Entire Margin Research Articles

<p><strong><em>Pedicularis khoiyangii</em></strong><strong> (Orobanchaceae), a new species from the Eastern Himalaya, India</strong></p>

Pedicularis khoiyangii D.Borah & R.Kr.Singh, is described as a new species from the Eastern Himalaya, India. The new species belongs to Pedicularis series Rudes Prain and is closely related to P. prainiana Maximowicz, but differs by its larger size, longer inflorescence, distal bracts ovate, shorter pedicels, smaller calyx, densely silky villous nature, calyx teeth shorter with entire margins, equal, smaller corolla tube, shortly beaked galea, tip slightly emarginate, labium as long as galea, lobes unequal, stamens inserted at the base of corolla tube, style projecting out of the galea. This is the tallest species of Pedicularis recorded so far from India.

Ferrovibrio terrae sp. nov., isolated from soil.

Designated strain K5T was isolated from soil on Jeju Island. The bacterium was aerobic, Gram-stain-negative, oxidase-positive, catalase-low activity, motile, short-rod shaped, opaque and formed white colonies that were circular, raised and had entire margins. Strain K5T was able to grow at 15-40 °C, pH 4-9 and at 0-2 % (w/v) NaCl concentration. Phylogenetic analysis based on its 16S rRNA gene sequences indicated that strain K5T is closely related to Ferrovibrio soli A15T (98.9 % sequence similarity), Ferrovibrio denitrificans Sp-1T (98.7 %) and Ferrovibrio xuzhouensis LM-6T (97.4 %). The sole respiratory quinone was determined to be ubiquinone-10. The dominant fatty acids of strain K5T were summed feature 8 (C18 : 1 ω7c / C18 : 1ω6c, 29.8 %), C19 : 0 cyclo ω8c (20.2 %) and C16 : 0 (24.4 %). DNA G+C content was 63.6 % and DNA-DNA relatedness between strain K5T and other three members of the genus Ferrovibrio ranged from 24 to 28 %. The major polar lipids were identified as phosphatidylglycerol, phosphatidylethanolamine and aminolipids. Moreover, polyphasic characterization revealed that strain K5T represents a novel species in the genus Ferrovibrio, for which the name Ferrovibrio terrae sp. nov. is proposed. The type strain is K5T (=KCCM 43295T=LMG 30611T).

Arterial revascularization following acute mesenteric ischemia.

Assessment of a pancreaticoduodenectomy specimen by pathologists requires specialized knowledge of anatomy. Standardized assessment, description and documentation of the retroperitoneal margin are crucial for the accurate interpretation of studies evaluating adjuvant therapy for pancreatic cancer patients.Twenty‐five patients who underwent a pancreaticoduodenectomy for pancreatic adenocarcinomas had their pathological specimens examined prospectively, using an anatomical‐based mapping approach. All margins, including the bile duct, pancreatic neck, superior mesenteric artery, superior mesenteric vein and posterior surface of the uncinate process, were microscopically examined in their entirety. The assessment of an R1 margin in terms of distance was assessed in two ways: first defining it as a tumour at the margin or secondary as tumour within 1 mm (1 mm rule).If the existing College of American Pathologists recommendations were applied (assessing only the bile duct, pancreatic neck and superior mesenteric artery margins), a R1 status would be achieved in only 9 of 25 patients. Extending the examination by assessment and reporting of the entire retroperitoneal resection margin, including the Superior Mesenteric Vein margin and the Posterior surface of the uncinate process margin, increased the number of patients with a R1 resection to 14 out of 25. Applying the 1‐mm rule further increased the number of patient with a R1 resection to 20 of 25 patients.The above findings illustrate that different approaches to the assessment and reporting of the retroperitoneal margin can change the results and adversely affect the final statistics used in pancreatic cancer studies and clinical trials.

