贵州册亨中三叠统坡段组巨鲕特征及其环境指示意义

赵俊杰; 黄云飞; 田力; 黄子航; 王延达; 吉霞; 张世岩; 童金南

doi:10.3799/dqkx.2023.087

Volume 48 Issue 8

Aug. 2023

Turn off MathJax

Article Contents

Article Navigation > Earth Science > 2023 > 48(8): 2822-2836

Zhao Junjie, Huang Yunfei, Tian Li, Huang Zihang, Wang Yanda, Ji Xia, Zhang Shiyan, Tong Jinnan, 2023. The Characteristics of Giant Ooids from the Poduan Formation during the Early Middle Triassic and Its Environmental Significance at Poduan Section, Ceheng, Guizhou Province. Earth Science, 48(8): 2822-2836. doi: 10.3799/dqkx.2023.087

Citation:

Zhao Junjie, Huang Yunfei, Tian Li, Huang Zihang, Wang Yanda, Ji Xia, Zhang Shiyan, Tong Jinnan, 2023. The Characteristics of Giant Ooids from the Poduan Formation during the Early Middle Triassic and Its Environmental Significance at Poduan Section, Ceheng, Guizhou Province. Earth Science, 48(8): 2822-2836. doi: 10.3799/dqkx.2023.087

Citation:

Zhao Junjie, Huang Yunfei, Tian Li, Huang Zihang, Wang Yanda, Ji Xia, Zhang Shiyan, Tong Jinnan, 2023. The Characteristics of Giant Ooids from the Poduan Formation during the Early Middle Triassic and Its Environmental Significance at Poduan Section, Ceheng, Guizhou Province. Earth Science, 48(8): 2822-2836. doi: 10.3799/dqkx.2023.087

PDF( 34389 KB)

The Characteristics of Giant Ooids from the Poduan Formation during the Early Middle Triassic and Its Environmental Significance at Poduan Section, Ceheng, Guizhou Province

doi: 10.3799/dqkx.2023.087

1.
School of Geosciences, Yangtze University, Wuhan 430100, China
2.
State Key Laboratory of Biogeology and Environmental Geology, China University of Geosciences, Wuhan 430074, China
3.
School of Earth Sciences, China University of Geosciences, Wuhan 430074, China

Received Date: 2023-01-30
Publish Date: 2023-08-25

Abstract

Abstract

Giant ooids have been considered as abnormal sediment and distributed globally in the aftermath of the end-Permian mass extinction, and represent a marine carbonate supersaturated state which is unfavourable to the survival of metazoans. The marine environment returned to normal in the early Middle Triassic when abnormal sediments became rare. However, the discovery of giant ooids in the early Middle Triassic at the Poduan section, Ceheng, Guizhou Province, could give us more insights into the marine environmental conditions during that time. In this study, the sedimentary microfacies and fabrics of the carbonate rocks at the bottom of the Poduan section were analyzed. The sedimentary environments of the giant ooid-bearing beds were comprehensively studied based on the oolitic characteristics, oolitic content, bioclastic content and sedimentary microfacies. It can be considered that there are two oolitic enrichment periods. Four kinds of oolitic grains have been found at the Poduan section, including common concentric oolitic grains, giant concentric oolitic grains, polycrystalline oolitic grains and mud crystal oolitic grains. Four sedimentary microfacies were identified based on rock structure and carbonate particle characteristics and could represent the interbedded deposition of platform margin oolitic shoal and bioclastic shoal. The development of giant ooids in this area indicated that the marine carbonate saturation is still very high and the abnormal marine environment occurred in this area during the early Middle Triassic. It suggests that there were obvious regional differences in the global marine environment during the Middle Triassic, which is an important reason for the complexity of the model of biotic recovery and radiation.
- Middle Triassic,
- giant ooids,
- biotic recovery,
- sedimentary microfacies,
- higher carbonate saturation state,
- sedimentology

FullText(HTML)

References(97)

References

Algeo, T. J., Kuwahara, K., Sano, H., et al., 2011. Spatial Variation in Sediment fluxes, Redox Conditions, and Productivity in the Permian-Triassic Panthalassic Ocean. Palaeogeography, Palaeoclimatology, Palaeoecology, 308(1-2): 65-83. https://doi.org/10.1016/j.palaeo.2010.07.007

