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  • Monty, C.

    Erscheinungsdatum: 1981

    Anbieter: Literaturhökerei Wiese, Hardegsen, Deutschland

    Bewertung: 4 Sterne, Learn more about seller ratings

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    Anzahl: 1

    In den Warenkorb

    Springer-Verlag Berlin etc.: 249pp, 121 figs, 10 pls 8vo, hardback, ex libr. copy, some labels on the back but inside clean and overall good cond.

  • C. Monty

    Verlag: Springer Berlin Heidelberg, 2011

    ISBN 10: 3642679153ISBN 13: 9783642679155

    Anbieter: AHA-BUCH GmbH, Einbeck, Deutschland

    Bewertung: 5 Sterne, Learn more about seller ratings

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    Buch

    EUR 32,99 Versand

    Von Deutschland nach USA

    Anzahl: 1

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    Taschenbuch. Zustand: Neu. Druck auf Anfrage Neuware - Printed after ordering - During the 2nd International Symposium on Fossil Algae, organized by the University P. & M. Curie, Paris, in April 1979, a special session was devoted to stromatolites; 29 papers were presented in French, English, or Russian. Among the papers selected originally, 16 were carried out to the final stage by their authors. They are presented here in their stratigraphical order. This selection does not pretend to cover the problem of Phanerozoic stromatolites in its entirety, but relates case histories. This should be the seed for further books analyzing and illus trating the paleoecology, the niche and the features of Phanerozoic stromatolites, namely throughout the Mesozoic and the Paleozoic, where the data are still scarce; this will lead to naturalistic views on the evolutionary features of Post Riphean stromes, and will sharpen tools to interpret their Precambrian ancestors. Let me introduce the papers. CLAUDE L. V. MONTY formalizes two basic types of crypt algal micro structures: the spongiostromate and the porostromate microstructures respectively; the rise of the latter around the Precambrian/Cambrian boundary represents a very significant step in the evolution of cyano bacterial microstructures and in their interaction with the environment. K. K. VERMA and G. BARMAN present a lower Phanerozoic stroma tolitic assemblage from Rajasthan associated with paralic alluvial fans fed by block faulting. Main stromatolite developments occurred during periods of low sedimentation and negligable tectonics, and formed in very shallow marine water. J.