Reconstruction of temperature in the Central Alps during the past 2000 yr from a δ18O stalagmite record

被引：200
|
作者：
Mangini, A
Spötl, C
Verdes, P
机构：
[1] Heidelberger Akad Wissensch, Forsch Stelle Radiometrie, D-69120 Heidelberg, Germany
[2] Univ Innsbruck, Inst Geol & Palaontol, A-6020 Innsbruck, Austria
来源：
EARTH AND PLANETARY SCIENCE LETTERS | 2005年 / 235卷 / 3-4期
关键词：
Medieval Warm Period; temperature; Central Alps; stalagmite record; Holocene; stable isotopes;
D O I：
10.1016/j.epsl.2005.05.010
中图分类号：
P3 [地球物理学]; P59 [地球化学];
学科分类号：
0708 ; 070902 ;
摘要：
The precisely dated isotopic composition of a stalagmite from Sparmagel Cave in the Central Alps is translated into a highly resolved record of temperature at high elevation during the past 2000 yr. Temperature maxima during the Medieval Warm Period between 800 and 1300 AD are in average about 1.7 degrees C higher than the minima in the Little Ice Age and similar to present-day values. The high correlation of this record to Delta C-14 Suggests that solar variability was a major driver of climate in Central Europe during the past 2 millennia. (c) 2005 Elsevier B.V. All rights reserved.
引用
收藏
页码：741 / 751
页数：11
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