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A full rollout of COVID-19 vaccination offers the most promising prospect of bringing the pandemic to an end. This study aimed to compare the coverage, safety, and confidence of COVID-19 vaccination between patients with Parkinson's disease (PD) and healthy individuals so as to give suggestions for future immunization programs. A web-based, nationwide, multicenter survey was carried out in China from 2021 to 2022. The age and sex-standardized vaccination rate was calculated. Multivariate stepwise logistic regression models were used to estimate the influencing factors of vaccination status. We also investigated vaccination safety, willingness, confidence, and reasons for hesitancy with some ad hoc questions. A total of 962 PD patients and 1208 healthy individuals participated in this survey with a vaccination rate of 71.1% vs 94.4% respectively. PD patients living in first-tier cities, with comorbidities, experiencing unstable PD with a longer course and levodopa use were less likely to get vaccinated, while healthy individuals living in first-tier cities and feeling physically poor exhibited a lower vaccination rate. For PD patients, concern about the adverse impact on existing illness and disagreement from doctors were the most common reasons for vaccination hesitancy. Whereas, no evidence was present that they experienced any local or systematic adverse events more frequently or seriously than healthy individuals, or their state of PD and comorbidities was seriously exacerbated after vaccination. A prominent transition from a little concerned to unconcerned about the security and efficacy of vaccines was evident among both two populations from pre-vaccination to post-vaccination. The COVID-19 vaccination rate was remarkably lower in PD patients than healthy individuals in China. The approved vaccines have shown an acceptable safety profile. Our findings would offer a reference to guide future clinical decision-making of COVID-19 vaccination and improve the immunization management of PD patients. [ABSTRACT FROM AUTHOR]

Abstract: The diurnal atmospheric phosphine (PH3) concentrations and fluxes at the water–air interface in Lake Taihu were reported. The results showed that the PH3 flux at the water–air interface ranged from −69.9±29.7 to 121±42ngm−2 h−1, with a mean flux of 14.4±22.5ngm−2 h−1. The fluxes were both negative and positive during the diurnal period, indicating that the lake can act as a sink and a source of PH3. In addition, the PH3 fluxes were positively correlated with water temperature, total soluble phosphorus and soluble reactive phosphorus, while they were negatively correlated with water redox potential. A similar diurnal variation curve of atmospheric PH3 concentrations was observed during all four seasons, with the maximum level occurring in early morning and the minimum appearing around midday. These findings suggest that light plays an important role in the elimination of atmospheric PH3. A significant positive correlation was also found between air temperature and atmospheric PH3 concentration. The mean flux of PH3 in Lake Taihu was higher than in other reported wetlands, with an estimated annual emission of PH3 to the atmosphere of 2.94×105 gy−1. [ABSTRACT FROM AUTHOR]

[Display omitted] • (1) Trachydacites have zircon U-Pb ages of 116 Ma and were coeval with the most extensive thinning of the North China Craton. • (2) 116 Ma trachydacites were related to subduction of Yangtze Craton and Paleo-Pacific plate. • (3) The mantle source underneath the southeastern North China Craton was modified by the subduction of the Yangtze Craton. The North China Craton has witnessed a large-scale lithospheric thinning event in the Mesozoic. The volcanic rocks of the Qingshan Group formed during the destruction of the North China Craton, therefore retaining important information to the deep processes in this region. Zircon U-Pb dating and geochemical analyses have been carried out on volcanic rocks of the Qingshan Group collected from southeastern margin of the Jiaolai Basin. In combination with previously published data on the volcanic rocks of the Qingshan Group, the newly acquired data show that: (1) the volcanic rocks of Qingshan Group in Mashan have SiO 2 content of 62.82 ∼ 66.3 wt% and total alkali content (K 2 O + Na 2 O) of 7.64 ∼ 9.34 wt%. According to TAS diagram, they belong to trachydacite which experienced strong fractionation between LREEs and HREEs with depletion of HFSEs and enrichment of LILEs. (2) The crystallization age of trachydacite in Mashan is 116.4 ± 2.3 Ma (MSWD = 1.9, n = 9). The magma originated from the partial melting of the ancient lower crust and the enriched lithospheric mantle metasomatized by the fluids/melts released from the subducted slab of the Yangtze Craton. (3) The formation age of magmatic rocks in western Shandong is generally earlier than that in eastern Shandong, while the lower crust delamination in western Shandong preceded that in eastern Shandong. The occurrence of magmatism in eastern Shandong is probably attributed to the delamination process in western Shandong as well as the ongoing tectonic activities along the Tan-Lu fault zone. The lithospheric thinning of the North China Craton was mainly controlled by the change of the subduction angle of the Paleo-Pacific plate, and is probably influenced by the continuous activity of the Tan-Lu fault zone in eastern Shandong. [ABSTRACT FROM AUTHOR]

