De Dreu Carsten K W, van Dijk Mathijs A
Institute of Psychology, Leiden University, Leiden, The Netherlands.
Center for Experimental Economics and Political Decision Making, University of Amsterdam, Amsterdam, The Netherlands.
PLoS One. 2018 Jan 24;13(1):e0190122. doi: 10.1371/journal.pone.0190122. eCollection 2018.
Human history is shaped by landmark discoveries in science and technology. However, across both time and space the rate of innovation is erratic: Periods of relative inertia alternate with bursts of creative science and rapid cascades of technological innovations. While the origins of the rise and fall in rates of discovery and innovation remain poorly understood, they may reflect adaptive responses to exogenously emerging threats and pressures. Here we examined this possibility by fitting annual rates of scientific discovery and technological innovation to climatic variability and its associated economic pressures and resource scarcity. In time-series data from Europe (1500-1900CE), we indeed found that rates of innovation are higher during prolonged periods of cold (versus warm) surface temperature and during the presence (versus absence) of volcanic dust veils. This negative temperature-innovation link was confirmed in annual time-series for France, Germany, and the United Kingdom (1901-1965CE). Combined, across almost 500 years and over 5,000 documented innovations and discoveries, a 0.5°C increase in temperature associates with a sizable 0.30-0.60 standard deviation decrease in innovation. Results were robust to controlling for fluctuations in population size. Furthermore, and consistent with economic theory and micro-level data on group innovation, path analyses revealed that the relation between harsher climatic conditions between 1500-1900CE and more innovation is mediated by climate-induced economic pressures and resource scarcity.
人类历史是由科学技术领域具有里程碑意义的发现所塑造的。然而,在时空范围内,创新的速度并不稳定:相对停滞的时期与创造性科学的爆发以及技术创新的快速涌现交替出现。虽然发现和创新速度起伏的根源仍鲜为人知,但它们可能反映了对外部出现的威胁和压力的适应性反应。在此,我们通过将科学发现和技术创新的年速率与气候变异性及其相关的经济压力和资源稀缺性进行拟合,来检验这种可能性。在欧洲的时间序列数据(公元1500年至1900年)中,我们确实发现,在地表温度长期寒冷(相对于温暖)以及存在(相对于不存在)火山尘埃幕的时期,创新速率更高。这种负温度 - 创新关联在法国、德国和英国的年度时间序列(公元1901年至1965年)中得到了证实。综合来看,在近500年以及5000多项有记录的创新和发现中,温度每升高0.5°C,创新就会相应大幅下降0.30 - 0.60个标准差。在控制人口规模波动后,结果依然稳健。此外,与经济理论以及关于群体创新的微观层面数据一致,路径分析表明,公元1500年至1900年期间更恶劣的气候条件与更多创新之间的关系是由气候引发的经济压力和资源稀缺所介导的。