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Map of sites (nsite = 40) within York Region of the Greater Toronto Area overlaid on the maximum value composite image of NDVI values for 2016. Symbol sizes are proportional to decomposition rates estimated at the site level.

Map of sites (nsite = 40) within York Region of the Greater Toronto Area overlaid on the maximum value composite image of NDVI values for 2016. Symbol sizes are proportional to decomposition rates estimated at the site level.

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Headwater streams accumulate, process, and export organic materials for use in downstream environments. Decomposition of organic material, an important ecosystem function, may be sensitive to land cover changes in urbanizing regions since headwater stream processes tend to be tightly coupled with riparian and catchment characteristics. Headwaters r...

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... Furthermore, the range of average tensile loss rates in our summer samples (1.12 to 4.27%/day) encapsulated all but the lowest of rates observed in 25 forested streams in northern Michigan, USA, sampled by Tiegs et al. (2013). In contrast, another southern Ontario study observed a median tensile loss in the spring season of nearly twice that observed in our study (2.43%/day and 1.22%/day, respectively), perhaps reflecting the urban nature of many of the streams used in the study (Kielstra et al. 2019). ...
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Background: Agricultural development of former wetlands has resulted in many headwater streams being sourced by subsurface agricultural drainage systems. Subsurface drainage inputs can significantly influence stream environmental conditions, such as temperature, hydrology, and water chemistry, that drive ecological function. However, ecological assessments of subsurface drainage impacts are rare. We assessed the impact of an agricultural drainage system on cellulose decomposition and benthic respiration using a paired stream study in a headwater branch of Nissouri Creek, in Ontario, Canada. Adjacent first order segments sourced by a spring-fed marsh and a cropped field with subsurface drainage, as well as the adjoining trunk segment, were sampled over a year using the cotton strip assay to measure cellulose decomposition and benthic respiration. Results: Assessments of cellulose decomposition revealed a one-third reduction in the drainage-sourced segment compared to marsh-sourced segment. Between segment differences in cellulose decomposition were associated with reduced summer temperatures in the drainage-sourced segment. Impacts of stream cooling from the drainage-sourced segment were transmitted downstream as cellulose decomposition was slower than expected throughout the drainage-sourced segment and for several hundred meters down the adjoining trunk segment. Benthic respiration only differed between the drainage- and marsh-sourced segments in spring, when stream temperatures were similar. Conclusions: Our findings suggest there may be a widespread reduction in cellulose decomposition in streams across similar agricultural regions where subsurface drainage is prevalent. However, cooling of streams receiving significant amounts of water inputs from subsurface drainage systems may impart increased resiliency to future climate warming.
... Promising options for low-cost monitoring programs may lie in remote sensing (Matejicev et al. 2003;Heasley et al. 2020), citizen science (Cartwright et al. 2015;Shupe 2017;Kielstra et al. 2019), inter-departmental collaboration within municipal governments, or collaboration with higher educational institutions. Using technology and stakeholder/citizen programs to gather information can lower costs and improve efficiency of data collection programs. ...
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... This represents a problem for water quality and ecological integrity on a catchment scale because a) if a large number of small streams is impacted within a short time, there is a large area of impaired habitat in the same catchment, and b) many small streams that intersect stands close to each other combine in the same network (Fig. 4) which may cause downstream cumulative effects. The severity of cumulative effects has been considered in urban and agricultural catchments (Jones et al., 2017;Kielstra et al., 2019;Mineau et al., 2015;Seitz et al., 2011), but has not been adequately and empirically addressed in production forests (Kuglerová et al., 2017;Richardson, 2019). This is problematic also because forested headwaters receive few mitigation measures (i.e., buffers, Kuglerová et al., 2020) to prevent impairments and thus the potential for cumulative effects is large. ...
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