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Journal Articles

Root endophytic bacterial and fungal communities in a natural hot desert are differentially regulated in dry and wet seasons by stochastic processes and functional traits

Taniguchi, Takeshi*; Isobe, Kazuo*; Imada, Shogo*; Eltayeb, M. M.*; Akaji, Yasuaki*; Nakayama, Masataka; Allen, M. F.*; Aronson, E. L.*

Science of the Total Environment, 899, p.165524_1 - 165524_13, 2023/11

 Times Cited Count:3 Percentile:77.07(Environmental Sciences)

Dryland ecosystems experience seasonal cycles of severe drought and moderate precipitation. Desert plants typically have patchy distributions, and many may develop symbiotic relationships with root endophytic microbes to survive under the repeated wet and extremely dry conditions. Although community coalescence has been found in many systems, the colonization by functional microbes and its relationship to seasonal transitions in arid regions are not well understood. Here we examined root endophytic microbial taxa, and their traits in relation to their root colonization, during the dry and wet seasons in a hot desert of the southwestern United States. We used high-throughput DNA sequencing of 16S rRNA and ITS gene profiling of five desert shrubs, and analyzed the seasonal change in endophytic microbial lineages. In summer, Actinobacteria increased, although this was not genus-specific. For fungi, Glomeraceae selectively increased in summer. In winter, Gram-negative bacterial genera, including those capable of nitrogen fixation and plant growth promotion, increased. Neutral model analysis revealed a strong stochastic influence on endophytic bacteria but a weak effect for fungi, especially in summer. The taxa with higher frequency than that predicted by the neutral model shared environmental adaptability and symbiotic traits, whereas the frequency of pathogenic fungi was at or under the predicted value. These results suggest that community assembly of bacteria and fungi is regulated differently. The bacterial community was affected by stochastic and deterministic processes via the bacterial response to drought (response trait) and beneficial effect on plants (effect trait). For fungi, mycorrhizal fungi were selected by plants in summer. The regulation of beneficial microbes by plants in both dry and wet seasons suggests the presence of plant-soil positive feedback in this natural desert ecosystem.

Journal Articles

Atmospheric ammonia deposition and its role in a cool-temperate fragmented deciduous broad-leaved forest

Katata, Genki*; Yamaguchi, Takashi*; Watanabe, Makoto*; Fukushima, Keitaro*; Nakayama, Masataka*; Nagano, Hirohiko*; Koarashi, Jun; Tateno, Ryunosuke*; Kubota, Tomohiro

Atmospheric Environment, 298, p.119640_1 - 119640_12, 2023/04

 Times Cited Count:1 Percentile:47.41(Environmental Sciences)

Journal Articles

Shift in the rhizosphere microbial communities between growing- and low-temperature dormant seasons in a northern hardwood forest

Nakayama, Masataka; Tateno, Ryunosuke*

Plant and Soil, 17 Pages, 2023/00

 Times Cited Count:0 Percentile:0.02(Agronomy)

${it Background and Aims}$ Microbial communities within the soil surrounding plant roots (rhizosphere) are distinct from those in the non-rhizosphere soil because of root exudation and symbiosis with plant roots and play important roles in plant growth. However, seasonal variations in these rhizosphere microbial communities are not well known, especially during the plant's dormant season in cool temperate forests. ${it Methods}$ We investigated the rhizosphere microbial communities in a cool-temperate deciduous broad-leaved forest at the growing season (mid-summer) and at the beginning and end of the plant's dormant season (early winter and early spring) using metabarcoding of prokaryotic 16S rRNA genes and fungal ITS region, microbial functional prediction, and co-occurrence network analysis. ${it Results}$ The rhizosphere dominant prokaryotic subgroup (occupying 19.4 $$pm$$ 3.2% of relative read counts) had non-significant seasonal fluctuations, and their relative read counts were correlated with physicochemical properties, including pH and water content. In contrast, the relative read count of ectomycorrhizal fungi was 1.4 times higher in the rhizosphere than that in the bulk soil in mid-summer. However, the relative read counts of ectomycorrhizal fungi within rhizospheres in winter and spring (28.5 $$pm$$ 18.9% and 20.8 $$pm$$ 13.8%, respectively) were similar to that in bulk soil (25.8 $$pm$$ 18.7% and 22.4 $$pm$$ 17.1%, respectively). ${it Conclusion}$ Ectomycorrhizal fungi reduced their occupancy within the rhizosphere during the plant's dormant seasons, whereas rhizosphere-dominant prokaryotic communities were stable during the seasonal change, implying the importance of prokaryotic rather than ectomycorrhizal fungal communities in the processes occurring within the rhizosphere during dormant seasons.