Important biogeochemical processes occur in sediments at fine scales. Sampling techniques capable of yielding information with high resolution are therefore needed to investigate chemical distributions and fluxes and to elucidate key processes affecting chemical fates. In this study, a high-resolution diffusive gradients in thin-films (DGT) technique was systematically developed and tested in a controlled sediment system to measure organic contaminants, antibiotics, for the first time. The DGT probe was used to resolve compound distributions at the mm scale. It also reflected the fluxes from the sediment pore-water and remobilization from the solid phase, providing more dynamic information. Through the fine scale detection, a reduction of re-supply was observed over time, which was concentration and location dependent. Compared to the Rhizon sampling method, antibiotic concentrations obtained by DGT probes were less than the pore-water concentrations, as DGT measures the labile fraction of the compounds. The DGT probe was also tested on an intact sediment core sampled from a lake in China and used to measure the distribution of labile antibiotics with depth in the core at the mm scale. The abuse of antibiotics and widespread of their residues influences the ecosystem, induces the generation of super-bacteria, and finally poses threat to human health. Sediments adsorbs pollutants from the aquatic environment, while may also release them back to the environment. We systematically developed DGT probe approach for measuring antibiotics in sediment in situ in high resolving power, it provides information at fine scale to help us investigate biogeochemical processes take place in sediment and sediment-water interface. [Display omitted] • Developed a new in situ high resolution sampling probe for studying antibiotics. • Resolving power reached the mm scale, better than conventional methods. • Vertical distribution of antibiotics in sediments and their transport were determined. • Antibiotics were detected in an intact sediment core using DGT probe. [ABSTRACT FROM AUTHOR]

Satellite autonomous systems are employed to address complex space applications through onboard data processing and mission planning. To take advantage of onboard autonomous systems, rapid onboard satellite visibility predictions are necessary for certain decision-making missions, including Earth observation resource allocation and satellite data transmission. We consider this visibility prediction process as a roots-finding problem for a multiple hump function, and design a metamodeling-based framework with a self-adaptive interpolation method. Metamodels are developed as surrogates for visibility prediction functions to reduce expensive computational costs. Our proposed framework has a broad range of applications for all orbital types and orbit propagators. We conduct the experiments using different metamodeling techniques, radial basis functions, Kriging, and support vector regression based upon real China's satellites. Numerical simulations indicate that the proposed framework outperforms existing interpolation methods, efficiently reducing the onboard computational cost. [ABSTRACT FROM AUTHOR]

• Two types of homogenites are found in the Shulu Sag based on sedimentary characteristics. • Earthquakes are the most reasonable triggers of homogenite formation. • Seismic shaking and basin morphology control the formation of homogenites. Homogenites are homogeneous and structureless, fine-grained rocks. They have been studied extensively in marine settings and are typically interpreted as being related to catastrophic events such as earthquakes. However, studies on lacustrine homogenite-like rocks are limited. New core data from the Shulu Sag in China reveal that thick massive calcilutites exist in the lower Shahejie 3 Formation, which formed during the middle Eocene rifting stage. Based on petrographic, geochemical, and mineralogical data, these massive calcilutites are interpreted as homogenites and grouped into two types. Type A homogenite is composed of intrabasinal materials characterized by high calcite, total organic carbon (TOC) content, and δ13C value. Type A homogenite has two facies successions, the first of which is characterized by homogeneous appearance capped by an erosional interface and the second is characterized by repeated massive-laminated calcilutite successions. Type B homogenite contains abundant allochthonous materials displaying relatively high dolomite content and low calcite, TOC, and δ13C content. Type B homogenite represents the topmost finer portion of a graded megabed which includes, from base to top, grain supported carbonate conglomerates, slumped deformed portions, and debrites. The whole unit can be considered as a megaturbidite. Earthquakes are the most reasonable triggers of homogenite formation in the Shulu Sag. Type A homogenites are thought to be derived by fluidification, resuspension, and decantation of lacustrine fines due to shock waves generated by an earthquake. Type B homogenites might be deposits of distal turbidity currents and turbid clouds transformed from other gravity flows. The results of this study provide a better understanding of the formation of homogenites caused by earthquakes in a confined lacustrine basin. [ABSTRACT FROM AUTHOR]

