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摘要:
Geodetic measurements of a Roman aqueduct in Caesarea,on the Mediterranean coast of central Israel,show that the massive structure preserved its original gradient of 0.05%in places where it was founded on rock,suggesting that that domain has been tectonically stable for the last two millennia.Consequently,since the land was stable,dated archaeological sealevel proxies that recorded their contemporaneous sealevels when the city was active,reflect global sealevel and their variations.The evidence suggests that sealevel was similar to the present some 2,000 years ago,it was nearly 0.5 m higher than the present some 1,300 years ago,and about 0.5 m lower nearly 800 years ago.These measurements match earlier climatological evidence of the early Mediaeval Warm Period and the early stages of the Little Ice Age,respectively.No sealevel evidence was encountered in Caesarea after the collapse of the Crusaders’kingdom.
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篇名 Caesarea in Coastal Israel:A Benchmark for Sealevel Changes during the 1st-13th Centuries
来源期刊 环境科学与工程:A 学科 地球科学
关键词 NEOTECTONIC stability geoarchaeological PROXIES SEALEVEL variations HISTORIC climate CHANGES
年,卷(期) hjkxygc-a_2019,(1) 所属期刊栏目
研究方向 页码范围 36-48
页数 13页 分类号 X
字数 语种
DOI
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研究主题发展历程
节点文献
NEOTECTONIC
stability
geoarchaeological
PROXIES
SEALEVEL
variations
HISTORIC
climate
CHANGES
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研究分支
研究去脉
引文网络交叉学科
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期刊影响力
环境科学与工程:A
月刊
2162-5301
武汉洪山区卓刀泉北路金桥花园C座4楼
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331
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