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Performing Virtual Global Wellness Diamond (GHE) pursuits in the middle of the international COVID-19 Outbreak: Ways to care for your Department of Defense GHE Business.
Soil DOM properties were modified by organic amendments towards higher aromaticity, molecular weight, and stability. VC resulted in a greater increase of humic-like fractions but reduced protein-like proportions in rhizosphere DOM over BC. Negative correlations were observed between humic-like fractions and available Cd in the rhizosphere. Likewise, VC (especially 5%VC) promoted the formation of Fe-plaque and limited Cd soil-to-root transport, while BC groups showed a reverse trend. The results of hydroponic experiments confirmed BC- and VC-derived DOM and Fe-plaque further inhibited Cd uptake by rice via the complexation with Cd and the sequestration of Cd, respectively. Hence, VC application combined with low Cd-accumulation rice could be an effective strategy for the safe utilization of Cd-contamination soils.Rising ocean temperature impacts the functionality and structure of ecosystems, further triggering the redistribution of biodiversity. Still, the magnitude and anticipated impacts of ocean warming are not expected to be uniform across marine space. Here, we developed a two-fold index-based approach to provide an integrated climatic vulnerability assessment of the marine surfaces which are enclosed within protected areas in the Mediterranean Sea. We first built a climatic stability index, based on metrics of analog-based velocity of climate change over a 120-year period (1950-2069), to assess patterns of climate dynamics within the marine protected surfaces. To provide a vulnerability ranking of protected surfaces under climate change, we combined this climate-related index with an index of community stability, reflecting the projected distribution shifts of 71 species of high conservation value. Our analyses revealed a highly heterogeneous and dynamic climatic space, with increasing but spatially inconsistent patterns of climate change velocities over successive 30-year periods. We found that about 62% of the protected marine surface might be subjected to low/very low climatic stability. About 70% of the protected waters were also found to be of limited community stability. Thus, protected surfaces across the Mediterranean basin were characterized by high vulnerability under changing climatic conditions, while only 5.7% of them exhibited high and very high stability based on both indices. Our findings suggest that combining information on climate change dynamics and biotic stability could offer spatially explicit insights which cannot be obtained based simply on the ecological dimensions of conservation planning.The phase state of biomass burning aerosols (BBA) remains largely unclear, impeding our understanding of their effects on air quality, climate and human health, due to its profound roles in mass transfer between gaseous and particulate phase. In this study, the phase state of BBA was investigated by measuring the particle rebound fraction ƒ combining field observations and laboratory experiments. We found that both ambient and laboratory-generated BBA had unexpectedly lower rebound fraction ƒ ( less then 0.6) under the dry conditions (RH = 20-50%), indicating that BBA were in non-solid state at such low RH. This was obviously different from the secondary organic aerosols (SOA) derived from the oxidation of both anthropogenic and biogenic volatile organic compounds, typically with a rebound fraction ƒ larger than 0.8 at RH below 50%. Therefore, we proposed that the diffusion coefficient of gaseous molecular in the bulk of BBA might be much higher than SOA under the dry conditions.Little information is available about the effects of drought on soil methane (CH4) uptake and the underlying feedback of the soil microbial community in forest biomes. More importantly, a meta-analysis of the current literature on this topic revealed that there are virtually no data available in subtropical forests. Lenalidomide To fill the abovementioned knowledge gap, we carried out a 3-year investigation of in situ CH4 efflux under drought in a subtropical forest, and found that drought significantly increased soil CH4 uptake (P less then 0.001). However, drought did not change oxidation potentials and abundances of methanotrophs, and similar methanotrophic communities were observed between the drought and ambient control sites based on metagenomic sequencing analysis. Active methanotrophic communities were dominated by the genus Methylosinus based on DNA stable-isotope probing analysis. Structural equation model analysis indicated that direct drought-derived pathway, i.e., increasing soil aerations, outweighs the indirect pathway, i.e., altering methanotrophic communities and activities, and plays a predominant role in driving soil CH4 uptake in forest ecosystems. To our knowledge, our work is the first study to investigate the effects of drought on in situ CH4 efflux and the underlying microbial mechanisms in subtropical forests.Ecological communities are structured by several mechanisms, including temporal, spatial and environmental factors. However, the simultaneous effects of these factors have rarely been studied. Here, we investigated their role on water beetle assemblages sampled over a period of 18 years. Water beetles were sampled in the spring of each year in lotic and lentic water bodies from mainland region of Kalmar and Öland Island in southeastern Sweden. We assessed how past assemblage structure, environmental factors and spatial variables correlated with current assemblage structure using a variation partitioning approach. We also tested for correlates of temporal beta diversity of water beetle assemblages with multiple regressions. We found that past water beetle assemblage structure explained current water beetle assemblage structure better than the environmental and spatial correlates. We also observed that temporal beta diversity of water beetle assemblages was mainly due to species gain rather than to species loss. Finally, environmental variables (e.g., hydroperiod, habitat size and hydrology) and timespan between sampling events explained part of temporal beta diversity and contribution of species loss to total assemblage dissimilarity variation. Despite the fact that most variation remained unexplained, we found that ecological factors that have been thought to be important for water beetle richness and abundance in past studies (e.g. water body size, water permanence, shore slope, and whether the water body is lentic or lotic) were also correlated to temporal beta diversity. From a conservation point of view, our study suggest that temporal variability of assemblage structure should be included in biological monitoring because of its potential to predict current assemblage structure.
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