[1] An Z.H., Jiang G.Q., Tong J.N., Tian L., Ye Q., Song H.Y., Song H.J.,2015. Stratigraphic position of the Ediacaran Miaohe biota and its constrains on the age of the upper Doushantuo δ13C anomaly in the Yangtze Gorges area, South China. Precambrian Research, 271, 243-253. https://doi.org/10.1016/j.precamres.2015.10.007.
[2] Anderson M.M., Misra S.B., 1968. Fossils found in the Pre-Cambrian Conception Group of south-eastern Newfoundland. Nature, 220 (5168), 680-681. https://doi.org/10.1038/220680a0.
[3] Canfield D.E., Poulton S.W., Knoll, A.H, Narbonne G.M., Ross G., Goldberg T., Strauss H., 2008. Ferruginous conditions dominated later Neoproterozoic deep-water chemistry. Science, 321(5891), 949-952. https:/doi.org/10.1126/science.1154499.
[4] Canfield D.E., Poulton S.W., Narbonne G.M., 2007. Late-Neoproterozoic deep-ocean oxygenation and the rise of animal life. Science, 315(5808), 92-95. https://doi.org/10.1126/science.1135013.
[5] Chen M.E., Xiao Z.Z., 1991. Discovery of the macrofossils in the Upper Sinian Doushantuo Formation at Miaohe, eastern Yangtze Gorges.Scientia Geological Sinica, 4, 317-324 (in Chinese with English abstract).
[6] Chen M.E., Chen Q.Y., Xiao Z.Z.,2000. Preliminary discussion on the early evolutionary history of macroscopic plants. Scientia Geologica Sinica, 35(1), 1-15. https://doi.org/10.3321/j.issn:0563-5020.2000.01.001 (in Chinese with English abstract).
[7] Chen M.E., Xiao Z.Z., Yuan X.L., 1994. A new assemblage of megafossils — Miaohe Biota from Upper Sinian Doushantuo Formation, Yangtze Gorges.Acta Palaeontologica Sinica, 33(4), 391-403 (in Chinese with English abstract).
[8] Chen X.H., Wang X.F.,2002. Morphology and systematics of fossils in the Sinian Wulingshan biota from western Hunan Province. Geological Bulletin of China, 21(10), 638-645. https://doi.org/10.3969/j.issn.1671-2552.2002.10.007 (in Chinese with English abstract).
[9] Chen X.H., Wang X.F., Wang C.S., Li Z.H., Chen L.D., 1999. A preliminary study on carbonaceous megafossils from the Late Sinian Liuchapo Formation of West Hunan.Geology and Mineral Resources of South China, (2), 15-30 (in Chinese with English abstract).
[10] Condon D., Zhu M.Y., Bowring S., Wang W., Yang A.H., Jin Y.G., 2005. U-Pb ages from the Neoproterozoic Doushantuo Formation, China. Science, 308(5718), 95-98. https://doi.org/10.1126/science.1107765.
[11] Ding L.F., Li Y., Hu X.S., Xiao Y.P., Su C.Q., Huang J., 1996. Sinian Miaohe Biota. Geological Publishing House, Beijing, pp. 221 (in Chinese).
[12] Dornbos S.Q., Oji T., Kanayama A., Gonchigdorj S., 2016. A new Burgess Shale-type deposit from the Ediacaran of western Mongolia. Scientific Reports, 6, 23438. https://doi.org/10.1038/srep23438.
[13] Fedonkin M.A.,1981. Belomorskaya biota venda.Akademiya Nauk SSSR, Trudy, 342, 1-100.
[14] Fedonkin M.A.,1985. Precambrian metazoans: The problems of preservation, systematics and evolution. Philosophical Transactions of the Royal Society of London, Series B, Biological Sciences, 311(1148), 27-45. https://doi.org/10.1098/rstb.1985.0136.
[15] Germs G.J.B.,1973. Possible sprigginid worm and a new trace fossil from the Nama Group, South West Africa. Geology, 1(2), 69-70. https://doi.org/10.1130/0091-7613(1973)1<69:PSWAAN>2.0.CO;2.
[16] Glaessner M.F.,1959. The oldest fossil faunas of South Australia. Geologische Rundschau, 47(2), 522-531. https://doi.org/10.1007/BF01800671.
