[1] Tucker M E, Wright V P, Dickson J A D. Carbonate sedimentology[M]. Oxford: Blackwell Scientific Publications, 1990: 1-496.
[2] Siewers F D. Oolite and coated grains[M]//Middleton G V, Church M J, Coniglio M, et al. Encyclopedia of sediments and sedimentary rocks. Dordrecht: Springer, 2003: 502-506.
[3]

Wilkinson B H, Owen R M, Carroll A R. Submarine hydrothermal weathering, global eustasy, and carbonate polymorphism in Phanerozoic marine oolites[J]. Journal of Sedimentary Research, 1985, 55(2): 171-183.
[4]

Opdyke B N, Wilkinson B H. Paleolatitude distribution of Phanerozoic marine ooids and cements[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1990, 78(1/2): 135-148.
[5] 李飞, 易楚恒, 李红, 等. 微生物成因鲕粒研究进展[J]. 沉积学报, 2022, 40(2): 319-334.

Li Fei, Yi Chuheng, Li Hong, et al. Recent advances in ooid microbial origin: A review[J]. Acta Sedimentologica Sinica, 2022, 40(2): 319-334.
[6]

Diaz M R, Eberli G P. Decoding the mechanism of formation in marine ooids: A review[J]. Earth-Science Reviews, 2019, 190: 536-556.
[7]

Wilson P A, Roberts H H. Carbonate-periplatform sedimentation by density flows: A mechanism for rapid off-bank and vertical transport of shallow-water fines[J]. Geology, 1992, 20(8): 713-716.
[8]

Harris P M, Purkis S J, Ellis J, et al. Mapping bathymetry and depositional facies on Great Bahama Bank[J]. Sedimentology, 2015, 62(2): 566-589.
[9] National Data Buoy Center. Environmental conditions within specified geographical regions: Offshore east and west coasts of the United States and in the gulf of Mexico: Final report[M]. Washington: National Oceanic and Atmospheric Administration, 1973: 1-882.
[10]

Lees A. Possible influence of salinity and temperature on modern shelf carbonate sedimentation[J]. Marine Geology, 1975, 19(3): 159-198.
[11] 李飞, 武思琴, 刘柯. 鲕粒原生矿物识别及对海水化学成分变化的指示意义[J]. 沉积学报, 2015, 33(3): 500-511.

Li Fei, Wu Siqin, Liu Ke. Identification of ooid primary mineralogy: A clue for understanding the variation in paleo-oceanic chemistry[J]. Acta Sedimentologica Sinica, 2015, 33(3): 500-511.
[12] Medwedeff D A, Wilkinson B H. Cortical fabrics in calcite and aragonite ooids[M]//Peryt T M. Coated grains. Berlin: Springer, 1983: 109-115.
[13]

Diaz M R, Eberli G P, Blackwelder P, et al. Microbially mediated organomineralization in the formation of ooids[J]. Geology, 2017, 45(9): 771-774.
[14]

Ries J B. Review: Geological and experimental evidence for secular variation in seawater Mg/Ca (calcite-aragonite seas) and its effects on marine biological calcification[J]. Biogeosciences, 2010, 7(9): 2795-2849.
[15]

Li F, Webb G E, Algeo T J, et al. Modern carbonate ooids preserve ambient aqueous REE signatures[J]. Chemical Geology, 2019, 509: 163-177.
[16]

Lu C J, Li F, Oehlert A M, et al. Reconstructing paleoceanographic conditions during the Middle Ediacaran: Evidence from giant ooids in South China[J]. Precambrian Research, 2020, 351: 105945.
[17]

Robinson L F, Belshaw N S, Henderson G M. U and Th concentrations and isotope ratios in modern carbonates and waters from the Bahamas[J]. Geochimica et Cosmochimica Acta, 2004, 68(8): 1777-1789.
[18]

Steuber T, Buhl D. Calcium-isotope fractionation in selected modern and ancient marine carbonates[J]. Geochimica et Cosmochimica Acta, 2006, 70(22): 5507-5521.
[19]

Voegelin A R, Nägler T F, Samankassou E, et al. Molybdenum isotopic composition of modern and Carboniferous carbonates[J]. Chemical Geology, 2009, 265(3/4): 488-498.
[20]

