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Advances in Stromatolite Geobiology pp 409–434Cite as

Tolypammina gregaria Wendt 1969-Frutexites Assemblage and Ferromanganese Crusts: A Coupled Nutrient-Metal Interplay in the Carnian Sedimentary Condensed Record of Hallstatt Facies (Austria)

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Part of the book series: Lecture Notes in Earth Sciences ((LNEARTH,volume 131))

Abstract

Foraminifera are the most abundant sessile organisms found on ferromanganese crusts and nodules (Greenslate 1974; Wendt 1974; Dugolinsky et al. 1977; Riemann 1983; von Stackelberg 1984; Mullineaux 1987, 1988; Verlaan 1992; Resig and Glenn 1997; Toscano and Raspini 2005). In fact, actual ferromanganesecrusts and nodules share numerous similarities with their fossil counterparts.

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Acknowledgments

We thank to Jose Castillejo grant program from Universidad de Alcalá. This investigation was gratefully supported by the Deutsche Forschungsgemeinschaft Research Unit FOR 571 Geobiology of Organo- and Biofilms, publication no. 51.

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  1. Departamento de Geología, Universidad de Alcalá, Edificio de Ciencias, N-II Km 33.6, 28871, Alcalá de Henares, Madrid, España

    Marta Rodríguez-Martínez

  2. Geoscience Centre, University of Göttingen, Goldschmidtstraße 3, 37077, Göttingen, Germany

    Christine Heim, Klaus Simon, Thomas Zilla & Joachim Reitner

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Rodríguez-Martínez, M., Heim, C., Simon, K., Zilla, T., Reitner, J. (2011). Tolypammina gregaria Wendt 1969-Frutexites Assemblage and Ferromanganese Crusts: A Coupled Nutrient-Metal Interplay in the Carnian Sedimentary Condensed Record of Hallstatt Facies (Austria). In: Advances in Stromatolite Geobiology. Lecture Notes in Earth Sciences, vol 131. Springer, Berlin, Heidelberg. https://doi.org/10.1007/978-3-642-10415-2_25

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