[17] Jenkins R.J.F.,1985. The enigmatic Ediacaran (late Precambrian) genus Rangea and related forms. Paleobiology, 11(3), 336-355. https://doi.org/10.1017/S0094837300011635.
[18] Jiang G.Q., Shi X.Y., Zhang S.H., Wang Y., Xiao S.H.,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.
[19] Kendall B., Komiya T., Lyons T.W., Bates S.M., Gordon G.W., Romaniello S.J., Jiang G.Q., Creaser R.A., Xiao S.,McFadden, K., Sawaki, Y., Tahata, M., Shu, D.G., Han, J., Li, Y., Chu, X.L., Anbar, A.D., 2015. Uranium and molybdenum isotope evidence for an episode of widespread ocean oxygenation during the late Ediacaran Period. Geochimica et Cosmochimica Acta, 156, 173-193. https://doi.org/10.1016/j.gca.2015.02.025.
[20] Li C., Planavsky N.J., Shi W., Zhang Z.H., Zhou C.M., Cheng M., Tarhan L.G., Luo G.M., Xie S.C., 2015. Ediacaran marine redox heterogeneity and early animal ecosystems. Scientific Reports, 5(1), 17097. https://doi.org/10.1038/srep17097.
[21] Liu B.J., Xu X., 1994. Atlas of the Lithofacies and Palaeogeography of South China (Sinian-Triassic). Beijing: Science Press, pp. 28-33 (in Chinese).
[22] Liu H.Y., Zhang Q.R., 1991. The Sinian System in China. Beijing: Science Press, pp. 1-388 (in Chinese).
[23] Lu M., Zhu M.Y., Zhang J.M.,Shields-Zhou, G., Li, G.X., Zhao, F.C., Zhao, X., Zhao, M.J., 2013. The DOUNCE event at the top of the Ediacaran Doushantuo Formation, South China: Broad stratigraphic occurrence and non-diagenetic origin. Precambrian Research, 225, 86-109. https://doi.org/10.1016/j.precamres.2011.10.018.
[24] Narbonne G.M., Hofmann H.J., 1987. Ediacaran biota of the Wernecke Mountains, Yukon, Canada.Palaeontology, 30(4), 647-676.
[25] Narbonne G.M.,2004. Modular construction of Early Ediacaran complex life forms. Science, 305(5687), 1141-1144. https://doi.org/10.1126/science.1099727.
[26] Narbonne G.M.,2005. The Ediacara biota: Neoproterozoic origin of animals and their ecosystems. Annual Review of Earth and Planetary Sciences, 33, 421-442. https://doi.org/10.1146/annurev.earth.33.092203.122519.
[27] Qin S.R., Zhu S.C., Zhu S.X., Chen Y.L., Wang Y.G., Yin G.Z., Zheng S.F., Luo Q.L., Wang F.X., Qian, Y., 1984. The Upper Precambrian and Sinian-Cambrian Boundary in Guizhou. Guiyang: The People’s Publishing House of Guizhou, pp. 37-76 (in Chinese).
[28] Rooney A.D., Cantine M.D., Bergmann K.D., Gómez-Pérez I., Al Baloushi B., Boag T.H., Busch J.F., Sperling E.A., Strauss J.V., 2020. Calibrating the coevolution of Ediacaran life and environment. Proceedings of the National Academy of Sciences of the United States of America, 117(29), 16824-16830. https://doi.org/10.1073/pnas.2002918117.
[29] Runnegar B.,1992. Evolution of the earliest animals. In: Schopf, J.W. (Ed.), Major Events in the History of Life. Boston: Jones and Bartlett, pp. 65-93.
[30] Sprigg R.C.,1947. Early Cambrian (?) jellyfish from the Flinders Ranges, South Australia.Transactions of the Royal Society of South Australia, 71, 212-224.
[31] Steiner M.,1994. Die Neoproterozoishen Megaalgen Südchinas.Berliner Geowissenschaftliche Abhandlungen, 15(E), 1-146 (in German).
