Journals / International Journal of Social Sciences and Education Research / 2023 / Cilt: 9 Sayı: 2

The role of climate changes in the intensification of agricultural activities in Anatolia during the late Roman-early Byzantine period

Pages
168–178
Publication Date
2023-06-30
DOI
—
🏛️Bibliographic metadata and full text access for this article are provided via DergiPark.
DergiPark Record ↗
✨

AI Summary & Key Takeaways

AI Insight
⚡ TL;DR(Too Long; Didn't Read)

However, cold and arid climatic conditions did not permanently and continuously affect agricultural activities and society, even though they may have caused temporary crises.

📌 3 Key Takeaways

🎯
Objective & Hypothesis:The intensive agricultural period called the Beyşehir Occupation Phase (BOP) in Anatolia peaked during the Late Roman and Early Byzantine Periods.
📊
Key Findings & Data:The findings suggest that favorable climatic conditions significantly contributed to the expansion of societies and the intensification of agricultural activities in general.
💡
Conclusion & Impact:However, cold and arid climatic conditions did not permanently and continuously affect agricultural activities and society, even though they may have caused temporary crises.
🔬Design:Research Article
📍Scope:Comprehensive Sample
⚙️Variables:Anatolia · Pollen · Paleoclimate

Abstract

The intensive agricultural period called the Beyşehir Occupation Phase (BOP) in Anatolia peaked during the Late Roman and Early Byzantine Periods. This study investigates whether climatic changes during this period influenced the intensification of agricultural activities. By evaluating pollen studies in Anatolia, the characteristics of agricultural activities were determined and compared with historical, archaeological, and paleoclimatic data to explore the relationship between BOP, climatic changes, and their impact on agricultural activities and social structures. The findings suggest that favorable climatic conditions significantly contributed to the expansion of societies and the intensification of agricultural activities in general. However, cold and arid climatic conditions did not permanently and continuously affect agricultural activities and society, even though they may have caused temporary crises.

🔖

Cite This Article

ÖREN, A. (2023). The role of climate changes in the intensification of agricultural activities in Anatolia during the late Roman-early Byzantine period. International Journal of Social Sciences and Education Research, Cilt: 9 Sayı: 2, 168–178. https://ajindex.com/articles/949821

📄 Full Text PDF Viewer

📄

PDF görüntüleyici hazırlanıyor...

References (12)

  1. Arjava, A. (2005). The Mystery Cloud of 536 CE in the Mediterranean Sources. Dumbart Oaks Pap., 59, 73–94. https://doi.org/10.2307/4128751
  2. Bakker, J., Paulissen, E., Kaniewski, D., Poblome, J., De Laet, V., Verstraeten, G., & Waelkens, M. (2013). Climate, people, fire and vegetation: new insights into vegetation dynamics in the Eastern Mediterranean since the 1st century AD. Climate of the Past, 9(1), 57-87. https://doi.org/10.5194/cpd-8-3379-2012
  3. Baillie, M. G. L. (1994). Dendrochronology raises questions about the nature of the AD 536 dust-veil event. Holocene, 4, 212-217. https://doi.org/10.1177/095968369400400211
  4. Banaji, J. (2007). Agrarian Change in Late Antiquity: Gold, Labour, and Aristocratic Dominance, Oxford Classical Monographs. Oxford: Oxford University Press.
  5. Behre, K. E. (1990). Some reflections on anthropogenic indicators and the record of prehistoric occupation phases in pollen diagrams from the Near East. In S. Bottema, G. Entjes-Nieborg, & W. van Zeist (Eds.), Man's Role in the Shaping of the Eastern Mediterranean Landscape (219-230). Rotterdam: A. A. Balkema. Bell, M., & Walker, M. J. C. (1992). Late Quaternary Environmental Change: Physical and human perspectives. Harlow: Longman Group UK Limited. https://doi.org/10.1016/0277-3791(93)90031-g
  6. Besonen, M. R., & Roosevelt, C. H. (2015). Late Holocene Climate in Central Western Turkey-evidence for a Period of Exceptional Aridity in the Mid-First Millennium AD. Birks, H. J. B. (1990). Indicator values of pollen types from post-6000 B.P. pollen assemblages from southern England and southern Sweden. Quaternary Studies in Poland, 10, 21-31.
  7. Bottema, S., & Woldring, H. (1984). Late Quaternary vegetation and climate of Southwestern Turkey. Part II. Palaeohistoria, 26, 123-149.
  8. Bottema, S., Woldring, H., & Aytuğ, B. (1986). Palynological investigations on the relations between prehistoric man and vegetation in Turkey: The Beyşehir Occupation Phase. In H. Demiriz, & N. Özhatay (Eds.), Proceedings of the 5th Optima Congress (315-328). September, 1986,
  9. İstanbul.
  10. Bottema, S., Woldring, H., & Aytuğ, B. (1993-1994). Late Quaternary vegetation history of northern Turkey. Palaeohistoria, 35/36, 13-72.
  11. Brewer, S., Guiot, J., & Barboni, D. (2007). Pollen data as climate proxies. In S. Elias (Eds.), Encyclopedia of Quaternary Sciences, vol. 3. Elsevier, Oxford, pp. 2498-2510.
  12. Brown, N. (1994). Climate Change and Human History. Some Indications from Europe, AD 400–1400. Environmental Pollution, 83, 37–43. htt