First Report of Xanthomonas campestris Infecting Invasive Garlic Mustard in the United States

HomePlant DiseaseVol. 104, No. 4First Report of Xanthomonas campestris Infecting Invasive Garlic Mustard in the United States PreviousNext DISEASE NOTES OPENOpen Access licenseFirst Report of Xanthomonas campestris Infecting Invasive Garlic Mustard in the United StatesMatthew A. Tancos and Reid D. FrederickMatthew A. Tancos†Corresponding author: M. A. Tancos; E-mail Address: matthew.tancos@ars.usda.govhttp://orcid.org/0000-0002-6317-3393Foreign Disease-Weed Science Research Unit, United States Department of Agriculture-Agricultural Research Service, Frederick, MD 21702Search for more papers by this author and Reid D. Frederickhttp://orcid.org/0000-0002-1672-5327Foreign Disease-Weed Science Research Unit, United States Department of Agriculture-Agricultural Research Service, Frederick, MD 21702Search for more papers by this author AffiliationsAuthors and Affiliations Matthew A. Tancos † Reid D. Frederick Foreign Disease-Weed Science Research Unit, United States Department of Agriculture-Agricultural Research Service, Frederick, MD 21702 Published Online:12 Feb 2020https://doi.org/10.1094/PDIS-09-19-1963-PDNAboutSectionsSupplemental ToolsAdd to favoritesDownload CitationsTrack Citations ShareShare onFacebookTwitterLinked InRedditEmailWechat Garlic mustard (Alliaria petiolata) is an aggressive nonnative cruciferous (Brassica) plant from Eurasia that was introduced into North America around the 19th century (Durka et al. 2005). The biennial Brassica herb has since rapidly invaded and displaced native flora in much of the eastern and midwestern United States and Canada, thriving in woodlands, hedgerows, lawns, and other shady environments. In May of 2019, foliar leaf symptoms developed on garlic mustard along the edge of a forested property in Frederick County, Maryland. Initial leaf symptoms were chlorotic angular V-shaped lesions originating from the leaf margins, characteristic of a bacterial infection. As the disease progressed, leaves wilted and lesions became necrotic, covering entire leaf margins. The disease was patchy along the property and nearby forest edge, but the disease was observed on both second-year mature flowering plants and first-year immature rosettes. Disease incidence in the affected area was 75 to 80%. Symptomatic leaf tissue was surface sterilized, macerated, and streaked onto yeast extract dextrose calcium carbonate agar (Wilson et al. 1967), from which bright yellow, mucoid bacterial colonies were isolated. The 16S rRNA gene was sequenced to confirm the bacterium was a Xanthomonas sp. (accession MN823168), followed by sequencing eight conserved loci (atpD, dnaK, efP, glnA, gyrB, rpoD, tpiA, and fyuA) for multilocus sequence analysis and pathovar determination (accessions MN444860 to MN444867) (Fargier et al. 2011). Gene sequences were aligned, concatenated, and compared with reference Brassica-associated X. campestris strains, for a total length of 4,485 nucleotides, and used to generate a maximum likelihood phylogram using W-IQ-TREE (Fargier et al. 2011; Lange et al. 2016; Trifinopoulos et al. 2016). Sequence analysis revealed the garlic mustard isolate (strain FDWSRU 18048) did not cluster with the agronomically damaging X. campestris pv. campestris or pv. raphani strains but instead clustered with nonpathogenic X. campestris strains, the weakly pathogenic strain CFBP 5814, and strains of X. campestris pv. incanae with bootstrap support of 99% (Fargier et al. 2011; Lange et al. 2016). To fulfill Koch’s postulates, true leaves of a healthy transplanted garlic mustard rosette were wound-inoculated with a sterile pin dipped into a 24-h-old culture and inoculated into the outer margin of a single leaf, and the petiole and midrib of a second leaf on the same plant (Vicente et al. 1998). A third leaf was mock inoculated with sterile water. Plants were grown in a growth chamber with 14 h of light at 26°C. Symptoms appeared between 10 and 14 days postinoculation, with chlorotic V-shaped leaf lesions extending from the sites of inoculation, whereas the petiole inoculation led to vascular blackening and leaf wilting. No symptoms were observed on the mock-inoculated leaves. Symptoms were identical to diseased field samples. Inoculations were repeated with the same results. Bacteria reisolated from symptomatic plants were sequence confirmed to be X. campestris. To our knowledge, this is the first confirmed report of X. campestris naturally infecting garlic mustard in the United States. Future studies will investigate the Brassica host range for this isolate due to the plant’s extensive distribution and potential to serve as a reservoir for X. campestris.The author(s) declare no conflict of interest.