[32] Steiner M., Erdtmann B.D., Chen J.Y., 1992. Preliminary assessment of new Late Sinian (Late Proterozoic) large siphonous and filamentous “megaalgae” from eastern Wulingshan, north-central Hunan, China.Berliner Geowissenschaftliche Abhandlungen, 3(E): 305-319 (in German).
[33] Tang F., Jin X.S., Wang Y., Ding M., Zhao Y.L., Gao L.Z.,2014. Is the Ediacaran Hiemalora the attachment disc of the Doushantuo macrofossil algae Gesinella? Geological Review, 60(5), 1009-1018. https://doi.org/10.3969/j.issn.0371-5736.2014.05.005 (in Chinese with English abstract).
[34] Tang F., Yin C.Y., Liu P.J., Duan D.L., Gao L.Z.,2008a. Morphological comparison of the Ediacaran Miaohe biota from South China: Implications for their affinities and ecology. Acta Geologica Sinica, 82(5), 601-611. https://doi.org/10.3321/j.issn:0001-5717.2008.05.004 (in Chinese with English abstract).
[35] Tang F., Yin C.Y., Liu P.J., Gao L.Z., Wang Z.Q.,2009. Neoproterozoic macrofossil records in South China and biostratigraphic successions and correlations. Acta Geoscientica Sinica, 30(4), 505-522. https://doi.org/10.3321/j.issn:1006-3021.2009.04.011 (in Chinese with English abstract).
[36] Tang F., Yin C.Y., Stefan B., Liu P.J., Wang Z.Q., Gao L.Z., 2008b. Octoradiate spiral organisms in the Ediacaran of South China. Acta Geologica Sinica - English Edition, 82(1), 27-34. https://doi.org/10.1111/j.1755-6724.2008.tb00321.x.
[37] Wang Y., Chen H.D., Wang X.L., Huang Y.M., 2011. Evolution of the Ediacaran Doushantuoian meta-paleo-community in Northeast Guizhou, South China. Acta Geologica Sinica - English Edition, 85(3), 533-543. https://doi.org/10.1111/j.1755-6724.2011.00448.x.
[38] Wang Y., Du W., Komiya T., Wang X.L., Wang Y., 2015a. Macroorganism paleoecosystems during the middle-late Ediacaran period in the Yangtze Block, South China. Paleontological Research, 19(3), 237-250. https://doi.org/10.2517/2015PR009.
[39] Wang Y., He M.H., Yu M.Y., Zhao Y.L., Peng J., Yang R.J., Zhang Z.H.,2005. Preliminary discussion on ecological characteristics and buried environments of Miaohe-type biota during the Late Doushantuoian of Sinian in northeastern Guizhou Province. Journal of Palaeogeography (Chinese Edition), 7(3), 327-335. https://doi.org/10.3969/j.issn.1671-1505.2005.03.004 (in Chinese with English abstract).
[40] Wang Y., Huang Z.Q., Chen H.D., Hou M.C., Yang Y.F., Du B.Y., 2012. Stratigraphical correlation of the Liuchapo Formation with the Dengying Formation in South China.Journal of Jilin University (Earth Science Edition), 42(S1), 328-335 (in Chinese with English abstract).
[41] Wang Y., Lei L.F., Chen H.D., Hou M.C.,2010. Development of the Ediacaran (Sinian) multicellular organisms and formation of the source rocks in the Yangtze area. Sedimentary Geology and Tethyan Geology, 30(3), 30-38. https://doi.org/10.3969/j.issn.1009-3850.2010.03.005 (in Chinese with English abstract).
[42] Wang Y., Wang X.L.,2006. The holdfasts of macroalgae in the Neoproterozoic Doushantuo Formation in northeastern Guizhou Province and their environmental significance. Acta Micropalaeontologica Sinica, 23(2), 154-164. https://doi.org/10.3969/j.issn.1000-0674.2006.02.004 (in Chinese with English abstract).
[43] Wang Y., Wang X.L., 2008. Annelid from the Neoproterozoic Doushantuo Formation in northeastern Guizhou, China. Acta Geologica Sinica - English Edition, 82(2), 257-265. https://doi.org/10.1111/j.1755-6724.2008.tb00576.x.
