Primary Inclusions Research Articles

Measuring costly behavioral bias factors in portfolio management: a review

Various factor models extended by Jensen’s (J Financ 23:389–416, 1968) alpha have been used to measure the retail investors’ portfolio (under-) performance compared to the market portfolio. The previous studies tried to explain this anomaly in behavioral finance by examining retail investors’ cognitive biases that induce irrational trading behavior. While operationalizing these cognitive biases in trading is not trivial, researchers still have found measures to proxy for biases and prove their statistical and economic significance. However, these studies only focused on linking one or a subset of behavioral biases and their effect on portfolio performance. In addition, different measures of biases across studies complicate the comparability of results. Therefore, this paper provides a structured overview of the current state of the literature regarding behavioral biases and their measurements to design a behavioral factor model that should help to explain the performance alpha from a behavioral finance perspective. The paper presents an overview of 11 behavioral bias factors and 29 corresponding measurements to consider inputting in such a model. With an application-oriented focus, it is recommended to include the most researched bias factors in a factor model, which are also the most detrimental to portfolio performance, as well as to include the most frequently used and least complex measures, which results in the primary inclusion of the following eight behavioral bias factors: disposition effect, under-diversification, home bias, local bias, lottery stock preference, trend chasing, overtrading, and trade clustering.

Methane genesis within olivine-hosted fluid inclusions in dolomitic marble of the Hida Belt, Japan

Abiotic synthesis of hydrocarbon-bearing fluids during geological processes has a significant impact on the evolution of both the Earth's biosphere and the solid Earth. Aqueous alteration of ultramafic rocks, i.e., serpentinization, which forms serpentinite, is one of the geological processes generating abiotic methane (CH4). However, abiotic CH4 generation is not limited to the serpentinization of mafic and ultramafic lithologies. Metasedimentary dolomitic marble from the Hida Belt, Japan, is characterized by the presence of forsterite-rich olivine (Fo~89–93), and olivine crystals contain abundant fluid inclusions (<1 to 10 μm in size). Raman spectroscopic analyses of olivine-hosted fluid inclusions found that both primary and secondary fluid inclusions contain CH4, lizardite/chrysotile, and brucite. This indicates that micro-scale interactions between COH fluid and host olivine produced CH4 through the reduction of CO2 by H2 released during local serpentinization within inclusions. Our observation implies that the dolomitic marble has the potential to be a key lithology for the synthesis and storage of abiotic CH4 in a shallower crustal portion of orogenic belts.

Effect of long-term aging on the microstructure evolution and fracture mechanism of 9% Cr steels

The fracture toughness of pressure pipe steels is vital for their design and safe operation. Understanding the deterioration of the fracture toughness and the corresponding fracture mechanisms is instructive and meaningful for material selection and development. The elastic–plastic fracture toughness of 9% Cr steels aged at 873 K and 923 K from the initial state to 20000 h was investigated at ambient temperature and 873 K. The deterioration of the fracture toughness and the corresponding fracture mechanisms are discussed in detail. For 9% Cr steels, voids mainly initiated from primary inclusions such as silicides, sulfides, alumina and manganides in as-received state, while voids initiated from both primary inclusions and secondary particles such as the Laves phase after long-term aging. These voids grew and coalesced with neighboring voids and crack tips subsequently until ultimately fracture. After aging at 873 K, the fracture toughness values tested at 873 K decreased from the initial state to 3000 h and then increased to 10000 h. The peculiar deterioration of the fracture properties after 3000 h of aging at 873 K can be attributed to the high number density of Laves phase particles in the steels. It was found that the densely distributed hard Laves phase particles induced strain concentration at the interface between the Laves phase and the matrix under plane-strain tension condition and promoted nucleation of voids. It was suggested that the spatial distribution of the Laves phase played a significant role on the void formation. 9% Cr steels with a denser distribution of Laves phases brings about voids with shorter interspaces, which are more susceptible to coalesce into crack tip, resulting in lower fracture resistance. After aging at 923 K from 10000 h to 20000 h, the number density, size and volume fraction of precipitates, block size, misorientation angle and dislocation density remained almost constant. The slight increase in the fracture toughness from 10000 h to 20000 h can be mainly ascribed to the coarsening of the martensite lath in this stage.