• Internal P loading in the diversion input shallow Lake Hengshui was studied. • High water P concentration was mainly regulated by the high internal P loading. • Littoral wetland showed higher sedimentation and P release than open water areas. • Detritus burial, coprecipitation, and deposition accelerate P retention in wetlands. • Fe-P dominated the internal P release in the lake, accompanied by Org-P. Diversion input lakes usually have a low catchment area/lake area ratio and pulsing pollution input. Various pollutants might accumulate in the lake continuously owing to the concentration effect under high evaporation but low precipitation over the entire area, typically for sedimentary cyclic elements such as phosphorus (P). However, the detailed transportation, sedimentation, and internal release mechanisms of P in the diversion input lakes remain unclear. This study conducted a year-long investigation of the littoral wetlands and open water areas of the shallow Lake Hengshui in the semi-humid region of North China. Results revealed that the average total P concentrations in the water and surficial sediment reached as high as 0.202 mg L−1 and 878.21 mg kg−1 in summer. The high water P levels in the lake were mainly regulated by the high internal P loading during summer and autumn, with the internal P loading being approximately nine times the external P loading. The littoral wetland area serves as a higher sedimentation sink and release source of P than the open water area. The concentrated P was continuously transported to the littoral wetland area through detritus burial, coprecipitation, and deposition of suspended particles. The release of P was mainly controlled by the dissolution of redox-sensitive Fe-P and Org-P at high temperatures and organic matter mineralization in the sediment, accompanied by the potential release capacity of apatite P (Ca-P). Future management of eutrophication and P levels in similar diversion input lakes should pay more attention to the high internal P loading in the sediment and the differentiated sedimentation and release processes in the littoral wetland and open water areas. [Display omitted] [ABSTRACT FROM AUTHOR]

In the Upper Ediacaran Dengying Formation of the Sichuan Basin, the presence of abundant, well-preserved microbial carbonates provides a unique opportunity to study Precambrian paleoceanography and microbial carbonate origins. Particularly, the underexplored coated grain dolostones of this formation, characterized by distinct microbially induced fabrics and intragranular dissolution, offer crucial insights for understanding late Ediacaran microbial mineralization and diagenetic sequences. Utilizing selected typical samples, we conducted detailed petrographic and geochemical analyses, revealing a dynamic interplay between microbial processes and sedimentary dynamics. We observe the coexistence of constructive micrite envelopes with microbially induced fabrics such as clots and laminations, highlighting microbial biomineralization's key role in fabric formation. The sedimentary dynamics critically determines the formation processes of the coated grains: low-energy settings foster grain agglomeration and consolidation through clot precipitation between grains, while high-energy settings favor smaller grains binding to microbial mats. Geochemically, micrite envelopes play an essential role in preserving distinct rare earth element (REE) signatures. The weak negative Ce anomalies and positive Eu anomalies within these envelopes point to a suboxic to anoxic depositional environment, directly indicative of the microenvironmental conditions conducive to microbial mineralization processes. Furthermore, our study sheds light on the structural evolution of coated grains with hollow nuclei, proposing that their internal pore formations are influenced by both mineral instability and selective dissolution by meteoric freshwater. These findings not only provide fresh insights into complex diagenetic processes in the Dengying Formation but also substantially advance our understanding of early microbial life and environmental adaptations during the Precambrian. • Revealed the relationship between micrite envelopes and microbially induced fabrics • Proposed a novel formation mechanism for coated grain dolostone in the Dengying Fm. • Investigated the diverse environmental responses of microbiolite fabrics • Established micrite envelopes as dependable records of seawater REE compositions [ABSTRACT FROM AUTHOR]