Sandberg P A. An oscillating trend in Phanerozoic non-skeletal carbonate mineralogy[J]. Nature, 1983, 305(5929): 19-22.
[21] Rankey E C, Reeder S L. Tidal sands of the Bahamian archipelago[M]//Davis R A, Jr, Dalrymple R W. Principles of tidal sedimentology. Dordrecht: Springer, 2012: 537-565.
[22] Loreau J P, Purser B H. Distribution and ultrastructure of Holocene ooids in the Persian Gulf[M]//Purser B H. The Persian Gulf. Berlin, Heidelberg: Springer, 1973: 279-328.
[23] Logan B W, Davies G R, Read J F, et al. Carbonate sedimentation and environments, Shark Bay, western Australia[M]. Tulsa: American Association of Petroleum Geologists, 1970: 1-205.
[24]

Rankey E C, Reeder S L, Garza-Perez J R. Controls on links between geomorphical and surface sedimentological variability: Aitutaki and Maupiti atolls, South Pacific Ocean[J]. Journal of Sedimentary Research, 2011, 81(12): 885-900.
[25]

Rankey E C, Reeder S L. Holocene ooids of Aitutaki atoll, Cook Islands, South Pacific[J]. Geology, 2009, 37(11): 971-974.
[26]

Harris P M, Purkis S J, Ellis J. Analyzing spatial patterns in modern carbonate sand bodies from Great Bahama Bank[J]. Journal of Sedimentary Research, 2011, 81(3): 185-206.
[27]

Li F, Gong Q L, Burne R V, et al. Ooid factories operating under hothouse conditions in the Earliest Triassic of South China[J]. Global and Planetary Change, 2019, 172: 336-354.
[28] 李飞. 二叠纪—三叠纪之交鲕粒结构特征及时空分布对古海洋环境的指示[D]. 武汉: 中国地质大学, 2016: 1-106.

Li Fei. The spatial and temporal distributions of ooids and their petrological and geochemical compositions: Implications for paleoceanographic conditions in the Permian-Triassic transition[D]. Wuhan: China University of Geosciences, 2016: 1-106.
[29]

James N P. Facies models 7. Introduction to carbonate facies models[J]. Geoscience Canada, 1977, 4(3): 123-125.
[30] Wilson J L. Carbonate facies in geologic history[M]. New York: Springer, 1975: 1-471.
[31]

Schlager W. Benthic carbonate factories of the Phanerozoic[J]. International Journal of Earth Sciences, 2003, 92(4): 445-464.
[32] Schlager W. Sedimentation rates and growth potential of tropical, cool-water and mud-mound carbonate systems[M]//Insalaco E, Skelton P W, Palmer T J. Carbonate platform systems: Components and interactions. London: Geological Society, 2000: 217-227.
[33] Schlager W. Carbonate sedimentology and sequence stratigraphy[M]. Tulsa: SEPM, 2005: 1-208.
[34]

Reijmer J J G. Marine carbonate factories: Review and update[J]. Sedimentology, 2021, 68(5): 1729-1796.
[35] Pomar L. chapter 12- Carbonate systems[M]//Scarselli N, Adam J, Chiarella D, et al. Regional geology and tectonics. 2nd ed. Amsterdam: Elsevier, 2020: 235-311.
[36]

Pomar L, Hallock P. Carbonate factories: A conundrum in sedimentary geology[J]. Earth-Science Reviews, 2008, 87(3/4): 134-169.
[37]

Pomar L, Haq B U. Decoding depositional sequences in carbonate systems: Concepts vs experience[J]. Global and Planetary Change, 2016, 146: 190-225.
[38] James N P, Jones B. Origin of carbonate sedimentary rocks[M]. Chichester: John Wiley & Sons, Inc., 2015: 1-464.
[39] Tucker M E, Jones S J. Sedimentary petrology [M] 4th ed. Chichester: John Wiley & Sons, Inc., 2023: 1-448.
[40]

Moore C H, Wade W J. Chapter 2 - The application of the concepts of sequence stratigraphy to carbonate rock sequences[J]. Developments in Sedimentology, 2013, 67: 23-38.
[41]

