scholarly journals Precipitation Controls on Soil Biogeochemical and Microbial Community Composition in Rainfed Agricultural Systems in Tropical Drylands

2021 ◽  
Vol 13 (21) ◽  
pp. 11848
Author(s):  
Thalita F. Abbruzzini ◽  
Morena Avitia ◽  
Karen Carrasco-Espinosa ◽  
Víctor Peña ◽  
Alberto Barrón-Sandoval ◽  
...  
Keyword(s):  
Microbial Diversity ◽  
Mean Annual Precipitation ◽  
Central Mexico ◽  
Negative Consequences ◽  
Rainfed Agriculture ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
Total N ◽  
Organic C ◽  
P Limitation

The current and expected expansion of agriculture in the drylands of Mexico, together with the decrease in precipitation occurring in the country, likely affect ecosystem processes and will bring great challenges for the suitability of rainfed agriculture for smallholder farmers. Here, we assessed metrics of the soil C, N, and P cycles, as well as soil microbial diversity, under rainfed maize and common bean cropping in arid and semiarid regions of central Mexico. The soil enzymatic vector angles of cultivated plots in both regions were above 45°, suggesting P limitation for microbial growth and crop productivity. Although changes were not observed in the intensity of this P-limitation with aridity, we found a negative effect of drought increase on the concentration of soil organic C and total N, with consequences for the C, N, and P balance in soils. Increasing aridity leads to the homogenization of microbial diversity. Considering a scenario in which decreases in mean annual precipitation would uncouple the biogeochemical cycles and homogenize soil biodiversity, the ecological implications could be an increase in the vulnerability of agricultural ecosystems to drought, with negative consequences for the suitability of rainfed agriculture in the drylands of central Mexico.

scholarly journals Elevation Alone Alters Leaf N and Leaf C to N Ratio of Picea crassifolia Kom. in China’s Qilian Mountains

Forests ◽  
2021 ◽  
Vol 12 (10) ◽  
pp. 1325
Author(s):  
Yalin Niu ◽  
Jianfang Kang ◽  
Haohai Su ◽  
Jan F. Adamowski ◽  
Asim Biswas ◽  
...  
Keyword(s):  
Leaf Nitrogen ◽  
Qilian Mountains ◽  
Mean Annual Precipitation ◽  
Mean Annual Temperature ◽  
Total N ◽  
Organic C ◽  
Picea Crassifolia ◽  
P Limitation ◽  
Leaf Stoichiometry ◽  
Qinghai Spruce

Leaf stoichiometry of plants can respond to variation in environments such as elevation ranging from low to high and success in establishing itself in a given montane ecosystem. An evaluation of the leaf stoichiometry of Qinghai Spruce (Picea crassifolia Kom.) growing at different elevations (2400 m, 2600 m, 2800 m, 3000 m, and 3200 m) in eastern China’s Qilian Mountains, showed that leaf carbon (LC) and leaf phosphorus (LP) were similar among elevations, with ranges of 502.76–518.02 g·kg−1, and 1.00–1.43 g·kg−1, respectively. Leaf nitrogen (LN) varied with changes of elevation, with a maxima of 12.82 g·kg−1 at 2600 m and a minima of 10.74 g·kg−1 at 2800 m. The LC:LN under 2400 m and 2600 m was lower than that under other elevations, while LC:LP and LN:LP were not different among these elevations. Except for LN and LC:LN, P. crassifolia’s other leaf stoichiometries remained relatively stable across elevations, partly supporting the homeostasis hypothesis. Variations in leaf stoichiometry across elevations were mainly linked to mean annual precipitation, mean annual temperature, soil pH, and the soil organic C to soil total N ratio. P. crassifolia growth within the study area was more susceptible to P limitation.

scholarly journals Improvement of Soil Microbial Diversity through Sustainable Agricultural Practices and Its Evaluation by -Omics Approaches: A Perspective for the Environment, Food Quality and Human Safety