A new method for the determination of 26 legacy and emerging per- and polyfluoroalkyl substances (PFASs) in marine sediment pore water was developed using online solid phase extraction coupled with liquid chromatography-tandem mass spectrometry. The proposed method requires only about 1 mL of pore water samples. Satisfactory recoveries of most target PFASs (83.55–125.30 %) were achieved, with good precision (RSD of 1.09–16.53 %), linearity (R 2 ≥ 0.990), and sensitivity (MDLs: 0.05 ng/L–5.00 ng/L for most PFASs). Subsequently, the method was applied to determine PFASs in the sediment pore water of five mariculture bays in the Bohai and Yellow Seas of China for the first time. Fifteen PFASs were detected with total concentrations ranging from 150.23 ng/L to 1838.48 ng/L (mean = 636.80 ng/L). The ∑PFASs and PFOA concentrations in sediment pore water were remarkably higher than those in surface seawater (tens of ng/L), indicating that the potential toxic effect of PFASs on benthic organisms may be underestimated. PFPeA was mainly distributed in pore water, and the partition of PFHpA (50.99 %) and PFOA (49.01 %) was almost equal in the solid and liquid phases. The proportions of all other PFASs partitioned in marine sediments were significantly higher than those in pore water. [Display omitted] • A convenient method for the detection of PFASs in marine sediment pore water was developed. • Only about 1 mL of actual sediment pore water is needed to determine various PFASs. • High levels of PFASs were detected in pore water from five mariculture bays of China. • Different PFASs exhibit varying partitioning behaviors at the sediment–pore water interface. • Great attention should be paid to PFASs in the sediment pore water of mariculture areas. [ABSTRACT FROM AUTHOR]

• A watershed P-SFA model with comprehensive subsystems and detailed P flows was developed. • The P utilization patterns of cultivation and livestock farming influence the P cycling. • The average annual growth rate of P emissions is 2.41%, from 1.67 × 104 t to 8.73 × 104 t. Understanding the historical patterns of phosphorus (P) cycling is essential for sustainable P management and eutrophication mitigation in watersheds. Currently, there is a lack of long-term watershed-scale models that analyze the flow of P substances and quantify the socioeconomic patterns of P flow. This study adopted a watershed perspective and incorporated crucial economic and social subsystems related to P production, consumption, and emissions throughout the entire life cycle. Based on this approach, a bottom-up watershed P flow analysis model was developed to quantify the P cycle for the first time in the Poyang Lake watershed from 1950 to 2020 and to explore the driving factors that influence its strength by analyzing multi-year P flow results. In general, the P cycle in the Poyang Lake watershed was no longer a naturally dominated cycle but significantly influenced by human activities during the flow dynamics between 1950 and 2015. Agricultural intensification and expansion of large-scale livestock farming continue to enhance the P flow in the study area. Fertilizer P inputs from cultivation account for approximately 60% of the total inputs to farming systems, but phosphate fertilizer utilization continues to decline. Feed P inputs have continued to increase since 2007. The expansion of large-scale farming and the demand for urbanization are the main factors leading to changes in feed P input patterns. The P utilization rate for livestock farming (PUEa) is progressively higher than international levels, with PUEa increasing from 0.64% (1950) to 9.7% (2020). Additionally, per capita food P consumption in the watershed increased from 0.67 kg to 0.80 kg between 1950 and 2020. The anthropogenic P emissions have increased from 1.67 × 104 t (1950) to 8.73 × 104 t (2020), with an average annual growth rate of 2.41%. Watershed-wide P pollution emissions have increased by more than five-fold. Population growth and agricultural development are important drivers of structural changes in P flows in the study area, and they induce changes in social conditions, including agricultural production, dietary structure, and consumption levels, further dominating the cyclic patterns of P use, discharge, and recycling. This study provides a broader and applicable P flow model to measure the characteristics of the P cycle throughout the watershed social system as well as provides methodological support and policy insights for large lakes in rapidly developing areas or countries to easily present P flow structures and sustainably manage P resources. [Display omitted] [ABSTRACT FROM AUTHOR]