Laugié M, Michel J, Pohl A, et al. Global distribution of modern shallow-water marine carbonate factories: A spatial model based on environmental parameters[J]. Scientific Reports, 2019, 9(1): 16432.
[42]

Michel J, Laugié M, Pohl A, et al. Marine carbonate factories: A global model of carbonate platform distribution[J]. International Journal of Earth Sciences, 2019, 108(6): 1773-1792.
[43]

Lomando A J. Structural influences on facies trends of carbonate inner ramp systems, examples from the Kuwait-Saudi Arabian Coast of the Arabian Gulf and Norhtern Yucatan, Mexico[J]. GeoArabia, 1999, 4(3): 339-360.
[44]

Rankey E C, Reeder S L. Holocene oolitic marine sand complexes of the Bahamas[J]. Journal of Sedimentary Research, 2011, 81(2): 97-117.
[45]

Newell N D, Purdy E G, Imbrie J. Bahamian oölitic sand[J]. The Journal of Geology, 1960, 68(5): 481-497.
[46]

Reeder S L, Rankey E C. Interactions between tidal flows and ooid shoals, northern Bahamas[J]. Journal of Sedimentary Research, 2008, 78(3): 175-186.
[47]

Rankey E C, Reeder S L. Controls on platform-scale patterns of surface sediments, shallow Holocene platforms, Bahamas[J]. Sedimentology, 2010, 57(6): 1545-1565.
[48] Harris P M. The Joulters ooid shoal, Great Bahama Bank[M]//Peryt T M. Coated grains. Berlin, Heidelberg: Springer, 1983: 132-141.
[49] Harris P M. Facies anatomy and diagenesis of a Bahamian ooid shoal[M]. Miami: University of Miami, 1979: 1-163.
[50]

Davies P J, Bubela B, Ferguson J. The formation of ooids[J]. Sedimentology, 1978, 25(5): 703-730.
[51]

Anderson N T, Cowan C A, Bergmann K D. A case for the growth of ancient ooids within the sediment pile[J]. Journal of Sedimentary Research, 2020, 90(8): 843-854.
[52] Cruz F E G. Processes, patterns and petrophysical heterogeneity of grainstone shoals at Ocean Cay, western Great Bahama Bank[D]. Miami: University of Miami, 2008: 1-245.
[53]

Cruz F E G, Eberli G P. Co-existence of skeletal and ooid shoals as a result of antecedent topography - Cat Cay shoal complex, Bahamas[J]. The Depositional Record, 2019, 5(3): 451-468.
[54] Purdy E G. Bahamian oölite shoals[M]//Peterson J A, Osmond J C. Geometry of sandstone bodies. Tulsa, OK: American Association of Petroleum Geologist, 1961: 53-62.
[55] Enos P. Bahamas[M]//Hopley D. Encyclopedia of modern coral reefs: Structure, form and process. Dordrecht: Springer, 2011: 85-93.
[56]

Purkis S J, Harris P M. The extent and patterns of sediment filling of accommodation space on Great Bahama Bank[J]. Journal of Sedimentary Research, 2016, 86(4): 294-310.
[57]

Dill R F, Shinn E A, Jones A T, et al. Giant subtidal stromatolites forming in normal salinity waters[J]. Nature, 1986, 324(6092): 55-58.
[58] Dill R F. Subtidal stromatolites, ooids and crusted-lime muds at the Great Bahama Bank margin[M]//Osborne R H. From shoreline to abyss: Contributions in marine geology in honor of Francis Parker Shepard. Tulsa, Oklahoma: SEPM Special Publications, 1991: 147-171.
[59]

Reid R P, Macintyre I G, Browne K M, et al. Modern marine stromatolites in the Exuma Cays, Bahamas: Uncommonly common[J]. Facies, 1995, 33(1): 1-17.
[60]

Purkis S J, Oehlert A M, Dobbelaere T, et al. Always a White Christmas in the Bahamas: Temperature and hydrodynamics localize winter mud production on Great Bahama Bank[J]. Journal of Sedimentary Research, 2023, 93(3): 145-160.
[61]

