Synchrotron-µ-XRF maps showing Fe (red) and Mn (green) distributions in (a) discoidal, (b) crust, and (c) spheroidal concretions from the Baltic Sea. The white scale bars equal 500 µm. Original reference: Wasiljeff et al. 2025: Mineral phases and growth conditions of morphologically diverse shelfal ferromanganese concretions. Geochimica et Cosmochimica Acta 400, 227–247, https://doi.org/10.1016/j.gca.2025.05.012
🧪New article on the mineralogy of Baltic Sea #ferromanganese concretions
🌊Mn layers are birnessite with microbially-mediated dendritic texture. Fe layers are ferrihydrite with admixed detrital grains; the layers remain after the dissolution of birnessite.
RCF #Fermaid project
doi.org/10.1016/j.gc...