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Deep-water stromatolites andFrutexites Maslov from the early and Middle Jurassic of S-Germany and Austria

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Summary

Despite extensive discussions during the last 20 years stromatolites are still used by many geologists as unequivocal indicators of very shallow-water conditions. We investigated four stratigraphic units from the Lower and Middle Jurassic of southern Germany (Posidonien-Schiefer, Amaltheen-Ton) and of the Northern Calcareous Alps (Adneter Kalk, Klauskalk), which were formerly interpreted as shallow marine sediments by some authors due to the occurrence of stromatolites. Our interpretations of the macro-, micro- and ultrafacies of these sediments are not compatible with shallow-water settings. We therefore propose a deep-marine, aphotic origin of these stromatolites.

Former interpretations of the Posidonien-Schiefer as a shallow-water deposit are mainly based on the occurrence of stromatolites. We favour the model of a temporarily stagnant, deep, aphotic basin for these planktonrich sediments. Particles resembling ooids, but lying within mudstones cannot be taken as evidence for shallow agitated water. They either formed within the mud or are allochthonous.

The deep-water setting of the red limestone of the Alpine Early and Middle Jurassic is indicated by a lack of platform-typical components like coated grains and phototrophic benthos and by shells of plankton and nekton forming a major part of the sediment. Stromatolites occur on the steep slope of a drowned Rhaetian reef with an estimated relief of 50–100 m and immediately below and within radiolarian limestones, deposited below the aragonite compensation depth (ACD).

The aphotic stromatolites show some morphological differences to their shallow water counterparts. In all of our sections they occurred during intervals of reduced sedimentation. They form only thin horizons and probably grew very slowly. Mineralizations by Fe−Mn oxides and phosphate are very common. The presence of a microbial film is evident from binding of sedimentary particles, but the nature of the microbes is not known. Growth habits within the very distinct environments of red limestone and black shales show some common features, but also clear differences.

The microproblematicumFrutexites Maslov is a very common component in deep-water stromatolites, but may also itself form small crusts or dendrolites. It occurs in two different forms. Opaque, slender forms with indistinct outlines probably grew within the weakly lithified sediment. Thicker, transparent forms with well defined outlines are found in cavities and probably also grew on the seafloor. Well preserved specimens display an internal fabric of radially arranged fibres of Fe−Mn oxides and calcite. It is suggested that calcite or aragonite were one original mineralogy ofFrutexites, which was later replaced by Fe−Mn oxides or phosphate.

It is not certain whetherFrutexites is an organic, biomineralized structure or an inorganic mineralization, but the variable mineralogy and growth forms in different environments point to an organic origin. But even if organic, the occurrence in cryptic habitats and negative phototactic growth-directions make it clear thatFrutexites was not phototrophic.

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References

  • Aldinger H. (1968): Die Paläogeographie des schwäbischen Jurabeckens.—Eclogae geol. Helv.,61, 167–182, Basel

    Google Scholar 

  • Awramik, S.M. (1991): Archaean and Proterozoic Stromatolites.— InRiding, R. (ed.): Calcareous Algae and Stromatolites. 289–304, Berlin (Springer)

    Google Scholar 

  • Bandel, K. &Knitter, H. (1986): On the origin and diagenesis of the bituminous Posidonia Shale (Toarcian) of southern Germany.—Mitt. Geol.-Paläont. Inst. Univ. Hamburg,60, 151–177, Hamburg

    Google Scholar 

  • Birzer, F. (1936): Die Monotis-Bank in den Posidonienschiefern, besonders Frankens.—Abh. geol. Landesuntersuch. Bayer. Oberbergamt,26, 3–32, München

    Google Scholar 

  • Böhm, F. (1992): Mikrofazies und Ablagerungsmilieu des Lias und Dogger der Nordöstlichen Kalkalpen.—Erlanger geol. Abh.,121, 57–217, Erlangen

    Google Scholar 

  • Böhm F. & Brachert, Th.C. (1990): Stromatolith-artige Krusten aus tiefmarinen Kalken (Jura, Nördliche Kalkalpen, Franken; Quartär, Rotes Meer) (Vortragskurzfassung).—5. Sedimentologen-Treffen 1990, 1 p., Bonn

  • Brachert, Th.C. &Dullo W.-Chr. (1991): Laminar Micrite Crusts and Associated Foreslope Processes, Red Sea.—J. Sed Petr.,61, 345–363, Lawrence

