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1 50% of the energy was allocated to annelids (earthworms).
2 ults showed that MCs could bioaccumulated in earthworm.
3 at was absent from soil yet observed in most earthworms.
4 nt protective effects against Cu toxicity to earthworms.
5 rmed As accumulation in the coelom of intact earthworms.
6 spatio-temporal database of introduced alien earthworms.
7 nd adapted for feeding on social insects and earthworms.
8 e rotifers, freshwater mussels, daphnids and earthworms.
9 low and deep soil, perhaps through mixing by earthworms.
10 hich suggests size-selective egestion by the earthworms.
11 increased soil C storage in the presence of earthworms.
12 The (68)Znen/(64)Znen ratios determined for earthworms (1.09 +/- 0.04), soils (1.09 +/- 0.02), and p
14 ty increased in inoculated seedlings without earthworms 12 months after inoculation, and general nega
16 tip density in inoculated seedlings without earthworms 6 months after inoculation, lower fine root t
17 on agriculture [CA]) significantly increased earthworm abundance (mean increase of 137% and 127%, res
18 production of key crops by analyzing maps of earthworm abundance, soil properties, and crop yields to
19 phytoaccumulation was minimal (BAF(dw) < 1), earthworms accumulated high loads (BAF(dw) up to 23), su
20 es Darwin, but several recent syntheses link earthworm activities to higher greenhouse gas emissions,
21 ot system parameters and mycorrhization, how earthworms affect the bare root system, and if mycorrhiz
22 ray and finally study slices within a living earthworm, allowing metabolite changes to be discerned w
23 ht; (c) set-up of the control plots (i.e. no earthworms, ambient nitrogen) used in this experiment.
24 derstand the joint effects of TNT and RDX on earthworms, an important ecological and bioindicator spe
27 0 +/- 2670 and 3000 +/- 200 mug/kg lipid for earthworms and detritivorous woodlice, respectively).
29 n nature, from individual organisms (notably earthworms and hydra), through communities of microbes,
30 ion site and is nontoxic to nerve tissues in earthworms and mammals, we have also developed in vivo p
33 three-level food web of predaceous beetles, earthworms and plants, Zhao et al. (2013) report evidenc
35 We conclude that the coordinated actions of earthworms and their associated soil biota were responsi
36 of these two important ecological groups of earthworms and their burrowing, feeding and casting acti
37 High abundance of an invasive pantropical earthworm (and the absence of indigenous lumbricid speci
38 the endogeic Aporrectodea rosea (rosy-tipped earthworm) and planted with Lolium perenne (perennial ry
39 tional groups of termites, ants, beetles and earthworms, and an increase in the abundance of small ma
42 and 'brown' belowground (soil arthropods and earthworms) animal food webs in tropical rainforests and
46 our study provides evidence that introduced earthworms are associated with declines in plant diversi
59 that correlated with soil C content, such as earthworm biomass and fungal/bacterial energy channel ra
61 a case study on the role of root growth and earthworm bioturbation in restoring the structure of a s
62 ated AC were comparable to those measured by earthworm biouptake (bioavailability) at both dose level
63 doalkyl betaine (6:2 FTAB) bioaccumulated in earthworms [BSAF ~ 2.5-5.4 (g(dw,worm)/g(dw,soil))(-1)]
64 ficant effects on the survival and growth of earthworms, but significantly reduced cocoon and juvenil
65 act as vectors to increase metal exposure in earthworms, but that the associated risk is unlikely to
66 n dating protocol has been developed to date earthworm calcite granules from the reference loess sequ
69 ecific cellular or molecular level damage to earthworms caused by chronic exposure to TiO(2) are warr
70 a distinct bacterial community defines these earthworms, clear family- and species-level modification
71 cal improvements enabled by the radiocarbon "earthworm clock" thus strongly enhance our understanding
72 in cytotoxicity of dissolved silver salt on earthworm coelomocytes and human cells (THP-1 cells, dif
73 ate change may have serious implications for earthworm communities and for the functions they provide
74 ect sizes of associations between introduced earthworm communities and plant diversity, cover of plan
76 s were found to be more important in shaping earthworm communities than soil properties or habitat co
78 this reflects the phylogenetic uniqueness of earthworms compared to the well-annotated model animals.
79 evaluated against a data set of 402 internal earthworm concentrations reported from the literature in
81 specially notable in the global South, where earthworms contribute 10% of total grain production in S
84 ses or control cauterization with artificial earthworms covered with earthworm wash (EWW) or distille
85 revealed that detrimental warming effects on earthworm densities and biomass could indeed be partly e
86 effects depends on presence of crop residue, earthworm density and type and rate of fertilization.
