Porotic lesions of immature skeletons have been attracting scientific attention for more than a century. These changes have been documented worldwide and are considered to be one of the indicators of health and/or nutritional status of past human populations. These lesions have frequently been referred to as a nutritional stress indicator, a manifestation of iron-deficiency anaemia, and a condition caused by chronic infections. In this study, 327 immature skeletons from the medieval graveyard of Stara Torina (Serbia) were examined for macroscopic signs of four types of porotic lesions: cribra orbitalia, femoral cribra, humeral cribra, and porotic hyperostosis. Femoral cribra was observed in 83.25% of femora, humeral cribra in 58.46% of cases, cribra orbitalia in 46.12% of orbits, while porotic hyperostosis was recorded in only 2.94% of skulls. The majority of skeletons affected by cribra presented symmetrical lesions. Association between all types of cribra was recorded in 33.33% of skeletons. Historical data supported the hypothesis that the investigated population was exposed to frequent infections, especially parasitic ones, which led to the development of porotic bone lesions via several mechanisms: parasite-induced blood loss and diarrhoea (both iron and magnesium malabsorption) or anaemia as a hepcidin-mediated body adaptive response to infection.