0000000000744901

AUTHOR

Ming Tang

showing 4 related works from this author

Additional file 1 of The genome sequence of the grape phylloxera provides insights into the evolution, adaptation, and invasion routes of an iconic p…

2020

Additional file 1: Figures. S1-S22, Table S1-S20, Methods and Results. Figure S1. Mitochondrial genome view of grape phylloxera. Figure S2. Proportion of transposable elements (TE) in the genome. Figure S3. GO terms of phylloxera-specific genes. Figure S4. Enriched GO terms in the phylloxera genome with and without TEs. Figure S5. Gene gain/loss at different nodes or branches. Figure S6. Species phylogenetic tree based on insect genomes and the transcriptomes of Planoccoccus citri and Adelges tsugae. Figure S7. Diagram of the gap-filling and annotation process. Figure S8. Urea cycle in D. vitifoliae and A. pisum. Figure S9. IMD immune pathway in D. vitifoliae.Figure S10. Phylogenetic tree o…

2. Zero hunger
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Additional file 1 of The genome sequence of the grape phylloxera provides insights into the evolution, adaptation, and invasion routes of an iconic p…

2020

Additional file 1: Figures. S1-S22, Table S1-S20, Methods and Results. Figure S1. Mitochondrial genome view of grape phylloxera. Figure S2. Proportion of transposable elements (TE) in the genome. Figure S3. GO terms of phylloxera-specific genes. Figure S4. Enriched GO terms in the phylloxera genome with and without TEs. Figure S5. Gene gain/loss at different nodes or branches. Figure S6. Species phylogenetic tree based on insect genomes and the transcriptomes of Planoccoccus citri and Adelges tsugae. Figure S7. Diagram of the gap-filling and annotation process. Figure S8. Urea cycle in D. vitifoliae and A. pisum. Figure S9. IMD immune pathway in D. vitifoliae.Figure S10. Phylogenetic tree o…

2. Zero hunger
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The genome sequence of the grape phylloxera provides insights into the evolution, adaptation, and invasion routes of an iconic pest

2020

Background: Although native to North America, the invasion of the aphid-like grape phylloxera Daktulosphaira vitifoliae across the globe altered the course of grape cultivation. For the past 150 years, viticulture relied on grafting-resistant North American Vitis species as rootstocks, thereby limiting genetic stocks tolerant to other stressors such as pathogens and climate change. Limited understanding of the insect genetics resulted in successive outbreaks across the globe when rootstocks failed. Here we report the 294-Mb genome of D. vitifoliae as a basic tool to understand host plant manipulation, nutritional endosymbiosis, and enhance global viticulture. Results: Using a combination of…

0106 biological sciencesFil·loxeraPhysiology[SDV]Life Sciences [q-bio]Introduced speciesPlant Science01 natural sciencesGenomeGene duplicationsStructural BiologyVitislcsh:QH301-705.5ComputingMilieux_MISCELLANEOUS2. Zero hunger0303 health scienceseducation.field_of_studyHost plant interactionsGenomeEndosymbiosisbiologyfood and beveragesBiological SciencesBiological EvolutionGeneral Agricultural and Biological SciencesRootstockInfectionDaktulosphaira vitifoliaeBiotechnologyResearch ArticlePopulation010603 evolutionary biologyGeneral Biochemistry Genetics and Molecular BiologyHemiptera03 medical and health sciencesGeneticsInsect pestsAnimalsPlagues d'insectesAdaptationBiological invasionsGenomeseducationPhylloxeraEcology Evolution Behavior and Systematics030304 developmental biologyObligateHuman GenomeViticulturaCell Biology15. Life on landbiology.organism_classificationBiologicalEffectorsClimate Actionlcsh:Biology (General)13. Climate actionEvolutionary biologyArthropod genomesPhylloxeraAdaptationIntroduced SpeciesInsectAnimal DistributionDevelopmental Biology
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The onset of deep recycling of supracrustal materials at the Paleo-Mesoarchean boundary.

2021

Abstract The recycling of supracrustal materials, and in particular hydrated rocks, has a profound impact on mantle composition and thus on the formation of continental crust, because water modifies the physical properties of lithological systems and the mechanisms of partial melting and fractional fractionation. On the modern Earth, plate tectonics offers an efficient mechanism for mass transport from the Earth's surface to its interior, but how far this mechanism dates back in the Earth's history is still uncertain. Here, we use zircon oxygen (O) isotopes to track recycling of supracrustal materials into the magma sources of early Archean igneous suites from the Kaapvaal Craton, southern …

MultidisciplinaryGeochemistryBoundary (topology)GeologyNational science review
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