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Why did doctrinal religions first appear in the Northern Subtropical Zone?
1Department of Experimental Psychology, University of Oxford, Radcliffe Observatory Quarter, Oxford OX2 6GG, UK.
Neolithic religions emerged in the northern Subtropical Zone due to increased community sizes and ecological factors. This zone
Area of Science:
- Anthropology
- Archaeology
- Sociology
Background:
- Doctrinal religions with gods, theologies, moral codes, and priesthoods emerged during the Neolithic period.
- These religious developments were concentrated in a specific latitudinal band: the northern Subtropical Zone.
- Hunter-gatherer societies typically had smaller community sizes compared to Neolithic societies.
Purpose of the Study:
- To investigate the emergence of doctrinal religions during the Neolithic.
- To explore the geographical and environmental factors influencing the development of large-scale religions.
- To understand the role of religion in community bonding and cohesion in response to societal changes.
Main Methods:
- Analysis of the geographical distribution of early doctrinal religions.
- Examination of Neolithic environmental conditions, including rainfall patterns and pathogen load.
- Correlation of latitude with the development of religion and language in contemporary societies.
Main Results:
- Doctrinal religions emerged in two phases during the Neolithic, primarily in the northern Subtropical Zone.
- Optimal conditions for rapid population growth (ecological release) existed in this zone.
- The northern Subtropical Zone's characteristics favored the evolution of large-scale religions for community cohesion.
Conclusions:
- The emergence of Neolithic religions was driven by the need for community bonding amidst increasing population sizes (scalar stress).
- Specific environmental conditions in the northern Subtropical Zone facilitated rapid population growth and the development of complex religions.
- Latitude and environmental factors played a crucial role in the evolution of religion as a mechanism for social cohesion.
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