Climate stability and the development of agricultural societies

被引:16
作者
Feynman, Joan [1 ]
Ruzmaikin, Alexander [1 ]
机构
[1] CALTECH, Jet Prop Lab, Pasadena, CA 91125 USA
基金
美国国家航空航天局;
关键词
ICE-CORE; OSCILLATION SIGNATURE; PHYTOLITH EVIDENCE; GREENLAND; ATLANTIC; DOMESTICATION; VARIABILITY; MAIZE; TEMPERATURE; COLLAPSE;
D O I
10.1007/s10584-007-9248-1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Although Modern Man had developed long before the migration from Africa began similar to 55,000 years ago no agricultural societies developed until about similar to 10,000 years ago. In the next 5,000 years agricultures developed independently in at least six regions of the world. It is virtually certain that it was not a chance occurrence that so many new agricultures appeared in the same 5,000 years. What inhibited agriculture world wide for 44,000 years and what changed similar to 10,000 years ago? Here we suggest that a major factor influencing the development of agricultural societies was climate stability. From the experience of four cultures we estimate that the development of agriculture needed similar to 2,000 years of climate free from significant climate variations on time scales of a few centuries. Using the Empirical Mode Decomposition technique specifically designed to exhibit the time history of the amplitude of variations in non-stationary time series such as climate proxy records, we find that between 50,000 years ago and the termination of the Younger Dryas similar to 11,600 years ago there was probably no time span as long as 2,000 years that was free of relatively large century scale variations. Furthermore variations on these time scales appear to have been relatively small since the Younger Dryas (YD) ended, supporting our proposition concerning the importance of climate stability in the history of human culture.
引用
收藏
页码:295 / 311
页数:17
相关论文
共 58 条
[1]  
[Anonymous], ABR CLIM CHANG IN SU
[2]  
Bar-Yosef O, 1998, EVOL ANTHROPOL, V6, P159, DOI 10.1002/(SICI)1520-6505(1998)6:5<159::AID-EVAN4>3.0.CO
[3]  
2-7
[4]   THE NORTH-ATLANTIC OSCILLATION SIGNATURE IN DEUTERIUM AND DEUTERIUM EXCESS SIGNALS IN THE GREENLAND ICE-SHEET PROJECT-2 ICE CORE, 1840-1970 [J].
BARLOW, LK ;
WHITE, JWC ;
BARRY, RG ;
ROGERS, JC ;
GROOTES, PM .
GEOPHYSICAL RESEARCH LETTERS, 1993, 20 (24) :2901-2904
[5]   Late quaternary paleoclimate in the eastern Mediterranean region from stable isotope analysis of speleothems at Soreq Cave, Israel [J].
BarMatthews, M ;
Ayalon, A ;
Kaufman, A .
QUATERNARY RESEARCH, 1997, 47 (02) :155-168
[6]   CORRELATIONS BETWEEN CLIMATE RECORDS FROM NORTH-ATLANTIC SEDIMENTS AND GREENLAND ICE [J].
BOND, G ;
BROECKER, W ;
JOHNSEN, S ;
MCMANUS, J ;
LABEYRIE, L ;
JOUZEL, J ;
BONANI, G .
NATURE, 1993, 365 (6442) :143-147
[7]   THE AGRICULTURAL REVOLUTION [J].
BRAIDWOOD, RJ .
SCIENTIFIC AMERICAN, 1960, 203 (03) :130-&
[8]  
BUTZER KW, 1976, EARLY HYDRAULIC CIVI, P54
[9]  
CLARK PU, 1999, GEOPHYS MONOGRAPH SE
[10]  
CLOTTES J, 2001, GROTTE CHAUVEL ART O