Soil Biology and Biochemistry, Journal Year: 2024, Volume and Issue: unknown, P. 109696 - 109696
Published: Dec. 1, 2024
Language: Английский
Soil Biology and Biochemistry, Journal Year: 2024, Volume and Issue: unknown, P. 109696 - 109696
Published: Dec. 1, 2024
Language: Английский
Soil Biology and Biochemistry, Journal Year: 2023, Volume and Issue: 189, P. 109252 - 109252
Published: Nov. 22, 2023
Language: Английский
Citations
23Global Change Biology, Journal Year: 2024, Volume and Issue: 30(2)
Published: Feb. 1, 2024
Highly weathered lowland (sub)tropical forests are widely recognized as nitrogen (N)-rich and phosphorus (P)-poor, the input of N P affects soil carbon (C) cycling storage in these ecosystems. Microbial residual C (MRC) plays a crucial role regulating organic (SOC) stability forest soils. However, effects long-term addition on MRC across different layers remain unclear. This study conducted 12-year experiment two typical subtropical plantation dominated by Acacia auriculiformis Eucalyptus urophylla trees, respectively. We measured plant (fine root biomass, fine C, litter C), microbial community structure, enzyme activity (C/N/P-cycling enzymes), mineral properties, MRC. Our results showed that continuous reduced subsoil (20-40 cm) both plantations (A. auriculiformis: 28.44% E. urophylla: 28.29%), whereas no significant changes occurred topsoil (0-20 cm). decreased (25.44%), but had A. auriculiformis. Combined (34.63%) not urophylla. The factors varied layers. In (0-10 cm), (the relative contributions to total variance was 20%, hereafter) protection (47.2%) were dominant factors. layer 10-20 cm, characteristics (41.3%) (32.3%) substantial effects, deeper predominantly regulated (37.9%) (18.8%). Understanding differential drivers depth, particularly layers, is for accurately predicting SOC its responses chronic enrichment and/or increased limitation forests.
Language: Английский
Citations
12Global Change Biology, Journal Year: 2023, Volume and Issue: 30(1)
Published: Nov. 13, 2023
Abstract Microbes inhabiting deep soil layers are known to be different from their counterpart in topsoil yet remain under investigation terms of structure, function, and how diversity is shaped. The microbiome soils (>1 m) expected relatively stable highly independent climatic conditions. Much less known, however, on these microbial communities vary along climate gradients. Here, we used amplicon sequencing investigate bacteria, archaea, fungi fifteen 18‐m depth profiles at 20–50‐cm intervals across contrasting aridity conditions semi‐arid forest ecosystems China's Loess Plateau. Our results showed that bacterial fungal α archaeal community similarity declined dramatically remained soil. Nevertheless, still the functional potential N cycling, plant‐derived organic matter degradation, resource exchange, water coordination. had closer taxa–taxa bacteria–fungi associations more influence dispersal limitation than microbiome. Geographic distance was influential bacteria archaea topsoil. We further negatively correlated with deep‐soil richness, similarity, relative abundance plant saprotroph, associations, but increased aerobic ammonia oxidation, manganese arbuscular mycorrhizal soils. Root depth, complexity, volumetric moisture, clay play bridging roles indirect effects microbes work indicates that, even nutrient cycling susceptible changes availability, consequences for understanding sustainability dryland whole‐soil response aridification. Moreover, propose neglecting may underestimate role moisture future scenarios.
Language: Английский
Citations
17The Science of The Total Environment, Journal Year: 2024, Volume and Issue: 918, P. 170295 - 170295
Published: Jan. 24, 2024
Language: Английский
Citations
7The Science of The Total Environment, Journal Year: 2024, Volume and Issue: 930, P. 172630 - 172630
Published: April 26, 2024
Language: Английский
Citations
6Global Change Biology, Journal Year: 2023, Volume and Issue: 29(24), P. 7159 - 7172
Published: Oct. 13, 2023
The frequency and intensity of droughts worldwide are challenging the conservation soil organic carbon (SOC) pool. Microbial necromass is a key component SOC, but how it responds to drought at specific depths remains largely unknown. Here, we conducted 3-year field experiment in forest plantation investigate impacts intensities under three treatments (ambient control [CK], moderate [30% throughfall removal], intensive [50% removal]) on microbial pools (i.e., bacterial carbon, fungal total carbon). We showed that effects depended groups, depth, intensity. While increased (+9.1% ± 3.3%) (+13.5% 4.9%) topsoil layer (0-15 cm), reduced (-31.6% 3.7%) (-43.6% 4.0%) subsoil (15-30 cm). In contrast, both significantly BNC subsoil. Our results suggested were more pronounced than those topsoil. This study highlights complex responses events depending community structure, depth with global implications when forecasting cycling climate change.
Language: Английский
Citations
14Biology and Fertility of Soils, Journal Year: 2024, Volume and Issue: 60(6), P. 799 - 812
Published: May 27, 2024
Language: Английский
Citations
5Environmental Science & Technology, Journal Year: 2024, Volume and Issue: 58(35), P. 15629 - 15637
Published: June 11, 2024
Foliar assimilation of elemental mercury (Hg
Language: Английский
Citations
5Global Change Biology, Journal Year: 2024, Volume and Issue: 30(2)
Published: Jan. 29, 2024
Abstract Terrestrial ecosystems are increasingly being exposed to metallic nanoparticles (MNPs). However, the global‐scale impact of MNPs on soil carbon dioxide (CO 2 ) emission remains unknown, limiting our understanding role in global cycle. We compiled a dataset comprising 1764 pairs experimental observations investigate effects exposure respiration parameters, including rates, related enzyme activities, and microbial variables. found that could stimulate or suppress basal rates across environments, depending largely type MNPs. further showed that, although inhibition most activities peaked short‐term (≤28 days), prolonged still inhibited organic degradation. Finally, we determined environmental conditions (e.g., pH presence/absence plants) were also important regulators influence parameters. Our findings underline CO depended type, design, factors, which is critical for predicting influencing cycle climate change.
Language: Английский
Citations
4Soil and Tillage Research, Journal Year: 2025, Volume and Issue: 248, P. 106450 - 106450
Published: Jan. 10, 2025
Language: Английский
Citations
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