Leaf litter inputs reinforce islands of nitrogen fertility in a lowland tropical forest

被引:20
|
作者
Osborne, Brooke B. [1 ]
Nasto, Megan K. [2 ]
Soper, Fiona M. [3 ]
Asner, Gregory P. [4 ]
Balzotti, Christopher S. [4 ]
Cleveland, Cory C. [3 ]
Taylor, Philip G. [5 ]
Townsend, Alan R. [6 ]
Porder, Stephen [1 ]
机构
[1] Brown Univ, Dept Ecol & Evolutionary Biol, Providence, RI 02912 USA
[2] Utah State Univ, Utah Forest Inst, Dept Wildland Resources, Logan, UT 84322 USA
[3] Univ Montana, Dept Ecosyst & Conservat Sci, Missoula, MT 59808 USA
[4] Arizona State Univ, Ctr Global Discovery & Conservat Sci, Tempe, AZ 94305 USA
[5] Univ Colorado, Inst Arctic & Alpine Res, Boulder, CO 80903 USA
[6] Colorado Coll, Environm Sci, Colorado Springs, CO 80303 USA
基金
美国安德鲁·梅隆基金会; 美国国家科学基金会;
关键词
Canopy chemistry; Carnegie airborne observatory; Imaging spectroscopy; Plant functional traits; Soil; RAIN-FOREST; NUTRIENT LIMITATION; DECOMPOSITION RATES; ORGANIC-MATTER; SOIL; AVAILABILITY; BIOGEOCHEMISTRY; TRAITS; TREES; CONSEQUENCES;
D O I
10.1007/s10533-020-00643-0
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The role of lowland tropical forest tree communities in shaping soil nutrient cycling has been challenging to elucidate in the face of high species diversity. Previously, we showed that differences in tree species composition and canopy foliar nitrogen (N) concentrations correlated with differences in soil N availability in a mature Costa Rican rainforest. Here, we investigate potential mechanisms explaining this correlation. We used imaging spectroscopy to identify study plots containing 10-20 canopy trees with either high or low mean canopy N relative to the landscape mean. Plots were restricted to an uplifted terrace with relatively uniform parent material and climate. In order to assess whether canopy and soil N could be linked by litterfall inputs, we tracked litter production in the plots and measured rates of litter decay and the carbon and N content of leaf litter and leaf litter leachate. We also compared the abundance of putative N fixing trees and rates of free-living N fixation as well as soil pH, texture, cation exchange capacity, and topographic curvature to assess whether biological N fixation and/or soil properties could account for differences in soil N that were, in turn, imprinted on the canopy. We found no evidence of differences in legume communities, free-living N fixation, or abiotic properties. However, soils beneath high canopy N assemblages received similar to 60% more N via leaf litterfall due to variability in litter N content between plot types. The correlation of N in canopy leaves, leaf litter, and soil suggests that, under similar abiotic conditions, litterfall-mediated feedbacks can help maintain soil N differences among tropical tree assemblages in this diverse tropical forest.
引用
收藏
页码:293 / 306
页数:14
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