Abstract
Alternations of thin-bedded limestone and shale, or ribbon rock, commonly occur throughout lower Palaeozoic carbonate successions; however, their formative processes are still unclear. In this study, we discuss the origin of the ribbon rocks of the upper Cambrian Hwajeol Formation, Korea, based on detailed microfacies analysis of a ~ 2-m-thick interval. Five sedimentary microfacies were identified: normally graded calcarenite to shale; parallel-laminated shale; lime mudstone; wackestone-to-packstone; and bioclastic–intraclastic packstone-to-conglomerate. Shale facies were most likely formed by frequent storm-induced bottom currents, whereas, lime mudstone facies were deposited in situ by suspension settling of micrite, mudflows, or growth of keratose sponges on the seafloor, and/or formed by early diagenetic growth. Conglomerate/packstone/wackestone indicate infrequent, larger-scale events, e.g., mega-storms, tsunamis, or earthquakes. We propose a new formative model for tempestite-type ribbon rock based on the Hwajeol example, and suggest that this model can be differentiated from the other types of ribbon rocks—tidalite, turbidite, and diagenetic types. Formation of the tempestite-type ribbon rocks would have been promoted by the characteristic environmental conditions of the early Palaeozoic, in particular sea-water chemistry that promoted calcite precipitation and the paucity of burrowers. Detailed microscopic observations can thus provide clues to elucidate previously unknown sedimentary processes in the deeper parts of carbonate platforms.
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References
Adams RD, Grotzinger J (1996) Lateral continuity of facies and parasequences in middle Cambrian platform carbonates, Carrara Formation, southeastern California, U.S.A. J Sediment Res 66:1079–1090. https://doi.org/10.1306/D42684AF-2B26-11D7-8648000102C1865D
Aigner T (1982) Calcareous tempestites: storm-dominated stratification in upper Muschelkalk limestones (middle Trias, SW Germany). In: Einsele G, Seilacher A (eds) Cyclic event and stratification. Springer-Verlag, Berlin, pp 180–198
Álvaro JJ, Vennin E (1997) Episodic development of Cambrian eocrinoid-sponge meadows in the Iberian Chains (NE Spain). Facies 37:49–64. https://doi.org/10.1007/BF02537370
Amberg CE, Collart T, Salenbien W, Egger LM, Munnecke A, Nielsen AT, Monnet C, Hammer O, Vandenbroucke TR (2016) The nature of Ordovician limestone-marl alternations in the Oslo-Asker district (Norway): witnesses of primary glacio-eustasy or diagenetic rhythms? Sci Rep 6:18787. https://doi.org/10.1038/srep18787
Aplin AC, Macquaker JHS (2011) Mudstone diversity: origin and implications for source, seal, and reservoir properties in petroleum systems. AAPG Bull 95:2031–2059. https://doi.org/10.1306/03281110162
Aplin AC, Matenaar IF, McCarty DK, van der Pluijm BA (2006) Influence of mechanical compaction and clay mineral diagenesis on the microfabric and pore-scale properties of deep-water Gulf of Mexico mudstones. Clays Clay Miner 54:500–514. https://doi.org/10.1346/CCMN.2006.0540411
Arzani N (2006) Primary versus diagenetic bedding in the limestone-marl/shale alternations of the epeiric seas, an example from the lower Lias (early Jurassic) of SW Britain. Carbonates Evaporites 21:94–109. https://doi.org/10.1007/BF03175469
