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As one of the pioneer palaeontologists, Professor Zhuoting Liao has contributed his lifetime to promoting palaeontological and stratigraphical research in China for 60 years, and he passed away in the field excursion in South China on June 20, 2020. In his palaeontological career, Liao has worked on Late Palaeozoic to Mesozoic palaeontology and stratigraphy of almost all regions across China, and his interests have also extended to the Permian–Triassic (P‐Tr) boundary and mass extinction. He has worked on palaeontology, palaeobiogeography, biostratigraphy, tectonostratigraphy, and their implications in mineral and oil‐gas industries. Liao has established 22 new genera and 172 new species of brachiopods, and, together with his colleagues, proposed 11 new genera and 25 new species of echinoderms. He dedicated his lifetime to work on Late Palaeozoic palaeontology and stratigraphy of the previously remote and tectonically complex Xinjiang and adjacent regions, north‐west China, and established integrated stratigraphical frameworks for the Carboniferous to Permian strata, providing fundamental basis for mineral and hydrocarbon exploration in the poorly understood Central Asian terranes. In addition, he has mentored many young palaeontologists and stratigraphers in various ways. This volume assembles 30 papers addressing the Late Palaeozoic to Mesozoic palaeontology and stratigraphy of China and adjacent regions, which pays tribute to the achievement of Professor Zhuoting Liao. [ABSTRACT FROM AUTHOR]

The Chinese government has launched the Rural Living Environment Improvement Initiative (RLEII) to solve the poor living conditions in rural areas. The initiative enhances rural greenery; provides sanitary toilets; and promotes proper disposal of animal manure, sewage, and household waste in rural areas. We collected data using in‐person interviews with 938 rural residents in Xinjiang, China, to elicit their preference, preference intensity, and preference heterogeneity for RLEII. Results indicated that rural residents prefer to see shortcomings of the RLEII addressed. Rural greening construction is identified with the highest preference intensity. We also find significant heterogeneity in rural residents' preferences for each attribute of RLEII. The preference heterogeneity is rooted in the region's economic condition (poor vs. nonpoor region). It is essential to understand rural residents' choice for rural public goods supply and to respect their preference intensity, sequence, and heterogeneity for RLEII to enhance the implementation performance. We discuss the implications of these findings. [ABSTRACT FROM AUTHOR]

Crude oil is the most exploited energy source and the best way to increase the yield of oil recovery is the use of middle‐phase microemulsions. But the consecutive formation of water‐in‐oil emulsions needs oil–water separation. Reversible middle‐phase microemulsions were prepared with tetradecane (equivalent alkane for crude oil from Xinjiang oilfields, China) and aqueous solutions containing 1‐pentanol, N,N‐dimethyltetradecylamine and NaCl, and stimulated with CO2. By adding and removing CO2, the conductivity of aqueous solutions without NaCl increases from 20 μS/cm to 3.6 mS/cm reversibly. Additionally, the surface and interfacial tensions of aqueous solution show reversible changes. The middle‐phase microemulsion is stable in CO2 atmosphere. After removing CO2, it becomes separated into oil and aqueous phases. However, by sparging CO2 and standing for 2 days, it becomes middle‐phase microemulsion again. This research is expected to launch a brand‐new avenue for the CO2‐stimulated reversible microemulsification. [ABSTRACT FROM AUTHOR]

The Middle Permian black shales from the eastern Junggar Basin of northern Xinjiang, north‐west China are one of the richest and thickest lacustrine hydrocarbon source rocks in China. The palaeoenvironmental settings and controlling factors of organic matter accumulation along the margins of the Middle Permian lacustrine basin remain unclear, although the same works have been undertaken in the centre of the Middle Permian lacustrine basins. Here, we performed a combination of mineralogical and geochemical analyses on the black shales of the Middle Permian Pingdiquan Formation from the eastern margin areas of the Junggar Basin. The results show that the Pingdiquan Formation black shales in the study areas are organic‐rich, with total organic carbon (TOC) contents of 0.74–17.61 wt% (avg. 5.81 wt%). Salinity proxies including Sr/Ba and Rb/K ratios, combined with traces of gypsum and halite in a few samples, suggest brackish to saline water conditions. Palaeoclimate proxies indicate a warm‐humid environment during the deposition of the Pingdiquan Formation black shales. The redox proxies V/(V + Ni), V/Cr and U/Th ratios, and Eu and Ce anomalies together indicate dysoxic‐anoxic conditions of lake water. Strong positive correlations between palaeoproductivity proxies (P/Al, Ni/Al, Cu/Al, and Zn/Al) and TOC contents imply that palaeoproductivity may have played an essential role in organic matter accumulation during the deposition of the black shales. In contrast, negative correlations between terrestrial detrital input proxies (Al and Ti) and TOC contents indicate that terrestrial detrital input may have acted as a diluent to organic matter accumulation. Additionally, although the correlation between redox proxies [V/(V + Ni) and U/Th] and TOC contents is not straightforward, dysoxic‐anoxic conditions of lake water are an essential prerequisite for organic matter accumulation in the Pingdiquan Formation black shales. [ABSTRACT FROM AUTHOR]

