Photoprotection in bryophytes: rate and extent of dark relaxation of non-photochemical quenching of chlorophyll fluorescence

Vascular plants are typically endohydric and are killed by drying beyond 30% relative water content. Bryophytes are ectohydric and are typically desiccation tolerant (DT). Mosses in open sun-exposed habitats show major electron flow to oxygen and high levels of non-photochemical quenching (NPQ) in chlorophyll fluorescence measurements. This has been regarded as a main source of photoprotection for these plants. The aim of the work described in this paper was to explore the rate and extent of relaxation of this quenching, and to seek evidence of its nature and consequences. Sequences of measurements were made during illumination at various intensities and a subsequent dark period. Light-response curves were constructed using dithiothreitol (DTT) as an inhibitor of violaxanthin de-epoxidase to provide additional evidence of the proportion of NPQ mediated by the xanthophyll cycle. The relaxation curves were fitted by exponential decay curves. A double-exponential fit to curves for the sun-adapted species gave a fast phase with a halflife of ca 6–16 seconds, and a slow phase with a halflife of ca 100–300 seconds. Shade species were best fitted by single-exponential curves. A persistent offset remained of ca 5–23% of the pre-darkening NPQ. Light-response curves for several species showed NPQ reduced in the presence of DTT to similar proportions of the control. Around 70–95% of NPQ in the bryophytes investigated relaxed with a halflife of ca 2–5 minutes. The fast phase of the double-exponential fit is consistent with likely rates of decay of the trans-thylakoid pH gradient and re-epoxidation of zeaxanthin. This leads to the same conclusion as the effect of DTT in depressing NPQ. The contrast in physiology between bryophytes and vascular plants reflects the different selection pressures facing leaf cells of poikilohydric plants and the mesophyll cells of vascular plants, and their divergent evolutionary histories since the mid-Palaeozoic.