Biogeochemical status of the Paleo-Pacific Ocean: clues from the early Cambrian of South Australia

References

• Abanda, P. A., & Hannigan, R. E. (2006). Effect of diagenesis on trace element partitioning in shales. Chemical Geology, 230(1–2), 42–59. https://doi.org/10.1016/j.chemgeo.2005.11.011
   Web of Science ®Google Scholar
• Adelson, J. M., Helz, G. R., & Miller, C. V. (2001). Reconstructing the rise of recent coastal anoxia; molybdenum in Chesapeake Bay sediments. Geochimica et Cosmochimica Acta, 65(2), 237–252. https://doi.org/10.1016/S0016-7037(00)00539-1
   Web of Science ®Google Scholar
• Algeo, T. J., & Lyons, T. W. (2006). Mo–total organic carbon covariation in modern anoxic marine environments: Implications for analysis of paleoredox and paleohydrographic conditions. Paleoceanography and Paleoceanography, 21(1), N/A–N/A. https://doi.org/10.1029/2004PA001112
   Google Scholar
• Babcock, L. E. (2003). Trilobites in Paleozoic predator–prey systems, and their role in reorganization of early Paleozoic ecosystems. In P. H. Kelley, M. Kowalewski & T. A. Hansen (Eds.), Predator–Prey interactions in the fossil record (pp. 55–92). Kluwer Academic/Plenum Publishers.
   Google Scholar
• Bau, M., & Dulski, P. (1996). Distribution of yttrium and rare-earth elements in the Peng and Kuruman iron-formations. Precambrian Research, 79(1–2), 37–55. https://doi.org/10.1016/0301-9268(95)00087-9
   Web of Science ®Google Scholar
• Berry, W. B. N., & Wilde, P. (1978). Progressive ventilation of the oceans; an explanation for the distribution of the lower Paleozoic black shales. American Journal of Science, 278(3), 257–275. https://doi.org/10.2475/ajs.278.3.257
   Web of Science ®Google Scholar
• Betts, M. J., Claybourn, T. M., Brock, G. A., Jago, J. B., Skovsted, C. B., & Paterson, J. R. (2019). Shelly fossils from the lower Cambrian White Point Conglomerate, Kangaroo Island, South Australia. Acta Palaeontologica Polonica, 64, 489–522. https://doi.org/10.4202/app.00586.2018
   Web of Science ®Google Scholar
• Betts, M. J., Paterson, J. R., Jacquet, S. M., Andrew, A. S., Hall, P. A., Jago, J. B., Jagodzinski, E. A., Preiss, W. V., Crowley, J. L., Brougham, T., Mathewson, C. P., García-Bellido, D. C., Topper, T. P., Skovsted, C. B., & Brock, G. A. (2018). Early Cambrian chronostratigraphy and geochronology of South Australia. Earth-Science Reviews, 185, 498–543. https://doi.org/10.1016/j.earscirev.2018.06.005
   Web of Science ®Google Scholar
• Bharati, S., Patience, R. L., Larter, S. R., Standen, G., & Poplett, I. J. (1995). Elucidation of the Alum Shale kerogen structure. Organic Geochemistry, 23(11–12), 1043–1058. https://doi.org/10.1016/0146-6380(95)00089-5
   Web of Science ®Google Scholar
• Bhatia, M. R., & Crook, K. A. W. (1986). Trace element characteristics of greywackes and tectonic setting discrimination of sedimentary basins. Contributions to Mineralogy and Petrology, 92(2), 181–193. https://doi.org/10.1007/BF00375292
   Web of Science ®Google Scholar
• Boyer, D. L., Owens, J. D., Lyons, T. W., & Droser, M. L. (2011). Joining forces: Combined biological and geochemical proxies reveal a complex but refined high-resolution palaeo-oxygen history in Devonian epeiric seas. Palaeogeography, Palaeoclimatology, Palaeoecology, 306(3–4), 134–146. https://doi.org/10.1016/j.palaeo.2011.04.012
   Web of Science ®Google Scholar
• Brasier, M. D. (1992). Background to the Cambrian explosion. Journal of the Geological Society, 149(4), 585–587. https://doi.org/10.1144/gsjgs.149.4.0585
   Google Scholar
• Brasier, M. D., & Hewitt, R. A. (1979). Environmental setting of fossiliferous rocks from the uppermost Proterozoic–lower Cambrian of central England. Palaeogeography, Palaeoclimatology, Palaeoecology, 27, 35–57. https://doi.org/10.1016/0031-0182(79)90092-0
   Web of Science ®Google Scholar
• Brennan, S. T., Lowenstein, T. K., & Horita, J. (2004). Seawater chemistry and the advent of biocalcification. Geology, 32(6), 473–476. https://doi.org/10.1130/G20251.1
   Web of Science ®Google Scholar
• Brock, G. A., Engelbretsen, M. J., Jago, J. B., Kruse, P. D., Laurie, J. R., Shergold, J. H., Shi, G. R., & Sorauf, J. E. (2000). Palaeobiogeographic affinities of Australian Cambrian faunas. Association of Australasian Palaeontologists, Memoir 23, 61.
   Google Scholar
• Brock, G. A., Jago, J. B., Kruse, P. D., Betts, M. J., Jacquet, S. M., Paterson, J. R., & García-Bellido, D. C. (2016). Cambrian of the Stansbury and Arrowie Basins. In P. D. Kruse & J. B. Jago (Eds.), Palaeo down under 2. Geological field excursion guide: Cryogenian–Ediacaran–Cambrian of the Adelaide Fold Belt (pp. 10–24). Department of State Development. Report Book 2016/00011.
   Google Scholar
• Calvert, D. E., & Pedersen, T. F. (1993). Geochemistry of Recent oxic and anoxic marine sediments: Implications for the geological record. Marine Geology, 113(1–2), 67–88. https://doi.org/10.1016/0025-3227(93)90150-T
   Web of Science ®Google Scholar
• Canfield, D. E. (1998). A new model for Proterozoic ocean chemistry. Nature, 396(6710), 450–453. https://doi.org/10.1038/24839
   Web of Science ®Google Scholar
• Canfield, D. E., & Farquhar, J. (2009). Animal evolution, bioturbation, and the sulfate concentration of the oceans. Proceedings of the National Academy of Sciences of the United States of America, 106(20), 8123–8127. https://doi.org/10.1073/pnas.0902037106
   PubMed Web of Science ®Google Scholar
• Canfield, D. E., Olesen, C. A., & Raymond, P. C. (2006). Temperature and its control of isotope fractionation by a sulphate-reducing bacterium. Geochimica et Cosmochimica Acta, 70(3), 548–561. https://doi.org/10.1016/j.gca.2005.10.028
   Web of Science ®Google Scholar
• Canfield, D. E., Poulton, S. W., & Narbonne, G. M. (2007). Late-Neoproterozoic deep-ocean oxygenation and the rise of animal life. Science (New York, N.Y.), 315(5808), 92–95. https://doi.org/10.1126/science.1135013
   PubMed Web of Science ®Google Scholar
• Canfield, D. E., & Teske, A. (1996). Late Proterozoic rise in atmospheric oxygen concentration inferred from phylogenetic and sulphur-isotope studies. Nature, 382(6587), 127–132. https://doi.org/10.1038/382127a0
   PubMed Web of Science ®Google Scholar
• Carson, M. (1994). The stratigraphy, sedimentology and thermal history of the Early Cambrian Heatherdale Shale, Fleurieu Peninsula [unpublished B.Sc. Honours thesis]. University of Adelaide.