Bayet-Goll A, Chen J, Moussavi-Harami R, Mahboubi A (2015) Depositional processes of ribbon carbonates in middle Cambrian of Iran (Deh-Sufiyan Formation, central Alborz). Facies 61:9. https://doi.org/10.1007/s10347-015-0436-6
Belka Z, Skompski S, Sobon-Podgorska J (1996) Reconstruction of a lost carbonate platform on the shelf of Fennosarmatia: evidence from Viséan polymictic debrites, Holy Cross Mountains, Poland. In: Strogen P, Somerville ID, Jones GL (eds) Recent advances in lower Carboniferous geology. Geological Society of London special publications, vol 107. Geological Society of London, London, pp 315–329. https://doi.org/10.1144/GSL.SP.1996.107.01.22
Bottjer DJ, Hagadorn JW, Dornbos SQ (2000) The Cambrian substrate revolution. GSA Today 10:1–7
Bova JA, Read JF (1987) Incipiently drowned facies within a cyclic peritidal ramp sequence, Early Ordovician Chepultepec interval, Virginia Appalachians. Geol Soc Am Bull 98:714–727. https://doi.org/10.1130/0016-7606(1987)98%3c714:IDFWAC%3e2.0.CO;2
Buatois LA, Mangano MG, Olea RA, Wilson MA (2016) Decoupled evolution of soft and hard substrate communities during the Cambrian explosion and Great Ordovician Biodiversification Event. Proc Natl Acad Sci 113:6945–6948. https://doi.org/10.1073/pnas.1523087113
Byun UH, Kwon YK (2020) Depositional origin of subtidal meter-scale cyclic successions in the Cambrian Hwajeol Formation. Geosci J 24:1–16. https://doi.org/10.1007/s12303-018-0085-1
Chen J, Chough SK, Chun SS, Han Z (2009) Limestone pseudoconglomerates in the Late Cambrian Gushan and Chaomidian Formations (Shandong Province, China): soft-sediment deformation induced by storm-wave loading. Sedimentology 56:1174–1195. https://doi.org/10.1111/j.1365-3091.2008.01028.x
Chen J, Han Z, Zhang X, Fan A, Yang R (2010) Early diagenetic deformation structures of the Furongian ribbon rocks in Shandong Province of China—a new perspective of the genesis of limestone conglomerates. Sci China Earth Sci 53:241–252. https://doi.org/10.1007/s11430-010-0010-6
Chen J, Chough SK, Han Z, Lee J-H (2011) An extensive erosion surface of a strongly deformed limestone bed in the Gushan and Chaomidian Formations (late middle Cambrian to Furongian), Shandong Province, China: sequence–stratigraphic implications. Sediment Geol 233:129–149. https://doi.org/10.1016/j.sedgeo.2010.11.002
Cheong CH (1969) Stratigraphy and paleontology of the Samcheog Coalfield, Gangweondo, Korea (I). J Geol Soc Korea 5:13–56
Choi DK, Chough SK, Kwon YK, Lee SB, Woo J, Kang I, Lee HS, Lee SM, Sohn JW, Shinn YJ, Lee DJ (2004) Taebaek Group (Cambrian-Ordovician) in the Seokgaejae section, Taebaeksan Basin: a refined lower Paleozoic stratigraphy in Korea. Geosci J 8:125–151. https://doi.org/10.1007/BF02910190
Chough SK (2013) Geology and sedimentology of Korean Peninsula. Elsevier insights. Elsevier. https://doi.org/10.1016/C2012-0-02847-5
Chow N, James NP (1987) Cambrian grand cycles: a northern Appalachian perspective. Geol Soc Am Bull 98:418–429. https://doi.org/10.1130/0016-7606(1987)98%3c418:CGCANA%3e2.0.CO;2
Chow N, James NP (1992) Synsedimentary diagenesis of Cambrian peritidal carbonates: evidence from hardgrounds and surface paleokarst in the Port au Port Group, western Newfoundland. Bull Can Pet Geol 40:115–127. https://doi.org/10.35767/gscpgbull.40.2.115
Coniglio M, James NP (1990) Origin of fine-grained carbonate and siliciclastic sediments in an early Palaeozoic slope sequence, Cow Head Group, western Newfoundland. Sedimentology 37:215–230. https://doi.org/10.1111/j.1365-3091.1990.tb00956.x