A large number of fossil woods were preserved in the Permian–Triassic sequences in the Junggar Basin of Xinjiang Uygur Autonomous Region. These wood fossils provide a lot of palaeoenvironmental information of the Junggar Basin during the Permian–Triassic transition. Here, we describe the fossil woods collected from the base of the Olenekian Shaofanggou Formation in Dalongkou Anticline. Anatomically, these wood remains closely resemble Junggaropitys dalongkouensis, but they lack growth rings and rays are higher. Thus, we suggest identifying them as J. cf. dalongkouensis. The growth pattern shows that J. cf. dalongkouensis is evergreen and developed under warm and humid environments. However, the data of geochemistry, palaeosol and certain sedimentary features reveal a dry climate. Thus, we speculate that the Olenekian Junggar Basin contained gallery forests in the arid environment. [ABSTRACT FROM AUTHOR]

The Upper Devonian of western Junggar, Xinjiang, northwestern China bears abundant marine fossils and has attracted much attention with respect to palaeontological and stratigraphical studies. However, the records of ammonoids are sparse and the previously established assemblages need to be supplemented or emended through further collections. Here, we describe the Gonioclymenia fauna from the Wulan Member of the Hongguleleng Formation based on thorough and systematic sampling, including Gonioclymenia junggarensis n. sp., a member of the Gonioclymenia subcarinata Group, an evolute clymeniid, Cymaclymenia sp., and an indeterminate species of the Sporadoceratidae or Prionoceratidae. The strata bearing the Gonioclymenia fauna in western Junggar can be correlated with the upper Famennian UD V‐A2 to V‐C of the Clymenia Ammonoid 'Stufe', approximately corresponding to the Bispathodusaculeatus aculeatus Conodont Zone (former Middle expansa Zone). The Gonioclymenia species from western Junggar indicate close relationships with Europe and North Africa, while the latter two regions show a higher abundance and species diversity within the genus. New specimens described here enrich the composition of the Gonioclymenia fauna of western Junggar, and shed lights on the stratigraphic correlation and subdivision of the Upper Devonian in this region at a fine resolution. [ABSTRACT FROM AUTHOR]

A silicified trunk, Zhuotingoxylon liaoi Wan, Yang, Wang, Liu et Wang gen. et sp. nov., is described from the uppermost part of Guodikeng Formation in South Taodonggou section, Turpan–Hami Basin, Xinjiang Uygur Autonomous Region, northwestern China. It is characterized by a solid pith, endarch primary xylem and pycnoxylic wood. The pith is composed of parenchyma and sclereids. Radial walls of primary xylem tracheids have spiral and scalariform thickenings. Secondary xylem consists of thick‐walled tracheids and parenchymatous rays. Uniseriate rounded pits with oval apertures are distributed on radial tracheidal walls separately. Cell walls of rays are homogeneous and smooth. Rays are 1–10 cells high in tangential section. Cross‐field pits are cupressoid. There are 1–4 bordered pits with slit‐like to oval apertures in each cross‐field. Based on the anatomical features of the pith and xylems, it is proposed that the new stem has a coniferous affinity. The new fossil stem adds to the knowledge of vascular plant diversity close to the Permian–Triassic boundary. [ABSTRACT FROM AUTHOR]

Since the 1990s, the idea that water should be treated as an economic good has become a widely acclaimed but also disputed principle. In Xinjiang, a dry region in north-west China, the idea has been translated into government water management policies and practices. Based on investigations in the Kaidu-Kongque River Basin, this paper describes how the idea is interpreted in concrete water fee policies and practices in local water management in irrigation agriculture, and discusses what problems exist in current water fee collection practices and expenditure, as well as in water management in irrigation agriculture. The main argument is that water management is deeply tied to the political, social and economic conditions of the state, and water pricing is part of the complex, diverse and changing social reality. In the study area, the interpretation of treating water as an economic good has not contributed to a fairer and more efficient use of scarce water resources, but rather it has been applied to achieve other political and economic goals as well as to strengthen a powerful and rapidly growing bureaucracy. [ABSTRACT FROM AUTHOR]

