M. Trockenbrodt, CALCIUM-OXALATE CRYSTALS IN THE BARK OF QUERCUS-ROBUR, ULMUS-GLABRA, POPULUS-TREMULA AND BETULA-PENDULA, Annals of botany, 75(3), 1995, pp. 281-284
Barks of different developmental stages of oak (Quercus robur L.), elm
(Ulmus glabra Huds.), poplar (Populus tremula I,.) and birch (Betula
pendula Roth) were analysed with regard to the variability of presence
, type, location, dimension, and quantity of calcium oxalate crystals.
Solitary crystals were present in all bark samples. In oak and poplar
they were located in thick-walled, chambered, lignified cells adjacen
t to fibre groups and in sclereids. In birch they were mostly present
in sclereids and occasionally in axial phloem parenchyma cells. In elm
, thin-walled, chambered axial phloem parenchyma cells contained solit
ary crystals. Druses were present in oak, poplar and birch, but not in
elm. They were located in thin-walled, chambered axial phloem parench
yma cells in the vicinity of the Vascular cambium, in axial phloem par
enchyma cells of the secondary phloem and in cortical cells. Presence,
type and location of bark crystals did not vary between bark samples
of different age. Therefore, these bark crystal. characteristics may f
orm reliable features for a diagnostic description of the barks invest
igated. The dimensions and quantity of bark crystals varied considerab
ly and may not serve as diagnostic features.