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Growth and water use of the mangroves Rhizophora apiculata and R. stylosa in response to salinity and humidity under ambient and elevated concentrations of atmospheric CO 2
Author(s) -
BALL M. C.,
COCHRANE M. J.,
RAWSON H. M.
Publication year - 1997
Publication title -
plant, cell and environment
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.646
H-Index - 200
eISSN - 1365-3040
pISSN - 0140-7791
DOI - 10.1046/j.1365-3040.1997.d01-144.x
Subject(s) - salinity , mangrove , relative humidity , relative growth rate , humidity , growth rate , arid , ecology , botany , biology , geography , geometry , mathematics , meteorology
Two mangrove species, Rhizophora apiculata and R. stylosa , were grown for 14 weeks in a multifactorial combination of salinity (125 and 350 mol m −3 NaCl), humidity (43 and 86% relative humidity at 30°C) and atmospheric CO 2 concentration (340 and 700 cm 3 m −3 ). Under ambient [CO 2 ], growth responses to different combinations of salinity and humidity were consistent with interspecific differences in distribution along natural gradients of salinity and aridity in northern Australia. Elevated [CO 2 ] had little effect on relative growth rate when it was limited by salinity but stimulated growth when limited by humidity. Both species benefited most from elevated [CO 2 ] under relatively low salinity conditions in which growth was vigorous, but relative growth rate was enhanced more in the less salt‐tolerant and more rapidly growing species, R. apiculata. Changes in both net assimilation rate and leaf area ratio contributed to changes in relative growth rates under elevated [CO 2 ], with leaf area ratio increasing with decrease in humidity. Increase in water use efficiency under elevated [CO 2 ] occurred with increase, decrease or no change in evaporation rates; water use characteristics which depended on both the species and the growth conditions. In summary, elevated [CO 2 ] is unlikely to increase salt tolerance, but could alter competitive rankings of species along salinity × aridity gradients.