In this study, an innovative MODIS fractional snow cover (SCF) data assimilation (DA) prototype framework that invokes machine learning (ML) techniques and Common land model (CoLM) is proposed to improve the estimation of the snow depth (SD) and the SCF. To validate our new framework, we analyzed two snow seasons from 2013 to 2015 at 46 stations in Northern Xinjiang in China. We developed 12 SCF DA schemes that represent different DA methods (direct insertion (DI) and Ensemble Kalman Filter (EnKF)), observational data (original data and gap‐filled MODIS SCF data), and observation operators (five new snow depletion curves (SDCs) defined using traditional multivariate nonlinear regression and four ML methods). While improving the frequency of the SCF observations in the DI‐based DA scheme only resulted in a marginal improvement in the snow estimates, by adding new SDCs fitted by ML techniques (e.g., deep belief network), and the gap‐filled MODIS SCF data to the EnKF‐based DA scheme, we were able to reduce model structural uncertainties of CoLM and achieve marked improvement in the accuracy of the snow estimates (RMSE = 5.92 cm, mean bias error = −1.94 cm, and average degree of improvement = 32.18% for SD estimates and RMSE = 15. 79%, mean bias error = −1.21%, and average degree of improvement = 47.95% for SCF estimates). Our results demonstrate the feasibility of improving snow estimates by combining the ML techniques with physically based snowpack model in a SCF DA framework. Key Points: An innovative MODIS fractional snow cover assimilation framework invokes machine learning techniques and Common Land Model is proposedFive new snow depletion curves (SDCs) are defined by using multiple nonlinear regression and four machine learning techniquesNew SDCs functions as both the improved parameterization scheme of Common Land Model and the observation operator of assimilation frame [ABSTRACT FROM AUTHOR]

Several hundred meteorites with a total mass of over 100 kg were collected as the Alatage Mountain (AM) strewn field located in the Kumtag desert, Xinjiang Province, China. Twelve AM meteorites were studied in this work. Petrography, mineralogy, bulk chemistry, bulk oxygen isotopic compositions, and light noble gas concentrations and isotopic compositions were determined for all or for a selection of the meteorites. The studied meteorites are L‐chondrites that suffered a very strong impact; impact melt veins and melt pockets are widely distributed. More than 50% of the troilite exists in the form of blebs and veins in olivine and pyroxene. Some of these meteorites are impact melt recrystallized rocks (e.g., AM 037). The strong impact caused the decomposition of troilite, which led in AM 034 to the sulfidization reaction of olivine. The metal in most meteorites is almost completely altered, and the troilite has been significantly oxidized. Weathering resulted in the depletion of Mg, Fe, Co, and Ni, and the enrichment of Sr, Ba, Pb, and U in these meteorites. The cosmic ray exposure (CRE) ages measured for these specimens range between 6.2 ± 1.9 Ma and 9.0 ± 2.7 Ma, depending on the cosmogenic nuclide used. The average CRE age is 7.6 ± 1.3 Ma. Both 4He and 40Ar gas retention ages indicate that the strong impact which caused the shock effects occurred about 320 Ma ago. [ABSTRACT FROM AUTHOR]

Genetic polymorphisms of human leucocyte antigen (HLA)‐DRB1, ‐DQA1 and ‐DQB1 among four main ethnic groups including Han (n = 70), Uyghur (n = 71), Kazakh (n = 52) and Hui (n = 40) subjects from Xinjiang Uyghur Autonomous Region were investigated using a polymerase chain reaction—sequence‐based typing (PCR‐SBT). In total, 32 HLA‐DRB1 alleles, eight HLA‐DQA1 alleles and 14 HLA‐DQB1 alleles were identified. The most predominant HLA‐DRB1, ‐DQA1 and ‐DQB1 alleles were DRB1*15:01 (12.50%), DQA1*01:02 (21.43%) and DQB1*03:01 (19.29%) in Han; DRB1*07:01 (18.48%), DQA1*05:01/03/05 (24.65%) and DQB1*02:01/02 (31.69%) in Uyghur; and DRB1*13:01 (13.64%), DQA1*05:01/03/05 (28.85%) and DQB1*02:01/02 (27.88%) in Kazakh, respectively. In Hui, DRB1*07:01, DRB1*11:01 and DRB1*14:01 were the most dominant alleles with the same frequency of 11.8%, while the predominant DQA1 and DQB1 alleles were DQA1*03:01/02/03 (23.75%) and DQB1*02:01/02 (16.25%), respectively. In addition, the most common two‐locus haplotypes were DQA1*05:01/03/5‐DQB1*03:01 (10.0%) in Han; DQA1*02:01‐DQB1*02:01/02 (18.31%) in Uyghur; DQA1*05:01/03/05‐DQB1*02:01/02 (15.38%) in Kazakh; and DQA1*03:01/02/03‐DQB1*03:03 (11.25%) in Hui. The phylogenetic dendrograms constructed based on the allele frequencies of HLA‐DRB1, ‐DQA1 and ‐DQB1 in 13 populations (e.g. Asian, Central Asian and European) revealed that the Han and Hui populations were clustered together and closest to Han population from China, while the Kazakh and Uyghur populations were closest to each other and two ethnic groups were clustered together with Central Asian and European populations. [ABSTRACT FROM AUTHOR]