Feldmann M, McKenzie J A. Stromatolite-thrombolite associations in a modern environment, Lee Stocking Island, Bahamas[J]. Palaios, 1998, 13(2): 201-212.
[62] Reijmer J J G, Swart P K, Bauch T, et al. A re-evaluation of facies on Great Bahama Bank I: New facies maps of western Great Bahama Bank[M]//Swart P K, Eberli G P, McKenzie J A, et al. Perspectives in carbonate geology: A tribute to the career of Robert Nathan Ginsburg. Hoboken: Wiley-Blackwell, 2009: 29-46.
[63]

Purkis S J, Harris P, Cavalcante G. Controls of depositional facies patterns on a modern carbonate platform: Insight from hydrodynamic modeling[J]. The Depositional Record, 2019, 5(3): 421-437.
[64]

Harris P. Lessons from a modern carbonate sandbody: A personal experience of comparative sedimentology[J]. The Depositional Record, 2019, 5(3): 438-450.
[65]

Dravis J. Rapid and widespread generation of recent oolitic hardgrounds on a high energy Bahamian platform, Eleuthera Bank, Bahamas[J]. Journal of Sedimentary Research, 1979, 49(1): 195-207.
[66]

Budd D A, Land L S. Geochemical imprint of meteoric diagenesis in Holocene ooid sands, Schooner Cays, Bahamas; correlation of calcite cement geochemistry with extant groundwaters[J]. Journal of Sedimentary Research, 1990, 60(3): 361-378.
[67] Riegl B, Poiriez A, Janson X, et al. The Gulf: Facies belts, physical, chemical, and biological parameters of sedimentation on a carbonate ramp[M]//Westphal H, Riegl B, Eberli G P. Carbonate depositional systems: Assessing dimensions and controlling parameters: The Bahamas, Belize and the Persian/Arabian Gulf. Dordrecht: Springer, 2010: 145-213.
[68]

Gischler E, Lomando A J. Offshore sedimentary facies of a modern carbonate ramp, Kuwait, northwestern Arabian-Persian Gulf[J]. Facies, 2005, 50(3/4): 443-462.
[69]

Amao A O, Al-Ramadan K. Discussions on Arabian Gulf ooids[J]. Carbonates and Evaporites, 2018, 33(4): 683-695.
[70]

Lokier S W, Fiorini F. Temporal evolution of a carbonate coastal system, Abu Dhabi, United Arab Emirates[J]. Marine Geology, 2016, 381: 102-113.
[71] Kendall C G S C, Alsharhan A S. Holocene geomorphology and recent carbonate-evaporite sedimentation of the coastal region of Abu Dhabi, United Arab Emirates[M]//Kendall C G S C, Alsharhan A S, Jarvis I, et al. Quaternary carbonate and evaporite sedimentary facies and their ancient analogues: A tribute to Douglas James Shearman. Hoboken: IAS Special Publication, 2011: 45-88.
[72]

Alsharhan A S, Kendall C G S C. Holocene coastal carbonates and evaporites of the southern Arabian Gulf and their ancient analogues[J]. Earth-Science Reviews, 2003, 61(3/4): 191-243.
[73]

Picha F. Depositional and diagenetic history of Pleistocene and Holocene oolitic sediments and sabkhas in Kuwait, Persian Gulf[J]. Sedimentology, 1978, 25(3): 427-450.
[74]

Chafetz H S, McIntosh A G, Rush P F. Freshwater phreatic diagenesis in the marine realm of recent Arabian Gulf carbonates[J]. Journal of Sedimentary Research, 1988, 58(3): 433-440.
[75]

Given R K, Wilkinson B H. Kinetic control of morphology, composition, and mineralogy of abiotic sedimentary carbonates[J]. Journal of Sedimentary Research, 1985, 55(1): 109-119.
[76]

Rankey E C. Contrasts between wave- and tide-dominated oolitic systems: Holocene of Crooked-Acklins platform, southern Bahamas[J]. Facies, 2014, 60(2): 405-428.
[77]

Jiang L Q, Feely R A, Carter B R, et al. Climatological distribution of aragonite saturation state in the global oceans[J]. Global Biogeochemical Cycles, 2015, 29(10): 1656-1673.
[78]

