

A review of the literature showed that plants grown with organic fertilizers often contain higher concentrations of vitamins B₁ (thiamin) and B₁₂ (cyanocobalamin) as compared with plants grown with inorganic fertilizers. Since plant roots were recently shown to be able to absorb B₁ and B₁₂, it was thus suspected that organic fertilizers (such as manure of diverse sources or sewage sludges which often contain relatively high concentrations of several vitamins) introduce additional vitamins into the soil which in turn leads to increased vitamins in the plants. This possibility was studied by measuring the B₁₂ content in the seeds of soybean and barley and in the leaves of spinach plants grown in soils amended with pure B₁₂ or cow dung (which is naturally rich in B₁₂). The addition of pure B₁₂ or cow dung did not alter the B₁₂ content in the soybean seeds but significantly increased that in the barley kernels and in the spinach leaves. For example, the addition of cow dung at the rate of 10 g kg⁻¹ increased the B₁₂ content in barley kernels by more than threefold (from 2.6 to 9.1 ng g⁻¹ DW) and in spinach leaves by close to twofold (from 6.9 to 17.8 ng g⁻¹ DW). Long-term addition of organic fertilizers to the soil also significantly increased the soil content of this vitamin. Since plants cannot synthesize B₁₂ and thus plant foods are normally fully devoid of (or have very low concentrations of) this vitamin, the finding that plants grown with organic fertilizers may contain relatively higher concentrations of this vitamin may have nutritional consequences in that the consumption of these plants by humans would inadvertently increase their intake of this vitamin. This may be of special benefit to people living by choice or by necessity on strict vegetarian diets who are known to be in danger of B₁₂ deficiency.
Plant and Soil publishes original papers and review articles exploring the interface of plant biology and soil sciences, and offering a clear mechanistic component. This includes both fundamental and applied aspects of mineral nutrition, plant-water relations, symbiotic and pathogenic plant-microbe interactions, root anatomy and morphology, soil biology, ecology, agrochemistry and agrophysics. Articles discussing a major molecular or mathematical component also fall within the scope of the journal.
Springer is one of the leading international scientific publishing companies, publishing over 1,200 journals and more than 3,000 new books annually, covering a wide range of subjects including biomedicine and the life sciences, clinical medicine, physics, engineering, mathematics, computer sciences, and economics.
This item is part of a JSTOR Collection.
For terms and use, please refer to our
Plant and Soil © 1994 Springer Nature