Benton, M. J., 2018. Hyperthermal-Driven Mass Extinctions: Killing Models during the Permian-Triassic Mass Extinction. Philosophical Transactions of the Royal Society A: Mathematical, Physical and Engineering Sciences, 376(2130): 20170076. https://doi.org/10.1098/rsta.2017.0076

Bo, J. F., Yao J. X., Xiao, J. F., et al., 2017. Scleractinian Coral and Conodont Biostratigraphy of the Middle-Upper Part of the Poduan Formation in Ceheng, Guizhou Province, South China. Acta Geologic Sinica, 91(2): 487-497 (in Chinese with English abstract).

Bottjer, D. J., Clapham, M. E., Fraiser, M. L., et al., 2008. Understanding Mechanisms for the End-Permian Mass Extinction and the Protracted Early Triassic Aftermath and Recovery. GSA Today, 18(9): 4. https://doi.org/10.1130/gsatg8a.1

Bustos-Serrano, H., Morse, J. W., Millero, F. J., 2009. The Formation of Whitings on the Little Bahama Bank. Marine Chemistry, 113(1/2): 1-8. https://doi.org/10.1016/j.marchem.2008.10.006

Chatalov, A., 2005a. Aragonitic-Calcitic Ooids from Lower to Middle Triassic Peritidal Sediments in the Western Balkanides, Bulgaria. Neues Jahrbuch für Geologie und Paläontologie-Abhandlungen, 237(1): 87-110. https://doi.org/10.1127/njgpa/237/2005/87

Chatalov, A., 2005b. Monomineralic Carbonate Ooid Types in the Triassic Sediments from Northwestern Bulgaria. Geologica Balcanica, 35(1/2): 63-91. https://doi.org/10.52321/geolbalc.35.1-2.63

Chen, Z. Q., Benton, M. J., 2012. The Timing and Pattern of Biotic Recovery Following the End-Permian Mass Extinction. Nature Geoscience, 5(6): 375-383. https://doi.org/10.1038/ngeo1475

Chen, Z. Q., Huang, Y. G., 2022. How to Evaluate Quantitatively Collapse and Recovery Processes of Ecosystems During and After Mass Extinctions? Earth Science, 47(10): 3827-3829 (in Chinese with English abstract).

Clarkson, M. O., Kasemann, S. A., Wood, R. A., et al., 2015. Ocean Acidification and the Permo-Triassic Mass Extinction. Science, 348(6231): 229-232. https://doi.org/10.1126/science.aaa0193

Dal Corso, J., Song, H. J., Callegaro, S., et al., 2022. Environmental Crises at the Permian-Triassic Mass Extinction. Nature Reviews Earth & Environment, 3(3): 197-214. https://doi.org/10.1038/s43017-021-00259-4

Erwin, D. H., 1994. The Permo-Triassic Extinction. Nature, 367(6460): 231-236. https://doi.org/10.1038/367231a0

Fan, J. S., Wu, Y. S., 2002. Sedimentary Characteristics and Environments of the Poduan Formation of Middle Triassic in Guanling of Guizhou Province. Journal of Palaeogeography, 4(1): 67-74+101-104 (in Chinese with English abstract). doi: 10.3969/j.issn.1671-1505.2002.01.008

Fan, J. X., Shen, S. Z., Erwin, D. H., et al., 2020. A High-Resolution Summary of Cambrian to Early Triassic Marine Invertebrate Biodiversity. Science, 367(6475): 272-277. https://doi.org/10.1126/science.aax4953

Feng, Z. Z., Bao, Z. D., Li, S. W., 1997. Lithofacies Palaeogeography of Middle and Lower Triassic of South China. Petroleum Industry Press, Beijing, 222 (in Chinese).

Flügel, E., 2004. Microfacies of Carbonate Rocks: Analysis, Interpretation and Application Ⅱ. Springer-Verlag, Berlin, 976.

Gao, D., Hu, M. Y., Li, A. P., et al., 2021. High-Frequency Sequence and Microfacies and Their Impacts on Favorable Reservoir of Longwangmiao Formation in Central Sichuan Basin. Earth Science, 46(10): 3520-3534 (in Chinese with English abstract).