Geothermometry of calcite spar at 10–50 °C

Carbonate geothermometry is a fundamental tool for quantitative assessment of the geothermal and geochemical evolution of diagenetic and hydrothermal systems, but it remains difficult to obtain accurate and precise formation temperatures of low-temperature calcite samples (below ~ 40 to 60 °C). Here, we apply three geothermometry methods (∆47-thermometry, nucleation-assisted fluid inclusion microthermometry—hereafter NA-FIM—and oxygen isotope thermometry) to slow-growing subaqueous calcite spar samples to cross-validate these methods down to 10 °C. Temperatures derived by NA-FIM and Δ47-thermometry agree within the 95% confidence interval, except for one sample. Regression analyses suggest that the real uncertainty of ∆47-thermometry exceeds the 1 SE analytical uncertainty and is around ± 6.6 °C for calcite spar that formed at 10–50 °C. The application of δ18O thermometry was limited to a few samples that contained sufficient primary fluid inclusions. It yielded broadly consistent results for two samples with two other geothermometers, and showed higher temperature for the third spar. We also found that calcite with steep rhombohedral morphologies is characteristic of low temperatures (11–13 °C), whereas blunt rhombohedra prevail in the 10–29 °C domain, and the scalenohedral habit dominates > 30 °C. This suggests that the calcite crystal morphology can be used to qualitatively distinguish between low- and higher-temperature calcite.

Effects of Cerium Content on the Nonmetallic Inclusions and Impact Toughness of Transformation‐Induced Plasticity Steel

The effects of Ce treatment on the inclusion evolution and impact toughness of as‐cast transformation‐induced plasticity (TRIP) steel are systematically investigated by scanning electron microscope (SEM) and impact toughness testing. The results reveal that in Fe‐2Mn‐1.5Al‐1Si‐0.2C steel without Ce, the primary inclusions consist of AlN, MnS, and Al2O3. After Ce addition, the inclusions evolve into Ce‐Al‐O, Ce2O2S, CeS, and Ce2O3 inclusions. The evolution of inclusions exhibits an initial reduction in both quantity and size with increasing Ce content, followed by a subsequent increase. In cases of excessive Ce content, there is an observable rise in the overall inclusion count, marked by the emergence of CeAs, CeP, and CeC2 inclusions. The segregation model suggests that P‐containing inclusions predominantly precipitate in the late solidification process, while As‐ and C‐containing inclusions form during the solid phase. When the Ce content reaches 0.0075 wt%, the minimum values of the number density and average diameter are 96.7 mm−2 and 1.6 μm, respectively. Furthermore, the influence of the size, morphology, quantity, and type of inclusions on the impact toughness are analyzed. The highest recorded impact energy is 6.8 J with a Ce content of 0.0075 wt%.

Analysis of the data in Jingwen Mao's paper on the stable isotopes (δDH2O, δ18OH2O, δ 34S) of the gold deposits in Jiaodong Peninsula, China

In 2008, Jingwen Mao published a paper on the stable isotopes of gold deposits in the Jiaodong Peninsula. The paper has a series of problems in obtaining δDH2O and δ18OH2O of ore-forming fluids and interpreting δ34S data. ① In order to obtain δDH2O and δ18OH2O data of ore-forming fluids, Jingwen Mao selected sericite (a total of 25 samples) as the target mineral. Sericite is not an independent mineral and has no fixed molecular formula. New research has shown that it is a fine-grained aggregate composed of muscovite, illite, and sodium mica (at least muscovite and sodium mica). The water content in sericite is very complicated, including structural water, interlayer water, fissure water, primary and secondary inclusion water. Jingwen Mao extracted water from sericite by crushing, and this mixed water cannot represent the ore-forming fluids. It is unreliable to determine the source of ore-forming fluids using δDH2O measured by this kind of mixed water. ② So far, no oxygen isotope fractionation coefficient relationship between sericite and water has been obtained, whether through theoretical calculation or experimental research. In order to calculate the δ18OH2O of ore-forming fluids by measuring the δ18O of sericite, Jingwen Mao used the oxygen isotope fractionation coefficient relationship between muscovite and water for calculation, which is completely wrong. ③ The data of δ18OH2O and δDH2O of ore-forming fluids obtained by Jingwen Mao using sericite are very different from the relevant data obtained by previous researchers using quartz as the target mineral (131 samples). Based on those unreliable data, Jingwen Mao believed that the ore-forming fluids came from the mixed source of crust and mantle, while the relevant data of previous researchers proved that the ore-forming fluids came from the products of atmospheric precipitation exchanging with Jiaodong Group metamorphic rocks under different temperatures and different W/R ratios. ④ For the relationship between the high or low δ 34S value of sulfide minerals and the large or small logfO2 value, Jingwen Mao's explanation is completely opposite to the research results of Ohmoto and Wang. Ohmoto believed that the two were negatively correlated, while Jingwen Mao believed that they were positively correlated. This is a common sense mistake.