Hybrid unconventional systems are composed of juxtaposed organic-rich and organic-lean intervals. Organic matter enrichment, hydrocarbon migration, and the spatial relationship of source rocks and reservoirs have important influences on differential hydrocarbon accumulation within the system. Most studies have ignored the complexity of hydrocarbon accumulation in unconventional oil reservoirs. A typical hybrid lithology system with a combination of marlstone and rudstone has been discovered in the lower part of the third member of the Shahejie Formation of the Shulu Sag, Bohai Bay Basin, Northern China. The basin showcases a strong heterogeneity in unconventional hydrocarbon production and is an appropriate case to study hydrocarbon accumulation within hybrid unconventional systems. However, relevant work in the study area was scarce. A study of the mechanisms of organic matter enrichment and hydrocarbon accumulation was required to understand the heterogeneity of the oil reservoirs. Nine units in ascending order, namely I L , I U , II L , II U , III L , III U , IV, V L , and V U , were proposed in this study. A detailed geochemical analysis was carried out to distinguish the organic matter sources and preservation conditions among the different units, and assess the migration patterns of the hydrocarbons. The results show that Unit II L has the highest total organic carbon (TOC) content. Unit II L has a higher quantity of aquatic sourced organic matter, with relatively high abundance of short chain n -alkanes, C 27 /C 29 sterane, and 4-methyl steranes. Based on the low ratios of pristane to phytane, the varve-like lamination structure of the lithology and suitable salinity, we can speculate that good organic matter preservation conditions existed in Unit II L. Maturity of the source rocks increases with depth. Biomarkers indicate that hydrocarbons within the marlstones were retained in situ, whereas hydrocarbons within the rudstones were derived from source rocks via short- or long-distance migrations. Fractures can act as effective pathways for hydrocarbon migration. Organic matter sources, preservation conditions, maturity, and hydrocarbon migration ways jointly controlled the formation of oil reservoirs in the Shulu Sag. The results of this study provide a better understanding of organic matter enrichment and hydrocarbon accumulation and guide further exploration in the basin. • Aquatic organic matter has the best hydrocarbon generation potential. • Three hydrocarbon accumulation pathways exist in the Shulu Sag. • Biomarkers related to thermal maturity can indicate hydrocarbon migration. • Source rock quality and migration ways influence oil reservoir heterogeneity. • Mature, high TOC source rocks can form high-quality oil reservoirs. [ABSTRACT FROM AUTHOR]

Understanding various biogeochemical processes, especially in eutrophic sediments, necessitates fine-scale phosphorus (P) measurements in pore waters. To the best of our knowledge, the fine-scale distributions of P across the sediment profiles of Lake Nansi have rarely been investigated. Herein we evaluated the dynamic distributions of labile P and Fe across the sediment-water interface (SWI) of Lake Nansi at two-dimensional (2D) and sub-millimeter resolution, using well-established colorimetric diffusive gradients in thin films (DGT) methodology. The concentrations of labile P in all investigated sediment profiles exhibited strong spatial variations, ranging from 0 to 1.50 mg/L with a considerable number of hotspots. Lake Nanyang (0.55 ± 0.21 mg/L) had the highest mean concentration of labile P, followed by Lake Dushan (0.38 ± 0.19 mg/L), Lake Weishan (0.28 ± 0.21 mg/L), and Lake Zhaoyang (0.18 ± 0.09 mg/L). The highest concentrations of labile P were always detected in Lake Dushan, which had been subjected to excessive exogenous P pollution. The co-distributions of labile P and Fe in the majority of the sediment of Lake Nansi confirmed highly positive correlations (P < 0.01), suggesting that the mobility of labile P throughout the SWI was likely governed by iron redox processes. The apparent diffusion fluxes of P across the SWI ranged from −7.7 to 33.6 μg/m2·d, with a mean value of 5.26 ± 7.80 μg/m2·d. Positive apparent fluxes for labile P were recorded in most sediment cores, demonstrating the strong upward mobility of P from the sediment to the overlying water. Our results provided accurate and extensive information regarding the micro-distribution and dynamic exchange of labile P across the SWI. This allows for a better understanding of eutrophication processes and the implementation of P management strategies in Lake Nansi. [Display omitted] • The spatial variation and mobility of P in Lake Nansi were characterized using DGT. • 2D, heterogeneously micro-distribution of P in the sediment profile was observed. • Labile P had a northward and downward spatial gradient, related to human activity. • The mobility of P across the SWI was likely governed by iron redox processes. • Fine-scale measurement improves the accuracy P-cycle depiction for eutrophic lake. [ABSTRACT FROM AUTHOR]

