CONCEPTACLE STRUCTURE OF THE PARASITIC CORALLINE RED ALGA CHOREONEMA THURETII (CORALLINALES) AND ITS TAXONOMIC IMPLICATIONS1

The major diagnostic features for erecting the red algal subfamily Choreonematoideae (Corallinales) were a combination of 1) absence of both cell fusions and secondary pit connections, 2) conceptacle roof and wall comprised of a single cell layer, and 3) presence of tetrasporangial pore plugs within a uniporate conceptacle in the monotypic taxon Choreonema thuretii (Bornet) Schmitz. Because this alga is a parasite, the absence of secondary cell connections is most likely an adaptation to a reduced thallus. This study shows that all conceptacles are not composed of a file of cells but rather a single layer of epithallial cells that are underlain by a thick layer of calcified acellular material; both epithallial cells and the calcified layer are produced by peripheral sterile cells. Although the outermost tetrasporangial pore canal is uniporate, there is a calcified acellular multiporate plate recessed just below the rim. The plate is produced by interspersed sterile cells and is continuous with the calcified layer supporting the conceptacle. These unique structures are likely due to parasitism rather than to the ancestral state. Based on these results and a reexamination of published micrographs depicting lenticular cells in Austrolithon intumescens Harvey et Woelkerling, we propose that both subfamily Choreonematoideae and Austrolithoideae are closely allied with subfamily Melobesioideae. This distant relationship to its host (Corallinoideae) plus a combination of unique conceptacle and unusual type of parasitism indicates that C. thuretii is an alloparasite and that it is likely the most ancient red algal parasite studied to date.     

Fine structure of the phylogenetically important marine algaRhodogorgon carriebowensis (Rhodophyta,Batrachospermales?)

Summary The fine structure of the recently described red algaRhodogorgon carriebowensis J. Norris et Bucher was studied by light microscopy and scanning and transmission electron microscopy to aid in the ordinal placement of this unusual alga. Most significant in this context were findings that pit plugs had two-layered plug caps, the outer layer of which formed a large dome and was composed of glycoprotein. Cap membranes appeared to be absent. Medullary cells were remarkable in having extremely thick, layered cell walls, whose inward deposition left little room for cytoplasm. Medullary filaments branched little except near the base of the cortex. The assimilatory filaments that made up most of the cortex contained almost all the pigmentation and starch reserves of the thallus. These filaments terminated in either slender apical cells with smooth cell walls or bulbous apical cells bearing spinulose projections. Two types of elongated cells were found in the cortex, those with calcified cell walls and those surrounded by multiple, spreading layers of wall material. Neither cell type was pigmented. The latter type sometimes supported normal assimilatory cells.The hypothesis is proposed thatRhodogorgon is a descendant of the marine progenitors of the Batrachospermales and thus is a member of this order.Abbreviations DIC differential interference contrast - PAS periodic acid Schiff - PTA-CA phosphotungstic acid-chromic acid     

Morphology, anatomy and reproduction of the eastern Mediterranean coralline Tenarea tortuosa and its relationship to members of the Lithophylloideae and Mastophoroideae (Rhodophyta, Corallinales)

One of the most characteristic organisms of the Mediterranean flora, the endemic coralline Tenarea tortuosa , has been collected along the Cretan coast and its vegetative and reproductive structures are reassessed. Gametophytes are described for the first time and are rare, observed only in one locality on the south coast. Reproductive structures suggest that the sexual life history is triphasic, but the present collections indicate unequal representation of males, carposporophytes and tetrasporophytes, and a dominance of bisporophytes suggesting that the alga is reproducing mainly asexually. The frond of Tenarea is formed by the coordinated growth of two elements (branches), growing back-to-back, each showing a simple Titanodema-type of organization; i.e. a monostromatic hypothallium of sinuous cells and a single layer of obliquely borne epithallial cells. Contiguous cells of the two opposite branches are not connected by secondary pit-plugs, and easily glide apart if decalcified. Natural splitting of the lamellae into its two branches may also occur, and single branches may fold regenerating the back-to-back organization. Analogous back-to-back growths occur in species of the distantly related genera Goniolithon (Lithophylloideae) and Leptophytum (Melobe-sioideae) and apparently represent cases of convergence. The affinities of Tenarea to related genera are discussed.     

