Abstract:Among freshwater systems, coldwater habitats are among the most threatened by climate change. Examining the impacts of increasing water temperature requires the use of both traditional biomonitoring efforts and measures of ecosystem function and structure. We examined fish and macroinvertebrate communities, leaf decomposition rates, periphyton production, and ecosystem metabolism to compare two branches of a trout stream in Minnesota with differing thermal regimes. The cooler South Branch had more coldwater fi… Show more
“…The other is for measuring the concentrations of particulate organic carbon (POC) and particulate organic nitrogen (PON) and δ 13 C in POC, in which 200 mL ~ 1,200 mL of water passed through each filter, in order to acquire adequate POC for δ 13 C analysis. The glass filters for measuring the concentration of chlorophyll-a were kept submerged in 90% acetone each in 6 ml plastic tube to be quantified using a calibrated fluorometer (Trilogy; Turner Design, San Jose, USA), according to EPA Method 445.0 [21]. The glass filters for measuring the concentrations of POC and PON and δ 13 C in POC were dried in oven at 50°C and kept in a desiccator with 12 N hydrochloric acid for 24 hour in order to eliminate particulate inorganic carbon using hydrochloric acid vapor.…”
This study uses stable isotope ratios to investigate the influences of terrestrial inputs of organic matter on the water properties and bottom sediments of coastal seas. The carbon stable isotope ratio (δ 13 C) of particulate organic carbon (POC) and the C/N ratio of particulate organic matter (POM) were obtained following a flood event in 2004, and under normal weather conditions in 2005, from the Seto Inland Sea, Japan. The δ 13 C of the bottom sediments was also measured in 2005. Under normal weather conditions, POM was derived mainly from phytoplankton, which sank to the seabed and became incorporated into the bottom sediments. During the flood event, terrestrial POC spread over 60 km from the source, and the extent of the influence was much larger than that seen in other coastal seas in Japan. The salinity distributions, as well as the concentration and stable isotope ratio of POM, indicated that residual currents such as estuarine circulation may play an important role in spreading terrestrial POC. The longitudinal gradient of δ 13 C-POC in the sediments indicated that the terrestrial POC also impacted on the composition of the seabed deposits.
“…The other is for measuring the concentrations of particulate organic carbon (POC) and particulate organic nitrogen (PON) and δ 13 C in POC, in which 200 mL ~ 1,200 mL of water passed through each filter, in order to acquire adequate POC for δ 13 C analysis. The glass filters for measuring the concentration of chlorophyll-a were kept submerged in 90% acetone each in 6 ml plastic tube to be quantified using a calibrated fluorometer (Trilogy; Turner Design, San Jose, USA), according to EPA Method 445.0 [21]. The glass filters for measuring the concentrations of POC and PON and δ 13 C in POC were dried in oven at 50°C and kept in a desiccator with 12 N hydrochloric acid for 24 hour in order to eliminate particulate inorganic carbon using hydrochloric acid vapor.…”
This study uses stable isotope ratios to investigate the influences of terrestrial inputs of organic matter on the water properties and bottom sediments of coastal seas. The carbon stable isotope ratio (δ 13 C) of particulate organic carbon (POC) and the C/N ratio of particulate organic matter (POM) were obtained following a flood event in 2004, and under normal weather conditions in 2005, from the Seto Inland Sea, Japan. The δ 13 C of the bottom sediments was also measured in 2005. Under normal weather conditions, POM was derived mainly from phytoplankton, which sank to the seabed and became incorporated into the bottom sediments. During the flood event, terrestrial POC spread over 60 km from the source, and the extent of the influence was much larger than that seen in other coastal seas in Japan. The salinity distributions, as well as the concentration and stable isotope ratio of POM, indicated that residual currents such as estuarine circulation may play an important role in spreading terrestrial POC. The longitudinal gradient of δ 13 C-POC in the sediments indicated that the terrestrial POC also impacted on the composition of the seabed deposits.
Climate change is likely to have large impacts on freshwater biodiversity and ecosystem function, especially in cold-water streams. Ecosystem metabolism is affected by water temperature and discharge, both of which are expected to be affected by climate change and, thus, require long-term monitoring to assess alterations in stream function. This study examined ecosystem metabolism in two branches of a trout stream in Minnesota, USA over 3 years. One branch was warmer, allowing the examination of elevated temperature on metabolism. Dissolved oxygen levels were assessed every 10 min from spring through fall in 2017–2019. Gross primary production (GPP) was higher in the colder branch in all years. GPP in both branches was highest before leaf-out in the spring. Ecosystem respiration (ER) was greater in the warmer stream in two of three years. Both streams were heterotrophic in all years (net ecosystem production—NEP < 0). There were significant effects of temperature and light on GPP, ER, and NEP. Stream discharge had a significant impact on all GPP, ER, and NEP in the colder stream, but only on ER and NEP in the warmer stream. This study indicated that the impacts of temperature, light, and discharge differ among years, and, at least at the local scale, may not follow expected patterns.
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