Search Results (57)

Prostate cancer is the most common non-cutaneous malignancy in men and is the second leading cause of male cancer-related mortality. Unlike many cancers, prostate cancer lacks clear genetic driver mutations, suggesting that factors in the tumor microenvironment contribute to the genesis and progression of this disease. Hypoxia, or a physiological state of low oxygen, is a universal characteristic of solid tumors that enhances disease progression and therapeutic resistance. Prostate cancer develops in a hypoxic microenvironment and primarily metastasizes to bone, where oxygen availability is similarly limited. Therefore, hypoxia is a major obstacle to the effective treatment of prostate cancer across all disease stages. Clinically, hypoxia is correlated with worse patient outcomes, largely because it drives resistance to the frontline therapies used to treat both primary and metastatic prostate cancer. Despite the established role of hypoxia in prostate cancer progression and drug resistance, it has not been successfully targeted therapeutically. Emerging evidence indicates that exposure to distinct temporal patterns of hypoxia (acute, cyclic, and chronic) elicits unique cellular adaptations that dictate tumor growth and survival. This review synthesizes current evidence regarding the role of hypoxia in promoting resistance to therapy in prostate cancer. Full article

Siliceous rocks of various colors and types are extensively developed within the Middle–Lower Ordovician carbonate along the Northwest Tarim Basin. Their genesis provides important insights into the evolution of basinal fluids and the associated diagenetic alterations of the carbonates. Based on petrographic, geochemical, fluid inclusion, and petrophysical analyses, this study investigates the origin of siliceous rocks within the Middle–Lower Ordovician carbonate formations (Penglaiba, Yingshan, and Dawangou formations) in the Kalpin area, Tarim Basin, and investigates the impact on hydrothermal reservoirs. The results reveal two distinct episodes of siliceous diagenetic fluids: The first during the Late Ordovician involved mixed hydrothermal fluids derived from deep magmatic–metamorphic sources, formation brines, and seawater. Characterized by high temperature and moderate salinity, it generated black chert dominated by cryptocrystalline to microcrystalline quartz through replacement processes. The second episode developed in the Middle–Late Devonian as a mixture of silicon-rich fluids from deep heat sources and basinal brines. In conditions of low temperature and high salinity, it generated gray-white siliceous rocks composed of micro- to fine crystalline quartz, spherulitic-fibrous chalcedony, and quartz cements via a combination of hydrothermal replacement and precipitation. A reservoir analysis reveals that the multi-layered black siliceous rocks possess significant reservoir potential amplified by the syndiagenetic tectonic fracturing. In contrast, the white siliceous rocks, despite superior petrophysical properties, are limited in scale as they predominantly infill late-stage fractures and vugs, mainly enhancing local flow conduits. Hydrothermal alteration in black siliceous rocks is more intense in dolostone host rocks than in limestone. Thus, thick (10–20 m), continuous black siliceous layers in dolostone and the surrounding medium-crystalline dolostone alteration zones, are promising exploration targets. This study elucidates the origins of Ordovician siliceous rocks and their implications for carbonate reservoir properties. The findings may offer valuable clues for deciphering the evolution and predicting the distribution of hydrothermal reservoirs, both within the basin and in other analogous regions worldwide. Full article

The field of study on intimate partner violence has long been characterized by a bitter debate between the following two opposing theoretical and ideological positions on the nature of the phenomenon: the first is typical of the feminist perspective and considers IPV as an expression of gender-based violence; the second is typical—among others—of the attachment-based perspective and maintains that IPV would be a neutral form of violence with respect to gender. The aim of this contribution is to try to show how it is possible to make a more heuristically fruitful comparison between these two antagonistic perspectives, shifting the focus on the conceptual frameworks that underlie them and on their two different corresponding key explanatory concepts as follows: on the one hand, gender-based power on which the feminist perspective hinges, and on the other, love and love-related emotional dynamics on which the attachment-based perspective focuses. Finally, we will argue how these two key explanatory concepts can be kept combined in a sort of binocular vision and integrated into a more complex “power-and-love” explanatory framework. To this end, we will refer to a systemic approach to IPV, in particular to the contribution of Virginia Goldner, who proposes a model based on the close interconnection between power dynamics and love-related dynamics in the genesis and perpetuation of male violence in heterosexual intimate relationships. Full article

