Rodríguez Martínez, MartaHeim, ChristineSimon, KlausZilla, ThomasReitner, JoachimReitner, JoachimQuéric, Nadia-ValérieArp, GernotTrauth, M. H.Stüwe, K.Yuen, D.Friedman, G. M.Seilacher, A.2023-06-202023-06-202010-12-03978-3-642-10414-510.1007/978-3-642-10415-2https://hdl.handle.net/20.500.14352/45787© Springer-Verlag Berlin Heidelberg 2011Foraminifera 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.engbook parthttps://doi.org/10.1007/978-3-642-10415-2https://link.springer.com/restricted access56:593.12(436)"622.262"563.12(436)"622.262"669.15'74-198(436)"622.262"Rare earth element patternFerromanganese crustRare earth elementFerromanganese noduleBioclastic debrisPaleontologíaMetalurgia2416 Paleontología2211.21 Metalurgia