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Gas Exchange Rates and Chlorophyll Content of Epi- and Endolithic Lichens from the Trieste Karst (NE Italy)

M. Tretiach and M. Pecchiari
The New Phytologist
Vol. 130, No. 4 (Aug., 1995), pp. 585-592
Published by: Wiley on behalf of the New Phytologist Trust
Stable URL: http://www.jstor.org/stable/2558728
Page Count: 8
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Gas Exchange Rates and Chlorophyll Content of Epi- and Endolithic Lichens from the Trieste Karst (NE Italy)
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Abstract

The photosynthetic activity of calcicolous endo- and epilithic lichens from the Trieste Karst area (NE Italy) was investigated. The data consist of: (a) gas exchange rates of Acrocordia conoidea, Petractis clausa, Rinodina immersa (endolithic), and Aspicilia calcarea (epilithic), recorded at different combinations of temperature, water content and radiation flux values, (b) chlorophyll content values of nine species, and (c) δ13C values measured in 24 lichen species with different growth-forms. The results show that: (1) the maximum photosynthetic rates of endolithic lichens are rather small, ranging between 0.2 and 1.5 μmol CO2 m-2 h-1 at optimal conditions; (2) the relation between thallus water content and photosynthesis differs from that of foliose and fruticose lichens; the optimum water content of endolithic lichens is particularly small, when expressed in g H2O cm-2; (3) the algae of endolithic lichens, which belong to different systematic groups, are light-saturated at a small radiation flux; (4) chlorophyll contents of endolithic lichens are rather large, being similar to those of some parmelioid lichens. The ecological implications of the endolithic growth-form are briefly discussed. Endolithic lichens should be regarded as slow-growing, stress-tolerant organisms, which are rather similar in their physiology to epilithic crustose lichens; they have a high resistance to CO2 diffusion, saturation being reached only at a very large CO2 concentration.

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