Library

Notes: Summary A total of 22 grass species were examined from 5 sites spanning the altitudinal range 1550–4350 m.a.s.l. The presence of the C3 or C4 photosynthetic pathway was determined from δ13C values and chilling tolerance was assessed on the basis of electrolyte leakage from leaf slices incubated on melting ice. Most of the grasses studied at the lower altitude sites of 1550 m.a.s.l. (annual mean of daily minimum temperature, 14.6° C) and 2600 m.a.s.l. (9.4° C) possessed C4 photosynthesis and were chill-sensitive. The single except ion was Agrostis avenacea, a montane chill-resistant C3 species which occurred at 2600 m.a.s.l. The three species apparently most sensitive to chilling were Ischaemum polystachyum, Paspalum conjugatum and Saccharum robustum, all occurring at 1550 m.a.s.l. At the higher altitude sites of 3280 (5.6° C), 3580 (4.0° C) and 4350 (−0.7°C) m.a.s.l., most of the grasses exhibited C3 photosynthesis and were chill-resistant. However, an Upland population of the C4 species, Miscanthus floridulus was found at 3280 m.a.s.l. which had acquired chill-resistance as confirmed by additional in vivo variable chlorophyll fluorescence measurements. Cell sap osmotic potential values of the upland grasses at altitudes of 3280–4350 m.a.s.l. were lower (−8.1 to −19.8 bars) than values in grasses from 1550 and 2600 m.a.s.l. (−3.9 to −7.5 bars) due mainly to the presence of non-electrolyte osmoticants, which may be involved in frost avoidance mechanism(s).

Notes: Abstract The organic-matter carbon isotope discrimination (Δ) of lichens with a wide range of photobiont and/or cyanobiont associations was used to determine the presence or absence of a carbon-concentrating mechanism (CCM). Two groups were identified within the lichens with green algal photobionts. One group was characterised by low, more C4-like Δ values (Δ 〈 15‰), the other by higher, more C3-like Δ values (Δ 〉 18‰). Tri-partite lichens (lichens with a green alga as the primary photobiont and cyanobacteria within internal or external cephalodia) occurred in both groups. All lichens with cyanobacterial photobionts had low Δ values (Δ 〈 15‰). The activity of the CCM, organic-matter Δ values, on-line Δ values and gas-exchange characteristics correlated with the presence of a pyrenoid in the algal chloroplast. Consistent with previous findings, lichens with Trebouxia as the primary photobiont possessed an active CCM while those containing Coccomyxa did not. Organic Δ values for lichens with Stichococcus as the photobiont varied between 11 and 28‰. The lichen genera Endocarpon and Dermatocarpon (Stichococcus + pyrenoid) had C4-like organic Δ values (Δ = 11 to 16.5‰) whereas the genus Chaenotheca (Stichococcus — pyrenoid) was characterised by high C3-like Δ values (Δ = 22 to 28‰), unless it associated with Trebouxia (Δ = 16‰). Gas-exchange measurements demonstrated that Dermatocarpon had an affinity for CO2 comparable to those species which possessed the CCM, with K0.5 = 200–215 μ1 · 1−1, compensation point (Γ) = 45–48 μl · l−1, compared with K0.5 = 195 μ1 · 1−1, Γ = 44μ1 · 1−1 for Trebouxioid lichens. Furthermore, lichens with Stichococcus as their photobiont released a small pool (24.2 ± 1.9 to 34.2 ± 2.5 nmol · mg−1 Chl) of inorganic carbon similar to that released by Trebouxioid lichens [CCM present, dissolved inorganic carbon (DIC) pool size = 51.0 ± 2.8 nmol · mg−1 Chl]. Lichens with Trentepohlia as photobiont did not possess an active CCM, with high C3-like organic Δ values (Δ = 18‰ to 23‰). In particular, Roccella phycopsis had very high on-line Δ values (Δ = 30 to 33‰), a low affinity for CO2 (K0.5 = 400 μ1 · 1−1,Γ = 120 μ1 · −1) and a negligible DIC pool. These responses were comparable to those from lichens with Coccomyxa as the primary photobiont with Nostoc in cephalodia (organic Δ = 17 to 25‰, on-line Δ = 16 to 21‰, k0.5 = 388 μ1 · 1−1, Γ = 85 μ1 · 1−1, DIC pool size = 8.5 ± 2.4 nmol · mg−1 Chl). The relative importance of refixation of respiratory CO2 and variations in source isotope signature were considered to account for any variation between on-line and organic Δ. Organic Δ was also measured for species of Anthocerotae and Hepaticae which contain pyrenoids and/or Nostoc enclosed within the thallus. The results of this screening showed that the pyrenoid is correlated with low, more C4-like organic Δ values (Δ = 7 to 12‰ for members of the Anthocerotae with a pyrenoid compared with Δ = 17 to 28‰ for the Hepaticae with and without Nostoc in vesicles) and confirms that the pyrenoid plays a fundamental role in the functioning of the CCM in microalgal photobionts and some bryophytes.