Opdyke B N, Wilkinson B H. Carbonate mineral saturation state and cratonic limestone accumulation[J]. American Journal of Science, 1993, 293(3): 217-234.
[79] Westphal H, Riegl B, Eberli G P. Carbonate depositional systems: Assessing dimensions and controlling parameters: The Bahamas, Belize and the Persian/Arabian Gulf[M]. Dordrecht: Springer, 2010: 1-235.
[80]

Gallagher S J, Reuning L, Himmler T, et al. The enigma of rare Quaternary oolites in the Indian and Pacific Oceans: A result of global oceanographic physicochemical conditions or a sampling bias?[J]. Quaternary Science Reviews, 2018, 200: 114-122.
[81]

Purkis S J, Harris P. Quantitative interrogation of a fossilized carbonate sand body: The Pleistocene Miami oolite of South Florida[J]. Sedimentology, 2017, 64(5): 1439-1464.
[82]

Cantine M D, Knoll A H, Bergmann K D. Carbonates before skeletons: A database approach[J]. Earth-Science Reviews, 2020, 201: 103065.
[83]

Higgins J A, Fischer W W, Schrag D P. Oxygenation of the ocean and sediments: Consequences for the seafloor carbonate factory[J]. Earth and Planetary Science Letters, 2009, 284(1/2): 25-33.
[84]

Takahashi T, Sutherland S C, Chipman D W, et al. Climatological distributions of pH, pCO2, total CO2, alkalinity, and CaCO3 saturation in the global surface ocean, and temporal changes at selected locations[J]. Marine Chemistry, 2014, 164: 95-125.
[85]

Li F, Yan J X, Burne R V, et al. Paleo-seawater REE compositions and microbial signatures preserved in laminae of Lower Triassic ooids[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 486: 96-107.
[86] Bathurst R G C. Carbonate sediments and their diagenesis [M]. Amsterdam: Elsevier, 1972: 1-658.
[87] Bergman K L, Westphal H, Janson X, et al. Controlling parameters on facies geometries of the Bahamas, an isolated carbonate platform environment[M]//Westphal H, Riegl B, Eberli G P. Carbonate depositional systems: Assessing dimensions and controlling parameters: The Bahamas, Belize and the Persian/Arabian Gulf. Dordrecht: Springer, 2010: 5-80.
[88]

Lopez-Gamundi C, Dobbelaere T, Hanert E, et al. Simulating sedimentation on the Great Bahama Bank:Sources, sinks and storms[J]. Sedimentology, 2022, 69(7): 2693-2714.
[89] 李扬凡, 李飞. 前寒武—寒武纪重大转折期生物礁是如何演化的[J]. 地球科学, 2023, 34(04): 1301-1307.

Li Yangfan, Li Fei. How did reefs evolve during the Precambrian-Cambrian transition[J]. Journal of Earth Science, 2023, 34(04): 1301-1307.
[90]

Li H, Li F, Li X, et al. Development and collapse of the Early Cambrian shallow-water carbonate factories in the Hannan-Micangshan area, South China[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 2021, 583: 110665.
[91] 李雅兰, 李飞, 吕月健, 等. 陕南勉县寒武系仙女洞组生物礁岩相学及古环境分析[J]. 沉积学报, 2024,42(2)：608-618.

Li Yalan, Li Fei, Yuejian Lü, et al. Petrographic features and paleoenvironmental significance of the Lower Cambrian reef in the Xiannüdong Formation, Mian county, southern Shaanxi[J]. Acta Sedimentologica Sinica, 2024,42(2)：608-618.
[92]

Lebrec U, Lang S C, Paumard V, et al. Discovery of Holocene ooid shoals in a siliciclastic delta, De Grey River, north west shelf, Australia[J]. Geology, 2023, 51(4): 366-371.
[93]

Hallock P, Schlager W. Nutrient excess and the demise of coral reefs and carbonate platforms[J]. Palaios, 1986, 1(4): 389-398.
[94]

Dorgham M M, Moftah A. Environmental conditions and phytoplankton distribution in the Arabian Gulf and gulf of Oman, September 1986[J]. Journal of the Marine Biological Association of India, 1989, 31(1/2): 36-53.
[95]

