Evaluating the role of morphological characters in the phylogeny of some trypanosomatid genera (Excavata,Kinetoplastea, Trypanosomatida)

Over the last three decades, it has been progressively assumed that morphology has become obsolete for trypanosomatid systematics. Traditional taxonomy, based on the occurrence of specific kinds of cell morphotypes during life cycles and the morphometry of such cells, is often rejected by molecular phylogenies inferred mostly from 18S rDNA alone or combined with GAPDH. In such context, we hypothesized the affinities of 35 representatives of seven trypanosomatid genera from separated and combined cladistics analyses of morphological and 18S matrices. Morphology is shown to be more consistent and to have stronger synapomorphy retention than the 18S data. The strict consensus of cladograms from separated analyses was mostly unresolved, while combined analysis produced a meaningful and robust phylogenetic pattern, as evidenced by partition congruence index, Bremer support and frequencies of groups present/contradicted. The results (1) corroborate the separation of Angomonas and Strigomonas from Crithidia, which is now shown to be monophyletic, (2) support the revalidation of the genus Wallaceina, and (3) place the genera Herpetomonas, Leptomonas and Phytomonas within a single clade. Overall, we demonstrate the belief that morphological characters are inferior to molecular ones for trypanosomatid systematics is a consequence of neglecting their inclusion in phylogenetic analyses.     

Cyanobacterial formation of intracellular Ca‐carbonates in undersaturated solutions

Cyanobacteria have long been thought to induce the formation of Ca‐carbonates as secondary by‐products of their metabolic activity, by shifting the chemical composition of their extracellular environment to conditions favoring mineral precipitation. Some cyanobacterial species forming Ca‐carbonates intracellularly were recently discovered. However, the environmental conditions under which this intracellular biomineralization process can occur and the impact of cyanobacterial species forming Ca‐carbonates intracellularly on extracellular carbonatogenesis are not known. Here, we show that these cyanobacteria can form Ca‐carbonates intracellularly while growing in extracellular solutions undersaturated with respect to all Ca‐carbonate phases, that is, conditions thermodynamically unfavorable to mineral precipitation. This shows that intracellular Ca‐carbonate biomineralization is an active process; that is, it costs energy provided by the cells. The cost of energy may be due to the active accumulation of Ca intracellularly. Moreover, unlike cyanobacterial strains that have been usually considered before by studies on Ca‐carbonate biomineralization, cyanobacteria forming intracellular carbonates may slow down or hamper extracellular carbonatogenesis, by decreasing the saturation index of their extracellular solution following the buffering of the concentration of extracellular calcium to low levels.     

<Emphasis Type="Italic">Halomonas tibetensis</Emphasis> sp. nov., isolated from saline lakes on Tibetan Plateau

Strains pyc13^T and ZGT13 were isolated from Lake Pengyan and Lake Zigetang on Tibetan Plateau, respectively. Both strains were Gram-negative, catalase- and oxidase-positive, aerobic, rod-shaped, nonmotile, and nonflagellated bacteria. Phylogenetic analysis based on 16S rRNA gene sequences showed that strains pyc13^T and ZGT13 belong to the genus Halomonas, with Halomonas alkalicola 56-L4-10aEn^T as their closest neighbor, showing 97.4% 16S rRNA gene sequence similarity. The predominant respiratory quinone of both strains was Q-9, with Q-8 as a minor component. The major fatty acids of both strains were C_18:1ω6c/C_18:1ω7c, C_16:1ω6c/C_16:1ω7c, C_16:0, and C_12:0 3OH. The polar lipids of both strains consisted of phosphatidylethanolamine, phosphatidylglycerol, diphosphatidylglycerol, glycolipid, phospholipids of unknown structure containing glucosamine, and unidentified phospholipids. The DNA G + C content of pyc13^T and ZGT13 were 62.6 and 63.4 mol%, respectively. The DNA-DNA hybridization values of strain pyc13^T were 34, 41, 61, 35, and 35% with the reference strains H. alkalicola 56-L4-10aEn^T, H. sediminicola CPS11^T, H. mongoliensis Z-7009^T, H. ventosae Al12^T, and H. fontilapidosi 5CR^T, respectively. Phenotypic, biochemical, genotypic, and DNA-DNA hybridization data showed that strains pyc13^T and ZGT13 represent a new species within the genus Halomonas, for which the name H. tibetensis sp. nov. is proposed. The type strain is pyc13^T (= CGMCC 1.15949^T = KCTC 52660^T).     

Strong effects of hydrologic environment and weak effects of elevated CO<Subscript>2</Subscript> on the invasive weed <Emphasis Type="Italic">Alternanthera philoxeroides</Emphasis> and the biocontrol beetle <Emphasis Type="Italic">Agasicles hygrophila</Emphasis>

Global change, such as elevated CO₂, may alter interactions between invasive plants and biocontrol agents, impacting biocontrol efficacy. Here, we conducted four experiments in Texas, USA to test how elevated CO₂ influences an invasive plant (Alternanthera philoxeroides) and its interactions with an introduced biocontrol beetle (Agasicles hygrophila) in terrestrial (well-watered) and flooded environments. We grew plants for 9 months in ambient or elevated CO₂ (800 ppm) chambers in continuously flooded or well-watered conditions. In no-choice trials, flooding increased leaf toughness and decreased beetle consumption but beetles only oviposited on ambient CO₂ leaves. In choice trials, beetles preferred to feed and oviposit on terrestrial plants but were also less likely to damage elevated CO₂ leaves. Caged beetle populations were larger in terrestrial conditions than aquatic conditions for a second set of plants grown in the chambers. With a third set of plants grown in the ambient or elevated CO₂ chambers, damage for plants placed in the field (aquatic setting) was higher for plants grown in terrestrial conditions vs. flooded conditions at ambient CO₂. Our results suggest that elevated CO₂ will have minor effects on the efficacy of this biocontrol agent by decreasing oviposition and number of leaves damaged, and hydrologic environment may affect invasive plant performance by altering herbivore oviposition and feeding preferences. A broader understanding of the effects of global change on biocontrol will help prevent and manage future spread of invasive plants.