Groves, J. R., Altiner, D., Rettori, R., 2005. Extinction, Survival, and Recovery of Lagenide Foraminifers in the Permian-Triassic Boundary Interval, Central Taurides, Turkey. Journal of Paleontology, 79(sp62): 1-38. https://doi.org/10.1666/0022-3360(2005)79[1:ESAROL]2.0.CO;2.

Hu, S. X., Zhang, Q. Y., Chen, Z. Q., et al., 2010. The Luoping Biota: Exceptional Preservation, and New Evidence on the Triassic Recovery from End-Permian Mass Extinction. Proceedings of the Royal Society B: Biological Sciences, 278(1716): 2274-2282. https://doi.org/10.1098/rspb.2010.2235

Huang, Y. G., Chen, Z. Q., Wignall, P. B., et al., 2016. Latest Permian to Middle Triassic Redox Condition Variations in Ramp Settings, South China: Pyrite Framboid Evidence. Geological Society of America Bulletin, 129(1/2): 229-243. https://doi.org/10.1130/b31458.1

Huang, Y. G., Chen, Z. Q., Wu, S. Q., et al., 2022. Anisian (Middle Triassic) Stromatolites from Southwest China: Biogeological Features and Implications for Variations of Filament Size and Diversity of Triassic Cyanobacteria. Palaeogeography, Palaeoclimatology, Palaeoecology, 601: 111150. https://doi.org/10.1016/j.palaeo.2022.111150

Hinojosa, J. L., Brown, S. T., Chen, J., et al., 2012. Evidence for End-Permian Ocean Acidification from Calcium Isotopes in Biogenic Apatite. Geology, 40(8): 743-746. https://doi.org/10.1130/g33048.1

Ji, G. F., Fang, H., Shi, Z. Q., et al., 2016. Characteristics and Geological Significance ofthe Late Triassic Carnian oolitic Limestone in Hanwang area, Northwest Sichuan Basin, China. Journal of Chengdu University ofTechnology (Science & TechnologyEdition), 43(1): 68-76(in Chinese with English abstract).

Jiang, L. Q., Feely, R. A., Carter, B. R., et al., 2015. Climatological Distribution of Aragonite Saturation State in the Global Oceans. Global Biogeochemical Cycles, 29(10): 1656-1673. https://doi.org/10.1002/2015gb005198

Jin, Z. K., Shi, L., Gao, B. S., et al., 2013. Carbonate Facies and Facies Models. Acta Sedimentologica Sinica, 31(6): 965-979 (in Chinese with English abstract).

Kump, L. R., Pavlov, A., Arthur, M. A., 2005. Massive Release of Hydrogen Sulfide to the Surface Ocean and Atmosphere during Intervals of Oceanic Anoxia. Geology, 33(5): 397-400. https://doi.org/10.1130/G21295.1

Lau, K. V., Maher, K., Altiner, D., et al., 2016. Marine Anoxia and Delayed Earth System Recovery after the End-Permian Extinction. Proceedings of the National Academy of Sciences, 113(9): 2360-2365. https://doi.org/10.1073/pnas.1515080113

Lehrmann, D. J., Enos, P., Payne, J. L., et al., 2005. Permian and Triassic Depositional History of the Yangtze Platform and Great Bank of Guizhou in the Nanpanjiang Basin of Guizhou and Guangxi, South China. Albertiana, 33(1): 149-168.

Lehrmann, D. J., Payne, J. L., Pei, D. H., et al., 2007. Record of the End-Permian Extinction and Triassic Biotic Recovery in the Chongzuo-Pingguo Platform, Southern Nanpanjiang Basin, Guangxi, South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 252(1/2): 200-217. https://doi.org/10.1016/j.palaeo.2006.11.044

Lehrmann, D. J., Minzoni, M., Li, X. W., et al., 2012. Lower Triassic Oolites of the Nanpanjiang Basin, South China: facies Architecture, Giant ooids, and Diagenesis-Implications for Hydrocarbon Reservoirs Geologic Note. American Association of Petroleum Geologists Bulletin, 96(8): 1389-1414. https://doi.org/10.1306 /01231211148 doi: 10.1306/01231211148

Li, F., Wang, X., Xue, W. Q., et al., 2010. Origin and Enviromental Significance of Giant Ooids in the Early Triassic, a new kind of Anachronistic Facies. Acta Sedimentologica Sinica, 28(3): 585-595(in Chinese with English abstract).