2021 ◽  
Vol 9 (7) ◽  
pp. 1400
Author(s):  
Marta Bertola ◽  
Andrea Ferrarini ◽  
Giovanna Visioli
Keyword(s):  
Microbial Diversity ◽  
Food Quality ◽  
Plant Biomass ◽  
Soil Microbial Communities ◽  
Well Being ◽  
Plant Health ◽  
Soil Microbiome ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
Soil Microbial

Soil is one of the key elements for supporting life on Earth. It delivers multiple ecosystem services, which are provided by soil processes and functions performed by soil biodiversity. In particular, soil microbiome is one of the fundamental components in the sustainment of plant biomass production and plant health. Both targeted and untargeted management of soil microbial communities appear to be promising in the sustainable improvement of food crop yield, its nutritional quality and safety. –Omics approaches, which allow the assessment of microbial phylogenetic diversity and functional information, have increasingly been used in recent years to study changes in soil microbial diversity caused by agronomic practices and environmental factors. The application of these high-throughput technologies to the study of soil microbial diversity, plant health and the quality of derived raw materials will help strengthen the link between soil well-being, food quality, food safety and human health.

scholarly journals Soil microbial diversity–biomass relationships are driven by soil carbon content across global biomes

2021 ◽  
Author(s):  
Felipe Bastida ◽  
David J. Eldridge ◽  
Carlos García ◽  
G. Kenny Png ◽  
Richard D. Bardgett ◽  
...  
Keyword(s):  
Microbial Diversity ◽  
Soil Carbon ◽  
Soil Microbial Communities ◽  
Ecosystem Functions ◽  
Arid Environments ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
Soil C ◽  
Soil Microbial ◽  
Biomass Ratio

AbstractThe relationship between biodiversity and biomass has been a long standing debate in ecology. Soil biodiversity and biomass are essential drivers of ecosystem functions. However, unlike plant communities, little is known about how the diversity and biomass of soil microbial communities are interlinked across globally distributed biomes, and how variations in this relationship influence ecosystem function. To fill this knowledge gap, we conducted a field survey across global biomes, with contrasting vegetation and climate types. We show that soil carbon (C) content is associated to the microbial diversity–biomass relationship and ratio in soils across global biomes. This ratio provides an integrative index to identify those locations on Earth wherein diversity is much higher compared with biomass and vice versa. The soil microbial diversity-to-biomass ratio peaks in arid environments with low C content, and is very low in C-rich cold environments. Our study further advances that the reductions in soil C content associated with land use intensification and climate change could cause dramatic shifts in the microbial diversity-biomass ratio, with potential consequences for broad soil processes.

scholarly journals Diversity and asynchrony in soil microbial communities stabilizes ecosystem functioning

2020 ◽  
Author(s):  
Cameron Wagg ◽  
Yann Hautier ◽  
Sarah Pellkofer ◽  
Samiran Banerjee ◽  
Bernhard Schmid ◽  
...  
Keyword(s):  
Microbial Diversity ◽  
Microbial Communities ◽  
Ecosystem Functioning ◽  
Temporal Dynamics ◽  
Temporal Stability ◽  
Soil Microbial Communities ◽  
Ecosystem Functions ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
Soil Microbial

AbstractTheoretical and empirical advances have revealed the importance of biodiversity for stabilizing ecosystem functions through time. Yet despite the global degradation of soils, how the loss of soil microbial diversity can de-stabilizes ecosystem functioning is unknown. Here we experimentally quantified the contribution diversity and the temporal dynamics in the composition of soil microbial communities to the temporal stability of four key ecosystem functions related to nutrient and carbon cycling. Soil microbial diversity loss reduced the temporal stability of all ecosystem functions and was particularly strong when over 50% of microbial taxa were lost. The stabilizing effect of soil biodiversity was linked to asynchrony among microbial taxa whereby different soil fungi and bacteria were associated with different ecosystem functions at different times. Our results emphasize the need to conserve soil biodiversity in order to ensure the reliable provisioning of multiple ecosystems functions that soils provide to society.

scholarly journals Grazing effects on soil characteristics and vegetation of grassland in northern China

