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Simple Summary: The bright red color of Erythraeid mites is conspicuous. The Erythraeid larvae are usually ectoparasitic on arthropods and easily observed. Both the genera Charletonia and Leptus are distributed worldwide. Charletonia has 86 species and Leptus has more than 240 species based on larvae, respectively. To date, two species of the genus Charletonia and 11 species of the genus Leptus have been reported from China. Here, four new species, Charletonia rectangia Xu and Jin sp. nov. collected from tropical rainforests in the Guangxi Province and Yunnan Province, Leptus (Leptus) bomiensis Xu and Jin sp. nov. from the Tibet Autonomous Region, where the altitude ranges from 2673 to 3374 m, Leptus (Leptus) longisolenidionus Xu and Jin sp. nov. from jungles in the Hainan Province (Hainan Island), and Leptus (Leptus) striatus Xu and Jin sp. nov. from Xishuangbanna tropical rainforests in the Yunnan Province. We believe that this study will contribute to further research on the taxonomy and phylogeny of the family. Four new species, Charletonia rectangia Xu and Jin sp. nov., Leptus (Leptus) bomiensis Xu and Jin sp. nov., Leptus (Leptus) longisolenidionus Xu and Jin sp. nov., and Leptus (Leptus) striatus Xu and Jin sp. nov. are described and illustrated based on larvae. All four new species are from biodiversity hotspots, L. (L.) bomiensissp. nov. from the Eastern Himalayas biodiversity hotspot, while the other three species from the Indo–Burma biodiversity hotspot. [ABSTRACT FROM AUTHOR]

Diplogyniopsis fluctuosumsp. nov. associated with passalid beetles is described based on females from China on undermined passalid beetles, as well as on females and males from Thailand on Aceraius helferi (Coleoptera: Passalidae). The species represents the second known species of Diplogyniopsis Trägårdh, prompting us to redefine the genus diagnosis. [ABSTRACT FROM AUTHOR]

• Two kinds of magnetite are identified at porphyry-related deposits in the Zhongdian region. • Some magnetite grains had undergone dissolution-reprecipitation processes. • The compositions of magnetite are affected by temperature, oxygen fugacity and hydrothermal alteration. The Zhongdian region in northwestern Yunnan (SW China) hosts a number of important porphyry and skarn deposits. In this study, we integrate petrographic observations, SEM-EDS elemental mapping, EPMA and LA-ICP-MS geochemical analyses on magnetite from several key deposits in the region. Magnetite grains from the Pulang porphyry Cu-Au, Lannitang porphyry Au-Cu, Langdu Cu skarn, Disuga porphyry, and andesite of Tumugou Formation were analyzed to unravel the magnetite formation mechanism, and the relative oxygen fugacity of the porphyry/skarn ore-related hydrothermal fluids in this region. Two types of magnetites (Magnetite I and II) have been identified. Magnetite I is commonly distributed in the chlorite and/or sericite alteration zone(s). Magnetite I grains are characterized by being textually inhomogeneous. The Magnetite I core (with local ilmenite exsolution lamellae) is Ti-Cr rich, indicative of a dominantly igneous origin. The Magnetite I core and its surrounding primary igneous minerals (biotite, amphibole and plagioclase) underwent late alteration. Magnetite I grains are characterized by core-rim texture, sharp core-rim contact, and irregular grain boundaries. These textural features indicate that Magnetite I may have undergone dissolution-reprecipitation processes, during which the Magnetite I core was chemically purified via losing Ti and gaining Fe. Magnetite II (in potassic and sericite alteration zones) is textually homogeneous with relatively low contents of Ti, Mg, Al, V, Ni, and Mn. We suggest that Magnetite II was formed by hydrothermal alteration. Compared to Magnetite II grains from the Pulang and Langdu deposits, those from the Lannitang deposit have lower Mn and V but higher Sn contents, indicative of higher oxygen fugacity of the hydrothermal fluids. We propose that binary plots such as Ti vs. Sc, V vs. Sn and Ga vs. Sn can distinguish the different origins of magnetites. From an exploration perspective, Magnetite II from the altered Disuga porphyries has similar texture and composition to its counterpart from the potassic-altered Pulang porphyries. This, together with the presence of Cu-sulfide inclusions in the Disuga Magnetite I, suggests significant mineralization potential in these porphyries. [ABSTRACT FROM AUTHOR]

Begomoviruses (family Geminiviridae) cause serious diseases in many crops. In this study, we characterized a begomovirus isolated from a tobacco plant with leaf curl in Puer, Yunnan Province, China. Analysis of the viral genome obtained from a symptomatic Nicotiana tabacum plant showed that it belonged to a novel monopartite begomovirus. The genome (2741 nt) shared the highest nucleotide sequence identity (83.43%) with that of tomato yellow leaf curl Vietnam virus (TYLCVV). Based on the current taxonomic criteria of the International Committee on Taxonomy of Viruses, this virus, for which the name "tobacco leaf curl Puer virus" is proposed, represents a new species of begomovirus. [ABSTRACT FROM AUTHOR]