    Google Scholar 

  • Brachert, Th.C., Dullo, W.-Chr. &Brandner, R. (1989): Rezente und triadische Riffhang-‘Stromatolithe’ (Rotes Meer/Südalpen).— Geol. Paläont. Mitt. Innsbruck,16, 13–14, Innsbruck

    Google Scholar 

  • Bruder, H.J. (1968): Ökologische, geochemische und sedimentologische Untersuchungen im Lias zeta (oberes Toarcium) Schwabens, mit Berücksichtigung des obersten Lias epsilon.—Arb. Geol. Paläont. Inst. TH-Stuttgart, N.F.,56, 165 p, Stuttgart

  • Byers, C.W. (1977): Biofacies patterns in euxinic basins: a general model.—Soc. Econ. Paleont. Min. Spec. Publ.,25, 5–17, Tulsa

    Google Scholar 

  • Cragg, B.A., Harvey, S.M., Fry, J.C., Herbert, R.A. &Parkes, R.J. (1992): Bacterial Biomass and Activity in the Deep Sediment Layers of the Japan Sea, Hole 798B-Leg 128.—Proc. ODP, Sci. Res.,127/128, 761–776, College Station

    Google Scholar 

  • Davies, G.R. (1970): Algal laminated sediments, Gladstone embayment, Shark Bay, Western Australia.—In:Logan, B.W., Davies, G.R., Read, J.F. & Cebulski, D.E. (eds.): Sedimentation and environment, Shark Bay, Western Australia.—Amer. Ass. Petrol. Geol., Mem.,13, 169–205, Tulsa

  • De Graciansky, P.C., Lemoine, M. & Tricart, P. (1988): Mesozoic Passive Margin of the Tethyan Ocean in the French Western Alps.—AAPG Mediterranean Basins Conference, Field Trip Guide #1, 53 p, Nice.

  • Delamette, M. (1990): Aptian, Albian and Cenomanian microbialites from the condensed phosphatic deposits of the Helvetic shelf, Western Alps.—Eclogae geol. Helv.,83, 99–121, Basel

    Google Scholar 

  • Dromart, G. (1989): Deposition of Upper Jurassic fine grained limestones in the western Subalpine Basin, France.—Palaeogeogr., Palaeoclimatol., Palaeoecol.,69, 23–43, Amsterdam

    Article  Google Scholar 

  • Dullo, W.-Chr., Moussavian, E. &Brachert, Th. (1990): The foralgal crust facies of the deeper fore reefs in the Red Sea: A deep diving survey by submersible.—Geobios,23, 261–281 Lyon

    Google Scholar 

  • Elder, R.L. &Smith, G.R. (1984): Fish taphonomy and paleoecology.— Geobios, Mém. Spec.,8, 287–291, Lyon

    Google Scholar 

  • — & — (1988): Fish taphonomy and environmental inference in paleolimnology.—Palaeogeogr., Palaeoclimatol., Palaeoecol.,62, 577–592, Amsterdam

    Article  Google Scholar 

  • Flügel, E. (1982): Microfacies analysis of limestones.—633 p, Berlin (Springer)

    Google Scholar 

  • Folk R.L., Chafetz, H.S. &Tiezzi, P. (1985): Bizarre Forms of Depositional and Diagenetic Calcite in Hot-Spring Travertines, Central Italy.—Soc. Econ. Paleont. Min. Spec. Publ.,36, 349–369, Tulsa

    Google Scholar 

  • Gaetani, M., Fois, E., Jadoul, F. &Nicora, A. (1981): Nature and evolution of Middle Triassic carbonate buildups in the Dolomites (Italy).—Mar. Geol.,44, 25–27, Amsterdam

    Article  Google Scholar 

  • Garett, P. (1970): Phanerozoic stromatolites: Noncompetitive ecologic restriction by grazing and burrowing animals.—Science,169, 171–173, Washington

    Article  Google Scholar 

  • Glover, E.D. (1961): Method of solution calcareous materials using the complexing agent, EDTA.—J. Sed. Petr.,31, 622–626, Tulsa

    Google Scholar 

  • Golubic, S., Friedmann, I. &Schneider, J. (1981): The Lithobiontic Ecological Niche, with Special Reference to Microorganisms.— J. Sed. Petr.,51, 475–478, Lawrence

    Google Scholar 

  • Grötsch, J. &Flügel, E. (1992): Facies of Sunken Early Cretaceous Atoll Reefs and their Capping Late Albian Drowning Succession (Northwestern Pacific).—Facies,27, 153–174, Erlangen