[44] Wang Y., Wang X.L., 2011. New observations on Cucullus Steiner from the Neoproterozoic Doushantuo Formation of Guizhou, South China. Lethaia, 44(3), 275-286. https://doi.org/10.1111/j.1502-3931.2010.00241.x.
[45] Wang Y., Wang X.L., Huang Y.M.,2007. Macroscopic algae from the Ediacaran Doushantuo Formation in Northeast Guizhou, South China. Earth Science, 32(6), 828-844. https://doi.org/10.3321/j.issn:1000-2383.2007.06.014 (in Chinese with English abstract).
[46] Wang Y., Wang X.L., Huang Y.M., 2008. Megascopic symmetrical metazoans from the Ediacaran Doushantuo Formation in the northeastern Guizhou, South China. Journal of China University of Geosciences, 19(3), 200-206. https://doi.org/10.1016/S1002-0705(08)60039-4.
[47] Wang, Y., Wang, Y., 2018. Globusphyton Wang et al., an Ediacaran macroalga, crept on the seafloor in the Yangtze Block, South China. Paleontological Research, 22(1), 64-74. https://doi.org/10.2517/2017PR005.
[48] Wang Y., Wang Y., Du W.,2017. A rare disc-like holdfast of the Ediacaran macroalga from South China. Journal of Paleontology, 91(6), 1091-1101. https://doi.org/10.1017/jpa.2017.43.
[49] Wang Y., Wang Y., Du W., Li Y.L., Liu F., Zhao M.S.,2021. Ediacaran pithy macroalga Lanceaphyton n. gen. from South China. Journal of Paleontology, 21, 1937-2337. https://doi.org/10.1017/jpa.2021.98.
[50] Wang Y., Wang Y., Du W., Wang X.L.,2014. The correlation between macroscopic algae and metazoans in the Ediacaran: A case study on the Wenghui biota in northeastern Guizhou, South China. Australian Journal of Earth Sciences, 61(7), 967-977. https://doi.org/10.1080/08120099.2014.956231.
[51] Wang Y., Wang Y., Du W., Wang X.L.,2015b. The Ediacaran macroalga Zhongbaodaophyton Chen et al. from South China. Alcheringa: An Australasian Journal of Palaeontology, 39(3), 377-387. https://doi.org/10.1080/03115518.2015.1001190.
[52] Wang Y., Wang Y., Du W., Wang X.L., 2016. New data of macrofossils in the Ediacaran Wenghui biota from Guizhou, South China. Acta Geologica Sinica - English Edition, 90(5), 1611-1628. https://doi.org/10.1111/1755-6724.12805.
[53] Wang Y., Wang Y., Tang F., Zhao M.S., 2020a. Ediacaran macroalgal holdfasts and their evolution: A case study from China. Palaeontology, 63(5), 821-840. https://doi.org/10.1111/pala.12485.
[54] Wang Y., Wang Y., Tang F., Zhao M.S., Liu P., 2020b. Lifestyle of the Octoradiate Eoandromeda in the Ediacaran. Paleontological Research, 24(1), 1-13. https://doi.org/10.2517/2019PR001.
[55] Wang Y., Zhao M.S., Yang Y.F., Wang X.L., 2009. Emergence of marco-organismal ecosystem of the Late Doushantuoian in South China and its significance.Journal of Palaeogeography (Chinese Edition), 11(6), 641-651 (in Chinese with English abstract).
[56] Wang Y.G., Qin S.R., Zhu S.C., Chen Y.L., Xie J.B., Liu Y.Z., Wei J.Y., 1987. Regional Geology of Guizhou Province. Beijing: Geological Publishing House, pp. 26-48 (in Chinese).
[57] Wu M.Y., Zhao Y.L., Peng J., Fu X.P., 2012. TheGesinella Steiner et al., 1992 from the Miaohe biota (Ediacaran) of Jiangkou, Guizhou Province. Acta Micropalaeontologica Sinica, 29(3), 312-319 (in Chinese with English abstract).
[58] Xiao S.H., Droser M., Gehling J.G., Hughes I.V., Wan B., Chen Z., Yuan X.L., 2013. Affirming life aquatic for the Ediacara biota in China and Australia.Geology, 41(10), 1095-1098.