Cook HE, Taylor ME (1977) Comparison of continental slope and shelf environments in the upper Cambrian and lowest Ordovician of Nevada. In: Cook HE, Enas P (eds) Deep-water carbonate environments. SEPM special publication, vol 25. SEPM, Tulsa, pp 51–81
Cowan CA, James NP (1992) Diastasis cracks: mechanically generated synaeresis-like cracks in upper Cambrian shallow water oolite and ribbon carbonates. Sedimentology 39:1101–1118. https://doi.org/10.1111/j.1365-3091.1992.tb01999.x
Cowan CA, James NP (1993) The interactions of sea-level change, terrigenous-sediment influx, and carbonate productivity as controls on upper Cambrian grand cycles of western Newfoundland, Canada. Geol Soc Am Bull 105:1576–1590. https://doi.org/10.1130/0016-7606(1993)105%3c1576:tioslc%3e2.3.co;2
Demicco RV (1983) Wavy and lenticular-bedded carbonate ribbon rocks of the upper Cambrian Conococheague Limestone, central Appalachians. J Sediment Petrol 53:1121–1132. https://doi.org/10.1306/212F8328-2B24-11D7-8648000102C1865D
Demicco RV, Hardie LA (1994) Sedimentary structures and early diagenetic features of shallow marine carbonates. SEPM atlas series, vol 1. SEPM, Tulsa
Droser ML, Bottjer DJ (1988) Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States. Geology 16:233–236. https://doi.org/10.1130/0091-7613(1988)016%3c0233:TIDAEO%3e2.3.CO;2
Droser ML, Li X (2001) The Cambrian radiation and the diversification of sedimentary fabrics. In: Zhuravlev AY, Riding R (eds) Ecology of the Cambrian radiation. Columbia University Press, New York, pp 137–169
Egenhoff SO, Fishman NS (2013) Traces in the dark—sedimentary processes and facies gradients in the upper shale member of the upper Devonian-lower Mississippian Bakken Formation, Williston Basin, North Dakota, U.S.A. J Sediment Res 83:803–824. https://doi.org/10.2110/jsr.2013.60
Eichenseer K, Balthasar U, Smart CW, Stander J, Haaga KA, Kiessling W (2019) Jurassic shift from abiotic to biotic control on marine ecological success. Nat Geosci 12:638–642. https://doi.org/10.1038/s41561-019-0392-9
Einsele G (1998) Event stratigraphy: recognition and interpretation of sedimentary event horizons. In: Doyle P, Bennett MR (eds) Unlocking the stratigraphical record: advances in modern stratigraphy. Wiley, New York, pp 145–193
Elrick M, Snider AC (2002) Deep-water stratigraphic cyclicity and carbonate mud mound development in the middle Cambrian Marjum Formation, House Range, Utah, USA. Sedimentology 49:1021–1047. https://doi.org/10.1046/j.1365-3091.2002.00488.x
Elrick M, Rieboldt S, Saltzman M, McKay RM (2011) Oxygen-isotope trends and seawater temperature changes across the late Cambrian Steptoean positive carbon-isotope excursion (SPICE event). Geology 39:987–990. https://doi.org/10.1130/g32109.1
Flügel E (2004) Microfacies of carbonate rocks: analysis, interpretation and application. Springer, Berlin
Glumac B, Walker KR (1997) Selective dolomitization of Cambrian microbial carbonate deposits: a key to mechanisms and environments of origin. Palaios 12:98–110. https://doi.org/10.2307/3515300
Glumac B, Walker KR (2000) Carbonate deposition and sequence stratigraphy of the terminal Cambrian grand cycle in the southern Appalachians, U.S.A. J Sediment Res 70:952–963. https://doi.org/10.1306/2dc40943-0e47-11d7-8643000102c1865d
