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Rivas-Lamelo et al. Magnetotactic bacteria as a new model for P sequestration in the ferruginous Lake Pavin Figure 1 Scanning transmission electron microscopy.

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Presentation on theme: "Rivas-Lamelo et al. Magnetotactic bacteria as a new model for P sequestration in the ferruginous Lake Pavin Figure 1 Scanning transmission electron microscopy."— Presentation transcript:

1 Rivas-Lamelo et al. Magnetotactic bacteria as a new model for P sequestration in the ferruginous Lake Pavin Figure 1 Scanning transmission electron microscopy analyses of MTB cells at the oxic-anoxic interface in Lake Pavin. Top: STEM-HAADF image showing a cluster of MTB cells. Magnetites are the brightest particles. Some cells contain two or four magnetite chains; some (bottom left) contain scattered magnetite. Polyphosphates appear as bright granules filling completely some of the cells (e.g., arrows). Bottom: EDXS maps. Figure 1 Scanning transmission electron microscopy analyses of MTB cells at the oxic-anoxic interface in Lake Pavin. Top: STEM-HAADF image showing a cluster of MTB cells. Magnetites are the brightest particles. Some cells contain two or four magnetite chains; some (bottom left) contain scattered magnetite. Polyphosphates appear as bright granules filling completely some of the cells (e.g., arrows). Bottom: EDXS maps. Rivas-Lamelo et al. (2017) Geochem. Persp. Let. 5, | doi: /geochemlet.1743 © 2017 European Association of Geochemistry

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