   Google Scholar
• Chen, F., Brock, G. A., Betts, M. J., Zhang, Z., Yun, H., Klaebe, R. M., Laing, B., & Zhang, Z. (2020). Sedimentology and integrated chronostratigraphy of the lower Heatherdale Shale (Cambrian, stages 2–3), Stansbury Basin, South Australia. Geological Magazine, 1–13. https://doi.org/10.1017/S0016756820001260
   Google Scholar
• Chen, J., Algeo, T. J., Zhao, L., Chen, Z-Q., Cao, L., Zhang, L., & Li, Y. (2015). Diagenetic uptake of rare earth elements by bioapatite, with an example from Lower Triassic conodonts of South China. Earth-Science Reviews, 149, 181–202. https://doi.org/10.1016/j.earscirev.2015.01.013
   Web of Science ®Google Scholar
• Clark, C., Kinny, P. D., & Harley, S. L. (2012). Sedimentary provenance and age of metamorphism of the Vestfold Hills, East Antarctica: Evidence for a piece of Chinese Antarctica? Precambrian Research, 196-197, 23–45. https://doi.org/10.1016/j.precamres.2011.11.001
   Web of Science ®Google Scholar
• Claypool, G. E., Holser, W. T., Kaplan, I. R., Sakai, H., & Zak, I. (1980). Age curves of sulphur and oxygen isotopes in marine sulphate and their mutual interpretation. Chemical Geology, 28, 199–206. https://doi.org/10.1016/0009-2541(80)90047-9
   Web of Science ®Google Scholar
• Collins, A. S., Kröner, A., Fitzsimons, I. C. W., & Razakamanana, T. (2003). Detrital footprint of the Mozambique ocean: U–Pb SHRIMP and Pb evaporation zircon geochronology of metasedimentary gneisses in eastern Madagascar. Tectonophysics, 375(1–4), 77–99. https://doi.org/10.1016/S0040-1951(03)00334-2
   Web of Science ®Google Scholar
• Collins, A. S., & Pisarevsky, S. A. (2005). Amalgamating eastern Gondwana: The evolution of the Circum-Indian Orogens. Earth-Science Reviews, 71(3–4), 229–270. https://doi.org/10.1016/j.earscirev.2005.02.004
   Web of Science ®Google Scholar
• Cox, G., Sansjofre, P., Blades, M. L., Farkas, J., & Collins, A. S. (2019). Dynamic interaction between basin redox and the biogeochemical nitrogen cycle in an unconventional Proterozoic petroleum system. Scientific Reports, 9(1), 5200. https://doi.org/10.1038/s41598-019-40783-4
   PubMedGoogle Scholar
• Daily, B., & Milnes, A. R. (1973). Stratigraphy, structure and metamorphism of the Kanmantoo Group (Cambrian) in its type section east of Tunkalilla Beach, South Australia. Transactions of the Royal Society of South Australia, 97, 199–214.
   Google Scholar
• Daily, B., Milnes, A. R., Twidale, C. R., & Bourne, J. A. (1979). Geology and geomorphology. In M. J. Tyler, J. K. Ling & C. R. Twidale (Eds.), Natural History of Kangaroo Island (pp. 1–38). Royal Society of South Australia.
   Google Scholar
• Daily, B., Moore, P. S., & Rust, B. R. (1980). Terrestrial–marine transition in the Cambrian rocks of Kangaroo Island, South Australia. Sedimentology, 27(4), 379–399. https://doi.org/10.1111/j.1365-3091.1980.tb01189.x
   Web of Science ®Google Scholar
• Daley, A. C., Paterson, J. R., Edgecombe, G. D., García-Bellido, D. C., & Jago, J. B. (2013). New anatomical information on Anomalocaris from the Cambrian Emu Bay Shale of South Australia and a reassessment of its preferred predatory habits. Palaeontology, 56, 971–990. https://doi.org/10.1111/pala.12029
   Web of Science ®Google Scholar
• Debrenne, F., & Gravestock, D. (1990). Archaeocyatha from the Sellick Hill Formation and Fork Tree Limestone on Fleurieu Peninsula, South Australia. In J. B. Jago & P. J. Moore (Eds), The evolution of a late Precambrian–early Palaeozoic rift complex: The Adelaide Geosyncline (pp. 290–309). Geological Society of Australia, Special Publication. 16.
   Google Scholar
• Derry, L. A., Kaufman, A. J., & Jacobsen, S. (1992). Sedimentary cycling and environmental change in the Late Proterozoic: Evidence from stable and radiogenic isotopes. Geochimica et Cosmochimica Acta, 56(3), 1317–1329. https://doi.org/10.1016/0016-7037(92)90064-P
   Web of Science ®Google Scholar
• Dong, X., Zhang, Z., Santosh, M., Wang, W., Yu, F., & Liu, F. (2011). Late Neoproterozoic thermal events in the northern Lhasa terrane, south Tibet: Zircon chronology and tectonic implications. Journal of Geodynamics, 52(5), 389–405. https://doi.org/10.1016/j.jog.2011.05.002
   Web of Science ®Google Scholar
• Erwin, D. H., Laflamme, M., Tweedt, S. M., Sperling, E. A., Pisani, D., & Peterson, K. J. (2011). The Cambrian conundrum: Early divergence and later ecological success in the early history of animals. Science (New York, N.Y.), 334(6059), 1091–1097. https://doi.org/10.1126/science.1206375
   PubMed Web of Science ®Google Scholar
• Felitsyn, S., & Morad, S. (2002). REE patterns in latest Neoproterozoic–early Cambrian phosphate concretions and associated organic matter. Chemical Geology, 187(3–4), 257–265. https://doi.org/10.1016/S0009-2541(02)00046-3
   Web of Science ®Google Scholar
• Fike, D. A., & Grotzinger, J. P. (2008). A paired sulfate–pyrite δ34S approach to understanding the evolution of the Ediacaran–Cambrian sulfur cycle. Geochimica et Cosmochimica Acta, 72(11), 2636–2648. https://doi.org/10.1016/j.gca.2008.03.021
   Web of Science ®Google Scholar
• Fike, D. A., Grotzinger, J. P., Pratt, L. M., & Summons, R. E. (2006). Oxidation of the Ediacaran Ocean. Nature, 444(7120), 744–747. https://doi.org/10.1038/nature05345
   PubMed Web of Science ®Google Scholar
• Fioretti, A. M., Black, L. P., Foden, J., & Visonà, D. (2005). Grenville-age magmatism at the South Tasman Rise (Australia): A new piercing point for the reconstruction of Rodinia. Geology, 33(10), 769–772. https://doi.org/10.1130/G21671.1
   Web of Science ®Google Scholar
• Flöttmann, T., & James, P. (1997). Influence of basin architecture on the style of inversion and fold-thrust belt tectonics—The southern Adelaide Fold-Thrust Belt, South Australia. Journal of Structural Geology, 19(8), 1093–1110. https://doi.org/10.1016/S0191-8141(97)00033-3
   Web of Science ®Google Scholar
• Flöttmann, T., Haines, P. W., Cockshell, C. D., & Preiss, W. V. (1998). Reassessment of the seismic stratigraphy of the Early Palaeozoic Stansbury Basin, Gulf St Vincent, South Australia. Australian Journal of Earth Sciences, 45(4), 547–557. https://doi.org/10.1080/08120099808728411
   Web of Science ®Google Scholar
• Foden, J., Elburg, M., Turner, S., Clark, C., Blades, M. L., Cox, G., Collins, A. S., Wolff, K., & George, C. (2020). Cambro-Ordovician magmatism in the Delamerian orogeny: Implications for tectonic development of the southern Gondwanan margin. Gondwana Research, 81, 490–521. https://doi.org/10.1016/j.gr.2019.12.006
   Web of Science ®Google Scholar
• Foden, J. D., Elburg, M. A., Dougherty-Page, J., & Burtt, A. (2006). The timing and duration of the Delamerian Orogeny: Correlation with the Ross Orogen and implications for Gondwana assembly. The Journal of Geology, 114(2), 189–210. https://doi.org/10.1086/499570
   Web of Science ®Google Scholar
• Foden, J. D., Sandiford, M., Dougherty-Page, J., & Williams, I. (1999). The geochemistry and geochronology of the Rathjen Gneiss: Implications for the early tectonic evolution of the Delamerian Orogen. Australian Journal of Earth Sciences, 46(3), 377–389. https://doi.org/10.1046/j.1440-0952.1999.00712.x
   Web of Science ®Google Scholar
• Foden, J. D., Turner, S. P., & Morrison, R. (1990). The tectonic implications of the Delamerian magmatism in South Australia and western Victoria. In J. B. Jago & P. S. Moore (Eds.), The evolution of a Late Precambrian–Early Palaeozoic Rift Complex: The Adelaide Geosyncline (pp. 483–495). Geological Society of Australia Special Publication. 16.
