Episodic release of methane bubbles from peatland during spring thaw.

Methane (CH(4)) flux into the atmosphere during spring thaw was investigated in a small ombrotrophic peatland (141 degrees 48'E, 43 degrees 19'N, Japan) using the conventional chamber method. More than 50 chamber deployments on top of the snow cover were carried out and continued for more than 165h until the surface snow and underlying ice cover on top of the peat layer had thawed completely. Methane emissions were almost absent in the presence of snow cover. At the very moment the surface ice cover thawed, a large CH(4) flush (>10mgCH(4)m(-2)h(-1)) was recorded, which was on the same order of magnitude as episodic ebullition previously observed in the high-summer. Gas bubbles trapped in the ice layer on top of the waterlogged peat were preliminarily analyzed for the volumetric percentage in the total ice volume and their gas species compositions. Results showed that the bubbles occupied about 3.2% volume and that the mixing ratio of CH(4) in the bubbles was about 20%. The abundance of the bubble-form CH(4) was sufficient to explain the observed episodic CH(4) release during the thaw. Results of this study show that CH(4) emissions during the thaw season have great temporal variability; emission occurs as an episodic release of bubble-form CH(4) stored in the frozen layer. The results also imply the possibility that gas-phase CH(4) plays an important role, not only during the growing season but also in cold-season CH(4) dynamics in northern peatlands.

High levels of manganese-containing superoxide dismutase and thermally induced DNA disruption in a dnaK7(Ts) mutant of Escherichia coli K12.

In dnaK7(Ts) mutant cells, scission of DNA strands occurred after temperature shift up. When cells at 30 degrees C were labeled with [3H]-thymidine and then shifted to 46 degrees or 49 degrees C for 20 min, the profiles of sedimentation of their cellular DNA in an alkaline sucrose gradient revealed a decrease in the size of DNA to a quarter of that at 30 degrees C in the mutant, but not in wild-type cells. The level of manganese-containing superoxide dismutase (MnSOD) in the mutant was about twice that in wild-type cells, even at the permissive temperature, implying increased production of superoxide radical anion, which may cleave DNA strands directly or indirectly in the mutant. Moderate increase in the MnSOD level on temperature shift up was observed in both strains. These results indicated that some components of the DnaK protein participate in protection of cellular membrane functions from thermal damage resulting from elevated production of the superoxide anion radical.