Association between Cord Blood Haematocrit and Neonatal Outcome among Neonates of Diabetic Mothers: A Cohort Study

Introduction: The perinatal mortality rate of Neonates of Diabetic Mothers (NDMs) over the years showed a reducing trend. Polycythaemia is common in NDMs, and such neonates have a risk of hyperviscosity, renal vein thrombosis, cardiac failure, metabolic abnormalities, and necrotising enterocolitis. Aim: To assess the association between cord blood haematocrit and neonatal outcomes among NDMs. Materials and Methods:The present study was a cohort study that included 130 neonates, which was conducted at Amala Institute of Medical Sciences (AIMS), Thrissur, Kerala, India, from December 2019 to June 2021. The primary inclusion criteria were singleton neonates of Gestational Diabetic Mothers (GDM) (diabetes detected after 20 weeks of gestation) and Overt Diabetes Mellitus (ODM) defined under White’s classification (known to be diabetic before the onset of pregnancy or detected in the initial visits). The parameters assessed were the frequency of distribution of hypoglycaemia, hypocalcaemia, and hyperbilirubinemia among the neonates of DM. Statistical analysis was done using Fisher’s exact test and Student’s t-test. Results: Among the 130 neonates, the majority of the mothers had GDM 111 (85.4%) than ODM 19 (14.6%). The majority were delivered by normal vaginal delivery 67 (51.5%). 10 (7.7%) of NDMs had a birth weight &gt; 4000 g. Significant associations were noted between cord Packed Cell Volume (PCV) and the presence of hypoglycaemia (p-value=0.003), hypocalcaemia (p-value=0.0001), and Neonatal Hyperbilirubinemia (NNH) (p-value=0.0001) among NDMs. Conclusion: Hypoglycaemia, hyperbilirubinemia, and hypocalcaemia were common complications noted in NDMs.

Multilocus Sequence Analysis of Aspergillus Species from Clinical Samples and the Surge of Cryptic Aspergillosis in Southern India: A Descriptive Cross-sectional Study

Introduction: Aspergillus species cause a broad range of infections, from Allergic Bronchopulmonary Aspergillosis (ABPA) to invasive aspergillosis. Accurate species-level identification is crucial for diagnosis and treatment, especially since some rare Aspergillus species exhibit increased resistance to common antifungal agents. Aim: To identify Aspergillus species at the species complex level and determine the emergence of cryptic Aspergillus species using Multilocus Sequence Analysis (MLSA). Materials and Methods: This descriptive cross-sectional study was conducted over eight months, from January 2023 to August 2023, in three tertiary care centres in Chennai, India. Sixty Aspergillus strains were isolated from various clinical samples. The primary inclusion criteria were patients with suspected aspergillosis, categorised based on the European Organszation for Research and Treatment of Cancer Mycoses Study Group (EORTC-MSG) criteria. Isolates were grown on Oatmeal Agar or Sabouraud Dextrose Agar (SDA) and phenotypically identified using tease mount and slide culture techniques. Genomic fungal Deoxyribonucleic acid (DNA) was extracted and amplified using specific primers for Internal transcribed spacer (ITS), beta-tubulin, hydrophobin, and calmodulin genes, followed by nucleic acid sequencing. Results: Among the 60 Aspergillus isolates, the Aspergillus flavus complex comprised 26 (43.3%), the Aspergillus fumigatus complex 16 (26.7%), the Aspergillus niger complex 12 (20%), and the Aspergillus terreus complex 6 (10%). Initial speciation relied on microscopic and cultural characteristics. Isolates were recovered from various clinical specimens: bronchial wash 6 (10%), Bronchoalveolar lavage (BAL) fluid 10 (16.7%), sputum 3 (5%), ear swab 20 (33.3%), endotracheal aspirate 8 (13.3%), pus and tissue from the nasal cavity and paranasal sinus 11 (18.3%), and tissue from other sites 2 (3.3%). MLSA identified common species such as A. flavus, A. fumigatus, A. terreus, and A. niger, as well as rare species including A. awamori, A. carneus, A. lentulus, A. oryzae, A. tamarii, A. tubingensis, and A. welwitschiae. Sequence identity ranged from 99% to 100%, confirming species diversity. Phylogenetic analysis using ITS, beta-tubulin, hydrophobin, and calmodulin genes supported species identification with robust bootstrap support (1000 replications). Conclusion: Cryptic Aspergillus species are prevalent in clinical samples from the South Indian population, with a notable presence from the section Nigri and the first-time isolation of Aspergillus carneus in clinical samples from India. Molecular identification is essential for determining the invasive potential and guiding appropriate antifungal therapy.

