Summary
Analysis of the taxonomic composition, diversity and guild structure of five “typical” reef and mud mound communities ranging in age from Late Devonian-Early Carboniferous indicates that each of these aspects of community organization changed dramatically in relation to three extinction events. These events include a major or mass extinction at the end of the Frasnian; reef communities were also effected by less drastic end-Givetian and mid-late Famennian extinctions of reef-building higher taxa.
Peak Paleozoic generic diversities for reef-building stromatoporoids and rugose corals occurred in the Eifelian-Givetian; reef-building calcareous algal taxa were longranging with peak diversity in the Devonian. These three higher taxa dominated all reef-building guilds (Constructor, Binder, Baffler) in the Frasnian and formed fossil reef communities with balanced guild structures. The extinction of nearly all reef-building stromatoporoids and rugose corals at the end of the Frasnian and the survival of nearly all calcareous algac produced mid-late Famennian reef communities dominated by the Binder Guild. Despite the survival of most calcareous algae and tabulate corals, the mid-late Famennian extinction of all remaining Paleozoic stromatoporoids and nearly all shelf-dwelling Rugosa brought the already diminished Devonian reef-building to a halt. These Devonian extinctions differ from mass extinctions by the absence of a statistically significant drop in taxonomic diversity and by their successional and cumulative effects on reef communities.
Tournaisian mud mounds contain communities markedly different from the frame-building communities in Late Devonian and Visean reefs. Mound-building biotas consist of an unusual association dominated by erect, weakly skeletonized members of the Baffler Guild (chiefly fenestrate Bryozoa; Pelmatozoa) and laterally expanded, mud-binding algae/stromatolites and reptant Bryozoa. The initial recovery to reefs with skeletal frameworks in the Visean was largely due to the re-appearance of new species of abundant colonial rugose corals (Constructor Guild) and fenestrate Bryozoa.
This Frasnian-Visean evolution in the taxonomic composition and structure of the reef-building guilds is also expressed by abrupt changes in biofacies and petrology of the reef limestones they produced. Thus, “typical” Frasnian reef limestones with balanced guild structures are framestones-boundstones-bafflestones, Famennian reefs are predominantly boundstones, Tournaisian mud mounds are bafflestones and Visean reefs are bafflestones-framestones.
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References
Adams, A.E. (1984): Development of algal-foraminiferal-coral reefs in the Lower Carboniferous of Furness, northwest England. —Lethaia17, 233–249
Alvarez, L.W., Alvarez, W., Asaro, F. &Michel, H.V. (1980): Extraterrestrial cause for the Cretaceous-Tertiary extinction.— Science,208, 1095–1108
Bambach, R.K. (1977): Species richness in marine benthic habitats through the Phanerozoic.—Paleobiology,3, 152–167.
Bathurst, R.G.C. (1959): The cavernous structure of some MississippianStromatactis reefs in Lancashire, England.—J. Geol.,67, 506–521
— (1980): Stromatactis—origin related to submarine cemented crusts in Paleozoic mud mounds.—Geology,8, 131–134
— (1982): Genesis of stromatactis cavities between submarine crusts in Palaeozoic carbonate buildups.—J. Geol. Soc. London,139, 165–181
Bechstädt, T. (1974): Origin of stromatactis—a replacement of colonial microbial accretions.—N. Jb. Paläont. Mh.,1974, 643–663
Boulvain, F. &Coen-Aubert, M. (1989): Modèle sédimentologique des monticules micritiques de la partie superieure Frasnian du massif de Phillippeville et corrélations séquentielles avec le bord nord du synclinorium de Dinant.—Comptes Rendu Acad. Sci. Paris,309, ser II, 81–87
Christopher, C.C. (1990): Late MississippianGirvanella-bryozoan mud mounds in southern West Virginia.—Palaios,5, 460–471, Lawrence
Chuvashov, B. &Riding, R. (1984): Principal floras of Paleozoic marine calcareous algae.—Palaeontology,27, 487–500.
