Pedogenic evidence sheds light on the post-Roman pedo-sedimentological and human history of Tarsus, the Roman capital of CE 60, Cilicia, Mersin, Türkiye

• Hydroxyapatite (hap) minerals forming in p accumulation horizon −chains of hap precipitating on weathered bone surface, • Is the p-rich horizon a phosphatic suffix π in wrb (2022), • Mortar fragments mixed wıth ash fibers indicate level of knowledge in technology, • Pedology of the pdms overlying the historical late Roman capital of Tarsus, Türkiye. The ancient city of Tarsus is underlying a sediment of 400 cm where the contemporary Tarsus grew. The diffusely stratified layers of the deposited sediment from the Kydnos (Tarsus) river overlying the Roman Road excavation site located in the heart of the modern city. The sediment is laden with technogenic materials. The profile of the stratigraphic layers represents a Pedocomplex (PDC) and its horizons are the Pedomembers (PDMs). All the PDMs were described and sampled for physical, chemical, mineralogical, micromorphological, and thermoluminescense analyses seeking pedogenic evidences. The origin of PDC materials is a fluvial and/or lagoon environment (archaeologically predicted date, about 60 CE , and they are calcareous, high in available P and some are high in total phosphorus contents). They have been partially modified by human activity in a settlement area, thus bringing some historical evidence suggesting that the site was part of the growing city after its abandonment. Thin sections show a vigorous biological degradation of the organic residues in the PDMs along with occasional evidence of soil-forming processes. The preliminary conclusions were extracted from the results obtained through the newly formed hydroxyapatite (Hap) determined by micromorphology, therefore proposing the new suffix π for the WRB soil naming system. Primary, high temperature and clay minerals together with TL analyses of the layers, were conducted to reveal the provenance and weathering phases of the horizons. The seeds recovered from an inhabited layer helped to interpret the food and medicinal habits of the local society and the contemporary presence of the lagoon.

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Journal
CATENA
Published
2024-11-20
DOI
https://doi.org/10.1016/j.catena.2024.108544
Primary Topic
Maritime and Coastal Archaeology
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article
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article

Pedogenic evidence sheds light on the post-Roman pedo-sedimentological and human history of Tarsus, the Roman capital of CE 60, Cilicia, Mersin, Türkiye

Franco Previtali, Enrico Casati, Süha Berberoğlu, Atike Nazik et al.
CATENA
Maritime and Coastal Archaeology
article

Pedogenic evidence sheds light on the post-Roman pedo-sedimentological and human history of Tarsus, the Roman capital of CE 60, Cilicia, Mersin, Türkiye

Franco Previtali, Enrico Casati, Süha Berberoğlu, Atike Nazik, Z. Yeḡingil, Osman Ahmet Polat, İrfan Özberk, Selım Kapur, Cenk Dönmez, Erhan Akça, Claudio Zucca, Ahmet Çilek, Muhsın Eren, Mehmet Z. Billor, Selahattın Kadır, Levent Zoroğlu, Alptekin Karagöz, Salvatore Madrau
article en

Abstract

• Hydroxyapatite (hap) minerals forming in p accumulation horizon −chains of hap precipitating on weathered bone surface, • Is the p-rich horizon a phosphatic suffix π in wrb (2022), • Mortar fragments mixed wıth ash fibers indicate level of knowledge in technology, • Pedology of the pdms overlying the historical late Roman capital of Tarsus, Türkiye. The ancient city of Tarsus is underlying a sediment of 400 cm where the contemporary Tarsus grew. The diffusely stratified layers of the deposited sediment from the Kydnos (Tarsus) river overlying the Roman Road excavation site located in the heart of the modern city. The sediment is laden with technogenic materials. The profile of the stratigraphic layers represents a Pedocomplex (PDC) and its horizons are the Pedomembers (PDMs). All the PDMs were described and sampled for physical, chemical, mineralogical, micromorphological, and thermoluminescense analyses seeking pedogenic evidences. The origin of PDC materials is a fluvial and/or lagoon environment (archaeologically predicted date, about 60 CE , and they are calcareous, high in available P and some are high in total phosphorus contents). They have been partially modified by human activity in a settlement area, thus bringing some historical evidence suggesting that the site was part of the growing city after its abandonment. Thin sections show a vigorous biological degradation of the organic residues in the PDMs along with occasional evidence of soil-forming processes. The preliminary conclusions were extracted from the results obtained through the newly formed hydroxyapatite (Hap) determined by micromorphology, therefore proposing the new suffix π for the WRB soil naming system. Primary, high temperature and clay minerals together with TL analyses of the layers, were conducted to reveal the provenance and weathering phases of the horizons. The seeds recovered from an inhabited layer helped to interpret the food and medicinal habits of the local society and the contemporary presence of the lagoon.

CATENAVol. 248
Aksaray University (TR), Selçuk University (TR), University of Turku (FI), University of Sassari (IT), Leibniz Centre for Agricultural Landscape Research (DE), Tarsus University (TR), Eskişehir Osmangazi University (TR), Mersin Üniversitesi (TR), Cukurova University (TR), University of Milano-Bicocca (IT), Harran University (TR), Auburn University (US)
Openalex Percentile: Top 64%
Maritime and Coastal Archaeology
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