doi:10.1007/s12583-019-1233-x

[1]	Amthor, J. E., Grotzinger, J. P., Schröder, S., et al., 2003. Extinction of Cloudina and Namacalathus at the Precambrian-Cambrian Boundary in Oman. Geology, 31(5): 431. https://doi.org/10.1130/0091-7613(2003)031 < 0431:eocana > 2.0.co; 2 doi: 10.1130/0091-7613(2003)031<0431:eocana>2.0.co;2
[2]	Bowring, S. A., Grotzinger, J. P., Condon, D. J., et al., 2007. Geochronologic Constraints on the Chronostratigraphic Framework of the Neoproterozoic Huqf Supergroup, Sultanate of Oman. American Journal of Science, 307(10): 1097-1145. https://doi.org/10.2475/10.2007.01
[3]	Cai, Y. P., Hua, H., Schiffbauer, J. D., et al., 2014. Tube Growth Patterns and Microbial Mat-Related Lifestyles in the Ediacaran Fossil Cloudina, Gaojiashan Lagerstätte, South China. Gondwana Research, 25(3): 1008-1018. https://doi.org/10.1016/j.gr.2012.12.027
[4]	Cai, Y. P., Xiao, S. H., Hua, H., et al., 2015. New Material of the Biomineralizing Tubular Fossil Sinotubulites from the Late Ediacaran Dengying Formation, South China. Precambrian Research, 261: 12-24. http://doi.org/10.1016/j.precamres.2015.02.002
[5]	Cai, Y. P., Xiao, S. H., Li, G. X., et al., 2019. Diverse Biomineralizing Animals in the Terminal Ediacaran Period Herald the Cambrian Explosion. Geology, 47(4): 380-384. https://doi.org/10.1130/g45949.1
[6]	Charvet, J., 2013. The Neoproterozoic-Early Paleozoic Tectonic Evolution of the South China Block: An Overview. Journal of Asian Earth Sciences, 74: 198-209. https://doi.org/10.1016/j.jseaes.2013.02.015
[7]	Chen, D. Z., Wang, J. G., Qing, H. R., et al., 2009. Hydrothermal Venting Activities in the Early Cambrian, South China: Petrological, Geochronological and Stable Isotopic Constraints. Chemical Geology, 258(3/4): 168-181. https://doi.org/10.1016/j.chemgeo.2008.10.016
[8]	Chen, D. Z., Zhou, X. Q., Fu, Y., et al., 2015. New U-Pb Zircon Ages of the Ediacaran-Cambrian Boundary Strata in South China. Terra Nova, 27(1): 62-68. http://doi.org/10.1111/ter.12134
[9]	Chen, Z., Zhou, C. M., Meyer, M., et al., 2013. Reply to Comment on "Trace Fossil Evidence for Ediacaran Bilaterian Animals with Complex Behaviors" [Precambrian Research. 224 (2013) 690-701]. Precambrian Research, 231: 386-387. https://doi.org/10.1016/j.precamres.2013.04.002
[10]	Chen, Z., Zhou, C. M., Xiao, S. H., et al., 2014. New Ediacara Fossils Preserved in Marine Limestone and Their Ecological Implications. Scientific Reports, 4(1): 4180-4190. https://doi.org/10.1038/srep04180
[11]	Compston, W., Zhang, Z., Cooper, J. A., et al., 2008. Further SHRIMP Geochronology on the Early Cambrian of South China. American Journal of Science, 308(4): 399-420. https://doi.org/10.2475/04.2008.01
[12]	Condon, D., 2005. U-Pb Ages from the Neoproterozoic Doushantuo Formation, China. Science, 308(5718): 95-98. https://doi.org/10.1126/science.1107765
[13]	Cui, L. L., Wang, X., 2014. Determination of Carbon and Oxygen Isotopes of Geological Samples with a Complicated Matrix: Comparison of Different Analytical Methods. Anal Methods, 6(22): 9173-9178. https://doi.org/10.1039/c4ay01717j
[14]	Ding, L. F., Li, Y., Chen, H. X., 1992a. Discovery of Micrhystridium Regulare from Sinian-Cambrian Boundary Strata in Yichang, Hubei, and Its Stratigraphic Significance. Acta Micropalaeontologica Sinica, 9(3): 303-309 (in Chinese with English Abstract)
[15]	Ding, L. F., Zhang, L. Y., Li, Y., et al., 1992b. The Study of the Late Sinian-Early Cambrian Biotas from the Northern Margin of the Yangtze Platform. Scientific and Technical Documents Publishing House, Beijing (in Chinese)