Cockbain, A.E. (1984): Stromatoporoids from the Devonian reef complexes, Canning Basin, Western Australia.—Geol. Surv. W. Australia, Bull.129, 108 pp., 28 Pls., 20 Figs., Perth
— (1989): Distribution of Frasnian and Famennian stromatoporoids. —Assoc. Australasian Paleontologists, Mem.8, 339–345, 2 Figs., 3 Tabs., Brisbane
Conil, R., Groessens, E., Laloux, M., Poty, E. &Tourneur, F. (1990): Carboniferous guide foraminifera, corals and conodonts in the Franco-Belgian and Campine Basins: their potential for widespread correlation.—Courier Forsch. Inst. Senckenberg,130, 15–30, 6 Figs., Frankfurt a.M.
Dupont, E. (1863): Sur le calcaire Carbonifère de la Belgique et du Hainaut Francaise.—Acad. Roy. Belgique, 2nd ser.,15, 86 pp.
Embry III, A.F. &Klovan, J.E. (1971): A Late Devonian reef tract on northeastern Banks Island, N.W.T..—Canadian Petroleum Geology, Bull.,19, 730–781, Calgary
Fagerstrom, J.A. (1985): Comparison of processes and guild structures in Holocene and ancient reef communities.—Proc. Fifth Intern. Coral Reef Congress,2, 126, Tahiti
— (1987): The evolution of reef communities.—600 pp., 51 pls., New York (Wiley)
— (1988): A structural model for reef communities.—Palaios,3, 217–220, 1 Tab., Lawrence
— (1991): Reef-building guilds and a checklist for determining guild membership.—Coral Reefs,10, 47–52
Fischer, A.G. (1982): Long-term climatic oscillations recorded in stratigraphy.—In:Berger, W. (ed) (1982): Climate in earth history, Natl. Research Council, Studies in Geophysics, Washington, 97–104
— (1984): The two Phanerozoic supercycles.—In:Berggren, W.A. &Vancouvering, J.A. (eds.): Catastrophies in earth history.—129–150, Princeton (Princeton Univ. Press)
Gould, S.J. (1989): Wonderful Life, The Burgess Shale and the Nature of History.—347 pp., New York (Norton)
Haikawa, T. &Ota, M. (1978): A lower Carboniferous coral reef found in theNagatophyllum satoi zone of the Akiyoshi Limestone Group, southwest Japan.—Akiyoshi-dai Mus. Nat. Hist., Bull.,13, 1–14, 8 Pls.
Heckel, P.H. (1972): Possible inorganic origin for stromatactis in calcilutite mounds in the Tully Limestone, Devonian of New York.—J. Sed. Petrol.,24, 7–18
Hill, D. & Jell, J.S. (1970): Devonian corals from the Canning Basin, Western Australia.—Geol. Surv. W. Australia, Bull.121, 158 pp., 20 Pls.
Joachimski, M.M. &Buggisch, W. (1993): Anoxic events in the Late Frasnian—causes of the Frasnian-Famennian faunal crisis?—Geology,21, 675–678
Kapp, U. (1975): Paleoecology of Middle Ordovician stromatoporoid mounds in Vermont.—Lethaia,8, 195–207
Kapp, U. &Stearn, C.W. (1975): Stromatoporoids of the Chazy Group (Middle Ordovician), Lake Champlaine, Vermont and New York.—J. Paleontology,49, 163–186
Kauffman, E.G. (1988): The dynamics of marine stepwise mass extinction.—Revista Espanola de Paleontologia, No. Extraordinario, 57–71
Kauffman, E.G. & Fagerstrom, J.A. (1993): The Phanerozoic evolution of reef diversity.—In:Ricklefs, R. & Schluter, D. (1993): Species diversity in ecological communities—p. 315–329 (Univ. of Chicago Press)
Lane, N.G. (1971): Crinoids and reefs.—N. Am. Paleontological Convention, Part J, 1430–1443, Lawrence
Larwood, G.P. (ed.): Extinction and survival in the fossil record.— 376 pp., 87 Figs., Oxford (Univ. Press)
Lees, A. (1964): The structure and origin of the Waulsortian (Lower Carboniferous) “reefs” of west-central Eire.—Phil. Trans. Roy. Soc. London, ser B,247, 483–531
Lees, A. (1982): The paleoenvironmental setting and distribution of the Waulsortian facies of Belgium and southern Britain.—In:Bolton, K., Lane, H.R. & Lemone, D.V. (eds) (1982): Symposium of the paleoenvironmental setting and distribution of the Waulsortian facies.—El Paso Geol. Soc. & Univ. Texas at El Paso, 1–16
— (1988): Waulsortian “reefs”: the history of a concept.—Inst. Geol., Univ. Louvain,34, 43–55
Lees A. &Conil, R. (1980): The Waulsortian reefs of Belgium.— Geobios. Mem. Special4, 35–46, 10 Figs., Lyon
Lees, A., Hallet, V. &Hibo, D. (1985): Facies variation in Waulsortian buildups, Part 1; a model from Belgium.—Geol. J.,20, 133–158
Lees, A. &Miller, J. (1985): Facies variation in Waulsortian buildups, Part 2: Mid- Dinantian buildups from Europe and North America.—Geol. J.,20, 159–180
Lees, A. & Miller, J. (in press): Waulsortian banks.—In:Monty, E.C., Bosence, D., Bridges, P. & Pratt, B. (eds) (in press): Mud mounds.—Intern. Assoc. Sedimentologists, Special Publ.
