejiang and Reconstruction of Palaeoclimate

Li Mingtao 1,2,Sun Bainian 1,2*,Xiao Liang 1,Ren Wenxiu 1,Li Xiangchuan 1,Dai Jing 1   

  1. 1.College of Earth and Environmental Sciences, Lanzhou University, Lanzhou 730000,China;2. State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology, Chinese Academy of Sciences, Nanjing 210008, China
  • Received:2007-12-08 Revised:2008-04-29 Online:2008-06-10 Published:2008-06-10

随着古气候和古环境研究的日渐深入,“特有种气候分析法”成为新生代定量重建古气候研究的重要方法之一。使用这一方法分析了浙江东部天台中新统下南山组的古亮叶桦(Betula mioluminifera Hu et Chaney)压型化石,研究了其叶结构特征及表皮微细构造,定量推论浙江天台中新世时年平均温度为12.5~22.1℃,春季平均温度为13.0~23.1℃,较现在温暖。我国内蒙、吉林、山东、云南等地的新近系发现过古亮叶桦,分布的北界为42°N。其现存最近亲缘种亮叶桦(Betula luminifera)生活在101~119°E,23~34°N之间,海拔500~1800 m的山区,是我国特有树种。亮叶桦分布范围的缩小显示中新世一段时期我国气候逐渐变冷的趋势。

Along with the strengthening of the research of palaeoclimate and palaeoenvironment, the “climate analysis of endemic species” method has become one of efficient methods that can reconstruct palaeoclimate quantitatively. The compression of fossil Betula mioluminifera Hu et Chaney in the Xia' nanshan Formation of the Miocene in Tiantai, Zhejiang province, China, was analyzed by this method, and the leaf architecture and cuticular structure of the fossil were studied. The mean annual temperature 12.5~22.1℃ and the spring temperature 13.0~23.1℃ in the Miocene of Eastern Zhejiang were quantitatively reconstructed. As a result, the palaeoclimate of the Miocene was warmer than that of today. Fossil Betula mioluminifera had been found in the Neogene in Inner Mongolia, Jilin, Shandong and Yunnan Provinces in China, and the northern boundary of its natural distribution is 42°N. The living Betula luminifera is the nearest living relative species of fossil Betula mioluminifera and is also an endemic species in China. It grows from 500~1 800 m above sea level, within the geographic range from 101°E to 119°E and 23°N to 34°N. The decrease of distribution range of Betula luminifera shows a gradual cool climate trend gradually in some time of the Miocene.

中图分类号: 

[1] Jin JianhuaLiao WenboWang Bosunet al. Global change in Cenozoic and evolution of flora in China [J]. Guihaia2003233: 217-225. [金建华,廖文波,王伯荪,等. 新生代全球变化与中国古植物区系的演变[J]. 广西植物,2003233: 217-225.]

[2] Liu DongshengZheng MianpingGuo Zhengtang. Initiation and evolution of the Asian monsoon system timely coupled with the ice-sheet growth and the tectonic movements in Asia [J]. Quaternary Sciences1998,(3: 194-204.[刘东生,郑绵平,郭正堂. 亚洲季风系统的起源和发展及其与两极冰盖和区域构造运动的时代耦合性[J]. 第四纪研究,1998,(3: 194-204.]

[3] Leng Qin. An effective method of observing fine venation from compressed angiosperm fossil leaves [J]. Acta Palaeontologica Sinica2000391: 157-158. [冷琴. 一种观察被子植物压膜化石细微叶结构特征的有效方法[J]. 古生物学报,2000391: 157-158.]

[4] Dilcher D L. Approaches to the identification of angiosperm leaf remains [J]. Botantical Review197440: 1-157.

[5] Li ChengsenWang YufeiSun Qigao. Climate analysis of Endemic Species—A novel method for quantitative analysis of global climate change since Tertiary [J]. Acta Botanica Sinica2001432: 217-220. [李承森,王宇飞,孙启高. 定量分析第三纪以来环境变化的新方法——特有种气候分析法[J]. 植物学报,2001432: 217-220.]

