浅析P/T界线层中牙形刺Hindeodus parvus的标准性
Brief Analysis on Setting Criterion of Conodont Hindeodus parvus in P/T Boundary

作者: 林联盛 , 方 豫 :江西省山江湖开发治理委员会办公室,南昌;江西省遥感信息系统中心,南昌; 万 梦 :江西省地质矿产勘查开发局916大队,九江;

关键词: 牙形刺Hindeodus parvus二叠纪/三叠纪生物地层界线Hindeodus parvus Permian/Triassic Biostratigraphic Boundary

摘要:
本文讨论了中国(江西修水东岭、四川广元上寺和浙江长兴煤山)、印度(克什米尔Guryul Ravine)、前苏联(阿塞拜疆Achura)等地的海相P/T界线层中牙形刺Hindeodus parvus,及其首次出现的点位,阐述了其标准性对海相P/T界线划分的重要意义。建议以产于单相且沉积连续剖面,主齿和细齿均保存完好的Hindeodus parvus的首次出现的点位,作为P/T生物地层界线划分的标准。

Abstract: The article discusses the Conodont Hindeodus parvus in marine P/T boundary layer in China (Dongling Village of Xiushui County, Jiangxi Province; Shangsi Village of Guangyuan City, Sichuan Province; Meishan Town of Changxing County, Zhejiang Province), India (Kashmir Guryul Ravine), and Union of Soviet Socialist Republics (Azerbaijan Achura), and the point location where they appear for the first time. It also explains the important significance of setting criterion for demar-cating marine P/T boundary layer, suggesting that the partition criterion for P/T biostratigraphic boundary would be set on the point locations where they firstly appear in single-phase sediment- successive section, with well-preserved cardinal tooth and serration of Hindeodus parvus.

文章引用: 林联盛 , 万 梦 , 方 豫 (2014) 浅析P/T界线层中牙形刺Hindeodus parvus的标准性。 自然科学, 2, 25-31. doi: 10.12677/OJNS.2014.23005

参考文献

[1] Waterhouse, J.B. (1973) An ophiceratid ammonoid from the New Zealand Permian and its implication for the Permian- Triassic boundary. Geology Magazine, 110, 305-329.

[2] Bando, Y., Bhart, D.K., et al. (1980) Some remarks on the conodont zonation and stratigraphy of the Permian. Recent Researches in Geology, 8, 1-53.

[3] Sweet, W.C. (1979) Graphic correlation of Permian-Triassic rocks in Kashmir, Pakistan and Iran. Geological et Palaeontologica, 13, 239-248.

[4] Yin, H.F., Yang, F.Q., Zhang, K.X., et al. (1988) A proposal to the biostratigraphic criterion of Per-mian-Triassic boundary. Memorie della Societa Geologica Italiana, 34, 329-344.

[5] (2000) 全球二叠--三叠纪界线层型剖面正式通过投票. http://www.cgs.gov.cn/dzzs/jdz/2003111801.htm

[6] 朱相水, 王成源 (1994) 江西二叠–三叠系界线. 微体古生物学报, 4, 439-452.

[7] 朱相水, 林联盛 (1996) 推荐一条GSSP的辅助剖面. 江西师范大学学报(自然科学版), 3, 264-268.

[8] 朱相水, 林联盛 (1997) 典型Hindeodus parvus及其意义—兼论二叠–三叠系界线. 江西师范大学学报(自然科学版), 1, 88-95.

[9] 朱相水, 林联盛 (1997) Hindeodus parvus及其“首次出现”. 江西师范大学学报(自然科学版), 3, 269-274.

[10] Kozur, H. and Pjatakova, M. (1976) Die Con-odontanart Anchignathodus parvus n. sp., Eine Wichtige Leitform der Basalen Trias. Koninkl. Nederl. Akademie van Wetenschappen-Amsterdam, Proceeding, Series B, 79, 123-128.

[11] Kozur, H. (1977) Revision der Conodontengatung Anchignathodus und irer Typusart. Zeitschrift für Geologische Wissenschaften, 9, 1113-1127.

[12] Kozur, H. (1989) Significance of events in conodont evolution for the Permian and Triassic stratigraphy. Courier Forschungsinstitut. Senckenberg, 117, 385-408.

[13] Matsuda, T. (1981) Early Triassic conodonts from Kashmir, India. Part 1: Hindeodus and isarcicella. Journal of Geosciences, Osaka City University, 24, 75-108.

[14] Wang, C.Y. (1990) Some problems on the guryul ravine section of Kashmir as Permian-Triassic boundary stratotype. Palaeontologia Cathayana, 5, 263-265.

[15] Yin, H.F. (1994) Reassessment of the index fossils at the Paleozoic-Mesozonic boundary. In: Jin, Y.G., et al., Eds., Permian Stratigraphy, Environments and Resources, Vol. 1: Palaeontology and Stratigraphy, Palaeoword, 4, Nanjing University Press, Nanjing, 234-248.

[16] 王志浩, 戴进业 (1981) 四川江油、北川地区三叠纪牙形刺. 古生物学报, 2, 138-150.

[17] 张景华, 戴进业, 田树刚 (1984) 四川北部广元上寺晚二叠世——早三叠世的牙形石生物地层. 国际交流地质学术论文集——为27届国际地质大会撰写, 1, 136-178.

[18] 张克信 (1984) 浙江长兴葆青剖面Otoceras层中牙形动物群的新资料. 地球科学——武汉地质学院学报, 3, 38.

[19] 张克信 (1987) 浙江长兴地区二叠纪与三叠纪之交牙形石动物群及地层意义. 地球科学——武汉地质学院学报, 2, 193-200.

[20] 王成源, 王志浩 (1981) 浙江长兴地区二叠纪龙塘组、长兴组牙形刺及其生态和地层意义. 中国微体古生物学会第一次学术会议论文选集, 科学出版社, 北京, 114-120.

[21] 王成源, 主编 (1993) 下扬子地区牙形刺——生物地层与有机变质成熟度的指标. 科学出版社, 北京, 1-326.

[22] 王成源 (1995) 二叠-三叠系界线层的牙形刺与生物地层界线. 古生物学报, 2, 129-151.

[23] 盛金章, 陈楚震等 (1983) 浙江长兴地区二叠纪与三叠纪界线层型研究. 地层学杂志, 4, 245-257.

分享
Top