Relationship between cover of Chondrus crispus (Gigartinales,Rhodophyta) and Phymatolithon (Corallinales,Rhodophyta) on friable rock substrata

Field observations in sublittoral Prince Edward Island, Canada, indicated that on a friable sandstone substratum Chondrus crispus was more commonly associated with Phymatolithon sp. than with bare rock. Thus, a substantial proportion of the population of Irish moss along the coast of Prince Edward Island occurs on this encrusting coralline. These observation may be explained on the basis of the relative stability of the substratum in contrast to other studies in which sloughing of epithallial cells by species of both Phymatolithon and Lithothamnium has been reported to limit epiphytism by fleshy macrophytes.Issued as NRCC 31426.     

Microcladia exserta sp. nov. (Ceramiaceae,Rhodophyta) from the East coast of South Africa

Microcladia exserta, a new species of the red algal genus Microcladia Greville (Ceramiaceae, Ceramiales), is described from the Natal coast of South Africa. This small, creeping alga, an epiphyte on the coralline alga Amphiroa anceps (Lamarck) Decaisne, is distinguished from other species in the genus by the following combination of characteristics: the prostrate habit, the exerted position of the tetrasporangia, and the presence in the cortex of numerous and conspicuous vesicle cells. Evidence is presented to demonstrate that the criterion of an erect habit in Microcladia vs. a prostrate habit in Herpochondria used to separate these genera is not sound.     

A unique algal ridge system in the Exuma Cays, Bahamas

 An algal ridge system discovered along the Exuma Cays, Bahamas constructs bioherms to a thickness of at least 1.5 m and is associated with modern intertidal stromatolites. These algal ridges are unique because they grow in atypical environments characterized by relatively low wave energy, high rates of sedimentation and low rates of herbivory. They also are composed primarily of the branching crustose coralline alga, Neogoniolithon strictum, which heretofore was not known to form algal ridges. Lateral growth rates of crusts, vertical growth rates of branches and survivorship of transplanted N. strictum were greatest in the shallow fore reef zone of the algal ridge. The alga is also capable of surviving and growing when covered with sediment for at least 100 days. Under such conditions it transforms from a branched to an unbranched morphology. Parrotfish grazing, which is said to limit the abundance of branched corallines and algal ridges, was two orders of magnitude lower than in published accounts from other reef systems of the Caribbean and one order of magnitude less than that found on nearby coral reefs of the west Exuma Sound. Neogoniolithon strictum, a delicate and open-branched coralline, persisted for over a year without grazing damage when transplanted to a depth of 2.3 m. This algal ridge-building coralline becomes a well-indurated limestone following submarine lithification of sediment that infills the open branch framework. As a result, N. strictum ridges are comparable to the dense frameworks associated with most algal ridges. Observations of N. strictum -associated bioherms along Central America suggest this ridge system may exist elsewhere under conditions similar to those described for the Bahamas. Accepted: 23 March 1996     

Bromine, Bromophenols and Floridorubin in the Red Alga Lenormandia prolifera

The pigment floridorunin was localized to the cuticle of the red alga Lenormandia prolifera (C. Ag.) J. Agardh by x-ray micro-analysis in Ihe transmission electron microscope and by its colour reactions in the light microscope. The pigment was set free from the cell wall by a pectinase. Bromine was also identified in the chloro-plasts. the middle lamellae, the intercellulars and the pore plugs of the alga. The content of bromophenols in the alga increases with increasing age. The cell walls of old plants are stratified and their outer parts are apparently shed. The bromophenols could have a function as regulators of the epiphytes or the shedding of parts of the outer cell wall.     

