{"refrec":{"BRefID":231599,"RR":"<b>Muchez, P.; Boulvain, F.; Dreesen, R.; Hou, H.F.</b> (1996). Sequence stratigraphy of the Frasnian-Famennian transitional strata: A comparison between south China and southern Belgium. <i>Palaeogeogr. Palaeoclimatol. Palaeoecol. 123(1-4)</i>: 289-296. <a href=\"http://dx.doi.org/10.1016/0031-0182(95)00122-0\" target=\"_blank\">dx.doi.org/10.1016/0031-0182(95)00122-0</a>","BEntID":223311,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":1,"RefStringPartII":". <i>Palaeogeogr. Palaeoclimatol. Palaeoecol. 123(1-4)</i>: 289-296. <a href=\"https://dx.doi.org/10.1016/0031-0182(95)00122-0\" target=\"_blank\">https://dx.doi.org/10.1016/0031-0182(95)00122-0</a>","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Muchez, P.; Boulvain, F.; Dreesen, R.; Hou, H.F.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Muchez, P. <i>et al.</i>","Englishabstract":"The sedimentological evolution of the Frasnian-Famennian transitional strata in South China and southern Belgium has been investigated. A similar trend in the deepening and shallowing of the sedimentation environment occurs in the two palaeogeographically distinct areas. The stratigraphic succession has been subdivided into depositional sequences. A general deepening occurs in the Palmatolepis rhenana conodont zone. During the most rapid rise in sea level, a transgressive systems tract formed. This transgressive systems tract is followed by a highstand systems tract in the late P. rhenana zone. A major sequence boundary within the latter zone is indicated by an unconformity in intraplatform and platform areas and by a conformity in the basinal area. The uppermost sediments within the late rhenana zone correspond to a lowstand systems tract. A rapid flooding took place near the base of the Palmatolepis linguiformis zone and dark shales and limestones formed. A second sequence boundary coincides with or is very close to the Frasnian-Famennian boundary (base P. triangularis zone). The global extinction event at the Frasnian-Famennian boundary coincides with an important eustatic fall in sea level. 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