Oxygen isotope ratios of plant available phosphate in lowland tropical forest soils

被引:28
|
作者
Gross, A. [1 ]
Turner, B. L. [2 ]
Wright, S. J. [2 ]
Tanner, E. V. J. [3 ]
Reichstein, M. [4 ]
Weiner, T. [1 ]
Angert, A. [1 ]
机构
[1] Hebrew Univ Jerusalem, Inst Earth Sci, IL-91904 Jerusalem, Israel
[2] Smithsonian Trop Res Inst, Balboa, Ancon, Panama
[3] Univ Cambridge, Dept Plant Sci, Cambridge CB2 1TN, England
[4] Max Planck Inst Biogeochem, D-07745 Jena, Germany
来源
SOIL BIOLOGY & BIOCHEMISTRY | 2015年 / 88卷
关键词
Stable oxygen isotopes; Lowland tropical soils; Phosphate microbial turnover; Bioavailable phosphate; RAIN-FOREST; PHOSPHORUS SOLUBILIZATION; ORGANIC PHOSPHORUS; PASTURE SOILS; MOIST FOREST; PANAMA; LITTERFALL; POTASSIUM; NUTRIENTS; NITROGEN;
D O I
10.1016/j.soilbio.2015.06.015
中图分类号
S15 [土壤学];
学科分类号
0903 ; 090301 ;
摘要
Phosphorus (P) cycles rapidly in lowland tropical forest soils, but the process have been proven difficult to quantify. Recently it was demonstrated that valuable data on soil P transformations can be derived from the natural abundance of stable oxygen isotopes in phosphate (delta(18)Op). Here, we measured the delta(18)Op of soils that had received long-term nutrient additions (P, nitrogen, and potassium) or litter manipulations in lowland tropical forest in Panama and performed controlled incubations of fresh soils amended with a single pulse of P. To detect whether delta(18)Op values measured in the incubations apply also for soils in the field, we examined the delta(18)Op values after rewetting dry soils. In the incubations, resin-P delta(18)Op values converged to similar to 3.5 parts per thousand above the expected isotopic equilibrium with soil water. This contrasts with extra-tropical soils in which the delta(18)Op of resin-P matches the expected equilibrium with soil water. Identical above-equilibrium resin-P delta(18)Op values were also found in field soils that did not receive P additions or extra litter. We suggest that the 3.5 parts per thousand above-equilibrium delta(18)Op values reflect a steady state between microbial uptake of phosphate (which enriches the remaining phosphate with the heavier isotopologues) and the release of isotopically equilibrated cell internal phosphate back to the soil. We also found that soil nutrient status affected the microbial turnover rate because in soils that had received chronic P addition, the original delta(18)Op signature of the fertilizer was preserved for at least eight weeks, indicating that the off-equilibrium delta(18)Op values produced during microbial phosphate turnover was not imprinted in these soils. Overall, our results demonstrate that ongoing microbial turnover of phosphate mediates its biological availability in lowland tropical soils. (C) 2015 Elsevier Ltd. All rights reserved.
引用
收藏
页码:354 / 361
页数:8
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