贵州青岩地区早-中三叠世生物地层

陈晶; 童金南; 牛志军; 周士钦; 宋海军; 易飞

doi:10.3799/dqkx.2010.006

Volume 35 Issue 1

Jan. 2010

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2010 > 35(1): 51-61

CHEN Jing, TONG Jin-nan, NIU Zhi-jun, ZHOU Shi-qin, SONG Hai-jun, YI Fei, 2010. Lower-Middle Triassic Strata in Qingyan, Guizhou Province, South China. Earth Science, 35(1): 51-61. doi: 10.3799/dqkx.2010.006

Citation:

CHEN Jing, TONG Jin-nan, NIU Zhi-jun, ZHOU Shi-qin, SONG Hai-jun, YI Fei, 2010. Lower-Middle Triassic Strata in Qingyan, Guizhou Province, South China. Earth Science, 35(1): 51-61. doi: 10.3799/dqkx.2010.006

Citation:

PDF( 722 KB)

Lower-Middle Triassic Strata in Qingyan, Guizhou Province, South China

doi: 10.3799/dqkx.2010.006

1.
Key Laboratory of Biogeology and Environmental Geology of the Ministry of Education, China University of Geosciences, Wuhan 430074, China
2.
Yichang Institute of Geology and Mineral Resources, Yichang Centre of Geological Survey, Yichang 443003, China

Received Date: 2009-07-15
Publish Date: 2010-01-01

Abstract

Abstract

The Lower-Middle Triassic strata in Qingyan, Guizhou are well exposed and have abundant fossils. In particular, the Qingyan fauna in Middle Triassic shows biota radiation. The stratigraphical sequence has been studied extensively for a better understanding of the course and pattern of the biotic recovery and radiation following the End-Permian mass extinction. Five conodont zones, including Neospathodus dieneri zone, Neospathodus waageni zone, Neospathodus pingdingshanensis zone, Neospathodus homeri zone, and Chiosella timorensis zone, 2 foraminifer assemblages and 6 bivalve assemblages are recognized. The boudaries of Induan-Olenekian and Olenekian-Anisian have been defined by the conodonts. Various fossils and their ecologic assemblages indicate that the first episode of recovery-radiation after the End-Permian extinction happened in the early Ainisian, and the fossil assemblages in Leidapo Member (Middle Anisian) reveal a typical prosperous biotic ecosystem after radiation. The brachiopod assemblages, Madoia sp. assemblage and Rhaetina angustaeformis assemblage, from the Middle Anisian Qingyan Formation represent the first radiation of brachiopod faunas from the recovery. In addition, the sedimentary evidence indicates two up-shallowing cycles of paleoenvironmental setting, basin-slope-platform-basin-slope-shelf.
- Lower-Middle Triassic,
- biostratigraphy,
- recovery and radiation,
- Qingyan of Guizhou

FullText(HTML)

References(44)

References

Bureau of Geology and Mineral Exploration of Guizhou Province, 1987. Regional geological survey battalion of Guizhou Province. Geological Publishing House, Beijing, 1-500 (in Chinese).

Chen, J.H., Cao, M.Z., Stiller, F., 2001. Preliminary palaeosynecological analyses on the Upper Anisian (Middle Triassic) Qingyan fauna. Acta Palaeontologica Sinica, 40(2): 262-268 (in Chinese with English abstract). http://search.cnki.net/down/default.aspx?filename=GSWX200102011&dbcode=CJFD&year=2001&dflag=pdfdown

Chen, J.H., Stiller, F., Komatsu, T., 2003. A bivalve radiation after the End-Permian extinction. Science Technology and Engineering, 3(5): 415-416, 420 (in Chinese with English abstract). http://www.en.cnki.com.cn/Article_en/CJFDTOTAL-KXJS200305007.htm

Fagerstrom, J.A., 1964. Fossil communities in paleoecology: their recognition and significance. Geological Society of America Buletin., 75: 1197-1216. doi: 10.1130/0016-7606(1964)75[1197:FCIPTR]2.0.CO;2

Gan, X.M., Yin, H.F., 1978. Bivalves. Paleontology Atlas in the southwest area of China, Guizou (Volums 2). Geological Publishing House, Beijing, 305-393 (in Chinese).

Gilinsky, N.L., Bennington, J.B., 1994. Estimating numbers of whole individuals from collections of body parts: a taphonomic limitation of the paleontological record. Paleobiology, 20(2): 245-258. doi: 10.1017/S0094837300012719

Guizhou Working Group of Stratigraphy and Palaeontology, 1977. Regional strata in the southwest area of China. Geological Publishing House, Beijing, 1-384 (in Chinese).

