Plant Response to Nutrient Availability Across Variable Bedrock Geologies

被引:65
作者
Castle, S. C. [1 ]
Neff, J. C. [1 ,2 ,3 ]
机构
[1] Univ Colorado, Dept Geol Sci, Boulder, CO 80309 USA
[2] Univ Colorado, Environm Studies Program, Boulder, CO 80309 USA
[3] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA
基金
美国安德鲁·梅隆基金会;
关键词
nutrient availability; bedrock; forest; foliage; resorption; stoichiometry; TREE SOIL INTERACTIONS; EXCHANGE-RESIN BAGS; TEMPERATE FORESTS; ALPINE SOILS; MINERAL-NUTRITION; PARENT MATERIAL; EOLIAN DUST; RESORPTION; NITROGEN; CANOPY;
D O I
10.1007/s10021-008-9210-8
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
We investigated the role of rock-derived mineral nutrient availability on the nutrient dynamics of overlying forest communities (Populus tremuloides and Picea engelmanni-Abies lasiocarpa v. arizonica) across three parent materials (andesite, limestone, and sandstone) in the southern Rocky Mountains of Colorado. Broad geochemical differences were observed between bedrock materials; however, bulk soil chemistries were remarkably similar between the three different sites. In contrast, soil nutrient pools were considerably different, particularly for P, Ca, and Mg concentrations. Despite variations in nutrient stocks and nutrient availability in soils, we observed relatively inflexible foliar concentrations and foliar stoichiometries for both deciduous and coniferous species. Foliar nutrient resorption (P and K) in the deciduous species followed patterns of nutrient content across substrate types, with higher resorption corresponding to lower bedrock concentrations. Work presented here indicates a complex plant response to available soil nutrients, wherein plant nutrient use compensates for variations in supply gradients and results in the maintenance of a narrow range in foliar stoichiometry.
引用
收藏
页码:101 / 113
页数:13
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