Growth interactions between littoral diatoms and juvenile marine algae

Interactions have been studied between juvenile plants of green, brown, and red marine algae and 31 diatom clones isolated from a variety of marine eulittoral habitats. The interactions seemed to be of an individual nature for both juvenile plants and diatoms. Germlings of Ulva lactuca L. mostly showed enhanced growth, often with significant increases in population sizes of the accompanying diatoms. Fucus spiralis L. germlings were mainly unaffected by growth in the presence of the diatom clones, but growth of the diatoms was often stimulated. Ascophyllum nodosum (L.) Le Jol. germlings were little affected, whilst the accompanying diatoms were less noticeably affected than with Fucus spiralis. Germlings of F. vesiculosus L. often showed growth inhibitions in the presence of diatoms, with many diatom populations showing enhanced growth. Similarly, the discoid encrusting sporelings of Chondrus crispus Stackh. showed growth inhibitions where there were measurable interactions, although the accompanying diatoms usually failed to show growth stimulations. The discoid sporelings of Gigartina stellata (Stackh. in With.) Batt. showed high mortalities, usually with marked increases in population sizes of accompanying diatoms.     

Golgi apparatus activity and membrane flow during scale biogenesis in the green flagellateScherffelia dubia (Prasinophyceae). I: Flagellar regeneration

Summary Cells ofScherffelia dubia regenerate flagella with a complete scale covering after experimental flagellar amputation. Flagellar regeneration was used to study Golgi apparatus (GA) activity during flagellar scale production. By comparing the number of scales present on mature flagella with the flagellar regeneration kinetics, it is calculated that each cell produces ca. 260 scales per minute during flagellar regeneration. Flagellar scales are assembled exclusively in the GA and abstricted from the rims of thetrans-most GA cisternae into vesicles. Exocytosis of scales occurs at the base of the anterior flagellar groove. The central portion of thetrans-most cisterna, containing no scales, detaches from the stack of cisternae and develops a coat to become a coated polygonal vesicle. Scale biogenesis involves continuous turnover of GA cisternae, and scale production rates indicate maturation of four cisternae per minute from each of the cells two dictyosomes. A possible model of membrane flow routes during flagellar regeneration, which involves a membrane recycling loop via the coated polygonal vesicles, is presented.     

The amino acid sequences of the cytochromes c553 from Porphyridium cruentum and Aphanizomenon flos-aquae

The amino acid sequences of cytochrome c₅₅₃ from the eukaryotic red alga Porphyridium cruentum and from the prokaryotic cyanobacterium Aphanizomenon flos-aquae have been determined from the tryptic and cyanogen bromide peptides. The results indicate that a charged region of these proteins has evolved with special rapidity to accomodate a rapid evolution of a binding site in the P₇₀₀ electron acceptor complex.     

Nitrous oxide production by cyanobacteria

Evidence is presented here that axenic cultures of Nostoc spp., Aphanocapsa (PCC 6308), and Aphanocapsa (PCC 6714) but not Anacystis nidulans R-2 (PCC 7942) produce N₂O and ammonia when grown on nitrite. The data suggest that the cyanobacteria produce N₂O by nitrite reduction to ammonia.Nonstandard abbreviations DCMU 3-(3,4-dichlorophenyl)-1,1-dimethyl urea - NIR nitrite reductase     

Formation of plastocyanin and cytochrome c-553 in different species of blue-green algae

Fifteen species from different genera of blue-green algae have been examined for their formation of plastocyanin (PC) and cytochrome c-553 (cyt c-553) in high or low Cu media. In addition to species which contain only cyt c-553 and those which completely exchange their cyt c-553 by PC, a new regulatory type was detected in which this exchange was incomplete. By comparing different species, it could be shown that either this incomplete exchange of cyt c-553 by PC as well as lack of PC in some other blue-green algae is not caused by restricted Cu uptake but is due to different biosynthetic and regulatory properties. Occurrence of PC and cyt c-553 cannot be used as a taxonomic criterium to classify blue-green algae. However, formation of either one or both of these redox components fits well into a line of evolution of the photosynthetic apparatus from the blue-green algae via green algae to higher plants.Abbreviations PC plastocyanin; cyt c-553, cytochrome c-553     

Depth distribution of Campostoma grazing scars in an Ozark stream

Synopsis Campostoma spp., widespread and abundant herbivorous minnows of eastern North America, produce distinctive grazing scars when feeding on algae attached to natural substrates in streams. These scars are particularly prominent upon the low growth forms of blue-green algae that dominate the attached algal flora of many upland streams. In one stream pool in the Ozark uplands of Oklahoma, numbers and sizes of grazing scars coincided with numbers and sizes of individual Campostoma that occurred across a depth gradient, demonstrating that the information contained in the scars can provide quantification of microhabitat use and grazing intensity of these important herbivores. The results also support the hypothesis that in environments free of aquatic predators, larger fish use deeper parts of available stream habitats, particularly if threats from terrestrial or avian predators exist.     

THE LIPID COMPOSITION OF THORACOSPHAERA HEIMII: EVIDENCE FOR INCLUSION IN THE DINOPHYCEAE1

The fatty acid, sterol and chlorophyll composition of the calcified, unicellular alga Thoracosphaera heimii (Lohmann) Kamptner are reported. The presence of 4,23,24-termethyl-5α-cholest-22E-en-3β-ol (dinosterol), 4,23,24-trimethyl-5α-cholest-22E-en-3-one (dinosterone) and the predominance of C₁₈, C₂₀ and C₂₂ unsaturated fatty acids, including the acid 18:5ω3, indicates that T. heimii is a dinoflagellate. The fatty acid: sterol ratio (1.3), is typical of dinoflagellates. The geochemical significance of dinosterone, the high relative concentration of 4-desmethyl-5α-stanols and the role of 23-methyl-5α-cholest-22E-en-3β-ol in the biosynthesis of dinosterol in T. heimii are also discussed.