Li, F., Yan, J. X., Algeo, T., et al., 2013. Paleoceanographic Conditions Following the End-Permian Mass Extinction Recorded by Giant Ooids (Moyang, South China). Global and Planetary Change, 105(3-4): 102-120. https://doi.org/10.1016/j.gloplacha.2011.09.009

Li, F., Yan, J. X., Chen, Z. Q., et al., 2015. Global Oolite Deposits Across the Permian-Triassic Boundary: A Synthesis and Implications for Palaeoceanography Immediately after the End-Permian Biocrisis. Earth-Science Reviews, 149: 163-180. https://doi.org/10.1016/j.earscirev.2014.12.006

Li, F., Yi, C. H., Li, H., et al., 2022. Recent Advances in Ooid Microbial Origin: A Review. Acta Sedimentologica Sinica, 40(2): 319-334 (in Chinese with English abstract).

Li, X. W., Trower, E. J., Lehrmann, D. J., et al., 2021. Implications of Giant Ooids for the Carbonate Chemistry of Early Triassic Seawater. Geology, 49(2): 156-161. https://doi.org/10.1130/g47655.1

Liu, Z. L., Tong, J. L., 2001. The Middle Triassic Stratigraphy and Sedimentary Paleogeography of South China. Acta Sedimentologica Sinica, 19(3): 327-332+356 (in Chinese with English abstract).

Liu, J., Sander, P. M., 2019. The Vossenveld Formation and Biotic Recovery from the Permo-Triassic Extinction. Grondboor & Hamer, 16(73): 147-152.

Luo, M., Chen, Z. Q., Zhao, L. S., et al., 2014. Early Middle Triassic Stromatolites from the Luoping Area, Yunnan Province, Southwest China: Geobiologic Features and Environmental Implications. Palaeogeography, Palaeoclimatology, Palaeoecology, 412(Special Issue): 124-140. https://doi.org/10.1016/j.palaeo.2014.07.028

Mary, M., Woods, A. D., 2008. Stromatolites of the Lower Triassic Union Wash Formation, CA: Evidence for Continued Post-Extinction Environmental Stress in Western North America through the Spathian. Palaeogeography, Palaeoclimatology, Palaeoecology, 261(1/2): 78-86. https://doi.org/10.1016/j.palaeo.2008.01.008

Mei, M. X., 2008. Implication for the Unusual Giant Oolites of the Phanerozoic and Their Morphological Diversity: A Case Study from the Triassic Daye Fomation at the Lichuan Section in Hubei Province South China. Geoscience, 22(5): 683-698 (in Chinese with English abstract).

Mei, M. X., 2012. Brief Introduction on New Advances on the Origin of Ooids. Acta Sedimentologica Sinica, 30(1): 20-32 (in Chinese with English abstract).

Payne, J. L., Lehrmann, D. J., Wei, J., et al., 2004. Large Perturbations of the Carbon Cycle during Recovery from the End-Permian Extinction. Science, 305(5683): 506-509. https://doi.org/10.1126/science.1097023

Payne, J. L., 2005. Evolutionary Dynamics of Gastropod Size Across the End-Permian Extinction and through the Triassic Recovery Interval. Paleobiology, 31(2): 269-290. https://doi.org/10.1666/0094-8373(2005)031[0269:edogsa]2.0.co;2

Payne, J. L., Lehrmann, D. J., Wei, J., et al., 2006. The Pattern and Timing of Biotic Recovery from the End-Permian Extinction on the Great Bank of Guizhou, Guizhou Province, China. Palaios, 21(1): 63-85. https://doi.org/10.2110/palo.2005.p05-12p

Pei, Y., Duda, J. P., Schönig, J., et al., 2021. Late Anisian Microbe-Metazoan Build-Ups in the Germanic Basin: Aftermath of the Permian-Triassic Crisis. Lethaia, 54: 823-844. https://doi.org/10.1111/let.12442

Sedlacek, A., 2013. Srontium Isotope Stratigraphy and Carbonate Sedimentology of the latest Permian to Early Triassic in the Western United States, Northern Iran and Southern China(Dissertation), Ohio State University, Ohio, 159.