Mamet, B. (1991): Carboniferous calcareous algae.—In:Riding, R. (ed) (1991): Calcareous algae and stromatolites,—p. 370–451, 3 Figs. Berlin (Springer)
Marshall, J.F. &Davies, P.J. (1988):Halimeda bioherms of the northern Great Barrier Reef.—Coral Reefs,6, 139–148
McKinney, F.K., McKinney, M.J. &Listokin, M.R.A. (1987): Erect bryozoans are more than baffling: enhanced sedimentation rate by a living unilaminate branched bryozoan and possible implications for fenestrate bryozoan mudmounds.—Palaios,2, 41–47
McKinney, F.K., & Jackson, J.B.C. (1989): Bryozoan evolution.— 238 p., 13 Tab., 159 Figs. (Univ. of Chicago Press)
McGhee, G.R., Jr. (1982): The Frasnian-Famennian extinction event: a preliminary analysis of Appalachian marine ecosystems. —Geol. Soc. Am., Special Paper190, 491–500, 8 Figs., 3 Tabs., Boulder
McGhee, G.R., Jr. (1989): The Frasnian-Famennian extinction event.—In:Donovan, S.K. (ed) (1990): Mass extinctions, processes and products.—p. 133–137, (Columbia Univ. Press)
McLaren, D.J. (1970): Time, life and boundaries.—J. Paleontology,44, 801–815
— (1982): Frasnian-Famennian extinctions.—Geol. Soc. Am., Special Paper190, 477–484, Boulder
— (1983): Bolides and biostratigraphy.—Geol. Soc. Am., Bull.,94, 313–324, Boulder
Monty, C. (1982): Cavity or fissure dwelling stromatolites (Endostromatolites) from Belgian Devonian mud mounds.— Annales Soc. Geol. Belgique.105, 343–344
Moore, R.C. (1955): Invertebrates and the geologic time scale.— Geol. Soc. Am. Special Paper62, 547–574
Nagy, K. (1985): Reef-forming algal chaetetid boundstone found in the Akiyoshi Limestone Group, southwest Japan.—Akiyoshi Mus. Nat. Hist., Bull.,20, 1–15
Oliver, JR., W.A. &Pedder, A.E.H. (1979): Rugose corals in Devonian stratigraphical correlation.—Spec. Papers Palaeont.23, 233–248, Boulder
Orme, G.R. &Salama, M.S. (1988): Form and seismic stratigraphy ofHalimeda banks in part of the northern Great Barrier Reef Province.—Coral Reefs,6, 131–137
Ota, M. (1968): The Akiyoshi Limestone Group: a geosynclinal organic reef complex.—Akiyoshi-dai Sci. Mus. Nat. Hist., Bull.,5, 1–44, 31 Pls.
— (1977): Geological studies of Akiyoshi; Part I, General Geology of the Akiyoshi Limestone Group.—Akiyoshi-dai Sci. Mus. Nat. Hist., Bull.,12, 1–33, 3 Pls.
