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The efficiency of heat-shock treatments for producing gynogenetic double haploids was evaluated using a rainbow trout (Oncorhynchus mykiss) strain locally adapted in Brazil (2002 broodstock). Eleven and 15 females produced by conventional reproduction (FC) or meiotic gynogenesis (FG) were used as egg donors, respectively. Oocytes from each female were randomly divided into five uneven lots which were submitted to different treatments: (C2n) Normal diploid control, (H) Haploid control, (G-Me) Meiotic gynogenetic, (G-Mi) Mitotic gynogenetic, and (4 n) Control of suppression of the 1st cell cleavage. Homozygous yellow-colored (Dominant albino - DA) males were used as semen donors. Gynogenesis was induced by insemination of eggs with DA semen genetically inactivated by ultraviolet irradiation. Diploidization of gynogenic individuals was induced by an early heat shock to block 2nd polar body extrusion (G-Me), or a late heat shock to suppress first mitosis (G-Mi). Overall mean survival rates to eyed-egg and first feeding stages of treated groups, relative to respective C2n control group were: 19.21 and 14.90%, 13.02 and 8.09%, and 29.94 and 16.48%, for treatments G-Me, G-Mi and 4 n, respectively. When compared with C2n, all treatments showed lower survival rates at both stages. Survival of G-Me and G-Mi progeny from FG females were significantly higher when compared to progeny from FC females for both stages. Progenies from two different females observed to be 100% homozygous in analyzed informative microsatellite markers were used in subsequent cycles of gynogenic reproduction. One line originally derived from a single gynogenic female was reproduced for nine successive generations of meiotic gynogenetic reproduction. Forty animals from the ninth successive generation of gynogenetic reproduction were analyzed with a low-density SNP (Single Nucleotide Polymorphism) panel. All individuals were observed to be homozygous for identical alleles at all SNPs, therefore indicating that the established mitotic gynogenetic line is composed of 100% clonal individuals.

Fungi have the capacity to assimilate a diverse range of both inorganic and organic sulfur compounds. It has been recognized that all sulfur sources taken up by fungi are in soluble forms. In this study, we present evidence that fungi can utilize gaseous carbonyl sulfide (COS) for the assimilation of a sulfur compound. We found that the filamentous fungus Trichoderma harzianum strain THIF08, which has constitutively high COS-degrading activity, was able to grow with COS as the sole sulfur source. Cultivation with 34S-labeled COS revealed that sulfur atom from COS was incorporated into intracellular metabolites such as glutathione and ergothioneine. COS degradation by strain THIF08, in which as much of the moisture derived from the agar medium as possible was removed, indicated that gaseous COS was taken up directly into the cell. Escherichia coli transformed with a COS hydrolase (COSase) gene, which is clade D of the ß-class carbonic anhydrase subfamily enzyme with high specificity for COS but low activity for CO2 hydration, showed that the COSase is involved in COS assimilation. Comparison of sulfur metabolites of strain THIF08 revealed a higher relative abundance of reduced sulfur compounds under the COS-supplemented condition than the sulfate-supplemented condition, suggesting that sulfur assimilation is more energetically efficient with COS than with sulfate because there is no redox change of sulfur. Phylogenetic analysis of the genes encoding COSase, which are distributed in a wide range of fungal taxa, suggests that the common ancestor of Ascomycota, Basidiomycota, and Mucoromycota acquired COSase at about 790-670 Ma. [ABSTRACT FROM AUTHOR]

Downward transport of stratospheric air into the troposphere (identified as stratospheric intrusions) could potentially modify the radiation budget and chemical of the Earth's surface atmosphere. As the highest and largest plateau on earth, the Tibetan Plateau including the Himalayas couples to global climate, and has attracted widespread attention due to rapid warming and cryospheric shrinking. Previous studies recognized strong stratospheric intrusions in the Himalayas but are poorly understood due to limited direct evidences and the complexity of the meteorological dynamics of the third pole. Cosmogenic 35S is a radioactive isotope predominately produced in the lower stratosphere and has been demonstrated as a sensitive chemical tracer to detect stratospherically sourced air mass in the planetary boundary layer. Here, we report 6-month (April-September 2018) observation of 35S in atmospheric sulfate aerosols (35SO4 2°) collected from a remote site in the Himalayas to reveal the stratospheric intrusion phenomenon as well as its potential impacts in this region. Throughout the sampling campaign, the 35SO4 2-concentrations show an average of 1,070 ± 980 atoms/m3. In springtime, the average is 1,620 ± 730 atoms/m3, significantly higher than the global existing data measured so far. The significant enrichments of 35SO4 2-measured in this study verified the hypothesis that the Himalayas is a global hot spot of stratospheric intrusions, especially during the springtime as a consequence of its unique geology and atmospheric couplings. In combined with the ancillary evidences, e.g., oxygen-17 anomaly in sulfate and modeling results, we found that the stratospheric intrusions have a profound impact on the surface ozone concentrations over the study region, and potentially have the ability to constrain how the mechanisms of sulfate oxidation are affected by a change in plateau atmospheric properties and conditions. This study provides new observational constraints on stratospheric intrusions in the Himalayas, which would further provide additional information for a deeper understanding on the environment and climatic changes over the Tibetan Plateau. [ABSTRACT FROM AUTHOR]