Stable Isotope Ecology (CER, Kyoto Univ.)
@stableisotopeecol.bsky.social
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Facility for Stable Isotope Ecology in CER, Kyoto U. (w Kei Koba, he/him). Papers using stable isotopes I just found, status of our IRMSs. http://www.ecology.kyoto-u.ac.jp/~keikoba/english/KobaEnglish.html
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stableisotopeecol.bsky.social
Mirabella, J., von Haden, A., Sanford, G. et al. Fate of synthetic fertilizer nitrogen in a maize system depends on dairy manure type: insights from an isotopic tracing field study. #stableisotopes Biol Fertil Soils 61, 1405–1421 (2025). doi.org/10.1007/s003...
Fate of synthetic fertilizer nitrogen in a maize system depends on dairy manure type: insights from an isotopic tracing field study - Biology and Fertility of Soils
Understanding the fate of fertilizer nitrogen (N) in cropping systems is critical to improving agricultural sustainability and minimizing environmental losses. However, efforts to trace fertilizer N are often complicated by manure application in dairy cropping systems. We used a stable isotope tracing approach to investigate how different manure products influence the fate of synthetic fertilizer N in a Midwestern maize silage system by tracking 15N-labled ammonium sulfate into crop biomass, soil organic matter fractions (particulate (POM) and mineral associated (MAOM)), and gaseous loss as nitrous oxide (N2O). Treatments included unprocessed liquid manure (LM), solid manure derived through chemical (CS) or physical (PS) separation, and a no-manure control (NM), combined with fertilizer rates of 90, 180, and 270 kg N ha−1. Cumulative N2O emissions increased significantly with both manure application and higher fertilizer rates, with PS having lower emissions than LM following fertilizer application. Fertilizer contributed similar proportions to cumulative N2O emissions regardless of manure treatment. Total fertilizer N uptake by crops did not differ among manure treatments, but crops took up more fertilizer N at higher fertilizer application rates. Notably, application of CS and PS enhanced fertilizer N retention in the 0–15 cm soil MAOM pool compared to LM and NM. These findings highlight that although manure type does not significantly affect fertilizer N uptake by crops or fertilizer-derived N2O emissions, solid manures (i.e., CS and PS) can significantly increase fertilizer N retention in soils, offering potential benefits for long-term soil fertility and reduced N losses.
doi.org
stableisotopeecol.bsky.social
Leuthold, S.J., Lavallee, J.M., Haddix, M.L. et al. Quantifying the contribution of MAOM to mineral nitrogen pools under various soil organic matter conditions. #stableisotopes Biol Fertil Soils 61, 1391–1404 (2025). doi.org/10.1007/s003...
Quantifying the contribution of MAOM to mineral nitrogen pools under various soil organic matter conditions - Biology and Fertility of Soils
In cropland soils, the majority of organic nitrogen (N) is stored in the mineral associated organic matter (MAOM) fraction of soil organic matter (SOM). Because strong bonds with mineral surfaces are thought to limit microbial access to MAOM, particulate organic matter (POM) is often assumed to drive N mineralization and nutrient cycling, despite being a smaller and more N-poor pool. Emerging evidence suggests that N in MAOM can be mobilized into mineralization pathways, challenging this assumption. Yet, when and how MAOM contributes to N mineralization remains unclear, particularly how SOM quantity, composition, and stoichiometry influence its contribution. To examine these dynamics, we reconstructed soils from physically isolated POM and MAOM fractions, systematically varying SOM composition. The MAOM was isolated from a soil previously amended with 15N fertilizer, which retained a distinct isotopic signature relative to the POM fraction. Leveraging this difference in isotopic composition, we applied a two-pool isotopic mixing model, with POM and MAOM as the endmembers, to quantify the contribution of both fractions to mineral N production. Across treatments, we observed strong effects of SOM content, POM C:N ratio, and POM:MAOM ratio on mineral N production. In the treatment most representative of agricultural soil conditions, ~ 75% of mineralized N originated from the MAOM. Higher POM C:N ratios increased the proportional contribution of MAOM to mineralized N, consistent with hypotheses around microbial N mining. While POM mineralized more rapidly on a per-unit basis, MAOM consistently contributed more total N to the mineralized pool. These findings demonstrate that MAOM can be a dominant source of mineralized N across a range of SOM conditions, even in the presence of high-quality POM. As MAOM represents the largest pool of organic N in cropland soils, understanding the factors governing its turnover is essential for improving nutrient management.
doi.org
stableisotopeecol.bsky.social
Zhang, S., Li, ZP., Wang, B. et al. Litter complexity rather than land-use intensity emerges as a key driver of taxonomic and isotopic diversity of Collembola in urban systems. #stableisotopes Biol Fertil Soils 61, 1329–1342 (2025). doi.org/10.1007/s003...
Litter complexity rather than land-use intensity emerges as a key driver of taxonomic and isotopic diversity of Collembola in urban systems - Biology and Fertility of Soils
Land-use changes caused by urbanization profoundly impact biodiversity and ecosystem functioning. The impact of land-use changes on soil invertebrate communities has garnered attention, but few studies focused on how the intensity of land-use change associated with urbanization affects soil invertebrates. In this study, we investigated variations in Collembola taxonomic and isotopic diversity in four land-use types (natural forests, urban forests, urban parks and green median strips) in a subtropical city, representing a gradient of increasing land-use intensity. Collembola richness and biomass did not follow the studied land-use intensity gradient, rather, they were high in urban parks but low in urban forests. Similarly, isotopic diversity, as an indicator of niche diversity of Collembola communities, did not correlate with land-use intensity, with isotopic richness peaking in natural forests and urban parks, while isotopic uniqueness being highest in urban forests. Litter properties explained major variations in both taxonomic and isotopic diversity of Collembola, with their impacts largely outweighing those of land-use intensity and soil properties. Particularly, litter complexity, as indicated by litter species richness and the amount of decomposed litter, was the major factor promoting Collembola richness, biomass and isotopic diversity, while litter nutrients and moisture content played a subordinate role. Overall, our study demonstrates that well-managed urban greenspaces can act as restoration hubs for soil invertebrate communities. To foster soil animal communities and associated ecological functions in city systems, management approaches promoting litter complexity by increasing native plant diversity and litter accumulation should be adopted.
doi.org
stableisotopeecol.bsky.social
Tidal pumping controls transport of foodborne microbial pathogens between coastal groundwater and seawater #stableisotopes ttps://www.sciencedirect.com/science/article/pii/S0304389425028225