Translations:Benutzer:Arian/Klett-Mini-Test/1446/en

Aus BiodynWiki

Just as the fully formed blossom dies into form and colour and into the volatilising fragrance substances, so does the leaf-and-shoot growth of the oak die into the outer bark. In it, everything that was formerly lived through becomes rigid, dead form; what was green becomes earth-brown and reddish, and what was bound in readily volatile aromatic substances has drifted away. Seen thus, there completes itself in the outer bark a sulphurisation process — a flowering process still close to earth and unfinished. The substances have not yet been entirely lifted free of their physical lawfulness. Calcium, however — raised up into the life of the plant — enters into a bond with the sulphurous oxalic acid that has arisen from this life. It crystallises into calcium oxalate in various crystal forms: rhombohedral, rod- and needle-shaped, or octahedral in double pyramids. One distinguishes crystal sand, individual crystals, twins, druses, and spherites.[1] The oxalic lime (calcium oxalate) arises in the cell plasma. In their early stage the crystals are always enclosed by a plasmatic sheath, which in the outer bark ripens and dies away. What remains in the outer bark of the manifold substance-compositions of the bark are sparingly volatile hydrocarbons and the calcium oxalate crystals. In the latter, the calcium is present in a structure that has received its impress from the living context of the oak. Life has withdrawn from the outer bark; the astral, however — which created this structure (form) — remains bound to the physical-material, and so too to the

  1. Hermann von Guttenberg: Lehrbuch der allgemeinen Botanik, Berlin 1952, 641 S.