Variations in sediment production of dissolved iron across a continental margin not dominated by major upwelling or riverine inputs

Despite the undeniable effect of iron on shaping patterns of ocean productivity, the relative importance of the different sources of this limiting nutrient to the ocean is still under debate. Although global estimates indicate that the benthic input of iron to the oceans is significant, most studies have investigated continental margins exposed to either upwelling or large riverine inputs, environments that are not representative of the majority of the oceans. Additionally, the number of studies that report dissolved iron concentrations in continental slope sediments is limited, despite the fact that these regions between the shelf edge and the continental rise make up >5% of the sedimentary surface area of the global ocean. The sedimentary flux of iron has traditionally been considered negligible due to the rapid oxidation of Fe2+ in oxic waters and poor solubility of the Fe(III) product. The recent realization that ferric iron may be stabilized in solution by organic ligands during oxidation near the sediment-water interface suggests that a significant fraction of the dissolved iron pool may be present under the form organic-Fe(III) complexes that could eventually reach the overlying waters. In this study, the speciation and biogeochemical importance of iron was determined in intact sediment cores along a transect across the entire continental margin near Cape Lookout, North Carolina, a region not dominated by upwelling or riverine inputs that is representative of most passive continental margins. Rates of diffusive oxygen uptake (DOU) and maximum diffusive fluxes of both dissolved Fe2+and organic-Fe(III) complexes decreased from the coastal zone to the continental shelf, remained low on the shelf and the upper continental slope, but rebounded to reach a maximum in mid-slope sediments where concentrations of Fe(III) oxides were the highest along the transect. In turn, DOU decreased and dissolved iron was below detection in lower-slope sediments, indicating that mid-slope sediments represent depocenters where Fe(III) oxides and organic matter may accumulate. Pore water sulfate and sulfide concentrations as well as separate sediment incubations confirmed that sulfate reduction does not greatly influence the cycling of iron in these sediments. The production of dissolved organic-Fe(III) in these continental margin sediments is likely regulated by a combination of aerobic oxidation in the presence of natural organic ligands near the sediment-water interface, dissimilatory iron reduction, or chemical oxidation of Fe(II) complexed to natural organic ligands. Fluxes of Fe2+ and organic-Fe(III) complexes across the sediment-water interface were not observed. However, diffusive fluxes of Fe2+ and organic-Fe(III) complexes into the oxic zone of these sediments (<1 cm from the sediment-water interface) and production of dissolved Fe(III) in sediment slurry incubations suggest that complexation of Fe(III) in these sediments may contribute to the stabilization and potential transport of dissolved iron into oxygenated deep ocean waters. Extrapolation to the global ocean suggests that mid-slope depocenters contribute considerably to the iron inventory of the ocean, thus warranting the need for measurement of benthic iron fluxes and dissolved iron speciation in these environments.

Subduction Polarity in Ancient Arcs: A Call to Integrate Geology and Geophysics to Decipher the Mesozoic Tectonic History of the Northern Cordillera of North America: REPLY

Subduction Polarity in Ancient Arcs: A Call to Integrate Geology and Geophysics to Decipher the Mesozoic Tectonic History of the Northern Cordillera of North America: REPLY

Miocene flora from the Siwalik of Arjun Khola area, Nepal and its palaeoclimatic and phytogeographic implications