Goldberg SL, Present TM, Finnegan S, Bergmann KD (2021) A high-resolution record of early Paleozoic climate. Proc Natl Acad Sci 118:e2013083118. https://doi.org/10.1073/pnas.2013083118
Hallam A (1986) Origin of minor limestone-shale cycles: climatically induced or diagenetic? Geology 14:609–612
Hips K (1998) Lower Triassic storm-dominated ramp sequence in northern Hungary: an example of evolution from homoclinal through distally steepened ramp to middle Triassic flat-topped platform. In: Wright VP, Burchette TP (eds) Carbonate ramps. Geological Society of London special publications, vol 149. Geological Society of London, London, pp 315–338. https://doi.org/10.1144/GSL.SP.1999.149.01.15
Jeong H, Lee YI (2000) Late Cambrian biogeography: conodont bioprovinces from Korea. Palaeogeogr Palaeoclimatol Palaeoecol 162:119–136. https://doi.org/10.1016/S0031-0182(00)00108-5
Kennedy WJ, Garrison RE (1975) Morphology and genesis of nodular chalks and hardgrounds in the upper Cretaceous of southern England. Sedimentology 22:311–386. https://doi.org/10.1111/j.1365-3091.1975.tb01637.x
Kershaw S, Li Q, Li Y (2021) Addressing a Phanerozoic carbonate facies conundrum—sponges or clotted micrite? Evidence from early Silurian reefs, south China Block. Sediment Rec 19:3–10. https://doi.org/10.2110/sedred.2021.1.03
Kim JC, Lee YI (1995) Flat-pebble conglomerate: a characteristic lithology of upper Cambrian and lower Ordovician shallow-water carbonate sequence. In: Cooper JD, Droser ML, Finney SC (eds) Ordovician Odyssey. Special publication, vol 77. SEPM Pacific Section, Fullerton, pp 371–374
Kim JC, Lee YI (1996) Marine diagenesis of lower Ordovician carbonate sediments (Dumugol Formation), Korea: cementation in a calcite sea. Sediment Geol 105:241–257. https://doi.org/10.1016/0037-0738(95)00141-7
Kobayashi T (1966) The Cambro-Ordovician formations and faunas of south Korea, part X, Stratigraphy of the Chosen Group in Korean and South Manchuria and its relation to the Cambro-Ordovician formations of other areas, section A. The Chosen Group of South Korea. J. Fac. Sci., Univ. Tokyo, Sect. II 16:1–84
Kreisa RD (1981) Storm-generated sedimentary structures in subtidal marine facies with examples from the middle and upper Ordovician of southwestern Virginia. J Sediment Petrol 51:823–848. https://doi.org/10.1306/212F7DBF-2B24-11D7-8648000102C1865D
Kwon YK, Chough SK (2005) Sequence stratigraphy of the cyclic successions in the Dumugol Formation (lower Ordovician), mideast Korea. Geosci J 9:305–324. https://doi.org/10.1007/BF02910319
Kwon YK, Chough SK, Choi DK, Lee DJ (2002) Origin of limestone conglomerates in the Choson Supergroup (Cambro-Ordovician), mid-east Korea. Sediment Geol 146:265–283. https://doi.org/10.1016/s0037-0738(01)00128-2
Kwon YK, Chough SK, Choi DK, Lee DJ (2006) Sequence stratigraphy of the Taebaek Group (Cambrian-Ordovician), mideast Korea. Sediment Geol 192:19–55. https://doi.org/10.1016/j.sedgeo.2006.03.024
Łabaj MA, Pratt BR (2016) Depositional dynamics in a mixed carbonate–siliciclastic system: middle-upper Cambrian Abrigo Formation, Southeastern Arizona, U.S.A. J Sediment Res 86:11–37. https://doi.org/10.2110/jsr.2015.96
Lash GG, Blood D (2004) Geochemical and textural evidence for early (shallow) diagenetic growth of stratigraphically confined carbonate concretions, upper Devonian Rhinestreet black shale, western New York. Chem Geol 206:407–424. https://doi.org/10.1016/j.chemgeo.2003.12.017