    Article  Google Scholar 

  • Grotzinger, J.P. (1986): Evolution of Early Proterozoic passivemargin carbonate platform, Rocknest Formation, Wopmay orogen, Northwest Territories, Canada.—J. Sed. Petr.,56, 831–847, Tulsa

    Google Scholar 

  • Hoffman, P. (1974): Shallow and deep-water stromatolites in Lower Proterozoic platform-to-basin facies change, Great Slave Lake, Canada.—Amer. Ass. Petrol. Geol., Bull,58, 856–867, Tulsa

    Google Scholar 

  • Huckriede, R. (1971): Rhyncholithen-Anreicherung (Oxfordium) an der Basis des Älteren Radiolarits der Salzburger Kalkalpen.— Geologica et Palaeontologica,5, 131–147, Marburg

    Google Scholar 

  • Hurley, N.F. &Van Der Voo, R. (1990): Magnetostratigraphy, Late Devonian iridium anomaly, and impact hypotheses.— Geology,18, 291–294, Boulder

    Article  Google Scholar 

  • Ingle, J.C., Suyehiro, K., von Breymann, M.T. &Shipboard Scientific Party (1990): Site 798.—Proc. ODP, Init. Repts.,128, 121–236, College Station

    Google Scholar 

  • Jenkyns, H.C. (1971): The Genesis of Condensed Sequences in the Tethyan Jurassic.—Lethaia,4, 327–352, Oslo

    Google Scholar 

  • Jordan, R. &Schmidt-Kaler, H. (1985): Der obere Lias (Toarcium) in Südfranken aufgrund neuer Bohrungen.—Geol. Jb., A84, 55–101, Hannover

    Google Scholar 

  • Kauffman, E.G. (1981): Ecological Reappraisal of the German Posidonienschiefer (Toarcian) and the Stagnant Basin Model. —In:Gray, J. (ed.): Communities of the past.—311–381, Stroudsbourg

  • Keupp, H. &Arp, G. (1990): Aphotische Stromatolithe aus dem süddeutschen Jura (Lias, Dogger).—Berliner geowiss. Abh. A,124, 3–33, Berlin

    Google Scholar 

  • Keupp, H. &Ilg, A. (1989): Die kalkigen Dinoflagellaten im Ober-Callovium und Oxfordium der Normandie/Frankreich. —Berliner geowiss. Abh. A,106, 165–205, Berlin

    Google Scholar 

  • Kieslinger, A. (1964): Die nutzbaren Gesteine Salzburgs—436 p., Salzburg (Bergland-Buch)

    Google Scholar 

  • Krajewski, K.P. (1981): Pelagiczne stromatolity z wapieni albu wierchorvego Tatr.—Kwart. Geol.,25, 731–759, Warszawa

    Google Scholar 

  • Krumbeck, L. (1943): Zur Stratigraphie und Faunenkunde des Lias zeta in Nordbayern, Teil 1.—Z. dtsch. geol. Ges.,95, 279–340, Berlin

    Google Scholar 

  • Krystyn, L. (1971): Stratigraphie, Fauna und Fazies der Klausschichten (Aalenium-Oxford) in den Östlichen Nordalpen.— Verh. Geol. B.-A.,1971, 486–509, Wien

    Google Scholar 

  • Land, L.S. &Moore, C.H. (1980): Lithification, micritization and syndepositional diagenesis of biolithites on the Jamaican island slope.—J. Sed. Petr.,50, 357–370, Tulsa

    Google Scholar 

  • Maslov, V.P. (1960): Stromatolity (ick genezis, metodizucheniya, svjaz's fatsiyami i geologicheskoe znachenie na primere Ordovika Sibirskoj Platformy).—Trudy Geol. Inst., vyp.,41, Moskva

  • Massari, F. (1981): Cryptalgal fabrics in the Rosso Ammonitico sequences of the Venetian Alps.—In:Farinacci, A. &Elmi, S. (eds.): Rosso Ammonitico Symposium Proceedings.—435–469, Rom (Edizioni Tecnoscienzia)

    Google Scholar 

  • Mauritsch, H.J. &Frisch, W. (1980): Paleomagnetic results from the Eastern Alps and their comparison with data from the Southern Alps and the Carpathians.—Mitt. österr. geol. Ges.,73, 5–13, Wien

