Zebra rock and other Ediacaran paleosols from Western Australia

References

• Abrajevitch, A., Pillans, B. J., Roberts, A. P., & Kodama, K. (2018). Magnetic properties and paleomagnetism of Zebra Rock, Western Australia: Chemical remanence acquisition in hematite pigment and Ediacaran geomagnetic field behavior. Geochemistry, Geophysics, Geosystems, 19(3), 732–748. https://doi.org/10.1002/2017GC007091
   Web of Science ®Google Scholar
• Aiello, I. W., Garrison, R. E., Moore, E. C., Kastner, M., & Stakes, D. S. (2001). Anatomy and origin of carbonate structures in a Miocene cold-seep field. Geology, 29(12), 1111–1114. https://doi.org/10.1130/0091-7613(2001)0291111:AAOOCS2.0.CO;2
   Web of Science ®Google Scholar
• Almohandis, A. A. (2002). Mineralogy and chemistry of desert roses, Ayn Dar area, Abqaiq, eastern province, Saudi Arabia. Qatar University Science Journal, 22, 191–204. http://hdl.handle.net/10576/9660
   Google Scholar
• Álvaro, J. J., Van Vliet-Lanoë, B., Vennin, E., & Blanc-Valleron, M. M. (2003). Lower Cambrian paleosols from the Cantabrian Mountains (northern Spain): A comparison with Neogene–Quaternary estuarine analogues. Sedimentary Geology, 163(1–2), 67–84. https://doi.org/10.1016/S0037-0738(03)00159-3
   Web of Science ®Google Scholar
• Antcliffe, J. B., Gooday, A. J., & Brasier, M. D. (2011). Testing the protozoan hypothesis for Ediacaran fossils: A developmental analysis of Palaeopascichnus. Palaeontology, 54(5), 1157–1175. https://doi.org/10.1111/j.1475-4983.2011.01058.x
   Web of Science ®Google Scholar
• Bao, H., Chen, Z. Q., & Zhou, C. (2012). An 17O record of late Neoproterozoic glaciation in the Kimberley region, Western Australia. Precambrian Research, 216-219(1), 152–161. https://doi.org/10.1016/j.precamres.2012.06.019
   Web of Science ®Google Scholar
• Barbour, M. M., & Farquhar, G. D. (2000). Relative humidity- and ABA-induced variation in carbon and oxygen isotope ratios of cotton leaves. Plant, Cell & Environment, 23(5), 473–485. https://doi.org/10.1046/j.1365-3040.2000.00575.x
   Web of Science ®Google Scholar
• Barbour, M. M., Walcroft, A. S., & Farquhar, G. D. (2002). Seasonal variation in δ13C and δ18O of cellulose from growth rings of Pinus radiata. Plant, Cell and Environment, 25(11), 1483–1499. https://doi.org/10.1046/j.0016-8025.2002.00931.x
   Web of Science ®Google Scholar
• Bavinton, O. A., & Taylor, S. R. (1980). Rare earth element geochemistry of Archean metasedimentary rocks from Kambalda, Western Australia. Geochimica et Cosmochimica Acta, 44(5), 639–648. https://doi.org/10.1016/0016-7037(80)90154-4
   Web of Science ®Google Scholar
• Belnap, J. (2003). Comparative structure of physical and biological soil crusts. In. J. Belnap & O. L. Lange (Eds.), Biological soil crusts: Structure, function and management (pp. 177–191). Springer.
   Google Scholar
• Benison, K. C., & Bowen, B. B. (2015). The evolution of end-member continental waters: The origin of acidity in southern Western Australia. GSA Today, 25(6), 4–10. https://doi.org/10.1130/GSATG231A.1
   Google Scholar
• Benison, K. C., Bowen, B. B., Oboh-Ikuenobe, F. E., Jagniecki, E. A., LaClair, D. A., Story, S. L., Mormile, M. R., & Hong, B. Y. (2007). Sedimentology of acid saline lakes in southern Western Australia: Newly described processes and products of an extreme environment. Journal of Sedimentary Research, 77(5), 366–388. https://doi.org/10.2110/jsr.2007.038
   Web of Science ®Google Scholar
• Bestland, E. A., Retallack, G. J., Rice, A. E., & Mindszenty, A. (1996). Late Eocene detrital laterites in central Oregon: Mass balance geochemistry, depositional setting and landscape evolution. Geological Society of America Bulletin, 108(3), 285–302. https://doi.org/10.1130/0016-7606(1996)1080285:LEDLIC2.3.CO;2
   Web of Science ®Google Scholar
• Bindeman, I. N., Eiler, J. M., Wing, B. A., & Farquhar, J. (2007). Rare sulfur and triple oxygen isotope geochemistry of volcanogenic sulfate aerosols. Geochimica et Cosmochimica Acta, 71(9), 2326–2343. https://doi.org/10.1016/j.gca.2007.01.026
   Web of Science ®Google Scholar
• Boas, J. F., Cashion, J. D., Chadwick, J., Clark, M. J., Mackie, R. D., & Mattievich, E. (2005). Electron paramagnetic resonance of defects and Fe3+ in Kimberley Zebra Rock. Abstracts of the National Congress of Australian Institute of Physics, 16, 268. http://aipcongress2005.anu.edu.au/pdf/AIPC_Handbook_V2.pdf
   Google Scholar
• Bockheim, J. G., & Hartemink, A. E. (2013). Classification and distribution of soils with lamellae in the USA. Geoderma, 206, 92–100. https://doi.org/10.1016/j.geoderma.2013.04.014
   Web of Science ®Google Scholar
• Bolhar, R., Van Kranendonk, M. J., & Kamber, B. S. (2005). A trace element study of siderite jasper banded iron formation in the 3.45 Ga Warrawoona Group, Pilbara Craton: Formation from hydrothermal fluids and shallow seawater. Precambrian Research, 137(1–2), 93–114. https://doi.org/10.1016/j.precamres.2005.02.001
   Web of Science ®Google Scholar
• Bowler, J. M. (1973). Clay dunes: Their occurrence, formation and environmental significance. Earth-Science Reviews, 9(4), 315–338. https://doi.org/10.1016/0012-8252(73)90001-9
   Web of Science ®Google Scholar