Lazar OR, Bohacs KM, Macquaker JHS, Schieber J, Demko TM (2015) Capturing key attributes of fine-grained sedimentary rocks in outcrops, cores, and thin sections: nomenclature and description guidelines. J Sediment Res 85:230–246. https://doi.org/10.2110/jsr.2015.11
Lee B-S (2014) Conodonts from the Sesong Slate and Hwajeol Formation (Guzhangian to Furongian) in the Taebaeksan Basin, Korea. Acta Geol Sin 88:35–45. https://doi.org/10.1111/1755-6724.12181
Lee J-H, Riding R (2018) Marine oxygenation, lithistid sponges, and the early history of Paleozoic skeletal reefs. Earth Sci Rev 181:98–121. https://doi.org/10.1016/j.earscirev.2018.04.003
Lee J-H, Riding R (2021) Keratolite–stromatolite consortia mimic domical and branched columnar stromatolites. Palaeogeogr Palaeoclimatol Palaeoecol 571:110288. https://doi.org/10.1016/j.palaeo.2021.110288
Lee B-S, Seo K-S (2008) Conodonts from the Hwajeol Formation (upper Cambrian) in the Seokgaejae area, southeast margin of the Taebaeksan Basin. Geosci J 12:233–242. https://doi.org/10.1007/s12303-008-0024-7
Lee J-H, Chen J, Woo J (2015) The earliest Phanerozoic carbonate hardground (Cambrian stage 5, series 3): Implications to the paleoseawater chemistry and early adaptation of hardground fauna. Palaeogeogr Palaeoclimatol Palaeoecol 440:172–179. https://doi.org/10.1016/j.palaeo.2015.07.043
Lee J-H, Hong J, Woo J, Oh J-R, Lee D-J, Choh S-J (2016a) Reefs in the early Paleozoic Taebaek Group, Korea: a review. Acta Geol Sin 90:352–367. https://doi.org/10.1111/1755-6724.12659
Lee J-H, Kim B-J, Liang K, Park T-Y, Choh S-J, Lee D-J, Woo J (2016b) Cambrian reefs in the western north China platform, Wuhai, inner Mongolia. Acta Geol Sin 90:1946–1954. https://doi.org/10.1111/1755-6724.1301410.1111/1755-6724.13014
Lee J-H, Choh S-J, Lee D-J (2018) Late Cambrian missing link in macroborer evolution preserved in intraclasts. Palaeogeogr Palaeoclimatol Palaeoecol 489:137–146. https://doi.org/10.1016/j.palaeo.2017.10.005
Liu J (2009) Marine sedimentary response to the Great Ordovician Biodiversification Event: examples from north China and south China. Paleontol Res 13:9–21. https://doi.org/10.2517/1342-8144-13.1.009
Luo C, Reitner J (2014) First report of fossil “keratose” demosponges in Phanerozoic carbonates: preservation and 3-D reconstruction. Naturwissenschaften 101:467–477. https://doi.org/10.1007/s00114-014-1176-0
Markello JR, Read JF (1981) Carbonate ramp-to-deeper shale shelf transitions of an upper Cambrian intrashelf basin, Nolichucky Formation, southwest Virginia Appalachians. Sedimentology 28:573–597. https://doi.org/10.1111/j.1365-3091.1981.tb01702.x
Markello JR, Read JF (1982) Upper Cambrian intrashelf basin, Nolichucky Formation, southwest Virginia Appalachians. AAPG Bull 66:860–878
McKenzie NR, Hughes NC, Myrow PM, Choi DK, Park T-y (2011) Trilobites and zircons link north China with the eastern Himalaya during the Cambrian. Geology 39:591–594. https://doi.org/10.1130/g31838.1
Meng X, Ge M, Tucker ME (1997) Sequence stratigraphy, sea-level changes and depositional systems in the Cambro-Ordovician of the north China carbonate platform. Sediment Geol 114:189–222. https://doi.org/10.1016/s0037-0738(97)00073-0
Möller NK, Kvingan K (1988) The genesis of nodular limestones in the Ordovician and Silurian of the Oslo region (Norway). Sedimentology 35:405–420. https://doi.org/10.1111/j.1365-3091.1988.tb00994.x
