Country | Tree species | Earthworm species | Study period | Isotope types | Major findings | References |
---|---|---|---|---|---|---|
Ecosystem | ||||||
Japan | Quercus crispula, Cinnamomum camphora, Castanopsis cuspidate var. sieboldii | Metaphire soulensis, Amynthas spp. | 1 time measure | 13C, 15N | Values of δ15N increased from litter to humus, to deeper soil; and the value of body tissue was higher in endogeic than in epigeic earthworms. Such 15N enrichments indicate that the niches of earthworm species were affected from available food sources | Uchida et al. [84] |
Evergreen broad-leaved forests | ||||||
Ireland | – | Lumbricus festivus | 14 days | 13C, 15N | Earthworm diet switched from clover (C3) to maize (C4); the dietary δ13C signature altered more rapidly in the mucus (4‰) than in the tissue (1‰) | Schmidt et al. [86] |
Artificial substrate | ||||||
Germany | Fagus sylvatica, Fraxinus excelsior | Octolasion tyrtaeum | 100 days | 14C | Earthworms’ mineralization on 14C labeled lignin was more pronounced in treatments without (+ 14.1%) than in those with (+ 8.6%) mineral soil (Bw-horizon) because of earthworm’s mixing of soil layers | Marhan & Scheu [97 ] |
Deciduous broad-leaved forests | Aporrectodea caliginosa, Lumbricus terrestris | 3 years | 15N | 6–14% of 15N released from leaf-litter was recovered in plants. Earthworms increased plant acquisition of nitrogen from 15N enriched leaf-litter; and higher degradability of litter resulted in the higher acquisition of nitrogen | Yang et al. [90] | |
Germany | – | Lumbricus terrestris | 7 days | 13C, 15N | 15N-labeled earthworms can transfer 15N through food web, into soil, plants, and aphids. 15N incorporation was highest in earthworm casts (11,751‰) followed by earthworm tissue (454‰), plant roots (62‰), leaves (50‰), and aphids (37‰) | Grabmaier et al. [89] |
Artificial substrate | ||||||
United States of America | Acer saccharum, A. rubrum, etc | Lumbricus terrestris | 1 time measure | 13C, 15N | Earthworm presence decreases δ13C of forest floor materials and mineral soil because they prefer leaves as food sources which have higher δ13C than stem and twigs | Bohlen et al. [51] |
Acer saccharum | Lumbricus terrestris, Lumbricus rubellus | 2 years | 13C, 15N | 13C-labeled litters had higher recovery without (61–68%) than with (20–29%) earthworms. Recovery of 15N was higher than 13C, with lower values for L. terrestris than L. rubellus | Fahey et al. [57] | |
No data | Amynthas hilgendorfi, Lumbricus rubellus, etc | 21Â days | 13C | Litter carbon-derived soil respiration was reduced by A. hilgendorfi, L. rubellus, and Eisenoides lonnbergi, but not by Octolasion lacteum | Chang et al. [88] | |
Acer saccharum | Lumbricus terrestris, Lumbricus rubellus | 6Â years | 13C | Earthworms stimulated carbon storage into soil aggregates. Soil food web was more enriched by 13C from roots than above-ground plant-litter | Fahey et al. [87] | |
Deciduous broad-leaved forests | Acer saccharum | Lumbricus terrestris, Lumbricus rubellus | 7 months | 13C, 15N | 15NO3− added to the soil was rapidly depleted in the presence of earthworms due to less retention of nitrogen in litter and upper soil layers, but not due to the acceleration of water penetration | Ewing et al. [96] |
Acer saccharum | Community dominated by Lumbricus rubellus | 3Â years | 13C, 15N | 13C- and 15N-labeled litter input in earthworm-invaded plots resulted in greater 13C and 15N of microbial biomass than the inorganic nitrogen pool; depletion of carbon and maintenance of soil nitrogen pool are caused by earthworm stimulation of microbial biomass and activity | Groffman et al. [91] | |
Populus grandidentata, Quercus rubra, Acer rubrum, etc | Community dominated by Dendrobaena octaedra, Aporrectodea spp., etc | 150Â days | 13C, 15N | Recovery of litter 15N depends on soil texture; it was greater in sandy loam (98.2%) than in sandy soil (66.2%) after earthworm additions. Earthworm tissue was a minor sink for 13C (0.56%) and 15N (2.26%), which was delivered from surface litter | Crumsey et al. [98] |