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. © 2011 Springer Berlin Heidelberg.
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APA
Reitner, J., Quéric, N.-V., & Arp, G. (2011). Advances in Stromatolite Geobiology, 131, 187–205. https://doi.org/10.1007/978-3-642-10415-2
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