• Breecker, D. O., & Retallack, G. J. (2014). Refining the pedogenic carbonate atmospheric CO2 proxy and application to Miocene CO2. Palaeogeography, Palaeoclimatology, Palaeoecology, 406, 1–8. https://doi.org/10.1016/j.palaeo.2014.04.012
   Web of Science ®Google Scholar
• Brimhall, G. H., Chadwick, O. A., Lewis, C. J., Compston, W., Williams, I. S., Danti, K. J., Dietrich, W. E., Power, M. E., Hendricks, D., & Bratt, J. (1992). Deformational mass transport and invasive processes in soil evolution. Science, 255(5045), 695–702. https://doi.org/10.1126/science.255.5045.695
   PubMed Web of Science ®Google Scholar
• Bureau of Meteorology. (2020). Climate statistics for Australian locations. Retrieved May 11, 2020, from http://www.bom.gov.au/climateaverages
   Google Scholar
• Cant, D. J., & Walker, R. G. (1978). Fluvial processes and facies sequences in the sandy braided South Saskatchewan River, Canada. Sedimentology, 25(5), 625–648. https://doi.org/10.1111/j.1365-3091.1978.tb00323.x
   Web of Science ®Google Scholar
• Chadwick, O. A., Brimhall, G. H., & Hendricks, D. M. (1990). From a black to a gray box—a mass balance interpretation of pedogenesis. Geomorphology, 3(3–4), 369–390. https://doi.org/10.1016/0169-555X(90)90012-F
   Google Scholar
• Chen, C., Barcellos, D., Richter, D. D., Schroeder, P. A., & Thompson, A. (2019). Redoximorphic Bt horizons of the Calhoun CZO soils exhibit depth-dependent iron-oxide crystallinity. Journal of Soils and Sediments, 19(2), 785–797. https://doi.org/10.1007/s11368-018-2068-2
   Web of Science ®Google Scholar
• Clauer, N., O’Neil, J. R., Bonnnot-Courtois, C., & Holtzapfel, T. (1990). Morphological, chemical, and isotopic evidence for an early diagenetic evolution of detrital smectite in marine sediments. Clays and Clay Minerals, 38(1), 33–46. https://doi.org/10.1346/CCMN.1990.0380105
   Web of Science ®Google Scholar
• Compton, J. S., White, R. A., & Smith, M. (2003). Rare earth element behavior in soils and salt pan sediments of a semi-arid granitic terrain in the Western Cape, South Africa. Chemical Geology, 201(3–4), 239–255. https://doi.org/10.1016/S0009-2541(03)00239-0
   Web of Science ®Google Scholar
• Conway Morris, S. (2006). Darwin’s dilemma: The realities of the Cambrian ‘‘explosion. Philosophical Transactions of the Royal Society B: Biological Sciences, 361(1470), 1069–1083. https://doi.org/10.1098/rstb.2006.1846
   PubMed Web of Science ®Google Scholar
• Corkeron, M. (2007). ‘Cap carbonates’ and Neoproterozoic glacigenic successions from the Kimberley region. Sedimentology, 54(4), 871–903. https://doi.org/10.1111/j.1365-3091.2007.00864.x
   Web of Science ®Google Scholar
• Corkeron, M. (2008). Deposition and palaeogeography of a glacigenic Neoproterozoic succession in the east Kimberley, Australia. Sedimentary Geology, 204(3–4), 61–82. https://doi.org/10.1016/j.sedgeo.2007.12.010
   Web of Science ®Google Scholar
• de Sá Paye, H., de Mello, J. W., de Magalhães Mascarenhas, G. R. L., & Gasparon, M. (2016). Distribution and fractionation of the rare earth elements in Brazilian soils. Journal of Geochemical Exploration, 161, 27–41. https://doi.org/10.1016/j.gexplo.2015.09.003
   Web of Science ®Google Scholar
• Dong, L., Xiao, S., Shen, B., & Zhou, C. (2008). Silicified Horodyskia and Palaeopascichnus from upper Ediacaran cherts in South China: Tentative phylogenetic interpretation and implications for evolutionary stasis. Journal of the Geological Society, 165(1), 367–378. https://doi.org/10.1144/0016-76492007-074
   Web of Science ®Google Scholar
• Dow, D. B., & Gemuts, I. (1969). Geology of the Kimberley Region, Western Australia: The East Kimberley. Bulletin of the Bureau of Mineral Resources Geology & Geophysics Canberra, 106, 135.
   Google Scholar
• Draut, A. E., & Rubin, D. M. (2008). The role of eolian sediment in the preservation of archeologic sites along the Colorado River corridor in Grand Canyon National Park. Arizona. U.S. Geological Survey Professional Paper, 1756, 1–71. https://doi.org/10.3133/pp1756
   Google Scholar
• Draut, A. E., Rubin, D. M., Dierker, J. L., Fairley, H. C., Griffiths, R. E., Hazel, J. E., Hunter, R. E., Kohl, K., Leap, L. M., Nials, F. L., Topping, D. J., & Yeatts, M. (2008). Application of sedimentary-structure interpretation to geoarchaeological investigations in the Colorado River Corridor, Grand Canyon, Arizona, USA. Geomorphology, 101(3), 497–509. https://doi.org/10.1016/j.geomorph.2007.04.032
   Web of Science ®Google Scholar
• Driese, S. G., Simpson, E. L., & Eriksson, K. A. (1995). Redoximorphic Paleosols in alluvial and lacustrine deposits, 1.8 Ga Lochness Formation, Mount Isa, Australia; pedogenic processes and implications for paleoclimate. Journal of Sedimentary Research, 65(4a), 675–689. https://doi.org/10.1306/D4268199-2B26-11D7-8648000102C1865D
   Google Scholar
• Duda, J. P., Blumenberg, M., Thiel, V., Simon, K., Zhu, M., & Reitner, J. (2014). Geobiology of a palaeoecosystem with Ediacara-type fossils: The Shibantan Member (Dengying Formation, South China). Precambrian Research, 255, 48–62. https://doi.org/10.1016/j.precamres.2014.09.012
   Web of Science ®Google Scholar
• Dunnet, D. (1965). A new occurrence of Proterozoic ‘jellyfish’ from the Kimberley Region, Western Australia. Report of the Bureau of Mineral Resources Geology and Geophysics, Canberra, 134, 5.
