Invasive earthworms unlock arctic plant nitrogen limitation

被引:44
作者
Blume-Werry, Gesche [1 ,2 ]
Krab, Eveline J. [2 ,3 ]
Olofsson, Johan [2 ]
Sundqvist, Maja K. [2 ,4 ]
Vaisanen, Maria [5 ,6 ]
Klaminder, Jonatan [2 ]
机构
[1] Ernst Moritz Arndt Univ Greifswald, Inst Bot & Landscape Ecol, Expt Plant Ecol, Soldmannstr 15, D-17487 Greifswald, Germany
[2] Umea Univ, Dept Ecol & Environm Sci, Climate Impacts Res Ctr, S-98107 Abisko, Sweden
[3] Swedish Univ Agr Sci, Dept Soil & Environm, S-75007 Uppsala, Sweden
[4] Univ Gothenburg, Dept Earth Sci, S-41320 Gothenburg, Sweden
[5] Univ Lapland, Arctic Ctr, POB 122, Rovaniemi 96101, Finland
[6] Univ Oulu, Ecol & Genet Res Unit, POB 3000, Oulu 90014, Finland
基金
瑞典研究理事会;
关键词
TUNDRA; SOIL; VEGETATION; DECOMPOSITION; LUMBRICIDAE; COMMUNITIES; FEEDBACKS; RESPONSES; PATTERNS; GROWTH;
D O I
10.1038/s41467-020-15568-3
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
Arctic plant growth is predominantly nitrogen (N) limited. This limitation is generally attributed to slow soil microbial processes due to low temperatures. Here, we show that arctic plant-soil N cycling is also substantially constrained by the lack of larger detritivores (earthworms) able to mineralize and physically translocate litter and soil organic matter. These new functions provided by earthworms increased shrub and grass N concentration in our common garden experiment. Earthworm activity also increased either the height or number of floral shoots, while enhancing fine root production and vegetation greenness in heath and meadow communities to a level that exceeded the inherent differences between these two common arctic plant communities. Moreover, these worming effects on plant N and greening exceeded reported effects of warming, herbivory and nutrient addition, suggesting that human spreading of earthworms may lead to substantial changes in the structure and function of arctic ecosystems. Arctic plant growth is predominantly nitrogen limited, where the slow nitrogen turnover in the soil is commonly attributed to the cold arctic climate. Here the authors show that the arctic plant-soil nitrogen cycling is also constrained by the lack of larger detritivores like earthworms.
引用
收藏
页数:10
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