2015 ◽  
Vol 7 (3) ◽  
pp. 2283-2309 ◽  
Author(s):  
Z. Wang ◽  
D. A. Johnson ◽  
Y. Rong
Keyword(s):  
Grazing Intensity ◽  
Northern China ◽  
Soil Heterogeneity ◽  
Soil Characteristics ◽  
Total Biomass ◽  
Negative Consequences ◽  
Total N ◽  
Organic C ◽  
Heavy Grazing ◽  
Vegetation Characteristics

Abstract. Large areas of grassland in the agro-pastoral region of northern China were converted into cropland for grain production, and the remaining grasslands are being overgrazed and seriously degraded. The objective of this study was to evaluate how reductions in grazing intensity affect the soil and vegetation characteristics in grasslands of northern China. Soil heterogeneity and vegetation characteristics were evaluated for ungrazed (UG), moderate grazing (MG), and heavy grazing (HG) sites. Grazing increased diversity, but heavy grazing decreased aboveground biomass and increased the non-grass component. Vegetation biomass was greatest at the UG site (220 g m−2) followed by the MG (99 g m−2) and HG (27 g m−2) sites (P < 0.05). The non-grass proportion of total biomass increased with grazing intensity, which was 8, 16, and 48 % for UG, MG, and HG sites, respectively. Species richness at the MG and HG sites was significantly higher than at the UG site (P < 0.05) with 3.6, 5.5, and 5.7 for UG, MG, and HG sites, respectively. Over grazing homogenized soil characteristics at a 10 m scale. The ranges of spatial autocorrelation for soil organic C (SOC) and total N were both > 120 m at the HG site, which was considerably larger than that at the MG and UG sites with corresponding distances of 17.3 and 20.8 m for the MG site and 25.8 and 15.0 m for the UG site, respectively. Therefore, MG was recommended as the preferred management alternative for grasslands in northern China because of increased plant diversity without negative consequences related to decreased forage quality and forage quantity, and soil heterogeneity in northern China's grasslands.

scholarly journals Diversity and asynchrony in soil microbial communities stabilizes ecosystem functioning

eLife ◽  
2021 ◽  
Vol 10 ◽  
Author(s):  
Cameron Wagg ◽  
Yann Hautier ◽  
Sarah Pellkofer ◽  
Samiran Banerjee ◽  
Bernhard Schmid ◽  
...  
Keyword(s):  
Microbial Diversity ◽  
Ecosystem Functioning ◽  
Temporal Stability ◽  
Soil Microbial Communities ◽  
Ecosystem Functions ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
Soil Microbial ◽  
Plant Soil ◽  
Soil Mesocosms

Theoretical and empirical advances have revealed the importance of biodiversity for stabilizing ecosystem functions through time. Despite the global degradation of soils, whether the loss of soil microbial diversity can destabilize ecosystem functioning is poorly understood. Here, we experimentally quantified the contribution of soil fungal and bacterial communities to the temporal stability of four key ecosystem functions related to biogeochemical cycling. Microbial diversity enhanced the temporal stability of all ecosystem functions and this pattern was particularly strong in plant-soil mesocosms with reduced microbial richness where over 50% of microbial taxa were lost. The stabilizing effect of soil biodiversity was linked to asynchrony among microbial taxa whereby different soil fungi and bacteria promoted different ecosystem functions at different times. Our results emphasize the need to conserve soil biodiversity for the provisioning of multiple ecosystem functions that soils provide to the society.

scholarly journals Grazing effects on soil characteristics and vegetation of grassland in northern China

Solid Earth ◽  
2016 ◽  
Vol 7 (1) ◽  
pp. 55-65 ◽  
Author(s):  
Z. Wang ◽  
D. A. Johnson ◽  
Y. Rong ◽  
K. Wang
Keyword(s):  
Soil Properties ◽  
Grazing Intensity ◽  
Northern China ◽  
Soil Heterogeneity ◽  
Soil Characteristics ◽  
Negative Consequences ◽  
Total N ◽  
Organic C ◽  
Heavy Grazing ◽  
Vegetation Characteristics

