Warming shifts 'worming': effects of experimental warming on invasive earthworms in northern North America

被引:19
|
作者
Eisenhauer, Nico [1 ,2 ]
Stefanski, Artur [3 ]
Fisichelli, Nicholas A. [4 ]
Rice, Karen [3 ]
Rich, Roy [3 ]
Reich, Peter B. [3 ,5 ]
机构
[1] German Ctr Integrat Biodivers Res iDiv, Deutsch Pl 5e, D-04103 Leipzig, Germany
[2] Univ Leipzig, Inst Biol, D-04103 Leipzig, Germany
[3] Univ Minnesota, Dept Forest Resources, St Paul, MN 55108 USA
[4] Natl Pk Serv, Nat Resource Stewardship & Sci, Ft Collins, CO 80525 USA
[5] Univ Western Sydney, Hawkesbury Inst Environm, Penrith, NSW 2751, Australia
来源
SCIENTIFIC REPORTS | 2014年 / 4卷
关键词
CLIMATE-CHANGE; LITTER DECOMPOSITION; HARDWOOD FORESTS; SOIL CARBON; TEMPERATE; RESPONSES; LUMBRICIDAE; ECOSYSTEM; GRASSLAND; SPRUCE;
D O I
10.1038/srep06890
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
Climate change causes species range shifts and potentially alters biological invasions. The invasion of European earthworm species across northern North America has severe impacts on native ecosystems. Given the long and cold winters in that region that to date supposedly have slowed earthworm invasion, future warming is hypothesized to accelerate earthworm invasions into yet non-invaded regions. Alternatively, warming-induced reductions in soil water content (SWC) can also decrease earthworm performance. We tested these hypotheses in a field warming experiment at two sites in Minnesota, USA by sampling earthworms in closed and open canopy in three temperature treatments in 2010 and 2012. Structural equation modeling revealed that detrimental warming effects on earthworm densities and biomass could indeed be partly explained by warming-induced reductions in SWC. The direction of warming effects depended on the current average SWC: warming had neutral to positive effects at high SWC, whereas the opposite was true at low SWC. Our results suggest that warming limits the invasion of earthworms in northern North America by causing less favorable soil abiotic conditions, unless warming is accompanied by increased and temporally even distributions of rainfall sufficient to offset greater water losses from higher evapotranspiration.
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页数:7
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