   Google Scholar
• Ehleringer, J. R., Buchmann, N., & Flanagan, L. B. (2000). Carbon isotope ratios in belowground carbon cycle processes. Ecological Applications, 10(2), 412–422.https://doi.org/10.1890/1051-0761(2000)010[0412:CIRIBC]2.0.CO;2
   Web of Science ®Google Scholar
• Ehleringer, J. R., & Cook, C. S. (1998). Carbon and oxygen isotope ratios of ecosystem respiration along an Oregon conifer transect: Preliminary observations based on small flask sampling. Tree Physiology, 18(8–9), 513–519. https://doi.org/10.1093/treephys/18.8-9.513
   PubMed Web of Science ®Google Scholar
• Evins, L. Z., Jourdan, F., & Phillips, D. (2009). The Cambrian Kalkarindji large igneous province: Extent and characteristics based on new 40Ar/39Ar and geochemical data. Lithos, 110(1–4), 294–304. https://doi.org/10.1016/j.lithos.2009.01.014
   Web of Science ®Google Scholar
• Ewing, S. A., Macalady, J. L., Warren‐Rhodes, K., McKay, C. P., & Amundson, R. (2008). Changes in the soil C cycle at the arid‐hyperarid transition in the Atacama Desert. Journal of Geophysics Research Biogeosciences, 113(G2), G02S90. https://doi.org/10.1029/2007JG000495
   Web of Science ®Google Scholar
• Fisk, H. N. (1951). Loess and Quaternary geology of the Lower Mississippi Valley. The Journal of Geology, 59(4), 333–356. https://doi.org/10.1086/625872
   Web of Science ®Google Scholar
• Fitzsimmons, K. E., Stern, N., & Murray-Wallace, C. V. (2014). Depositional history and archaeology of the central Lake Mungo lunette, Willandra Lakes, southeast Australia. Journal of Archaeological Science, 41, 349–364. https://doi.org/10.1016/j.jas.2013.08.004
   Web of Science ®Google Scholar
• Foden, J. D., Nesbitt, R. W., & Rutland, R. W. R. (1984). The geochemistry and crustal origin of the Archaean acid intrusive rocks of the Agnew Dome, Lawlers, Western Australia. Precambrian Research, 23(3–4), 247–271. https://doi.org/10.1016/0301-9268(84)90046-9
   Web of Science ®Google Scholar
• Food and Agriculture Organization. (1978). Soil map of the World 1:5,000,000. Vol. X. Australasia (p. 21). UNESCO.
   Google Scholar
• Frey, M. (1987). Very low grade metamorphism of clasticsedimentary rocks. In M. Frey (Ed.), Low temperature metamorphism (pp. 9–58). Blackie.
   Google Scholar
• Gallagher, T. M., & Sheldon, N. D. (2013). A new paleothermometer for forest paleosols and its implications for Cenozoic climate. Geology, 41(6), 647–650. https://doi.org/10.1130/G34074.1
   Web of Science ®Google Scholar
• Gariboldi, K., Gioncada, A., Bosio, G., Malinverno, E., Di Celma, C., Tinelli, C., Cantalamessa, G., Landini, W., Urbina, M., & Bianucci, G. (2015). The dolomite nodules enclosing fossil marine vertebrates in the East Pisco Basin, Peru: Field and petrographic insights into the Lagerstätte formation. Palaeogeography, Palaeoclimatology, Palaeoecology, 438, 81–95. https://doi.org/10.1016/j.palaeo.2015.07.047
   Web of Science ®Google Scholar
• Gastaldo, R. A., Allent, G., & Huci, A. Y. (2009). The tidal character of fluvial sediments of the modern Mahakam River delta, Kalimantan, Indonesia. In B. W. Flemming (Ed.), Tidal signatures in modern and ancient sediments (Vol. 28, pp. 171–181). Special Publication of the International Association of Sedimentologists.
   Google Scholar
• Gehling, J. G. (2000). Environmental interpretation and a sequence stratigraphic framework for the terminal Proterozoic Ediacara Member within the Rawnsley Quartzite, South Australia. Precambrian Research, 100(1–3), 65–95. https://doi.org/10.1016/S0301-9268(99)00069-8
   Web of Science ®Google Scholar
• Gehling, J. G., & Droser, M. L. (2009). Textured organic surfaces associated with the Ediacara biota in South Australia. Earth-Science Reviews, 96(3), 196–206. https://doi.org/10.1016/j.earscirev.2009.03.002
   Web of Science ®Google Scholar
• Gehling, J. G., & Narbonne, G. M. (2007). Spindle-shaped Ediacara fossils from the Mistaken Point assemblage, Avalon zone, Newfoundland. Canadian Journal of Earth Sciences, 44(3), 367–387. https://doi.org/10.1139/e07-003
   Web of Science ®Google Scholar
• Geidans, L. (1981). Zebra rock of Western Australia. Abstracts of the Geological Society of Australia, 3, 22.
   Google Scholar
• Glaessner, M. F. (1969). Trace fossils from the Precambrian and basal Cambrian. Lethaia, 2(4), 369–393. https://doi.org/10.1111/j.1502-3931.1969.tb01258.x
   Web of Science ®Google Scholar
• Grazhdankin, D. V., Goy, Y. Y., & Maslov, A. V. (2012). Late Riphean microbial colonies adapted to desiccating environments. Doklady Earth Sciences, 446(2), 1157–1161. https://doi.org/10.1134/S1028334X12100157
   Web of Science ®Google Scholar
• Grey, K. (1981a). Proterozoic “jellyfish” from the Mount Brooking area, Lissadell Sheet, Kimberley region. Geological Survey of Western Australia Palaeontology Report, 29, 1–4. https://dmpbookshop.eruditetechnologies.com.au/product/proterozoic-jellyfish-from-the-mount-brooking-area-lissadell-sheet-kimberley-region.do
   Google Scholar
• Grey, K. (1981b). Additional samples of Proterozoic “jellyfish” from the Mount Brooking area, Lissadell Sheet, Kimberley region. Geological Survey of Western Australia Palaeontology Report, 52, 1–2. https://dmpbookshop.eruditetechnologies.com.au/product/additional-samples-of-proterozoic-jellyfish-from-the-mount-brooking-area-lissadell-sheet-kimberley-region.do
   Google Scholar
• Grey, K., & Corkeron, M. (1998). Late Neoproterozoic stromatolites in glacigenic successions of the Kimberley region, Western Australia: Evidence for a younger Marinoan glaciation. Precambrian Research, 92(1), 65–87. https://doi.org/10.1016/S0301-9268(98)00068-0
   Web of Science ®Google Scholar
• Grimley, D. A., Follmer, L. R., & McKay, E. D. (1998). Magnetic susceptibility and mineral zonation controlled by provenance in loess along the Illinois and central Mississippi Valley. Quaternary Research, 49(1), 24–36. https://doi.org/10.1006/qres.1997.1947
   Web of Science ®Google Scholar
• Haines, P. W. (2000). Problematic fossils in the late Neoproterozoic Wonoka Formation, South Australia. Precambrian Research, 100(1–3), 97–108. https://doi.org/10.1016/S0301-9268(99)00070-4
   Web of Science ®Google Scholar
• Harden, J. W. (1982). A quantitative index of soil development from field descriptions: Examples from a chronosequence in central California. Geoderma, 28(1), 1–28. https://doi.org/10.1016/0016-7061(82)90037-4
   Web of Science ®Google Scholar
• Hawco, J. B., Kenchington, C. G., & McIlroy, D. (2019). A quantitative and statistical discrimination of morphotaxa within the Ediacaran genus Palaeopascichnus. Papers in Palaeontology. https://doi.org/10.1002/spp2.1290
   Google Scholar
• Hayes, J. L., Riebe, C. S., Holbrook, S. W., Flinchum, B. A., & Hartsough, P. C. (2019). Porosity production in weathered rock: Where volumetric strain dominates over chemical mass loss. Science Advances, 5(9), eaao0834. https://doi.org/10.1126/sciadv.aao0834
   PubMed Web of Science ®Google Scholar
• Hebert, C. L., Kaufman, A. J., Penniston-Dorland, S. C., & Martin, A. J. (2010). Radiometric and stratigraphic constraints on terminal Ediacaran (post-Gaskiers) glaciation and metazoan evolution. Precambrian Research, 182(4), 402–412. https://doi.org/10.1016/j.precamres.2010.07.008
   Web of Science ®Google Scholar
• Hobson, R. A. (1930). Zebra rock from Kimberley. Journal of the Royal Society of Western Australia, 16, 57–70.
