在古典玛雅文明崩期间的干旱量化
Nicholas P Evans1, Thomas K Bauska2, Fernando Gázquez-Sánchez2
1Godwin Laboratory for Palaeoclimate Research, Department of Earth Sciences, University of Cambridge, Cambridge CB2 3EQ, UK. ne243@cam.ac.uk.
概括
古玛雅文明面临着严重的干旱,每年降水量下降高达70%. 这项研究使用湖泊沉积物同位素来量化过去的气候变化及其对社会的影响.
科学领域:
- 古气候学
- 考古学
- 水文学
背景情况:
- 终极古典时期 (公元800-1000年) 见证了低地古典玛雅文明的崩,这往往与气候变化有关.
- 之前对水文变化的估计依赖于间接的气候代理,产生不确定结果.
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