Diurnal Oscillations of Gas Production and Effluxes (CO2 and CH4) in Cores from a Peat Bog

Peat cores (15 cm diam X 30 cm deep) from Ellergower Moss, New Galloway, Scotland were kept and monitored at constant temperature (10 ± 0.1ºC) for gas production using a 1.6 mm diam stainless steel probe fitted with a membrane inlet and connected to a quadrupole mass spectrometer. In the headspace, O₂, CO₂ and CH₄ (measured at m/z values 32, 44 and 15 respectively) showed diurnal fluctuations in low-intensity natural daylight and under a light-dark (LD, 12:12) regime. Over the first few cycles O₂ and CO₂ increased together in the dark and decreased in the light, whereas CH₄ showed variations in antiphase with the other two gases. CO₂ and CH₄ also showed diurnal oscillations at 15 cm depth, but these decreased together in the light whereas argon (m/z = 40) was not varying. A highly-damped free-run of the oscillations in gas concentrations at 15cm depth was evident for only 3 cycles in complete darkness and at constant temperature. This might suggest desynchronization between individual plants with different free-running periods. A hydrocarbon signal (m/z = 26) at 15 cm depth also showed diurnal cycles but out of phase with CO 2 and CH 4. We postulate a circadian control of microbiological activities imposed by the vascular plants (Carex, Eriophorum, Molinia, Calluna, Erica). Under natural conditions the pronounced temperature sensitivity of CO₂ and CH₄ emission results in entrainment to daily temperature cycles. The amplitudes of the rhythms are greatest when temperature and light intensity changes are most pronounced, i.e. when the fluctuations in environmental factors are most potent as synchronizers (zeitgebers) and as masking factors.     

Study of permeation and blocker binding in TMEM16A calcium-activated chloride channels

We studied the effects of mutations of positively charged amino acid residues in the pore of X. tropicalis TMEM16A calcium-activated chloride channels: K613E, K628E, K630E; R646E and R761E. The activation and deactivation kinetics were not affected, and only K613E showed a lower current density. K628E and R761E affect anion selectivity without affecting Na⁺ permeation, whereas K613E, R646E and the double mutant K613E + R646E affect anion selectivity and permeability to Na⁺. Furthermore, altered blockade by the chloride channel blockers anthracene-9-carboxylic acid (A-9-C), 4, 4''-Diisothiocyano-2,2''-stilbenedisulfonic acid (DIDS) and T16inh-A01 was observed. These results suggest the existence of 2 binding sites for anions within the pore at electrical distances of 0.3 and 0.5. These sites are also relevant for anion permeation and blockade.