   Google Scholar
• Gaines, R. R., & Droser, M. L. (2010). The paleoredox setting of Burgess Shale-type deposits. Palaeogeogaphy, Palaeoclimatology, Palaeoecology, 297(3–4), 649–661. https://doi.org/10.1016/j.palaeo.2010.09.014
   Web of Science ®Google Scholar
• Gaines, R. R., Paterson, J. R., Jago, J. B., Gehling, J. G., & García-Bellido, D. C. (2016). Palaeoenvironmental and depositional setting of the Emu Bay Shale, a unique early Cambrian Lagerstätte. Geological Society of Australia Abstracts, 117, 29.
   Google Scholar
• García-Bellido, D. C., Paterson, J. R., Edgecombe, G. D., Jago, J. B., Gehling, J. G., & Lee, M. S. Y. (2009). The bivalved arthropods Isoxys and Tuzoia with soft-part preservation from the Lower Cambrian Emu Bay Shale Lagerstätte (Kangaroo Island, Australia. Palaeontology, 52(6), 1221–1241. https://doi.org/10.1111/j.1475-4983.2009.00914.x
   Google Scholar
• Garver, J. I., & Scott, T. J. (1995). Trace elements in shale as indicators of crustal provenance and terrane accretion in the southern Canadian Cordillera. Geological Society of America Bulletin, 107(4), 440–453. https://doi.org/10.1130/0016-7606(1995)107<0440:TEISAI>2.3.CO;2
   Web of Science ®Google Scholar
• Gatehouse, C. G., Jago, J. B., & Cooper, B. J. (1990). Sedimentology and stratigraphy of the Carrickalinga Head Formation (low stand fan to high stand systems tract), Kanmantoo Group, South Australia. In J. B. Jago & P. S. Moore (Eds.), The evolution of a Late Precambrian–Early Palaeozoic rift complex: The Adelaide geosyncline (pp. 351–368). Geological Society of Australia Special Publication. 16.
   Google Scholar
• Gatehouse, C. G., Jago, J. B., Clough, B. J., & McCulloch, A. J. (1993). The Early Cambrian volcanics from Red Creek, eastern Mt Lofty Ranges, South Australia. Transactions of the Royal Society of South Australia, 117, 57–66.
   Google Scholar
• Gehling, J. G., Jago, J. B., Paterson, J. R., García-Bellido, D. C., & Edgecombe, G. D. (2011). The geological context of the lower Cambrian (Series 2) Emu Bay Shale Lagerstätte and adjacent stratigraphic units, Kangaroo Island, South Australia. Australian Journal of Earth Sciences, 58(3), 243–257. https://doi.org/10.1080/08120099.2011.555487
   Web of Science ®Google Scholar
• Gill, B. C., Lyons, T. W., Young, S. A., Kump, L. R., Knoll, A. H., & Saltzman, M. R. (2011). Geochemical evidence for widespread euxinia in the Late Cambrian ocean. Nature, 469(7328), 80–83. https://doi.org/10.1038/nature09700
   PubMed Web of Science ®Google Scholar
• Goldberg, T., Poulton, S. W., & Strauss, H. (2005). Sulphur and oxygen isotope signatures of late Neoproterozoic to early Cambrian sulphate, Yangtze Platform, China: Diagenetic constraints and seawater evolution. Precambrian Research, 137(3–4), 223–241. https://doi.org/10.1016/j.precamres.2005.03.003
   Web of Science ®Google Scholar
• Goldberg, T., Strauss, H., Guo, Q., & Liu, C. (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
   Web of Science ®Google Scholar
• Gorjan, P., Walter, M. R., & Swart, R. (2003). Global Neoproterozoic (Sturtian) post-glacial sulfide-sulfur isotope anomaly recognised in Namibia. Journal of African Earth Sciences, 36(1–2), 89–98. https://doi.org/10.1016/S0899-5362(03)00002-2
   Web of Science ®Google Scholar
• Gravestock, D. I. (1995). Early and Middle Palaeozoic. In J. F. Drexel & W. V. Preiss (Eds.), The Geology of South Australia, Vol. 2: The Phanerozoic (pp. 3–61). South Australia Geological Survey Bulletin. 54.
   Google Scholar
• Gravestock, D. I., Alexander, E. M., Demidenko, Y. E., Esakova, N. B., Holmer, L. E., Jago, J. B., Lin, T. R., Melnikova, N., Parhaev, P. Y., Rozanov, A. Y., Ushatinskaya, G. T., Zang, W. L., Zhegallo, E. A., & Zhuravlev, A. Y. (2001). The Cambrian biostratigraphy of the Stansbury Basin, South Australia. Russian Academy of Sciences. Transactions of the Palaeontological Institute, 282, 1–341.
   Google Scholar
• Gum, J. C. (1998). The sedimentology, sequence stratigraphy and mineralisation of the Silverton Subgroup [unpublished PhD thesis]. South Australia University of South Australia.
   Google Scholar
• Guo, Q., Shields, G. A., Liu, C., Strauss, H., Zhu, M., Pi, D., Goldberg, T., & Yang, X. (2007). Trace element chemostratigraphy of two Ediacaran–Cambrian successions in South China: Implications for organosedimentary metal enrichment and silicification in the early Cambrian. Palaeogeography, Palaeoclimatology, Palaeoecology, 254(1–2), 194–216. https://doi.org/10.1016/j.palaeo.2007.03.016
   Web of Science ®Google Scholar
• Haines, P. W., Flöttmann, T., Gum, J. C., Jago, J. B., & Gatehouse, C. G. (1996). Integrated approach to the reinterpretation of the Cambrian Kanmantoo Group type section, South Australia. Geological Society of Australia Abstracts, 41, 77.
   Google Scholar
• Haines, P. W., Jago, J. B., & Gum, J. C. (2001). Turbidite deposition in the Cambrian Kanmantoo Group, South Australia. Australian Journal of Earth Sciences, 48(3), 465–478. https://doi.org/10.1046/j.1440-0952.2001.00872.x
   Web of Science ®Google Scholar
• Haines, P. W., Turner, S. P., Foden, J., & Jago, J. (2009). Isotopic and geochemical characterization of the Cambrian Kanmantoo Group, South Australia: Implications for stratigraphy and provenance. Australian Journal of Earth Sciences, 56(8), 1095–1110. https://doi.org/10.1080/08120090903246212
   Web of Science ®Google Scholar
• Hall, P. A., McKirdy, D. M., Halverson, G. P., Jago, J. B., & Gehling, J. G. (2011). Biomarker and isotopic signatures of an early Cambrian Lagerstätte in the Stansbury Basin, South Australia. Organic Geochemistry, 42(11), 1324–1330. https://doi.org/10.1016/j.orggeochem.2011.09.003
   Web of Science ®Google Scholar
• Halverson, G. P., & Hurtgen, M. T. (2007). Ediacaran growth of the marine sulfate reservoir. Earth and Planetary Science Letters, 263(1–2), 32–44. https://doi.org/10.1016/j.epsl.2007.08.022
   Web of Science ®Google Scholar
• Halverson, G. P., Hurtgen, M. T., Porter, S. M., & Collins, A. S. (2009). Neoproterozoic–Cambrian biogeochemical evolution. In C. Gaucher, A. N. Sial, G. P. Halverson & H. E. Frimmel (Eds.), Developments in Precambrian Geology (Vol. 16, pp. 351–365). Elsevier.