    Google Scholar 

  • Meyer, R.K.F. & Schmidt-Kaler, H. (1992): Wanderungen in der Erdgeschichte (5). Durch die Fränkische Schweiz.—169 p, München (Pfeil)

  • Monty, M.C. (1973): Les nodules de manganese sont des stromatolithes oceaniques.—C. R. Acad. Sc. Paris, Serie. D,276, 3285–3288, Paris

    Google Scholar 

  • Myrow, P.M. &Coniglio, M. (1991): Origin and Diagenesis of Cryptobiontic Frutexites in the Chapel Island Formation (Vendian to Early Cambrian) of Southeast Newfoundland, Canada.—Palaios,6, 572–585, Lawrence

    Google Scholar 

  • Peitgen, H.-O. (1988): Fantastic Deterministic Fractals.—In:Peitgen, H.-O. &Saupe, D. (eds.): The Science of Fractal Images.—169–218, New York (Springer)

    Google Scholar 

  • Pentecost, A. (1990): The formation of travertine shrubs: Mammoth Hot Springs, Wyoming.—Geol. Mag.,127, 159–168, London

    Article  Google Scholar 

  • Playford, P.E., Cockbain, A.E., Druce, E.C. &Wray, J.L. (1976): Devonian stromatolites from the Canning Basin, Western Australia.—Developments in Sedimentology,20, 543–564, Amsterdam

    Article  Google Scholar 

  • Pober, E. &Faupl, P. (1988): The chemistry of detrital chromian spinels and its implications for the geodynamic evolution of the Eastern Alps.—Geolog. Rdsch.,77, 641–670, Stuttgart

    Article  Google Scholar 

  • Pratt, B. (1982): Stromatolite decline—A reconsideration.— Geology,10, 512–515, Boulder

    Article  Google Scholar 

  • Prauss, M., Ligouis, B. & Luterbacher, H. (1991): Organic matter and palynomorphs in the ‘Posidonienschiefer’ (Toarcian, Lower Jurassic) of southern Germany.—In:Tyson, R.V. & Pearson, T.H. (eds.): Modern and Ancient Continental Shelf Anoxia.— 335–351, London

  • Reiss, Z. &Hottinger, L. (1984): The Gulf of Aqaba-Ecological micropaleontology.—354p., Berlin (Springer)

    Google Scholar 

  • Riding, R. (1991a): Classification of Microbial Carbonates.—InRiding, R. (ed.): Calcareous Algae and Stromatolites.—21–51, Berlin (Springer)

    Google Scholar 

  • — (1991b): Calcified Cyanobacteria.—InRiding, R. (ed.): Calcareous Algae and Stromatolites.—55–87, Berlin (Springer)

    Google Scholar 

  • Riding, R. &Voronova, L. (1982): Recent freshwater oscillatoriacean analogue of the Lower Palaeozoic calcareous algaAngulocellularia.—Lethaia,15, 105–114, Oslo

    Google Scholar 

  • Rieber, H. (1973): Fauna und Stratigraphie einer oolithischen Kalkbank aus dem Toarcium von Gipf (Kanton Aargau, Schweiz).—Eclogae geol. Helvetiae,66, 657–665, Basel

    Google Scholar 

  • Riegraf, W., Werner, G. & Lörcher, F. (1984): Der Posidonienschiefer, Biostratigraphie, Fauna und Fazies des südwestdeutschen Untertoarciums (Lias epsilon).—195 p, Stuttgart

  • Ruttner, A. (1980): Bericht 1979 über ergänzende Begehungen westlich Gaming und südlich Lunz am See auf Blatt 71 Ybbsitz.— Verh. Geol. B.-A.,1980, A45-A47, Wien

    Google Scholar 

  • Schäfer, P. (1979): Fazielle Entwicklung und palökologische Zonierung zweier obertriadischer Riffstrukturen in den nördlichen Kalkalpen (Oberrhät-Riff-Kalke, Salzburg).—Facies,1, 3–245, Erlangen

    Article  Google Scholar 

  • Schlager, W. &Schöllnberger, W. (1974): Das Prinzip der stratigraphischen Wenden in der Schichtenfolge der Nördlichen Kalkalpen.—Mitt. Geol. Ges. Wien,66/67, 165–193, Wien

    Google Scholar 

  • Schröder, B. (1968): Erläuterungen zur geologischen Karte von Bayern 1∶25 000 Blatt Nr. 6332 Erlangen-Nord.—München (Geol. Landesamt)