   Google Scholar
• Hoffman, P. F., Kaufman, A. J., Halverson, G. P., & Schrag, D. P. (1998). A Neoproterozoic Snowball Earth. Science, 281(5381), 1342–1346. https://doi.org/10.1126/science.281.5381.1342
   PubMed Web of Science ®Google Scholar
• Huang, C-M., Wang, C-S., & Tang, Y. (2005). Stable carbon and oxygen isotopes of pedogenic carbonates in Ustic Vertisols: Implications for paleoenvironmental change. Pedosphere, 15(4), 539–544.
   Web of Science ®Google Scholar
• Hunter, R. E. (1977). Basic types of stratification in small eolian dunes. Sedimentology, 24(3), 361–387. https://doi.org/10.1111/j.1365-3091.1977.tb00128.x
   Web of Science ®Google Scholar
• Isbell, R. F. (1996). The Australian soil classification (revised ed., pp. 144). CSIRO Publishing.
   Google Scholar
• Jafarzadeh, A. A., & Burnham, C. P. (1992). Gypsum crystals in soils. Journal of Soil Science, 43(3), 409–420. https://doi.org/10.1111/j.1365-2389.1992.tb00147.x
   Google Scholar
• Jarraggirrem. (2017). Gija-English online dictionary. Retrieved May 28, 2020, from https://issuu.com/jarraggirrem/docs/gija-english-dictionary
   Google Scholar
• Jensen, S. (2003). The Proterozoic and Earliest Cambrian trace fossil record: Patterns, problems, and perspectives. Integrative and Comparative Biology, 43(1), 219–228. https://doi.org/10.1093/icb/43.1.219
   PubMed Web of Science ®Google Scholar
• Jourdan, F., Hodges, K., Sell, B., Schaltegger, U., Wingate, M. T. D., Evins, L. Z., Söderlund, U., Haines, P. W., Phillips, D., & Blenkinsop, T. (2014). High-precision dating of the Kalkarindji large igneous province, Australia, and synchrony with the Early–Middle Cambrian (Stage 4–5) extinction. Geology, 42(6), 543–546. https://doi.org/10.1130/G35434.1
   Web of Science ®Google Scholar
• Kelka, U., Veveakis, M., Koehn, D., & Beaudoin, N. (2017). Zebra rocks: Compaction waves create ore deposits. Scientific Reports, 7(1), 1–9. https://doi.org/10.1038/s41598-017-14541-3
   PubMed Web of Science ®Google Scholar
• Kennedy, M. J. (1996). Stratigraphy, sedimentology, and isotopic geochemistry of Australian Neoproterozoic postglacial cap dolostones; deglaciation, δ13C excursions, and carbonate precipitation. Journal of Sedimentary Research, 66(6), 1050–1064. https://doi.org/10.2110/jsr.66.1050
   Web of Science ®Google Scholar
• Knauth, L. P., Brilli, M., & Klonowski, S. (2003). Isotope geochemistry of caliche developed on basalt. Geochimica et Cosmochimica Acta, 67(2), 185–195. https://doi.org/10.1016/S0016-7037(02)01051-7
   Web of Science ®Google Scholar
• Knoll, A., Walter, M., Narbonne, G., & Christie-Blick, N. (2006). The Ediacaran Period: A new addition to the geologic time scale. Lethaia, 39(1), 13–30. https://doi.org/10.1080/00241160500409223
   Web of Science ®Google Scholar
• Kolesnikov, A. V., Rogov, V. I., Bykova, N. V., Danelian, T., Clausen, S., Maslov, A. V., & Grazhdankin, D. V. (2018). The oldest skeletal macroscopic organism Palaeopascichnus linearis. Precambrian Research, 316, 24–37. https://doi.org/10.1016/j.precamres.2018.07.017
   Web of Science ®Google Scholar
• Kruse, P. D., Laurie, J. R., & Webby, B. D. (2004). Cambrian geology and palaeontology of the Ord Basin. Memoirs of the Association of Australasian Palaeontologists, 30, 1–58. http://hdl.handle.net/1959.14/41350
   Google Scholar
• Kurtz, A. C., Derry, L. A., & Chadwick, O. A. (2001). Accretion of Asian dust to Hawaiian soils: Isotopic, elemental, and mineral mass balances. Geochimica et Cosmochimica Acta, 65(12), 1971–1983. https://doi.org/10.1016/S0016-7037(01)00575-0
   Web of Science ®Google Scholar
• Lan, Z. W., & Chen, Z. Q. (2012). Possible animal body fossils from the late Neoproterozoic interglacial successions in the Kimberley region, northwestern Australia. Gondwana Research, 21(1), 293–301. https://doi.org/10.1016/j.gr.2011.05.014
   Web of Science ®Google Scholar
• Lan, Z. W., & Chen, Z. Q. (2013). Proliferation of MISS-forming microbial mats after the late Neoproterozoic glaciations: Evidence from the Kimberley region, NW Australia. Precambrian Research, 224, 529–550. https://doi.org/10.1016/j.precamres.2012.11.008
   Web of Science ®Google Scholar
• Lan, Z. Q., Zhang, S., Li, X. H., Pandey, S. K., Sharma, M., Shukla, Y., Ahmad, S., Sarkar, S., & Zhai, M. (2020). Towards resolving the ‘jigsaw puzzle’ and age-fossil inconsistency within East Gondwana. Precambrian Research, 345, 105775. https://doi.org/10.1016/j.precamres.2020.105775
   Web of Science ®Google Scholar
• Larcombe, C. O. G. (1927). Some rocks from four miles east of Argyle Station, Ord River, King district, Kimberley division. Annual Progress Report of the Geological Survey of Western Australia, for 1926, 23–24. https://www.dmp.wa.gov.au/Documents/About-Us-Careers/AnnualReport_1926.pdf
   Google Scholar
• Larcombe, C. O. G. (1925). Rock specimens from Ord River and Oakover River respectively. Annual Progress Report of the Geological Survey of Western Australia, for 1924 (Vol. 19). Geological Survey of Western Australia.