   Google Scholar
• Hatch, J. R., & Leventhal, J. S. (1992). Relationship between inferred redox potential of the depositional environment and geochemistry of the Upper Pennsylvanian (Missourian) Stark Shale Member of the Dennis Limestone, Wabaunsee County, Kansas, U.S.A. Chemical Geology, 99(1–3), 65–82. https://doi.org/10.1016/0009-2541(92)90031-Y
   Web of Science ®Google Scholar
• Helly, J. J., & Levin, L. A. (2004). Global distribution of naturally occurring marine hypoxia on continental margins. Deep Sea Research Part I: Oceanographic Research Papers, 51(9), 1159–1168. https://doi.org/10.1016/j.dsr.2004.03.009
   Web of Science ®Google Scholar
• Helz, G. R., Miller, C. V., Charnock, J. M., Mosselmans, J. L. W., Pattrick, R. A. D., Garner, C. D., & Vaughan, D. J. (1996). Mechanisms of molybdenum removal from the sea and its concentration in black shales: EXAFS evidence. Geochimica et Cosmochimica Acta, 60(19), 3631–3642. https://doi.org/10.1016/0016-7037(96)00195-0
   Web of Science ®Google Scholar
• Hofmann, M., Linnemann, U., Rai, V., Becker, S., Gärtner, A., & Sagawe, A. (2011). The India and South China cratons at the margin of Rodinia—Synchronous Neoproterozoic magmatism revealed by LA-ICP-MS zircon analyses. Lithos, 123(1–4), 176–187. https://doi.org/10.1016/j.lithos.2011.01.012
   Web of Science ®Google Scholar
• Holmes, J. D., Paterson, J. R., & García-Bellido, D. C. (2020a). The trilobite Redlichia from the lower Cambrian Emu Bay Shale Konservat-Lagerstätte of South Australia: Systematics, ontogeny and soft-part anatomy. Journal of Systematic Palaeontology, 18(4), 295–334. https://doi.org/10.1080/14772019.2019.1605411
   Web of Science ®Google Scholar
• Holmes, J. D., Paterson, J. R., & García-Bellido, D. C. (2020b). The post-embryonic ontogeny of the early Cambrian trilobite Estaingia bilobata from South Australia: Trunk development and phylogenetic implications. Papers in Palaeontology. https://doi.org/10.1002/spp2.1323
   Google Scholar
• Holser, W. T. (1997). Evaluation of the application of rare-earth elements to paleoceanography. Palaeogeography, Palaeoclimatology, Palaeoecology, 132(1–4), 309–323. https://doi.org/10.1016/S0031-0182(97)00069-2
   Web of Science ®Google Scholar
• Holser, W., & Kaplan, I. (1966). Isotope geochemistry of sedimentary sulfates. Chemical Geology, 1, 93–135. https://doi.org/10.1016/0009-2541(66)90011-8
   Google Scholar
• Hurtgen, M. T., Arthur, M. A., Suits, N. S., & Kaufman, A. J. (2002). The sulfur isotopic composition of Neoproterozoic seawater sulfate: Implications for a snowball Earth? Earth and Planetary Science Letters, 203(1), 413–430. https://doi.org/10.1016/S0012-821X(02)00804-X
   Web of Science ®Google Scholar
• Ireland, T. R., Flöttmann, T., Fanning, C. M., Gibson, G. M., & Preiss, W. V. (1998). Development of the early Paleozoic Pacific margin of Gondwana from detrital zircon ages across the Delamerian orogen. Geology, 26(3), 243–246. https://doi.org/10.1130/0091-7613(1998)026<0243:DOTEPP>2.3.CO;2
   Web of Science ®Google Scholar
• Jacquet, S. M., Jago, J. B., & Brock, G. A. (2016). An enigmatic univalve mollusc from the lower Cambrian (Series 2, Stage 3) Heatherdale Shale, South Australia. Australasian Palaeontological Memoirs, 49, 21–30.
   Google Scholar
• Jago, J. B., Bentley, C. J., Paterson, J. R., Holmes, J. D., Lin, T. R., & Sun, X. W. (2021). The stratigraphic significance of early Cambrian (Series 2, Stage 4) trilobites from the Smith Bay Shale near Freestone Creek. Kangaroo Island. Australian Journal of Earth Sciences, 68(2), 205–213. https://doi.org/10.1080/08120099.2020.1749882
   Web of Science ®Google Scholar
• Jago, J. B., Daily, B., von der Borch, C. C., Cernovskis, A., & Saunders, N. (1984). First reported trilobites from the Lower Cambrian Normanville Group, Fleurieu Peninsula, South Australia. Transactions of the Royal Society of South Australia, 108, 207–211.
   Google Scholar
• Jago, J. B., Dyson, I. A., & Gatehouse, C. G. (1994). The nature of the sequence boundary between the Normanville and Kanmantoo Groups on Fleurieu Peninsula, South Australia. Australian Journal of Earth Sciences, 41(5), 445–453. https://doi.org/10.1080/08120099408728154
   Web of Science ®Google Scholar
• Jago, J. B., & Gatehouse, C. G. (2009). The type section of the Cambrian Backstairs Passage Formation, Kanmantoo Group, South Australia. Transactions of the Royal Society of South Australia, 133(1), 150–163. https://doi.org/10.1080/03721426.2009.10887114
   Web of Science ®Google Scholar
• Jago, J. B., Gehling, J. G., Paterson, J. R., Brock, G. A., & Zang, W. L. (2012). Cambrian stratigraphy and biostratigraphy of the Flinders Ranges and the north coast of Kangaroo Island, South Australia. Episodes, 35(1), 247–255. https://doi.org/10.18814/epiiugs/2012/v35i1/024
   Web of Science ®Google Scholar
• Jago, J. B., Gum, J. C., Burtt, A. C., & Haines, P. W. (2003). Stratigraphy of the Kanmantoo Group: A critical element of the Adelaide Fold Belt and the Palaeo-Pacific plate margin, Eastern Gondwana. Australian Journal of Earth Sciences, 50(3), 343–363. https://doi.org/10.1046/j.1440-0952.2003.00997.x
   Web of Science ®Google Scholar
• Jago, J. B., & Kruse, P. D. (2020). Significance of the middle Cambrian (Wuliuan) trilobite Pagetia from Yorke Peninsula, South Australia. Australian Journal of Earth Sciences, 67(7), 1003–1008. https://doi.org/10.1080/08120099.2019.1643405
   Web of Science ®Google Scholar
• Jago, J. B., Sun, X., & Zang, W. (2002). Correlation within early Palaeozoic basins of eastern South Australia (2002/033). PIRSA Report Book.
   Google Scholar
• Jago, J. B., Zang, W., Sun, X., Brock, G. A., Paterson, G. A., & Skovsted, C. (2006). A review of the Cambrian biostratigraphy of South Australia. Palaeoworld, 15(3–4), 406–488. https://doi.org/10.1016/j.palwor.2006.10.014
   Google Scholar
• James, P. R., & Clark, I. F. (2002). Geology. In M. Davies, C. R. Twidale & M. J. Tyler (Eds.), Natural History of Kangaroo Island (2nd ed., pp. 1–22). Royal Society of South Australia.
   Google Scholar
• Jenkins, R. J. F., Cooper, J. C., & Compston, W. (2002). Age and biostratigraphy of Early Cambrian tuffs from SE Australia and southern China. Journal of the Geological Society of Society, London, 159(6), 645–658. https://doi.org/10.1144/0016-764901-127
   Google Scholar
• Jenkins, R. J. F., & Hasenohr, P. (1989). Trilobites and their trails in a black shale: Early Cambrian of the Fleurieu Peninsula, South Australia. Transactions of the Royal Society of South Australia, 113, 195–203.
