RESUMEN
For the Western North America Mercury Synthesis, we compiled mercury records from 165 dated sediment cores from 138 natural lakes across western North America. Lake sediments are accepted as faithful recorders of historical mercury accumulation rates, and regional and sub-regional temporal and spatial trends were analyzed with descriptive and inferential statistics. Mercury accumulation rates in sediments have increased, on average, four times (4×) from 1850 to 2000 and continue to increase by approximately 0.2µg/m(2) per year. Lakes with the greatest increases were influenced by the Flin Flon smelter, followed by lakes directly affected by mining and wastewater discharges. Of lakes not directly affected by point sources, there is a clear separation in mercury accumulation rates between lakes with no/little watershed development and lakes with extensive watershed development for agricultural and/or residential purposes. Lakes in the latter group exhibited a sharp increase in mercury accumulation rates with human settlement, stabilizing after 1950 at five times (5×) 1850 rates. Mercury accumulation rates in lakes with no/little watershed development were controlled primarily by relative watershed size prior to 1850, and since have exhibited modest increases (in absolute terms and compared to that described above) associated with (regional and global) industrialization. A sub-regional analysis highlighted that in the ecoregion Northwestern Forest Mountains, <1% of mercury deposited to watersheds is delivered to lakes. Research is warranted to understand whether mountainous watersheds act as permanent sinks for mercury or if export of "legacy" mercury (deposited in years past) will delay recovery when/if emissions reductions are achieved.
RESUMEN
We compared genetic variation in three introduced North American populations of Passer montanus with an ancestral German population, a native Swedish population, and an introduced Australian population. The North American P. montanus were less variable genetically than the ancestral German birds, presumably a result of the founding event. The genetic structure of all six populations of P. montanus can be explained in terms of interaction among mutation, genetic drift, effective population size, and unknown selective factors. Cluster analyses and an ordination of distance measures derived from electrophoretic data generally showed relationships in phenetic space among populations consistent with the magnitude of their geographic separation. An exception occurred with the Swedish population, which was closer in the ordination to a North American population than to the geographically neighboring German population. This seemingly anomolous juxtaposition was attributed to the relative abundance of alleles present in the Swedish birds. Populations of P. montanus seem to have diverged in a manner similar to that seen in conspecific disjunct populations, i.e., at present showing no trenchant indication of genetic speciation.
