西藏南部吉隆盆地晚中新世—早更新世沃马组介形虫动物群

陈奋宁; 徐亚东; 江尚松; 周修高

doi:10.3799/dqkx.2010.095

Volume 35 Issue 5

Sep. 2010

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CHEN Fen-ning, XU Ya-dong, JIANG Shang-song, ZHOU Xiu-gao, 2010. Late Miocene-Early Pleistocene Ostracoda Fauna of Oma Formation in Gyirong Basin, Southern Tibet. Earth Science, 35(5): 821-827. doi: 10.3799/dqkx.2010.095

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CHEN Fen-ning, XU Ya-dong, JIANG Shang-song, ZHOU Xiu-gao, 2010. Late Miocene-Early Pleistocene Ostracoda Fauna of Oma Formation in Gyirong Basin, Southern Tibet. Earth Science, 35(5): 821-827. doi: 10.3799/dqkx.2010.095

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Late Miocene-Early Pleistocene Ostracoda Fauna of Oma Formation in Gyirong Basin, Southern Tibet

doi: 10.3799/dqkx.2010.095

1.
Xi'an Institute of Geology and Mineral Resources, Xi'an 710054, China
2.
Key Laboratory of Biogeology and Environmental Geology of Ministry of Education, China University of Geosciences, Wuhan 430074, China
3.
Faculty of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2010-05-31
Publish Date: 2010-09-01

Abstract

Abstract

Diverse and abundant ostracoda fossils were found in the Gyirong basin in the south of the Tibet. Our research is based on 37 species of ostracoda including 8 undefined ones that belong to 9 generas. On the basis of the characteristics of ostracoda fossil succession, the ostracoda fauna in this area can be divided into 2 ostracoda assembldges in ascending order as follows: Ilyocypris pentanoda-Qaidamothere vena assembldge and Leucocythere mirabilis-Leucocytherella assembldge. We compared the ostracoda assembldges of Oma Formation with those worldwide at the same stratum and concluded that the age of Oma Formation is Late Miocene to Early Pleistocene.
- Gyirong basin,
- Oma Formation,
- Late Miocene-Early Pleistocene,
- ostracoda assembldge,
- Tibet

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References(24)

References

Exploration and Development Research Institute, Qinghai Petroleum Administration, Nanjing Institute of Geology and Paleontology, Academia Sinica, 1988. Tertiary ostracode fauna from Qaidam basin, China. Nanjing University Press, Nanjing, 22-37 (in Chinese).

Francisco, R., María, G., Manuel, A., et al., 2008. Pliocene ostracods of southwestern Europe ostracodes pliocènes du sud-ouest de l'Europe. Geobios, 41(2008): 845-859. doi: 10.1016/j.geobios.2007.07.004

Harrison, T.M., Copeland, P., Kidd, W.S.F., et al., 1992. Raising Tibet. Science, 255(5052): 1663-1670. doi: 10.1126/science.255.5052.1663

Huang, B.R., 1964. Ostracods from Gansen district, Qaidam basin. Acta Palaeontologica Sinica, 12(2): 241-255, 260-269 (in Chinese).

Huang, B.R., 1984. Ostracodes of Pliocene- and early Pleistocene in Gonghe basin, Qinghai. In: Collections of Nanjing Institute of Geology and Palaeontology, CAS(19). Science Press, Beijing, 1-12 (in Chinese).

Huang, B.R., Yang, H.R., You, K.Y., 1982. Quaternary and Pliocene ostracoda from southwestern and southern in Tibet. In: Sun, H.L., ed., Tibetan plateau series of scientific expedition, paleontology(the fourth fascicle). Science Press, Beijing, 326-348 (in Chinese).

Gengo, T., Shin-ichi, N., 2009. Late Miocene and Pliocene ostracoda from the Shimajiri Group, Kume-jima Island, Japan: biogeographical significance of the timing of the formation of back-arc basin (Okinawa Trough). Palaeogeography, 275(1-4): 56-68. doi: 10.1016/j.palaeo.2009.02.023

Li, Y.G., 1966. Cenozoic ostracoda of Lantian and Weinan in Shaanxi Province. In: Insitute of Vertebrate Paleontology and Paleoanthropology, ed., Corpus of Cenozoic on-site meeting at Lantian, Shaanxi, 255-275 (in Chinese).