   Google Scholar
• Jiang, S. Y., Zhao, H. X., Chen, Y. Q., Yang, T., Yang, J. H., & Ling, H. F. (2007). Trace and rare earth element geochemistry of phosphate nodules from the lower Cambrian black shale sequence in the Mufu Mountain of Nanjing, Jiangsu province, China. Chemical Geology, 244(3–4), 584–604. https://doi.org/10.1016/j.chemgeo.2007.07.010
   Web of Science ®Google Scholar
• Johnston, D. T., Farquhar, J., & Canfield, D. E. (2007). Sulfur isotope insight into microbial sulphate reduction: When microbes meet models. Geochimica et Cosmochimica Acta, 71(16), 3929–3947. https://doi.org/10.1016/j.gca.2007.05.008
   Web of Science ®Google Scholar
• Jones, B., & Manning, D. A. C. (1994). Comparison of geochemical indices used for the interpretation of palaeoredox conditions in ancient mudstones. Chemical Geology, 111(1–4), 111–129. https://doi.org/10.1016/0009-2541(94)90085-X
   Web of Science ®Google Scholar
• Keeman, J., Turner, S., Haines, P. W., Belousova, E., Ireland, T., Brouwer, P., Foden, J., & Wörner, G. (2020). New U–Pb, Hf and O isotope constraints on the provenance of sediments from the Adelaide Rift Complex—documenting the key Neoproterozoic to early Cambrian succession. Gondwana Research, 83, 248–278. https://doi.org/10.1016/j.gr.2020.02.005
   Web of Science ®Google Scholar
• Kelsey, D. E., Wade, B. P., Collins, A. S., Hand, M., Sealing, C. R., & Netting, A. (2008). Discovery of a Neoproterozoic basin in the Prydz belt in East Antarctica and its implications for Gondwana assembly and ultrahigh temperature metamorphism. Precambrian Research, 161(3–4), 355–388. https://doi.org/10.1016/j.precamres.2007.09.003
   Web of Science ®Google Scholar
• Kenig, F., Hudson, J. D., Sinninghe Damsté, J. S., & Popp, B. N. (2004). Intermittent euxinia: Reconciliation of a Jurassic black shale with its biofacies. Geology, 32(5), 421–424. https://doi.org/10.1130/G20356.1
   Web of Science ®Google Scholar
• Kennedy, M. J., Pevear, D. R., & Hill, R. J. (2002). Mineral surface control of organic carbon in black shale. Science, 295(5555), 657–660. https://doi.org/10.1126/science.1066611
   PubMed Web of Science ®Google Scholar
• Kennedy, M. J., & Wagner, T. (2011). Clay mineral continental amplifier for marine carbon sequestration in a greenhouse ocean. Proceedings of the National Academy of Sciences, 108(24), 9776–9781. https://doi.org/10.1073/pnas.1018670108
   PubMed Web of Science ®Google Scholar
• Kidder, D. L., Krishnaswamy, R., & Mapes, R. H. (2003). Elemental mobility in phosphatic shales during concretion growth and implications for provenance analysis. Chemical Geology, 198(3–4), 335–353. https://doi.org/10.1016/S0009-2541(03)00036-6
   Web of Science ®Google Scholar
• Kimura, H., & Watanabe, Y. (2001). Oceanic anoxia at the Precambrian–Cambrian boundary. Geology, 29(11), 995–998. https://doi.org/10.1130/0091-7613(2001)029<0995:OAATPC>2.0.CO;2
   Web of Science ®Google Scholar
• Klemme, H. D., & Ulmishek, G. F. (1991). Effective petroleum source rocks of the world: Stratigraphic distribution and controlling depositional factors. American Association of Petroleum Geologists Bulletin, 75, 1809–1851.
   Web of Science ®Google Scholar
• Lee, M. S. Y., Jago, J. B., García-Bellido, D. C., Edgecombe, G. D., Gehling, J. G., & Paterson, J. R. (2011). Modern optics in exceptionally preserved eyes of Early Cambrian arthropods from Australia. Nature, 474(7353), 631–634. https://doi.org/10.1038/nature10097
   PubMed Web of Science ®Google Scholar
• Lehmann, B., Nägler, T. F., Holland, H. D., Wille, M., Mao, J., Pan, J., Ma, D., & Dulski, P. (2007). Highly metalliferous carbonaceous shale and early Cambrian seawater. Geology, 35(5), 403–406. https://doi.org/10.1130/G23543A.1
   Web of Science ®Google Scholar
• Li, Z. X., Bogdanova, S. V., Collins, A. S., Davidson, A., De Waele, B., Ernst, R. E., Fitzsimons, I. C. W., Fuck, R. A., Gladkochub, D. P., Jacobs, J., Karlstrom, K. E., Lu, S., Natapov, L. M., Pease, V., Pisarevsky, S. A., Thrane, K., & Vernikovsky, V. (2008). Assembly, configuration, and break-up history of Rodinia: A synthesis. Precambrian Research, 160(1–2), 179–210. https://doi.org/10.1016/j.precamres.2007.04.021
   Web of Science ®Google Scholar
• Lindsay, J. F. (2002). Supersequences, superbasins, supercontinents—Evidence from the Neoproterozoic basins of Central Australia. Basin Research, 14(2), 207–223. https://doi.org/10.1046/j.1365-2117.2002.00170.x
   Web of Science ®Google Scholar
• Lloyd, J., Blades, M. L., Counts, J., Collins, A. S., Amos, K., Wade, B., Hall, J., Hore, S., Ball, A., Shahin, S., & Drabsch, M. (2020). Neoproterozoic geochronology and provenance of the Adelaide Superbasin. Precambrian Research, 350, 105849. https://doi.org/10.1016/j.precamres.2020.105849
   Web of Science ®Google Scholar
• Mancktelow, N. S. (1990). The structure of the southern Adelaide Fold Belt, South Australia. In J. B. Jago & P. S. Moore (Eds.), The evolution of a late Precambrian–Early Palaeozoic rift complex: The Adelaide Geosyncline (pp. 369–395). Geological Society of Australia Special Publication. 16.
   Google Scholar
• McKenzie, N. R., Hughes, N. C., Myrow, P. M., Choi, D. K., & Park, T. (2011). Trilobites and zircons link north China with the eastern Himalaya during the Cambrian. Geology, 39(6), 591–594. https://doi.org/10.1130/G31838.1
   Web of Science ®Google Scholar
• McKirdy, D. M. (1994). Biomarker geochemistry of the Early Cambrian oil show in Wilkatana-1: Implications for oil generation in the Arrowie and Stansbury Basins. PESA Journal, 22, 3–17.
   Google Scholar
• McKirdy, D. M., Hall, P. A., Nedin, C., Halverson, G. P., Michaelsen, B. H., Jago, J. B., Gehling, J. G., & Jenkins, R. J. F. (2011). Palaeoredox status and thermal alteration of the lower Cambrian (Series 2) Emu Bay Shale Lagerstätte, South Australia. Australian Journal of Earth Sciences, 58(3), 259–272. https://doi.org/10.1080/08120099.2011.557439
   Web of Science ®Google Scholar
• McLennan, S. M. (1989). Rare earth elements in sedimentary rocks: Influence of provenance and sedimentary processes. In B. R. Lipin & G. A. McKay (Eds.), Geochemistry and Mineralogy of Rare Earth Elements (pp. 169–200). Mineralogical Society of America. Reviews in Mineralogy and Geochemistry, 21.