Journal Articles

Soil microbial community responding to moderately elevated nitrogen deposition in a Japanese cool temperate forest surrounded by fertilized grasslands

Nagano, Hirohiko; Nakayama, Masataka*; Katata, Genki*; Fukushima, Keitaro*; Yamaguchi, Takashi*; Watanabe, Makoto*; Kondo, Toshiaki*; Atarashi-Andoh, Mariko; Kubota, Tomohiro*; Tateno, Ryunosuke*; et al.

Soil Science and Plant Nutrition, 67(5), p.606 - 616, 2021/10

 Times Cited Count:2 Percentile:18.14(Plant Sciences)

We analyzed the relationships between nitrogen deposition (deposition of nitrate and ammonium ions) and soil microbial properties in a cool temperate forest surrounded by normally fertilized pasture grasslands in northern Japan. The aim of the present study was to gain the primary information on soil microbial response to moderately elevated nitrogen deposition ($$<$$ 10 kg N ha$$^{-1}$$ y$$^{-1}$$). We established three experimental plots in the forest edge adjacent to grasslands and other three plots in the forest interior at least 700 m away from the grasslands. During May to November 2018, nitrogen deposition in each plot was measured. In August 2018, litter and soil (0-5 cm depth) samples were collected from all plots to measure net nitrogen mineralization and nitrification rates as indicators of microbial activity, and microbial biomass carbon and nitrogen and various gene abundances (i.e. bacterial 16S rRNA, fungal ITS, bacterial amoA, and archaeal amoA genes) as indicators of microbial abundance and structure. Nitrogen deposition in the forest edge was 1.4-fold greater than that in the forest interior, even while the maximum deposition was 3.7 kg N ha$$^{-1}$$. Nitrogen deposition was significantly correlated to the net nitrogen mineralization and nitrification rates and the 16S rRNA and bacterial amoA gene abundances. Microbial community structures were different between litter and soil samples but were similar between the forest edge and interior. Significant correlations of nitrogen deposition to the soil carbon to nitrogen ratio, and the nitrate and ammonium contents were also observed. Thus, our results show that moderately elevated nitrogen deposition in nitrogen-limited forest edges can stimulate microbial activities and abundances in soils.

Journal Articles

Rapid measurement of the chloride diffusion coefficient in concrete from combination of non-steady-state migration experiment and EPMA

Ogino, Masataka*; Owaki, Eiji*; Shirase, Mitsuyasu*; Nakayama, Masashi

Konkurito Kogaku Nenji Rombunshu (DVD-ROM), 39(1), p.703 - 708, 2017/07

no abstracts in English

JAEA Reports

Design study of the low level Radioactive waste retrieval facility (II)

Asahina, Kiyoshi*; Soya, Masataka*; Ogawa, Hikaru*; Akasaka, Takayuki*; Iwata, Toshio*; Fukutome, Yutaka*; Nakayama, Jumpei*

PNC TJ4058 89-005, 178 Pages, 1989/06

PNC-TJ4058-89-005.pdf:27.12MB

None

Oral presentation

Carbon and nitrogen cycling in forest; Is interdisciplinary collaboration needed?

Katata, Genki*; Fukushima, Keitaro*; Koarashi, Jun; Yamaguchi, Takashi*; Watanabe, Makoto*; Nagano, Hirohiko; Nakayama, Masataka*; Tateno, Ryunosuke*; Kinose, Yoshiyuki*

no journal, , 

no abstracts in English

Oral presentation

Microbial life on plastics and its implication on elemental cycling in the aquatic environment

Battulga, B.; Nakayama, Masataka; Atarashi-Andoh, Mariko; Koarashi, Jun

no journal, , 

A growing attention has been addressed on microbial attachment and biofilm formation on plastic debris especially on microplastics (MPs; sizes: $$<$$5 mm) in the aquatic environment. The current study is focused on bacterial and fungal community composition, diversity, and structure in MP-associated biofilms to emphasize potential alteration of elemental cycling by the presence of MPs in the coastal aquatic environment. We collected MP, surface water, bottom sediment, and coastal sand samples from two contrasting coastal areas of Japan on a seasonal basis. Surface morphology and attached microorganisms on MPs were visually inspected by scanning electron microscopy (SEM). A high-throughput sequencing using Illumina MiSeq was performed in the collected samples to investigate the microbial community composition and diversity among different samples.

