A test of "annual resolution" in stalagmites using tree rings

被引:21
作者
Betancourt, JL
Grissino-Mayer, HD
Salzer, MW
Swetnam, TW
机构
[1] US Geol Survey, Desert Lab, Tucson, AZ 85745 USA
[2] Univ Tennessee, Dept Geog, Knoxville, TN 37996 USA
[3] Univ Arizona, Tree Ring Res Lab, Tucson, AZ 85721 USA
关键词
speleothems; paleoclimate; annual resolution; tree-ring chronologies;
D O I
10.1006/qres.2002.2354
中图分类号
P9 [自然地理学];
学科分类号
0705 ; 070501 ;
摘要
So-called annual banding has been identified in a number of speleothems in which the number of bands approximates the time interval between successive U-series dates. The apparent annual resolution of speleothem records, however, remains largely untested. Here we statistically compare variations in band thickness from a late Holocene stalagmite in Carlsbad Cavern, Southern New Mexico, USA, with three independent tree-ring chronologies form the same region. We found no correspondence. Although there may be various explanations for the discordance, this limited exercise suggests that banded stalagmites should be held to the same rigorous standards in chronology building and climatic inference as annually resolved tree rings, corals, and ice cores. (C) 2002 University of Washington.
引用
收藏
页码:197 / 199
页数:3
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