[16]	Ding, Q. X., Xing, Y. S., Wang, Z. Q., et al., 1993. Tubular and Trace Fossils from the Sinian Dengying Dormation in the Miaohe-Liantuo Area, Hubei Province. Geological Review, 39(1): 118-125 (in Chinese with English Abstract)
[17]	Ding, Y., Chen, D. Z., Zhou, X. Q., et al., 2018. Paired δ¹³C_carb- δ¹³C_org Evolution of the Dengying Formation from Northeastern Guizhou and Implications for Stratigraphic Correlation and the Late Ediacaran Carbon Cycle. Journal of Earth Science. https://doi.org/10.1007/s12583-018-0886-1
[18]	Duda, J. P., Blumenberg, M., Thiel, V., et al., 2014. Geobiology of a Palaeoecosystem with Ediacara-Type Fossils: The Shibantan Member (Deng-ying Formation, South China). Precambrian Research, 255: 48-62. http://doi.org/10.1016/j.precamres.2014.09.012
[19]	Duda, J. P., Zhu, M. Y., Reitner, J., 2016. Depositional Dynamics of a Bituminous Carbonate Facies in a Tectonically Induced Intra-Platform Basin: The Shibantan Member (Dengying Formation, Ediacaran Period). Carbonates and Evaporites, 31(1): 87-99. https://doi.org/10.1007/s13146-015-0243-8
[20]	Goldberg, T., Strauss, H., Guo, Q. J., et al., 2007. Reconstructing Marine Redox Conditions for the Early Cambrian Yangtze Platform: Evidence from Biogenic Sulphur and Organic Carbon Isotopes. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 175-193. https://doi.org/10.1016/j.palaeo.2007.03.015
[21]	Grotzinger, J. P., Bowring, S. A., Saylor, B. Z., et al., 1995. Biostratigraphic and Geochronologic Constraints on Early Animal Evolution. Science, 270(5236): 598-604. https://doi.org/10.1126/science.270.5236.598
[22]	Guo, J. F., Li, Y., Li, G. X., 2014. Small Shelly Fossils from the Early Cambrian Yanjiahe Formation, Yichang, Hubei, China. Gondwana Research, 25(3): 999-1007. https://doi.org/10.1016/j.gr.2013.03.007
[23]	Hua, H., Chen, Z., Yuan, X. L., 2007. The Advent of Mineralized Skeletons in Neoproterozoic Metazoa—New Fossil Evidence from the Gaojiashan Fauna. Geological Journal, 42(3/4): 263-279. https://doi.org/10.1002/gj.1077
[24]	Hua, H., Chen, Z., Yuan, X. L., et al., 2005. Skeletogenesis and Asexual Reproduction in the Earliest Biomineralizing Animal Cloudina. Geology, 33(4): 277. https://doi.org/10.1130/g21198.1
[25]	Ishikawa, T., Ueno, Y., Komiya, T., et al., 2008. Carbon Isotope Chemostratigraphy of a Precambrian/Cambrian Boundary Section in the Three Gorge Area, South China: Prominent Global-Scale Isotope Excursions Just before the Cambrian Explosion. Gondwana Research, 14(1-2): 193-208. http://doi.org/10.1016/j.gr.2007.10.008
[26]	Ishikawa, T., Ueno, Y., Shu, D. G., et al., 2013. Irreversible Change of the Oceanic Carbon Cycle in the Earliest Cambrian: High-Resolution Organic and Inorganic Carbon Chemostratigraphy in the Three Gorges Area, South China. Precambrian Research, 225: 190-208. http://doi.org/10.1016/j.precamres.2011.10.004
[27]	Jenkins, R. J. F., Cooper, J. A., Compston, W., 2002. Age and Biostratigraphy of Early Cambrian Tuffs from SE Australia and Southern China. Journal of the Geological Society, 159(6): 645-658. https://doi.org/10.1144/0016-764901-127
[28]	Jiang, G. Q., Kaufman, A. J., Christie-Blick, N., et al., 2007. Carbon Isotope Variability across the Ediacaran Yangtze Platform in South China:Implications for a Large Surface-to-Deep Ocean δ¹³C Gradient. Earth and Planetary Science Letters, 261(1/2): 303-320. https://doi.org/10.1016/j.epsl.2007.07.009
[29]	Jiang, G. Q., Shi, X. Y., Zhang, S. H., et al., 2011. Stratigraphy and Paleogeography of the Ediacaran Doushantuo Formation (ca. 635-551 Ma) in South China. Gondwana Research, 19(4): 831-849. https://doi.org/10.1016/j.gr.2011.01.006