Abstract. Large areas of grassland in the agro-pastoral region of northern China were converted into cropland for grain production, and the remaining grasslands are being overgrazed and seriously degraded. The objective of this study was to evaluate how reductions in grazing intensity affect the soil and vegetation characteristics in grasslands of northern China. Soil heterogeneity and vegetation characteristics were evaluated for ungrazed (UG), moderate grazing (MG), and heavy grazing (HG) sites. Grazing increased diversity, but heavy grazing decreased aboveground biomass and increased the non-grass component. The non-grass proportion of total biomass increased with grazing intensity, which was 8, 16 and 48 % for UG, MG and HG sites, respectively. Species richness at the MG and HG sites was significantly higher than at the UG site (P< 0.05) with 3.6, 5.5 and 5.7 for UG, MG and HG sites, respectively. Strong spatial dependence of the examined soil properties at 10 m scale for all grazed sites was revealed by the ratio of nugget to total variation (0–23 %). Overgrazing homogenized soil characteristics at a 10 m scale. The ranges of spatial autocorrelation for soil organic C (SOC) and total N were both > 120 m at the HG site, which was considerably larger than that at the MG and UG sites with corresponding distances of 17.3 and 20.8 m for the MG site and 8.6 and 15.0 m for the UG site, respectively. The sampling density and sampling space for the HG site could be decreased under this scale sampling interval (10 m). Therefore, MG was recommended as the preferred management alternative for grasslands in northern China because of increased plant diversity without negative consequences related to decreased forage quality, forage quantity and soil heterogeneity for the investigated soil properties in northern China's grasslands.

Microbial biomass and microbial biodiversity in some soils from New South Wales, Australia

Soil Research ◽  
2004 ◽  
Vol 42 (7) ◽  
pp. 777 ◽  
Author(s):  
Nargis A. Banu ◽  
Balwant Singh ◽  
Les Copeland
Keyword(s):  
Microbial Biomass ◽  
Microbial Diversity ◽  
Climatic Factors ◽  
Microbial Biomass Carbon ◽  
New South ◽  
New South Wales ◽  
Total N ◽  
Organic C ◽  
Free Iron ◽  
South Wales

Eight surface soils (0–15 cm) including 1 Ferrosol, 2 Tenosols, 2 Kurosols, 1 Sodosol, 1 Chromosol, and 1 Kandosol were collected from mainly pasture sites in New South Wales. The soils had different physico-chemical properties and there were some differences between the sites in climatic conditions. Soil microbial biomass carbon (MBC) was estimated by the chloroform-fumigation extraction method, and substrate utilisation patterns determined by the Biolog method were used to assess the amount, functional diversity, substrate richness and evenness, and community structure of the microorganisms in these soils. The amount of MBC (585 µg C/g) and the microbial diversity (H´ = 3.24) were high in soils that had high clay (33%), organic C (5.96%), total N (0.45%), free iron (7.06%), moisture content (50%), and cation exchange capacitiy (133.5 mmolc/kg). These soil properties, e.g. soil moisture (r2 = 0.72), organic C (r2 = 0.58), total N (r2 = 0.63), free iron (r2 = 0.44), and EC (r2 = 0.53), were positively correlated with MBC and microbial diversity index, whereas pH and sand and silt content showed negative correlations. The climatic factors (temperature and rainfall) had no significant influence on either MBC or diversity.

scholarly journals High Microbial Diversity Promotes Soil Ecosystem Functioning

2018 ◽  
Vol 84 (9) ◽  
Author(s):  
Pierre-Alain Maron ◽  
Amadou Sarr ◽  
Aurore Kaisermann ◽  
Jean Lévêque ◽  
Olivier Mathieu ◽  
...  
Keyword(s):  
Organic Matter ◽  
Ecosystem Services ◽  
Microbial Diversity ◽  
Functional Redundancy ◽  
Plant Residues ◽  
Soil Ecosystem ◽  
Soil Microbial Diversity ◽  
Soil Biodiversity ◽  
C Cycling ◽  
Autochthonous Organic Matter