The Role of Encrusting Coralline Algae in the Diets of Selected Intertidal Herbivores

Kalk Bay, South Africa, has a typical south coast zonation pattern with a band of seaweed dominating the mid-eulittoral and between two molluscan-herbivore dominated upper and lower eulittoral zones. Encrusting coralline algae were very obvious features of these zones. The most abundant herbivores in the upper eulittoral were the limpet, Cymbula oculus (10.4 ± 1.6 individuals m⁻²; 201.65 ± 32.68 g.m⁻²) and the false limpet, Siphonaria capensis (97.07± 19.92 individuals m⁻²; 77.93 16.02 g.m⁻²). The territorial gardening limpet, Scutellastra cochlear, dominated the lower eulittoral zone, achieving very high densities (545.27 ± 84.35 m⁻²) and biomass (4630.17 ± 556.13 g.m⁻²), and excluded all other herbivores and most seaweeds, except for its garden alga and the encrusting coralline alga, Spongites yendoi (35.93 ± 2.26% cover). In the upper eulittoral zone, encrusting coralline algae were only present in the guts of the chiton Acanthochiton garnoti (30.5 ± 1.33%) and the limpet C. oculus (2.9 ± 0.34%). The lower eulittoral zone limpet, Scutellastra cochlear also had a large percentage of encrusting coralline algae in its gut with limpets lacking gardens having higher (45.1 ± 1.68%) proportions of coralline algae in their guts than those with gardens (25.6 ± 0.8%). Encrusting coralline algae had high organic contents, similar to those of other encrusting and turf-forming algae, but higher organic contents than foliose algae. Radula structure, grazing frequencies as a percentage of the area grazed (upper eulittoral 73.25 ± 3.60% d⁻¹; lower eulittoral 46.0 ± 3.29% d⁻¹), and algal organic content provided evidence to support the dietary habits of the above herbivores. The data show that many intertidal molluscs are actively consuming encrusting coralline algae and that these seaweeds should be seen as an important food source.     

Keratinization of fish skin with special reference to the catfish Bagarius bagarius

Summary Histochemical reactions indicating keratinization have previously been demonstrated in parts of the epidermis of Bagarius bagarius. Fluorescence histochemistry and electron microscopy have now confirmed these results. Elevated areas of the epidermis are capped by a layer of dead cells with altered contents. On the outer aspect of these cells a dense layer, 18 nm thick, beneath the plasma membrane corresponds to the resistant envelope found in keratinized cells in tetrapod vertebrates. In Bagarius this layer does not extend to all faces of the keratinized cells, but a similar envelope has been detected in two other sites of piscine keratinized epidermis investigated, namely in the breeding tubercles of Phoxinus phoxinus and in the teeth of Lampetra fluviatilis. In the elevated areas of Bagarius-epidermis, the epithelial cells undergo progressive changes in cytoplasmic organization as they become more superficial. The second tier from the surface is sealed by tight junctions and is separated from the overlying keratinized cells by a sub-corneal space resembling that found in keratinized amphibian epidermis. Histochemical evidence of a high lipid content in the outer layers of the epidermis correlates with the presence of lipid inclusions and lamellated membranous profiles in the material studied by electron microscopy. Histochemical results show that the fin skin of Blennius pholis is not keratinized, but secretes a cuticle, histochemically reactive for both proteins and glycoproteins.     

