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Currently the two main sources of Fulvic acid are alluvial soil and Shilajit. The difference between Shilajit based fulvic acid and alluvial soil derived fulvic acids lies in the core structures of the fulvic acids (FAs) in these compositions. Shilajit-Fulvic acids contains 3,8-oxygenated dibenzo-.alpha.-pyrone as the core nucleus. These upon repeated oxidation by nucleophile-containing oxygen, nitrogen and carbon ions, in association with various lipid moieties, produce a multiplayer micellar structure. In contrast, alluvial soil-Fulvic acids are composed essentially of aromatic hydroxy acids and polyphenols derived from phenolic oxidations. Both these Fulvic acids contain different metal ions, especially Fe, Co, Zn, Ca, etc., associated with the FAs. The metals in Shilajit-FAs are well-organized, multicentered, metal-ion associated products which, in the case of iron, maintains the metal in the reduced state and produce different iron-containing enzymes. Such trace ion-metal associations are not possible for soil-Fulvic acid because they have a much less organized heteropolycondensate structure whose micellar structure is irregular. Shilajit - the Himalayan mountain sourced one is available in a relatively pure environment in the high altitudes of snow capped Himalayan mountains. It has been formed over several thousands of years and is by far considered as the best source of fulvic ac
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