Morse JW, Gledhill DK, Millero FJ (2003) CaCO3 precipitation kinetics in waters from the great Bahama bank: implications for the relationship between bank hydrochemistry and whitings. Geochim Cosmochim Acta 67:2819–2826. https://doi.org/10.1016/s0016-7037(03)00103-0
Moshier SO (1986) Carbonate platform sedimentology, upper Cambrian Richland Formation, Lebanon Valley, Pennsylvania. J Sediment Petrol 56:204–216
Munnecke A, Samtleben C (1996) The formation of micritic limestones and the development of limestone-marl alternations in the Silurian of Gotland, Sweden. Facies 34:159–176. https://doi.org/10.1007/BF02546162
Myrow PM, Tice L, Archuleta B, Clark B, Taylor JF, Ripperdan RL (2004) Flat-pebble conglomerate: its multiple origins and relationship to metre-scale depositional cycles. Sedimentology 51:973–996. https://doi.org/10.1111/j.1365-3091.2004.00657.x
Myrow PM, Chen J, Snyder Z, Leslie S, Fike D, Fanning M, Yuan J, Tang P (2015) Depositional history, tectonics, and provenance of the Cambrian-Ordovician succession in the western margin of the north China Block. Geol Soc Am Bull 127:1174–1193. https://doi.org/10.1130/B31228.1
Nohl T, Munnecke A (2019) Reconstructing time and diagenesis of limestone-marl alternations from the selective compaction of colonies of the tabulate coral Halysites. Bull Geosci 94:279–298. https://doi.org/10.3140/bull.geosci.1752
Nohl T, Jarochowska E, Munnecke A (2019) Revealing the genesis of limestone-marl alternations: a taphonomic approach. Palaios 34:15–31. https://doi.org/10.2110/palo.2018.062
O’Brien NR (1990) Significance of lamination in Toarcian (lower Jurassic) shales from Yorkshire, Great Britain. Sediment Geol 67:25–34. https://doi.org/10.1016/0037-0738(90)90025-O
O’Brien NR (1996) Shale lamination and sedimentary processes. In: Kemp AES (ed) Paleoclimatology and paleoceanography from laminated sediments. Geological Society of London special publications, vol 116. Geological Society of London, London, pp 23–36. https://doi.org/10.1144/GSL.SP.1996.116.01.04
Park J, Lee J-H, Hong J, Choh S-J, Lee D-C, Lee D-J (2015) An upper Ordovician sponge-bearing micritic limestone and implication for early Palaeozoic carbonate successions. Sediment Geol 319:124–133. https://doi.org/10.1016/j.sedgeo.2015.02.002
Pfeil RW, Read JF (1980) Cambrian carbonate platform margin facies, Shady Dolomite, southwestern Virginia, U.S.A. J Sediment Petrol 50:91–116. https://doi.org/10.1306/212F7978-2B24-11D7-8648000102C1865D
Pohler SML, James NP (1989) Reconstruction of a lower/middle Ordovician carbonate shelfmargin: Cow Head Group, Western Newfoundland. Facies 21:189–262. https://doi.org/10.1007/BF02536836
Pratt BR, Bordonaro OL (2007) Tsunamis in a stormy sea: middle Cambrian inner-shelf limestones of western Argentina. J Sediment Res 77:256–262. https://doi.org/10.2110/jsr.2007.032
Pratt BR, James NP (1986) The St George Group (Lower Ordovician) of western Newfoundland: tidal flat island model for carbonate sedimentation in shallow epeiric seas. Sedimentology 33:313–343. https://doi.org/10.1111/j.1365-3091.1986.tb00540.x
Rankey EC, Walker KR, Srinivasan K (1994) Gradual establishment of Iapetan “passive” margin sedimentation: Stratigraphic consequences of Cambrian episodic tectonism and eustasy, southern Appalachians. J Sediment Res B64:298–310. https://doi.org/10.1306/D4267FB4-2B26-11D7-8648000102C1865D