    Google Scholar 

  • Seilacher, A. (1982): Posidonia shales (Toarcian, S. Germany)-stagnant basin model revalidated.—In:Montanaro Gallitelli, E. (ed.): Proc. 1st int. meeting on palaeontology, essential of historical geology, Venice, 25–55, Modena

  • Seilacher, A. & Westphal, F. (1971): ‘Fossil-Lagerstätten’.—InMüller, G. (ed.): Sedimentology of parts of Central Europe, Guidebook.—Internat. Sedimentol. Congress 8, 327–335, Frankfurt

  • Smith, A.G. &Briden, J.C. (1977): Mesozoic and Cenozoic Paleocontinental Maps.—63 p, Cambridge (Cambridge University Press)

    Google Scholar 

  • Stone Soup Group (1991): Fractint, Version 16.12 (public domain software).-

  • Stoyan, D. &Stoyan, H. (1992): Fraktale, Formen, Punktfelder. Methoden der Geometrie-Statistik.—394 p, Berlin (Akademie Verlag)

    Google Scholar 

  • Szulczewski, M. (1963): Stromatolites from the high-tatric Bathonian of the Tatra Mountains.—Acta Geol. Pol.,13, 125–141, Warschau

    Google Scholar 

  • Tollmann, A. (1976): Analyse des klassischen Mesozoikums. Stratigraphie, Fauna und Fazies der Nördlichen Kalkalpen.— Bd. 2, 580 p, Wien (Deuticke)

    Google Scholar 

  • — (1977): Geologie von Österreich. Band 1, Die Zentralalpen.— 766 p, Wien (Deuticke)

    Google Scholar 

  • Trauth, F. (1922): Über die Stellung der ‘pienidischen Klippenzone’ und die Entwicklung des Jura in den niederösterreichischen Voralpen.—Mitt. Geol. Ges. Wien,14/2, 105–265, Wien

    Google Scholar 

  • Tsien, H.H. (1979): Paleoecology of Algal-Bearing Facies in the Devonian (Couvinian to Frasnian) Reef Complexes of Belgium. —Palaegeogr., Palaeoclim., Palaeoecol.,27, 103–127, Amsterdam

    Article  Google Scholar 

  • Urlichs, M. (1971): Alter und Genese des Belemnitenschlachtfeldes im Toarcien von Franken.—Geol. BI. NO-Bayern,21, 65–83, Erlangen

    Google Scholar 

  • Vecsei, A., Frisch, W., Pirzer, M. &Wetzel, A. (1989): Origin and Tectonic Significance of Radiolarian Chert in the Austroalpine Rifted Continental Margin.—inHein, J.R. &Obradovic, J. (eds.): Siliceous Deposits of the Tethys and Pacific Regions.—65–80, New York (Springer)

    Google Scholar 

  • Walter, M.R., Awramik, S.M. (1979): Frutexites from stromatolites of the Gunflint Iron Formation of Canada, and its biological affinities.—Precambrian Research,9, 23–33, Amsterdam

    Article  Google Scholar 

  • Wendt, J. (1970): Stratigraphische Kondensation in triadischen und jurassischen Cephalopodenkalken der Tethys.—N. Jb. Geol. Pal. Mh.,1970, 433–449, Stuttgart

    Google Scholar 

  • Winterer, E.L. &Bosellini, A. (1981): Subsidence and sedimentation on Jurassic passive continental margin, Southern Alps, Italy.—Amer. Ass. Petrol. Geol., Bull.,65, 394–421, Tulsa

    Google Scholar 

  • Zeiss, A. (1984): The Lower Jurassic of Central and Southern Franconia.—Int. Symp. Jurassic Stratigr., Guide Book, 46–53, Erlangen

  • Ziegler, P.A. (1988): Evolution of the Arctic-North Atlantic and the Western Tethys.—Amer. Ass. Petrol. Geol., Mem.,43, 198 p, Tulsa

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  1. Institut für Paläontologie, Universität Erlangen, Loewenichstr. 28, D-91054, Erlangen

    Florian Böhm

  2. Institut für Geowissenschaften-Paläontologie, Universität Mainz, Saarstr. 21, D-55122, Mainz

    Thomas C. Brachert

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Böhm, F., Brachert, T.C. Deep-water stromatolites andFrutexites Maslov from the early and Middle Jurassic of S-Germany and Austria. Facies 28, 145–168 (1993). https://doi.org/10.1007/BF02539734

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