Playford, P.E. (1980): Devonian “Great Barrier Reef” of Canning Basin, Western Australia.—Am. Assoc. Petroleum Geologists, Bull.,64, 814–840
Playford, P.E. &Cockbain, A.E. (1989): Devonian reef complexes, Canning Basin, Western Australia: a review.—Assoc. Australasian Paleontologists, Mem.8, 401–412
Playford, P.E., Cockbain, A.E., Druce, E.C. &Wray, J.L. (1976): Devonian stromatolites from the Canning, Basin, Western Australia.—In:Walter, M.R. (ed.) (1976): Stromatolites.— p. 543–563, Amsterdam (Elsevier)
Playford, P.E., McLaren, D.J., Orth, C.J., Gilmore, J.S., &Goodfellow, W.D. (1984): Iridium anomaly in the Upper Devonian of the Canning Basin, Western Australia.—Science,226, 437–439
Playford, P.E. & Lowry, D.C. (1966): Devonian reef complexes of the Canning Basin, Western Australia.—Geol. Surv. W. Australia, Bull.,118, 150 pp., Perth
Poty, E. (1984): Rugose corals at the Devonian-Carboniferous boundary.—Cour. Forsch.-Inst. Senckenberg,67, 29–35, Frankfurt a.M.
— (1986): Late Devonian to Early Tournaisian rugose corals.— Annales Soc. Geol. Belgique.109, 65–74
Pratt, B.R. (1982): Stromatolitic framework of carbonate mud mounds.—J. Sed. Petrol.,52, 1203–1227
Pray, L.C. (1958): Fenestrate bryozoan core facies, Mississippian bioherms, southwestern United States.—J. Sed. Petrol.,28, 261–273
Raup, D.M. &Sepkosky JR., J.J. (1982): Mass extinctions in the marine fossil record.—Science,215, 1501–1502, 2 Figs.
Riding, R. (1975):Girvanella and other algae as depth indicators. —Lethaia8, 173–179
— (1977): Problems of affinity in Paleozoic calcareous algae.—In:Flügel, E. (ed.) (1977): Fossil algae, 202–211, Berlin (Springer)
Rigby, J.K. (1986): Late Devonian sponges of Western Australia. —Geol. Surv. W. Australia, Report18, 59 pp., 7 Pls., Perth
Root, R.B. (1967): The niche exploitation pattern of the blue-gray gnatcatcher.—Ecological Monographs,97, 317–350
Ross JR., R.J., Jaanusson, V. & Friedman, I. (1975): Lithology and origin of Middle Devonian calcareous mudmound at Meiklejohn Peak, southern Nevada.—U.S. Geol. Surv., Professional Paper871, 48 pp.
Roux, A. (1985): Introduction a l'etude des algues fossiles Paleozoiques (de la bacterie a la tectonique des plaques).—Centres Recherche Explor.-Prod. Elf-Aquitaine,9, 465–699, 5 Tabs., 6 Pls., Pau
Rowland, S.M. (1984): Were there framework reefs in the Cambrian?—Geology,12, 181–183
Sandberg, C.A., Ziegler, W., Dreesen, R. &Butler, J. (1988): Late Frasnian mass extinction: conodont event stratigraphy, global changes, and possible causes; Part 3.—Cour. Forsch.-Inst. Senckenberg,102, 263–307, 2 Pls., 15 Figs., 6 Tabs., Frankfurt, a.M.
Sepkoski, J.J. (1993): Ten years in the library: new data confirm paleontological patterns.—Paleobiology,19, 43–51
Shilo, N.A., Bouckaert, J., Afanasoeva, G.A., Bless, M.J.M., Conil, R., Erlanger, O.A., Gagiev, M.H., Lazarev, S.S., Onoprienko, Y.I., Poty, E., Razina, T.P., Simakov, K.V., Smirnova, L.V., Streel, M. &Swennen, R. (1984): Sedimentological and paleontological atlas of the Late Famennian and Tournaisian deposits in the Omolon region (NE-USSR).— Annals Geol. Soc. Belgique,107, 137–247, 4 Figs., 3 Tabs., 52 Pls.
Sorauf, J.E. (1989): Rugosa and the Frasnian-Famennian extinction event: a progress report.—Assoc. Australasian Palaeontologists, Mem.8, 327–338
Sorauf, J.E. &Pedder, A.E.H. (1986): Late Devonian rugose corals and the Frasnian-Famennian crisis.—Canadian J. Earth Sci.,23, 1265–1287
Stearn, C.W. (1982): The unity of the Stromatoporoidea.—Third N. Am. Paleontological Convention, Proc., p. 511–516, Montreal
— (1987): Effect of the Frasnian-Famennian extinction event on the stromatoporoids.—Geology,15, 677–679
— (1988): Stromatoporoids from the Famennian (Devonian) Wabamum Formation, Normandville oilfield, north-central Alberta, Canada.—J. Paleontology,62, 411–419
— (1993): Revision of the Order Stromatoporida.—Palaeontology,36, 201–229, 2 pls., 8 text-figs.
