QQ客服 官方微博 反馈留言

	A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810-1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ
	Railsback, L. Bruce; Brook, George A.; Liang, Fuyuan; Voarintsoa, Ny Riavo G.; Cheng, Hai; Edwards, R. Lawrence
刊名	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY
	2018
卷号	506页码:139-153
关键词	Rainfall Speleothem Bone Cave Africa Global warming Tambora
ISSN号	0031-0182
URL标识	查看原文
内容类型	期刊论文
URI标识	http://www.corc.org.cn/handle/1471x/2919211
专题	西安交通大学
推荐引用方式 GB/T 7714	Railsback, L. Bruce,Brook, George A.,Liang, Fuyuan,et al. A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810-1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ[J]. PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,2018,506:139-153.
APA	Railsback, L. Bruce,Brook, George A.,Liang, Fuyuan,Voarintsoa, Ny Riavo G.,Cheng, Hai,&Edwards, R. Lawrence.(2018).A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810-1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ.PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY,506,139-153.
MLA	Railsback, L. Bruce,et al."A multi-proxy climate record from a northwestern Botswana stalagmite suggesting wetness late in the Little Ice Age (1810-1820 CE) and drying thereafter in response to changing migration of the tropical rain belt or ITCZ".PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY 506(2018):139-153.

个性服务

查看访问统计

相关权益政策

暂无数据

收藏/分享

除非特别说明，本系统中所有内容都受版权保护，并保留所有权利。