Photosynthetic acclimation to photon irradiance and its relation to chlorophyll fluorescence and carbon assimilation in the halotolerant green alga Dunaliella viridis

被引:37
作者
Gordillo, FJL
Jiménez, C
Chavarría, J
Niell, FX
机构
[1] Queens Univ Belfast, Dept Agr & Environm Sci, Aquat Syst Grp, Belfast BT9 5PX, Antrim, North Ireland
[2] Univ Malaga, Fac Ciencias, Dept Ecol, E-29071 Malaga, Spain
关键词
carbon release; Dunaliella; fluorescence; irradiance; photoinhibition; quenching; xanthophyll;
D O I
10.1023/A:1012969324756
中图分类号
Q94 [植物学];
学科分类号
071001 ;
摘要
This work describes the long-term acclimation of the halotolerant microalga Dunaliella viridis to different photon irradiance, ranging from darkness to 1500 mu mol m(-2) s(-1.) In order to assess the effects of long-term photoinhibition, changes in oxygen production rate, pigment composition, xanthophyll cycle and in vivo chlorophyll fluorescence using the saturating pulse method were measured. Growth rate was maximal at intermediate irradiance (250 and 700 mu mol m(-2) s(-1)). The increase in growth irradiance from 700 to 1500 mu mol m(-2) s(-1) did not lead to further significant changes in pigment composition or EPS, indicating saturation in the pigment response to high light. Changes in Photosystem II optimum quantum yield (Fv/Fm) evidenced photoinhibition at 700 and especially at 1500 mu mol m(-2) s(-1). The relation between photosynthetic electron flow rate and photosyntetic O-2 evolution was linear for cultures in darkness shifting to curvilinear as growth irradiance increased, suggesting the interference of the energy dissipation processes in oxygen evolution. Carbon assimilation efficiencies were studied in relation to changes in growth rate, internal carbon and nitrogen composition, and organic carbon released to the external medium. All illuminated cultures showed a high capability to maintain a C:N ratio between 6 and 7. The percentage of organic carbon released to the external medium increased to its maximum under high irradiance (1500 mu mol m(-2) s(-1)). These results suggest that the release of organic carbon could act as a secondary dissipation process when the xanthophyll cycle is saturated.
引用
收藏
页码:225 / 235
页数:11
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