An extensive study on the plant fossils (leaf and fruit impressions/compressions) collected from the Miocene of Siwalik sediments, Arjun Khola area, western Nepal has been carried out. It revealed the existence of a variety of angiosperm plant taxa represented by 43 genera and 47 species belonging to 24 families. Of these, 34 species are reported for the first time from the studied area. Quite a number of fossils out of the entire lot, were described much prior to the present study from other represented by the Siwalik localities. Most of the leaf and fruit specimens are assignable to families of dicots but a single fossil leaf Clinogyne Salisb. has been assigned to the monocot family Marantaceae. The families which are highly represented in the assemblage are Fabaceae, Sapindaceae, Dipterocarpaceae and Annonaceae. Fabaceae which appeared in Upper Paleocene became a major component of the evergreen forest during middle Miocene. A majority of the families are generally represented by leaf forms but Sindora Miq. and Butea Roxb. ex Willd. of the Fabaceae and Terminalia L. of the Combretaceae are represented by fruits. Most of the fossil leaves in the assemblage showed large to medium size with drip tips, entire margins and apparent greater venation density. All the above characters collectively indicated the existence of tropical to sub–tropical type of vegetation during the Miocene all along the Himalayan foot hills of Nepal. Out of the identified specimens, the majority (more than 69%) resembled modern taxa, distributed in the tropical evergreen forests of different geographical regions of the world and recovery of similar looking fossil elements from the Arjun Khola area, indicated existence of similar forest types in and around the area at the time of Siwalik sedimentation. In contrast, the present day vegetation in and around the area is quite different from the past as it includes elements that generally constitute plants of dry deciduous forests. A number of plants migrated from south–east Asia to India via Myanmar and vice–versa. Consequently, many taxa, especially members of Dipterocarpaceae and Fabaceae, existing in south–east Asia in the Paleogene appeared on the Indian subcontinent and Nepal in the Neogene. Phytogeographical data also suggests that taxa flourishing in the Himalayan foot–hills during Siwalik sedimentation have migrated elsewhere in modern times possibly towards south and southeast in search of favourable conditions for luxuriant growth.Present day distribution of all the recovered species from the Siwalik Foreland Basins of Arjun Khola area shows that they are found today in the tropical forests of North–east India, Bangladesh, Myanmar and Malaysia where favourable climatic conditions exist and only little amount of taxa are found to grow presently in the Himalayan foothills. Thus, it may infer that a fair change in floral composition has taken since the Miocene. The nearest living relative (NLR) method of palaeoclimate construction suggests that the Arjun Khola area enjoyed a tropical climate having Mean Annual Temperature (MAT) 22–28ºC and Mean Annual Precipitation (MAP) 2200–3200 mm during the deposition of the sediments.

Management of Conjunctivochalasis

Conjunctivochalasis is defined as a redundant, nonedematous conjunctiva that causes a wide variety of symptoms. Excess conjunctival tissue may not cause any symptoms and may cause some symptoms like subconjunctival hemorrhage, epiphora, dry eye findings and corneal ulceration. Disturbance of tear meniscus, impaired tear distribution and punctal occlusion play a role in the onset of symptoms.&#x0D; Although the etiopathogenesis of the disease is not yet clearly understood, several theories have been proposed. According to the mechanical theory, age-related mechanical changes in the conjunctiva lead to a chronic obstruction of the lymphatic flow and lymphatic dilatation after this chronic obstruction leads to conjunctivochalasis. According to inflammatory theory, collagenolytic activity increases as a result of inflammation on the ocular surface, causing degeneration of elastic fibers. As a result, degeneration of elastic fibers lead to alterations in the extracellular components of the conjunctival tissue. This inflammatory changes resulting in conjunctival laxity.&#x0D; Although conjunctivosalasis (CCh) is a clinical diagnosis, it is often overlooked by clinicians. CCh patients are can be symptomatic or asymptomatic. Medical and / or surgical treatment is generally needed in symptomatic patients, whereas treatment is not necessary in asymptomatic patients. Medical treatment is the first choice in the treatment of conjunctivochalasis. Artificial tear preparations are widely used in the treatment of CCh due to the deterioration of the tear film layer and dry eye symptoms. In clinical practice, topical anti-inflammatory eye drops are often preferred to reduce ocular surface inflammation. In cases where medical treatment is not sufficient, surgical treatment should be performed.&#x0D; Today, there are many studies showing that surgical treatment is effective in reducing ocular symptoms and ocular surface damage in patients with CCh and in cases with and without dry eye.The surgical treatment plan should include the loose conjunctival tissue located in the lower part, as well as the excess conjunctival tissue located in the nasal and temporal regions and aim to correct the tear meniscus along the entire lower lid margin. The most preferred surgical method is crescent excision of CCh tissue and primary suture of the conjunctiva. Other surgical approaches include fibrin glue and amniotic membrane transplantation and direct scleral suture of CCh tissue. Another surgical method is electrocauterization of the conjunctival tissue. It is applied 5 mm away from limbus and there is no harm to fornixes.