   Google Scholar
• Bas, M. J. L., Maitre, R. W. L., Streckeisen, A., & Zanettin, B. (1986). A chemical classification of volcanic rocks based on the total alkali-silica diagram. Journal of Petrology, 27(3), 745–750. https://doi.org/10.1093/petrology/27.3.745
   Web of Science ®Google Scholar
• Liivamägi, S., Somelar, P., Mahaney, W. C., Kirs, J., Vircava, I., & Kirsimäe, K. (2014). Late Neoproterozoic Baltic paleosol: Intense weathering at high latitude? Geology, 42(4), 323–326. https://doi.org/10.1130/G35209.1
   Web of Science ®Google Scholar
• Lohmann, K. G. (1988). Geochemical patterns of meteoric diagenetic systems and their application to studies of paleokarst. In N. P. James & P. W. Choquette (Eds.), Paleokarst (pp. 59–80). Springer.
   Google Scholar
• Loughnan, F. C., & Roberts, F. I. (1990). Composition and origin of the ‘zebra rock’ from the East Kimberley region of Western Australia. Australian Journal of Earth Sciences, 37(2), 201–205. https://doi.org/10.1080/08120099008727920
   Web of Science ®Google Scholar
• Ludvigson, G. A., González, L. A., Fowle, D. A., Roberts, J. A., Driese, S. G., Villarreal, M. A., Smith, J. J., Suarez, M. B., & Nordt, L. C. (2013). Paleoclimatic applications and modern process studies of pedogenic siderite. In S. G. Driese & L. C. Nordt (Eds.), New Frontiers in Paleopedology and Terrestrial Paleoclimatology (pp. 79–87, Vol. 104). Society of Economic Paleontologists & Mineralogists Special Publication.
   Google Scholar
• Ludvigson, G. A., González, L. A., Metzger, R. A., Witzke, B. J., Brenner, R. L., Murillo, A. P., & White, T. S. (1998). Meteoric sphaerosiderite lines and their use for paleohydrology and paleoclimatology. Geology, 26(11), 1039–1042. https://doi.org/10.1130/0091-7613(1998)026<1039:MSLATU>2.3.CO;2
   Web of Science ®Google Scholar
• Marshall, P. E., Widdowson, M., & Murphy, D. T. (2016). The Giant Lavas of Kalkarindji: Rubbly pāhoehoe lava in an ancient continental flood basalt province. Palaeogeography, Palaeoclimatology, Palaeoecology, 441, 22–37. https://doi.org/10.1016/j.palaeo.2015.05.006
   Web of Science ®Google Scholar
• Martin, E., & Bindeman, I. (2009). Mass-independent isotopic signatures of volcanic sulfate from three supereruption ash deposits in Lake Tecopa, California. Earth and Planetary Science Letters, 282(1–4), 102–114. https://doi.org/10.1016/j.epsl.2009.03.005
   Web of Science ®Google Scholar
• Mattievich, E., Chadwick, J., Cashion, J. D., Boas, J. F., Clark, M. J., Mackie, R. D. (2003). Macroscopic ferronematic liquid crystals determine the structure of Kimberley Zebra Rock [Paper presentation]. Conference Handbook Annual Condensed Matter Physics Meeting Wagga, Wagga, 27, 1–3. http://www.aip.org.au/wp-content/uploads/cmm/2003/WW03_33.pdf
   Google Scholar
• Mawson, D., & Segnit, E. R. (1949). Purple slates of the Adelaide System. Transactions of the Royal Society of South Australia, 72, 276–280.
   Google Scholar
• McKenzie, N., Jacquier, D., Isbale, R., & Brown, K. (2004). Australian soils and landscapes (p. 416). CSIRO.
   Google Scholar
• Mehmood, M., Yaseen, M., Khan, E. U., & Khan, M. J. (2018). Dolomite and dolomitization model—a short review. International Journal of Hydrology, 2(5), 549–553. https://doi.org/10.15406/ijh.2018.02.00124
   Google Scholar
• Melim, L. A., Swart, P. K., & Eberli, G. P. (2004). Mixing zone diagenesis in the subsurface of Florida and the Bahamas. Journal of Sedimentary Research, 74(6), 904–913. https://doi.org/10.1306/042904740904
   Web of Science ®Google Scholar
• Mory, A. J., & Beere, G. M. (1985). Palaeozoic stratigraphy of the Ord Basin, Western Australia and Northern Territory. Geological Survey of Western Australia Reports, 14, 36–45. https://dmpbookshop.eruditetechnologies.com.au//product/Palaeozoic-stratigraphy-of-the-Ord-Basin-Western-Australia-and-Northern-Territory.do
   Google Scholar
• Murphy, C. P. (1983). Point counting pores and illuvial clay in thin section. Geoderma, 31(2), 133–150. https://doi.org/10.1016/0016-7061(83)90004-6
   Web of Science ®Google Scholar
• Nance, W. B., & Taylor, S. R. (1976). Rare earth element patterns and crustal evolution—I. Australian post-Archean sedimentary rocks. Geochimica et Cosmochimica Acta, 40(12), 1539–1551. https://doi.org/10.1016/0016-7037(76)90093-4
   Web of Science ®Google Scholar
• Navarro-González, R., Rainey, F. A., Molina, P., Bagaley, D. R., Hollen, B. J., de la Rosa, J., Small, A. M., Quinn, R. C., Grunthaner, F. J., Cáceres, L., Gomez-Silva, B., & McKay, C. P. (2003). Mars-like soils in the Atacama Desert, Chile, and the dry limit of microbial life. Science (New York, N.Y.), 302(5647), 1018–1021. https://doi.org/10.1126/science.1089143
   PubMed Web of Science ®Google Scholar
• Neaman, A., Chorover, J., & Brantley, S. L. (2005a). Element mobility patterns record organic ligands in soils on early Earth. Geology, 33(2), 117–120. https://doi.org/10.1130/G20687.1
   Web of Science ®Google Scholar
• Neaman, A., Chorover, J., & Brantley, S. L. (2005b). Implications of the evolution of organic acid moieties for basalt weathering over geological time. American Journal of Science, 305(2), 147–185. https://doi.org/10.2475/ajs.305.2.147
   Web of Science ®Google Scholar
• Nesbitt, H. W., & Young, G. M. (1982). Early Proterozoic climates and plate motions inferred from major element chemistry of lutites. Nature, 299(5885), 715–717. https://doi.org/10.1038/299715a0
   Web of Science ®Google Scholar
• Nesbitt, H. W., & Young, G. M. (1989). Formation and diagenesis of weathering profiles. The Journal of Geology, 97(2), 129–147. https://doi.org/10.1086/629290
   Web of Science ®Google Scholar
• Noffke, N. (2010). Geobiology: Microbial mats in sandy deposits from the Archean Era to today. Springer.
