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Abstract
The development of organisms is changing drastically because of anthropogenic changes
in once-limited nutrients. Although the importance of changing macronutrients, such
as nitrogen and phosphorus, is well-established, it is less clear how anthropogenic
changes in micronutrients will affect organismal development, potentially changing
dynamics of selection. We use butterflies as a study system to test whether changes
in sodium availability due to road salt runoff have significant effects on the development
of sodium-limited traits, such as neural and muscle tissue. We first document how
road salt runoff can elevate sodium concentrations in the tissue of some plant groups
by 1.5-30 times. Using monarch butterflies reared on roadside- and prairie-collected
milkweed, we then show that road salt runoff can result in increased muscle mass (in
males) and neural investment (in females). Finally, we use an artificial diet manipulation
in cabbage white butterflies to show that variation in sodium chloride per se positively
affects male flight muscle and female brain size. Variation in sodium not only has
different effects depending on sex, but also can have opposing effects on the same
tissue: across both species, males increase investment in flight muscle with increasing
sodium, whereas females show the opposite pattern. Taken together, our results show
that anthropogenic changes in sodium availability can affect the development of traits
in roadside-feeding herbivores. This research suggests that changing micronutrient
availability could alter selection on foraging behavior for some roadside-developing
invertebrates.
Salinization is the accumulation of water-soluble salts in the soil solum or regolith to a level that impacts on agricultural production, environmental health, and economic welfare. Salt-affected soils occur in more than 100 countries of the world with a variety of extents, nature, and properties. No climatic zone in the world is free from salinization, although the general perception is focused on arid and semi-arid regions. Salinization is a complex process involving the movement of salts and water in soils during seasonal cycles and interactions with groundwater. While rainfall, aeolian deposits, mineral weathering, and stored salts are the sources of salts, surface and groundwaters can redistribute the accumulated salts and may also provide additional sources. Sodium salts dominate in many saline soils of the world, but salts of other cations such as calcium, magnesium, and iron are also found in specific locations. Different types of salinization with a prevalence of sodium salts affect about 30% of the land area in Australia. While more attention is given to groundwater-associated salinity and irrigation salinity, which affects about 16% of the agricultural area, recent investigations suggest that 67% of the agricultural area has a potential for "transient salinity", a type of non-groundwater-associated salinity. Agricultural soils in Australia, being predominantly sodic, accumulate salts under seasonal fluctuations and have multiple subsoil constraints such as alkalinity, acidity, sodicity, and toxic ions. This paper examines soil processes that dictate the exact edaphic environment upon which root functions depend and can help in research on plant improvement.
Chloride concentrations are increasing at a rate that threatens the availability of fresh water in the northeastern United States. Increases in roadways and deicer use are now salinizing fresh waters, degrading habitat for aquatic organisms, and impacting large supplies of drinking water for humans throughout the region. We observed chloride concentrations of up to 25% of the concentration of seawater in streams of Maryland, New York, and New Hampshire during winters, and chloride concentrations remaining up to 100 times greater than unimpacted forest streams during summers. Mean annual chloride concentration increased as a function of impervious surface and exceeded tolerance for freshwater life in suburban and urban watersheds. Our analysis shows that if salinity were to continue to increase at its present rate due to changes in impervious surface coverage and current management practices, many surface waters in the northeastern United States would not be potable for human consumption and would become toxic to freshwater life within the next century.
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