Correlation between Dyslipedemia and Urine Albumin Excretion in Non Diabetic Obese Subjects: A Cross-sectional Study

Introduction: Obesity is a global health concern, and recent research has shown that it can cause kidney problems, especially in non diabetics. Obesity-related dyslipedemia, characterised by aberrant lipid profiles, may contribute to kidney damage. Aim: The purpose of the present cross-sectional study was to shed light on the complex interaction between dyslipedemia and renal health by examining the relationship between dyslipedemia and urine albumin excretion in non diabetic obese adults. Materials and Methods: The cross-sectional investigation was conducted in the Outpatient Obesity Clinic of the Endocrinology Department at a Tertiary Hospital in Kerala, India. A total of 144 non diabetic obese individuals between the ages of 18 and 65 years. All subjects provided informed consent, and ethical approval was obtained. The primary inclusion criteria were a Body Mass Index (BMI) of less than 25.0, the absence of Type 2 Diabetes Mellitus (T2DM), and the absence of proteinuria. Urine and blood samples were collected for laboratory testing, and statistical analysis was conducted using International Business Machines (IBM) Statistical Package for Social Sciences (SPSS) Statistics 20.0. Results: Dyslipedemia was found to be common, with low High-Density Lipoproteins (HDL) levels in 41.4% of participants, high Low-Density Lipoproteins (LDL) levels in 49.6%, high Triglycerides (TG) levels in 29.7%, and high Total Cholesterol (TC) levels in 43%. The study revealed that obese individuals with dyslipedemia excrete albumin at a significantly higher rate than obese individuals without dyslipedemia. Furthermore, a weak correlation between TG levels and the Urine Albumin Creatinine Ratio (UACR) was discovered. However, UACR did not significantly correlate with metabolic risk markers such as Fasting Plasma Glucose (FPG), serum insulin, blood pressure, HDL, LDL, TC, and systolic/Diastolic Blood Pressure (DBP). Conclusion: The results of the present study demonstrate that dyslipedemia significantly contributes to kidney damage in non diabetic obese individuals. The presence of dyslipedemia in obese then could serve as an early warning sign of potential renal problems. Further research is needed to fully understand the complex interactions between obesity, dyslipedemia, and renal health. These insights could be crucial for developing effective preventative and intervention methods in this context.

Diagenesis of the Permian Fengcheng Formation in the Mahu Sag, Junggar Basin, China

The Fengcheng Formation in the Mahu sag of the Junggar Basin was primarily composed of detritus, pyroclastic material, carbonates, and evaporites. In order to establish the diagenesis pathways of the Fengcheng Formation, some methods of polarized light microscope, SEM, CL, EPMA, LR, and fluid inclusion analysis were applied to discuss the diagenesis process. The results showed the following: (a) The formation of an alkaline lake was the result of the influence of a high concentration of sodium-rich sources, and it led to the preservation of alkaline minerals in the stratum. (b) After the sediments were buried, three mineral assemblages were formed in the Fengcheng Formation, which are carbonate mineral assemblages (i.e., calcite + ferreous dolomite), reedmergnerite and carbonate mineral assemblages (i.e., reedmergnerite + calcite + ferreous dolomite), and reedmergnerite and alkaline mineral assemblages (i.e., reedmergnerite + shortite + trona), respectively. (c) According to the homogenization temperature of reedmergnerite primary fluid inclusions, the alkaline diagenesis of Fengcheng Formation was divided into an early stage (≤100 °C) and a middle stage (&gt;100 °C), respectively. The earlier stage is marked by the formation of ferrous saddle dolomite, quartz dissolution, and the agglutination of laumontite. These processes occurred under normal burial conditions. The latter is marked by the reedmergnerite’s appearance, which is correlated with the deep hydrothermal activity controlled by faults. (d) Based on sedimentary and diagenetic factors, including climate, provenance, diagenetic surroundings, and the action of subsurface fluid, the alkaline deposition-diagenesis model for shale series in four stages of the Fengcheng Formation was established.

