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Hodson, M. E.

Publications and source records attributed to Hodson, M. E..

3 recordsLinked to original sources

The response of Allolobophora chlorotica to drought stress in four soils

Earthworms are key contributors to healthy and productive soils, yet their reliance on water makes them vulnerable to the increased frequency and severity of droughts predicted under climate change. To avoid desiccation, some earthworms induce aestivation, a period of reduced metabolism during which they coil up and seal themselves into a chamber until conditions improve. However, the environmental conditions that trigger aestivation remain poorly understood. Here the responses of Allolobophora chlorotica, a common UK earthworm, to gradual air drying (at 15 {+/-} 1 {degrees}C) were examined in four soils differing in texture. Earthworm activity (active or aestivating) and mass change relative to initial values (pre- and post-24 hours hydration) were measured at three gravimetric moisture contents (~19.7, 15.55 and 12.39 wt%) and three water potentials (~pF 1.59, 2.92 and 4.05). Water potential, rather than bulk water content, was the strongest predictor of behaviour. All earthworms remained active and gained ~36-53 % mass at the highest water availability (~pF 1.59), but 100 % aestivated at the lowest (~pF 4.05) in all but the sandiest soil. In contrast, responses at equal gravimetric moisture contents varied by soil type. All individuals in the clay aestivated and lost up to ~45 % mass, whereas those in sand and sandy loam soil largely remained active and gained mass. Differences likely reflect textural constraints on movement and the construction of aestivation chambers, which were fragile in sandy soils but more robust in clay-rich soils. After 24 hours of hydration, all earthworms had increased beyond their starting mass, indicating changes in mass were largely due to reversible water loss. However, some residual mass differences between control and drying treatments suggest differences in tissue mass, potentially attributable to suspended feeding and clitellum regression, characteristic features of aestivation. Overall, these findings show that Al. chlorotica is highly desiccation tolerant, but that soil texture strongly modulates both the onset and viability of aestivation, with implications for predicting earthworm resilience under future drought regimes.

ecology↗

The effect of repeated periods of drought and aestivation on Allolobophora chlorotica reproductive output

Increasing drought frequency under climate change is expected to intensify periods of suboptimal soil moisture, adversely affecting earthworms and other soil biota. To survive desiccation, some earthworms enter aestivation, a state of reduced metabolic activity during which reproduction and ecosystem service provision are suspended. However, the capacity of earthworms to recover from repeated drying events remains poorly understood. This study examined how multiple drought-aestivation cycles influence the reproductive performance of Allolobophora chlorotica, one of the most common UK earthworm species. Adults were exposed to one, two or three 14-day drying periods to gravimetric moisture contents of [~]11-13 wt% in loamy soil, each followed by three days under favourable moisture conditions. After the final exposure, earthworms were placed in groups of four into optimally moist soil for 50 days to reproduce. Cocoon number, mass, viability and incubation time were measured as indicators of reproductive success. Cocoon production declined significantly with increasing aestivation frequency (p < 0.001), being lowest during Days 1-10 of recovery ([~]0-0.02 cocoons earthworm-1 day-1), peaking between Days 20-30 ([~]0.08-0.16 cocoons earthworm-1 day-1) and declining over the final 20 days ([~]0.08-0.12 cocoons earthworm-1 day-1). Unexpectedly, earthworms previously exposed to drying and aestivation produced more (226 vs 171 cocoons, p < 0.05) and heavier (6.701 {+/-} 1.205 vs 6.036 {+/-} 1.256 mg, p < 0.05) cocoons than those kept under constant high moisture, suggesting compensatory growth upon rehydration and possibly reflecting food limitation or soil compaction in controls. Cocoon viability and incubation time did not differ significantly between treatments. Across treatments, earthworm mass strongly predicted fecundity as heavier individuals produced more (p < 0.001) and heavier (p <0.001) cocoons, and cocoon mass was positively correlated with hatching success (p < 0.001). Overall, Al. chlorotica displayed resilience to short-term, intermittent drought through aestivation, but reproductive success remained sensitive to the combined effects of soil moisture, food availability, and soil structure. These findings highlight the importance of considering multiple environmental constraints when predicting soil fauna responses to increasing drought frequency and duration.

ecology↗

Coping with extremes: How Epigenetic and Molecular Adaptations Enable Earthworms to Thrive in Volcanic Soils

Earthworms thriving in naturally occurring geothermal soils offer rare insight into rapid adaptation to environmental extremes. Here, we show that the pantropical earthworm Amynthas gracilis survives and flourishes in soils of the Furnas Volcano (Sao Miguel Island, Azores), where conditions include elevated temperatures (up to 40 {degrees}C), high CO2 (88.6%), low O2 (10%), toxic metals, and mildly acidic pH. In a reciprocal-transplant, mesocosm-based experiment between soils overlying areas of active degassing volcanic gassing (hereafter active degassing soils) and reference soils, convergence of the epidermal thickness of the transplanted earthworms to the resident-soil phenotype (24 {+/-} 3.9 {micro}m active degassing soil, 43.8 {+/-} 8 {micro}m reference soil), was observed within 31 days. Combining RNA-Seq, DNA (5-cytosine) methylation mapping, and microRNA profiling, this phenotypic change results from coordinated transcriptional and epigenetic reprogramming. While gene-body methylation occurred at [~]98 % of loci, levels varied, and differentially methylated regions were enriched ffor genes with altered expression under volcanic stress. Multi-omics network analysis identified epithelial morphogenesis, circulatory system formation, and neural development as regulatory hubs, highlighted by a set of 41 epithelial-morphogenesis genes showing consistent methylation and miRNA patterns. Additional modules governing ion transport and signal transduction complemented the adaptive response. Collectively these findings demonstrate that A. gracilis employs dynamic DNA methylation and microRNA regulation alongside transcriptional reprogramming to generate a persistent phenotypic adjustment to a volcanic stress. This work advances our understanding of extremophile resilience and provides a scalable model for predicting organismal adaptive capacity in the face of environmental extremes.

molecular biology↗