Variability and seasonality of the growth of some corticolous pleurocarpous mosses

Abstract

Field measurements of the elongation of shoots of Hypnum cupressiforme and lsothecium myosuroides reveal considerable variation. Differences in growth rates in the following situations were found to be significant: at different heights on a trunk, on different sides of sloping trunks, on different species of tree and, over a period, on different trees of a single species at a site.

Monthly growth measurements of H. cupressiforme and Platygyrium repens in Wytham Wood, Berkshire, show that H. cupressiforme grows faster, but that the growth patterns of these species are similar. Most of the annual growth for 1970 and 1971 took place during the autumn and winter. Growth between April and August was very slight. The seasonality of the growth of four pleurocarpous mosses at Wychwood, Oxfordshire, was very similar to the species measured at Wytham. Comparison of seasonal growth records with climatic records for stations near Oxford shows a close correlation Qetween growth and wetness. Monthly rainfall minus potential evapotranspiration (Rf–Et) is particularly closely related to monthly shoot growth.

At Roborough, North Devon, growth of H. cupressiforme was measured every 3 months. Considerable growth occurred during autumn and winter. At this site the summers are wetter and this appears to permit an extension of the growing period, considerable growth occurring between May and October.

In 1970 and 1971 summer growth at several localities was compared. Summer growth was again closely related to Rf–Et. The summer growth in wetregions does not seem to be accompanied by a proportionally high winter growth rate. The wetter the climate, the earlier in the year the peak period of bryophyte growth occurs and the more closely the annual pattern of growth correlates with temperature and day length.     

Cation contents of acrocarpous and pleurocarpous mosses growing on a strontium-rich substratum

Abstract

A new species, Nanobryum thorsbornei, is described from northern Queensland, Australia, and compared with N. dummeri, an African species to which it seems most closely allied. They both have a remarkable persistent protonema which is partly pseudothallose but the leaves of the Australian species are trilobate, a feature lacking in the African species. The relationship of Nanabryum with Fissidens, particularly F. gladiolus, is discussed.     

Testing morphological concepts of orders of pleurocarpous mosses (Bryophyta) using phylogenetic reconstructions based on TRNL-TRNF and RPS4 sequences

The ordinal classification of pleurocarpous mosses rests on characters such as branching mode and architecture of the peristome teeth that line the mouth of the capsule. The Leucodontales comprise mainly epiphytic taxa, characterized by sympodial branching and reduced peristomes, whereas the Hypnales are primarily terricolous and monopodially branching. The third order, the Hookeriales, is defined by a unique architecture of the endostome. We sampled 78 exemplar taxa representing most families of these orders and sequenced two chloroplast loci, the trnL-trnF region and the rps4 gene, to test the monophyly and relationships of these orders of pleurocarpous mosses. Estimates of levels of saturation suggest that the trnL-trnF spacer and the third codon position of the rps4 gene have reached saturation, in at least the transitions. Analyses of the combined data set were performed under three optimality criteria with different sets of assumptions, such as excluding hypervariable positions, downweighting the most likely transformations, and indirect weighting of rps4 codon positions by including amino acid translations. Multiple parallelism in nonsynonymous mutations led to little or no improvement in various indices upon inclusion of amino acid sequences. Trees obtained under likelihood were significantly better under likelihood than the trees derived from the same matrix under parsimony. Our phylogenetic analyses suggest that (1) the pleurocarpous mosses, with the exception of the Cyrtopodaceae, form a monophyletic group which is here given formal recognition as the Hypnidae; (2) the Leucodontales are at least paraphyletic; and (3) the Hypnales form, with most members of the Leucodontalean grade, a monophyletic group sister to a Hookerialean lineage. The Hypopterygiaceae, Hookeriales, and a clade composed of Neorutenbergia, Pseudocryphaea, and Trachyloma likely represent a basal clade or grade within the Hypnidae. These results suggest that mode of branching and reduced peristomes are homoplastic at the ordinal level in pleurocarpous mosses.     

