Nutrient uptake in streams draining agricultural catchments of the midwestern United States

1. Agriculture is a major contributor of non‐point source pollution to surface waters in the midwestern United States, resulting in eutrophication of freshwater aquatic ecosystems and development of hypoxia in the Gulf of Mexico. Agriculturally influenced streams are diverse in morphology and have variable nutrient concentrations. Understanding how nutrients are transformed and retained within agricultural streams may aid in mitigating increased nutrient export to downstream ecosystems. 2. We studied six agriculturally influenced streams in Indiana and Michigan to develop a more comprehensive understanding of the factors controlling nutrient retention and export in agricultural streams using nutrient addition and isotopic tracer studies. 3. Metrics of nutrient uptake indicated that nitrate uptake was saturated in these streams whereas ammonium and phosphorus uptake increased with higher concentrations. Phosphorus uptake was likely approaching saturation as evidenced by decreasing uptake velocities with concentration; ammonium uptake velocity also declined with concentration, though not significantly. 4. Higher whole‐stream uptake rates of phosphorus and ammonium were associated with the observed presence of stream autotrophs (e.g. algae and macrophytes). However, there was no significant relationship between measures of nutrient uptake and stream metabolism. Water‐column nutrient concentrations were positively correlated with gross primary production but not community respiration. 5. Overall, nutrient uptake and metabolism were affected by nutrient concentrations in these agriculturally influenced streams. Biological uptake of ammonium and phosphorus was not saturated, although nitrate uptake did appear to be saturated in these ecosystems. Biological activity in agriculturally influenced streams is higher relative to more pristine streams and this increased biological activity likely influences nutrient retention and transport to downstream ecosystems.     

Multi‐nutrient vs. nitrogen‐only effects on carbon sequestration in grassland soils

Human activities have greatly increased the availability of biologically active forms of nutrients [e.g., nitrogen (N), phosphorous (P), potassium (K), magnesium (Mg)] in many soil ecosystems worldwide. Multi‐nutrient fertilization strongly increases plant productivity but may also alter the storage of carbon (C) in soil, which represents the largest terrestrial pool of organic C. Despite this issue is important from a global change perspective, key questions remain on how the single addition of N or the combination of N with other nutrients might affect C sequestration in human‐managed soils. Here, we use a 19‐year old nutrient addition experiment on a permanent grassland to test for nutrient‐induced effects on soil C sequestration. We show that combined NPKMg additions to permanent grassland have ‘constrained’ soil C sequestration to levels similar to unfertilized plots whereas the single addition of N significantly enhanced soil C stocks (N‐only fertilized soils store, on average, 11 t C ha^?1 more than unfertilized soils). These results were consistent across grazing and liming treatments suggesting that whilst multi‐nutrient additions increase plant productivity, soil C sequestration is increased by N‐only additions. The positive N‐only effect on soil C content was not related to changes in plant species diversity or to the functional composition of the plant community. N‐only fertilized grasslands show, however, increases in total root mass and the accumulation of organic matter detritus in topsoils. Finally, soils receiving any N addition (N only or N in combination with other nutrients) were associated with high N losses. Overall, our results demonstrate that nutrient fertilization remains an important global change driver of ecosystem functioning, which can strongly affect the long‐term sustainability of grassland soil ecosystems (e.g., soils ability to deliver multiple ecosystem services).     

The aquaporin MePIP2;7 improves MeMGT9-mediated Mg2+ acquisition in cassava

Aquaporins are important transmembrane water transport proteins which transport water and several neutral molecules. However, how aquaporins are involved in the synergistic transport of Mg²⁺and water remains poorly understood. Here, we found that the cassava aquaporin Me PIP2;7 was involved in Mg²⁺transport through interaction with Me MGT9, a lower affinity magnesium transporter protein. Knockdown of Me PIP2;7 in cassava led to magnesium deficiency in basal mature leaves wi...     

Nutrient uptake and accumulation by sugarcane cell cultures in relation to the growth cycle

Growth characteristics and nutrient changes in medium and cells of batch-grown sugarcane cultures were investigated over a period of 14 days. Amino acids, PO ₄ ³⁻ and K⁺ were substantially removed from the medium during the first seven days of culture; a strong preference for uptake of organic nitrogen over inorganic nitrogen was observed. Sodium uptake increased during the time when K⁺ was becoming deficient in the medium. The main anions taken up were SO ₄ ²⁻ and PO ₄ ³⁻ . Strong acidification and a virtually total extracellular hydrolysis of sucrose in the medium during the first seven days of culture were also observed. Tapering off of the rapid growth phase was accompanied by an increase of intra-cellular sucrose and a decrease of intracellular protein. As cells went from rapid growth into stationary phase, cytoplasmic space of the cells decreased slightly in favor of vacuolar space. Overall cell volume stayed constant throughout the growth cycle, except during a short period before onset of rapid growth. Transport of the glucose analog 3-O-methyl glucose remained constant in terms of K_m value but the V_max was slightly higher in rapidly growing cells. Published with the approval of the Director as paper no. 495 in theJournal Series of the Experiment Station, Hawaiian Sugar Planters' Association     

