Fluorescence image analysis using the calcium indicator fluo-3 was used to examine changes in [Ca2+]i induced by glutamate in mixed glia populations cultured from neonatal rat brains. [Ca2+]i responses were correlated with glia type by performing immunohistochemistry using markers specific for type 1 and type 2 astrocytes on the same cells used in the imaging experiments. Glutamate (30-500 microM) induced two markedly different [Ca2+]i responses in the two astrocyte types: the response in type 1 astrocytes consisted of an initial fast transient followed by varying degrees of oscillations, whereas the predominant response in type 2 astrocytes was a slow rise in [Ca2+]i to a more or less sustained and nonoscillatory level. In some type 2 astrocytes, an initial spikelike transient similar to that in type 1 astrocytes was observed; the overall size of the spike, however, was smaller than in type 1 astrocytes. Two agonists for the ionotropic glutamate receptor, alpha-amino-3-hydroxy-5-methylisoxazole-4-propionate (AMPA) and kainate, elicited a 6-cyano-7-dinitroquinoxaline-2,3-dione (CNQX)-sensitive, external Ca(2+)-dependent, sustained [Ca2+]i rise in type 2 but not type 1 astrocytes. The initial spike in type 2 astrocytes was less dependent on external Ca2+ and not blocked by CNQX. [Na+]i as measured by the Na(+)-fluorescence dye SBFI, was elevated by kainate in both astrocyte types, though the increase was larger in type 2 astrocytes. This increase was reduced by CNQX, suggesting this [Ca2+]i increase was mediated, at least in part, by ionotropic glutamate receptors. The results are discussed in terms of the relative distribution of two classes of glutamate receptors on these two astrocyte types: one, the ionotropic class, is linked directly to an ion channel, and the other, the metabotropic class, induces internal mobilization of Ca2+ via inositol phospholipid hydrolysis.

Wildfires alter forested ecosystems, which include large stores of mercury (Hg) and organic carbon, two compounds that are closely linked in vegetation, soils, and streamwater. Studies have shown that wildfires release elevated levels of mercury to the atmosphere which can be locally redeposited and leave charred organic material (vegetation and litter) on the soil surface. Both can contribute to the elevated mobilization of Hg into lakes and streams. However, no studies have conducted a detailed examination of hydrological transport of Hg following a wildfire. This study investigates the coupled transport of mercury and carbon at Twomile Run, a headwater stream located in the forested mountains of Shenandoah National Park, in the year following a low-severity wildfire. Weekly baseflow samples and bi-hourly high-flow storm samples were analyzed for dissolved and particulate mercury (Hg and Hg, respectively), dissolved organic carbon (DOC), UV absorbance at 254 nm (UV, surrogate for DOC quantity and character), and total suspended solids (TSS), and were compared with identical measurements taken from a nearby unburned watershed. For all flow conditions sampled at the burned site (which did not include the 2 months following the fire), streamwater Hg and DOC concentrations, and corresponding UV, were similar to the unburned system. TSS concentrations varied between sites but overall differences were relatively small in magnitude and likely attributable to site differences rather than fire effects. Notably, the Hg per unit of TSS at the burned site was an order of magnitude higher than the unburned site (2.66 and 0.13 ng Hg per mg TSS, respectively) for 8 months following the fire, resulting in elevated Hg concentrations for the range of flow conditions, after which there was a rapid return to non-disturbed conditions. Streamwater total Hg fluxes roughly doubled (0.55 to 1.04 μg m yr) as a consequence of the fire, indicating that in addition to changing atmospheric and terrestrial Hg cycling, fires can rapidly and significantly alter the streamwater Hg which has implication for downstream ecosystems. These findings are particularly relevant as the occurrence and severity of wildfires are expected to increase in the mid-latitudes in response to climate change.

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