INITIAL TWIG INJURY TO HIGH ELEVATION PICEA RUBENS IN EASTERN NORTH AMERICA CAUSED BY INADEQUATE PERIDERM FORMATION

Apical dieback is the predominant injury symptomatology associated with growth declines of high elevation Picea rubens Sarg, trees in North America. Histological observations of uninjured tissues and of initial injury to tissues were made to understand the mechanism of injury to this species. Observations were made of hundreds of grab samples of apparently uninjured tissues and of uninjured twigs from trees growing on mountains of the Adirondack Mt., NY; Mount Mansfield, VT; Mt. Mitchell, NC; and Clingman's Dome, TN, from March 1985 to April 1986. In the normal growth pattern of red spruce, three buds elongate from each twig terminus during spring. These buds expand into shoot increments during the growing season and three new buds will form at the tip of each of the three elongated increments. The timing of developmental events varied markedly among buds of individual trees and among trees. Bud break occurred between mid-June to the end of July. Most shoot elongation was completed and periderm formation began near the end of August or in early September. A phellogen, one cell thick, formed and a phellem layer developed from phellogen derivatives during autumn 1985. Many twig samples taken in October and November had produced only one, or at most two, phellem layers external to the phellogen during the relatively short growing season. In some samples, three or more phellem layers were present between November 1985 and March 1986. In some cases a distinct phellem was not developed at all. Usually a phelloderm one cell thick developed in autumn of the first year. Tissue necrosis occurred in twigs during their first overwintering period. Injured twigs with necrotic tissues had only one or two continuous or discontinuous phellem layers. In samples that exhibited initial injury, necrotic tissues consisted mostly of cortical cells and phloem subjacent to this meager periderm. Frequently, necrotic tissues developed initially near the bases of needles and at branch “nodes” (transition zone tissues with older twigs). In contrast, twigs of healthy appearance had two or more continuous phellem layers external to the phellogen.     

CYANOPHYTE CEPHALODIA IN THE LICHEN GENUS NEPHROMA

The lichens, Nephroma expallidum (Nyl.) Nyl. and N. arcticum (L.) Torss., consistently have at least two symbionts in a single thallus: a green alga in the algal layer and a blue-green alga in the internal cephalodia. The cephalodia originate from algal cells in contact with the lower surface of the lichen, in the zone of rhizine formation. The rhizines surround the epiphytic algal colony and form a second cortical layer; following dissociation of the original lower cortex, further growth of the two organisms results in the cyanophyte colony being enveloped by a compact layer of fungal tissue and positioned in the lichen medulla. The colony may eventually assume a superior or inferior position in relation to the lichen thallus, depending in part on the lichen species. Nephroma anticum may have two distinct morphological forms of blue-green algae in the same thallus and occasionally in the same cephalodium. It appears that the relationship that exists between the cephalodial algae and the lichen thallus is antagonistic and results, in some cases, in the exclusion of the green algal layer and death to the cephalodial cyanophytes.     

ULTRASTRUCTURE OF THE CORALLINACEAE (RHODOPHYTA) II. VEGETATIVE CELLS OF LITHOTHRIX ASPERGILLUM1

The ultrastructure of the calcareous red coralline alga Lithothrix aspergillum Gray and the development of the various tissue types has been studied. The sub-apical meristematic tissue alternately produces genicular or intergenicular cells. The genicular cells rapidly elongate and their cell walls thicken and become denser as more fibrillar wall material is laid down within the cell wall. These cells contain little cytoplasm and few organelles. The inter genicular cells which elongate only slightly during development have a small vacuole and many free starch grains in the cytoplasm. The peripheral cells in each inter genicular layer remain meristematic and form a cortical cell layer over the genicular cells. These cortical cells and the apical meristematic cells are covered by small epidermal cells which have extensive cell wall ingrowths between the chloroplasts. The inter genicular cells are calcified. Although the CaCO₃ is laid down within the cell walls, there is always a thin layer of CaCO₃-free organic cell wall material between the plasmalemma and the CaCO₃ impregnated wall. Only the distal tips of the genicular cells are calcified. In old genicular tissues of Lithothrix, secondary deposits of CaCO₃ of unknown crystallography are also found in the spaces between the cell walls. Thus there appear to be at least two mechanisms of calcification in this alga.     

