[1] Antoshkina A.,2015. Ooid-stromatolite association as a precursor of bioevents (Silurian, Timan-northern Ural Region).Palaeoworld, 24(1-2): 198-206.
[2] Bathurst R.G.C.,1967. Oölitic films on low energy carbonate sand grains, Bimini Lagoon, Bahamas.Marine Geology, 5(2): 89-109.
[3] Bathurst R.G.C., 1975. Carbonate Sediments and Their Diagenesis. Second Enlarged Edition. Amsterdam: Elsevier Scientific Publishing Company, pp.1-658.
[4] Brehm U., Krumbein W., andPalinska K., 2006. Biomicrospheres generate ooids in the laboratory.Geomicrobiology Journal, 23(7): 545-550.
[5] Brehm U., Palinska K.A., andKrumbein W.E., 2004. Laboratory cultures of calcifying biomicrospheres generate ooids - A contribution to the origin of oolites.Carnets De Géologie, 3: 1-6.
[6] Chen B.B., Qi Y.A., Zheng W., andLi X.Y., 2019b. Micritic calcites in ooids and their genetic analysis from the Cambrian Mantou Formation in Yiyang area, western Henan Province.Journal of Palaeogeoraphy (Chinese Edition), 21(04): 603-612 (in Chinese with English Abstract).
[7] Chen, Z.Q, Tu C., Pei Y., Ogg J., Fang Y., Wu S., Feng X., Huang Y., Guo Z., andYang H., 2019a. Biosedimentological features of major microbe-metazoan transitions (MMTs) from Precambrian to Cenozoic.Earth-Science Reviews, 189: 21-50.
[8] Chen, Z.Q, Zhou C.M., andStanley G., 2017. Biosedimentary records of China from the Precambrian to present.Palaeogeography, Palaeoclimatology, Palaeoecology, 474: 1-6.
[9] Dai M.Y., Qi Y.A., Chen Y., andLi D., 2014. Giant ooids and their genetic analysis from the Zhangxia Formation of Cambrian Series 3 in Mianchi area, western Henan Province.Journal of Palaeogeoraphy (Chinese Edition), 16(5): 726-734 (in Chinese with English Abstract).
[10] Dai M.Y., Qi Y.A., Zhang X.Y., andLi D., 2016. Girvanella in Oncoids from the Mantou Formation (Cambrian Series 3), Mianchi, Western Henan.Earth Science, 41(6): 919-930 (in Chinese with English Abstract).
[11] Davaud E., andGirardclos S., 2001. Recent freshwater ooids and oncoids from Western Lake Geneva (Switzerland): Indications of a common organically mediated origin.Journal of Sedimentary Research, 71(3): 423-429.
[12] Davies P., Bubela B., andFerguson J., 1978. The formation of ooids.Sedimentology, 25(5): 703-730.
[13] Diaz M., andEberli G., 2019. Decoding the mechanism of formation in marine ooids: A review.Earth-Science Reviews, 190: 536-556.
[14] Diaz M., Eberli G., Blackwelder P., Phillips B., andSwart P., 2017. Microbially mediated organomineralization in the formation of ooids.Geology, 45(9): 771-774.
[15] Diaz M., Piggot A., Eberli G., andKlaus J., 2013. Bacterial community of oolitic carbonate sediments of the Bahamas Archipelago.Marine Ecology Progress Series, 485: 9-24.
[16] Diaz M., Van Norstrand J., Eberli G., Piggot A., Zhou J., andKlaus J., 2014. Functional gene diversity of oolitic sands from Great Bahama Bank.Geobiology, 12(3): 231-249.
[17] Duguid S.M.A., Kyser T.K., James N.P., andRankey E.C., 2010. Microbes and ooids.Journal of Sedimentary Research, 80(3): 236-251.
[18] Dupraz C., andVisscher P., 2005. Microbial lithification in marine stromatolites and hypersaline mats.Trends in Microbiology, 13(9): 429-438.
[19] Dupraz C., Reid R., Braissant O., Decho A., Norman R., andVisscher P., 2009. Processes of carbonate precipitation in modern microbial mats.Earth-Science Reviews, 96(3): 141-162.
[20] Fahraeus L.E., Slatt R.M., andNowlan G.S., 1974. Origin of carbonate pseudopellets.Journal of Sedimentary Research, 44(1): 27-29.