Silk, as one of the representative artifacts of China, profoundly affects the communication between eastern and western civilizations, and dyes, as the color support of silks, reflected crucial historical, cultural and technological information. Surface enhanced Raman spectroscopy (SERS) characterized by vibrational information has been extensively employed in dye analysis. However, since natural plants with complex coloring compositions in ancient China were broadly applied in dying textiles, the existing SERS methods often misinterpret results in dye analysis. Besides, semi-quantification of each component was of great difficulty by SERS, limiting the exquisite comparative analyses of different historical samples. For the first time, a dual-mode strategy combining SERS with high mass resolution MALDI FTICR MS was developed in virtue of core-shell silver nanoparticles (AgNPs@PDA), which realized the precise identification and semi-quantification of complex dye mixtures, thus significantly improving the accuracy and applicability of traditional SERS method. Four typical dye components (alizarin, purpurin, berberine and indigo) have been identified and semi-quantified in unearthed dyed silks from Tang Dynasty based on the method. More interestingly, multiple dye components with different contents and their ratio could be precisely determined, which might help in further investigating their dyeing techniques. This dual-mode strategy represents a promising tool for providing solid support for cognition, evaluation and restoration of textile objects in museums and conservation centers. [Display omitted] • Core-shell AgNPs were used as both SERS enhancement reagent and MALDI matrix. • Multiple types of typical dyes were investigated through the dual-mode analysis. • Dye mixtures can be identified and semi-quantified based on the dual-mode strategy. • Four typical dye components were detected in ancient dyed silks from Tang Dynasty. [ABSTRACT FROM AUTHOR]

Abstract: For centuries, Patrinia heterophylla had been used in China to treat many diseases including tumor. Triterpenes has been identified as the major active constituents in Patrinia heterophylla. To elucidate the antitumor mechanism of triterpenes from Patrinia heterophylla1 (TPH), a proteomic analysis is carried out with TPH treatment in K562 cells. The total proteins extracted from TPH treated K562 cells are analyzed by two dimensional gel electrophoresis (2-DE) and compared with those untreated K562 cells. Mass spectrometry is applied to identify the differentially expressed proteins. Twenty-three differentially expressed significant proteins are discovered. Eight proteins are later identified by mass spectrometry (MALDI-TOF-MS) and Mascot software. Among them, four proteins are up-regulated (Aldolase A, Glyceraldehyde-3-phosphate dehydrogenase, Flavin reductase and Hemoglobin subunit) and four proteins were down-regulated (Heat-shock protein 90 〈Alpha〉 (HSP90-〈Alpha〉), Eukaryotic translation initiation factor 5A, Moesin, tublin) by TPH treatment in K562 cells. The identified proteins are associated with energy metabolism, oxidative stress, apoptosis, signal transduction, differential induction, and protein biosynthesis. These findings might provide valuable insights into the antitumor mechanism of TPH in K562 cells. [Copyright &y& Elsevier]

The Shanganning Carbonate Platform (SCP) of the North China Craton (NCC) was located in the Trade Winds belt during the Cambrian, which influenced its facies development. In recent years, numerous drillcores have been recovered from these units, but the depositional environments and facies architecture of this large (~2.0 × 105 km2) carbonate platform system have not yet been reported in detail. In this study, we integrate sedimentological and magnetic fabric data collected from outcrops and drillcores in order to document variation in microfacies and facies associations within the SCP, to infer paleowind directions and constrain the paleogeographic location of the SCP, and to evaluate eolian controls on platform development. This analysis documented numerous carbonate microfacies belonging to six fabric types (mudstone, wackestone, packstone, grainstone, framestone, and dolostone) along with rarer siliciclastic sediments. These microfacies belong to facies associations representing tidal flat, open platform, platform margin, slope, and deep basinal depositional environments. Anisotropy of magnetic susceptibility (AMS) measurements yielded mean paleocurrent directions for the Early, Middle, and Late Cambrian of 114°, 63°, and 83° (± ~30°) from paleo-north, respectively, that were relatively consistent for 12 out of 13 platform-margin sites, all vectors being corrected for a post-Cambrian ~150° clockwise rotation of the NCC. These wind orientations are consistent with the SCP shifting from south of the paleo-Equator in the Early Cambrian to north of it by the Middle Cambrian. Paleo-Trade Winds influenced facies patterns across the platform, producing a distinct windward-leeward zonation. The windward margin is characterized by well-sorted oolitic grainstone, as well as (favositids) coral and (dasycladacean) algal-sponge framestone, and the leeward margin by poorly-sorted oolitic wackestone-grainstone and fine bioclastic sediments. The present study is innovative in 1) integrating microfacies and AMS analyses in order to establish paleowind patterns and influences on an ancient carbonate platform, 2) documenting windward-leeward variation in quantifiable sediment properties across the SCP, and 3) constraining the paleo-hemispheric location of the NCC during the Cambrian. • Analysis of microfacies and depositional environments of Cambrian in Ordos Basin • Quantitative measurements of sediment properties across the platform were documented. • Paleo-hemispheric location of North China Craton was constrained during Cambrian. • Paleo-Trade Winds influenced windward versus leeward facies zonation patterns. • An integrated methodology of magnetic anisotropy and standard petrographic data [ABSTRACT FROM AUTHOR]