SEPTAL PLUGS IN A GREEN ALGA

Septal plugs, resembling those found in red algae, occur in the transverse wall between all cells in a newly discovered marine green alga, Pilinia earleae Gallagher & Humm.³ No plasmodesmata traverse the cross-wall, and the septal plug blocks cytoplasmic continuity between cells. The septal plug consists of an electron-translucent core bordered at each end by two electron-opaque caps. Cytochemical procedures demonstrate that the plug consists of protein and polysaccharide, but lacks peroxidase. The outer cap is highly proteinaceous while the inner cap is composed primarily of polysaccharide. The plug core is not routinely stained by Coomassie Blue but it is pronase sensitive and probably proteinaceous. Historically, septal plugs have been considered unique to the red algae and the fungi, but ultrastructural and biochemical data provide no support for derivation of the septal plug in this green alga from a symbiotic relationship. The discovery of septal plugs in a green alga makes the hypothesis of an independent origin of this structure in a number of plant groups more likely.     

Facultative mutualism between an herbivorous crab and a coralline alga: advantages of eating noxious seaweeds

Because encrusting coralline algae rely on herbivory or low light levels to prevent being overgrown by competitively superior fleshy algae, corallines are relatively rare in shallow areas with low rates of herbivory. In contrast to this general trend, the branching coralline alga Neogoniolithon strictum occurs primarily in shallow seagrass beds and along the margins of shallow reef flats where herbivory on macrophytes is low. This alga apparently persists in these habitats by providing refuge to the herbivorous crab Mithrax sculptus at mean densities of 1 crab per 75 g of algal wet mass. When crabs were removed from some host corallines, hosts without crabs supported 9 times the epiphytic growth of hosts with crabs after only 30 days. Crabs without access to a coralline alga were rapidly consumed by reef fishes, while most of those tethered near a host alga survived. These results suggest that the crabs clean their algal host of fouling seaweeds and associate with the host to minimize predation. However, to effectively clean the host, the crab must consume the wide array of macroalgae that commonly co-occur with coralline algae in these habitats, including chemically defended species in the genera Halimeda, Dictyota, and Laurencia. Crabs did readily consume these seaweeds, which were avoided by, and are chemically defended from, herbivorous fishes. Even though crabs readily consumed both Halimeda and Dictyota in whole-plant feeding assays, chemical extracts from these species significantly reduced crab feeding, suggesting that factors other than secondary chemistry (e.g., food value, protein, energy content), may determine whole-plant palatability. Having the ability to use a wide variety of foods, and choosing the most profitable rather than the least defended foods, would diminish foraging time, increase site fidelity, and allow the crab to function mutualistically with the host alga. Despite the obvious benefit of associating with N. strictum, M. sculptus did not prefer it over other habitats offering a structurally similar refuge, suggesting that these crabs are not N. strictum specialists, but rather occupy multiple habitats that provide protection from predators. Structurally complex organisms like N. strictum may commonly suppress competitors by harboring protective symbionts like M. sculptus. It is possible that diffuse coevolution has occurred between these two groups; however, this seems unlikely because both herbivore and host appear to respond most strongly to selective pressures from predators and competitors outside this association.     

ANALYSIS OF ANCIENT DNA FROM FOSSIL CORALLINES (CORALLINALES,RHODOPHYTA)1

The field of molecular paleontology has recently made significant contributions to anthropology and biology. Hundreds of ancient DNA studies have been published, but none has targeted fossil coralline algae. Using regions of the SSU gene, we analyzed rDNA from fossil coralline algae of varying ages and states of preservation from Spain, Papua New Guinea (PNG), and the Great Barrier Reef (GBR). Specimens from PNG, GBR, and some localities from Spain did not contain endogenous ancient DNA. Reproducible sequence data were obtained from specimens ～550 years old from near Cadiz, Spain, and from rocky‐shore deposits in Carboneras, Almeria Province of Spain (～78,000 years before present [YBP]). Based on BLAST searches and a phylogenetic analysis of sequences, an undescribed coralline alga belonging to the Melobesioideae was discovered in the Carboneras material as well as the following coralline genera: Jania, Lithophyllum, Lithothamnion, Mesophyllum, and Phymatolithon. DNA from fleshy brown and red macroalgae was also discovered in the specimens from Carboneras. The coralline algae identified using molecular techniques were in agreement with those based on morphological methods. The identified taxa are common in the present‐day southeastern Spain littoral zone. Amino acid racemization, concentration ratios, and specific concentrations failed to show a correlation between biomolecular preservation and PCR amplification success. Results suggest that molecular investigations on fossil algae, although limited by technical difficulties, are feasible. Validity of our results was established using authentication criteria and a self‐critical approach to compliance.     

