Paleolimnological evidence for recent acidification of Big Moose Lake,Adirondack Mountains,N.Y. (USA)

Big Moose L. has become significantly more acidic since the 1950s, based on paleolimnological analyses of sediment cores. Reconstruction of past lakewater pH using diatom assemblage data indicates that from prior to 1800 to ca. 1950, lakewater pH was about 5.8. After the mid-1950s, the inferred pH decreased steadily and relatively quickly to about 4.6. Alkalinity reconstructions indicate a decrease of about 30 eq · l^-1 during the same period. There was a major shift in diatom assemblage composition, including a nearly total loss of euplanktonic taxa. Chrysophyte scale assemblages and chironomid (midge larvae remains also changed in a pattern indicating decreasing lakewater pH starting in the 1950s. Accumulation rates of total Ca, exchangeable and oxide Al, and other metals suggest recent lake-watershed acidification. Cores were dated using²¹⁰Pb, pollen, and charcoal. Indicators of watershed change (deposition rates of Ti, Si, Al) do not suggest any major erosional events resulting from fires or logging. Accumulation rates of materials associated with combustion of fossil fuels (polycyclic aromatic hydrocarbons, coal and oil soot particles, some trace metals, and sulfur) are low until the late 1800s-early 1900s and increase relatively rapidly until the 1920s–1930s. Peak rates occurred between the late 1940s and about 1970, when rates declined.The recent decrease in pH of Big Moose L. cannot be accounted for by natural acidification or processes associated with watershed disturbance. The magnitude, rate and timing of the recent pH and alkalinity decreases, and their relationship to indicators of coal and oil combustion, indicate that the most reasonable explanation for the recent acidification is increased atmospheric deposition of strong acids derived from combustion of fossil fuels.     

Membrane lipid changes in erythrocytes, liver and kidney in acute and chronic experimental liver disease in rats

Lipid molecules in lipoprotein surfaces exchange with their counterparts in cell plasma membranes. In human or experimental liver disease, plasma lipoprotein surfaces are enriched in cholesterol and deficient in arachidonate; corresponding alterations occur in membrane lipids of erythrocytes. To determine whether similar changes take place in membranes of nucleated cells, the lipid content of plasma and of erythrocyte, liver and kidney membranes was measured in rats with acute (3-day) galactosamine-induced hepatitis or chronic (3-week) biliary obstruction. In both models of liver injury the cholesterol:phospholipid ratio in plasma and in erythrocytes was significantly increased (P less than 0.001). Although this ratio was also elevated in liver and kidney microsomes, only in liver microsomes of obstructed rats was the increase significant (P less than 0.001). However, the cholesterol:phospholipid ratio of kidney brush-border membranes, was significantly higher in bile-duct-ligated rats; presumably, compensating mechanisms limit cholesterol accumulation in intracellular membranes. Kidney brush-border membranes from obstructed rats were deficient in arachidonate as were plasma and erythrocytes. However, arachidonate levels were unchanged in kidney microsomes; renal delta 6-desaturase, the rate-limiting enzyme in the conversion of linoleic acid to arachidonic acid, was increased by 50% (P less than 0.001) and may have counteracted a reduced supply of exogenous lipoprotein arachidonate. We conclude that in experimental liver disease lipoprotein-induced lipid abnormalities can occur in renal membranes, although compensatory mechanisms may operate; the alterations seen, cholesterol accumulation and arachidonate depletion, would be expected to interfere with sodium transport and prostaglandin production, respectively. Our findings support the hypothesis that lipid abnormalities in kidney membranes contribute to the renal dysfunction which is a frequent complication of human liver disease.     

The length but not the sequence of the polyoma virus late leader exon is important for both late RNA splicing and stability.

Polyoma virus late RNA processing provides a convenient model system in which to study the mechanics of splicing in vivo. In order to understand further the role of the untranslated "late leader" unit in late RNA processing we have constructed a group of polyoma viruses with deletions and substitutions in the leader exon. This has allowed us to determine that there is a minimum exon size required for both pre-mRNA splicing and stability in this system. We show here that the non-viability of a mutant (ALM) with a 9 base late leader unit is due to a general defect in late RNA splicing. In addition, ALM-infected cells show at least 40-fold depression in the accumulation of late nuclear RNA (spliced or unspliced). The ALM late promoter, however, functions nearly normally. Substituted leader variants with 51- to 96-base long exons of unrelated sequence are viable (G. Adami and G. Carmichael, J. Virol. 58, 417-425, 1986). We show here that late RNA from one of these substituted leader mutants (containing a 51-base leader exon) is spliced at wild type levels, with virtually no defect in accumulation. Thus, in the polyoma system, splice sites separated by only 9 bases can inhibit each others usage, presumably by steric interference. We suggest that this type of inhibition leads to extreme RNA instability.     

Immunological Detection and Quantitation of Tryptophan Decarboxylase in Developing Catharanthus roseus Seedlings

l-Tryptophan decarboxylase (TDC) (EC 4.2.1.27) enzyme activity was induced in cell suspension cultures of Catharanthus roseus after treatment with a Pythium aphanidermatum elicitor preparation. The enzyme was extracted from lyophilized cells containing high levels of TDC and the protein was purified to homogeneity. The pure protein was used to produce highly specific polyclonal antibodies, and an enzyme-linked immunosorbent assay (ELISA) was developed to quantitate the level of TDC antigen during seedling development and in leaves of the mature plant. Western immunoblotting of proteins after SDS-PAGE with anti-TDC antibodies detected several immunoreactive proteins (40, 44, 54.8, 55, and 67 kilodaltons) which appeared at different stages during seedling development and in leaves of the mature plant. The major 54.8 and 55 kilodalton antigenic proteins in immunoblots appeared transiently between days 1 to 5 and 5 to 8 of seedling development, respectively. The 54.8 kilodalton protein was devoid of TDC enzyme activity, whereas the appearance of the 55 kilodalton protein coincided with the appearance of this decarboxylase activity. The minor immunoreactive proteins (40, 44, and 67 kilodaltons) appeared after day 5 of seedling development and in older leaves of the mature plant, and their relationship, if any, to TDC is presently unknown. Results suggest that the synthesis and degradation of TDC protein is highly regulated in Catharanthus roseus and that this regulation follows a preset developmental program.