Page 48 - Algae
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General Overview                                                             31

                 appearance of these organisms, all photosynthetic organisms were anaerobic bacteria that used light
                 to couple the reduction of carbon dioxide to the oxidation of low free energy molecules, such as H 2 S
                 or preformed organics. Cyanobacteria developed a metabolic process, the photosynthesis, which
                 exploits the energy of visible light to oxidize water and simultaneously reduces CO 2 to organic
                 carbon represented by (CH 2 O)n using light energy as a substrate and chlorophyll a as a requisite
                 catalytic agent. Formally oxygenic photosynthesis can be summarized as:

                                                       Chlorophyll a
                                      CO 2 þ H 2 O þ light         ! (CH 2 O)n þ O 2

                     All other oxygen producing algae are eukaryotic, that is, they contain internal organelles,
                 including a nucleus, one or more chloroplasts, one or more mitochondria, and, most importantly,
                 in many cases they contain a membrane-bound storage compartment or vacuole. The three
                 major algal lineages of primary plastids are the Glaucophyta lineage, the Chlorophyta lineage,
                 and the Rhodopyta lineage (Figure 1.48).
                     Glaucophyta lineage occupies a key position in the evolution of plastids. Unlike other plastids,
                 the plastids of glaucophytes retain the remnant of a Gram-negative bacterial cell wall of the type
                 found in cyanobacteria, with a thin peptidoglycan cell wall and cyanobacterium-like pigmentation
                 that clearly indicate its cyanobacterial ancestry. In fact, the Cyanophora paradoxa plastid genome
                 shows the same reduction as other plastids when compared with free-living cyanobacteria (it is
                 136 kb and contains 191 genes). The peptidoglycan cell wall of the plastid is thus a feature retained
                 from their free-living cyanobacterial ancestor. In this context, the Glaucophyta are remarkable only
                 for their retention of an ancestral character present in neither green nor red plastids. No certain case
                 of a secondary plastid derived from Glaucophyta is known.
                     Green algae (Chlorophyta) constitute the second lineage of primary plastids. The simple two-
                 membrane system surrounding the plastid, the congruence of phylogenies based on nuclear and
                 organellar genes, and the antiquity of the green algae in the fossil record all indicate that the
                 green algal plastid is of primary origin. In these chloroplasts, chlorophyll b was synthesized as a
                 secondary pigment and phycobiliproteins were lost. Another hypothesis is that the photosynthetic
                 ancestor of green lineage was a prochlorophyte that possessed chlorophylls a and b and lacked
                 phycobiliproteins.
                     The green lineage played a major role in oceanic food webs and the carbon cycle from about 2.2
                 billion years ago until the end-Permian extinction, approximately 250 million years ago. It was this
                 similarity to the pigments of plants that led to the inference that the ancestors of land plants (i.e.,
                 embryophytes) would be among the green algae, and is clear that phylogenetically plants are a
                 group of green algae adapted to life on land. Euglenophyta and Chlorarachniophyta are derived
                 from this primary plastid lineage by secondary endosymbiosis; the green algal plastid present in
                 Euglenophyta is bounded by three membranes, while the green algal plastid present in the Chlor-
                 arachniophyta is bound by four membranes.
                     Since that time, however, a second group of eukaryotes has risen to ecological prominence; that
                 group is commonly called the “red lineage.” The plastids of the red algae (Rhodophyta) constitute
                 the third primary plastid lineage. Like the green algae, the red algae are an ancient group in the
                 fossil record, and some of the oldest fossils interpreted as being of eukaryotic origin are often
                 referred to the red algae, although clearly these organisms were very different from any extant
                 alga. Like those of green algae, the plastids of red algae are surrounded by two membranes.
                 However, they are pigmented with chlorophyll a and phycobiliproteins, which are organized
                 into phycobilisomes. Phycobilisomes are relatively large light-harvesting pigment/protein
                 complexes that are water-soluble and attached to the surface of the thylakoid membrane.
                 Thylakoids with phycobilisomes do not form stacks like those in other plastids, and consequently
                 the plastids of red algae (and glaucophytes) bear an obvious ultrastructural resemblance to
                 cyanobacteria.
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