Neoproterozoic trace fossils vs. microbial mat structures: Examples from the Tandilia Belt of Argentina

[1]  N. Noffke.  Microbially induced sedimentary structures in Archean sandstones: A new window into early life , 2007 .

[2]  S. Jensen,et al.  Trace fossil preservation and the early evolution of animals , 2005 .

[3]  N. Noffke,et al.  Benthic cyanobacteria and their influence on the sedimentary dynamics of peritidal depositional systems (siliciclastic, evaporitic salty, and evaporitic carbonatic) , 2003 .

[4]  D. Poiré,et al.  The Cambrian-Ordovician siliciclastic platform of the Balcarce Formation (Tandilia System, Argentina): Facies, trace fossils, palaeoenvironments and sequence stratigraphy , 2003 .

[5]  J. Stolz.  Structure of Marine Biofilms , 2003 .

[6]  G. Zavarzin,et al.  Fossil and Recent Biofilms , 2003 .

[7]  M. Kühl,et al.  GROWTH, STRUCTURE AND CALCIFICATION POTENTIAL OF AN ARTIFICIAL CYANOBACTERIAL MAT , 2003 .

[8]  H. Porada,et al.  Mat-related sedimentary structures in Neoproterozoic peritidal passive margin deposits of the West African Craton (Anti-Atlas, Morocco) , 2002 .

[9]  Wolfgang E. Krumbein,et al.  Microbially Induced Sedimentary Structures: A New Category within the Classification of Primary Sedimentary Structures , 2001 .

[10]  W. Krumbein,et al.  Microbially induced sedimentary structures indicating climatological, Hydrological and depositional conditions within recent and pleistocene coastal facies zones (Southern Tunisia) , 2001 .

[11]  J. Banner,et al.  Evolution of the Sr and C Isotope Composition of Cambrian Oceans , 2000 .

[12]  D. Bottjer,et al.  The Cambrian Substrate Revolution , 2000 .

[13]  N. Noffke,et al.  Microbial signatures in peritidal siliciclastic sediments: a catalogue , 2000 .

[14]  S. Jensen,et al.  Complex trace fossils from the terminal Proterozoic of Namibia , 2000 .

[15]  H. Porada,et al.  Microbial shrinkage cracks in siliciclastic rocks of the Neoproterozoic Nosib Group (Damara Supergroup) of central Namibia , 2000 .

[16]  D. Bottjer,et al.  Restriction of a late Neoproterozoic biotope; suspect-microbial structures and trace fossils at the Vendian-Cambrian transition , 1999 .

[17]  A. Seilacher.  Biomat-related lifestyles in the Precambrian , 1999 .

[18]  David M. Paterson,et al.  Biostabilization of Sediments , 1994 .

[19]  S. Donovan.  The palaeobiology of trace fossils , 1994 .

[20]  H. Gemerden.  Microbial mats: A joint venture , 1993 .

[21]  T. Crimes.  The Record of Trace Fossils across the Proterozoic—Cambrian Boundary , 1992 .

[22]  J. Lipps,et al.  The Origin and Early Evolution of Metazoa , 1992 .

[23]  P. A. Cross,et al.  Lecture notes in Earth sciences: Vol. 12. S. Turner (Editor), Applied Geodesy VIII, Springer, Berlin, F.R.G., 1987, 393pp, DM78.00, ISBN 3 540 182195 , 1989 .

[24]  D. Bottjer,et al.  Trends in depth and extent of bioturbation in Cambrian carbonate marine environments, western United States , 1988 .

[25]  C. Cingolani,et al.  Resultados geocronológicos en niveles pelíticos intercalados en las dolomias de Sierras Bayas [Grupo La Tinta], provincia de Buenos Aires , 1988 .

[26]  Daniel Poiré.  Mineralogía y sedimentología de la formación Sierras Bayas en el núcleo septentrional de las sierras homónimas, partido de Olavarría, provincia de Buenos Aires , 1987 .

[27]  A. M. Killick.  A preliminary account of the geology of the Kamtsas formation of the Damara sequence, eastern Gobabis district, South West Africa/Namibia , 1983 .

[28]  R. Park.  The preservation potential of some recent stromatolites , 1977 .

[29]  A. Gunatilaka.  Some aspects of the biology and sedimentology of laminated algal mats from mannar lagoon, Northwest Ceylon , 1975 .

[30]  F. Young.  Early Cambrian and Older Trace Fossils from the Southern Cordillera of Canada , 1972 .

[31]  M. Glaessner.  TRACE FOSSILS FROM THE PRECAMBRIAN AND BASAL CAMBRIAN , 1969 .

[32]  D. J. McLaren,et al.  Possible Metazoans from the Early Proterozoic of the Canadian Shield , 1963, Nature.