Speleothems and climate:: a special issue of The Holocene

被引：73
|
作者：
Lauritzen, SE
Lundberg, J
机构：
[1] Univ Bergen, Dept Geol, N-5007 Bergen, Norway
[2] Carleton Univ, Dept Geog, Ottawa, ON K1S 5B6, Canada
来源：
HOLOCENE | 1999年 / 9卷 / 06期
关键词：
speleothems; caves; palaeoclimate; stable isotopes; laminations; trace elements; environmental reconstruction; uranium-series dating; Holocene;
D O I：
10.1191/095968399666229065
中图分类号：
P9 [自然地理学];
学科分类号：
0705 ; 070501 ;
摘要：
Speleothems (cave dripstones) are formed as a part of the meteoric water cycle and therefore variations in their growth rare and composition reflect environmental changes on the land surface above the cave. Since they are continental deposits. and possess a remarkably accurate dating potential, using TIMS U-series techniques, speleothems are important palaeoclimatic archives for the terrestrial environment, complementing the marine and ice-core records, The climatic proxies that can be deciphered from speleothems are growth rate, stable isotope composition (delta(18)O, delta(13)C), organic (humic) matter and trace element composition, as well as luminescent laminae, which may display annual rhythms. The nine papers in this special issue of The Holocene present the latest results in palaeoclimatic analysis from speleothems.
引用
收藏
页码：643 / 647
页数：5
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