Shen, S. Z., Zhang, H., 2017. What Caused the Five Mass Extinctions? China Science Bulletin, 62(11): 1119-1135(in Chinese). doi: 10.1360/N972017-00013

Shi, Z. Q., An, H. Y., Yi, H. S., et al., 2011. Classification and Characters of the Early Triassic Anomalous Carbonate Rocks in Upper Yangtze Area. Journal of Palaeogeography, 13(1): 1-10(in Chinese with English abstract).

Simone, L., 1981. Ooids: a Review. Earth-Science Reviews, 16: 319-355. https://doi.org/10.1016/0012-8252(80)90053-7

Song, H. J., Wignall, P. B., Chu, D. L., et al., 2014. Anoxia/high Temperature Double Whammy during the Permian-Triassic Marine Crisis and its Aftermath. Scientific Reports, 4(1): 1-7. https://doi.org/10.1038/srep04132

Song, H. J., Tong, J. N., Xiong, Y. L., et al., 2012. The Large Increase of δ ¹³C Carb-Depth Gradient and the End-Permian Mass Extinction. Science China Earth Sciences, 55(7): 1101-1109. https://doi.org/10.1007/s11430-012-4416-1

Song, H. J., Tong, J. N., 2016. Mass Extinction and Survival during the Permian-Triassic Crisis. Earth Sciences, 41(6): 901-918(in Chinese with English abstract).

Song, H., Wignall, P. B., Dunhill, A. M., 2018. Decoupled Taxonomic and Ecological Recoveries from the Permo-Triassic Extinction. Science Advances, 4(10): eaat5091. https://doi.org/10.1126/sciadv.aat5091

Song, H. J., Huang, S., Jia, E. H., et al., 2020. Flat Latitudinal Diversity Gradient Caused by the Permian-Triassic Mass Extinction. Proceedings of the National Academy of Sciences, 117(30): 17578-17583. https://doi.org/10.1073/pnas.1918953117

Song, H. J., Song, H. Y., Tong, J. N., et al., 2021. Conodont Calcium Isotopic Evidence for Multiple Shelf Acidification Events during the Early Triassic. Chemical Geology, 562(1): 120038. https://doi.org/10.1016/j.chemgeo.2020.120038

Summer, D. A., Grotzinger, J. P., 1993. Numerical Modeling of Ooid Size and the Problem of Neoproterozoic Giant Ooids. Joumal of Sedimentary Petrology, 63: 974-982. https://doi.org/10.1306/d4267c5d-2b26-11d7-8648000102c1865d

Richter, D. K., 1983. Calcareous Ooids: a Synopsis. In: Peryt, T. M., ed., Coated Grains. Springer-Verlag, Berlin, 71-99.

Tan, X. C., Li, L., Liu, H., et al., 2013. Mega-Shoaling in Carbonate Platform of the Middle Triassic Leikoupo Formation, Sichuan Basin, Southwest China. Science China Earth Sciences, 57(3): 465-479. https://doi.org/10.1007/s11430-013-4667-5

Tang, R. C., Li, R., Wang, Y., 2018. Sedimentary Characteristics of the Middle Triassic Longtou Formation in Guizhou Province, South China: Implications for Sea-Level Change. Journal of Palaeogeography, 20(3): 389-408(in Chinese with English abstract).

Tian, L., Tong, J. N., Sun, D. Y., et al., 2014. The Microfacies and Sedimentary Responses to the Mass Extinction during the Permian-Triassic Transition at Yangou Section, Jiangxi Province, South China. Science China Earth Sciences, 57(9): 2195-2207. https://doi.org/10.1007/s11430-014-4869-5

Tian, L., Bottjer, D. J., Tong, J., et al., 2015. Distribution and Size Variation of Ooids in the Aftermath of the Permian-Triassic Mass Extinction. Palaios, 30(9): 714-727. https://doi.org/10.2110/palo.2014.110

Tong, J. N., Yin, H. F., 2002. The Lower Triassic of South China. Journal of Asian Earth Sciences, 20(7): 803-815. https://doi.org/10.1016/s1367-9120(1)00058-x

Tong, J. N., Yin, H. F., 2009. Advance in the Study of Early Triassic Life and Environment. Acta Palaeontologica Sinica, 48(3): 497-508(in Chinese with English abstract). doi: 10.3969/j.issn.0001-6616.2009.03.020

