14:10 〜 14:25
[AHW20-02] Biodiversity and phosphorus cycling in the river ecosystem
キーワード：生物多様性、生物学的リン循環、生態系機能、付着藻類、栄養螺旋モデル、リン酸-酸素安定同位体分析
Introduction
Phosphorous (P) is a key element to determine ecosystem processes because its natural abundance is rare in the bio-available form. Because of its scarcity relative to other macronutrients, anthropogenically loaded P often causes cultural eutrophication and biodiversity loss in aquatic ecosystems. The anthropogenic disturbances in the P cycling also result in deterioration of ecosystem services in quality and quantity through the loss of ecosystem functions provided by biodiversity. In spite of such a pivotal role, P dynamics, including biological recycling, have been poorly understood. Considering such social and ecological backgrounds, we applied two advanced technique, nutrient spiral metrics and phosphate oxygen isotope (δ18Op) analysis, to estimate biological P recycling in the river ecosystem in situ. In addition, we examined how epilithic microbial community properties can determine the P recycling function of river ecosystem.
Materials & Methods
We conducted the synoptic research in the whole catchment of Yasu River in the Lake Biwa Watershed, Japan, in 2016. We set 63 monitoring sites at its tributary streams, which vary in catchment size and land use pattern. For these sites, we measured concentration of soluble reactive P (SRP) and physical characteristics. We also collected GIS data in their catchments. For nutrient spiral metrics, we used a modified method of SPARROW (Smith et al. 1997). We estimated P uptake rate, defined as microbial phosphate uptake per unit area of riverbed and per unit time, incorporating the above environmental and GIS data into the model.
At 30 out of 63 monitoring sites, we also collected epilithons from the riverbeds to characterize algal and bacterial community properties for each stream. For each epilithic sample, algal taxa were identified under microscopic observation and then their abundances were counted. For the epilithic bacteria, operation taxonomic units are identified on the basis of 16S rRNA gene using a MiSeq sequencer.
For the δ18Op analysis, we collected river water samples from the 30 biological sampling sites. These samples were converted into solid Ag3PO4 to determine their δ18Op values using a TC/EA-IRMS. Based on an isotope exchange equilibrium value δ18Op-IEE, we estimated how much dissolved phosphate is biologically recycled in river waters. If the dissolved phosphate is completely turned over, a measured value of δ18Op converges to the δ18Op-IEE.
Results & Discussion
P uptake rate showed great variation among streams within a whole catchment. It was positively associated with green algal abundance and/or taxa richness (Fig. 1a, b), but not with bacterial community properties. As previously reported (Cashman et al. 2013), the green algae are sensitive to nutrient availability, so that they may play an important role in P recycling in the river ecosystem. Our study demonstrated that fluvial microbial diversity has positive effects on ecosystem functioning in nature.
The δ18Op analysis revealed that river water δ18Op had a wide range of isotopic values across the streams. While these isotopic values might be imprinted partly by source signatures derived from external P loading, they tended to converge to the δ18Op-IEE in streams where P uptake rate is higher (Fig. 2), suggesting that both methods can be promising tools to estimate biological P recycling in situ.
Phosphorous (P) is a key element to determine ecosystem processes because its natural abundance is rare in the bio-available form. Because of its scarcity relative to other macronutrients, anthropogenically loaded P often causes cultural eutrophication and biodiversity loss in aquatic ecosystems. The anthropogenic disturbances in the P cycling also result in deterioration of ecosystem services in quality and quantity through the loss of ecosystem functions provided by biodiversity. In spite of such a pivotal role, P dynamics, including biological recycling, have been poorly understood. Considering such social and ecological backgrounds, we applied two advanced technique, nutrient spiral metrics and phosphate oxygen isotope (δ18Op) analysis, to estimate biological P recycling in the river ecosystem in situ. In addition, we examined how epilithic microbial community properties can determine the P recycling function of river ecosystem.
Materials & Methods
We conducted the synoptic research in the whole catchment of Yasu River in the Lake Biwa Watershed, Japan, in 2016. We set 63 monitoring sites at its tributary streams, which vary in catchment size and land use pattern. For these sites, we measured concentration of soluble reactive P (SRP) and physical characteristics. We also collected GIS data in their catchments. For nutrient spiral metrics, we used a modified method of SPARROW (Smith et al. 1997). We estimated P uptake rate, defined as microbial phosphate uptake per unit area of riverbed and per unit time, incorporating the above environmental and GIS data into the model.
At 30 out of 63 monitoring sites, we also collected epilithons from the riverbeds to characterize algal and bacterial community properties for each stream. For each epilithic sample, algal taxa were identified under microscopic observation and then their abundances were counted. For the epilithic bacteria, operation taxonomic units are identified on the basis of 16S rRNA gene using a MiSeq sequencer.
For the δ18Op analysis, we collected river water samples from the 30 biological sampling sites. These samples were converted into solid Ag3PO4 to determine their δ18Op values using a TC/EA-IRMS. Based on an isotope exchange equilibrium value δ18Op-IEE, we estimated how much dissolved phosphate is biologically recycled in river waters. If the dissolved phosphate is completely turned over, a measured value of δ18Op converges to the δ18Op-IEE.
Results & Discussion
P uptake rate showed great variation among streams within a whole catchment. It was positively associated with green algal abundance and/or taxa richness (Fig. 1a, b), but not with bacterial community properties. As previously reported (Cashman et al. 2013), the green algae are sensitive to nutrient availability, so that they may play an important role in P recycling in the river ecosystem. Our study demonstrated that fluvial microbial diversity has positive effects on ecosystem functioning in nature.
The δ18Op analysis revealed that river water δ18Op had a wide range of isotopic values across the streams. While these isotopic values might be imprinted partly by source signatures derived from external P loading, they tended to converge to the δ18Op-IEE in streams where P uptake rate is higher (Fig. 2), suggesting that both methods can be promising tools to estimate biological P recycling in situ.