Seagrass Transplanting in Cockburn Sound, Western Australia: A Comparison of Manual Transplantation Methodology Using Posidonia sinuosa Cambridge et Kuo

Seagrass transplants (plant units [PUs]) were established to examine the feasibility of seagrass rehabilitation in Cockburn Sound, Western Australia. Five hundred and twenty plant units (plugs and sprigs) of Posidonia sinuosa Cambridge et Kuo were placed at seven locations at depths of 3, 5, and 9 m and monitored to determine the influence of transplant method, location, and depth upon survival and growth over 2 years. Depending on the site, more plugs had survived at the completion of the trial (mean survival 41%) than sprigs (mean survival 15%). Plug and sprig survival differed significantly with transplant depth, decreasing overall with increasing depth. Forty‐five percent of surviving plugs and 50% of sprigs exhibited horizontal rhizome extension. Mean rhizome extension after 2 years was 9.5 cm/plug (1–23 cm) and 18.3 cm/sprig (0.5–31 cm). Declines in PU survival and variable growth correlate with site‐specific variability in light climate. Plug transplantation was deemed the most suitable method for further manual seagrass rehabilitation, exhibiting higher survival across all sites and conditions; however, they are costly to deploy. Sprig PUs have greatest potential in shallow water with fine sands, moderate water movement, and maximum light availability. The low cost of deploying sprigs may outweigh their lower survival compared to plugs; further efforts should be directed to enhancing survival of sprig PUs under a wider range of conditions. Suitable locations for future rehabilitation efforts in Cockburn Sound were the Eastern and Western Banks and shallow areas off Woodman Point and Mangles Bay.     

SEM studies on vessels in ferns. 17. Psilotaceae

Perforation plates are reported in aerial and subaerial axes of Psilotum nudum and in aerial axes of Tmesipteris obliqua. In Psilotum, both perforations lacking pit membranes and perforations with pit membrane remnants were observed. Perforation plates in Psilotum may consist wholly of one type or the other. In Tmespteris, perforations have threadlike pit membranes or consist of porose pit membranes. Wide perforations alternating with narrow pits, a conformation observed in various ferns, were observed in Psilotum (subaerial axes). In Psilotum, perforations are more common in metaxylem than in protoxylem; perforations in protoxylem consist of primary wall areas containing small circular porosities or relatively large circular to oval perforations. There are no modifications in the secondary wall framework of protoxylem or metaxylem in Psilotum or Tmesipteris that would permit one to distinguish presence of perforations or perforation plates with light microscopy, and scanning electron microscopy (SEM) is required for demonstration of porose walls or perforations. The tracheary elements of the Psilotaceae studied have no features not also observed in other ferns with SEM.     

The tegumental surface of Phyllodistomum conostomum (Olsson, 1876) (Digenea), revealed by scanning electron microscopy

The external surface of P. conostomum is characterized by relatively large ridges encircling the anterior part of the worm at regular intervals. On the posterior part depressions on the ventral side at regular intervals and relatively small ridges on the dorsal side are present. Ventroposteriorally cobblestone-like protuberances observed are arranged in longitudinal rows. No corresponding arrangement was found dorsally. Only domed papillae (with and without a central knob) were observed, tentatively identified as sensory organs. The regular pattern of these papillae on the ventral and oral sucker is described, in addition to their arrangement ventrally and at the anterior end. A frontal pit anterior of oral suckers and a notch at the posterior end are figured and briefly described. No spines were observed on the body tegument.     

Microbially mediated aluminosilicate formation in acidic anaerobic environments: A cell‐scale chemical perspective

Through the use of scanning transmission electron microscopy (STEM) combined with other complementary techniques (SEM, cryo‐TEM, HRTEM, and EELS), we have studied the interaction of microorganisms inhabiting deep anoxic waters of acidic pit lakes with dissolved aluminum, silica, sulfate, and ferrous iron. These elements were close to saturation (Al, SiO₂) or present at very high concentrations (0.12 m Fe(II), 0.12–0.22 m SO₄^2?) in the studied systems. The anaerobic conditions of these environments allowed investigation of geomicrobial interactions that are difficult to see in oxidized, Fe(III)‐rich environments. Detailed chemical maps and through‐cell line scans suggest both extra‐ and intracellular accumulation of Al, Si, S, and Fe(II) in rod‐like cells and other structures (e.g., spherical particles and bacteriomorphs) of probable microbial origin. The bacterial rods showed external nanometric coatings of adsorbed Fe(II) and Al on the cell surface and cell interiors with significant presence of Al, Si, and S. These microbial cells coexist with spherical particles showing similar configuration (Fe(II) external coatings and [Al, Si, S]‐rich cores). The Al:Si and Al:S ratios and the good Al–Si correlation in the cell interiors suggest the concurrent formation of two amorphous phases, namely a proto‐aluminosilicate with imogolite‐like composition and proto‐hydrobasaluminite. In both cases, the mineralization appears to comprise two stages: a first stage of aluminosilicate and Al‐hydroxysulfate precipitation within the cell or around cellular exudates, and a second stage of SO₄^2? and Fe(II) adsorption on surface sites existing on the mineral phases in the case of (SO₄^2?) or on presumed organic molecules [in the case of Fe(II)]. These microbially related solids could have been formed by permineralization and mineral replacement of senescent microbial cells. However, these features could also denote biomineralization by active bacterial cells as a detoxification mechanism, a possibility which should be further explored. We discuss the significance of the observed Al/microbe and Si/microbe interactions and the implications for clay mineral formation at low pH.     