   Google Scholar
• Nordt, L. C., & Driese, S. D. (2010). New weathering index improves paleorainfall estimates from Vertisols. Geology, 38(5), 407–410. https://doi.org/10.1130/G30689.1
   Web of Science ®Google Scholar
• Novoselov, A. A., & de Souza Filho, C. R. (2015). Potassium metasomatism of Precambrian paleosols. Precambrian Research, 262, 67–83. https://doi.org/10.1016/j.precamres.2015.02.024
   Web of Science ®Google Scholar
• Olawsky, K. J., & Kofod, F. (2019). Miriwoong Woorlang Yawoorroonga-Woor. Mirima Dawang Woorlab-garring Language and Cultural Center.
   Google Scholar
• Öpik, A. A. (1970). Redlichia of the Ordian (Cambrian) of Northern Australia and New South Wales. Bulletin of the Bureau of Mineral Resources Geology and Geophysics Canberra, 114, 1–66.
   Google Scholar
• Óskarsson, B. V., Riishuus, M. S., & Arnalds, Ó. (2012). Climate-dependent chemical weathering of volcanic soils in Iceland. Geoderma, 189-190, 635–651. https://doi.org/10.1016/j.geoderma.2012.05.030
   Web of Science ®Google Scholar
• Parcha, S. K., & Pandey, S. (2011). Ichnofossils and their significance in the Cambrian successions of the Parahio Valley in the Spiti Basin, Tethys Himalaya, India. Journal of Asian Earth Sciences, 42(6), 1097–1116. https://doi.org/10.1016/j.jseaes.2011.04.028
   Web of Science ®Google Scholar
• Peckmann, J., Goedert, J. L., Thiel, V., Michaelis, W., & Reitner, J. (2002). A comprehensive approach to the study of methane‐seep deposits from the Lincoln Creek Formation, western Washington State, USA. Sedimentology, 49(4), 855–873. https://doi.org/10.1046/j.1365-3091.2002.00474.x
   Web of Science ®Google Scholar
• Plumb, K. A., Derrick, G. M., Needham, R. S., & Shaw, R. D. (1981). The Proterozoic of northern Australia. In. D. R. Hunter (Ed.), Precambrian of the southern hemisphere. (pp. 205–307, Vol. 2). Elsevier.
   Google Scholar
• Prave, A. R. (2002). Life on land in the Proterozoic: Evidence from the Torridonian rocks of northwest Scotland. Geology, 30(9), 811–814. https://doi.org/10.1130/0091-7613(2002)0300811:LOLITP2.0.CO;2
   Web of Science ®Google Scholar
• Pu, J. P., Bowring, S. A., Ramezani, J., Myrow, P., Raub, T. D., Landing, E., Mills, A., Hodgin, E., & Macdonald, F. A. (2016). Dodging snowballs: Geochronology of the Gaskiers glaciation and the first appearance of the Ediacaran biota. Geology, 44(11), 955–958. https://doi.org/10.1130/G38284.1
   Web of Science ®Google Scholar
• Ramakrishnan, D., & Tiwari, K. C. (1999). REE chemistry of arid zone calcrete profiles–A case study from the Thar Desert. India. Turkish Journal of Earth Sciences, 7(2), 97–104. https://journals.tubitak.gov.tr/earth/abstract.htm?id=2002
   Google Scholar
• Rawling, J. E. (2000). A review of lamellae. Geomorphology, 35(1–2), 1–9. https://doi.org/10.1016/S0169-555X(00)00015-5
   Web of Science ®Google Scholar
• Renaut, R. W., & Tiecerlin, J-J. (1994). Lake Bogoria, Kenya Rift Valley − a sedimentological overview. In R. W. Renaut & W. M. Last (Eds.), Sedimentology and Geochemistry of Modern and Ancient Saline Lakes (pp. 101–124, Vol. 50). Society for Sedimentary Geology Special Publication.
   Google Scholar
• Retallack, G. J. (1976). Triassic palaeosols in the upper Narrabeen Group of New South Wales. Part I: Features of the palaeosols. Journal of the Geological Society of Australia, 23(4), 383–399. https://doi.org/10.1080/00167617608728953
   Google Scholar
• Retallack, G. J. (1991a). Untangling the effects of burial alteration and ancient soil formation. Annual Review of Earth and Planetary Sciences, 19(1), 183–206. https://doi.org/10.1146/annurev.ea.19.050191.001151
   Google Scholar
• Retallack, G. J. (1991b). Miocene paleosols and ape habitats of Pakistan and Kenya. Oxford University Press.
   Google Scholar
• Retallack, G. J. (2005). Pedogenic carbonate proxies for amount and seasonality of precipitation in paleosols. Geology, 33(4), 333–336. https://doi.org/10.1130/G21263.1
   Web of Science ®Google Scholar
• Retallack, G. J. (2008). Cambrian paleosols and landscapes of South Australia. Australian Journal of Earth Sciences, 55(8), 1083–1106. https://doi.org/10.1080/08120090802266568
   Web of Science ®Google Scholar
• Retallack, G. J. (2011). Neoproterozoic loess and limits to Snowball Earth. Journal of the Geological Society of London, 168(2), 289–308. https://doi.org/10.1144/0016-76492010-051
   Web of Science ®Google Scholar
• Retallack, G. J. (2012a). Criteria for distinguishing microbial mats and earths. In N. Noffke & H. Chafetz (Eds.), Microbial mats in siliciclastic sediments (pp. 136–152). Society of Economic Paleontologists and Mineralogists Special Paper. 101.
   Google Scholar
• Retallack, G. J. (2012b). Mallee model for mammal communities of the early Cenozoic and Mesozoic. Palaeogeography, Palaeoclimatology, Palaeoecology, 342-343, 111–129. https://doi.org/10.1016/j.palaeo.2012.05.009
   Web of Science ®Google Scholar
• Retallack, G. J. (2013). Ediacaran life on land. Nature, 493(7430), 89–92. https://doi.org/10.1038/nature11777
   PubMed Web of Science ®Google Scholar
• Retallack, G. J. (2014). Affirming life aquatic for the Ediacara biota in China and Australia: COMMENT. Geology, 42(3), e325–e325. https://doi.org/10.1130/G35030C.1
   Web of Science ®Google Scholar
• Retallack, G. J. (2015a). Silurian vegetation stature and density inferred from fossil soils and plants in Pennsylvania, U.S.A. Journal of the Geological Society London, 172(6), 693–709. https://doi.org/10.1144/jgs2015-022
   Web of Science ®Google Scholar
• Retallack, G. J. (2015b). Late Ordovician glaciation initiated by early land plant evolution, and punctuated by greenhouse mass-extinctions. The Journal of Geology, 123(6), 509–538. https://doi.org/10.1086/683663
   Web of Science ®Google Scholar
• Retallack, G. J. (2016). Field and laboratory tests for recognition of Ediacaran paleosols. Gondwana Research, 36, 107–110. https://doi.org/10.1016/j.gr.2016.05.001
   Web of Science ®Google Scholar
• Retallack, G. J. (2018). Oldest recognized paleosols on Earth, Panorama Formation (3.46 Ga), Western Australia. Palaeogeography Palaeoclimatology Palaeoecology, 489, 230–248. https://doi.org/10.1016/j.palaeo.2017.10.013
   Web of Science ®Google Scholar
• Retallack, G. J. (2019). Interflag sandstone laminae, a novel fluvial sedimentary structure with implication for Ediacaran paleoenvironments. Sedimentary Geology, 379, 60–76. https://doi.org/10.1016/j.sedgeo.2018.11.003
   Web of Science ®Google Scholar
• Retallack, G. J. (2020). Boron paleosalinity proxy for deeply buried Paleozoic and Ediacaran fossils. Palaeogeography Palaeoclimatology Palaeoecology, 540, 109536. https://doi.org/10.1016/j.palaeo.2019.109536
   Web of Science ®Google Scholar
• Retallack, G. J., & Broz, A. P. (2020). Arumberia and other Ediacaran–Cambrian fossils of central Australia. Historical Biology. https://doi.org/10.1080/08912963.2020.175581.