Telipogon mayoi (Orchidaceae), a new species from the Western Andes of Colombia

Telipogon mayoi, from the western Colombian Andes, is proposed as a new species. The species was found in “La Elvira” National Protective Forest in the Yumbo Municipality, one of the oldest protected areas in Colombia, close to the Farallones de Cali National Park, both localities in the Dapa Mountains. Specimens of Telipogon mayoi were previously misidentified as Telipogon lankesteri Ames and T. williamsii P.Ortiz, but detailed analysis of the floral morphology revealed that it is different. Telipogon mayoi is most similar to T. lankesteri but it is characterized by the crenulated margins of the leaves (vs. entire margins), the ovate oblong lip (vs. oblong lanceolate) and furcate setae on the column (vs. simple setae). We provide a description, illustrations, a plate, in situ photographs, a distribution map, and ecological notes.&#x0D; Key Words: Andes, cloud forest, Colombia, miniature Telipogon, Oncidiinae

Influence of Incoming Plate Relief on Overriding Plate Deformation and Earthquake Nucleation: Cocos Ridge Subduction (Costa Rica)

AbstractWe present a 2‐D P wave velocity model and a coincident multichannel seismic reflection profile characterizing the structure of the southern Costa Rica margin and incoming Cocos Ridge. The seismic profiles image the ocean and overriding plates from the trench across the entire offshore margin, including the structures involved in the 2002 Osa earthquake. The overriding plate consists of three domains: Domain I displays thin‐skinned deformation of an imbricate thrust system composed of fractured rocks. Domain II shows ~15‐km‐long landward dipping reflection packages and active deformation of the shelf sediment. Domain III is little fractured and appears to be dominated by elastic deformation, overlain by ~2‐km‐thick landward dipping strata. The velocity structure supports the argument that the bulk of the margin is highly consolidated rock. Thick‐skinned tectonics probably causes the uplift of Domains II and III. The oceanic plate shows crustal thickness variations from ~14 km at the trench (Cocos Ridge) to 6–7 km beneath the shelf. We combine (1) interplate geometry and fracturing degree, (2) tectonic stresses and brittle strain, and (3) earthquake locations, to investigate relationships between structure and earthquake generation. The 2002 Osa sequence nucleated at the leading flank of subducting seamounts in the area of highest tectonic overpressure. Both estimated rock fracturing and modeled brittle strain steadily increase from the leading flank of the subducting seamounts to their top, reflecting the progressive damage caused by the seamount. Therefore, the seismicity and structural‐mechanical evolution of the upper plate reflect the downward propagation of the leading edge of seamounts.

Phytogeographical implications of the probable occurrence of the gnetalean plant Welwitschiophyllum in the Late Cretaceous (Cenomanian) of Africa

A new fossil plant specimen, identified as a probable leaf of Welwitschiophyllum Dilcher et al. (2005) is reported from the Gara Sbaa Member of the? Lower Cenomanian to Turonian Akrabou Formation of south east Morocco. Previously Welwitschiophyllum was only known from the Early Cretaceous of Brazil, and this discovery considerably extends its temporal and geographical ranges. It is identified on account of its characteristic elongate shape, entire margins, parallel venation and an arcuate margin of the base. The new specimen expands our knowledge of the poorly-known Gara Sbaa florule, and is the first possible gnetophyte recorded from this locality, adding crucial knowledge to African Cretaceous floral diversity. Comparison with similar leaf types from the Aptian-aged Nova Olinda Member of the Crato Formation of north east Brazil hint at a xerophytic or perhaps halophilic floral province in equatorial Gondwana prior to the opening of the South Atlantic Ocean. This province is at least 3500 km from north to south.