[21] Fang Q., Hong H., Chen Z., Yu J., Wang C., Yin K., Zhao L., Liu Z., Cheng F., Gong N., andFurnes H., 2016. Microbial proliferation coinciding with volcanism during the Permian-Triassic transition: New, direct evidence from volcanic ashes, South China.Palaeogeography, Palaeoclimatology, Palaeoecology, 474: 164-186.
[22] Feng Z.Z., andZhang Y.B., 2013. Petrography of carbonate rocks. In: Feng, Z.Z. (Ed.). Sedimentology of China (2nd Edition). Beijing: Petroleum Industry Press, pp. 137-198 (in Chinese with English Abstract).
[23] Feng Z.Z., Wang Y.H., Zhang J.S., Zuo W.Q., Zhang X.L., Hong G.L., Wu S.H., Chen Y.T., Chi Y.L., andYang C.Y., 1990. Lithofacies Paleogeography of the Early Paleozoic of North China Platform. Beijing: Geological Publishing House (in Chinese with English Abstract).
[24] Flügel, E., 2004. Microfacies of Carbonate Rocks. Springer, Berlin, 842 pp.
[25] Folk R., andLeo Lynch F., 2001. Organic matter, putative nannobacteria and the formation of ooids and hardgrounds.Sedimentology, 48(2): 215-229.
[26] Folk R.L.,1993. SEM imaging of bacteria and nannobacteria in carbonate sediments and rocks.SEPM Journal of Sedimentary Research, 63: 990-999.
[27] Gerdes G., Dunajtschik-Piewa K., Riege H., Taher A., Krumbein W., andReineck H., 1994. Structural diversity of biogenic carbonate particles in microbial mats.Sedimentology, 41(6): 1273-1294.
[28] Hillgartner H., Dupraz C., andHug W., 2001. Microbially induced cementation of carbonate sands: are micritic meniscus cements good indicators of vadose diagenesis?Sedimentology, 48(1): 117-131.
[29] Jones B., andPeng X., 2012. Amorphous calcium carbonate associated with biofilms in hot spring deposits. Sedimentary Geology, 269-270: 58-68.
[30] Li F., Wang X., Xue W.Q., andYan J.X., 2010. Origin and environmental significance of giant ooids in the Early Triassic: a new kind of anachronistic facies.Acta Sedimentologica Sinica, 28(3): 585-595 (in Chinese with English Abstract).
[31] Li F., Yan J., Algeo T., andWu X., 2013. Paleoceanographic conditions following the end-Permian mass extinction recorded by giant ooids (Moyang, South China).Global and Planetary Change, 105: 102-120.
[32] Li F., Yan J., Burne R., Chen Z., Algeo T., Zhang W., Tian L., Gan Y., Liu K., andXie S., 2017. Paleo-seawater REE compositions and microbial signatures preserved in laminae of Lower Triassic ooids.Palaeogeography, Palaeoclimatology, Palaeoecology, 486: 96-107.
[33] Liu W., andZhang X., 2012. Girvanella-coated grains from Cambrian oolitic limestone.Facies, 58(4): 779-787.
[34] Mei M.X.,2008. Implication for the unusual giant oolites of the Phanerozoic and their morphological diversity: A case study from the Triassic Daye Formation at the Lichuan Section in Hubei Province, South China.Geoscience, 22(5): 683-698 (in Chinese with English Abstract).
[35] Mei M.X.,2012a. Brief introduction on new advances on the origin of ooids.Acta Sedimentologica Sinica, 30(1): 20-32 (in Chinese with English Abstract).
[36] Mei M.X.,2012b. Organomineralization derived from the biomineralization: An important theme within the framework of geology.Geological Review, 58(5): 937-951 (in Chinese with English Abstract).
[37] Mei M.X.,2021. Giant ooids induced and predominated by photosynthetic biofilms of filamentous cyanobacteria: An example from the Miaolingian Xuzhuang Formation at the Shijing section in Xinan County of Henan Province, North-China Platform.Journal of Palaeogeography (Chinese Edition), 23(1): 105-124 (in Chinese with English Abstract).
[38] Mei M.X., andGao J.H., 2012. Giant Induan oolite: A case study from the Lower Triassic Daye Formation in the western Hubei Province, South China.Geoscience Frontiers, 3(6): 843-851.
