1 Pu, J. P., Bowring, S. A., Ramezani, J. & Myrow, P. Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota. Geology (Boulder) 44, 955-958, doi:10.1130/G38284.1 (2016).
2 Shen, B., Dong, L., Xiao, S. & Kowalewski, M. The Avalon explosion: Expansion and saturation of Ediacara morphospace. Science 319, 81-84 (2008).
3 Fike, D. A., Grotzinger, J. P., Pratt, L. M. & Summons, R. E. Oxidation of the Ediacaran ocean. Nature 444, 744-747, doi:10.1038/nature05345 (2006).
4 Zhu, M., Zhang, J. & Yang, A. Integrated Ediacaran (Sinian) chronostratigraphy of South China. Palaeogeography, Palaeoclimatology, Palaeoecology 254, 7-61, doi:10.1016/j.palaeo.2007.03.025 (2007).
5 Mitchell, R. N. et al. Sutton hotspot: Resolving Ediacaran-Cambrian Tectonics and true polar wander for Laurentia. American Journal of Science 311, 651-663, doi:10.2475/08.2011.01 (2011).
6 Robert, B. et al. Constraints on the Ediacaran inertial interchange true polar wander hypothesis: A new paleomagnetic study in Morocco (West African Craton). Precambrian Research 295, 90-116, doi:https://doi.org/10.1016/j.precamres.2017.04.010 (2017).
7 Robert, B., Greff-Lefftz, M. & Besse, J. True Polar Wander: A Key Indicator for Plate Configuration and Mantle Convection During the Late Neoproterozoic. Geochemistry, Geophysics, Geosystems 19, 3478-3495, doi:10.1029/2018gc007490 (2018).
8 Wen, B., Evans, D. A. D., Anderson, R. P. & McCausland, P. J. A. Late Ediacaran paleogeography of Avalonia and the Cambrian assembly of West Gondwana. Earth and Planetary Science Letters 552, 116591, doi:https://doi.org/10.1016/j.epsl.2020.116591 (2020).
9 Hoffman, P. F., Kaufman, A. J., Halverson, G. P. & Schrag, D. P. A Neoproterozoic snowball Earth. Science 281, 1342-1346 (1998).
10 Hoffman, P. F. et al. Snowball Earth climate dynamics and Cryogenian geology-geobiology. Science Advances 3 (2017).
11 Hoffman, P. F. & Li, Z.-X. A palaeogeographic context for Neoproterozoic glaciation. Palaeogeography, Palaeoclimatology, Palaeoecology 277, 158-172, doi:10.1016/j.palaeo.2009.03.013 (2009).
12 Li, Z.-X., Evans, D. A. D. & Halverson, G. P. Neoproterozoic glaciations in a revised global palaeogeography from the breakup of Rodinia to the assembly of Gondwanaland. Sedimentary Geology 294, 219-232, doi:http://dx.doi.org/10.1016/j.sedgeo.2013.05.016 (2013).
13 Hebert, C. L., Kaufman, A. J., Penniston-Dorland, S. C. & Martin, A. J. Radiometric and stratigraphic constraints on terminal Ediacaran (post-Gaskiers) glaciation and metazoan evolution. Precambrian Research 182, 402-412, doi:10.1016/j.precamres.2010.07.008 (2010).
14 Bowring, S., Myrow, P., Landing, E., Ramezani, J. & Grotzinger, J. Geochronological constraints on terminal Neoproterozoic events and the rise of metazoans. Geophysical Research Abstracts 5, 13219 (2003).
15 Xiao, S., Yuan, X., Steiner, M. & Knoll, A. H. Macroscopic carbonaceous compressions in a terminal Proterozoic shale: A systematic reassessment of the Miaohe biota, South China. Journal of Paleontology 76, 347-376 (2002).
16 Liu, P. et al. High-resolution biostratigraphic and chemostratigraphic data from the Chenjiayuanzi section of the Doushantuo Formation in the Yangtze Gorges area, South China: Implication for subdivision and global correlation of the Ediacaran System. Precambrian Research 249, 199-214, doi:http://dx.doi.org/10.1016/j.precamres.2014.05.014 (2014).
17 Hua, H., Chen, Z., Yuan, X., Zhang, L. & Xiao, S. Skeletogenesis and asexual reproduction in the earliest biomineralizing animal Cloudina. Geology 33, 277-280 (2005).
18 Chen, Z., Zhou, C., Yuan, X. & Xiao, S. Death march of a segmented and trilobate bilaterian elucidates early animal evolution. Nature 573, 412-415, doi:10.1038/s41586-019-1522-7 (2019).
19 Zhu, M., Zhuravlev, A. Y., Wood, R. A., Zhao, F. & Sukhov, S. S. A deep root for the Cambrian explosion: Implications of new bio- and chemostratigraphy from the Siberian Platform. Geology 45, 459-462, doi:10.1130/g38865.1 (2017).
20 Shen, B., Xiao, S., Dong, L., Zhou, C. & Liu, J. Problematic macrofossils from Ediacaran successions in the North China and Chaidam blocks: implications for there evolutionary root and biostratigraphic significance. Journal of Paleontology 81, 1396-1411 (2007).
21 Pang, K. et al. New Ediacara-type fossils and late Ediacaran stratigraphy from the northern Qaidam Basin (China): Paleogeographic implications. Geology, doi:10.1130/g48842.1 (2021).
22 Zhou, C., Yuan, X., Xiao, S., Chen, Z. & Hua, H. Ediacaran integrative stratigraphy and timescale of China. Sci. China Earth Sci. 62, 7-24, doi:10.1007/s11430-017-9216-2 (2019).