Magmatic–Fluid System of the Vysokogorskoe Porphyry Tin Deposit (Sikhote-Alin, Kavalerovo Ore District, Primorsky Krai, Russia): a Magmatic Stage

Inclusions of the mineral-forming media in quartz of the Vysokogorskoe deposit are studied in detail. The compositions of the melts correspond to peraluminous potassium granites of normal alkalinity, depleted in rare alkalis, F, and Cl. The water content in the melts reached 7–9 wt %; CO2 and CH4 were also important in mineralizing fluids. Quartz crystallized at 620–650°C. Assemblages of four types have been identified as primary fluid inclusions: (1) inclusions of carbonate or sulfate aqueous solutions coexisting with melt inclusions, (2) low-density vapor-dominated primarily magmatic inclusions, (3) presumably postmagmatic low-salinity aqueous and vapor-dominated inclusions, and (4) multiphase fluid inclusions associated with vapor-dominated ones also formed at the postmagmatic stage. Daughter pyrosmalite–(Fe) and hibbingite, which was found for the first time in inclusions from quartz of the Vysokogorskoe deposit, made it possible to characterize the solutions as high-salinity chloride Na/K and Fe2+. Presumably, those solutions may have been the most efficient in Sn transport during the formation of fluid–explosive breccias and vein mineralization of the Vysokogorskoe deposit. The magma chamber itself most likely served as a heat source and, to a large extent, a source of aqueous fluid for the hydrothermal system of the deposit.

Epithermal Deposits of Kamchatka, Russia

The results of studying the epithermal deposits of Kamchatka, one of the most promising gold-mining provinces of the Russian Federation, are generalized. The deposits are divided into acid–sulfate (Ac-Sul) and adularia–sericite (Ad-Ser) types (Heald et al., 1987). The disadvantages of the scheme, which is the most popular in the English-language literature and is based on the sulfidation state of mineral parageneses in ores (LS, IS, and HS types), are shown. The classification that we proposed includes differences in mineral associations in circum–ore metasomatites, which are determined by the acidity–alkalinity and an oxidation state of mineral-forming fluids, and are clearly diagnosed at the first stages of studying the deposits. Kamchatka epithermal deposits of the Ad-Ser-type are associated with andesite volcanism of the volcanic belts. Gold ore associations are concentrated in quartz, carbonate–quartz, and adularia–quartz veins, as well as in sericitized metasomatites, which are replaced by argillizites and propylites towards the periphery. The Ad-Ser-type is characterized by combination with polysulfide (Pb, Zn) (Amethyst, Kumroch, Vilyuchinskoe deposits), sulfosalt (Ag, Sb, As, Bi, Sn) (Ozernovskoe, Baranyevskoe), and selenide (Ag, Se) (Amethyst, Asachinskoe, Rodnikovoe) assemblages. Low-fineness native gold (220–310‰) is typical of the early polysulfide assemblage. With an increase in the fugacity of Te and Se, the gold fineness increases to 510–740‰, and with the progressive activity of Sb, As and Bi and the formation of sulfosalt associations, it reaches 998‰. The homogenization temperatures of primary fluid inclusions in quartz from gold-bearing associations of the Ad-Ser-type are 260–250°C; the minerals crystallize from solutions containing no more than 3 wt % NaCl eq. Maletoyvayam, the only Ac-Sul-type deposit in Kamchatka, is localized in quartz, secondary quartzites, and alunite–sericite–kaolinite–quartz metasomatites. Gold-bearing parageneses indicate the leading role of selenium in mineral formation, contain high-fineness native gold, sulfoselenotellurides, tellurides, and selenides of Au, which crystallize from acidic fluids with salinity of 1–5 wt % NaCl eq. at temperatures of 290–175°C.