The Qianjiang Depression is a typical Eocene hypersaline lake basin developing good source rocks in the Qianjiang Formation, which have recently been identified as a potential target for saline lacustrine shale oil exploration. Previous studies have only focused on estimates of source rock potential and reservoir quality. However, studies on organic matter enrichment mechanisms in evaporative environments are limited. Based on organic geochemical and mineralogical data, as well as sedimentological analyses, we researched the factors controlling differences in organic matter enrichment in the basin. The results show that total organic carbon (TOC) contents are closely associated with lithofacies with distinct variations. Three main lithofacies associations (LAs) were identified: (1) glauberite-rich LA1 with medium TOC; (2) carbonate-rich LA2 with high TOC; and (3) anhydrite-rich LA3 with low TOC. The distribution of biomarkers from 14 samples indicate both higher land plants and aquatic organisms were involved in the organic matter accumulations. Combining experimental results on gammacerane/C 30 hopane, extended tricyclic terpane ratio (ETR), Sr/Ba, V/Ni, and sedimentary characteristics, we analyzed the sedimentary environments of the three LAs. LA1 was deposited in a salinity stratified waterbody with strong evaporation, LA2 was deposited in a still, stratified deep waterbody, whereas LA3 was deposited in a disturbed, saline waterbody. Sedimentary environments not only controlled the formation of the lithofacies, but also influenced the organic matter sources and preservation. Relatively low salinity, strong anoxic condition without physical disturbance, appropriate nutritional terrigenous material inputs, and algal blooms produced the best organic matter enrichment in the saline lake system. • We studied a hypersaline lake rhythmite from the Qianjiang Formation, Hubei, China. • Saline lake environments influence organic matter accumulation. • Hypersalinity is unfavorable for organic matter enrichment. • ETR is a valid biomarker to assess redox conditions in saline lake sediments. • High lake levels with anoxic conditions favor organic matter accumulation. [ABSTRACT FROM AUTHOR]

The piedmont depression in the western Junggar Basin is a typical large-scale thrust belt rich in hydrocarbons, but there is still a debate whether its structural properties relate to a foreland basin. This controversy hinders the understanding of regional hydrocarbon plays, giving rise to this study. As a conclusion, we discovered that - it was a foreland basin in the Permian that accounted for the structural properties of the piedmont depression. The basin was generated by continuous thrusting of the Western Junggar Orogenic Belt against the Junggar–Tuha Plate. This occurred after the formation of the Western Junggar Orogenic Belt in the Carboniferous. The western basin in this study can be divided into five different zones moving from the Western Junggar Orogenic Belt to the internal plate, which are: the foreland thrust belt (the Ke–Bai and Wu–Xia thrust belts), the foreland depression (the western part of the Mahu Sag), the foreland slope (the eastern part of the Mahu Sag), the forebulge (the Dabasong Uplift), and the back-bulge basin (the Western Pen 1 Well Sag). Based on the characteristics of geological structure, and the sedimentary strata of the western Junggar Basin, the evolution of the basin was split into two distinctive stages: the Permian development stage and the Mesozoic–Cenozoic burial stage. Throughout the entire process three suites of hydrocarbon source rocks were developed, regional seal rocks, and four types of trap and reservoir assemblages. The western Junggar Basin should be considered as a typical petroliferous foreland basin. • The Permian Junggar Basin are typical of a foreland basin with five structure units. • The Basin evolution can be divided into foreland basin stage and burial stage. • The Junggar Basin could be regarded as a typical petroliferous foreland basin. [ABSTRACT FROM AUTHOR]