ABSTRACTIn soil, the link between microbial diversity and carbon transformations is challenged by the concept of functional redundancy. Here, we hypothesized that functional redundancy may decrease with increasing carbon source recalcitrance and that coupling of diversity with C cycling may change accordingly. We manipulated microbial diversity to examine how diversity decrease affects the decomposition of easily degradable (i.e., allochthonous plant residues) versus recalcitrant (i.e., autochthonous organic matter) C sources. We found that a decrease in microbial diversity (i) affected the decomposition of both autochthonous and allochthonous carbon sources, thereby reducing global CO2emission by up to 40%, and (ii) shaped the source of CO2emission toward preferential decomposition of most degradable C sources. Our results also revealed that the significance of the diversity effect increases with nutrient availability. Altogether, these findings show that C cycling in soil may be more vulnerable to microbial diversity changes than expected from previous studies, particularly in ecosystems exposed to nutrient inputs. Thus, concern about the preservation of microbial diversity may be highly relevant in the current global-change context assumed to impact soil biodiversity and the pulse inputs of plant residues and rhizodeposits into the soil.IMPORTANCEWith hundreds of thousands of taxa per gram of soil, microbial diversity dominates soil biodiversity. While numerous studies have established that microbial communities respond rapidly to environmental changes, the relationship between microbial diversity and soil functioning remains controversial. Using a well-controlled laboratory approach, we provide empirical evidence that microbial diversity may be of high significance for organic matter decomposition, a major process on which rely many of the ecosystem services provided by the soil ecosystem. These new findings should be taken into account in future studies aimed at understanding and predicting the functional consequences of changes in microbial diversity on soil ecosystem services and carbon storage in soil.

Effect of crop management on C and N in long-term crop rotations after adopting no-tillage management: Comparison of soil sampling strategies

1998 ◽  
Vol 78 (1) ◽  
pp. 155-162 ◽  
Author(s):  
C. A. Campbell ◽  
F. Selles ◽  
G. P. Lafond ◽  
B. G. McConkey ◽  
D. Hahn
Keyword(s):  
Organic Matter ◽  
Crop Rotations ◽  
No Tillage ◽  
Negative Consequences ◽  
Total N ◽  
Organic C ◽  
Soil C ◽  
Soil C And N ◽  
C And N ◽  
Over Time

Society is interested in increasing C storage in soil to reduce CO2 concentration in the atmosphere, because the latter may contribute to global warming. Further, there is considerable interest in the use of straw for industrial purposes. Using soil samples taken from the 0- to 7.5-cm and 7.5- to 15-cm depths in May 1987 and September 1996, we determined organic C and total N in five crop rotations (nine treatments) using automated Carlo Erba combustion analyzer. The experiment was managed using conventional mechanical tillage from 1957 to 1989; it was changed to no-tillage management in 1990. Our objective was to determine: (a) if change to no-tillage management had changed soil C and N storage, and (b) if method of calculating organic C and N change would influence interpretation of the results. All three methods of calculation confirmed the efficacy of employing best management practices (e.g., fertilization based on soil tests, reducing summerfallow, including legumes in rotations) for increasing or maintaining soil organic matter, and showed that the latter was directly associated with the amount of crop residues returned to the soil. Where bulk density was significantly different between sampling times, the often used mass per fixed depth (MFD) (i.e., volume basis) calculation can lead to erroneous conclusions. When the recently recommended mass per equal depth (MED) method of calculation was used, it showed that 6 yr of no-tillage did not increase soil organic C or total N. However, in unfertilized systems, where crop yields are gradually decreasing since the change, there is an accompanying decrease in organic matter, while fertilized, or high-fertility systems that include legume hay crops, in which wheat yields have been maintained have tended to maintain the organic matter level over time. When the MFD calculation was used, there was no change in C over time when straw was harvested in the F–W–W system; however, the MED calculation and concentrations tend to show a decrease in soil C and N. This suggests that in time, industrial use of straw may have negative consequences for soil conservation. We concluded that concentrations may be as effective as MED for assessing changes in organic matter, provided "amounts" are not required. Key words: Straw removal, fertilizers, legumes, cropping frequency, C mass calculation

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