Genesis of the Yidonglinchang gold deposit, Lesser Xing’an Range, China: Insights from fluid inclusions, H-O-S-Pb isotopes, and Sm-Nd and U-Pb geochronology

The origin and evolution of the newly discovered Yidonglinchang gold deposit in the Lesser Xing’an Range, Northeast China, remain poorly understood. This article focuses on the investigations of the geological characteristics, fluid inclusions, H-O-S-Pb stable isotopes and geochronology of the deposit. The Yidonglinchang gold deposit is mainly controlled by NEE-trending faults, and the ore bodies are present in volcanic rocks of the Early Cretaceous Ningyuancun Formation (K1n). Silicification, pyritisation, and argillization zones develop sequentially from near the ore center outwards. The ore minerals mainly include electrum and argentite. The gangue minerals are mainly quartz, calcite, and a small amount of sericite, plagioclase and adularia. The main gold-bearing minerals are quartz and calcite. The primary fluid inclusion types in quartz are pure-liquid-phase, gas-rich-phase, and liquid-rich-phase inclusions. Most of the inclusions are classified as a H2O-NaCl system which were formed under low-temperature, low-salinity conditions, indicating that Yidonglinchang is an epithermal gold deposit. The occurrence of boiling fluid inclusion assemblage indicates that the fluids underwent decompression boiling. Sm-Nd dating of calcite from the main ore-forming stage yields an age of 97.5 ± 2.3 Ma, which is interpreted as the timing of mineralisation. Zircon U-Pb dating of dioritic porphyrite yields ages of 98.8 ± 1.1 and 98.0 ± 1.3 Ma, which are consistent with the mineralisation age, suggesting a potential genetic link between the intrusive rocks and the ore formation. H-O-S-Pb isotopic compositions indicate that the ore-forming fluids were magmatic water during the early mineralisation stage, with the addition of meteoric water during the late stage. These isotopic compositions are also indicative of an origin of the ore-forming materials from the mixed crustal and mantle components. The mineralisation of the Yidonglinchang gold deposit was related to the slab rollback of the subducted Palaeo-Pacific Plate in the early Late Cretaceous.

H2O and Cl in deep crustal melts: the message of melt inclusions in metamorphic rocks

Abstract. The use of NanoSIMS on primary melt inclusions in partially melted rocks is a powerful approach to clarify the budget of volatiles at depth during crust formation and its reworking. Anatectic melt inclusions are indeed gateways to quantify H2O, halogens and other species (e.g. CO2, N) partitioned into the deep partial melts generated during metamorphism of the continental crust. Here we present new datasets of NanoSIMS measurements of H2O and Cl in preserved melt inclusions from metamorphic rocks with different protoliths – magmatic or sedimentary – which underwent partial melting at different pressure–temperature–fluid conditions. These new datasets are then compared with similar data on natural anatectic melts available in the literature to date. Our study provides novel, precise constraints for the H2O content in natural melts formed at high pressure, a field previously investigated mostly via experiments. We also show that H2O heterogeneities in partial melts at the microscale are common, regardless of the rock protolith. Correlations between H2O contents and P–T values can be identified merging new and old data on anatectic inclusions via NanoSIMS. Overall, the data acquired so far indicate that silicate melt generation in nature always requires H2O, even for the hottest melts found so far (&gt;1000 ∘C). Moreover, in agreement with previous work, preserved glassy inclusions always appear to be poorer in H2O than crystallized ones, regardless of their chemical system and/or P–T conditions of formation. Finally, this study reports the very first NanoSIMS data on Cl (often in amounts &gt;1000 ppm) acquired in situ on natural anatectic melts, showing how anatectic melt inclusions – additionally to magmatic ones – may become a powerful tool to clarify the role of halogens in many geological processes, not only in crustal evolution but also in ore deposit formation.

Cytotoxic activity of isoquinoline alkaloids and herbal extracts from selected plants against human cancer cell lines: harnessing the research potential in cancer drug discovery with modern scientific trends and technology.

The increasing prevalence of cancer has led to a growing interest in alternative medicine methods and treatments. This study aimed to assess the cytotoxicity of isoquinoline alkaloids and herbal extracts from selected plants against human cancer cell lines, including melanoma and squamous cell carcinoma. The investigation involved in vitro cell viability assays using various cancer cell lines and normal skin fibroblasts as control cells. Additionally, a zebrafish model was employed for in vivo evaluation of cytotoxic activity. The results indicated that the tested alkaloids and extracts exhibited promising cytotoxic effects, showing higher potency than standard chemotherapeutic drugs. In comparison, these findings support the exploration of isoquinoline alkaloids and herbal extracts as potential candidates for developing novel anti-melanoma and anti-squamous cell carcinoma drugs. The primary inclusion criterion that was taken into consideration in this study effort was the therapeutic application of the cytotoxic effects of specific plant-based pharmacological components or chemicals produced from herbal extracts that are ordinarily cytotoxic.