87 ults indicate that PFAA bioaccumulation into earthworms depends on soil concentrations, soil characte
88 oluminescent systems (those of limpet Latia, earthworms Diplocardia and Fridericia and higher fungi),
90 nin, a pore-forming toxin extracted from the earthworm E. fetida, inserts large conductance nanopores
94 cal disturbances should encourage beneficial earthworm effects and support multiple ecosystem service
95 both exotic earthworms and N addition, such earthworm effects on the nematode community were negated
96 ed weekly throughout the life history of the earthworm Eisenia andrei to test the hypothesis that the
99 ular and cellular toxicity mechanisms in the earthworm Eisenia fetida exposed to AgNPs (83 +/- 22 nm)
101 oparticle recognition by coelomocytes of the earthworm Eisenia fetida using E. fetida coelomic protei
102 that such dual strokes occur as well in the earthworm Eisenia fetida which inhabits moist sediments
105 investigate arsenic (As) bioaccumulation in earthworms (Eisenia andrei) exposed to six field-collect
106 , 1, 3, 6, and 12 months of soil incubation, earthworms (Eisenia andrei) were introduced for 72 h exp
107 re compared to actual PAH bioaccumulation in earthworms (Eisenia fetida) and rye grass (Lolium multif
108 ccumulation factors (BSAFs) were assessed in earthworms (Eisenia fetida) exposed to soil microcosms a
111 erns, and biomagnification of PFASs in soil, earthworms (Eisenia fetida), and Bank voles (Myodes glar
112 copolymers were assessed in laboratory-grown earthworms (Eisenia fetida, triplicate of exposure tests
113 Lysenin is a pore-forming toxin from the earthworm Eisenida foetida, of which both the soluble an
115 od for maintaining the prostate gland of the earthworm, Eudrilus eugeniae ex vivo and examine its pot
116 for estimating pesticide bioconcentration in earthworms exhibit limited applicability across differen
117 extracts of E. fetida tissue suggested that earthworms exhibited significant changes in their metabo
123 tperformed existing models in characterizing earthworm exposure to pesticides in soil, but it could a
124 dings support the hypothesis that introduced earthworms facilitate particular plant species adapted t
125 oxicological effect of microcystins (MCs) on earthworms, filter paper acute toxicity test, avoidance
127 vel luciferin from a bioluminescent Siberian earthworm Fridericia heliota was recently described.
128 CHEMHIST upon in situ imaging, we sampled an earthworm from its natural habitat and created an intera
131 he probably continuous introduction of alien earthworms, from a variety of sources and introduction p
132 s at the cut ends of invertebrate myelinated earthworm giant axons beginning with the formation of a
133 structures, which form after transection of earthworm giant axons, are very dynamic in the short ter
135 insights into the variations of ARGs in the earthworm gut and highlight the vital role of viruses in
137 ve disruption of microbiome and resistome in earthworm gut by chiral fungicides and offer significant
138 act the inhibitory effects of polyphenols on earthworm gut enzymes, and high-polyphenol diets increas
140 il solution (0.01 M CaCl2), but in synthetic earthworm guts desorption was higher from microplastics
143 ibility of maintaining the prostate gland of earthworms in an ex vivo setting, providing a valuable m
144 sment underlined a moderate to high risk for earthworms in arable soils mostly attributed to insectic
145 t at two sites in Minnesota, USA by sampling earthworms in closed and open canopy in three temperatur
146 e FASA-based copolymers were taken up by the earthworms in concentrations between 19 and 33 ng/g of d
147 suggest that warming limits the invasion of earthworms in northern North America by causing less fav
148 and offspring generations of two species of earthworms in order to evaluate possible mechanisms of a
149 ercial mycorrhization with truffles, and how earthworms in the inoculation substrate would affect the
152 et al. () explored how N addition and exotic earthworms interacted to impact on the plant-feeding nem
155 t region that to date supposedly have slowed earthworm invasion, future warming is hypothesized to ac
156 ies richness or evenness did not change with earthworm invasion, our results indicate clear changes i
159 een the uptake of the two forms of Zn by the earthworm L. rubellus, with the dietary pathway accounti
161 this obstacle can be removed by our proposed earthworm-like peristaltic crawling motion mechanism, ba
162 robotic control problems by a case study of earthworm-like peristaltic crawling without traditional
163 d.w.), and higher concentrations of PFAS in earthworms living in sludge-amended soil compared to non
164 , uptake pathways by, and biokinetics in the earthworm Lumbricus rubellus were investigated using sta
165 , we studied the survival and fitness of the earthworm Lumbricus terrestris (Oligochaeta, Lumbricidae
167 hexagonal bilayer hemoglobin (HBL Hb) of the earthworm Lumbricus terrestris provided masses of 3.41 t
171 ability models for predicting Cu toxicity to earthworms (Lumbricus rubellus, Aporrectodea longa, and
172 trate here the formation of PFOA and PFOS in earthworms (Lumbricus terrestris) from a group of four z
173 b encompassing land-applied biosolids, soil, earthworms (Lumbricus), deer mice (Peromyscus maniculatu
175 The extracellular hemoglobin (Hb) of the earthworm, Lumbricus terrestris, has four major O2-bindi
176 tion of exposure, and that accumulation into earthworms may be a potential route of entry of PFAAs in
177 ts indicated that the conduction velocity of earthworm medial giant nerve fiber decreased significant
181 higher on the experimental site in the soil, earthworms, mice (livers), and European starling eggs, b
183 o be integrated with models that account for earthworm movement and fluctuating soil pesticide concen
184 in vivo procedures that permanently maintain earthworm myelinated medial giant axons whose functional
185 cterizing the major metal-binding protein in earthworms, namely the two isoforms of metallothionein.