Pharmacognostic study of tradescantia fluminensis vell. Leaves

Tradescantia fluminensis Vell (Family: Commelinaceae) is an ornamental plant used traditionally to improve the kidney function, as an analgesic and for wound healing. The leaves are reported to possess significant analgesic, anti-inflammatory, and lipoxygenase inhibition properties. Thus far, the pharmacognostic study of the leaves of T. fluminensis has not yet been reported in the literature. The present paper deals with the establishment of standardization parameters through the pharmacognostic study of leaves. Pharmacognostical study included macroscopic and microscopic characters of the leaves. Physicochemical parameters like ash value and extractive values were determined. Preliminary phytochemical screening of various leaf extracts were studied. The macroscopic characters demonstrated simple, entire margin, parallel venation, and alternate phyllotaxis. Microscopic studies revealed the presence of bulliform cells, calcium oxalate crystals, and uniseriate covering trichomes. Conjoint and collateral vascular bundles arranged in a parallel series are seen. Powder microscopic studies showed the presence of paracytic stomata, fragments of mesophyll, fragments of epidermal cells showing palisade cells beneath them, non-lignified phloem fibers, covering trichomes and crystals of calcium oxalate. Preliminary phytochemical studies showed the presence of tannins, flavonoids, and steroids in the leaves. Fluorescence analysis showed typical coloured fluorescence when the extracts were examined under UV light. The study could serve as a basis of establishing pharmacognostic standards for T. fluminensis and help in differentiating from other related species. Further, it will help to authenticate and identify adulteration in the plant material. The diagnostic microscopic characters and physicochemical data will be helpful in the development of the herbal monograph for the species.

Habitat suitability and environmental niche comparison of cold-water coral species along the Brazilian continental margin

In face of increasing anthropogenic disturbance in the deep sea, it is a priority to better understand the regional distribution of cold-water corals (CWC). These organisms create some of the most species-rich habitats in the deep sea and, for this reason, they must be properly protected and managed. In this study, we aimed to identify suitable habitat for multiple CWC taxa off the Brazilian continental margin and compare their environmental niches. Habitat suitability models were developed using the Maxent approach, which allowed for the prediction of species distribution and for the identification of potential ‘hot spot’ areas that may be important for biodiversity conservation. Ecological niches were determined by a PCA-env approach, and niche similarity and equivalence were evaluated based on niche overlap using the Schoener's D metric. Potentially suitable habitat for Octocorallia covered a broad latitudinal range encompassing nearly the entire Brazilian continental margin, whereas Scleractinia had greater potentially suitable habitat in the Central and Southern areas. Scleractinian species were observed to slightly differ in their environmental niche, with non-reef-forming species being more tolerant to a wider range of environmental conditions in comparison with reef-forming species, inhabiting a wider area of the South American continental margin. Due to the high potential suitability for several CWC species, the Central and Southern parts of the Brazilian continental margin should be considered as potential areas high CWC diversity. Considering the current state of the art and strategic assessment tools, these areas are important targets for conservation, management, and environmental impact assessment. Most reef-forming species had similar but not directly equivalent ecological niches, indicating that mapping efforts and management planning should consider CWCs at the species level.

Pseudomonas mangiferae sp. nov., isolated from bark of mango tree in Thailand.