Ore-Forming Fluids of Orogenic Gold Deposit In Tamilouw-Haya, Seram Island, Indonesia

The Tamilouw-Haya orogenic gold deposit is located in the southern arm of Seram Island, Indonesia, occupying Tehoru Metamorphic Complex. Gold mineralization is predominantly in the form of veins, stockwork, and breccia, although minor dissemination is slightly appeared in the rock float samples. Ore-mineral assemblages are dominated by native gold, pyrite, chalcopyrite, sphalerite, tetrahedrite-tennantite (sulfosalt), galena, pyrrhotite, marcasite, realgar, kalininite, and arsenopyrite. Covellite, hematite, goethite, and malachite appear as supergene minerals. High-grade gold ores in this area are generally found in quartz-carbonate veins with the main alteration processes involving silicification, carbonatization, and sericitic. The P-T history of the mineralization was revealed by fluid inclusions, and this study implies the depth of ore deposit and its evolution during mineralization. The primary fluid inclusions from three different types of quartz/quartz-carbonate veins in Tamilouw-Haya crystallized at the homogenization temperature (Th) of 240 °C to 340 °C, with a fluid salinity from 3.87 to 0.70 wt. % NaCl equivalent, and melting temperature (Tm) of -0.4 to -2.3 oC. The ore-forming fluids consist mainly of two-phase (VCO2+LH2O) liquid-rich aqueous inclusions, characterized by low to rich CO2, low salinity, and moderate temperature. There are three vein types as the ore-bearing fluids with precious metals and anomalous high basemetal contents. Quartz type 1- veins (V1); concordant veins, formed at a temperature of 240-307 oC with an average salinity of 1.8 wt. % NaCl equivalent. Quartz type 2- veins (V2) tend to cut the rock foliation which are formed at temperature range from 293-336 oC with the average salinity that shows a value of 2.4 wt. % NaCl equivalent. Meanwhile, type 3 quartz-carbonate veins (V3) are formed at the temperature range of 240-340 oC and the average salinity of 2.72 wt. % NaCl equivalent. These quartz-carbonate veins cut the wall-rock foliation, which is identified as the late stage and associated with ore deposition in Tamilouw-Haya. The gold deposit in Tamilouw-Haya is formed at a depth of about 5.5-9 km of paleosurface, and the pressure between 1.7-2.4 Kbar in epizonal to mesozonal zones. Keywords: Tamilouw-Haya, orogenic gold, fluid inclusion, microthermometry, ore-forming fluids

Age of Carlin-type gold mineralization in the Youjiang basin, South China: Constraint from hydrothermal zircon geochronology in the Badu dolerite-hosted gold deposit

Selecting a robust chronometer is crucial to determine the primary mineralization age of the deposits that have witnessed multiple hydrothermal events. The Youjiang basin of South China hosts the world’s second-largest Carlin-type gold province. However, the age of the Carlin-type gold mineralization remains highly debated, partly due to the presence of multiple hydrothermal events that may have disturbed the primary isotopic system with low durability. Hydrothermal zircon is a robust chronometer that can survive multiple hydrothermal events. To this end, in this study, we report in-situ secondary ion mass spectrometry (SIMS) and laser ablation inductively coupled plasma-mass spectrometry (LA-ICP-MS) U–Pb dating results of hydrothermal zircon identified in carbonate–sericite–sulfide–altered dolerite from the Badu Carlin-type gold deposit to constrain the timing of gold mineralization.The hydrothermal zircons exhibit subhedral to anhedral morphologies, sector cathodoluminescence zonings, and contain gold-related mineral assemblages of arsenian pyrite, quartz, sericite, and carbonate. Primary two-phase fluid inclusions also commonly occur in the hydrothermal zircons. Compositionally, these zircons feature relatively flat light rare-earth element (REE) patterns, high La contents, low (Sm/La)N values, and small Eu and Ce anomalies, which are different from the magmatic counterparts of the Badu pluton but consistent with those of hydrothermal zircons reported worldwide. These features indicate that the hydrothermal zircons are probably paragenetically associated with the gold mineralization. Consequently, the U–Pb ages of ca. 140 Ma of these zircons, which are much younger than those of the magmatic zircon in the fresh dolerite, can represent the timing of primary gold mineralization of Badu. Our new data suggests that there truly was an episode of gold mineralization during the Early Cretaceous in the Youjiang basin, which may have been driven by large-scale lithospheric extension in the interior of South China. This study demonstrates that hydrothermal zircon could be a robust clock for investigating the timing of magmatic rock-hosted Carlin-type gold deposits.