Al-Thani J A, Soliman Y, Al-Maslamani I A, et al. Physical drivers of chlorophyll and nutrients variability in the southern-central Arabian Gulf[J]. Estuarine, Coastal and Shelf Science, 2023, 283: 108260.
[96]

Hallock P. The role of nutrient availability in bioerosion: Consequences to carbonate buildups[J]. Palaeogeography, Palaeoclimatology, Palaeoecology, 1988, 63(1/2/3): 275-291.
[97] Radtke G, Golubic S. Microbial euendolithic assemblages and microborings in intertidal and shallow marine habitats: Insight in cyanobacterial speciation[M]//Reitner J, Quéric N V, Arp G. Advances in stromatolite geobiology. Berlin, Heidelberg: Springer, 2011: 233-263.
[98] Witzke B J. Palaeoclimatic constraints for Palaeozoic palaeolatitudes of Laurentia and Euramerica[M]//McKerrow W S, Scotese C R. Palaeozoic palaeogeography and biogeography. London: The Geological Society, 1990: 57-73.
[99]

Li F, Yan J X, Chen Z Q, et al. Global oolite deposits across the Permian-Triassic boundary: A synthesis and implications for palaeoceanography immediately after the end-Permian biocrisis[J]. Earth-Science Reviews, 2015, 149: 163-180.
[100]

Tian L, Bottjer D J, Tong J N, et al. Distribution and size variation of ooids in the aftermath of the Permian-Triassic mass extinction[J]. Palaios, 2015, 30(9): 714-727.
[101]

Pomar L, Aurell M, Bádenas B, et al. Depositional model for a prograding oolitic wedge, Upper Jurassic, Iberian Basin[J]. Marine and Petroleum Geology, 2015, 67: 556-582.
[102]

Pierre A, Durlet C, Razin P, et al. Spatial and temporal distribution of ooids along a Jurassic carbonate ramp: Amellago outcrop transect, High-Atlas, Morocco[J]. Geological Society, London, Special Publications, 2010, 329(1): 65-88.
[103]

Prather B E, Goldstein R H, Kopaska-Merkel D C, et al. Dolomitization of reservoir rocks in the Smackover Formation, southeastern gulf coast, U.S.A[J]. Earth-Science Reviews, 2023, 244: 104512.
[104]

Burchette T P, Paul Wright V, Faulkner T J. Oolitic sandbody depositional models and geometries, Mississippian of southwest Britain: Implications for petroleum exploration in carbonate ramp settings[J]. Sedimentary Geology, 1990, 68(1/2): 87-115.
[105]

Elrick M, Read J F. Cyclic ramp-to-basin carbonate deposits, Lower Mississippian, Wyoming and Montana; A combined field and computer modeling study[J]. Journal of Sedimentary Research, 1991, 61(7): 1194-1224.
[106] 邢凤存, 陆永潮, 郭彤楼, 等. 碳酸盐岩台地边缘沉积结构差异及其油气勘探意义: 以川东北早三叠世飞仙关期台地边缘带为例[J]. 岩石学报, 2017, 33(4): 1305-1316.

Xing Fengcun, Lu Yongchao, Guo Tonglou, et al. Sedimentary texture diversity of different carbonate platform margins and it its significance for petroleum exploration: A case study of carbonate platform margins in Feixianguan period of the Early Triassic, NE Sichuan Basin, China[J]. Acta Petrologica Sinica, 2017, 33(4): 1305-1316.
[107]

Pomar L, Hallock P, Mateu-Vicens G, et al. Why do bio-carbonates exist?[J]. Journal of Marine Science and Engineering, 2022, 10(11): 1648.
[108]

Kump L R, Bralower T J, Ridgwell A. Ocean acidification in deep time[J]. Oceanography, 2009, 22(4): 94-107.
[109]

Trecalli A, Spangenberg J, Adatte T, et al. Carbonate platform evidence of ocean acidification at the onset of the early Toarcian oceanic anoxic event[J]. Earth and Planetary Science Letters, 2012, 357-358: 214-225.