Abstract:1. Anthropogenic stressors such as climate change, ozone depletion and acidification may act in concert to alter ultraviolet (UV) light and temperature regimes in freshwater ecosystems. These physical and chemical changes will inevitably affect zooplankton community dynamics, but little is known about their relative effects on different species in natural communities. During spring, species that migrate to surface waters to take advantage of warmer temperatures may be especially vulnerable as UV levels can be … Show more
“…This finding agreed with the reported suppression of copepods under warmed, fishless conditions (McKee et al 2002). Further, combined exposure to UV and cold temperatures can be advantageous for copepods, such as Leptodiaptomus minutus, that can rely on photoprotective pigmentation (Leech and Williamson 2000;Persaud and Williamson 2005).…”
Climate warming has been shown to increase the frequency of extreme weather effects on small lakes by increasing the variability of terrigenic inputs and surface water temperatures. We hypothesized that the effect of thermal variability on boreal plankton depends on dissolved terrigenic matter (i.e., temperature-terrigenic interaction). A two-factor mesocosm (1500-L capacity) experiment consisting of three terrigenic treatment levels (control, [2] runoff, [+] runoff) and three temperature treatment levels (control, warm, and cold) was conducted in triplicate for a total of 27 mesocosms deployed in Lake 302S of the Experimental Lakes Area in Canada. The warming treatment amplified the positive effect of terrigenic amendment on total phytoplankton biomass by stimulating large (.35-mm Greatest Axial Linear Dimension; GALD) taxa during the 50-d experiment. In comparison, removal of terrigenic matter increased the abundance of smaller (,35-mm GALD) phytoplankton along with copepods and cladocerans under cold and warm conditions, respectively. We also attempted to corroborate our experimental findings by comparing planktonic communities collected from reference Lake 239 during climatically contrasting summers between 1970 and 2001. Although planktonic communities in Lake 239 also differed significantly between years characterized by cold, wet vs. warm, dry ice-free conditions, their responses ran opposite to those detected during the experiment, highlighting the potential overriding importance of other scale-dependent factors (e.g., fish predation, vertical migration) mediating the effects of climate on lake communities.
“…This finding agreed with the reported suppression of copepods under warmed, fishless conditions (McKee et al 2002). Further, combined exposure to UV and cold temperatures can be advantageous for copepods, such as Leptodiaptomus minutus, that can rely on photoprotective pigmentation (Leech and Williamson 2000;Persaud and Williamson 2005).…”
Climate warming has been shown to increase the frequency of extreme weather effects on small lakes by increasing the variability of terrigenic inputs and surface water temperatures. We hypothesized that the effect of thermal variability on boreal plankton depends on dissolved terrigenic matter (i.e., temperature-terrigenic interaction). A two-factor mesocosm (1500-L capacity) experiment consisting of three terrigenic treatment levels (control, [2] runoff, [+] runoff) and three temperature treatment levels (control, warm, and cold) was conducted in triplicate for a total of 27 mesocosms deployed in Lake 302S of the Experimental Lakes Area in Canada. The warming treatment amplified the positive effect of terrigenic amendment on total phytoplankton biomass by stimulating large (.35-mm Greatest Axial Linear Dimension; GALD) taxa during the 50-d experiment. In comparison, removal of terrigenic matter increased the abundance of smaller (,35-mm GALD) phytoplankton along with copepods and cladocerans under cold and warm conditions, respectively. We also attempted to corroborate our experimental findings by comparing planktonic communities collected from reference Lake 239 during climatically contrasting summers between 1970 and 2001. Although planktonic communities in Lake 239 also differed significantly between years characterized by cold, wet vs. warm, dry ice-free conditions, their responses ran opposite to those detected during the experiment, highlighting the potential overriding importance of other scale-dependent factors (e.g., fish predation, vertical migration) mediating the effects of climate on lake communities.
“…Grazing may increase UV transparency through decreasing the density and altering the size structure of phytoplankton or decreasing the release of dissolved organic matter (DOM) by phytoplankton; thus, zooplankton can contribute to the development of a UV clear-water phase (Williamson et al 2007). UVR can also affect survival and fecundity of zooplankton (Leech and Williamson 2000;Grad et al 2003;Persaud and Williamson 2005), as well as alter abundance of food resources or predators (''solar cascade hypothesis ''-Williamson 1995;Williamson et al 1999).…”
Section: Effect Of Ultraviolet Radiationmentioning
Recently, major advances in the climatezooplankton interface have been made some of which appeared to receive much attention in a broader audience of ecologists as well. In contrast to the marine realm, however, we still lack a more holistic summary of recent knowledge in freshwater. We discuss climate change-related variation in physical and biological attributes of lakes and running waters, high-order ecological functions, and subsequent alteration in zooplankton abundance, phenology, distribution, body size, community structure, life history parameters, and behavior by focusing on community level responses. The adequacy of large-scale climatic indices in ecology has received considerable support and provided a framework for the interpretation of community and species level responses in freshwater zooplankton. Modeling perspectives deserve particular consideration, since this promising stream of ecology is of particular applicability in climate change research owing to the inherently predictive nature of this field. In the future, ecologists should expand their research on species beyond daphnids, should address questions as to how different intrinsic and extrinsic drivers interact, should move beyond correlative approaches toward more mechanistic explanations, and last but not least, should facilitate transfer of biological data both across space and time.
“…Zooplankton survival and reproduction can be severely reduced at UVR levels found in the surface waters of highly-transparent lakes; however, effects are species-specific and may depend on other environmental factors such as temperature (Leech & Williamson, 2000;Williamson et al, 2002;Persaud & Williamson, 2005). In a laboratory experiment with monochromatic light, Storz & Paul (1998) found that Daphnia magna were positively phototactic to light from the visible spectrum but negatively phototactic to UVR.…”
The objective of this study was to expand the spatial scale of previous experiments on the effects of ultraviolet radiation (UVR) on diel vertical migration (DVM) by freshwater zooplankton. We conducted an in situ mesocosm experiment in highly UVR transparent Lake Giles, Pennsylvania, in which we imposed two treatments: ambient UVR and UVR-shielded. Mesocosms (3440 L, 0.74 m diameter, 8 m deep) were large enough to include a spatial refuge from UVR and permit relatively large-scale DVM. Daphnia catawba adopted a significantly deeper distribution during the day in the ambient UVR treatment compared to the UVR-shielded treatment, but effects of UVR were absent at night. In contrast, DVM by Leptodiaptomus minutus was unaffected by the UVR treatment. In both treatments, Leptodiaptomus minutus were most abundant at the bottom of the mesocosms during the day and exhibited a more uniform distribution across depths at night. These results suggest that UVR, along with temperature, algal resources, and predators, may affect zooplankton DVM in aquatic ecosystems.
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