The Eocene lacustrine carbonates in the western Dongying Depression, Bohai Bay Basin were examined based on integrated analysis of 3D seismic data, cores, thin-sections, and geochemical testing. Seismic profiles and geomorphological mapping revealed a landmass-attached (semi-isolated) carbonate platform restricted by marginal syn-sedimentary faults and surrounded by three deep sags. 3D topographic analysis of the platform revealed six districts characterized by variable buried depths, topographic gradient, and fault combinations, including two flat-topped areas (PFW and SD; topographic gradient <4°) and four transitional zones above deep sags (P1, P2, S1, and S2; 4–10°). Eight lithofacies types were identified, forming five lithofacies associations: reef-shoal complex deposits, small bio-buildups, shoal-intershoal deposits, event flow deposits, and near-landmass mixed deposits. Well cross-sections revealed that facies distributions were closely associated with the geomorphological districts. Therefore, a geomorphology-dominated carbonate platform model was constructed, which highlighted the relationship of platform topography, hydrodynamic conditions, and facies distributions. The littoral facies is mainly composed of medium–high-energy deposits including reef-shoal and shoal sediments, which are mostly distributed in flat-topped areas. The sublittoral facies is dominated by low-to medium-energy deposits but influenced by storm activities, especially in the windward step-fault transitional zones. The profundal facies is positioned away from the platform marginal faults and joined with surrounding deep sags. Besides the regional geomorphology and its controlled hydrodynamic zones, the formation of such considerable lacustrine carbonates throughout the whole basin may have occurred because the global warming of late Eocene period induced sea transgression, which facilitated the development of lacustrine carbonates via marine-sourced reef-builders and biologically-induced carbonate precipitation. Furthermore, the East-Asian paleomonsoon climate influenced regional windfield may also have enhanced the prevailing southeast wind, which influenced the distribution of lithofacies and favorable reservoirs. Porosity-permeability analysis revealed that reservoir properties have a close relationship with geomorphology and lithofacies, thus geomorphology-associated facies prediction is essential for further hydrocarbon prospecting in this area. • A new geomorphology-dominated model was constructed to depict the detailed architecture of the lacustrine carbonate platform.. • The global-warming-induced sea transgression faciliated the development of lacustrine carbonates in the Dongying Depression Geomorphological districts of the carbonate platform controlled the distributions of lithofacies and their associations.. • Lacustrine carbonate reservoir properties were strongly controlled by geomorphology and lithofacies-caused heterogeneity. • Paleomonsoon-climate-enhanced regional windfield could cause local redistribution of carbonate deposits on the platform. [ABSTRACT FROM AUTHOR]

• Provenances of Permo-Triassic clastic rocks in eastern CAOB change from single to bidirectional. • The mixing of the Angaran and Cathaysian floras occurred during the Late Permian-Middle Triassic. • The PAO closed via a scissor-like closure model from west to east with bidirectional subduction. The mixture of the Cathaysian and Angaran floras signifies the evolution of the Paleo-Asian Ocean (PAO). In this study, we present new zircon U-Pb-Hf isotope analyses from the Jiefangcun Formation, Sidonggou Formation, Kedao Group, and Kaishantun Formation in the Yanbian area, NE China. The Kaishantun Formation contains the Kaishantun flora, which is dominated by the Cathaysian flora with a few Angaran elements. The Jiefangcun Formation is characterized by the Jiefangcun flora, which is dominated by the Angaran taxa and contains some Cathaysian elements. The ages of these strata are widely accepted as Permian. However, in this study, the youngest zircon ages of the rock samples from the Jiefangcun Formation, Kedao Group and Sidonggou Formation are 243–245 Ma. Only the Kaishantun Formation is assigned to the Late Permian. The Kaishantun Formation has age peaks at 758, 934, 1856, and 2493 Ma with negative ε Hf (t) values, and this formation is therefore mainly derived from the North China Craton (NCC). In contrast, the Kedao Group and Jiefangcun Formation have zircon age peaks at ~260, 338 and ~460 Ma with positive and negative ε Hf (t) values, at 800–1000 Ma with mostly positive ε Hf (t) values, and at ~1800 Ma with positive and negative ε Hf (t) values, which suggest bidirectional provenances, including the Jiamusi-Mongolia Block and the NCC. Thus, the mixing between the Angaran and Cathaysian floras occurred during the Late Permian-Middle Triassic, suggesting a scissor-like closure model of the PAO, and the Solonker suture zone extends eastward to the Yanbian area with bidirectional subduction of the PAO. [ABSTRACT FROM AUTHOR]