   Google Scholar
• McLennan, S. M., & Taylor, S. R. (1991). Sedimentary rocks and crustal evolution: Tectonic setting and secular trends. The Journal of Geology, 99(1), 1–21. http://www.jstor.org/stable/30068762 https://doi.org/10.1086/629470
   Web of Science ®Google Scholar
• Meert, J. G., & Lieberman, B. S. (2008). The Neoproterozoic assembly of Gondwana and its relationship to the Ediacaran–Cambrian radiation. Gondwana Research, 14(1–2), 5–21. https://doi.org/10.1016/j.gr.2007.06.007
   Web of Science ®Google Scholar
• Merdith, A. S., Collins, A. S., Williams, S. E., Pisarevsky, S., Foden, J. F., Archibald, D. A., Blades, M. L., Alessio, B. L., Armistead, S., Plavsa, D., Clark, C., & Müller, R. D. (2017). A full-plate global reconstruction of the Neoproterozoic. Gondwana Research, 50, 84–134. https://doi.org/10.1016/j.gr.2017.04.001
   Web of Science ®Google Scholar
• Merdith, A. S., Williams, S. E., Brune, S., Collins, A. S., & Müller, R. D. (2019). Rift and plate boundary evolution across two supercontinent cycles. Global and Planetary Change, 173, 1–14. https://doi.org/10.1016/j.gloplacha.2018.11.006
   Web of Science ®Google Scholar
• Merdith, A. S., Williams, S. E., Müller, R. D., & Collins, A. S. (2017). Kinematic constraints on the Rodinia to Gondwana transition. Precambrian Research, 299, 132–150. https://doi.org/10.1016/j.precamres.2017.07.013
   Web of Science ®Google Scholar
• Morris, B. J. (1991). Kanmantoo Trough geological investigations Karinya Syncline drilling report (Report Book 91/20). South Australian Department of Mines and Energy.
   Google Scholar
• Morse, J. W., & Luther, G. W. III. (1999). Chemical influences on trace metal–sulfide interactions in anoxic sediments. Geochimica et Cosmochimica Acta, 63(19–20), 3373–3378. https://doi.org/10.1016/S0016-7037(99)00258-6
   Web of Science ®Google Scholar
• Maruyama, S., & Santosh, M. (2008). Models on Snowball Earth and Cambrian explosion: A synopsis. Gondwana Research, 14(1–2), 22–32. https://doi.org/10.1016/j.gr.2008.01.004
   Web of Science ®Google Scholar
• Myrow, P. M., Hughes, N. C., Goodge, J. W., Fanning, C. M., Williams, I. S., Peng, S., Bhargava, O. N., Parcha, S. K., & Pogue, K. R. (2010). Extraordinary transport and mixing of sediment across Himalayan central Gondwana during the Cambrian–Ordovician. Geological Society of America Bulletin, 122(9–10), 1660–1670. https://doi.org/10.1130/B30123.1
   Web of Science ®Google Scholar
• Naqvi, S. M., Uday Raj, B., Subba Rao, D. V., Manikyamba, C., Nirmal Charan, S., Balaram, V., & Srinivasa Sarma, D. (2002). Geology and geochemistry of arenite–quartzwacke from the Late Archaean Sandur schist belt—implications for provenance and accretion processes. Precambrian Research, 114(3–4), 177–197. https://doi.org/10.1016/S0301-9268(01)00227-3
   Web of Science ®Google Scholar
• Naqvi, S. W. A., Naik, H., Jayakumar, D. A., Shailaja, M. S., & Narvekar, P. V. (2006). Seasonal oxygen deficiency over the western continental shelf of India. In L. N. Neretin (Ed.), Past and Present Water Column Anoxia (pp. 195–224, NATO Science Series: IV). Earth and Environmental Sciences. 64.
   Google Scholar
• Nedin, C. (1995). The palaeontology and palaeoenvironment of the Early Cambrian Emu Bay Shale Kangaroo Island, South Australia [unpublished PhD thesis]. University of Adelaide.
   Google Scholar
• Och, L. M., & Shields-Zhou, G. A. (2012). The Neoproterozoic oxygenation event: Environmental perturbations and biogeochemical cycling. Earth-Science Reviews, 110(1–4), 26–57. https://doi.org/10.1016/j.earscirev.2011.09.004
   Web of Science ®Google Scholar
• Och, L. M., Shields-Zhou, G. A., Poulton, S. W., Manning, C., Thirlwall, M. F., Li, D., Chen, X., Ling, H., Osborn, T., & Cremonese, L. (2013). Redox changes in Early Cambrian black shales at Xiaotan section, Yunnan Province, South China. Precambrian Research, 225, 166–189. https://doi.org/10.1016/j.precamres.2011.10.005
   Web of Science ®Google Scholar
• Paterson, J. R., García-Bellido, D. C., Jago, J. B., Gehling, J. G., Lee, M. S. Y., & Edgecombe, G. D. (2016). The Emu Bay Shale Konservat-Lagerstätte: A view of Cambrian life from East Gondwana. Journal of the Geological Society, 173(1), 1–11. https://doi.org/10.1144/jgs2015-083
   Web of Science ®Google Scholar
• Paterson, J. R., García-Bellido, D. C., Lee, M. S. Y., Brock, G. A., Jago, J. B., & Edgecombe, G. D. (2011). Acute vision in the giant Cambrian predator Anomalocaris and the origin of compound eyes. Nature, 480(7376), 237–240. https://doi.org/10.1038/nature10689
   PubMed Web of Science ®Google Scholar
• Paterson, J. R., Jago, J. B., Gehling, J. G., García-Bellido, D. C., Edgecombe, G. D., & Lee, M. S. Y. (2008). Early Cambrian arthropods from the Emu Bay Shale Lagerstätte, South Australia. In I. Rábano, R. Gozalo & D. García-Bellido (Eds.), Advances in Trilobite Research (pp. 319–325). Instituto Geológico y Minero de España.
   Google Scholar
• Pi, D-H., Liu, C-Q., Shields-Zhou, G. A., & Jiang, S-Y. (2013). Trace and rare earth element geochemistry of black shale and kerogen in the early Cambrian Niutitang Formation in Guizhou province, South China: Constraints for redox environments and origin of metal enrichments. Precambrian Research, 225, 218–229. https://doi.org/10.1016/j.precamres.2011.07.004
   Web of Science ®Google Scholar
• Piper, D. Z., & Calvert, S. E. (2009). A marine biogeochemical perspective on black shale deposition. Earth-Science Reviews, 95(1–2), 63–96. https://doi.org/10.1016/j.earscirev.2009.03.001
   Web of Science ®Google Scholar
• Powell, C. M., Preiss, W. V., Gatehouse, C. G., Krapez, B., & Li, Z. X. (1994). South Australian record of a Rodinian epi-continental basin and its mid-Neoproterozoic breakup (∼700 Ma) to form the Palaeo-Pacific Ocean. Tectonophysics, 237(3–4), 113–140. https://doi.org/10.1016/0040-1951(94)90250-X
   Web of Science ®Google Scholar
• Powell, W. G. (2009). Comparison of geochemical and distinctive mineralogical features associated with the Kinzers and Burgess Shale formations and their associated units. Palaeogeography, Palaeoclimatology, Palaeoecology, 277(1–2), 127–140. https://doi.org/10.1016/j.palaeo.2009.02.016
   Web of Science ®Google Scholar
• Powell, W. G., Johnston, P. A., & Collom, C. J. (2003). Geochemical evidence for oxygenated bottom waters during deposition of fossiliferous strata of the Burgess Shale Formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 201(3–4), 249–268. https://doi.org/10.1016/S0031-0182(03)00612-6
   Google Scholar
• Preiss, W. V., (1995). Delamerian orogeny. In J. F. Drexel & W. V. Preiss, (Eds.), The Geology of South Australia, Vol. 2: The Phanerozoic (pp. 45–60). Geological Survey of South Australia Bulletin. 54.
