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Lecanora muralis (Schreber) Rabenh., top-wall, Botanical Garden, Wü rzburg, Germany, 6 March, 1996. Diel courses of CO 2 exchange (upper panel), corresponding photosynthetic photon flux density (PPFD, second panel) and apparent PSII photosynthetic quantum yield (W) and calculated relative electron transport rate (ETR, third panel). Bottom panel: lichen net photosynthesis (CO 2exchange) in relation to electron transport rate.

Lecanora muralis (Schreber) Rabenh., top-wall, Botanical Garden, Wü rzburg, Germany, 6 March, 1996. Diel courses of CO 2 exchange (upper panel), corresponding photosynthetic photon flux density (PPFD, second panel) and apparent PSII photosynthetic quantum yield (W) and calculated relative electron transport rate (ETR, third panel). Bottom panel: lichen net photosynthesis (CO 2exchange) in relation to electron transport rate.

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Extensive investigations made in the past two decades on lichen photosynthesis in relation to water content have shown two features of particular interest: first, the depression of net photosynthesis at high water contents, suprasaturation (i.e. the lichen contains more water than necessary to saturate photosynthesis), and, second, the ability of g...

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... the first daily course, presented for 6 March 1996 (Fig. 5), the lichen had been wetted the previous day and had a relatively constant respiratory rate throughout the night. During the day the lichen maintained a moderate WC. Apparent photosynthetic quantum yield (W, 1 s saturating light pulses; methods see Leisner et al., 1997) remained high and NP tracked incident PPFD reaching a maximal ...
Context 2
... see Leisner et al., 1997) remained high and NP tracked incident PPFD reaching a maximal value around 2 mmol m À2 s À1 at about 300 mmol m À2 s À1 PPFD. Respiration continued the following night showing that the lichen had not dried out. Calculated ETR was almost linearly related to NP during this day, when the lichen was not suprasaturated (Fig. 5, lower ...