An aerobic, Gram-stain-negative, rod-shaped bacterium, designated DMKU BBB3-04T, was isolated from bark of mango tree . Colonies were circular, convex with entire margins when grown on nutrient agar medium for 2 days. The bacterium was motile by means of lophotrichous flagella and produced black-brown pigment. The strain grew at 12-40 °C (optimum, 28-30 °C) and at pH 6.0-8.0 (pH 6.5). Growth was observed in the presence of up to 5 % (w/v) NaCl. Strain DMKU BBB3-04T showed the highest 16S rRNA gene sequence similarity to Pseudomonas furukawaii KF707T (97.1 %), Pseudomonas indica NBRC 103045T (97.0 %), Pseudomonas tarimensis MA-69T (96.9 %) and Pseudomonas azotifigens 6H33bT (96.8 %), suggesting that strain DMKU BBB3-04T should be classified within the genus Pseudomonas. Analysis of strain DMKU BBB3-04T was also performed using three housekeeping genes (gyrB,rpoB and rpoD) and further confirmed the phylogenetic assignment of the strain. The major fatty acids found in strain DMKU BBB3-04T were summed feature 8 (C18 : 1 ω7c/C18 : 1 ω6c), C16 : 0 and summed feature 3 (C16 : 1 ω7c/C16 : 1 ω6c) (35, 22 and 19 %, respectively). The major polar lipids consisted of diphosphatidylglycerol, phosphatidylethanolamine and phosphatidylglycerol. The respiratory quinone was Q-9. The DNA G+C content of the strain DMKU BBB3-04T was 67.6 mol%. On the basis of phenotypic characteristics, chemotaxonomic data and phylogenetic analysis, strain DMKU BBB3-04T is considered to represent a novel species in the genus Pseudomonas. We propose the name Pseudomonasmangiferae sp. nov. for this novel species. The type strain of the novel species is DMKU BBB3-04T (=TBRC 7080T=JCM 32061T).

English

Fadogia cienkowskii is a shrub used in folklore medicine. Evaluations of the leaves were carried out to determine the macroscopic, microscopic, chemomicroscopic, physicochemical and phytochemical profiles using standard methods. The macroscopic examination revealed fresh leaves are green, odourless with a bitter taste. The leaf is oblong-elliptic in shape and sub-acute at apex; rounded at the base with entire margin. Microscopic examination indicated the presence of calcium oxalate crystals, starch grains, xylem, phloem, trichomes, epidermal cells, collenchyma cells, paracytic stomata and reticulate vessels. Chemomicroscopic characters present are lignin, starch, cellulose, mucilage and calcium oxalate crystals. The physicochemical evaluation indicated 4.6% moisture content, 1.4% total ash value, 0.8% acid insoluble ash value, 0.4% water soluble ash value, 7.8% water soluble extractive value and 9.0% alcohol soluble extractive value. The phytochemical evaluation revealed the presence of tannins (17.6%), saponins (1%), glycosides (2.5%), alkaloids (3.3%), steroids (1.1%), terpenoids (6.6%), phenols (8.8%), flavonoids (17.7%) and the absence of hydrogen cyanide. This study is useful in pharmacognostic standardization of this plant. The parameters laid down will be useful and suitable for compilation of a monograph and help in identifying this plant in its crude form and prevent it from adulteration and ensure its therapeutic efficacy. Key words: Fadogia cienkowskii, pharmacognostic, phytochemical, physicochemical, macroscopic, microscopic, chemomicroscopic. &nbsp

Two new species of Microlicia D.Don (Melastomataceae) from campos rupestres in eastern Brazil

Two new species of Microlicia (Melastomataceae) endemic to campos rupestres in Serra do Cipó, Minas Gerais, Brazil, are described, illustrated and compared with their putative relatives. Microlicia rugosa sp. nov. is similar to M. minutiflora and M. martiana by having fastigiate branches, ascending, lanceolate or oblanceolate leaves with obtuse apex, attenuate base and entire margin, flower with short pedicels (1−2 mm long), magenta petals, and dimorphic stamens. Microlicia rugosa is further characterized by wrinkled surface of hypanthium and sepals, and both leaf surfaces with distinct depressions, which sometimes contain short‐stalked glandular trichomes. Microlicia viscida sp. nov. is similar to M. martiana, M. furnensis and M. rugosa mainly by having fastigiate branches, terete stems without leaves at the base and the bark gradually peeling to reveal the underlying brownish wood and leaves with similar size and shape. Microlicia viscida is characterized by a conspicuous secretion covering branches, leaves, hypanthium and sepals, giving a smooth and bright appearance. The leaf anatomy of both new species is briefly described. Microlicia rugosa and M. viscida are assessed as ‘Endangered’ and ‘Critically Endangered’ respectively, due to its limited extent of occurrence and area of occupancy, according to the IUCN categories and criteria.

