Changes in soil carbon mineralization related to earthworm activity depend on the time since inoculation and their density in soil

被引:14
作者
Garnier, Patricia [1 ]
Makowski, David [2 ]
Hedde, Mickael [3 ]
Bertrand, Michel [4 ]
机构
[1] Univ Paris Saclay, INRAE, AgroParisTech, UMR Ecosys, F-91120 Palaiseau, France
[2] Univ Paris Saclay, INRAE, AgroParisTech, UMR MIA 518, F-91120 Palaiseau, France
[3] INRAE, UMR Eco & Sols, 2 Pl Viala, F-34070 Montpellier, France
[4] Univ Paris Saclay, INRAE, AgroParisTech, UMR AGRON, F-91120 Palaiseau, France
关键词
SHORT-TERM; RESIDUES; MEGASCOLECIDAE; DECOMPOSITION; LUMBRICIDAE; RESPIRATION; EMISSIONS; DYNAMICS; BEECH; STRAW;
D O I
10.1038/s41598-022-17855-z
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
Earthworms play a key role in soil carbon mineralization, but their effect is highly uncertain and suspected to vary as a function of several factors, particularly the earthworm density and time from earthworm inoculation. We conducted a meta-analysis considering these factors based on 42 experiments comparing carbon mineralization in the absence and presence of earthworms at different times. The results reveal an average carbon mineralization increase of 24% (sd 41%) in the presence of earthworms with an initial median earthworm density of 1.95 mg/g soil DM (Dry Mass) (sd 48%). We show that carbon mineralization due to earthworms was related to their density and time from inoculation. From a simple regression model using these two variables, the estimated impact of earthworms on carbon mineralization was 20% increase from 0 to 60 days and 14% decrease at day 350 for a density of worms commonly found in soils (0.5 mg/g soil DM). Finally, we proposed a simple equation that could be used in organic matter decomposition models that do not take macrofauna into account.
引用
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页数:10
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