Late Triassic Anyuan Flora from Northeast Jiangxi Province, South China
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摘要: 通过对赣东北上饶地区宋村、司铺和东山村3条剖面保存的植物化石全面研究, 讨论了赣东北安源组地层分布特征, 安源植物群的组成、特征及其地质时代.鉴定并统计安源植物群有28属60种, 其中苏铁类及本内苏铁类11属33种, 占植物群总数55.0%, 居植物群首位; 真蕨类5属11种, 占植物群总数18.3%, 居植物群第2位; 种子蕨4属6种, 占植物群总数10.0%;有节类2属3种, 占植物群3.0%, 然而丰度高; 银杏类4属5种, 占8.3%, 松柏类及繁殖器官2属2种, 占3.4%.该植物群归于晚三叠世Ptilozamites-Anthrophyopsis组合.安源植物群组成分子中, 喜湿植物14种, 占植物群23.3%, 耐旱植物46种, 占植物群76.7%, 属于半潮湿型.喜热植物45种, 占植物群75.0%, 广温植物15种, 占植物群25.0%, 属炎热型, 代表中国南方滨海型热带亚热带半潮湿气候.Abstract: The composition, features and geological time of the flora in the Anyuan Formation, Shangrao City, Jiangxi Province have been studied. The fossil plants obtained are identified to be of 60 species belonging to 28 genera: 26 known species, 10 similar species and 24 undetermined species. Of the Anyuan flora, Cycadophytes accounts for 55%, Pteridphytes, 18. 3%, Pteridospermophytes, 10%, Ginkgophytes, 8. 3%, Coniferophytes, 3.4%. The flora should be classified as Ptilozamites-Asthrophyopsis assemblage in the lower part of the Dictyophyllum-Clathropteris series. This important Upper Triassic flora is widely distributed in Sweden, Germany, eastern Greenland, Russia, Vietnam and Japan. In China, it has been found in the Xujiahe Formation of Sichuan, Shazhenxi Formation of Hubei, Lalijian Formation of Anhui, Fanjiatang Formation of Jiangsu, Dakeng Formation of Fujian, Wuzao Formation of Zhejiang and so on. The philotherm of the flora represents hot and semi hu mid climate of South Ch/na coastal areas.
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Key words:
- Irate Triassic /
- Anyuan Formation /
- stratigraphy /
- paleoflora /
- Northeast Jiangxi
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图 4 江西省上饶地区上三叠统安源组三丘田段柱状剖面对比(其他图例同图 3)
Fig. 4. Some columnar sections of the Upper Triassic Anyuan Formation in Shangrao area, Jiangxi Province
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[1] Guo, B. K., Zhang, Y. M., 1959. On the Mesozoic coal series of western Kiangsi. Acta Geologica Sinica, 39(1): 85-93(in Chinese with English abstract). https://en.cnki.com.cn/Article_en/CJFDTOTAL-DZXE195901007.htm [2] He, D. C., Shen, X. P., 1980. Fossil of Mesozoic coal-bearing strata in Hunan and Jiangxi Province, 4: Fossil plants. China Coal Industry Press, Beijing, 1-49(in Chinese). [3] Huang, Q. S., 1995. Paleoclimate and coal-forming characteristics of the Late Triassic Xujiahe stage in northern Sichuan. Geological Review, 41(1): 92-99(in Chinese with English abstract). https://www.sciencedirect.com/science/article/pii/S1871174X15000931 [4] Huang, Q. S., Lu, Z. S., Huang, J. Y., 1998. Early Jurassic Linshan flora from Northeast Jiangxi Province, China. Earth Sciences-Journal of China University of Geosciences, 23 (3): 219-224(in Chinese with English abstract). https://en.cnki.com.cn/Article_en/CJFDTotal-DQKX803.000.htm [5] Huang, T.K., Hsu, K.C., 1936. Mesozoic orogenic movements in the Pinghsiang coalfield, Kiangsi. Bulletin of Geological Society, China, 177-193. [6] Li, P. J., 1964. Fossil plants from the Hsuchiaho series of Kwangyuan, northern Szechuan. Mem. Institute of Geological Paleontology, Academic Sinica, 3: 101-178(in Chinese with English abstract). [7] Si, X.J., 1956. Older Mesozoic plants of the Yenchang Formation, northern Shensi. Palaeonto Sinica, Whole No 139, NSA, 5: 1-217(in Chinese). [8] Si, X. J., Li, X. X., 1963. Mesozoic plants from China. Science Press, Beijing, 1-429(in Chinese). [9] Wu, S. Q., Ye, M. N., Li, B. X., 1980. Upper Triassic and Lower-Middle Jurassic plants from the Hsiangchi Group, western Hubei. Mem. Nanjing Institute of Geological Paleontology, Academic Sinica, 14: 63-131(in Chinese with English abstract). http://www.researchgate.net/publication/269390293_Upper_Triassic_and_Lower_and_Middle_Jurassic_Plants_from_the_Hsiangchi_Group_Western_Hubei [10] Xu, R., Zhu, J. N., Chen, Y., et al., 1979. Late Triassic Baoding flora of China. Science Press, Beijing, 1-130 (in Chinese). [11] Ye, M. N., Liu, X. Y., Huang, G. Q., et al., 1986. Late Triassic and Early-Middle Jurassic fossil plants from Northeast Sichuan. Anhui Science and Technology Publishing House, Hefei, 13-110(in Chinese). [12] Zhou, Z. Y., 1989. Late Triassic plants from Shaqiao, Hengyang, Hunan Province. Palaeontologica Cathayana, 4: 131-197. [13] 郭伯康, 张友明, 1959. 赣西地区中生代含煤沉积. 地质学报, 39(1): 85-93. https://www.cnki.com.cn/Article/CJFDTOTAL-DZXE195901007.htm [14] 何德长, 沈襄鹏, 1980. 湘赣地区中生代含煤地层化石(第四分册: 植物化石). 北京: 煤炭工业出版社, 1-49. [15] 黄其胜, 1995. 川北晚三叠世须家河期古气候及成煤特征. 地质论评, 41(1): 92-99. https://www.cnki.com.cn/Article/CJFDTOTAL-DZLP199501012.htm [16] 黄其胜, 卢宗盛, 黄剑勇, 1998. 赣东北早侏罗世林山植物群. 地球科学- - 中国地质大学学报, 23(3): 219-224. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX803.000.htm [17] 李佩娟, 1964. 四川须家河组植物化石. 中国科学院南京地质古生物所集刊, 3: 101-178. https://cdmd.cnki.com.cn/Article/CDMD-10358-1020092868.htm [18] 斯行健, 1956. 陕北中生代延长层植物群. 中国古生物志, 总号第139册, 新甲种, 5: 1-217. [19] 斯行健, 李星学, 1963. 中国中生代植物. 北京: 科学出版社, 1-149. [20] 吴舜卿, 叶美娜, 厉宝贤, 1980. 鄂西香溪群- - 晚三叠世及早中侏罗世植物化石. 中国科学院南京地质古生物研究所集刊, 14: 63-131. https://www.cnki.com.cn/Article/CJFDTOTAL-LDZK1988S1013.htm [21] 徐仁, 朱家楠, 陈烨, 等, 1979. 中国晚三叠世宝鼎植物群. 北京: 科学出版社, 1-130. [22] 叶美娜, 刘兴义, 黄国清, 等, 1986. 川东北地区晚三叠世及早中侏罗世植物化石. 合肥: 安徽科学技术出版社.