Fig. 10. Thin section of the tibia GPIT/RE/3724 of ornithopod dinosaur Dysalotosaurus lettowvorbecki Pompeckj, 1920, from Kimmeridgian, Late Jurassic of Tendaguru, Tanzania, cut within the lower third of the long bone shaft. Most of the marrow cavity is filled by fine, calcareous marl. Note that the top of the cavity has been filled subsequently by calcite crystals, which indicates that the bone was embedded in the substrate as oriented as in this image.

Published as part of Hübner, Tom R., Foth, Christian, Heinrich, Wolf-Dieter, Schwarz, Daniela & Bussert, Robert, 2021, Research history, taphonomy, and age structure of a mass accumulation of the ornithopod dinosaur Dysalotosaurus lettowvorbecki from the Upper Jurassic of Tanzania, pp. 275-300 in Acta Palaeontologica Polonica 66 (2) on page 285, DOI: 10.4202/app.00687.2019, http://zenodo.org/record/12196857