[30]	Jiang, G. Q., Wang, X. Q., Shi, X. Y., et al., 2012. The Origin of Decoupled Carbonate and Organic Carbon Isotope Signatures in the Early Cambrian (ca. 542-520 Ma) Yangtze Platform. Earth and Planetary Science Letters, 317-318: 96-110. https://doi.org/10.1016/j.epsl.2011.11.018
[31]	Kaufman, A., Knoll, A., 1995. Neoproterozoic Variations in the C-Isotopic Composition of Seawater: Stratigraphic and Biogeochemical Implications. Precambrian Research, 73(1/2/3/4): 27-49. https://doi.org/10.1016/0301-9268(94)00070-8
[32]	Lan, Z. W., Li, X. H., Chu, X. L., et al., 2017. SIMS U-Pb Zircon Ages and Ni-Mo-PGE Geochemistry of the Lower Cambrian Niutitang Formation in South China: Constraints on Ni-Mo-PGE Mineralization and Stratigraphic Correlations. Journal of Asian Earth Sciences, 137: 141-162. https://doi.org/10.1016/j.jseaes.2016.12.046
[33]	Li, C., Hardisty, D. S., Luo, G., et al., 2017. Uncovering the Spatial Heterogeneity of Ediacaran Carbon Cycling. Geobiology, 15(2): 211-224. http://doi.org/10.1111/gbi.12222
[34]	Li, D., Ling, H. F., Jiang, S. Y., et al., 2009. New Carbon Isotope Stratigraphy of the Ediacaran-Cambrian Boundary Interval from SW China: Implications for Global Correlation. Geological Magazine, 146(4): 465-484. https://doi.org/10.1017/s0016756809006268
[35]	Li, D., Ling, H. F., Shields-Zhou, G. A., et al., 2013. Carbon and Strontium Isotope Evolution of Seawater across the Ediacaran-Cambrian Transition: Evidence from the Xiaotan Section, NE Yunnan, South China. Precambrian Research, 225: 128-147. https://doi.org/10.1016/j.precamres.2012.01.002
[36]	Li, X. H., Tang, G. Q., Gong, B., et al., 2013. Qinghu Zircon: A Working Reference for Microbeam Analysis of U-Pb Age and Hf and O Isotopes. Chinese Science Bulletin, 58(36): 4647-4654. https://doi.org/10.1007/s11434-013-5932-x
[37]	Linnemann, U., Ovtcharova, M., Schaltegger, U., et al., 2019. New High-Resolution Age Data from the Ediacaran-Cambrian Boundary Indicate Rapid, Ecologically Driven Onset of the Cambrian Explosion. Terra Nova, 31(1): 49-58. http://doi.org/10.1111/ter.12368
[38]	Liu, S. G., Sun, W., Luo, Z. L., et al., 2013. Xingkai Taphrogenesis and Petroleum Exploration from Upper Sinian to Cambrian Strata in Sichuan Basin. Journal of Chengdu University of Technology, 40(5): 511-520 (in Chinese with English Abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=cdlgxyxb201305003
[39]	Lyons, T. W., Reinhard, C. T., Planavsky, N. J., 2014. The Rise of Oxygen in Earth's Early Ocean and Atmosphere. Nature, 506(7488): 307-315. https://doi.org/10.1038/nature13068
[40]	Maloof, A. C., Porter, S. M., Moore, J. L., et al., 2010. The Earliest Cambrian Record of Animals and Ocean Geochemical Change. Geological Society of America Bulletin, 122(11/12): 1731-1774. https://doi.org/10.1130/b30346.1
[41]	Marshall, C. R., 2006. Explaining the Cambrian "Explosion" of Animals. Annual Review of Earth and Planetary Sciences, 34(1): 355-384. http://doi.org/10.1146/annurev.earth.33.031504.103001
[42]	Meyer, M., Xiao, S. H., Gill, B. C., et al., 2014. Interactions between Ediacaran Animals and Microbial Mats: Insights from Lamonte Trevallis, a New Trace Fossil from the Dengying Formation of South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 396: 62-74. https://doi.org/10.1016/j.palaeo.2013.12.026
[43]	Narbonne, G. M., 2005. The Ediacara Biota: Neoproterozoic Origin of Animals and Their Ecosystems. Annual Review of Earth and Planetary Sciences, 33(1): 421-442. https://doi.org/10.1146/annurev.earth.33.092203.122519