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... For example, the distribution of the maximum water holding capacity in a lichen and bryophyte community may affect carbon sequestration by these communities, since it will affect community hydrology and thereby the duration of the metabolic activity (Lange et al., 2001). Because of such effects of functional trait distributions, there has been increasing interest in exploring the functional composition of lichen and bryophyte communities. ...
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... The phenomenon, therefore, can be considered broadly in the context of the entire ecological group of lichens and not only as the specificity of individual species (see also TABLE 1). This probably implies difference between spatial distribution of forest and generalist lichens, especially when taking into account the realities of the natural environment and field performance of lichens (see Jonsson Čabrajić et al. 2010;Lange et al. 2001;Pintado et al. 1997;Pirintsos et al. 2011). ...
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... By contrast, most rainfall events supersaturate the lichen with excess water creating a film outside lichen surfaces that blocks the CO 2 uptake pathways and thereby causes strong depression of photosynthesis (Lange and Tenhunen 1981). Temporal suprasaturation depression is frequently documented (e.g., Lange and Matthes 1981;Lange et al., 1993Lange et al., , 2001, but less is known about how long-lasting continuous rain affects epiphytic vegetation in situ. Bryophytes replace lichens on trees within the more intense spray zone from waterfalls (Nilsson et al., 2022), and river regulations reducing the discharge of water can result in a great decrease in hygrophilous bryophytes and an increase in lichens (Odland et al., 1991). ...
... Most lichens have an optimal water content for photosynthesis, which approximately corresponds to the respective species' internal water holding capacity (Solhaug et al., 2021) measured after removing external water by blotting (Gauslaa 2014). Lichens need water to activate photosynthesis, but too much water reduces the CO 2 uptake by suprasaturation depression (Lange and Matthes 1981;Lange et al. 1993Lange et al. , 2001. Growth chamber experiments show that continuous hydration over two weeks is detrimental to lichens, which need to dry at least once a day to perform well (e.g., Solhaug and Gauslaa 2004). ...
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... In contrast, most bryophytes are reliant on liquid water (Proctor 2000;Proctor et al. 2007), mostly from rainfall (Proctor 2000), but also from dew (Csintalan et al. 1999), or cloud droplets (Leon-Vargas et al. 2006). Second, for lichens, oversaturation with water can limit photosynthesis via limited CO 2 diffusion (Lange et al. 1993(Lange et al. , 2001, whereas most bryophytes can thrive under continuously wet conditions (Proctor 2000). Finally, net photosynthesis is positive at a lower and narrower range of temperatures for lichens (Palmqvist 2008) than for bryophytes (Furness and Grime 1982;Liu et al. 2001). ...
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... Low YPSII is a consequence of suboptimal intrathalline CO 2 concentration caused by limitation in the diffusion of CO 2 molecules in fully hydrated cyanolichen thalli. It is believed that exopolysacharidic cellular envelopes in cyanobacteria and their high diffusion resistance for CO 2 in a fully hydrated state are the underlying mechanism causing the supersaturation effect [26]. Recently, we showed that in several Antarctic lichen species in natural conditions, the dehydrationdependent drop in FV/FM and YPSII was species-specific, starting at an RWC range of 22-32%. ...
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Climate warming in the Antarctic tundra will affect locally dominant cryptogams. Being adapted to low temperatures and freezing, little is known about the response of the polar lichens’ primary photochemistry to warming and desiccation. Since 2008, we have monitored the ecophysiological responses of lichens to the future warming scenario during a long-term warming experiment through open top chambers (OTCs) on Fildes Peninsula. We studied the primary photochemical response (potential Fv/Fm and effective efficiency of photosystem II YPSII) of different lichen taxa and morphotypes under desiccation kinetics and heat shock experiments. As lichens grow slowly, to observe changes during warming we methodologically focused on carbon and nitrogen content as well as on the stable isotope ratios. Endemic Himantormia lugubris showed the strongest effect of long-term warming on primary photochemistry, where PSII activity occurred at a lower %RWC inside the OTCs, in addition to higher Fv/Fm values at 30 °C in the heat shock kinetic treatment. In contrast, Usnea aurantiaco-atra did not show any effect of long-term warming but was active at a thallus RWC lower than 10%. Both Cladonia species were most affected by water stress, with Cladonia aff. gracilis showing no significant differences in primary photochemical responses between the warming and the control but a high sensibility to water deficiency, where, at 60% thallus RWC, the photochemical parameters began to decrease. We detected species-specific responses not only to long-term warming, but also to desiccation. On the other hand, the carbon content did not vary significantly among the species or because of the passive warming treatment. Similarly, the nitrogen content showed non-significant variation; however, the C/N ratio was affected, with the strongest C/N decrease in Cladonia borealis. Our results suggest that Antarctic lichens can tolerate warming and high temperature better than desiccation and that climate change may affect these species if it is associated with a decrease in water availability
... Lichens not only tolerate but require regular cycles of wetting and drying (Armstrong, 1976). Prolonged saturation, by contrast, can be physiologically limiting by slowing CO 2 and O 2 diffusion (Lange et al., 2001), particularly for phototrophs lacking mechanisms to counteract this (see Section VII). ...
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Lichens are the symbiotic outcomes of open, interspecies relationships, central to which are a fungus and a phototroph, typically an alga and/or cyanobacterium. The evolutionary processes that led to the global success of lichens are poorly understood. In this review, we explore the goods and services exchange between fungus and phototroph and how this propelled the success of both symbiont and symbiosis. Lichen fungal symbionts count among the only filamentous fungi that expose most of their mycelium to an aerial environment. Phototrophs export carbohydrates to the fungus, which converts them to specific polyols. Experimental evidence suggests that polyols are not only growth and respiratory substrates but also play a role in anhydrobiosis, the capacity to survive desiccation. We propose that this dual functionality is pivotal to the evolution of fungal symbionts, enabling persistence in environments otherwise hostile to fungi while simultaneously imposing costs on growth. Phototrophs, in turn, benefit from fungal protection from herbivory and light stress, while appearing to exert leverage over fungal sex and morphogenesis. Combined with the recently recognized habit of symbionts to occur in multiple symbioses, this creates the conditions for a multiplayer marketplace of rewards and penalties that could drive symbiont selection and lichen diversification.
... Estimating of parameters of primary photosynthesis based on the analysis of chlorophyll fluorescence (CF) induction kinetics (including parameters of 'fast' and stationary phases of inductive curves) is extensively applied in lichen biology in order to access the physiological state of these supraorganismal systems (Lange et al. 2001;Kalaji et al. 2016; Barták 2014;Stirbet et al. 2014;Goltsev et al. 2016;Palharini et al. 2020;Kuusinen et al. 2020). These parameters largely depend on the environmental conditions, embracing the presenceof pollutants and physiological conditions . ...
... On the one hand, the assimilation efficiency depends on intrathalline CO 2 availability which is affected by hydration status of the thallus (Lange et al. 2006(Lange et al. 1999. These data may be obtained from the experiments of CO 2 exchange measurements as a function of lichen water potential (Lange et al. 2001). On the other hand, it depends on the primary processes of photosynthesis. ...
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The measurements of chlorophyll fluorescence play an important role in studies of lichen physiology. Usually, for foliose lichens fluorescence kinetics is recorded from the upper thalline side often exhibiting green color reflecting the presence of photosynthetic pigments. The lower side of such lichens is grey, dark-brown or black. At the first time, we evaluated photosynthetic activity distribution by chlorophyll fluorescence analysis on both lower and upper thallus sides for the foliose lichen Nephroma arcticum. We have demonstrated that photosynthesis proceeds not only on the green-colored upper side, but also on the gray lower side of the curled growing edges of the thallus lobes. These sides were differed in terms of PSII photochemical quantum yield, activity of non-regulatory dissipation and non-photochemical quenching of excited chlorophyll states (NPQ). Upper side was characterized by higher maximal PSII efficiency, whereas the lower one of the curled edges was characterized by higher actual photochemical quantum yield during actinic light acclimation. NPQ was higher on the upper surface, whereas, on the lower side (of the curled edges) non-regulatory dissipation was predominant. In terms of photosynthetic activity measurements, these results show, that actinic and measuring light reached the layer of phycobiont despite its shielding by mycobiont hyphae. On the melanized lower side in the basal thalline zone attached to the substratum photosynthesis was not detected. Lower side demonstrated higher level of light scattering in the reflectance spectra. We believe that different photoprotective mechanisms against high light are crucial on the upper and lower sides: NPQ on the upper surface, and light scattering and shielding by mycobiont on the lower side. Possible biological role of photosynthesis on the lower side is discussed.