Oral presentation

Moderately elevated nitrogen deposition altering soil carbon dynamics

Nagano, Hirohiko*; Nakayama, Masataka; Katata, Genki*; Fukushima, Keitaro*; Yamaguchi, Takashi*; Watanabe, Makoto*; Atarashi-Andoh, Mariko; Tateno, Ryunosuke*; Hiradate, Shuntaro*; Koarashi, Jun

no journal, , 

Oral presentation

Effects of different parent materials of forest soils on heterotrophic respiration in the subsoil

Abe, Yukiko; Nakayama, Masataka; Tange, Takeshi*; Atarashi-Andoh, Mariko; Koarashi, Jun

no journal, , 

Soil is the largest carbon pool in terrestrial ecosystems, and forest soils in particular play an important role as a C reservoir in the global C cycle. Organic matter in the soil is released to the atmosphere as carbon dioxide through microbial decomposition (heterotrophic respiration). Decomposition of organic matter accumulated in the subsoil may contribute significantly to heterotrophic respiration, but it is not clear. Therefore, the objective of this study was to determine the heterotrophic respiration rate from the surface to the lower layers of forest soils with different parent materials. This presentation will report on the relationship between soil physicochemical and organic matter properties and heterotrophic respiration.

Oral presentation

Characterizations of formed biofilms and microbial communities on microplastics in coastal rivers of Japan

Battulga, B.; Nakayama, Masataka; Atarashi-Andoh, Mariko; Koarashi, Jun

no journal, , 

Plastic debris in the aquatic environment has become a growing concern due to their long-term ecological consequences. The current study is focused on microbial community composition on microplastics (MPs; sizes $$<$$5 mm) and characteristics of MP-associated biofilms in coastal river environments of Japan in order to understand the impact of MP-associated biofilms on aquatic organic matter cycling. The aims of the current study are i) extraction and characterization of microbial biofilms on MPs and ii) identification of diversity and composition of microbial communities on MP surfaces and in surrounding surface waters and sediments. The samples were collected from two coastal rivers during 2021-2022 on a seasonal basis. In this study, we proposed a new method to extract biofilms from MPs using ultrasound-assisted syringe treatment for isotopic analysis. Morphotypes of MPs and associated specific microbial taxa as well as seasonal differences were also observed.

Oral presentation

Effect of artificial root exudates on the forest soil microbial community and nitrogen dynamics

Nakayama, Masataka; Tateno, Ryunosuke*

no journal, , 

Root exudates, carbon compounds secreted from plant fine roots, enhance nutrient cycles within root surrounding soil (rhizosphere) by stimulating microbial activities and growth. However, there is a lack of knowledge about the effect of the differences in the chemical composition of root exudates and the diversity of root exudates on the nitrogen cycle within the rhizosphere. Here, we investigated the impact of the differences in root exudates on the nitrogen cycles and microbial community using artificial root exudates (ARE). We added ARE from the simulated fine root and changed their diversity from 1 to 3 per incubation system. Soil microbial gene abundances varied among ARE types and diversity, but the differences were not statistically significant. In addition, there was a non-significant effect of ARE on nitrogen cycling processes. These results indicated that the diversity and compositions of root exudates did not affect the microbial community and nitrogen cycle for at least a short time.

Oral presentation

Nitrogen mineralization in surface and subsurface layers at forest ecosystems having different soil types

Nakayama, Masataka; Abe, Yukiko; Atarashi-Andoh, Mariko; Koarashi, Jun

no journal, , 

Plants take up nitrogen mainly from surface soil, while under the nutrient competition, they utilize nitrogen from subsurface soil layers. However, nitrogen dynamics in the subsoil layer is unclear. Here, we investigated the soil profiles (0-60 cm depth) of net nitrogen mineralization and nitrification rates at four Japanese broad-leave forest having two different soil types (volcanic ash and non-volcanic ash soil). The results showed that net nitrogen mineralization decreased with increase of soil depth in the sites of volcanic ash soil, but the trend was not observed in the sites of non-volcanic ash soil. When the rates represented per unit soil volume, the vertical differences in nitrogen mineralization were non-significant for these two soil types. Similar to the factors regulating the spatial variations of nitrogen dynamics, the vertical trends were regulated by the soil total carbon and nitrogen contents and microbial biomass. These results suggested that the quantities of soil organic material and microbes regulated both of the horizontal and vertical differences in the nitrogen dynamics, and that the subsurface soil, as well as surface soil, was quantitatively important nitrogen source for plants.