Nutrient dynamics at the interface between surface waters and groundwaters

1. The surface water/groundwater (SW/GW) interface is a crucial control point for lateral nutrient fluxes between uplands and aquatic ecosystems and for upstream/downstream (longitudinal) processes in lotic ecosystems. 2. Hydrological and biogeochemical dynamics of the SW/GW ecotone are linked to the degree of channel constraint and the sediment characteristics of the floodplain and stream bed. 3. The availability of specific chemical forms of electron donors and electron acceptors affects the spatial distribution of biogeochemical processes at the SW/GW interface. Temporal change in discharge is also a major factor affecting the rate and extent of these processes. 4. The magnitude of SW/GW interactions in lotic ecosystems is predicted to be a major determinant of solute retention. Channel morphology, stream bed composition and discharge are predicted to be important controls on SW/GW interactions. 5. Interdisciplinary research involving hydrologists, geomorphologists, aquatic ecologists, microbial ecologists and landscape ecologists is needed to further our present understanding of this critical interface linking terrestrial and aquatic ecosystems.     

Determination of the Limiting Plant Nutrient in the Water of Lake Balaton by Algal Assay Procedure

Algal assays were performed on water samples taken from different sites in Lake Balaton. Selenastrum capricornutum was used in the test to determine the primarily limiting plant nutrient. The results of supplementary nutrient additions to the bottle tests were evaluated by cell counts. The tests have indicated phosphorus as growth rate limiting, and in two cases as biomass limiting plant nutrient, but periodic occurrences of nitrogen limitation cannot be excluded.     

青藏高原典型冰川小流域土壤微生物生物量及胞外酶活性分布特征

土壤微生物释放的胞外酶是决定碳(C)、氮(N)、磷(P)生物地球化学循环的关键因素,为了阐明青藏高原典型小流域土壤微生物生物量和胞外酶活性沿海拔和土层的分布特征并揭示影响该分布格局的主要养分限制状况,于2021年8月采集了青藏高原廓琼岗日冰川小流域5个海拔梯度(4900 m; 5000 m; 5100 m; 5200 m; 5300 m)中4个土壤发生层(A层：腐殖质层、E层：淋溶层、B层：淀积层和C层：母质层)的土壤样品,定量分析了土壤基本理化性质、微生物生物量、胞外酶活性等指标。结果表明：1)微生物生物量碳氮磷的海拔差异变化规律不同,随着土层加深微生物生物量碳氮磷随海拔变化越小。同时,各海拔之间微生物生物量均有随土层加深而显著降低的趋势(P<0.05);2)四种酶活性的海拔间变化规律各异,但整体呈现随海拔升高而升高的趋势且在表层(A和E层)增长趋势更明显,而且随土层加深显著降低(P<0.05);3)该区域土壤微生物受到碳和磷共同限制,土层越深限制越高,而且海拔越高C限制越强,但P限制降低;4)青藏高原典型冰川小流域土壤微生物生物量和胞外酶活性在海拔和土层之间存在较明显的...     

Nutrients Changed the Assembly Processes of Profuse and Rare Microbial Communities in Coals

Nutrient stimulation is considered effective for improving biogenic coalbed methane production potential. However, our knowledge of the microbial assembly process for profuse and rare microbial communities in coals under nutrient stimulation is still limited. This study collected 16S rRNA gene data from 59 microbial communities in coals for a meta-analysis. Among these communities, 116 genera were identified as profuse taxa, and the remaining 1,637 genera were identified as rare taxa. Nutrient stimulation increased the Chao1 richness of profuse and rare genera and changed the compositions of profuse and rare genera based on nonmetric multidimensional scaling with Bray-Curtis dissimilarities. In addition, many profuse and rare genera belonging to Proteobacteria and Acidobacteria were reduced, whereas those belonging to Euryarchaeota and Firmicutes were increased under nutrient stimulation. Concomitantly, the microbial co-occurrence relationship network was also altered by nutrient addition, and many rare genera mainly belonging to Firmicutes, Bacteroides, and Euryarchaeota also comprised the key microorganisms. In addition, the compositions of most of the profuse and rare genera in communities were driven by stochastic processes, and nutrient stimulation increased the relative contribution of dispersal limitation for both profuse and rare microbial community assemblages and that of variable selection for rare microbial community assemblages. In summary, this study strengthened our knowledge regarding the mechanistic responses of coal microbial diversity and community composition to nutrient stimulation, which are of great importance for understanding the microbial ecology of coals and the sustainability of methane production stimulated by nutrients.