Stearn, C.W., Halim-Dihardia, M.K. &Nishida, D.K. (1987): An oil-producing stromatoporoid patch reef in the Famennian (Devonian) Wabamum Formation, Normandville Field, Alberta. —Palaios,2, 560–570, 14 Figs., 2 Tabs.
Stockman, K.W., Ginsburg, R.N. &Shinn, E.A. (1967): The production of lime mud by algae in south Florida.—J. Sed. Petrol.,37, 633–648
Termier, H., Termier, G. &Tsien, H.H. (1981) Spongaires des calcaires recifaux du Frasnien de l'Ardenne.—Soc. Belge de Geologie,90, 287–298
Termier, H., Termier, G. & Vachard, D. (1977): On Moravamminida and Aoujgaliida (Porifera, Ischyrospongia).—In:Flügel, E. (ed.) (1977): Fossil algae.—p. 215–219 (Springer)
Tourneur, F., Conil, R. &Poty, E. (1989): Donnees preliminaires sur les tabules et les chaetetides du Dinantien de la Belgique.— Soc. Belge Geol. Bull.,98, 401–442, 12 Pls.
Tsien, H.H. (1979): Paleoecology of algal-bearing facies in the Devonian (Couvinian to Frasnian) reef complexes of Belgium. —Palaeogeography, Palaeoclimatology, Palaeoecology,27, 103–127
— (1985a): Origin ofStromatactis—a replacement of colonial microbial accretions.—In:Toomey, D.F. &Nitecki, M.H. (eds) (1985): Paleoalgology—Contemporaneous research and applications. —274–289, 7 Figs., Berlin (Springer)
— (1985b): The algal-bacterial origin of micrites in mud-mounds. —In:Toomey, D.F. &Nitecki, M.H. (eds) (1985): Palaeoalgology —Contemporaneous research and applications.—290–296, 4 Figs., Berlin (Springer)
— (1990): Ancient reefs and micrite mounds, their concepts, nomenclature and recognition.—Geol. Soc. China, Proc.,33, 261–287
Ubaghs, G., et al. (1978): Echinodermata2 (1), Crinoidea. Treatise on Invert. Paleontology, Part T, 401 p. (Geol. Soc. Am. & Univ. Kans. Press)
Wang, K., Attrep JR., M. &Orth, C.J., (1993): Global iridium anomaly, mass extinction and redox change at the Devonian-Carboniferous boundary.—Geology,21, 1071–1074
Webb, G.E. (1991): Late Visean coral-algal bioherms from the Lion Creek Formation of Queensland, Australia.—11th Cong. Intern. Stratigraphie Geologie Carbonifere, Compte Rendu,3, 282–295
Weidlich, O., Bernecker, M. &Flügel, E. (1993): Combined quantitative analysis and microfacies studies of ancient reefs: an integrated approach to Upper Permian and Upper Triassic reef carbonates (Sultanate of Oman).—Facies,28, 115–144
Wilde, P. &Berry, W.B.N. (1984): Destabilization of the oceanic density structure and its significance to marine “extinction” events.—Palaeogeog., Palaeoclimat., Palaeoecol.,48, 143–162
Wilson, J.L. (1975): Carbonate facies in geologic history.—471 pp., New York, (Springer)
Wolfenden, E.B. (1958): Paleoecology of the Carboniferous reef complex and shelf limestones in northwest Derbyshire, England. —Geol. Soc. Am. Bull.,69, 871–898
Wray, J.L. (1967): Upper Devonian calcareous algae from the Canning Basin, Western Australia.—Colorado School Mines, Prof. Contrib.,3, 76 pp., Golden
— (1972): Environmental distribution of calcareous algae in Upper Devonian reef complexes.—Geol. Rundschau,61, 578–584
Wray, J.L. &Playford, P.E. (1970): Some occurrences of Devonian reef-building algae in Alberta.—Canadian Petroleum Geology, Bull.,18, 544–554, 2 Pls., Calgary
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Fagerstrom, J.A. The history of Devonian-Carboniferous reef communities: Extinctions, effects, recovery. Facies 30, 177–191 (1994). https://doi.org/10.1007/BF02536896
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DOI: https://doi.org/10.1007/BF02536896