Trotter, J. A., Williams, I. S., Nicora, A., et al., 2015. Long-Term Cycles of Triassic Climate Change: A New Δ¹⁸O Record from Conodont Apatite. Earth and Planetary Science Letters, 415(2): 165-174. https://doi.org/10.1016/j.epsl.2015.01.038

Trower, E. J., Lamb, M. P., Fischer, W. W., 2017. Experimental Evidence that Ooid Size Reflects a Dynamic Equilibrium between Rapid Precipitation and Abrasion Rates. Earth and Planetary Science Letters, 468(1): 112-118. https://doi.org/10.1016/j.epsl.2017.04.004

Trower, E. J., Lamb, M. P., Cantine, M. D., et al., 2018. Active Ooid Growth Driven by Sediment Transport in a HighLamb, M. P., Energy Shoal, Little Ambergris Cay, Turks and Caicos Islands. Journal of Sedimentary Research, 88(9): 1132-1151. https://doi.org/10.2110/jsr.2018.59

Trower, E. J., Smith, B. P., Koeshidayatullah, A. I., et al., 2022. Marine Ooid Sizes Record Phanerozoic Seawater Carbonate Chemistry. Geophysical Research Letters, 49(22): e2022GL100800. https://doi.org/10.1029/2022gl100800

Tucker, M. E., Wright, V. P., 1990. Carbonate Sedimentology. Blackwell Sciences, Oxford, 482.

Varkouhi, S., Jaques Ribeiro, L. M., 2020. Bimineralic Middle Triassic Ooids from Hydra Island: Diagenetic Pathways and Implications for Ancient Seawater Geochemistry. The Depositional Record, 7(2): 344-369. https://doi.org/10.1002/dep2.117

Wang, L. T., 1999. Discussion on Mid-Triassic Ecological Differentiation in Guizhou. Guizhou Geology, 16(1): 17-21 (in Chinese with English abstract).

Wilson, J. L., 1975. Carbonate Facies in Geologic History. Springer-Verlag, Berlin, 471.

Woods, A. D., 2013. Microbial Ooids and Cortoids from the Lower Triassic (Spathian) Virgin Limestone, Nevada, USA: Evidence for an Early Triassic Microbial Bloom in Shallow Depositional Environments. Global and Planetary Change, 105(4-5): 91-101. https://doi.org/10.1016/j.gloplacha.2012.07.011

Xiong, X. Q., Huang, Y. F., Tong, J. N., 2010. Triassic Bivalve Biostratigraphic Sequence in Zunyi, ‚Guizhou Province. Geological Science and Technology Information, 29(6): 7-14 (in Chinese with English abstract).

Xu, G. R., 1992. Middle Triassic Dasycladaceae from Bazichang of Guanling, Guizhou Province. Earth Science, 17(5): 503-511 (in Chinese with English abstract).

Zhao, X. M., Tong, J. N., Yao, H. Z., et al., 2008. Anachronistic Facies in the Lower Triassic of South China and their Implications to the Ecosystems during the Recovery Time. Science in China Series D: Earth Sciences, 51(11): 1646-1657. https://doi.org/10.1007/s11430-008-0128-y

薄婧方, 姚建新, 肖加飞, 等, 2017. 贵州册亨中三叠统坡段组中上部石珊瑚及牙形石生物地层. 地质学报, 91(2): 487-497. doi: 10.3969/j.issn.0001-5717.2017.02.014

陈中强, 黄元耕. 2022. 如何定量评价大灭绝时期生态系统的坍塌与重建过程? 地球科学, 47(10): 3827-3829. doi: 10.3799/dqkx.2022.827

范嘉松, 吴亚生, 2002. 贵州关岭中三叠统坡段组沉积特征及其形成环境. 古地理学报, 4(1), 67-74+101-104. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX200201010.htm

冯增昭, 鲍志东, 李尚武, 1997. 中国南方早中三叠世岩相古地理. 石油工业出版社, 北京, 222页. https://cdmd.cnki.com.cn/Article/CDMD-10424-1012277311.htm