THE BIOLOGY OF HARVEYELLA MIRABILIS (CRYPTONEMIALES,RHODOPHYCEAE). VI. TRANSLOCATION OF PHOTOASSIMILATED 14C122

Pulse-chase labelling experiments demonstrate that photoassimilated ¹⁴C-bicarbonate is translocated from the host red alga Odonthalia floccosa (Esper) Falkenberg to the parasite Harveyella mirabilis (Reinsch) Schmitz & Reinke. The primary path of translocation is from host cortical cells (the site of photoassimilation) to the erumpent parasite pustule via the zone of interdigitation. The latter is a tissue region in which rhizoidal cells of Harveyella grow between, and establish secondary pit plugs with medullary cells of Odonthalia. A secondary translocation pathway occurs from isolated host cells dispersed in the pustule of Harveyella to adjacent parasite cells.     

Skeletal ultrastructure of the calcified red alga Galaxaura oblongata,Hainan Island,China

Aragonite calcification in the red alga Galaxaura oblongata (Ellis et Solander) Lamouroux (Chaetangiaceae, Nemaliales) from southern China, occurs at three sites in the cortex: (1) intercellular spaces (ICS); (2) the cell wall; and (3) the inner surface of the cortex. The ICS is the principal site of calcification and contains aragonite mainly in the form of equidimensional granules ∼1–2 μm in size, although needle-like crystals up to 3 μm in length are also present locally. Granules range from densely to loosely packed. A dense and even layer peripheral to the ICS is interpreted to represent calcification of the cell wall. Coarser radial clumps of elongate crystals, forming a thin discontinuous layer on the inner surface of the cortex, resemble a cement fringe facing into the medulla, but form during the life of the alga. Calcification in these specimens shows similarities, and differences, to both coralline red algae, in which calcification is limited to the cell wall, and halimedacean green algae in which it is limited to the ICS. Some members of the Palaeozoic family Moniliporellaceae show similarities in their skeletal organization to Galaxaura.     

Consistency in a marine algal‐grazer interaction over multiple scales

Coralline algae are conspicuous members of many marine assemblages, especially those characterized by intense grazing pressure. We explored whether articulated species, especially Corallina vancouveriensis, depend on grazing invertebrates to both establish and flourish in an exposed rocky intertidal setting, and whether this plant–grazer relationship varied over more than three orders of magnitude (≈100–>300,000 μm). Three experimental manipulations, supplemented by observations on recruitment, demonstrated that (i) C. vancouveriensis failed to recover rapidly from disturbed areas when grazers were experimentally excluded; (ii) recruitment occurred in the presence of grazers; (iii) increasing surface texture of molded surfaces enhanced coralline recruitment more when grazers were present; and (iv) settlement occurred predominately in microtopographical low areas of a molded surface, whereas a competitively superior fleshy red alga tended to recruit to high areas. These results confirm that coralline algal establishment and persistence are enhanced by grazers and reveal that this relationship is consistent over a range of biologically relevant scales.     

FORMATION OF CALLOSE AND LIGNIN DURING LEAF ABSCISSION

Deblading of bean leaves promoted the formation of callose and lignin in the abscission zone. The abscission layer became evident three days after deblading. The greatest increase in callose occurred in about two layers of cells during the development of the abscission layer. Four days after deblading, only a few layers of cells on the distal side of the abscission layer showed an increase in lignin. Lignification continued to expand to 8–10 layers of cells at the time of separation. After separation, the lignified cells remained with the petiole. Sieve elements in the abscission zone were covered with callose plugs and the vessels were occluded with tyloses.