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Eimeria Leuckarti in Equid Coprolites From the Sassanid Era (2Nd–6Th Century Ce) Excavated in Chehrabad Salt Mine Archaeological Site, Iran Publisher Pubmed



Askari Z1 ; Sazmand A2 ; Mowlavi G1, 3 ; Ruehli F4 ; Naddaf SR5 ; Rezaeian M1 ; Stollner T6, 7 ; Aali A8 ; Paknezhad N1 ; Otranto D2, 9
Authors
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Authors Affiliations
  1. 1. Department of Parasitology and Mycology, School of Public Health, Tehran University of Medical Sciences, Tehran, Iran
  2. 2. Department of Pathobiology, Faculty of Veterinary Medicine, Bu-Ali Sina University, Hamedan, Iran
  3. 3. Center for Research of Endemic Parasites of Iran (CREPI), Tehran University of Medical Sciences, Tehran, Iran
  4. 4. Institute of Evolutionary Medicine, University of Zurich, Switzerland
  5. 5. Department of Parasitology, Pasteur Institute of Iran, Tehran, Iran
  6. 6. Ruhr-University Bochum, Institute for Archaeological Science, Bochum, Germany
  7. 7. German Mining Museum, Bochum, Germany
  8. 8. Archaeological Museum of Zanjan, Zanjan, Iran
  9. 9. Department of Veterinary Medicine, University of Bari, Bari, Valenzano, 70010, Italy

Source: International Journal of Paleopathology Published:2024


Abstract

Objective: This study reports coccidian oocysts in an equid coprolite dated to the Sassanid Empire (2nd–6th century CE) recovered in Chehrabad Salt Mine archaeological site, Iran. Methods: Between 2015 and 2017, an archaeoparasitological investigation led to the discovery of an equid coprolite in the Chehrabad Salt Mine archeological site, (Douzlakh), western Iran. Samples were rehydrated using trisodium phosphate solution and were examined by light microscopy. Results: Seven oocysts of Eimeria leuckarti (Flesch, 1883) were identified; they were in various stages of sporulation. Conclusion: This is the first report of ancient coccidian oocysts from equids. The importance of this observation is discussed, and current knowledge of eimeriid oocysts at archaeological sites is reviewed. Significance: The observations of E. leuckarti increases current knowledge of parasite biodiversity in ancient Iran when it rested along the Silk Road, a network of trade routes connecting the East and West that was central to economic, cultural, political, and religious interactions between these regions, and to livestock movement that could contribute to the transmission of the parasites from/to other regions. Limitations: The contextual information about animal species present in and around the Salt Mine during its working periods, including Achaemenid dynasty (6th to 4th century BCE) and Sassanid era (2nd to 6th century CE), is very limited and does not allow secure conclusions regarding the host origin of the coprolites. Suggestions for Further Research: Application of molecular biology tools to identify the correct host origin of the coprolites and to detect more parasite species is advocated. © 2023 Elsevier Inc.