Scientific analysis of a calcified object from a post-medieval burial in Vienna, Austria

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Abstract

Calcifications commonly occur in association with soft tissue inflammation. However, they are not often discussed in palaeopathological literature, frequently due to problems of identification and diagnosis. We present a calcified object (40 × 27 × 27 cm) found with a middle-aged male from a post-medieval cemetery in Vienna. It was not recognized during excavation, thus its anatomical location within the body remains unknown.

The object was subject to X-ray, SEM and CT scanning and compared to historic pathological objects held in the collection of the Natural History Museum Vienna. Two of closest resemblance, a thyroid adenoma and goitre were subject to similar analytical techniques for comparison. Despite similarities between all objects, the structure of the object most closely conforms to a thyroid tumor. Nevertheless, due to similar pathophysiological pathways and biochemical composition of calcified soft tissue, a secure identification outside of its anatomical context is not possible.

The research further highlights the fact that recognition of such objects during excavation is crucial for a more conclusive diagnosis. Historic medical records indicate that they were common and might therefore be expected to frequently occur in cemeteries. Consequently, an increasing the dataset of calcifications would also aid in extending the knowledge about diseases in past human populations.

Introduction

Despite the relatively common occurrence of pathological calcifications in modern clinical contexts (Black and Kanat, 1985), in the palaeopathological literature such objects are only occasionally reported for archaeological human skeletal remains. In addition, in most cases the identification of these structures remains tentative. Calcifications in the human body can result from a large number of different pathological conditions including vascular, infectious, inflammatory, metabolic, and neoplastic entities (see Table 1) and can occur in virtually all anatomical regions of the body (Banks et al., 2005; Bohndorf et al., 2006: 288). Patho-physiologically, they are classified into organic concretions and calcifications of pathological lesions in soft tissue. Soft tissue calcifications are further subdivided into dystrophic, accounting for 93–95% of all observed cases, and metastatic, which are generally rare (Banks et al., 2005, Kumar et al., 2013a). Metastatic forms occur in living tissue and are always related to an imbalance of the mineral metabolism, whereby dystrophic forms arise from necrotic tissue and do not involve any metabolic changes (Bohndorf et al., 2006: 288). While metastatic calcifications are usually associated with significant morbidity and mortality, dystrophic calcifications are often asymptomatic and relatively common. In a large-scale roentgenological study carried out in the central US in the 1940s, 63% of patients were found to have calcifications in the thoracic cavity resulting from atherosclerosis, silicosis or infectious diseases such as histoplasmosis, tuberculosis or other parasitic infections (Felson, 1969).

In the palaeopathological literature, several different types of calcified structures have been reported dating back as far as the Neolithic period, including parasite cysts (e.g. Perry et al., 2008, Waters-Rist et al., 2014), tumorous calcifications (e.g. Strouhal and Jungwirth, 1977, Komar and Buikstra, 2003, Quintelier, 2009), vascular calcifications (Binder and Roberts, 2014) as well as organic concretions (e.g. Özdemir et al., 2013). However, specific identifications are often impossible due to the wide range of potential underlying causes and unspecific morphology of the objects. Furthermore the lesions develop through similar underlying pathophysiological mechanisms and the biochemical composition of most soft tissue calcifications is indistinguishable from bone (Baud and Kramar, 1991). This paper reports the finding of an ovoid calcified object (40 × 27 × 27 mm, Fig. 1) of unknown origin in the burial of a middle adult male individual (Fig. 2) from the post-medieval cemetery of St.-Bartholomäus-Platz in Vienna, Austria.

Section snippets

Materials & methods

St. Bartholomäus church is located in the northern part of Vienna, which was once a small village until its integration into the municipality in the 19th century. The large cemetery surrounding the church was in use between the 15th and 18th centuries. Parish records indicate that the church belonged to an increasingly urbanised community living at the outskirts of the expanding city and comprised peasants, craftsmen, traders, servants and soldiers. Parts of the cemetery were excavated in 2007

Results

The ovoid calcified object is 40 × 27 × 27 mm in size and is composed of a very dense, hard, yellow substance (Fig. 1). Radiographic (Fig. 4a) and CT-examination (Fig. 4b) of the structure revealed a smooth-walled, ovoid lobe with a hollow space, comprising one third of the object. The remaining part of the object constitutes an irregular network of a calcified substance with a spiky irregular surface and numerous irregular hollow spaces. While the hollow space potentially represents a liquid-filled

Discussion

Based on the X-ray and CT-scan results, several types of pathological calcifications can be excluded as potential differential diagnostic options and these are summarized in Table 2. Consequently, an identification of the object as dystrophic calcification seems most likely, however, as these can occur in virtually all forms of necrotic soft tissue lesions, again several possible origins have to be taken into account.

Shape, size and internal structure suggest that the object represents a

Conclusion

Macroscopic, radiographic and comparative studies of the calcified object from St. Bartholomäus-Platz suggest that it most likely represents a calcified soft tissue tumor. Although both size and morphological features of the calcified object are consistent with a calcified thyroid adenoma or goitre, it is not possible to reach a more conclusive diagnosis based on macroscopic and radiographic investigation alone, given the wide range of possible areas of origin. Nevertheless, this research

Acknowledgements

The authors would like to thanks K. Fischer-Ausserer (Stadtarchäologie Wien) for permission to analyse the material., S. Kneissl (Veterinary University, Vienna) for access to X-ray and CT scan facilities and K. Neufeld (NHM Wien) for assistance with the SEM. Thanks are also due to the Vienna Institute for Archaeological Science (VIAS) for access to the SEM. Object photographs were provided by W. Reichmann (NHM Wien). T. Jakob (Department of Archaeology, Durham University), K. Plomp (Department

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