[39] Mei M.X., Muhammad R., Lin L., andMeng Q.F., 2019. Leiolite bioherm dominated by cyanobacterial mats of the Furongian: An example from the Qijiayu Section in Laiyuan County, Hebei Province.Geological Review 65(5): 1103-1122 (in Chinese with English Abstract).
[40] Meng X., Ge M., andTucker M., 1997. Sequence stratigraphy, sea-level changes and depositional systems in the Cambro-Ordovician of the North China carbonate platform.Sedimentary Geology, 114(1-4): 189-222.
[41] Middleton G.V., Church M.J., andConiglio M., 2003. Encyclopedia of Sediments and Sedimentary Rocks. London: Kluwer Academic Publishers.
[42] Mitterer R.,1968. Amino acid composition of organic matrix in calcareous oolites.Science, 162(3861): 1498-1499.
[43] Mitterer R.,1972. Biogeochemistry of aragonite mad and oolites.Geochimica et Cosmochimica Acta, 36(12): 1407-1422.
[44] Newell N.D.,1960. Bahamian oolitic sands.Journal of Geology, 68: 481-497.
[45] O'Reilly S., Mariotti G., Winter A., Newman S., Matys E., McDermott F., Pruss S., Bosak T., Summons R., andKlepac-Ceraj V., 2016. Molecular biosignatures reveal common benthic microbial sources of organic matter in ooids and grapestones from Pigeon Cay, The Bahamas.Geobiology, 15(1): 112-130.
[46] Pacton M., Ariztegui D., Wacey D., Kilburn M., Rollion-Bard C., Farah R., andVasconcelos C., 2012. Going nano: A new step toward understanding the processes governing freshwater ooid formation.Geology, 40(6): 547-550.
[47] Paul J., Peryt T.M., andBurne R.V., 2011. Kalkowsky's Stromatolites and Oolites (Lower Buntsandstein, Northern Germany). In: Reitner, J., Quéric, N.-V., Arp, G., (Eds.). Advances in Stromatolite Geobiology. Lecture Notes in Earth Sciences, vol. 131. Springer, Berlin, Heidelberg, pp. 13-28. https://doi.org/10.1007/978-3-642-10415-2_2.
[48] Pei F., Zhang H.Q., andYan G.S., 2008. Stratigraphic Paleontology Research of Henan Province, Early Paleozoic Era, North China. Zhengzhou: Yellow River Water Resources Press, pp. 1-302 (in Chinese with English Abstract).
[49] Plée K., Ariztegui D., Martini R., andDavaud E., 2008. Unravelling the microbial role in ooid formation Results of an in situ experiment in modern freshwater Lake Geneva in Switzerland.Geobiology, 6(4): 341-350.
[50] Plée K., Pacton M., andAriztegui D., 2010. Discriminating the role of photosynthetic and heterotrophic microbes triggering low-Mg calcite precipitation in freshwater biofilms (Lake Geneva, Switzerland).Geomicrobiology Journal, 27(5): 391-399.
[51] Qi Y.A., Chai S., Zhang X.Y., Dai M.Y., andWang M., 2016. Oncoids and their depositional features from the Second Member of Mantou Formation (Cambrian Series 3), Weijui Area, Henan Province.China Sciencepaper, 11(21): 2416-2421 (in Chinese with English Abstract).
[52] Qi Y.A., Dai M.Y., Chang Y.G., Wang M., andLi D., 2013. The oncoids from the Second Member of Mantou Formation (The Third Series, Cambrian), Mianchi Area, Western Henan Province.Geological Journal of China Universities, 19(4): 919-930 (in Chinese with English Abstract).
[53] Qi Y.A., Zhang X.Y., Dai M.Y., andWang. M., 2017. Girvanella fossils and their microstructure from Cambrian microbialites of western Henan.Acta Palaeontologica Sinica, 56(2): 154-167 (in Chinese with English Abstract).
[54] Reitner J., Arp G., Thiel V. and Michaelis W., 1997. Organic matter in Great Salt Lake ooids (Utah, USA) - First approach to a formation via organic matrices.Facies, 36, 210-219.
[55] Reitner J., Peckmann J., Blumenberg M., Michaelis W., Reimer A., andThiel V., 2005. Concretionary methane-seep carbonates and associated microbial communities in Black Sea sediments.Palaeogeography, Palaeoclimatology, Palaeoecology, 227(1-3): 18-30.
[56] Richter D.K.,1983. Calcareous Ooids: A Synopsis. In: Peryt, T.M., (Ed.). Coated Grains. Berlin, Heidelberg: Springer, Berlin Heidelberg, pp. 71-99.
