The third, which lies far out in the Mediterranean, and which is possibly the oldest, is much higher in Na₂O and seems to be characterized by the presence of peculiar soda minerals, such as ænigmatite and ægirine, nepheline also occurring in places.

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Autofluorescence was observed mostly in epidermis cell walls, trichromes and vascular bundles, while it was very low in parenchymatic cells (Fig 4, control panels).

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