A transporter regulating silicon distribution in rice shoots

Rice (Oryza sativa) accumulates very high concentrations of silicon (Si) in the shoots, and the deposition of Si as amorphous silica helps plants to overcome biotic and abiotic stresses. Here, we describe a transporter, Lsi6, which is involved in the distribution of Si in the shoots. Lsi6 belongs to the nodulin-26 intrinsic protein III subgroup of aquaporins and is permeable to silicic acid. Lsi6 is expressed in the leaf sheath and leaf blades as well as in the root tips. Cellular localization studies revealed that Lsi6 is found in the xylem parenchyma cells of the leaf sheath and leaf blades. Moreover, Lsi6 showed polar localization at the side facing toward the vessel. Knockdown of Lsi6 did not affect the uptake of Si by the roots but resulted in disordered deposition of silica in the shoots and increased excretion of Si in the guttation fluid. These results indicate that Lsi6 is a transporter responsible for the transport of Si out of the xylem and subsequently affects the distribution of Si in the leaf.     

Observations on the distribution of meroplankton during an upwelling event

The distribution of the larvae of benthic invertebrates wasinvestigated relative to hydrographic structures as a test ofthe hypothesis that larvae behave as if they are passive particles.Observations of larval and oceanographic distributions weremade off Duck, North Carolina, USA in August 1994. Conditionswere characterized by wind-driven coastal upwelling; flow wasgenerally offshore near the surface and onshore below the pycnocline.Within 5 km of the shore the pycnocline was bent upward by theupwelling and it intersected the surface along most of the transects.In zooplankton samples, 20 taxa of larvae were counted (10 bivalveveligers, nine gastropod veligers and one polychaete larvae).Using cluster analysis, larvae were separated into groups withsimilar patterns of distribution and similar affinities to waterproperties. The larvae in Cluster 3 did not display a consistentdistribution pattern beyond that they tended to be found inwarmer surface waters. An earlier paper described the distributionof larvae in the same location during a downwelling event [A.Shanks et al. (2002) J. Plankton Res., 24, 391–416]. Twoof the clusters identified during this previous study were quitesimilar in composition to Clusters 1 and 2 in this study. Inboth studies, Cluster 1 larvae were found below the pycnocline,but during the upwelling event they were transported shorewardwith the advection of the subpycnocline waters by the upwellingcirculation. Within 5 km of the shore, Cluster 1 larvae werefound at depths shallower than the base of the pycnocline andwere often found in patches of high larval concentration. Thepatches were located where the waters were upwelling. Cluster2 larvae were found within 5 km of the shore in both studiesand tended to be highly concentrated in convergences or divergences.Larvae in Cluster 1 generally appeared to be dispersing as passiveparticles, except within the zone of upwelling where they mayhave been swimming against the upwelling flow leading to higherlarval concentrations. Cluster 2 larvae appeared to be consistentlyconcentrated in areas of vertical currents, suggesting thatthey may be attempting to maintain a preferred depth in theface of the vertical flow which would lead to high larval concentrationand nearshore larval distributions despite extensive cross-shelfmovement of water. Despite their slow swimming speeds, the larvaein Clusters 1 and 2 were not swept offshore by the upwellingevent.     

Observations on the distribution of the Gm- and Inv-groups in Hungary

Summary The authors report the distribution of Gm- and Inv-groups in Hungary. In our total material of 378 males and females of different age, the frequency of the following Gm-phenotypes turned out: Gm (1, 2, 4, 5, 10)=4.1%, Gm(1,-2, 4, 5, 10)=25.3%, Gm(1,-2,-4,-5,-10)=3.4%, Gm(1, 2,-4,-5,-10)=0.4%, and Gm(-1,-2, 4, 5, 10)=66.8%. The alleles frequencies have been calculated to be Gm¹=0.1622, Gm^{1, 2}=0.0228, Gm^{4, 5, 10}=0.8150. Observed and expected Gm-phenotypes frequencies are in good agreement under the assumption of the 3-alleles-model Gm¹, Gm^{1, 2}, Gm^{4, 5, 10}. The Invphenotypes frequencies came out to be: Inv(1,-2)=0.5$, Inv(1,2)=8.2%, and Inv(-1,-2)=91.3%.Among our Hungarian samples no significant differences were found, neither in the distribution of Gm-nor Inv-phenotypes and alleles. There exist no significant differences in the distribution of Inv-groups between our Hungarian sample and two German samples, but the Hungarian sample differs clearly from Czechoslovakian and Yugoslavian ones in the distribution of the Gm-phenotypes.Supported by a grant from the Caisse Nationale de Sécurité Sociale.Attaché de Recherche á l'I.N.S.E.R.M.     