[57] Shi X.Y., Chen J.Q., andMei S.L., 1997. Cambrian sequence chronostratigraphic framework of the North China Platform.Earth Science Frontier, 4(3): 161-173 (in Chinese with English Abstract).
[58] Simone L.,1980. Ooids: A review.Earth-Science Reviews, 16: 319-355.
[59] Sorby H.C.,1879. The structure and origin of limestones.Proceeding of Geological Society of London, 35: 56-95.
[60] Sumner D.A., andGrotzinger J.P., 1993. Numerical modeling of ooid size and the problem of Neoproterozoic giant ooids.Journal of Sedimentary Petrology, 63: 974-982.
[61] Tan Q., Shi Z., Tian Y., Wang Y., andWang C., 2017. Origin of ooids in ooidal-muddy laminites: A case study of the Lower Cambrian Qingxudong Formation in the Sichuan Basin, South China.Geological Journal, 53(5): 1716-1727.
[62] Tang D., Shi X., Shi Q., Wu J., Song G., andJiang G.2015. Organomineralization in Mesoproterozoic giant ooids.Journal of Asian Earth Sciences, 107: 195-211.
[63] Thorie A., Mukhopadhyay A., Banerjee T., andMazumdar P., 2018. Giant ooids in a Neoproterozoic carbonate shelf, Simla Group, Lesser Himalaya, India: An analogue related to Neoproterozoic glacial deposits.Marine and Petroleum Geology, 98: 582-606.
[64] Tomás S., Homann M., Mutti M., Amour F., Christ N., Immenhauser A., Agar S., andKabiri L., 2013. Alternation of microbial mounds and ooid shoals (Middle Jurasssic, Morocco): Response to paleoenvironmental changes.Sedimentary Geology, 294: 68-82.
[65] Trower E.,2020. The enigma of Neoproterozoic giant ooids Fingerprints of extreme climate? Geophysical Research Letters, 47 (4): e2019GL086146. DOI: 10.1002/essoar.10501113.1.
[66] Trower E., andGrotzinger J., 2010. Sedimentology, diagenesis, and stratigraphic occurrence of giant ooids in the Ediacaran Rainstorm Member, Johnnie Formation, Death Valley region, California.Precambrian Research, 180(1-2): 113-124.
[67] Tucker M.E., andWright V.P., 1990. Carbonate Sedimentology. Blackwell Science, Oxford, pp. 1-482.
[68] Wang Y.H., Yang C.Y., andZhang X.L., 1983. Relationship between the changes of ooidal texture and the property and strength of diagenesis.Acta Sedimentologica Sinica, 1(2): 77-87 (in Chinese with English Abstract).
[69] Woods A.,2013. Microbial ooids and cortoids from the Lower Triassic (Spathian) Virgin Limestone, Nevada, USA: Evidence for an Early Triassic microbial bloom in shallow depositional environments.Global and Planetary Change, 105: 91-101.
[70] Xin H., Xiao E.Z., Qin Y.L., andZhang Z.W., 2019. Sedimentary characteristics of large columnar stromatolites in Fengshan Formation at the Xianrendong Section of Western Shandong Area.Journal of Northeast Petroleum University, 43(3): 1-11 (in Chinese with English Abstract).
[71] Xin H., Xiao E.Z., Wang L., Li Y.R., andZhang Z.W., 2020. Sedimentary succession of Cambrian microbial carbonates at Dengjiazhuang Section at Feicheng.Acata Sedimentologica Sinica, 38(1): 64-75 (in Chinese with English Abstract).
[72] Zhang W.H., Shi X.Y., Tang D.J., andWang X.Q., 2014. Mass-occurrence of oncoids in the Early-Middle Cambrian transition at western margin of North China Platform: A response of microbial community to shallow marine anoxia. Journal of Palaeogeography (Chinese Edition), 16(3): 305-318 (in Chinese with English Abstract).
[73] Zhao Z.,Wang Y.L., and Zang, G.C., 1984. The Ooides Artificially Synthesized under the Condition of Still Water, and the Sinian Suberathem Oolites, Jixian, Hebei Province. Science Press, Beijing: pp. 81-86.
[74] Zhou S.X.,1982. Origin and identification of carbonate ooids.Geology-Geochemistry, 1(2): 16-20 (in Chinese with English Abstract). |