Cc. Grant et al., DEMARCATION OF POTENTIALLY MINERAL-DEFICIENT AREAS IN CENTRAL AND NORTHERN NAMIBIA BY MEANS OF NATURAL CLASSIFICATION SYSTEMS, Onderstepoort journal of veterinary research, 63(2), 1996, pp. 109-120
Mineral deficiencies that lead to production losses often occur concur
rently with climatic and management changes. To diagnose these deficie
ncies in time to prevent production losses, long-term monitoring of mi
neral status is advisable. Different classification systems were exami
ned to determine whether areas of possible mineral deficiencies could
be identified, so that those which were promising could then be select
ed for further monitoring purposes. The classification systems address
ed differences in soil, vegetation and geology, and were used to defin
e the cattle-ranching areas in the central and northern districts of N
amibia. Copper (Cu), iron (Fe), zinc (Zn), manganese (Mn) and cobalt (
Co) concentrations were determined in cattle livers collected at abatt
oirs. Pooled faecal grab samples and milk samples were collected by fa
rmers, and used to determine phosphorus (P) and calcium (Ca), and iodi
ne (I) status, respectively. Areas of low P concentrations could be id
entified by all classification systems. The lowest P concentrations we
re recorded in samples from the Kalahari-sand area, whereas faecal sam
ples collected from cattle on farms in the more arid areas, where the
harder soils are mostly found, rarely showed low P concentrations. In
the north of the country, low iodine levels were found in milk samples
collected from cows grazing on farms in the northern Kalahari broad-l
eaved woodland. Areas supporting animals with marginal Cu status, coul
d be effectively identified by the detailed soil-classification system
of irrigation potential. Copper concentrations were lowest in areas o
f arid soils, but no indication of Co, Fe, Zn, or Mn deficiencies were
found. For most minerals, the geological classification was the best
single indicator of areas of lower concentrations. Significant monthly
variation for all minerals could also be detected within the classifi
cation system. It is concluded that specific classification systems ca
n be useful as indicators of areas with lower mineral concentrations o
r possible deficiencies.