[44]	Okada, Y., Sawaki, Y., Komiya, T., et al., 2014. New Chronological Constraints for Cryogenian to Cambrian Rocks in the Three Gorges, Weng'an and Chengjiang areas, South China. Gondwana Research, 25(3): 1027-1044. http://doi.org/10.1016/j.gr.2013.05.001
[45]	Shen, B., Xiao, S. H., Zhou, C. M., et al., 2009. Yangtziramulus Zhangi New Genus and Species, a Carbonate-Hosted Macrofossil from the Ediacaran Dengying Formation in the Yangtze Gorges Area, South China. Journal of Paleontology, 83(4): 575-587. http://doi.org/10.1666/08-042r1.1
[46]	Sláma, J., Košler, J., Condon, D., et al., 2008. Plešovice Zircon—A New Natural Reference Material for U-Pb and Hf Isotopic Microanalysis. Chemical Geology, 249(1-2): 1-35. http://doi.org/10.1016/j.chemgeo.2007.11.005
[47]	Steiner, M., Li, G. X., Qian, Y., et al., 2007. Neoproterozoic to Early Cambrian Small Shelly Fossil Assemblages and a Revised Biostratigraphic Correlation of the Yangtze Platform (China). Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 67-99. http://doi.org/10.1016/j.palaeo.2007.03.046
[48]	Sun, W. G., 1986. Late Precambrian Pennatulids (Sea Pens) from the Eastern Yangtze Gorge, China: Paracharnia Gen. Nov. Precambrian Research, 31(4): 361-375. http://doi.org/10.1016/0301-9268(86)90040-9
[49]	Wang, J., Li, Z. X., 2003. History of Neoproterozoic Rift Basins in South China: Implications for Rodinia Break-Up. Precambrian Research, 122(1/2/3/4): 141-158. https://doi.org/10.1016/s0301-9268(02)00209-7
[50]	Wang, D., Ling, H. F., Li, D., et al., 2012. Carbon Isotope Stratigraphy of Yanjiahe Formation across the Ediacaran-Cambrian Boundary in the Three Gorges Area. Journal of Stratigraphy, 26(6): 715-720 (in Chinese with English Abstract) http://www.wanfangdata.com.cn/details/detail.do?_type=perio&id=dcxzz201201003
[51]	Wang, J. G., Chen, D. Z., Wang, D., et al., 2012a. Petrology and Geochemistry of Chert on the Marginal Zone of Yangtze Platform, Western Hunan, South China, during the Ediacaran-Cambrian Transition. Sedimentology, 59(3): 809-829. https://doi.org/10.1111/j.1365-3091.2011.01280.x
[52]	Wang, J. G., Chen, D. Z., Yan, D. T., et al., 2012b. Evolution from an Anoxic to Oxic Deep Ocean during the Ediacaran-Cambrian Transition and Implications for Bioradiation. Chemical Geology, 306-307: 129-138. http://doi.org/10.1016/j.chemgeo.2012.03.005
[53]	Wang, X. Q., Shi, X. Y., Jiang, G. Q., et al., 2012. New U-Pb Age from the Basal Niutitang Formation in South China: Implications for Diachronous Development and Condensation of Stratigraphic Units across the Yangtze Platform at the Ediacaran-Cambrian Transition. Journal of Asian Earth Sciences, 48: 1-8. https://doi.org/10.1016/j.jseaes.2011.12.023
[54]	Wang, X. Q., Shi, X. Y., Jiang, G. Q., et al., 2014. Organic Carbon Isotope Gradient and Ocean Stratification across the Late Ediacaran-Early Cambrian Yangtze Platform. Science China Earth Sciences, 57(5): 919-929. https://doi.org/10.1007/s11430-013-4732-0
[55]	Weber, B., Steiner, M., Zhu, M. Y., 2007. Precambrian-Cambrian Trace Fossils from the Yangtze Platform (South China) and the Early Evolution of Bilaterian Lifestyles. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 328-349. https://doi.org/10.1016/j.palaeo.2007.03.021
[56]	Wiedenbeck, M., Allé, P., Corfu, F., et al., 1995. Three Natural Zircon Standards for U-Th-Pb, Lu-Hf, Trace Element and Ree Analyses. Geostandards and Geoanalytical Research, 19(1): 1-23. https://doi.org/10.1111/j.1751-908x.1995.tb00147.x
[57]	Xiao, S. H., Laflamme, M., 2009. On the Eve of Animal Radiation: Phylogeny, Ecology and Evolution of the Ediacara Biota. Trends in Ecology & Evolution, 24(1): 31-40. https://doi.org/10.1016/j.tree.2008.07.015