Oral presentation

Soil microbial fluctuation and CO$$_{2}$$ release increase under dry-wet cycles

Suzuki, Yuri*; Nagano, Hirohiko*; Hiradate, Shuntaro*; Atarashi-Andoh, Mariko; Abe, Yukiko; Koarashi, Jun; Nakayama, Masataka

no journal, , 

Oral presentation

Importance of canopy absorption of atmospheric ammonia in a fragmented deciduous broad-leaved forest in Hokkaido

Katata, Genki*; Yamaguchi, Takashi*; Watanabe, Makoto*; Fukushima, Keitaro*; Nakayama, Masataka; Nagano, Hirohiko*; Koarashi, Jun; Tateno, Ryunosuke*; Kubota, Tomohiro

no journal, , 

no abstracts in English

Oral presentation

Effects of increased moisture fluctuation on soil microorganisms; An Investigation using ten soils in Japan

Suzuki, Yuri*; Nagano, Hirohiko*; Hiradate, Shuntaro*; Atarashi-Andoh, Mariko; Abe, Yukiko; Nakayama, Masataka; Koarashi, Jun

no journal, , 

no abstracts in English

Oral presentation

Priming effects in forest soils with different parent materials

Abe, Yukiko; Nakayama, Masataka; Atarashi-Andoh, Mariko; Koarashi, Jun

no journal, , 

Subsoils contain more than half of the global soil carbon. Decomposition of organic matter accumulated in the subsoil is thought to contribute significantly to heterotrophic respiration, and the supply of new organic matter to the subsoil may accelerate the decomposition of soil organic matter (priming effect). However, the carbon dynamics in the subsoil are unknown. The aim of this study was to evaluate the decomposition response to a new supply of organic matter, focusing on the differences in the interaction between organic matter and minerals in the presence and absence of volcanic ash. The surface and subsoil layers of four study sites with volcanic and non-volcanic ash soils were prepared to 64% of water holding capacity (WHC) and incubated at 20$$^{circ}$$C and 30$$^{circ}$$C after addition of 1% of WHC or a sucrose solution labeled at $$^{13}$$C. Sucrose addition had a positive priming effect in the lower layers of the volcanic ash soils, but the difference in carbon release after 90 days of incubation was about half of the addition in all soils, with and without sucrose addition. Therefore, sucrose addition to the soil enhanced organic matter decomposition, but it was suggested that some of the sucrose may remain in the soil.

Oral presentation

Spatial and temporal variations in soil respiration rate and their controlling factors in a ${it Pinus thunbergii}$ plantation on a coastal dune

Abe, Yukiko; Teramoto, Munemasa*; Nakayama, Masataka; Atarashi-Andoh, Mariko; Liang, N.*; Koarashi, Jun

no journal, , 

Carbon dioxide released from the soil, known as soil respiration, is a major component of the carbon cycle in terrestrial ecosystems, but it is highly spatiotemporally variable. Therefore, observations of soil respiration have been conducted around the world to accurately estimate the total amount of soil respiration, but observations in coastal dune environments are very limited. To quantify the response of soil respiration to climate change, it is necessary to understand soil respiration in different regions and ecosystems and to clarify its controlling factors. The objective of this study was to determine the spatiotemporal variability of soil respiration rates and its controlling factors in coastal dune environments. The study site was a ${it Pinus thunbergii}$ plantation on a coastal dune in the Arid Land Research Center of Tottori University. In June 2023, we established 20 points for soil respiration measurement within the study site and started measuring soil respiration rates. In addition, soil samples were collected every 3 months to measure soil composition. Large spatial variability was observed in soil respiration rates from June to December 2023, with coefficients of variation ranging from 43 to 67%. Seasonal changes in soil respiration rates from June to December 2023 were exponential with increasing soil temperatures, but a temporary decrease was observed in August. Soil respiration rates were positively correlated with WEOC. This suggests that WEOC may contribute to the spatial variability in soil respiration rate in sandy soils with a low organic matter content.

Oral presentation

A Measurement method for diffusivity coefficient of concrete by application of EPMA to an electrophoretic test of non-static state

Ogino, Masataka*; Owaki, Eiji*; Shirase, Mitsuyasu*; Nakayama, Masashi

no journal, , 

no abstracts in English

Oral presentation

Relationship between nitrogen deposition and soil microbial property in a deciduous broad-leaved forest

Nagano, Hirohiko; Atarashi-Andoh, Mariko; Fukushima, Keitaro*; Nakayama, Masataka*; Katata, Genki*; Yamaguchi, Takashi*; Watanabe, Makoto*; Kondo, Toshiaki*; Tateno, Ryunosuke*; Koarashi, Jun

no journal, , 

no abstracts in English

23 (Records 1-20 displayed on this page)