A comparison of distribution patterns in British and Irish mosses and liverworts

Abstract

We classified 747 species of British and Irish mosses into 10 clusters, based on their recorded distribution in 10×10 km grid squares (hectads). We generated the clusters in a two-stage process using the CLUSTASPEC program, the method that we had earlier used for British and Irish liverworts and hornworts. The clusters are named after the species with distributions which are most similar to those of the clusters as a whole. Clusters of widespread species (Bryum capillare), southern, lowland species (Rhynchostegium confertum), widespread calcifuges (Pleurozium schreberi), upland species (Blindia acuta), and montane calcifuges (Kiaeria falcata) closely match clusters recognised in the liverworts. The remaining clusters (Tortella flavovirens, Weissia longifolia, Mnium stellare, Encalypta alpina, Mnium lycopodioides) are less similar. The classification of mosses into 15 and 20 clusters generates additional clusters of hyperoceanic and montane mosses which also resemble liverwort clusters. The influence of calcareous bedrock has a more marked effect in determining moss distributions and, unlike the liverworts, the 10 moss clusters include one which is predominantly coastal. Mosses tend to be a less upland group than liverworts; a smaller proportion of their species have northern and western distributions and the lowland clusters are characterised by more extreme environmental conditions. As with the liverworts, geographically restricted clusters of species with predominantly Mediterranean-Atlantic, Arctic-montane and Boreo-arctic Montane world ranges include marked concentrations of threatened species, and species which are not recorded as fruiting in the British Isles.     

Chromium distribution in shoots of macrophyte Callitriche cophocarpa Sendtn.

The aim of the study was the analysis of Cr distribution in shoots of the macrophyte Callitriche cophocarpa by means of two X-ray-based techniques: micro X-ray fluorescence (μXRF) and electron probe X-ray microanalysis (EPXMA). Plants were treated with 100 μM (5.2 mg l^?1) chromium solutions for 7 days. Cr was introduced independently at two speciations as Cr(III) and Cr(VI), known for their diverse physicochemical properties and different influence on living organisms. A comparative analysis of Cr(III)-treated plants by EPXMA and μXRF demonstrated high deposition of Cr in epidermal glands/hairs localized on leaves and stems of the plant shoots. Cr in Cr(III)-treated plants was recorded solely in glands/hairs, and the element was not present in any other structures. On the other hand, Cr in Cr(VI)-treated group of plants was rather found in vascular bundles. Moreover, the concentration of Cr in Cr(VI)-treated plants was significantly lower than in plants incubated in Cr(III) solution. The results obtained in this work suggest differences in chromium uptake, transport and accumulation dependent on the oxidative state of the element.     

Observations on the vertical distribution of the benthos in a Malaysian stream

An apparatus is described wbich is capable of sampling tbe bentbic fauna to a depth of 50 cm by providing a natural substrate for colonization. Tbe results obtained from an area of visually uniform sediments demonstrate that stream animals occur in significant numbers deep in tbe bottom sediments and that, at most, only about half tbe bentbos lives in tbe upper 10 cm usually ‘quantitatively’ sampled in stream surveys. The significance of a deep-living fauna in regulating community density, in recolonizing denuded areas and in optimizing utilization of available food resources is discussed.     

Observations on the structure of kefir grains and the distribution of the microflora

The mixed flora of yeasts and lactobacilli of kefir is held together in non-dispersible structures which build up into large grains. The fibrillar extracellular material of the matrix in which the microflora is embedded was stained by ruthenium red and periodic acid-thiosemicarbazide silver proteinate, indicating that it was largely composed of carbohydrate. It is suggested that the carbohydrate is of bacterial origin and that this is produced by a population of lactobacilli which resides within the matrix and which separates non-carbohydrate-producing populations of lactobacilli and yeasts so that sheet-like structures are formed which show asymmetry, with yeasts predominating on one side and lactobacilli on the other.     

Notes on the mosses of Rhodes and Kos

Abstract

The habitat of glaciokarst plains in the Dolomites corresponds to ancient cirques carved by glaciers during the Pleistocene era and now determined by karstic processes. It has a rich bryological flora (eighty-seven species). Some of them proved to be statistically significant for indicating vegetation types. The latter are clearly correlated with different types of karstic landforms, each of which corresponding to a well-defined microenvironment.     

