Young developing soybean seeds contain relatively large amounts of calcium
oxalate (CaOx) monohydrate crystals. A test for Ca and CaOx indicated that
Ca deposits and crystals initially occurred in the funiculus, where a singl
e vascular bundle enters the seed. Crystals formed in the integuments until
the embryo enlarged enough to crush the inner portion of the inner integum
ent. Crystals then appeared in the developing cotyledon tissues and embryo
axis. All crystals formed in cell vacuoles. Dense bodies and membrane compl
exes were evident in the funiculus. In the inner integument, cell vacuoles
assumed the shape of the future crystals. This presumed predetermined cryst
al mould is reported here for the first time for soybean seeds, As crystals
in each tissue near maturity, a wall forms around each crystal. This intra
cellular crystal wall becomes contiguous with the cell wall. Integument cry
stals remain visible until the enlarging embryo crushes the integuments; th
e crystals then disappear. A related study revealed that the highest percen
t of oxalate by dry mass was reached in the developing + 16 d (post-fertili
zation) seeds. and then decreased during late seed maturation. At +60 d, Ca
Ox formation and disappearance are an integral part of developing soybean s
eeds. Our results suggest that Ca deposits and crystals functionally serve
as Ca storage for the rapidly enlarging embryos. The oxalate, derived from
one or more possible metabolic pathways, could be involved in see storage p
rotein synthesis. (C) 2001 Annals of Botany Company.