   Google Scholar
• Preiss, W. V. (2000). The Adelaide Geosyncline of South Australia and its significance in Neoproterozoic continental reconstructions. Precambrian Research, 100(1–3), 21–63. https://doi.org/10.1016/S0301-9268(99)00068-6
   Web of Science ®Google Scholar
• Racka, M., Marynowski, L., Filipiak, P., Sobstel, M., Pisarzowska, A., & Bond, D. P. G. (2010). Anoxic Annulata events in the late Famennian of the Holy Cross Mountains (Southern Poland): Geochemical and palaeontological record. Palaeogeography, Palaeoclimatology, Palaeoecology, 297(3–4), 549–575. https://doi.org/10.1016/j.palaeo.2010.08.028
   Web of Science ®Google Scholar
• Rimmer, S. M. (2004). Geochemical paleoredox indicators in Devonian–Mississipian black shales. Chemical Geology, 206(3–4), 373–391. https://doi.org/10.1016/j.chemgeo.2003.12.029
   Web of Science ®Google Scholar
• Schmitt, R. S., Fragoso, R. A., & Collins, A. S. (2018). Suturing Gondwana in the Cambrian—the orogenic events of the final amalgamation. In S. Siegesmund, M. A. S. Basei, P. Oyhantçabal & S. Oriolo (Eds.), Geology of Southwest Gondwana. Regional Geology Reviews. Springer. https://doi.org/10.1007/978-3-319-68920-3_15
   Google Scholar
• Scott, C., Lyons, T. W., Bekker, A., Shen, Y., Poulton, S. W., Chu, X., & Anbar, A. D. (2008). Tracing the stepwise oxygenation of the Proterozoic ocean. Nature, 452(7186), 456–459. https://doi.org/10.1038/nature06811
   PubMed Web of Science ®Google Scholar
• Shen, Y., Schidlowski, M., & Chu, X. (2000). Biogeochemical approach to understanding phosphogenic events of the terminal Proterozoic to Cambrian. Palaeogeography, Palaeoclimatology. Palaeoecology, 158(1–2), 99–108. https://doi.org/10.1016/S0031-0182(00)00033-X
   Web of Science ®Google Scholar
• Shields, G. A., Mills, B. J. W., Zhu, M., Raub, T. D., Daines, S. J., & Lenton, T. M. (2019). Unique Neoproterozoic carbon isotope excursions sustained by coupled evaporite dissolution and pyrite burial. Nature Geoscience, 12(10), 823–827. https://doi.org/10.1038/s41561-019-0434-3
   Web of Science ®Google Scholar
• Shields, G., Kimura, H., Yang, J., & Gammon, P. (2004). Sulphur isotopic evolution of Neoproterozoic–Cambrian seawater: New francolite-bound sulphate δ34S data and critical appraisal of the existing record. Chemical Geology, 204(1–2), 163–182. https://doi.org/10.1016/j.chemgeo.2003.12.001
   Web of Science ®Google Scholar
• Shields, G., Strauss, H., Howe, S. S., & Siegmund, H. (1999). Sulphur isotope compositions of sedimentary phosphorites from the basal Cambrian of China: Implications for Neoproterozoic–Cambrian biogeochemical cycling. Journal of the Geological Society, 156(5), 943–955. https://doi.org/10.1144/gsjgs.156.5.0943
   Google Scholar
• Shields, G., & Stille, P. (2001). Diagenetic constrains on the use of cerium anomalies as palaeoseawater proxies: An isotopic and REE study of Cambrian phosphorites. Chemical Geology, 175(1–2), 29–48. https://doi.org/10.1016/S0009-2541(00)00362-4
   Web of Science ®Google Scholar
• Sholkovitz, E., Landing, W. M., & Lewis, B. L. (1994). Ocean particle chemistry: The fractionation of the rare earth elements between suspended particles and seawater. Geochimica et Cosmochimica Acta, 58(6), 1567–1580. https://doi.org/10.1016/0016-7037(94)90559-2
   Web of Science ®Google Scholar
• Squire, R. J., Campbell, I. H., Allen, C. M., & Wilson, C. J. L. (2006). Did the Transgondwanan Supermountain trigger the explosive radiation of animals on Earth? Earth and Planetary Science Letters, 250(1–2), 116–133. https://doi.org/10.1016/j.epsl.2006.07.032
   Web of Science ®Google Scholar
• Steiner, M., Li, G., Qian, Y., Zhu, M., & Erdtmann, B. (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. https://doi.org/10.1016/j.palaeo.2007.03.046
   Web of Science ®Google Scholar
• Strauss, H. (2002). The isotopic composition of Precambrian sulphides–seawater chemistry and biological evolution. International Association of Sedimentologists Special Publication, 33, 67–105.
   Google Scholar
• Strauss, H. (2006). Anoxia through time. In L. N. Neretin (Ed.), Past and Present Water Column Anoxia (pp. 3–19), NATO Science Series: IV). Earth and Environmental Sciences. 64.
   Google Scholar
• Suto, A. (2011). Structure of the Kangaroo Island Fleurieu Peninsula Shear Zone and the provenance of its host sediments—The Kanmantoo Group—South Eastern Australia [unpublished B.Sc. Honours thesis]. University of Adelaide.
   Google Scholar
• Taylor, S. R., & McLennan, S. M. (1985). The Continental Crust: Its Composition and Evolution. Blackwell Scientific Publications.
   Google Scholar
• Thickpenny, A., & Leggett, J. K. (1987). Stratigraphic distribution and palaeo-oceanographic significance of European early Palaeozoic organic-rich sediments. In J. Brooks & A. J. Fleet (Eds.), Marine Petroleum Source Rocks (pp. 231–247). Geological Society Special Publication. 26.
   Google Scholar
• Thomson, B. P. (1969). The Kanmantoo Group and Early Palaeozoic Tectonics. In L. W. Parkin (Ed.), Handbook of South Australian Geology (pp. 97–108). Geological Survey of South Australia.
   Google Scholar
• Thomson, J., Jarvis, I., Green, D. R. H., Green, D., & Clayton, T. (1998). Mobility and immobility of redox-sensitive elements in deep-sea turbidites during shallow burial. Geochimica et Cosmochimica Acta, 62(4), 643–656. https://doi.org/10.1016/S0016-7037(97)00378-5
   Web of Science ®Google Scholar
• Tissot, B. P., & Welte, D. H. (1984). Petroleum Formation and Occurrence (2nd ed.). Springer-Verlag.
   Google Scholar
• Tostevin, R., & Mills, B. J. W. (2020). Reconciling proxy records and models of Earth’s oxygenation during the Neoproterozoic and Palaeozoic. Interface Focus, 10(4), 20190137. https://doi.org/10.1098/rsfs.2019.0137
   PubMed Web of Science ®Google Scholar
• Tribovillard, N., Algeo, T. J., Baudin, F., & Riboulleau, A. (2012). Analysis of marine environmental conditions based on molybdenum–uranium covariation—Applications to Mesozoic paleoceanography. Chemical Geology, 324-325, 46–58. https://doi.org/10.1016/j.chemgeo.2011.09.009
   Web of Science ®Google Scholar
• Tribovillard, N., Algeo, T. J., Lyons, T., & Riboulleau, A. (2006). Trace metals as paleoredox and paleoproductivity proxies: An update. Chemical Geology, 232(1–2), 12–32. https://doi.org/10.1016/j.chemgeo.2006.02.012
   Web of Science ®Google Scholar
• Tribovillard, N., Bout-Roumazeilles, V., Algeo, T. J., Lyons, T. W., Sionneau, T., Montero-Serrano, J. C., Riboulleau, A., & Baudin, F. (2008). Paleodepositional conditions in the Orca Basin as inferred from organic matter and trace metal contents. Marine Geology, 254(1–2), 62–72. https://doi.org/10.1016/j.margeo.2008.04.016
   Web of Science ®Google Scholar
• Tribovillard, N., Riboulleau, A., Lyons, T., & Baudin, F. (2004). Enhanced trapping of molybdenum by sulfurized organic matter of marine origin as recorded by various Mesozoic formations. Chemical Geology, 213(4), 385–401. https://doi.org/10.1016/j.chemgeo.2004.08.011
   Web of Science ®Google Scholar
• Turner, B. L. (1994). Cambrian black shales in the Karinya Syncline: stratigraphic distribution, sedimentology and kerogen composition [unpublished B.Sc. Honours thesis]. University of Adelaide.
   Google Scholar
• Turner, S. P., Adams, C. J., Flöttmann, T., & Foden, J. D. (1993). Geochemical and geochronological constraints on the Glenelg River Complex, Western Victoria. Australian Journal of Earth Sciences, 40(3), 275–292. https://doi.org/10.1080/08120099308728080
   Web of Science ®Google Scholar
• Turner, S. P., Haines, P. W., Foster, D., Powell, R., Sandiford, M., & Offler, R. (2009). Did the Delamerian Orogeny start in the Neoproterozoic? The Journal of Geology, 117(5), 575–583. https://doi.org/10.1086/600866
   Web of Science ®Google Scholar
• Tyson, R. V. (1995). Sedimentary Organic Matter—Organic Facies and Palynofacies (p. 615). Chapman & Hall.