Fluid Regime of Crystallization of the Calcite–Quartz Carbonatitoids of the Murun Massif

Abstract —Primary melt and fluid inclusions in quartz and dalyite of calcite–quartz carbonatitoids of the Murun massif have been studied. They contain CO2, N2, CH4, C2H6, C3H8, H2, and H2S as well as sulfates and hydrocarbonates as solid daughter phases. The inclusion solutions contain HS- and chlorides. In addition, disordered carbon and bitumen are present. It is concluded that the magmatic fluid phase that was in equilibrium with quartz was characterized by a predominantly H2O–CO2–H2S composition and a reduced state. This explains the appearance of sulfides at the magmatic stage of crystallization of calcite–quartz carbonatitoids of the Murun massif. We substantiate the hypothesis that the sulfates, hydrocarbons, and H2 detected in the inclusions form at decreasing temperature as a result of shift of the redox equilibrium.

Cavernous Malformations and Hemangioblastomas of the Spinal Cord Show Distinct Differences in Clinical Course - A Retrospective Single-Center Analysis of 112 Patients.

Retrospective cohort study. Cavernous malformations (CMs) and hemangioblastomas (HBs) of the spinal cord exhibit distinct differences in histopathology but similarities in the neurological course. The aim of our study was to analyze the clinical differences between the vascular pathologies and a benign tumor of the spinal cord in a perioperative situation. We performed a retrospective analysis of patients who had undergone surgery for lesions in the spinal cord between 1984 and 2015. Patients were screened for CMs and HBs as the primary inclusion criteria. General patient information, surgical data, and disease-specific data were collected from the records. Cooper-Epstein scores for clinical symptoms were evaluated preoperatively, at discharge, and at the 6-month follow-up. A total of 112 patients were included, of which 46 had been diagnosed with CMs and 66 with HBs. Patients with CMs often demonstrated more preoperative neurological deterioration compared to those with HBs (P < .05); accordingly, in took longer to diagnose HBs. Complete resection was possible for 96.8% of all patients with CMs and 90% of those with HBs. At the 6-month follow-up, patients with HBs more often presented with persisting neurologic impairment of the upper extremities compared to the CM patients (P < .001). CMs and HBs of the spinal cord have similarities but also exhibit significant differences in neurological presentation and perioperative course. Surgical therapy is the treatment of choice for symptomatic lesions, and complete surgical resection is possible in the majority of cases for both entities. Neurologic outcomes are usually favorable, although patients with HBs retain neurologic deficits more often.

Fracturing timing of Jurassic reservoirs in the Dibei-Tuziluoke gas field, Kuqa foreland basin: Evidence from petrography, fluid inclusions, and clumped isotopes

Determining the timing of fracturing is crucial for understanding reservoir evolution and hydrocarbon accumulation in foreland basins. Using fracturing data from cores, borehole images, and outcrops, combined with the clumped isotope (Δ47) and fluid inclusion analyses of carbonate minerals filled in pores and fractures, this study ascertained the fracturing timing of the Jurassic reservoirs in the Dibei-Tuziluoke Gas Field, Kuqa Foreland Basin. Data from outcrops and borehole images show two dominant fracture sets in the study area: W-E and NE-SW striking fractures. Some W-E striking fractures are carbonate-filled, while NE-SW striking fractures lack mineral fillings. Bitumen veins, not easy to be identified in borehole images, are prevalent in cores. The petrographic analysis reveals that these bitumen veins formed before the calcite cementation in pores and display high viscosity and low maturity. Homogenization temperatures (Th) from primary fluid inclusion assemblages in two representative calcite vein samples were notably lower than TΔ47 values from corresponding samples. This suggests the Δ47 signature underwent alteration due to partial reordering during burial. Thus, Δ47-derived temperatures (apparent temperatures) may not faithfully represent the mineral precipitation temperatures. When plotting these apparent temperatures vs. the burial history, only the possible latest ages of fracturing emerged. These ages were further refined by considering petroleum charging, tectonic evolution, and stress orientation. Bitumen-filled fractures likely resulted from the Late Cretaceous uplift, marking the migration of low-maturity hydrocarbons in the study area. Carbonate-filled E-W striking fractures emerged during the late Miocene (∼13–6.5 Ma) alongside fold development. NE-striking fractures that crosscut W-E ones possibly formed recently due to stress reorientation.