He, Y., 1984. Middle Triassic foraminifera from central and southern Guizhou, China. Acta Palaeontologica Sinica, 23(4): 420-431 (in Chinese with English abstract). http://www.researchgate.net/publication/284937559_Middle_Triassic_foraminifera_from_central_and_southern_Guizhou_China

He, Y., 1988. Early and Middle Triassic foraminifera from Jiangsu and Anhui Provinces, China. Acta Micropalaeontologica Sinica, 5(1): 85-92 (in Chinese with English abstract). http://en.cnki.com.cn/article_en/cjfdtotal-wsgt198801012.htm

He, Y., 1993. Triassic foraminifera from Northeast Sichuan and South Shanxi, China. Acta Palaeontologica Sinica, 32(2): 170-187 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-GSWX199302005.htm

Heath, R.S., Apthorpe, M.C., 1986. Middle and Early (?) Triassic foraminifera from the Northwest shelf, western Australia. Journal of Foraminiferal Research, 16(4): 313-333. doi: 10.2113/gsjfr.16.4.313

Hsu, T.Y., 1943. Triassic formations of Kweichow. Bulletin of the Geological Society of China, 23(3-4): 121-128.

Hsu, T.Y., Chen, K., 1943. Revision of the Chingyen Triassic fauna from Kweichou. Bulletin of the Geological Society of China, 23(3-4): 129-138. http://www.onacademic.com/detail/journal_1000035188065010_c4f7.html

Kobayashi, F., Rossana, M., Roberto, R., et al., 2006. Triassic foraminifers of the Lampang Group (northern Thailand). Journal of Asian Earth Sciences, 27(3): 312-325. doi: 10.1016/j.jseaes.2005.04.003

Koken, E., 1900. Vber triassische Versteinerungen aus China, neues Jahrb. Min. Geol. Paleont., Bd. 1.

Kristan-Tollmann, E., 1983a. Foraminiferen aus dem oberanis von Leidapo bei Guiyang in Suedchina. Mitteilungen der Oesterreichischen Geologischen Gesellschaft, Vienna, 76: 289-323.

Kristan-Tollmann, E., 1983b. Ostracoden aus dem oberanis von Leidapo bei Guiyang in Suedchina. Schriftenreihe der Erdwissenchaftlichen Kommissionen, 5: 121-176. http://www.researchgate.net/publication/285243464_Ostracoden_aus_dem_Oberanis_von_Leidapo_bei_Guiyang_in_Sudchina

Liu, B.J., Zhang, J.Q., Ye, H.Z., 1987. Shelf-slope sedimentary environment of Middle Triassic in Southwest Guiznou. Acta Sedimentologica Sinica, 5(2): 1-13 (in Chinese with English abstract). http://en.cnki.com.cn/Article_en/CJFDTOTAL-CJXB198702000.htm

Stiller, F., 1995. Palaeosynoekologie einer oberanisischen flachmarinen Fossil vergesells chaftung von Leidapo, Guizhou, SW-China. Muenstersche Forschungen zur Geologie und Palaeontologie, 77: 329-356. http://www.researchgate.net/publication/281577441_Palaosynokologie_einer_oberanisischen_flachmarinen_Fossilvergesellschaftung_von_Leidapo_Guizhou_SW-China

Stiller, F., 1999. Neoretziid brachiopods from the Upper Anisian (Middle Triassic) of Qingyan, south-western China. Muenstersche Forschungen zur Geologie und Palaeontologie, 86: 51-68. http://www.researchgate.net/publication/281543485_Scaphopods_from_the_Upper_Anisian_Middle_Triassic_of_Qingyan_south-western_China

Stiller, F., 2000. Two early Millericrinids and an unusual crinoid of uncertain systematic position from the lower Upper Anisian (Middle Triassic) of Qingyan, southwestern China. Journal of Palaeontology, 74(1): 32-51. doi: 10.1666/0022-3360(2000)074<0032:TEMAAU>2.0.CO;2

Stiller, F., Chen, J.H., 2004. Eophilobryoidella sinoanisica new genus and species, an early philobryid bivalve from the Upper Anisian (Middle Triassic) of Qingyan, southwestern China. Journal of Paleontology, 78(2): 414-419. doi: 10.1666/0022-3360(2004)078<0414:ESNGAS>2.0.CO;2

Stiller, F., Chen, J.H., 2006. New Mysidiellidae (Bivalvia) from the Anisian (Middle Triassic) of Qingyan, South-west China. Palaeontology, 49(1): 213-227. doi: 10.1111/j.1475-4983.2005.00524.x

Tong, J.N., 2004. Paleozoic-Mesozoic foraminifera evolution in South China. In: Rong, J.Y., Fang, Z.J., eds., Mass extinction and recovery: evidences from the Palaeozoic and Triassic of South China. Science and Technology of China Press, Hefei, 701-718, 1070 (in Chinese).