Reid RP, Macintyre IG, James NP (1990) Internal precipitation of microcrystalline carbonate: a fundamental problem for sedimentologists. Sediment Geol 68:163–170. https://doi.org/10.1016/0037-0738(90)90109-7
Reineck HE, Singh IB (1972) Genesis of laminated sand and graded rhythmites in storm-sand layers of shelf mud. Sedimentology 18:123–128. https://doi.org/10.1111/j.1365-3091.1972.tb00007.x
Reinhardt J, Hardie LA (1976) Selected examples of carbonate sedimentation, lower Paleozoic of Maryland. Maryland geological survey guidebook, vol 5. Maryland geological survey
Reitner J (1993) Modern cryptic microbialite/metazoan facies from Lizard Island (Great Barrier Reef, Australia) formation and concepts. Facies 29:3–40. https://doi.org/10.1007/BF02536915
Sami T, Desrochers A (1992) Episodic sedimentation on an early Silurian, storm-dominated carbonate ramp, Becscie and Merrimack Formations, Anticosti Island, Canada. Sedimentology 39:355–381. https://doi.org/10.1111/j.1365-3091.1992.tb02122.x
Sawyer DE, Flemings PB, Buttles J, Mohrig D (2012) Mudflow transport behavior and deposit morphology: role of shear stress to yield strength ratio in subaqueous experiments. Mar Geol 307–310:28–39. https://doi.org/10.1016/j.margeo.2012.01.009
Schieber J, Yawar Z (2009) A new twist on mud deposition—mud ripples in experiment and rock record. Sediment Rec 7:4–8. https://doi.org/10.2110/sedred.2009.2
Sepkoski JJ Jr (1982) Flat pebble conglomerates, storm deposits, and the Cambrian bottom fauna. In: Einsele G, Seilacher A (eds) Cyclic event and stratification. Springer-Verlag, Berlin, pp 371–388
Sepkoski JJ Jr, Bambach RK, Droser ML (1991) Secular changes in Phanerozoic event bedding and the biological overprint. In: Einsele G, Richen W, Seilacher A (eds) Cycles and events in stratigraphy. Springer, Berlin, pp 298–312
Shanmugam G, Benedict GL (1978) Fine-grained carbonate debris flow, Ordovician basin margin, southern Appalachians. J Sediment Petrol 48:1233–1240. https://doi.org/10.1306/212F7644-2B24-11D7-8648000102C1865D
Shinn EA, Steinen RP, Lidz BH, Swart PK (1989) Whitings, a sedimentologic dilemma. J Sediment Petrol 59:147–161. https://doi.org/10.1306/212F8F3A-2B24-11D7-8648000102C1865D
Sohn JW, Choi DK (2005) Revision of the upper Cambrian trilobite biostratigraphy of the Sesong and Hwajeol formations, Taebaek Group, Korea. J Paleontol Soc Korea 21:195–200
Sohn JW, Choi DK (2007) Furongian trilobites from the Asioptychaspis and Quadraticephalus zones of the Hwajeol Formation, Taebaeksan Basin, Korea. Geosci J 11:297–314. https://doi.org/10.1007/BF02857047
Southard JB, Boguchwal LA (1990) Bed configurations in steady unidirectional water flows. Part 2. Synthesis of flume data. J Sediment Petrol 60:658–679. https://doi.org/10.1306/212F9241-2B24-11D7-8648000102C1865D
Srinivasan K, Walker KR (1993) Sequence stratigraphy of an intrashelf basin carbonate ramp to rimmed platform transition: Maryville Limestone (middle Cambrian), southern Appalachians. Geol Soc Am Bull 105:883–896. https://doi.org/10.1130/0016-7606(1993)105%3c0883:ssoaib%3e2.3.co;2
Trabucho-Alexandre J, Dirkx R, Veld H, Klaver G, de Boer PL (2012) Toarcian black shales in the Dutch Central Graben: record of energetic, variable depositional conditions during an oceanic anoxic event. J Sediment Res 82:104–120. https://doi.org/10.2110/jsr.2012.5
