Abstract

The LH1 complex is the major light-harvesting antenna of purple photosynthetic bacteria. Its role is to capture photons, and then store them and transfer the excitation energy to the photosynthetic reaction center. The structure of LH1 is modular and it cooperatively self-assembles from the subunits composed of short transmembrane polypeptides that reversibly bind the photoactive cofactors: bacteriochlorophyll and carotenoid. LH1 assembly, the intra-complex interactions and the light-harvesting features of LH1 can be controlled in micellar media by varying the surfactant concentration and by adding carotenoid and/or a co-solvent. By exploiting this approach, we can manipulate the size of the assembly, the intensity of light absorption, and the energy and lifetime of its first excited singlet state. For instance, via the introduction of Ni-substituted bacteriochlorophyll into LH1, the lifetime of this electronic state of the antenna can be shortened by almost three orders of magnitude. On the other hand, via the exchange of carotenoid, light absorption in the visible range can be tuned. These results show how in a relatively simple self-assembling pigment-polypeptide system a sophisticated functional tuning can be achieved and thus they provide guidelines for the construction of bio-inspired photoactive nanodevices.

Highlights

  • The evolution of photosynthesis on Earth began approximately 3.5 billion years ago with the appearance of anaerobic phototrophic bacteria in the oceans, soon followed by the emergence of oxygenic cyanobacteria, and by plants [1]

  • We show how it can be exploited to allow the essential functional and structural properties of a biological photodevice—the bacterial photosynthetic antenna LH1—to be controlled and tuned

  • 5%, the B820 heterodimer was dissociated to the monomeric B780 subunits, comprised of single α and β polypeptides, each coordinating a single bacteriochlorophyll a (BChla) molecule [30]

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Summary

Introduction

The evolution of photosynthesis on Earth began approximately 3.5 billion years ago with the appearance of anaerobic phototrophic bacteria in the oceans, soon (in geological terms) followed by the emergence of oxygenic cyanobacteria, and by plants [1]. Millions of years of efficient solar energy conversion by photosynthetic autotrophs resulted in a surplus of biomass and molecular oxygen. The accumulation of this very reactive by-product of oxygenic photosynthesis led to the oxidation of the planetary crust and the reductive primary atmosphere being turned into an oxidative one, saturated to a high degree with oxygen. Purple photosynthetic bacteria seem to be a direct descendent of these archaic phototrophic bacteria. Their relatively simple photosynthetic apparatus, composed of a photosynthetic reaction center (RC) surrounded by a modular ring-shaped light-harvesting antenna.

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