• Energy Research

Live feed organisms are essential for the larval stages of many fish species grown in aquaculture, and juvenile fish reared on live feeds often exhibit higher survival and growth than those reared on formulated feed. The terrestrial enchytraeid (white worm), Enchytraeus albidus, has potential as a sustainable source of live feed because it can easily be mass produced, feeds on a wide range of organic waste materials and has high contents of protein and long-chain poly-unsaturated fatty acids. In the present study, we observed the effect of temperature on population growth over five months using soil microcosms. At the outset, each microcosm was supplied with approximately the same number of cocoons. Hatched enchytraeids were given rolled oats ad libitum as feed. We followed the population growth at seven temperatures in the range of 4-25 °C and investigated body composition in order to find optimal temperature for mass production. Results showed that E. albidus has a broad thermal optimum range and displays almost similar biomass production in the range of 15-22 °C with specific growth rates between 6.5 and 6.8%. In this temperature range, protein contents were 40-45%, glycogen contents 20-25% and total fatty acid contents 15-20% of dry weight. The temperature had a highly significant effect on fatty acid composition. In particular, the abundance of omega-3 fatty acids (18:3ω3 and 20:5ω3) was largest at low temperature. For what concerns achievable density of worms in mass cultures, our results surpassed previous results and showed that densities close to 100 g L-1 substrate are realistic. Maximum production of biomass can likely reach 80 g live worms L-1 month-1 at temperatures between 15 and 22 °C.

Knowledge of the effect of plant secondary compounds (PSCs) on belowground interactions in the more diffuse community of species living outside the rhizosphere is sparse compared with what we know about how PSCs affect aboveground interactions. We illustrate here that PSCs from foliar tissue, root exudates, and leaf litter effectively influence such belowground plant-plant, plant-microorganism, and plant-soil invertebrate interactions. Climatic factors can induce PSC production and select for different plant chemical types. Therefore, climate change can alter both quantitative and qualitative PSC production, and how these compounds move in the soil. This can change the soil chemical environment, with cascading effects on both the ecology and evolution of belowground species interactions and, ultimately, soil functioning.

AbstractClimate change has led to pronounced shifts in phenology, varying across taxa. The Arctic is experiencing particularly rapid warming, but long‐term data on phenological changes are rare in this region, especially for arthropods—a diverse taxonomic group that form important links to other trophic levels. Understanding the environmental drivers of arthropod phenological variation is necessary for predicting future trends across taxa and habitats to climate change. Here, we analyze temporal trends and climate associations in arthropod phenology using 25 years of standardized monitoring data from four habitat types in high‐Arctic Greenland. We observed earlier peak activity in the arthropod community, with responses varying considerably among families and habitats. Snowmelt timing was a key driver of peak activity, especially for late‐active taxa, while temperature was a less important driver, but arthropods generally exhibited earlier activity with warming. Responses in the duration of activity were more complex, with family‐ and habitat‐specific responses to climate variation. Notably, taxa in habitats with late snowmelt responded strongly to snowmelt timing, while those in the pond habitat responded strongly to temperature. Mixed feeders and parasitoids showed rapid peak phenological shifts to earlier snowmelt and warming; however, mixed feeders shortened their activity periods, while parasitoids extended theirs. Our findings highlight the complexity of arthropod community phenological responses to climate change, with potential implications for trophic interactions dependent on temporal overlap. By analyzing phenological metrics across entire activity seasons for taxa with different functional and life‐history traits, we identify general trends and consistent patterns that enhance our understanding of arthropod responses to climate change.

Earthworm distribution in global soils Earthworms are key components of soil ecological communities, performing vital functions in decomposition and nutrient cycling through ecosystems. Using data from more than 7000 sites, Phillips et al. developed global maps of the distribution of earthworm diversity, abundance, and biomass (see the Perspective by Fierer). The patterns differ from those typically found in aboveground taxa; there are peaks of diversity and abundance in the mid-latitude regions and peaks of biomass in the tropics. Climate variables strongly influence these patterns, and changes are likely to have cascading effects on other soil organisms and wider ecosystem functions. Science , this issue p. 480 ; see also p. 425