The fulvic mineral matrix inside B.E.N. Minerals comes from one of the rarest organic-origin mineral deposits of its type, naturally formed over millions of years. The deposit holds a dense concentration of mature fulvic micronutrients, naturally protected from environmental contamination by the geology that surrounds it.
Its formation reaches back tens of millions of years. Over that span, organic and mineral material accumulated, layer upon layer, in conditions that allowed slow transformation under stable pressure and undisturbed cycles. Prehistoric plant life once thrived there, drawing minerals and trace nutrients from deep below the surface. Repeated, undisturbed life cycles gradually transformed this environment into a nutrient-rich substrate, eventually giving rise to a concentrated spectrum of organic acid compounds.
The fulvic acid complex derived from this source has a mineral and organic acid composition that differs from fulvic materials commonly obtained from lignite, leonardite, or fermented peat. Its natural complexity is so specific that it cannot be artificially reproduced or reverse-engineered in a lab.
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