高达, 胡明毅, 李安鹏, 等, 2021. 川中地区龙王庙组高频层序与沉积微相及其对有利储层的控制. 地球科学, 46(10): 3520-3524. doi: 10.3799/dqkx.2020.382

姬国锋, 范鸿, 时志强, 等, 2016. 川西北汉旺地区卡尼期鲕粒灰岩特征及地质意义. 成都理工大学学报(自然科学版), 43(1): 68-76. https://www.cnki.com.cn/Article/CJFDTOTAL-CDLG201601007.htm

金振奎, 石良, 高白水, 等, 2013. 碳酸盐岩沉积相及相模式. 沉积学报, 31(6): 965-979. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201306003.htm

李飞, 王夏, 薛武强, 等, 2010. 一种新的错时相沉积物-巨鲕及其环境意义. 沉积学报, 28(3): 585-595. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201003024.htm

李飞, 易楚恒, 李红, 等, 2022. 微生物成因鲕粒研究进展. 沉积学报, 40(2): 319-334. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB202202003.htm

刘志丽, 童金南. 2001. 中国南方中三叠世地层及沉积古地理分异. 沉积学报, 19(3): 327-332+356. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB200103001.htm

梅冥相, 2008. 显生宙罕见的巨鲕及其鲕粒形态多样性的意义: 以湖北利川下三叠统大冶组为例. 现代地质, 22(5): 683-698. https://www.cnki.com.cn/Article/CJFDTOTAL-XDDZ200805001.htm

梅冥相, 2012. 鲕粒成因研究的新进展. 沉积学报, 30(1): 20-32. https://www.cnki.com.cn/Article/CJFDTOTAL-CJXB201201003.htm

时志强, 安红艳, 伊海生, 等, 2011. 上扬子地区早三叠世异常碳酸盐岩的分类与特征. 古地理学报, 13(1): 1-10. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201101003.htm

沈树忠, 张华, 2017. 什么引起五次生物大灭绝?科学通报, 62(11): 1119-1135. https://www.cnki.com.cn/Article/CJFDTOTAL-KXTB201711007.htm

宋海军, 童金南, 2016. 二叠纪-三叠纪之交生物大灭绝与残存. 地球科学, 41(6): 901-918. doi: 10.3799/dqkx.2016.077

谭睿昶, 李荣, 王垚, 2018. 贵州地区中三叠统垄头组沉积特征及其海平面变化意义. 古地理学报, 20(3): 389-408. https://www.cnki.com.cn/Article/CJFDTOTAL-GDLX201803004.htm

谭秀成, 李凌, 刘宏, 等. 2014. 四川盆地中三叠统雷口坡组碳酸盐台地巨型浅滩化研究. 中国科学: 地球科学, 44: 457-471. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK201403007.htm

童金南, 殷鸿福, 2009. 早三叠世生物与环境研究进展. 古生物学报, 48(3): 497-508. https://www.cnki.com.cn/Article/CJFDTOTAL-GSWX200903019.htm

王立亭, 1999. 贵州中三叠世生物生态分异初探. 贵州地质, 16(1): 17-21. https://www.cnki.com.cn/Article/CJFDTOTAL-GZDZ199901002.htm

熊鑫琪, 黄云飞, 童金南, 2010. 贵州遵义地区早-中三叠世双壳类生物地层研究. 地质科技情报, 29(6): 7-14. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201006002.htm

徐桂荣, 1992. 贵州关岭扒子场中三叠世绒枝藻植物群的发现. 地球科学, 17(5): 503-511. https://www.cnki.com.cn/Article/CJFDTOTAL-DQKX199205003.htm

赵小明, 童金南, 姚华舟, 等, 2008. 华南早三叠世错时相沉积及其对复苏期生态系的启示. 中国科学: 地球科学, 38(12): 1564-1574. https://www.cnki.com.cn/Article/CJFDTOTAL-JDXK200812010.htm

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(8) / Tables(2)

Get Citation

PDF

XML

Article views (705) PDF downloads(94)

The Characteristics of Giant Ooids from the Poduan Formation during the Early Middle Triassic and Its Environmental Significance at Poduan Section, Ceheng, Guizhou Province

doi: 10.3799/dqkx.2023.087

Abstract

References

Proportional views

Catalog

通讯作者: 陈斌, bchen63@163.com

Proportional views

Export File

Citation

Format

Content