The Meiling Cu‐polymetallic deposit is located in the Kalatag Cu metallogenic belt of the East Tianshan, Xinjiang, NW China. Multiple‐stage hydrothermal activities have resulted in the silicification, chlorite alteration and sericite alteration in this deposit. At least three mineralization stages are recorded: (a) a phase comprising quartz–pyrite veining, (b) a quartz–chalcopyrite–pyrite–sphalerite phase and (c) a quartz–calcite phase, respectively. LA–ICP–MS zircon U–Pb dating yielded 302 ± 2.1 Ma for an ore‐bearing quartz porphyry and 296 ± 3.2 Ma for a post‐mineralization diorite porphyry dyke, respectively, indicating that the copper mineralization took place during the Late Carboniferous period (302–296 Ma). Fluid evolution during the three stages of mineralization was determined by a detailed fluid inclusion study: (a) Stage I fluids were trapped under two‐phase conditions, as evidenced by the coexistence of vapour‐rich (type II) inclusions (Th = 183–242°C, average salinity = 4.8 wt% NaCl equiv.), liquid‐rich (type I) inclusions (Th = 171–259°C, average salinity = 5.3 wt% NaCl equiv.), and daughter‐bearing (type III) inclusions (Th = 192–208°C, average salinity = 8.6 wt% NaCl equiv.). (b) Stage II fluid inclusions in quartz were also trapped under two‐phase conditions (boiling), as identified by the coexistence of V‐ and L‐type fluid inclusions; L‐type inclusions Th between 136 and 218°C (average = 189°C), with salinities of 2.2–7.6 wt% NaCl equiv. (average = 3.8 wt% NaCl equiv.). V‐type inclusions homogenized temperatures between 153 and 226°C (average = 192°C), with salinities of 2.4–6.7 wt% NaCl equiv. (average = 3.5 wt% NaCl equiv.). (c) Stage III fluids are represented by inclusions in barren quartz–carbonate veinlets, characterized by homogenization temperatures ranging from 98 to 177°C (average = 135°C) and salinities between 0.5 and 3.2 wt% NaCl equiv. (average = 1.9 wt% NaCl equiv.). The initial hydrothermal fluids are characterized by low–intermediate temperature, low‐salinity and near‐neutral pH condition, belonging to a H2O–NaCl bearing hydrothermal system. The mineralization of the Meiling deposit occurred at a shallow crustal level (~0.5 km), and the decrease of temperature was likely an important factor responsible for metal accumulation and deposition in the subvolcanic hydrothermal system. [ABSTRACT FROM AUTHOR]

The article focuses on the Uyghur Muslims community in China's autonomous territory of Xinjiang. It discusses the terrorists attacks in Xinjiang as inspired by the Islamist organizations Taliban and Al-Qaeda. It looks at the possibility of Palestinization of the Uyghur conflict as reflected through the book "My West China: Your East Turkestan" by Chinese dissident Wang Lixiong due to the policy of repression, restriction, and investment by the People's Republic of China (PRC) in 1949.

The article focuses on the wilt disease of Amygdalus communis caused by the fungus Verticillium dahliae in the Xinjiang municipality in China. The inclusion of wilts of leaves and twigs, and the brownish discoloration of vascular tissues characterized the disease. A verticillium sp. was isolated from the woody part of diseased branches on the potato dextrose agar (PDA) producing dark colonies. Verticillium dahliae was identified based on the morphological characteristics obtained. The fungus was previously recorded in the Xinjiang municipality and other provinces in china that infects many plants, but the V. dahliae associated with wilt of A. communis was first reported.

The article focuses on the Hop stunt viroid (HSVd) which is recently observed from hop in Xinjiang, China. Its previous detection in grapevine, peach, plum, apricot and citrus in China has led to the study of its distribution. Along the study, extracted RNA from the hop leaf samples of different varieties that were gathered from commercial hop field in Changji districts of Xinjiang, China, were subjected to dot blot hybridization. The result of the study is discussed. It is noted that future investigation will focus on clarifying whether the varied infection rate of the hop leaf samples are correlated with possible levels of resistance.