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Hypersaline ecosystems are distributed all over the globe. They are subjected to poly-extreme stresses and are inhabited by halophilic microorganisms possessing multiple adaptations. The halophiles have many biotechnological applications such as nutrient supplements, antioxidant synthesis, salt tolerant enzyme production, osmolyte synthesis, biofuel production, electricity generation etc. However, halophiles are still underexplored in terms of complex ecological interactions and functions as compared to other niches. The advent of metagenomics and the recent advancement of next-generation sequencing tools have made it feasible to investigate the microflora of an ecosystem, its interactions and functions. Both target gene and shotgun metagenomic approaches are commonly employed for the taxonomic, phylogenetic, and functional analyses of the hypersaline microbial communities. This review discusses different types of hypersaline niches, their residential microflora, and an overview of the metagenomic approaches used to investigate them. Various applications, hurdles and the recent advancements in metagenomic approaches have also been focused on here for their better understanding and utilization in the study of hypersaline microbiome. [ABSTRACT FROM AUTHOR]

Fossil leaves, fruits, and woods assigned to Rhamnaceae have been recorded from India, however, there are no previous reports of rhamnaceous fossil flowers from India. Here, we report the first fossil flowers in appreciable numbers from the early Eocene (Palana Formation) sedimentary sequences of Gurha Lignite Mine, Rajasthan, western India, and show that they are attributable to Rhamnaceae. We examined variation in flower morphology among extant and extinct rhamnaceous species as a basis for interpreting our fossil flowers. The specimens are small star‐like, pentamerous, actinomorphic, gamosepalous flowers with triangular, keeled sepals with acute apices, spathulate, short‐clawed petals alternating with sepals, shallow, five‐lobed nectary disc with prominent pentagonal outer margin, and a centrally placed globose ovary with stigma scar. The flowers co‐occur with ziziphoid leaves and are recognized as a new species Eopaliura indica Patel, Rana & Khan sp. nov. Because of aforesaid characteristics, fossil flowers are easily identifiable as Rhamnaceae and should provide a reliable means of documenting the evolutionary history of this family during the Cenozoic. [ABSTRACT FROM AUTHOR]

Eucalypt fossils were widely reported from the Cenozoic deposits across the Southern Hemisphere (Australia, New Zealand, and Argentina). However, no attached reproductive and vegetative fossil remains of this myrtaceous clade have been discovered till now. We report and describe for the first time a fossil eucalypt twig with attached foliage, flower buds, and mature flowers from the early Eocene (~55–52 Ma) sediments (Palana Formation) of Rajasthan, western India. As both vegetative and reproductive organs are in organic connection, they clearly represent the same species. In addition, here we also introduce fossil materials of isolated leaves, flower buds, inflorescence, and flowers recovered from the same stratigraphic level. Our Eocene fossils and extant members of the eucalypt clade are related morphologically by means of robust, thick petiolate lanceolate‐shaped leaves with intramarginal secondary veins; operculate flower buds consisting of imbricate petals with discernable margins; solitary inflorescence with three flowers per umbellaster, epigynous and bisexual flowers. Based upon combined characteristics of leaf, flower, and bud morphology, these fossils conform to the Eucalypt clade and are recognized as a new fossil genus and species: Hindeucalyptus eocenicus Patel, R.F. Almeida, Ali et Khan gen. nov. et sp. nov. We also compare it with extant and extinct eucalypts using morphological phylogeny and character mapping analyses. In addition, we briefly discuss its phytogeographic and paleoclimatic implications regarding the distribution and habitat of fossil and modern eucalypts. [ABSTRACT FROM AUTHOR]

Here we have identified and characterized a devastating virus capable of inducing yellow mosaic on the leaves of Patchouli [Pogostemon cablin (Blanco) Benth]. The diagnostic tools used were host range, transmission studies, cytopathology, electron microscopy, serology and partial coat protein (CP) gene sequencing. Evidence from biological, serological and sequence data suggested that the causal virus belonged to genus Potyvirus, family Potyviridae. The isolate, designated as Patchouli Yellow Mosaic Virus (PaYMV), was transmitted through grafting, sap and the insect Myzus persicae (Sulz.). Flexuous rod shaped particles with a mean length of 800 nm were consistently observed in leaf-dip preparations from natural as well as alternate hosts, and in purified preparation. Cytoplasmic cylindrical inclusions, pinwheels and laminar aggregates were observed in ultra-thin sections of infected patchouli leaves. The purified capsid protein has a relative mass of 43 kDa. Polyclonal antibodies were raised in rabbits against the coat protein separated on SDS – PAGE; which were used in ELISA and western blotting. Using specific antibodies in ELISA, PaYMV was frequently detected at patchouli plantations at Lucknow and Bengaluru. Potyvirus-specific degenerate primer pair (U335 and D335) had consistently amplified partial CP gene from crude preparations of infected tissues by reverse transcription polymerase chain reaction (RT-PCR). Comparison of the PCR product sequence (290 bp) with the corresponding regions of established potyviruses showed 78–82% and 91–95% sequence similarity at the nucleotide and amino acid levels, respectively. The results clearly established that the virus under study has close homology with watermelon mosaic virus (WMV) in the coat protein region and therefore could share a common ancestor family. Further studies are required to authenticate the identity of PaYMV as a distinct virus or as an isolate of WMV. [ABSTRACT FROM AUTHOR]

The reactions of [Zn 3 Cl 2 (3,5-Me 2 PzH) 4 ( t -BuPO 3 ) 2 ] with organostibonic acid in varying reaction conditions have been investigated. Single-crystal X-ray diffraction studies reveal the formation of [Zn 2 ( p -ClC 6 H 4 Sb) 2 (O) 2 (OCH 3 ) 2 ( t -BuPO 3 ) 3 (py) 2 ] ( 1 ), [Zn 2 ( p -ClC 6 H 4 Sb V ) 4 (Sb III ) 2 (O) 8 ( t -BuPO 3 H) 4 ( t -BuPO 3 ) 2 (py) 2 Cl 2 ] ( 2 ), and [Zn 2 (RSb) 4 (O) 4 (OCH 3 ) 4 ( t -BuPO 3 ) 4 (py) 2 ], where R = p -ClC 6 H 4 ( 3 ) and R = p -iPrC 6 H 4 ( 4 ), respectively. Interestingly, in the synthesis of 2 , complete dearylation of organoantimony moieties followed by C-F bond formation, a reduction from Sb (V) to Sb (III), and Sb···Cl weak intermolecular interactions have been observed. ESI-MS studies suggested that clusters 1 - 4 maintained their structural integrity in the solution state also. Solution NMR studies ( 1 H, 31 P, and 13 C) support well the observed solid-state structures. 1 - 4 were tested for antibacterial activity using a microdilution assay. 1 and 4 showed the best activity with lower MIC values (0.78-6.25 μg/mL) against all the tested pathogens. The total antioxidant activity of 1 - 4 was evaluated through the phosphomolybdenum assay, which showed a total antioxidant activity ranging from 28.96 to 86.46 mg AAE/g compound with the ascorbic acid standard.