Trotter JA, Williams IS, Barnes CR, Lecuyer C, Nicoll RS (2008) Did cooling oceans trigger Ordovician biodiversification? Evidence from conodont thermometry. Science 321:550–554. https://doi.org/10.1126/science.1155814
Warnke K (1995) Calcification processes of siliceous sponges in Viséan Limestones (Counties Sligo and Leitrim, northwestern Ireland). Facies 33:215–228. https://doi.org/10.1007/BF02537453
Westphal H (2006) Limestone–marl alternations as environmental archives and the role of early diagenesis: a critical review. Int J Earth Sci 95:947–961. https://doi.org/10.1007/s00531-006-0084-8
Westphal H, Head MJ, Munnecke A (2000) Differential diagenesis of rhythmic limestone alternations supported by palynological evidence. J Sediment Res 70:715–725. https://doi.org/10.1306/2DC40932-0E47-11D7-8643000102C1865D
Westphal H, Munnecke A, Böhm F, Bornholdt S (2008) Limestone-marl alternations in epeiric sea settings—witnesses of environmental changes, or of rhythmic diagenesis? In: Holmden C, Pratt BR (eds) Dynamics of epeiric seas. Geological Association of Canada special paper, vol 48. Geological Association of Canada, pp 389–406
White WS (1943) Occurrence of manganese in eastern Aroostook County, Maine. Geological survey bulletin, vol 940-E. US Government Printing Office, Washington, D.C.
Wilson MA, Palmer TJ, Guensburg TE, Finton CD, Kaufman LE (1992) The development of an early Ordovician hardground community in response to rapid sea-floor calcite precipitation. Lethaia 25:19–34. https://doi.org/10.1111/j.1502-3931.1992.tb01789.x
Wright VP, Cherns L (2016a) How far did feedback between biodiversity and early diagenesis affect the nature of early Palaeozoic sea floors? Palaeontology 59:753–765. https://doi.org/10.1111/pala.12258
Wright VP, Cherns L (2016b) Leaving no stone unturned: the feedback between increased biotic diversity and early diagenesis during the Ordovician. J Geol Soc 173:241–244. https://doi.org/10.1144/jgs2015-043
Zhang Y, Chen D, Zhou X, Guo Z, Wei W, Mutti M (2015) Depositional facies and stratal cyclicity of dolomites in the lower Qiulitag Group (upper Cambrian) in northwestern Tarim Basin, NW China. Facies 61:417. https://doi.org/10.1007/s10347-014-0417-1
Zhou Z-C, Willems H, Li Y, Luo H (2011) A well-preserved carbonate tempestite sequence from the Cambrian Gushan Formation, eastern North China Craton. Palaeoworld 20:1–7. https://doi.org/10.1016/j.palwor.2010.12.001
Zhuravlev AY, Wood RA (2008) Eve of biomineralization: controls on skeletal mineralogy. Geology 36:923–926. https://doi.org/10.1130/g25094a.1
Acknowledgements
This study was supported by grants from the National Research Foundation of Korea to JHL (2019R1A2C4069278) and SJC (2018R1A2A2A05018469). We thank S.-W. Kwon for help with fieldwork and preparation of thin sections and sedimentary logs, and A. Munnecke, J. Wheeley and T. Nohl for their constructive comments. This study is a contribution to IGCP Project 735 “Rocks and the Rise of Ordovician Life: Filling knowledge gaps in the Early Palaeozoic Biodiversification”.
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Lee, JH., Cho, S.H., Jung, D.Y. et al. Ribbon rocks revisited: the upper Cambrian (Furongian) Hwajeol Formation, Taebaek Group, Korea. Facies 67, 19 (2021). https://doi.org/10.1007/s10347-021-00630-3
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DOI: https://doi.org/10.1007/s10347-021-00630-3