190 the multiple direct and indirect impacts of earthworms on ecosystem functions within an ecological m
193 for the first time the impacts of introduced earthworms on plant diversity and community composition
195 aquatic (snail and mussel) and terrestrial (earthworm) organisms and for monitoring the environmenta
197 at inactivated coelomic fluid (HI-CF) of the earthworm, Perionyx excavatus as a potential alternative
198 burrowing horizontally to acquire nutrients) earthworm Pontoscolex corethrurus that was added to the
201 ecological policies and practices to support earthworm populations and overall soil biodiversity coul
202 ultivation practices is expected to increase earthworm populations and their contributions to ecosyst
203 orted on the effects of tillage intensity on earthworm populations, attributed in narrative reviews t
205 s that favor growth-promoting rhizobacteria, earthworms, predatory mites, and other beneficial organi
207 escribing 21 ecosystem functions showed that earthworm presence generally enhanced multifunctionality
208 e show, using meta-analysis, that on average earthworm presence in agroecosystems leads to a 25% incr
209 show, in a unique two-year experiment, that earthworm presence increases the combined cumulative emi
216 ed to examine the response of Eisenia fetida earthworms raised from juveniles for 20-23 weeks in soil
218 olomics provides a more sensitive measure of earthworm response to TiO(2) materials in soil and that
220 to determine total As within both the whole earthworm's body (AsE) and coelomic fluid extracts (AsF)
222 two phyla (a waterbird, freshwater fish, and earthworms) sampled in different geographical areas and
225 city was found in the filter paper test, and earthworms showed no avoidance response to MCs exposure.
227 m uptake and elimination studies using three earthworm species (Lumbricus terrestris, Aporrectodea ca
229 sts) on the springtail Folsomia candida, the earthworm species Aporectodea caliginosa and Eisenia fet
230 of Zn and Pb in thin sections of two epigeic earthworm species collected from a Pb/Zn-mine soil.
235 farm and regional levels by sampling plants, earthworms, spiders and bees in 1470 fields of 205 rando
237 tic relationships, with the exception of the earthworm, suggesting that the reported presence of J ch
238 ts the Open Air Laboratories (OPAL) Soil and Earthworm Survey as an example of public participation i
241 ed in Shao et al. (): (a) the endogeic (i.e. earthworms that typically live in the soil, burrowing ho
244 Detection and quantification of (68)Zn-E in earthworm tissue was possible after only 4 h of dermal e
247 the arsenious soils, the As distribution in earthworms was examined by micro-X-ray fluorescence spec
249 f airborne odorants (amyl acetate, limonene, earthworm wash vapor, fish water vapor, earthworms, gold
250 mites), and soil biota (including mites and earthworms), we assess the impacts of synergistic intera
251 BDE-209 burdens in sludge-amended soil and earthworms were 7500 +/- 2800 mug/kg TOC and 6500 +/- 41
252 noculation, lower fine root tip density when earthworms were added, the specific root tip density inc
254 ta soil accumulation factors (BSAFs) for the earthworms were calculated after 28 days of exposure for
260 d, more importantly, the bigger-sized anecic earthworms were the most sensitive ecological groups to
261 e compositions of the soils, pore waters and earthworms were then determined using multiple collector
262 suggest that MCs induces oxidative stress on earthworms, which leads to disruption of the antioxidant
263 (BMF) > 1 was detected for Bank vole(whole)/earthworm(whole) for perfluorooctansulfonate in the skii
265 Uptake routes were isolated by introducing earthworms with sealed and unsealed mouthparts into test
266 rs generally predicted PAH concentrations in earthworms within a factor of 10, although correlations