23 Halverson, G. P., Hoffman, P. F., Schrag, D. P., Maloof, A. C. & Rice, A. H. N. Toward a Neoproterozoic composite carbon-isotope record. Geological Society of America Bulletin 117, 1181-1207 (2005).
24 Grotzinger, J. P., Fike, D. A. & Fischer, W. W. Enigmatic origin of the largest-known carbon isotope excursion in Earth's history. Nature Geosci 4, 285-292 (2011).
25 Tahata, M. et al. Carbon and oxygen isotope chemostratigraphies of the Yangtze platform, South China: Decoding temperature and environmental changes through the Ediacaran. Gondwana Research 23, 333-353, doi:10.1016/j.gr.2012.04.005 (2013).
26 Rooney, A. D. et al. Calibrating the coevolution of Ediacaran life and environment. Proc Natl Acad Sci U S A 117, 16824-16830, doi:10.1073/pnas.2002918117 (2020).
27 Gong, Z. & Li, M. Astrochronology of the Ediacaran Shuram carbon isotope excursion, Oman. Earth and Planetary Science Letters 547, 116462, doi:https://doi.org/10.1016/j.epsl.2020.116462 (2020).
28 Xiao, S. et al. The Neoproterozoic Quruqtagh Group in eastern Chinese Tianshan: Evidence for a post-Marinoan glaciation. Precambrian Research 130, 1-26 (2004).
29 Shen, B. et al. Carbon, sulfur, and oxygen isotope evidence for a strong depth gradient and oceanic oxidation after the Ediacaran Hankalchough glaciation. Geochimica et Cosmochimica Acta 75, 1357-1373, doi:http://dx.doi.org/10.1016/j.gca.2010.12.015 (2011).
30 Xu, B. et al. SHRIMP zircon U–Pb age constraints on Neoproterozoic Quruqtagh diamictites in NW China. Precambrian Research 168, 247-258, doi:https://doi.org/10.1016/j.precamres.2008.10.008 (2009).
31 Jiang, G., Kaufman, A. J., Christie-Blick, N., Zhang, S. & Wu, H. 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, 303-320, doi:10.1016/j.epsl.2007.07.009 (2007).
32 Pokrovskii, B. G., Melezhik, V. A. & Bujakaite, M. I. Carbon, oxygen, strontium, and sulfur isotopic compositions in late Precambrian rocks of the Patom Complex, central Siberia: Communication 1. results, isotope stratigraphy, and dating problems. Lithol Miner Resour 41, 450-474, doi:10.1134/s0024490206050063 (2006).
33 Swanson-Hysell, N. L. et al. Cryogenian Glaciation and the Onset of Carbon-Isotope Decoupling. Science 328, 608-611, doi:10.1126/science.1184508 (2010).
34 Linnemann, U. et al. A ~565 Ma old glaciation in the Ediacaran of peri-Gondwanan West Africa. International Journal of Earth Sciences 107, 885-911, doi:10.1007/s00531-017-1520-7 (2018).
35 Chumakov, N. M. The Baykonurian glaciohorizon of the Late Vendian. Stratigraphy and Geological Correlation 17, 373-381, doi:10.1134/S0869593809040029 (2009).
36 McCausland, P. J. A., Hankard, F., Van der Voo, R. & Hall, C. M. Ediacaran paleogeography of Laurentia: Paleomagnetism and 40Ar–39Ar geochronology of the 583Ma Baie des Moutons syenite, Quebec. Precambrian Research 187, 58-78, doi:https://doi.org/10.1016/j.precamres.2011.02.004 (2011).
37 Maslov, A. V. et al. New constraints for the age of Vendian glacial deposits (Central Urals). Doklady Earth Sciences 449, 303-308, doi:10.1134/S1028334X13030203 (2013).
38 Finnegan, S. et al. The Magnitude and Duration of Late Ordovician–Early Silurian Glaciation. Science 331, 903-906, doi:10.1126/science.1200803 (2011).
39 Fielding, C. R. et al. Stratigraphic imprint of the Late Palaeozoic Ice Age in eastern Australia: a record of alternating glacial and nonglacial climate regime. Journal of the Geological Society 165, 129-140, doi:10.1144/0016-76492007-036 (2008).
40 Ehlers, J. & Gibbard, P. L. The extent and chronology of Cenozoic Global Glaciation. Quaternary International 164-165, 6-20, doi:https://doi.org/10.1016/j.quaint.2006.10.008 (2007).
41 Wang, Z. et al. Wide but not ubiquitous distribution of glendonite in the Doushantuo Formation, South China: Implications for Ediacaran climate. Precambrian Research 338, 105586, doi:https://doi.org/10.1016/j.precamres.2019.105586 (2020).
42 Evans, S., Diamond, C., Droser, M. & Lyons, T. Dynamic oxygen and coupled biological and ecological innovation during the second wave of the Ediacara Biota. Emerging Topics in Life Sciences 2, ETLS20170148, doi:10.1042/ETLS20170148 (2018).
43 Rothman, D. H., Hayes, J. M. & Summons, R. E. Dynamics of the Neoproterozoic carbon cycle. Proceedings of the National Academy of Sciences of the United States of America 100, 8124-8129 (2003).
44 Cook, P. J. & Shergold, J. H. Phosphate deposits of the world, Volume 1, Proterozoic and Cambrian Phosphorites. (Cambridge University Press, 1986).
45 Xiao, S. H. et al. Towards an Ediacaran Time Scale: Problems, Protocols, and Prospects. International Union of Geological Sciences 39, 540-555, doi:10.18814/epiiugs/2016/v39i4/103886 (2016).
46 Xiao, S. H. & Narbonne, G. M. in Geologic Time Scale 2020 (eds Felix M. Gradstein, James G. Ogg, Mark D. Schmitz, & Gabi M. Ogg) 521-561 (Elsevier, 2020).