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231.
Alan L. Mayo Rachel M. Henderson David Tingey William Webber 《Hydrogeology Journal》2010,18(3):725-747
The 1,750-km2 endorheic Honey Lake basin (California–Nevada, USA) was part of the 22,000-km2 Pleistocene Lake Lahontan pluvial lake system which existed between 5,000 and 40,000 years BP. The basin consists of two subbasins separated by a low elevation divide. Groundwater in the western subbasin has a maximum total dissolved solids (TDS) content of only ~1,300 mg/L; however eastern subbasin groundwater has a maximum TDS of ~46,000 mg/L. This TDS distribution is unexpected because 94% of surface water TDS loading is to the western subbasin. In situ reactions and upwelling thermal groundwater contributing to groundwater chemistry were modeled using NETPATH. The TDS difference between the subbasins is attributed to post-Lake Lahontan isostatic rebound about 13,000 years ago. Prior to rebound the subbasins did not exist and the low point of the basin was in the eastern area where hydraulic isolation from the larger Lake Lahontan and frequent desiccation of the basin surface water resulted in evaporite mineral deposition in accumulating sediments. After rebound, the terminal sink for most surface water shifted to the western subbasin. Although most closed basins have not been impacted by isostatic rebound, results of this investigation demonstrate how tectonic evolution can impact the distribution of soluble minerals accumulating in shallow basins. 相似文献
232.
Sophie Arnaud-Haond Núria Marbà Elena Diaz-Almela Ester A. Serrão Carlos M. Duarte 《Estuaries and Coasts》2010,33(4):878-889
The diversity–stability relationship is the subject of a long-standing debate in ecology, but the genetic component of diversity
has seldom been explored. In this study, we analyzed the interplay between genetic diversity and demographic responses to
environmental pressures. This analysis included 30 meadows formed by the Mediterranean endemic seagrass, Posidonia oceanica, showing a wide range of population dynamics ranging from a near equilibrium state to steep decline due to strong environmental
pressures close to aquaculture installations. Our results show that sedimentation rates are much better predictors of mortality
than clonal or genetic components. An unexpected positive trend was observed between genotypic diversity and mortality, along
with a negative relationship between allelic richness and net population growth. Yet such trends disappeared when excluding
the most extreme cases of disturbance and mortality, suggesting the occurrence of a threshold below which no relationship
exists. These results contrast with the positive relationship between genotypic diversity and resistance or resilience observed
in previous manipulative experiments on seagrass. We discuss the reasons for this discrepancy, including the difficulties
in designing experiments reflecting the complexity of natural meadows. 相似文献