   Google Scholar
• Retallack, G. J., & Huang, C. (2010). Depth to gypsic horizon as a proxy for paleoprecipitation in paleosols of sedimentary environments. Geology, 38(5), 403–406. https://doi.org/10.1130/G30514.1
   Web of Science ®Google Scholar
• Retallack, G. J., Krinsley, D. H., Fischer, R., Razink, J. J., & Langworthy, K. A. (2016). Archean coastal-plain paleosols and life on land. Gondwana Research, 40, 1–20. https://doi.org/10.1016/j.gr.2016.08.003
   Web of Science ®Google Scholar
• Retallack, G. J., & Mao, X. (2019). Paleoproterozoic (ca. 1.9 Ga) megascopic life on land in Western Australia. Palaeogeography, Palaeoclimatology, Palaeoecology, 532, 109266. https://doi.org/10.1016/j.palaeo.2019.109266
   Web of Science ®Google Scholar
• Retallack, G. J., Marconato, A., Osterhout, J. T., Watts, K. E., & Bindeman, I. N. (2014). Revised Wonoka isotopic anomaly in South Australia and Late Ediacaran mass extinction. Journal of the Geological Society of London, 171(5), 709–722. https://doi.org/10.1144/jgs2014-016
   Web of Science ®Google Scholar
• Retallack, G. J., & Mindszenty, A. (1994). Well preserved Late Precambrian paleosols from northwest Scotland. Journal of Sedimentary Research, A64(2), 264–281. https://doi.org/10.1306/D4267D7A-2B26-11D7-8648000102C1865D
   Google Scholar
• Ruhe, R. V., & Olson, C. G. (1980). Clay mineral indicators of glacial and non-glacial sources of Wisconsinan loesses in southern Indiana, USA. Geoderma, 24(4), 283–297. https://doi.org/10.1016/0016-7061(80)90056-7
   Web of Science ®Google Scholar
• Runnegar, B. (1995). Vendobionta or metazoa? Developments in understanding the Ediacara ‘‘fauna. Neues Jahrbuch Für Geologie Und Paläontologie—Abhandlungen, 195(1–3), 303–318. https://doi.org/10.1127/njgpa/195/1995/303
   Google Scholar
• Sadek, S., Rabih, S., & Lagzi, I. (2010). Liesegang patterns in nature: A diverse scenery across the sciences. Precipitation Patterns in Reaction-Diffusion Systems, 661, 1–43.
   Google Scholar
• Schulz, M., Stonestrom, D., Lawrence, C., Bullen, T., Fitzpatrick, J., Kyker-Snowman, E., Manning, J., & Mnich, M. (2016). Structured heterogeneity in a marine terrace chronosequence: Upland mottling. Vadose Zone Journal, 15(2), vzj2015.07.0102. https://doi.org/10.2136/vz/2015.07.0102 https://doi.org/10.2136/vzj2015.07.0102
   Web of Science ®Google Scholar
• Scotese, C. R. (2009). Late Proterozoic plate tectonics and palaeogeography: A tale of two supercontinents, Rodinia and Pannotia. In J. Craig, J. Thurow, B. Thusu, A. Whitham & Y. Abutarruma (Eds.), Global Neoproterozoic Petroleum Systems: The Emerging Potential in North Africa (pp. 67–83). Geological Society of London, Special Publication, 326. https://doi.org/10.1144/SP326.4
   Google Scholar
• Seilacher, A., Grazhdankin, D., & Legouta, A. (2003). Ediacaran biota: The dawn of animal life in the shadow of giant protists. Paleontological Research, 7(1), 43–54. https://doi.org/10.2517/prpsj.7.43
   Google Scholar
• Setti, M., Marinoni, L., & Lopez-Galindo, A. (2004). Mineralogical and geochemical characteristics (major, minor, trace elements and REE) of detrital and authigenic clay minerals in a Cenozoic sequence from Ross Sea. Clay Minerals, 39(4), 405–421. https://doi.org/10.1180/000985503540143
   Web of Science ®Google Scholar
• Sheldon, N. D. (2003). Pedogenesis and geochemical alteration of the Picture Gorge subgroup, Columbia River basalt, Oregon. Geological Society of America Bulletin, 115(11), 1377–1387. https://doi.org/10.1130/B25223.1
   Web of Science ®Google Scholar
• Sheldon, N. D., & Retallack, G. J. (2001). Equation for compaction of paleosols due to burial. Geology, 29(3), 247–250. https://doi.org/10.1130/0091-7613(2001)0290247:EFCOPD2.0.CO;2
   Web of Science ®Google Scholar
• Sheldon, N. D., Retallack, G. J., & Tanaka, S. (2002). Geochemical climofunctions from North American soils and application to paleosols across the Eocene–Oligocene boundary in Oregon. The Journal of Geology, 110(6), 687–696. https://doi.org/10.1086/342865
   Web of Science ®Google Scholar
• Shen, B., Xiao, S., Zhou, C., & Yuan, X. (2009). Yangtziramulus zhangi new genus and species, a carbonate-hosted macrofossil from the Ediacaran Dengying Formation in the Yangtze Gorges area. Journal of Paleontology, 83(4), 575–587. https://doi.org/10.1666/08-042R1.1
   Web of Science ®Google Scholar
• Soil Survey Staff. (2014). Keys to soil taxonomy. Natural Resources Conservation Service.
   Google Scholar
• Sprigg, R. C. (1949). Early Cambrian “jellyfishes” at Ediacara, South Australia and Mount John, Kimberley District, Western Australia. Transactions of the Royal Society of South Australia, 73(1), 72–99.