浓香型白酒窖泥放线菌的群落结构及其多样性

以泸州老窖1、50、100和400年窖泥为研究对象,采用变性梯度凝胶电泳(DGGE)研究浓香型白酒窖泥放线菌的群落结构及其多样性。DGGE图谱显示,除1年样品外,其余窖底泥多样性指数(H)均低于同窖龄窖壁泥,但均匀度指数(EH)较高。不同窖池相同部位窖泥的群落结构变化趋势为:随窖龄的延长,窖壁泥H值逐渐上升,为1.74—2.28;窖底泥下降,为1.73—2.07。EH值均为波动下降,分别在0.986—0.991和0.971—0.994之间。窖底泥相似性系数(SC)逐渐上升,为0.46—0.82;窖壁泥为0.31—0.62。DGGE条带测序结果显示,窖泥放线菌归于Olsenella、Atopobium、Streptomyces和Corynebacterium 4个属。Olsenella和Atopobium属为共有的优势属,且在窖壁泥中的优势度(di)均随窖龄延长而降低,在窖底泥中升高。实验结果表明,浓香型白酒窖泥蕴藏着丰富的放线菌资源,群落结构和多样性存在差异,菌群演替呈现一定规律性。     

泸型酒酒醅与窖泥中梭菌群落结构、演替和功能差异

梭菌对泸型酒风味品质的发酵形成具有重要作用,但目前对酒醅和窖泥中梭菌群落的物种组成、发酵演替规律以及代谢功能的差异尚缺少深入认识。采用分子微生态学技术,在种水平上对比了同一窖池的酒醅和窖泥中梭菌纲细菌群落的结构差异和演替规律,并通过纯培养方法分离和评价了梭菌菌株的主要挥发性脂肪酸组成差异。结果表明,窖泥发酵过程中梭菌纲细菌和总细菌的基因拷贝数比值相对稳定(71.5%–91.2%),而酒醅中梭菌的变化则较大(0.9%–36.5%)。酒醅中优势梭菌纲细菌主要是梭菌属(Clostridium,19.9%)、沉积物菌属(Sedimentibacter,8.8%)和氢孢菌属(Hydrogenispora,7.2%),而窖泥中主要为氢孢菌属(57.2%)、沉积物菌属(5.4%)和产己酸菌属(Caproiciproducens,4.9%)。窖泥及酒醅发酵过程中梭菌群落结构差异显著(P=0.001)。分离获得的20株梭菌菌株具有不同的产挥发性脂肪酸能力。结果表明,窖池中梭菌纲细菌群落存在时空异质性,其结构和功能差异对泸型酒风味形成具有影响。     

浓香型白酒窖泥中可培养细菌的分离鉴定及产酸研究

为系统了解浓香型白酒窖泥中可培养细菌的多样性,采用平板稀释涂布法分离筛选窖泥中可培养菌株。扩增纯培养细菌的16SrRNA基因,测序并与EzBioCloud数据库比对,所有序列已在GenBank中注册。结果共从窖泥中筛选出42株差异性较大的菌株,其中5株与模式菌株相似性低于97％,共包括14个属,以Bacillus、Lysinibacillus、Sporosarcina、Staphylococcus四个属为主;高效液相色谱检测各个菌发酵液结果表明,有机酸包括乙酸、乳酸、酒石酸、苹果酸、柠檬酸、琥珀酸、α-酮戊二酸、草酸;其中尤以乙酸、乳酸的产量较高。     

Estrogen directly down-regulates the bone-resorbing activity of mature osteoclasts through nuclear estrogen receptor α

The decrease in estrogen level that follows the onset ofmenopause causes rapid bone loss, resulting in osteoporosis.However, the mechanism remains unclear, especially concerningthe regulation of bone-resorbing osteoclasts. Here we analyzedthe function of estrogen and its receptor in matureosteoclasts. We found that estrogen directly inhibitedbone-resorption by purified rabbit mature-osteoclasts.Moreover, using a RT-PCR technique, we report that nuclearestrogen receptor (ER) but not ER is expressed in mature osteoclasts. The antisense oligodeoxynucleotide for ER inhibited the reductionin osteoclastic bone-resorbing activity caused by estrogen. We conclude that in part estrogen directly inhibits the bone-resorbing activity of mature osteoclasts through the ER.