[58]	Xiao, S. H., Narbonne, G. M., Zhou, C. M., et al., 2016. Towards an Ediacaran Time Scale: Problems, Protocols, and Prospects. Episodes, 39(4): 540. https://doi.org/10.18814/epiiugs/2016/v39i4/103886
[59]	Xiao, S. H., Shen, B., Zhou, C. M., et al., 2005. A Uniquely Preserved Ediacaran Fossil with Direct Evidence for a Quilted Bodyplan. Proceedings of the National Academy of Sciences, 102(29): 10227-10232. https://doi.org/10.1073/pnas.0502176102
[60]	Yang, B., Steiner, M., Zhu, M. Y., et al., 2016. Transitional Ediacaran-Cambrian Small Skeletal Fossil Assemblages from South China and Kazakhstan: Implications for Chronostratigraphy and Metazoan Evolution. Precambrian Research, 285: 202-215. http://doi.org/10.1016/j.precamres.2016.09.016
[61]	Yang, C., Li, X. H., Zhu, M. Y., et al., 2017. SIMS U-Pb Zircon Geochronological Constraints on Upper Ediacaran Stratigraphic Correlations, South China. Geological Magazine, 154(6): 1202-1216. https://doi.org/10.1017/s0016756816001102
[62]	Yao, W. H., Li, Z. X., Li, W. X., et al., 2015. Detrital Provenance Evolution of the Ediacaran-Silurian Nanhua Foreland Basin, South China. Gondwana Research, 28(4): 1449-1465. http://doi.org/10.1016/j.gr.2014.10.018
[63]	Zhou, C. M., Xiao, S. H., 2007. Ediacaran δ¹³C Chemostratigraphy of South China. Chemical Geology, 237(1/2): 89-108. https://doi.org/10.1016/j.chemgeo.2006.06.021
[64]	Zhou, C. M., Yuan, X. L., Xiao, S. H., et al., 2019. Ediacaran Integrative Stratigraphy and Timescale of China. Science China Earth Sciences, 62(1): 7-24. https://doi.org/10.1007/s11430-017-9216-2
[65]	Zhu, M., Zhuravlev, A. Y., Wood, R. A., et al., 2017. A Deep Root for the Cambrian Explosion: Implications of New Bio- And Chemostratigraphy from the Siberian Platform. Geology, 45(5): 459-462. https://doi.org/10.1130/g38865.1
[66]	Zhu, M. Y., 2010. The Origin and Cambrian Explosion of animals: Fossil Evidences from China. Acta Palaeontologica Sinica, 49(3): 269-287 (in Chinese with English Abstract) http://d.old.wanfangdata.com.cn/Periodical/zggdxxxswz-swx200801017
[67]	Zhu, M. Y., Babcock, L. E., Peng, S. C., 2006. Advances in Cambrian Stratigraphy and Paleontology: Integrating Correlation Techniques, Paleobiology, Taphonomy and Paleoenvironmental Reconstruction. Palaeoworld, 15(3/4): 217-222. https://doi.org/10.1016/j.palwor.2006.10.016
[68]	Zhu, M. Y., Lu, M., Zhang, J. M., et al., 2013. Carbon Isotope Chemostratigraphy and Sedimentary Facies Evolution of the Ediacaran Doushantuo Formation in Western Hubei, South China. Precambrian Research, 225: 7-28. https://doi.org/10.1016/j.precamres.2011.07.019
[69]	Zhu, M. Y., Yang, A. H., Yuan, J. L., et al., 2019. Cambrian Integrative Stratigraphy and Timescale of China. Science China Earth Sciences, 62(1): 25-60. https://doi.org/10.1007/s11430-017-9291-0
[70]	Zhu, M. Y., Zhang, J. M., Steiner, M., et al., 2003. Sinian-Cambrian Stratigraphic Framework for Shallow- to Deep-Water Environments of the Yangtze Platform: An Integrated Approach. Progress in Natural Science, 13(12): 951-960. https://doi.org/10.1080/10020070312331344710
[71]	Zhu, M. Y., Zhang, J. M., Yang, A. H., 2007. Integrated Ediacaran (Sinian) Chronostratigraphy of South China. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1/2): 7-61. https://doi.org/10.1016/j.palaeo.2007.03.025
[72]	Zhu, R. X., Li, X. H., Hou, X. G., et al., 2009. SIMS U-Pb Zircon Age of a Tuff Layer in the Meishucun Section, Yunnan, Southwest China: Constraint on the Age of the Precambrian-Cambrian Boundary. Science in China Series D: Earth Sciences, 52(9): 1385-1392. https://doi.org/10.1007/s11430-009-0152-6