[6] Li ChengsenWang YufeiSun Qigao. The quantitative reconstruction of palaeoenvironments and palaeoclimates based on plants [J]. Chinese Bulletin of Botany2003204: 430-438. [李承森,王宇飞,孙启高. 植物对环境的响应——定量重建古气候的研究进展[J]. 植物学通报,2003204: 430-438.]

[7] Wang YufeiLi ChengsenMargaret E Collinsonet al. EucommiaEucommiaceae),a potential biothermometer for the reconstruction of paleoenvironments [J]. American Journal of Botany2003901: 1-7.

[8] Wang KaifaJiang HuiZheng Zhuoet al. Sporo-pollen and siliceous algae assemblages from the intercalated bed of basaltic sediments in TiantaiXinchangShengxian of Zhejiang [J]. Journal of Stratigraphy198591: 28-36. [王开发,蒋辉,郑卓,等. 浙江天台、新昌、嵊县地区玄武岩沉积夹层的孢粉、硅藻组合[J]. 地层学杂志,198591: 28-36.]

[9] Li Haomin. Neogene floras from eastern ZhejiangChina [C]Whyte R Oed. The Evolution of the East Asian Environment Vol. II. PalaeobotanyPalaeozoology and Palaeoanthropology. Hong Kong:Centre of Asian StudiesUniversity of Hong Kong1984:461-466.

[10] Delectis Florae Reipublicae Popularis Sinica Agendae Academiae Sinicae Edita. Flora Reipublicae Popularis Sinicaein Chinese),Tomus 21 [M]. Beijing: Science Press1979: 103-137.[中国科学院中国植物志编辑委员会. 中国植物志,第21[M]. 北京: 科学出版社,1979: 103-137.]

[11] Editorial Board of Flora of Zhejiang. Flora of Zhejiangin Chinese),Vol.2 [M]. Hangzhou: Zhejiang Science and Technology Publishing House1992: 31-41. [浙江植物志编辑委员会. 浙江植物志,第2[M]. 杭州: 浙江科学技术出版社,1992: 31-41.]

[12] Cenozoic Plants from China Writing Group of Institute of BotanyNanjing Institute of Geology and PalaeontologyAcademia Sinica. Fossil Plants of ChinaCenozoic Plants from Chinain Chinese),3[M]. Beijing: Science Press1978: 57-71171-219. [中国科学院北京植物研究所,南京地质古生物研究所《中国新生代植物》编写组.中国植物化石,中国新生代植物. 第三册[M]. 北京: 科学出版社,1978: 57-71171-219.]

[13] Wu ZichengWang Yuehui. Community character for selection and improvement technique of Betula luminifera [J]. Journal of Sichuan Forestry Science and Technology1996174: 17-28. [吴子诚,王乐辉. 光皮桦选择群体特征和改良技术[J]. 四川林业科技,1996174: 17-28.]

[14] Jiang Jingmin. The study of the geographical distribution of the Betula in China [J]. Forest Research199031: 55-62. [姜景民. 中国桦木属植物地理分布的研究[J]. 林业科学研究,199031: 55-62.]

[15] Sun Bo. Shanwang Fossil Plants [M]. Ji'nan: Shandong Science and Technology Publishing House1999: 31. [孙博.山旺植物化石[M]. 济南: 山东科学技术出版社,1999: 31.]

[16] Sun BainianCong PeiyunYan Defeiet al. Cuticular structure of two angiosperm fossils in Neogene from TengchongYunnan province and its palaeoenvironmental significance [J]. Acta Palaeontologica Sinica2003422: 216-222. [孙柏年,丛培允,阎德飞,等. 云南腾冲新近纪两种被子植物化石的角质层构造及其古环境意义[J]. 古生物学报,2003422: 216-222.]

[17] Dong JianwenChen CiluChen Dongyanet al. A study on zoology and biological specific properties of Betula luminifera Winkl [J]. Acta Agriculturae Universitatis Jiangxiensis2001232: 220-223. [董建文,陈慈禄,陈东阳,等. 光皮桦栽培生物学特性研究[J]. 江西农业大学学报,2001232: 220-223.] 

[18] Chen ZhiduanLu Anmin. Origin and early evolution of the Betulaceae [J]. Journal of Graduate SchoolAcademia Sinica1995122: 199-204. [陈之端,路安民. 桦本科植物的起源和早期演化[J].中国科学院研究生院学报,1995122: 199-204.]