   Google Scholar
• Tyson, R. V., & Pearson, T. H., (1991). Modern and ancient continental shelf anoxia: an overview. In R. V. Tyson & T. H. Pearson (Eds.), Modern and Ancient Continental Shelf Anoxia (pp. 1–24). Geological Society, Special Publication. 58. https://doi.org/10.1144/GSL.SP.1991.058.01.01
   Google Scholar
• Veevers, J. J., Belousova, E. A., Saeed, A., Sircombe, K., Cooper, A. F., & Read, S. R. (2006). Pan-Gondwanaland detrital zircons from Australia analysed for Hf-isotopes and trace elements reflect an ice-covered Antarctic provenance of 700–500 Ma age, TDM of 2.0–1.0 Ga, and alkaline affinity. Earth-Science Reviews, 76(3–4), 135–174. https://doi.org/10.1016/j.earscirev.2005.11.001
   Web of Science ®Google Scholar
• Walker, J. C. G. (1986). Global geochemical cycles of carbon, sulfur and oxygen. Marine Geology, 70, 159–174. https://doi.org/10.1016/0025-3227(86)90093-9
   PubMed Web of Science ®Google Scholar
• Wang, X., Shi, X., Jiang, G., & Zhang, W. (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
   Web of Science ®Google Scholar
• Wani, H., & Mondal, M. E. A. (2011). Evaluation of provenance, tectonic setting and paleo-redox conditions of the Mesoproterozoic–Neoproterozoic basins of the Bastar craton, Central Indian Shield: Using petrography of sandstones and geochemistry of shales. Lithosphere, 3(2), 143–154. https://doi.org/10.1130/L74.1
   Web of Science ®Google Scholar
• Wignall, P. B., & Twitchett, R. J. (1996). Oceanic anoxia and the end Permian mass extinction. Science, 272(5265), 1155–1158. https://doi.org/10.1126/science.272.5265.1155
   PubMed Web of Science ®Google Scholar
• Wilde, P., Lyons, T. W., & Quinby-Hunt, M. S. (2004). Organic carbon proxies in black shales: molybdenum. Chemical Geology, 206(3–4), 167–176. https://doi.org/10.1016/j.chemgeo.2003.12.005
   Web of Science ®Google Scholar
• Wilde, P., Quinby-Hunt, M. S., & Erdtmann, B. D. (1996). The whole-rock cerium anomaly: A potential indicator of eustatic sea-level changes in shales of the anoxic facies. Sedimentary Geology, 101(1–2), 43–53. https://doi.org/10.1016/0037-0738(95)00020-8
   Web of Science ®Google Scholar
• Wombacher, F., & Münker, C. (2000). Pb, Nd, and Sr isotopes and REE systematic of Cambrian sediments from New Zealand: Implications for the reconstruction of the Early Palaeozoic Gondwana margin along Australia and Antarctica. The Journal of Geology, 108(6), 663–686. https://doi.org/10.1086/317950
   Web of Science ®Google Scholar
• Wu, N., Farquhar, J., Strauss, H., Kim, S., & Canfield, D. E. (2010). Evaluating the S-isotope fractionation associated with Phanerozoic pyrite burial. Geochimica et Cosmochimica Acta, 74(7), 2053–2071. https://doi.org/10.1016/j.gca.2009.12.012
   Web of Science ®Google Scholar
• Xie, S., Wu, Y., Gao, S., Liu, X., Zhou, L., Zhao, L., & Hu, Z. (2012). Sr–Nd isotopic and geochemical constraints on provenance of late Paleozoic to early Cretaceous sedimentary rocks in the Western Hills of Beijing, North China: Implications for the uplift of the northern North China Craton. Sedimentary Geology, 245–246, 17–28. https://doi.org/10.1016/j.sedgeo.2011.12.005
   Web of Science ®Google Scholar
• Yan, X., Kerrich, R., & Hendry, M. J. (2000). Trace element geochemistry of a thick till and clay-rich aquitard sequence, Saskatchewan, Canada. Chemical Geology, 164(1–2), 93–120. https://doi.org/10.1016/S0009-2541(99)00141-2
   Web of Science ®Google Scholar
• Yan, Y., Xia, B., Lin, G., Carter, A., Hu, X., Cui, X., Liu, B., Yan, P., & Song, Z. (2007). Geochemical and Nd isotope composition of detrital sediments on the north margin of the South China Sea: Provenance and tectonic implications. Sedimentology, 54(1), 1–17. https://doi.org/10.1111/j.1365-3091.2006.00816.x
   Web of Science ®Google Scholar
• Yang, J. H., Jiang, S. Y., Ling, H. F., Feng, H. Z., Chen, Y. Q., & Chen, J. F. (2004). Paleoceanographic significance of redox-sensitive metals of black shales in the basal Lower Cambrian Niutitang Formation in Guizhou Province, South China. Progress in Natural Science, 14(2), 152–157. https://doi.org/10.1080/10020070412331343291
   Web of Science ®Google Scholar
• Yang, J., Torres, M., McManus, J., Algeo, T. J., Hakala, A., & Verba, C. (2017). Controls on rare earth element distributions in ancient organic-rich sedimentary sequences: Role of post-depositional diagenesis of phosphorus phases. Chemical Geology, 466, 533–544. https://doi.org/10.1016/j.chemgeo.2017.07.003
   Web of Science ®Google Scholar
• Yu, B., Dong, H., Widom, E., Chen, J., & Lin, C. (2009). Geochemistry of basal Cambrian black shales and cherts from the Northern Tarim Basin, Northwest China: Implications for depositional setting and tectonic history. Journal of Asian Earth Sciences, 34(3), 418–436. https://doi.org/10.1016/j.jseaes.2008.07.003
   Web of Science ®Google Scholar
• Zhang, L., Algeo, T. J., Cao, L., Zhao, L., Chen, Z-Q., & Li, Z. (2016). Diagenetic uptake of rare earth elements by conodont apatite. Palaeogeography, Palaeoclimatology, Palaeoecology, 458, 176–197. https://doi.org/10.1016/j.palaeo.2015.10.049
   Web of Science ®Google Scholar
• Zhang, Q. R., & Piper, J. D. A. (1997). Palaeomagnetic study of Neoproterozoic glacial rocks of the Yangzi Block: Palaeolatitude and configuration of South China in the late Proterozoic Supercontinent. Precambrian Research, 85(3–4), 173–199. https://doi.org/10.1016/S0301-9268(97)00031-4
   Web of Science ®Google Scholar
• Zhang, T., Chu, X., Zhang, Q., Feng, L., & Huo, W. (2003). Variations of sulphur and carbon isotopes in seawater during the Doushantuo stage in late Neoproterozoic. Chinese Science Bulletin, 48(13), 1375–1380. https://doi.org/10.1007/BF03184182
   Google Scholar
• Zheng, Y., Anderson, R. F., van Geen, A., & Kuwabara, J. (2000). Authigenic molybdenum formation in marine sediments: A link to pore water sulfide in the Santa Barbara Basin. Geochimica et Cosmochimica Acta, 64(24), 4165–4178. https://doi.org/10.1016/S0016-7037(00)00495-6
   Web of Science ®Google Scholar
• Zhou, C., & Jiang, S. Y. (2009). Palaeoceanographic redox environments for the lower Cambrian Hetang Formation in South China: Evidence from pyrite framboids, redox-sensitive trace elements, and sponge biota occurrence. Palaeogeography, Palaeoclimatology, Palaeoecology, 271(3–4), 279–286. https://doi.org/10.1016/j.palaeo.2008.10.024
   Web of Science ®Google Scholar