The distribution of phytophagous and predacious mites on leaves and shoots of apple trees

Zusammenfassung Es wurde gezeigt, dass die Verteilung der RaubmilbeTyphlodromus pyri scheuten und der phytophagen MilbeMetatetranychus ulmi Koch auf den Bl?ttern von Apfelb?umen sehr ?hnlich ist. Eine Korrelation zwischen beiden Komponenten konnte aber nicht festgestellt werden. Beobachtungen zu drei verschiedenen Zeitpunkten w?hrend des Sommers zeigten, dass die Raubmilben keine Vorliebe für bestimmte Bl?tter haben. Die Obstbaumspinnmilbe zeigt aber im Frühjahr eine deutliche Vorliebe für die basalen Bl?tter.      

Observations on the ultrastructure and distribution of chromatophores in the skin of chelonians

Alibardi, L. 2011. Observations on the ultrastructure and distribution of chromatophores in the skin of chelonians. —Acta Zoologica (Stockholm) 00 :1–11. The cytology and distribution of chromatophores responsible for skin pigmentation in chelonians is analyzed. Epidermal melanocytes are involved in the formation of dark spots or stripes in growing shelled and non‐shelled skin. Melanocytes rest in the basal layer of the epidermis and transfer melanosomes into keratinocytes during epidermal growth. Dermal melanophores and other chromatophores instead remain in the dermis and form the gray background of the skin. When dermal melanophores condense, they give origin to the dense spots or stripes in areas where no epidermal melanocytes are present. In the latter case, the epidermis and the corneous layer are transparent and reveal the dermal distribution of melanophores and other chromatophores underneath. As a result of this basic process of distribution of pigment cells, the dark areas visible in scales can have a double origin (epidermal and dermal) or a single origin (epidermal or dermal). Xanthophores, lipophores, and a cell containing both pterinosomes and lipid droplets are sparse in the loose dermis while iridophores are rarely seen in the skin of chelonians analyzed in the present study. Xanthophores and lipophores contribute to form the pale, yellow or oranges hues present among the dark areas of the skin in turtles.     

Shuttle-like movements of Golgi vesicles in the tip of growingChara rhizoids

Summary In tip-growingChara rhizoids, the in-vivo saltatory movements of Golgi vesicles were recorded. The movements in radial direction back and forth between the ER aggregate and the plasma membrane occurred three times more often than movements passing the ER aggregate tangentially. The mean velocity of the class of Golgi vesicles observed (0.4–1 m in diameter) was approx. 0.3 m/s. Higher speed of 1–1.5 m/s occurred only in radial directions. Possibly, the ER aggregate is involved in guidance of the Golgi vesicles.Abbreviations DIC differential interference contrast - ER endoplasmic reticulum - OsFeCN osmium tetroxide-potassium ferricyanide Dedicated to the memory of Professor O. Kiermayer     

The evolution of root hairs and rhizoids

Background

Almost all land plants develop tip-growing filamentous cells at the interface between the plant and substrate (the soil). Root hairs form on the surface of roots of sporophytes (the multicellular diploid phase of the life cycle) in vascular plants. Rhizoids develop on the free-living gametophytes of vascular and non-vascular plants and on both gametophytes and sporophytes of the extinct rhyniophytes. Extant lycophytes (clubmosses and quillworts) and monilophytes (ferns and horsetails) develop both free-living gametophytes and free-living sporophytes. These gametophytes and sporophytes grow in close contact with the soil and develop rhizoids and root hairs, respectively.

Scope

Here we review the development and function of rhizoids and root hairs in extant groups of land plants. Root hairs are important for the uptake of nutrients with limited mobility in the soil such as phosphate. Rhizoids have a variety of functions including water transport and adhesion to surfaces in some mosses and liverworts.

Conclusions

A similar gene regulatory network controls the development of rhizoids in moss gametophytes and root hairs on the roots of vascular plant sporophytes. It is likely that this gene regulatory network first operated in the gametophyte of the earliest land plants. We propose that later it functioned in sporophytes as the diploid phase evolved a free-living habit and developed an interface with the soil. This transference of gene function from gametophyte to sporophyte could provide a mechanism that, at least in part, explains the increase in morphological diversity of sporophytes that occurred during the radiation of land plants in the Devonian Period.