   Google Scholar
• Stace, H. C. T., Hubble, G. D., Brewer, R., Northcote, K. H., Sleeman, J. R., Mulcahy, M. J., & Hallsworth, E. G. (1968). A handbook of Australian soils. Rellim.
   Google Scholar
• Stimson, M. R., Miller, R. F., MacRae, R. A., & Hinds, S. J. (2017). An ichnotaxonomic approach to wrinkled microbially induced sedimentary structures. Ichnos, 24(4), 291–316. https://doi.org/10.1080/10420940.2017.1294590
   Web of Science ®Google Scholar
• Sugahara, H., Sugitani, K., Mimura, K., Yamashita, F., & Yamamoto, K. (2010). A systematic rare-earth elements and yttrium study of Archean cherts at the Mount Goldsworthy greenstone belt in the Pilbara Craton: Implications for the origin of microfossil-bearing black cherts. Precambrian Research, 177(1–2), 73–87. https://doi.org/10.1016/j.precamres.2009.10.005
   Web of Science ®Google Scholar
• Surge, D. M., Savarese, M., Dodd, J. R., & Lohmann, K. C. (1997). Carbon isotopic evidence for photosynthesis in Early Cambrian oceans. Geology, 25(6), 503–506. https://doi.org/10.1130/0091-7613(1997)0250503:CIEFPI2.3.CO;2
   Web of Science ®Google Scholar
• Sweet, I. P., Mendum, J. R., Morgan, C. M., & Pontifex, I. R. (1974). The geology of the Northern Victoria River Region, NT. Bureau of Mineral Resources Geology and Geophysics Report (Vol. 166). Bureau of Mineral Resources Geology and Geophysics. https://ecat.ga.gov.au/geonetwork/srv/eng/catalog.search#/metadata/15078
   Google Scholar
• Sweet, I. P., Pontifex, I. R., & Morgan, C. M. (1974). Geology of the Auvergne 1:250 000 Sheet Area, NT (excluding Bonaparte Gulf Basin). Bureau of Mineral Resources Geology and Geophysics Report (Vol. 161). Bureau of Mineral Resources Geology and Geophysics. https://ecat.ga.gov.au/geonetwork/srv/eng/catalog.search#/metadata/15076
   Google Scholar
• Talbot, M. R. (1990). A review of the palaeohydrological interpretation of carbon and oxygen isotopic ratios in primary lacustrine carbonates. Chemical Geology: Isotope Geoscience Section, 80(4), 261–279. https://doi.org/10.1016/0168-9622(90)90009-2
   Google Scholar
• Taylor, R. S., Hawco, J. B., Nichols, R., & McIlroy, D. (2019). A critical reappraisal of the holotype of Beothukis mistakensis, a unique exceptionally preserved rangeomorph organism from Mistaken Point, Newfoundland, Canada. Estudios Geológicos, 75(2), e117. https://doi.org/10.3989/egeol.43586.572
   Web of Science ®Google Scholar
• Terry, R. D., & Chilingar, G. V. (1955). Summary of “Concerning some additional aids in studying sedimentary formations,” by MS Shvetsov. Journal of Sedimentary Research, 25(3), 229–234. https://doi.org/10.1306/74D70466-2B21-11D7-8648000102C1865D
   Google Scholar
• Trainer, D. W. (1931). Zebra Rock. American Mineralogist, 16, 221–225.
   Google Scholar
• Ufnar, D. F., Gröcke, D. R., & Beddows, P. A. (2008). Assessing pedogenic calcite stable-isotope values: Can positive linear covariant trends be used to quantify palaeo-evaporation rates?. Chemical Geology, 256(1–2), 46–51. https://doi.org/10.1016/j.chemgeo.2008.07.022
   Web of Science ®Google Scholar
• Veizer, J., Ala, D., Azmy, K., Bruckschen, P., Buhl, D., Bruhn, F., Carden, G. A. F., Diener, A., Ebneth, S., Godderis, Y., Jasper, T., Korte, C., Pawellek, F., Podlaha, O. G., & Strauss, H. (1999). 87Sr/86Sr, δ13C and δ18O evolution of Phanerozoic seawater. Chemical Geology, 161(1–3), 59–88. https://doi.org/10.1016/S0009-2541(99)00081-9
   Web of Science ®Google Scholar
• Vepraskas, M. J., & Sprecher, S. W. (1997). Summary. In M. J. Vepraskas & S. W. Sprecher (Eds.), Aquic conditions and hydric soils: The problem soils (pp. 153–156). Soil Science Society of America Special Publication 150.
   Google Scholar
• Wallace, M. W., & Hood, A. S. (2018). Zebra textures in carbonate rocks: Fractures produced by the force of crystallization during mineral replacement. Sedimentary Geology, 368, 58–67. https://doi.org/10.1016/j.sedgeo.2018.03.009
   Web of Science ®Google Scholar
• Walter, M. R. (1976). Stromatolites. Elsevier.
   Google Scholar
• Wan, B., Chen, Z., Yuan, X., Pang, K., Tang, Q., Guan, C., Wang, X., Pandey, S. K., Droser, M. L., & Xiao, S. (2020). A tale of three taphonomic modes: The Ediacaran fossil Flabellophyton preserved in limestone, black shale, and sandstone. Gondwana Research, 84, 296–314. https://doi.org/10.1016/j.gr.2020.04.003
   Web of Science ®Google Scholar
• Weinberger, R. (2001). Evolution of polygonal patterns in stratified mud during desiccation: The role of flaw distribution and layer boundaries. Geological Society of America Bulletin, 113(1), 20–31.https://doi.org/10.1130/0016-7606(2001)1130020:EOPPIS2.0.CO;2
   Web of Science ®Google Scholar
• Williams, G. E., Gostin, V. A., McKirdy, D. M., & Preiss, W. V. (2008). The Elatina glaciation, late Cryogenian (Marinoan Epoch), South Australia: Sedimentary facies and palaeoenvironments. Precambrian Research, 163(3–4), 307–331. https://doi.org/10.1016/j.precamres.2007.12.001
   Web of Science ®Google Scholar
• Winchester, J. A., & Floyd, P. A. (1977). Geochemical discrimination of different magma series and their differentiation products using immobile elements. Chemical Geology, 20, 325–343. https://doi.org/10.1016/0009-2541(77)90057-2
   Web of Science ®Google Scholar
• Ziegenbalg, S. B., Brunner, B., Rouchy, J. M., Birgel, D., Pierre, C., Böttcher, M. E., Caruso, A., Immenhauser, A., & Peckmann, J. (2010). Formation of secondary carbonates and native sulphur in sulphate-rich Messinian strata, Sicily. Sedimentary Geology, 227(1–4), 37–50. https://doi.org/10.1016/j.sedgeo.2010.03.007
   Web of Science ®Google Scholar