[59] Xiao S.H., Yuan X.L., Steiner M., Knoll A.H., 2002. Macroscopic carbonaceous compressions in a terminal Proterozoic shale: A systematic reassessment of the Miaohe biota, South China. Journal of Paleontology, 76(2), 347-376. https://doi.org/10.1017/S0022336000041743.
[60] Xue Y.S., Tang T.F., Yu C.L.,1989. Stratigraphic division and correlation of Sinian in South Anhui and West Hunan. Journal of Stratigraphy, 13(1), 52-58. https://doi.org/10.19839/j.cnki.dcxzz.1989.01.008 (in Chinese with English abstract).
[61] Yang C., Rooney A.D., Condon D.J., Li X., Grazhdankin D.V., Bowyer F.T., Hu C., Macdonald F.A., Zhu M.Y., 2021. The tempo of Ediacaran evolution. Science Advances, 7(45), eabi9643. https://doi.org/10.1126/sciadv.abi9643.
[62] Ye Q., Tong J.N., An Z.H., Hu J., Tian L., Guan K.P., Xiao S.H.,2017. A systematic description of new macrofossil material from the upper Ediacaran Miaohe Member in South China. Journal of Systematic Palaeontology, 17(3), 183-238. https://doi.org/10.1080/14772019.2017.1404499.
[63] Ye Q., Tong J.N., Xiao S.H., Zhu S.X., An Z.H., Tian L., Hu J., 2015. The survival of benthic macroscopic phototrophs on a Neoproterozoic snowball Earth. Geology, 43(6), 507-510. https://doi.org/10.1130/G36640.1.
[64] Yuan X.L., Li J., Chen M.E.,1995. Development and their fossil records of metaphytes from Late Precambrian. Acta Palaeontologica Sinica, 34(1), 90-102. https://doi.org/10.19800/j.cnki.aps.1995.01.007
(in Chinese with English abstract).Yuan X.L., Li J., Cao R.J., 1999. A diverse metaphyte assemblage from the Neoproterozoic black shales of South China. Lethaia, 32(2), 143-155. https://doi.org/10.1111/j.1502-3931.1999.tb00533.x.
[65] Zhao Y.L., Chen M.E., Peng J., Yu M.Y., He M.H., Wang Y., Yang R.J., Wang P.L., Zhang Z.H., 2004. Discovery of a Miaohe-type biota from the Neoproterozoic Doushantuo Formation in Jiangkou County, Guizhou Province, China. Chinese Science Bulletin, 49(20), 2224-2226. https://doi.org/10.1007/BF03185792.
[66] Zhou C.M., Ouyang Q., Wang W., Wan B., Guan C.G., Chen Z., Yuan X.L., 2021. Lithostratigraphic subdivision and correlation of the Ediacaran in China. Journal of Stratigraphy, 45(3), 211-222 (in Chinese with English abstract). https://doi.org/10.19839/j.cnki.dcxzz.2021.0021.
[67] Zhou C.M., Xiao S.H., Wang W., Guan C.G., Ouyang Q., Chen Z.,2017. The stratigraphic complexity of the middle Ediacaran carbon isotopic record in the Yangtze Gorges area, South China, and its implications for the age and chemostratigraphic significance of the Shuram excursion. Precambrian Research, 288, 23-38. https://doi.org/10.1016/j.precamres.2016.11.007.
[68] Zhu B., Becker H., Jiang S.Y., Pi D.H.,Fischer-Gödde, M., Yang, J.H., 2013. Re-Os geochronology of black shales from the Neoproterozoic Doushantuo Formation, Yangtze Platform, South China. Precambrian Research, 225, 67-76. https://doi.org/10.1016/j.precamres.2012.02.002.
[69] Zhu M.Y., Gehling J.G., Xia S.H., Zhao Y.L., Droser M.L., 2008. Eight-armed Ediacara fossil preserved in contrasting taphonomic windows from China and Australia. Geology, 36(11), 867-870. https://doi.org/10.1130/G25203A.1.
[70] 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.
[71] Zhu W.Q., Chen M.E., 1984. On the discovery of macrofossil algae from the Late Sinian in the eastern Yangtze Gorges, South China.Acta Botanica Sinica, 26(5), 558-560. |