Da. Reid et al., Mineral nutrition in white spruce (Picea glauca [Moench] Voss) seeds and somatic embryos; II. EDX analysis of globoids and Fe-rich particles, PLANT SCI, 141(1), 1999, pp. 19-27
The elemental compositions of globoids and Fe-rich particles were investiga
ted in white spruce (Picea glauca [Moench] Voss) somatic embryos, zygotic e
mbryos and female gametophytes using energy dispersive X-ray analysis. Glob
oids, phytate deposits in seed protein bodies, were found throughout the fe
male gametophyte of seeds and in the ground meristem and procambium from al
l regions of both somatic and zygotic embryos. Iron-rich particles, believe
d to be Fe-associated phytate deposits in seed proplastids, were found thro
ughout the female gametophyte of seeds and in the protoderm, ground meriste
m, and procambium from all regions of both somatic and zygotic embryos, Glo
boids in somatic and zygotic embryos ranged from 0.5-3.0 mu m in diameter,
but globoids typically ranged from 1.5-2.0 mu m in diameter in somatic embr
yos and from 2.0-3.0 mu m in diameter in zygotic embryos. Globoids in femal
e gametophyte tissue ranged from 0.5-6.0 mu m in diameter. All Fe-rich part
icles studied from somatic embryos and from seeds ranged from 0.14-0.25 mu
m in diameter. Globoids in somatic embryos and seeds contained high P, mode
rate K and Mg with occasional traces of Fe and little if any Ca and Zn. Glo
boids in the zygotic embryo cotyledon procambium tissue also contained mode
rate levels of Fe and had significantly higher Fe:P ratios, which were not
found in any other regions in seeds or in somatic embryos. Iron-rich partic
les in somatic embryos and seeds contained high P and Fe, moderate K and Mg
, and little if any Ca and Zn. Typically, spectra of Fe-rich particles in s
omatic embryos had P peaks higher than Fe peaks and spectra of Fe-rich part
icles in seeds had P peaks lower than Fe peaks. Overall, the composition of
globoids and Fe-rich particles in somatic embryos and zygotic embryos were
very similar with only minimal differences found. (C) 1999 Elsevier Scienc
e Ireland Ltd. All rights reserved.