Articular calcified cartilage canals in the third metacarpal bone of 2‐year‐old thoroughbred racehorses

We describe morphological aspects of the articular calcified cartilage mineralizing front ‘tidemark’ in the distal joint surface of the third metacarpal bone from 14 horses. Compositional backscattered electron scanning electron microscopy and confocal scanning light microscopy were conducted on polymethylmethacrylate (PMMA)‐embedded medio‐lateral slices. After maceration, scanning electron microscopy (SEM) was used to study the calcified cartilage surface in the ‘wedges’ intervening between the slices. An anatomically reproducible clustering of canals in the calcified cartilage was found at one site on the sagittal ridge in all the horses. The site is one that is relatively less loaded during joint function. These canals through calcified cartilage result from osteoclastic resorption (cutting cones) penetrating from bone through to the non‐mineralized hyaline articular cartilage. Their presence may indicate a pathway for connection between bone and cartilage extracellular fluid. In one horse, repair of such canals by plugging with new calcified cartilage was demonstrated. Differences in the degree of mineralization of regions of cartilage were seen in the combined compositional‐cum‐topographical backscattered SEM images of the macerated ‘tidemark’ front. More‐or‐less circular patches of lower mineralization density were frequently centred on (and may possibly originate from) canals. These microanatomical features should be searched for in other joints, at other ages and in other species to discover their frequency and significance.