Geoarchaeological evidence from Peru for a 5000 years BP onset of El Nino

被引:264
作者
Sandweiss, DH
Richardson, JB
Reitz, EJ
Rollins, HB
Maasch, KA
机构
[1] UNIV MAINE,INST QUATERNAY STUDIES,ORONO,ME 04469
[2] UNIV PITTSBURGH,DEPT ANTHROPOL,PITTSBURGH,PA 15206
[3] UNIV PITTSBURGH,CARNEGIE MUSEUM NAT HIST,DIV ANTHROPOL,PITTSBURGH,PA 15206
[4] UNIV GEORGIA,MUSEUM NAT HIST,DEPT ANTHROPOL,ATHENS,GA 30602
[5] UNIV GEORGIA,MUSEUM NAT HIST,LAB ZOOARCHAEOL,ATHENS,GA 30602
[6] UNIV PITTSBURGH,DEPT GEOL,PITTSBURGH,PA 15260
[7] UNIV MAINE,DEPT GEOL SCI,ORONO,ME 04469
关键词
D O I
10.1126/science.273.5281.1531
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
For the tropical west coast of South America, where El Nino/Southern Oscillation (ENSO) is most pronounced, archaeological and associated paleontological deposits in northern Peru revealed a major climate change at about 5000 years before the present (yr B.P.). The data implied the presence of stable, warm tropical water as far south as 10 degrees S during the early mid-Holocene (about 8000 to 5000 yr B.P.). These data suggest that ENSO did not occur for some millennia preceding 5000 yr B.P., when global and regional climate was warmer than today.
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收藏
页码:1531 / 1533
页数:3
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