Pang, Q.Q., 1980. Late Cenozoic ostracoda fossils and its geological significance at Tanggula Mountain, in the Qinghai-Tibet plateau. Journal of Shijiazhuang University of Economics, 2: 67-77 (in Chinese).

Yang, P., Qiao, Z.Z., Zhang, H.Q., et al., 2006. Features of the Cenozoic ostracod fauna and environmental significance in Qaidam basin. Journal of Palaeogeography, 8(2): 143-156 (in Chinese with English abstract). http://epub.cnki.net/grid2008/docdown/docdownload.aspx?filename=GDLX200602001&dbcode=CJFD&year=2006&dflag=pdfdown

Yin, A., Kapp, P.A., Murphy, M.A., et al., 1999. Significant Late Neogene east-west extension in northern Tibet. Geology, 27: 787-790. doi: 10.1130/0091-7613(1999)027<0787:SLNEWE>2.3.CO;2

Zhang, K.X., Wang, G.C., Chen, F.N., et al., 2007. Coupling between the uplift of Qinghai-Tibet plateau and distribution of basins of Paleogene-Neogene. Earth Science—Journal of China University Geosciences, 32(5): 583―597 (in Chinese with English abstract).

Zhang, K.X., Wang, G.C., Ji, J.L., et al., 2010. Paleogene-Neogene stratigraphic realm and sedimentary sequence of the Qinghai-Tibet plateau and their response to the uplift of the plateau. Science in China (Earth Sciences), 53(9): 1271-1294. doi: 10.1007/s11430-010-4048-2

Zhu, D.G., Meng, X.G., Shao, Z.G., et al., 2007. Evolution of the paleovegetation, paleoenvironment and paleoclimate during Pliocene-Early Pleistocene in Zhada basin, Ali, Tibet. Acta Geologica Sinica, 81(3): 295-306(in Chinese with English abstract). http://www.researchgate.net/publication/285896181_Evolution_of_the_paleovegetation_paleoenvironment_and_paleoclimate_during_Pliocene-early_Pleistocene_in_Zhada_basin_Ali_Tibet

黄宝仁, 1964. 柴达木盆地甘森区介形类化石. 古生物学报, 12(2): 241-255, 260-269. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX196402006.htm

黄宝仁, 1984. 青海共和盆地上新世及早更新世介形类. 见: 中国科学院南京地质古生物研究所集刊(19), 北京: 科学出版社, 1-12.

黄宝仁, 杨恒仁, 尤坤元, 1982. 西藏南部和西南部上新世及第四纪介形类. 见: 孙鸿烈编, 青藏高原科学考察丛书, 西藏古生物(第四分册), 北京: 科学出版社, 326-348.

李友桂, 1966. 陕西蓝田、渭南新生界介形虫化石. 见: 中国科学院古脊椎动物与古人类研究所编, 陕西蓝田新生代地层现场会议编文集, 255-275.

刘超, 王国灿, 王岸, 等, 2007. 喜马拉雅山脉新生代差异隆升的裂变径迹热年代学证据. 地学前缘, 14(6): 273-281. doi: 10.3321/j.issn:1005-2321.2007.06.034

庞其清, 1980. 青藏高原唐古拉山口晚新生代介形虫化石及其地质意义. 石家庄经济学院院报, 2: 67-77. https://www.cnki.com.cn/Article/CJFDTOTAL-HBDX198002004.htm

青海石油管理局勘探开发研究院, 中国科学院南京地质古生物研究所, 1988. 柴达木盆地第三纪介形类动物群. 南京: 南京大学出版社, 22-37.

杨潘, 乔子真, 张海泉, 等, 2006. 柴达木盆地新生代介形类动物群特征及环境意义. 古地理学报, 8(2): 143-156. doi: 10.3969/j.issn.1671-1505.2006.02.001

张克信, 王国灿, 陈奋宁, 等, 2007. 青藏高原古近纪-新近纪隆升与沉积盆地分布耦合. 地球科学—中国地质大学学报, 32(5): 583-597. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX200705002.htm

朱大岗, 孟宪刚, 邵兆刚, 等, 2007. 西藏阿里札达盆地上新世-早更新世的古植被、古环境与古气候演化. 地质学报, 81(3): 295-306. doi: 10.3321/j.issn:0001-5717.2007.03.002

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Late Miocene-Early Pleistocene Ostracoda Fauna of Oma Formation in Gyirong Basin, Southern Tibet

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