[19] Chen BinglinFang DeqingChe Qipenget al. On the geological age of the Laoliangdi formation and the ZhaowudaJU UD formation Chifeng Inner Mongolia [J]. Journal of Daqing Petroleum Institute1992162: 1-4.[陈秉麟,方德庆,车启鹏,等. 内蒙赤峰上第三系老梁底组及昭乌达组的时代问题[J]. 大庆石油学院学报,1992162:1-4.]

[20] Shang PingJin JianhuaSun Dejunet al. Early Miocene flora from Pingzhuang basin of Inner Mongolia and its paleoenvironment [J]. Acta Scientiarum Naturalium Universitatis Sunyatseni Nature Science),2001405: 108-112. [商平,金建华,孙德君,等.内蒙古平庄盆地中新世早期植物群与古环境[J]. 中山大学学报: 自然科学版,2001405:108-112.]

[21] Li Yuntonget al. Stratigraphy of ChinaNo.13),The Tertiary system of China [M]. Beijing: Geological Publishing House1984:1-341.[李云通,等. 中国地层第13册,中国的第三系[M]. 北京: 地质出版社,1984:1-341.]

[22] Li XikangTan XiaohongGao Ziyinget al. The geological period and sedimentation environment Mangbang formation in Tengchong areaYunnan [J]. Yunnan Geology2004232:241-251.[李锡康,谭筱虹,高子英,等.腾冲上新统芒棒组地质时代及沉积环境[J]. 云南地质,2004232: 241-251.]

[23] Climatic Data CenterNational Meteorological Information CenterCMA. The Annual Surface Climate Normals of Internatinal Exchanging Stations of China1961-1990[DB/OL]. 2005.[中国气象局,国家气象信息中心. 中国地面国际交换站气候标准值年值数据集(1961-1990[DB/OL]. 2005]

[24] Cao JiankangChen LiFang Lejin. Effects of light and temperature on storage and germination of-Betula lum inifera-seeds [J]. Journal of Northeast Forestry University2007355:17-18.[曹健康,陈黎,方乐金. 光温因子对光皮桦种子贮藏和萌发的影响[J]. 东北林业大学学报,2007355: 17-18.]

[25] Tao Junrong. The Evolution of the Late Cretaceous-Cenozoic Floras in Chinain Chinese[M]. Beijing: Science Press200073-7792-103. [陶君容. 中国晚白垩世至新生代植物区系发展演变[M]. 北京: 科学出版社,200073-7792-103.]

[26] Liang MingmeiWang YufeiLi Chengseng. Palaeovegetation succession and quantitative Palaeoclimate reconstruction of the Miocene Shanwang assemblage [J]. Journal of Palaeogeography200133: 11-20. [梁明媚,王宇飞,李承森. 山旺中新世植被演替及古气候定量研究[J]. 古地理学报,200133: 11-20. ]

[27] Sun QigaoWang YufeiLi Chengsen. The Miocene vegetation succession and environmental changes in Shanwang BasinShandong provinceChina [J]. Earth Science Frontiers200293: 15-23. [孙启高,王宇飞,李承森.中新世山旺盆地植被演替与环境变迁[J].地学前缘,200293: 15-23.]

[28] Sun XiangjunWang Pinxian. How old is the Asian Mosoon System-Palaeobotanical Constraints from China [J]. Journal of Tongji UniversityNatural Science),2005339: 1 137-1 143. [孙湘君,汪品先. 从中国古植被记录看东亚季风的年龄[J]. 同济大学学报: 自然科学版,2005339: 1 137-1 143.]

[29] Xiao LiangSun BainianYan Defeiet al. Cuticular Structure of Quercus pannosa Hand-Mazz. from the Pliocene in BaoshanYunnan province and its palaeoenvironmental significance [J]. Acta Micropalaeontologica Sinica2006231: 23-30. [肖良,孙柏年,阎德飞,等. 云南保山上新统黄背栎Quercus pannosa-Hand-Mazz角质层特征及古环境意义[J]. 微体古生物学报,2006231: 23-30.]

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