“…where Y ST i is the number of thousand years elapsed since the Neolithic Revolution in country i, as reported by Putterman (2008); V OL i is the temperature volatility prevalent in country i during either the contemporary or the historical (1500-1900) time horizon; T M EAN i is the mean temperature (in degrees Celsius) of country i during the corresponding time period; LDIST i is the log of the great-circle distance (in kilometers) to the closest Neolithic frontier, included here as a control for the timing of the arrival of agricultural practices via spatial technological di¤usion from the frontier; 13 LAT i is the absolute latitude (in degrees) of the geodesic centroid of country i, as reported by the CIA World Factbook ; AREA i is the total land area (in millions of square kilometers) of country i, as reported by the World Bank's World Development Indicators; 14 i is a vector of continental dummies; i is a vector of biogeographic variables employed by the study of Olsson and Hibbs (2005), such as climate, the size and geographic orientation of the landmass, and the numbers of prehistoric domesticable species of plants and animals, included here as controls for the impact of biogeographic endowments as hypothesized by Diamond (1997); and, …nally, " i is a country-speci…c disturbance term. 15 To …x priors, the reduced-form prediction of the theory -i.e., that intermediate levels of climatic volatility should be associated with an earlier adoption of agriculture -implies that, in the context of the regression speci…cation, the timing of the Neolithic Revolution, Y ST i , and temperature volatility, V OL i , should be characterized by a hump-shaped relationship across countries -i.e., 1 > 0, 2 < 0, and V OL = 1 = (2 2 ) 2 V OL min ; V OL max .…”