&lt;i&gt;Monostroma alittorale&lt;/i&gt;, a marine green algal species newly recorded in Korea

A marine green algal species (Chlorophyta) was collected from the eastern coast of Korea. It is morphologically characterized by monostromatic thallus, usually undulate and entire margins, cap-like chloroplast and several pyrenoids per cell. In a phylogenetic tree based on molecular data, the Korean alga nests in the same clade as Monostroma alittorale originally described from Japan, as a sister clade of M. grevillei from France. The genetic distance for ITS (Internal Transcribed Spacer) sequences among Monostroma species ranges from 2.3% to 38.2%. The value between the Korean entity and M. alittorale was calculated as 0.01%, considered to be intraspecific divergence. This Korean entity is identified as Monostroma alittorale based on morphological and molecular analyses. This is the first record of M. alittorale in Korea.

New record of &lt;i&gt;Ulva sublittoralis&lt;/i&gt; (Ulvales, Chlorophyta) in Korea

A marine ulvalean species (Chlorophyta) was collected from the eastern coast of Korea. This species is morphologically characterized by a distromatic, dark to medium green and mostly irregularly orbicular or irregularly expanded thallus with entire or undulate margin without serrations. Vegetative cells are irregularly polygonal with distinctly rounded corners in shape, and have chloroplast completely covering the outer cell wall and one to two pyrenoids per cell. In a phylogenetic tree based on ITS (Internal Transcribed Spacer) sequences, this Korean alga nests in the same clade with Ulva sublittoralis, as a sister clade of U. californica, U. flexuosa and U. tanneri, which share the irregularly orbicular or expanded thallus normally without teeth cells. The genetic divergence between them is intraspecific within Ulva. Accordingly, it is identified as U. sublittoralis based on the morphological and molecular data. This is the first record of Ulva sublittoralis in the Korean marine algal flora.

Alb-Cenomanian granitoid magmatism and copper ore genesis of the Sikhote-Alin

Late Albian-early Cenomanin epoch of Au-Cu porphyry mineralization has been distinguished within the Sikhote-Alin. It is associated with the Alb-Cenomanian granitic rocks which emplacement coincided with the processes of orogeny and neoformation of continental lithosphere caused by compressive stress in the setting of transform continental margins of that time. The intrusion of the granitic magma into the crust of Jurassic accretionary wedge terranes and Early Cretaceous terrane of epicontinental turbidite basin provoked development of Au-Mo-Cu and Cu-Au-W ore genesis, respectively. U-Pb dating of zircons from host granites of the Malmuzh Au-Cu deposit yielded Alb-Cenomania age of 100-95 Ma. This age harmonizes with the age data reported by other researchers on the granitic rocks of East and Southeast Asia which are productive for hydrothermal mineral deposits of copper, gold, tin and other metals. Such age consistency suggests that there is Albian-Cenomanian metallogenic megabelt extending throughout the entire East Asian continental margin.

Clinoform growth and sediment flux into late Cenozoic Qiongdongnan shelf margin, South China Sea

AbstractThe South China Sea continental margin in the Qiongdongnan Basin (QDNB) area has incrementally prograded since 10.5 Ma generating a margin sediment prism more than 4km‐thick and 150–200 km wide above the well‐dated T40 stratigraphic surface. Core and well log data, as well as clinoform morphology and growth patterns along 28 2D seismic reflection lines, illustrate the evolving architecture and margin morphology; through five main seismic‐stratigraphic surfaces (T40, T30, T27, T20 and T0) frame 15 clinothems in the southwest that reduce over some 200 km to 8 clinoforms in the northeast. The overall margin geometry shows a remarkable change from sigmoidal, strongly progradational and aggradational in the west to weakly progradational in the east. Vertical sediment accumulation rate increased significantly across the entire margin after 2.4 Ma, with a marked increase in mud content in the succession. Furthermore, an estimate of sediment flux across successive clinoforms on each of the three selected seismic cross sections indicate an overall decrease in sediment discharge west to east, away from the Red River depocenter, as well as a decrease in the percentage of total discharge crossing the shelf break in this same direction. The QDNB Late Cenozoic continental margin growth, with its overall increased sediment flux, responded to the climate‐induced, gradual cooling and falling global sea level during this icehouse period.