Tong, J.N., Huang, S.J., 1992. The development of the Middle Triassic buildup in Gizhou and its geochemical facies. Earth Science—Journal of China University of Geosciences, 17(3): 319-327 (in Chinese with English abstract).

Tong, J.N., Wang, D.H., 2005. Triassic chronostratigraphy and biotic recovery. Advance in Earth Sciences, 20(12): 1321-1326 (in Chinese with English abstract).

Toshifumi, K., Chen, J.H., Cao, M.Z., et al., 2004. Middle Triassic (Anisian) diversified bivalves: depositional environments and bivalve assemblages in the Leidapo Member of the Qingyan Formation, southern China. Palaeogeography, Palaeoclimatology, Palaeoecology, 208(3-4): 207-223. doi: 10.1016/j.palaeo.2004.03.005

Yang, Z.Y., Xu, G.R., 1966. Triassic brachiopods of Central Guizhou (Kweichow) Province, China. Geological Publishing House, Beijing, 1-151 (in Chinese).

Yin, H., Yochelson, E.L., 1983a. Middle Triassic Gastropoda from Qingyan, Guizhou Province, China, 1, Pleurotomariacea and Murchisoniacea. Journal of Paleontology, 57: 162-187. http://jpaleontol.geoscienceworld.org/content/57/1_Part_I/162

Yin, H.F., Yochelson, E.L., 1983b. Middle Triassic Gastropoda from Qingyan, Guizhou Province, China, 2, Trochacea and Neritacea. Journal of Paleontology, 57: 515-538. http://www.onacademic.com/detail/journal_1000038965308410_ca89.html

Yin, H.F., Yochelson, E.L., 1983c. Middle Triassic Gastropoda from Qingyan, Guizhou Province, China, 3, Euomphalacea and Loxonematacea. Journal of Paleontology, 57(5): 1098-1127. http://jpaleontol.geoscienceworld.org/content/57/5/1098

陈金华, 曹美珍, Stiller, F., 2001. 中三叠世青岩生物群的群体古生态学初步研究. 古生物学报, 40(2): 262-268. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200102011.htm

陈金华, Stiller, F., 小松俊文, 2003. 二叠纪末大灭绝后双壳类新的辐射. 科学技术与工程, 3(5): 415-416, 420. https://www.cnki.com.cn/Article/CJFDTOTAL-KXJS200305007.htm

甘修明, 殷鸿福, 1978. 瓣鳃纲. 西南地区古生物图册, 贵州分册(二). 北京: 地质出版社.

贵州省地层古生物工作队, 1977. 西南地区区域地层表, 贵州省分册. 北京: 地质出版社, 1-384.

贵州省地质矿产局, 1987. 贵州省区域地质志. 北京: 地质出版社, 1-500.

何炎, 1984. 黔中、黔南中三叠世有孔虫的发现. 古生物学报, 23(4): 420-431. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX198404003.htm

何炎, 1988. 苏、皖早、中三叠世有孔虫. 微体古生物学报, 5(1): 85-92. https://www.cnki.com.cn/Article/CJFDTOTAL-WSGT198801012.htm

何炎, 1993. 川东北及陕南三叠纪有孔虫. 古生物学报, 32(2): 170-187. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX199302005.htm

刘宝珺, 张锦泉, 叶红专, 1987. 黔西南中三叠世陆棚-斜坡沉积特征. 沉积学报, 5(2): 1-13. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB198702000.htm

童金南, 2004. 华南古生代-中生代之交有孔虫的类群演替. 生物大灭绝与复苏——来自华南古生代和三叠纪的证据. 见: 戎嘉余, 方宗杰. 生物大灭绝与复苏——来自华南古生代和三叠纪的证据. 合肥: 中国科学技术出版社, 701-718, 1070.

童金南, 黄思骥, 1992. 贵州中三叠世岩隆沉积史及地球化学相. 地球科学——中国地质大学学报, 17(3): 319-327. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199203014.htm

童金南, 王德辉, 2005. 三叠纪年代地层与生物复苏. 地球科学进展, 20(12): 1321-1326. https://www.cnki.com.cn/Article/CJFDTOTAL-DXJZ200512006.htm

杨遵仪, 徐桂荣, 1966. 贵州中部中上三叠统腕足类. 北京: 中国工业出版社, 1-151.

Relative Articles

Supplements(0)

Cited By

Proportional views

Proportional views

通讯作者: 陈斌, bchen63@163.com

1.
沈阳化工大学材料科学与工程学院沈阳 110142

Figures(2)

Get Citation

PDF

XML

Article views (3790) PDF downloads(153)

Lower-Middle Triassic Strata in Qingyan, Guizhou Province, South China

doi: 10.3799/dqkx.2010.006

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content