{"refrec":{"BRefID":231497,"RR":"<b>Hubert, B.L.M.; Zapalski, M.K.; Zapalski, M.K.; Nicollin, J.-P.; Mistiaen, B.; Brice, D.</b> (2007). Selected benthic faunas from the Devonian of the Ardennes: an estimation of palaeobiodiversity. <i>Acta Geol. Pol. 57(2)</i>: 223-262","BEntID":223209,"PublicFlag":1,"CheckedFlag":1,"wosflag":1,"vabbflag":0,"RefStringPartII":". <i>Acta Geol. Pol. 57(2)</i>: 223-262","DocTypID":8,"DocType":"Journal article","MarineFlag":1,"FreshFlag":0,"BrackishFlag":0,"TerrestrialFlag":0,"Authorstring":"Hubert, B.L.M.; Zapalski, M.K.; Zapalski, M.K.; Nicollin, J.-P.; Mistiaen, B.; Brice, D.","OrigTitleTranslFlag":0,"Authorstringtrunc":"Hubert, B.L.M. <i>et al.</i>","Englishabstract":"A survey of the principal benthic faunas from the Devonian of the Ardennes is presented. The alpha-diversity is very high ( 707 species, including 138 species of stromatoporoids, 113 species of tabulates, hydroids and chaetetids, and 456 species of brachiopods). Analysis of their distribution through time indicates two brachiopod diversity peaks ( Emsian/Eifelian and Frasnian), a single stromatoporoid diversity peak ( Givetian), and no clear peak of tabulate corals ( with the highest diversification during the Eifelian - Frasnian). The highest diversity of bioconstructors in the Givetian correlates with a decrease in brachiopod diversity. Changes in the vertical distribution of the faunas are correlated with the facies development: the development of carbonates correlates with the abundance of stromatoporoids and tabulates, while brachiopods were most abundant before and after the peak of carbonate development. 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