Iron oxide–apatite (IOA) deposits are important for the global supply of iron resources. Currently, there is considerable debate regarding the evolution of their mineralization mechanisms. The Heshangqiao iron deposit is a significant IOA deposit situated within the Ningwu ore district of the Middle–Lower Yangtze River Metallogenic Belt in China. This deposit exhibits distinct characteristics of multi-stage mineralization, forming disseminated ores, brecciated ores, and vein-type ores, from early to late stages. This study undertook a systematic elemental analysis of the magnetite and hematite from three mineralization stages of the Heshangqiao deposit. In the three mineralization stages of the Heshangqiao deposit, the elemental genesis indicators of ore genesis suggest that the hematite and magnetite both have magmatic hydrothermal genesis, characterized by high Ti and low Mg/Al and relatively high Ti and low Ni/Cr, respectively. The Cr and Sn contents of magnetite and hematite exhibit similar variation from the first to third mineralization stage, with an increase followed by a subsequent decrease. Meanwhile, the contents of V, Co, Ni, and Mn in magnetite and hematite exhibited an opposite trend, declining from the first to the second stage but eventually increasing from the second to the third stage. These changes in the genesis indicator also suggest that the multiple mineralization stages of the Heshangqiao deposit are independent of one another. The replacement of magnetite by hematite in each mineralization stage is not caused by the superposition of subsequent fluids, but rather by the residual fluid. It is noted that in the replacement the elements Cr, Co, and Ga were minimally migrated. These elements remained relatively stable and can be considered new potential discriminant indicators for the genesis of iron oxides. Full article

This paper tries to analyse what “interaction” with classical Greek literature may mean in the case of ancient Christian texts. Two case studies show the existence of a “hermeneutical circle” between the reception of Greek texts among Christians and Christian ideas. The Christians were influenced by the Greek texts they commented on, but, on the other hand, their reception of such texts was determined by their Christian intellectual presuppositions. The first case (the emergence of the “Trinity” among the “apologists”) illustrates a cross-reading of Matthew 28:19 and Ps.-Plato’s Letter 2. The second case shows how the term ὁμοίωσις, in Genesis 1:26, was read in the light of Theaetetus 176a-b, and vice versa. Full article

The Jiapigou mining district (>180 t Au) is an important gold district in China. For a long time, the ore genesis of the gold deposits in the Jiapigou district has been a subject of controversy and differing opinions, which has severely hindered metallogenic theories and mineral exploration. Here we present a comprehensive investigation including geology, fluid inclusions (FIs), and H–O–S isotopic data for the Naizhigou deposit in the Jiapigou district to elucidate the sources of orefluids and metals, as well as the metallogenic mechanism. The results show the following: (1) The Naizhigou deposit is characterized by quartz vein-type ores and is hosted in the Middle Jurassic granitic pluton. Native gold and sulfides were mainly deposited in the second stage (quartz–polymetallic sulfides) compared with the first (quartz–pyrite–molybdenite) and third (quartz–calcite) stages. (2) The FI studies indicated that the orefluids evolved from the early–main-stage CO₂–H₂O–NaCl system to the late-stage H₂O–NaCl system and have homogenization temperatures of 289–363, 210–282, and 124–276 °C and salinities of 4.1–20.9, 5.8–16.4, and 6.1–12.7 wt% NaCl equivalent, respectively. Fluid boiling and fluid mixing collectively controlled the precipitation of gold and ore-forming elements. (3) The δD values of the FIs hosted in quartz from the three stags range from −81 to −75 ‰, from −99 to −86 ‰, and from −110 to −101 ‰, while δ¹⁸O_water values of these FIs range from 5.3 to 5.9 ‰, from 1.1 to 5.2 ‰, and from −2.1 to −0.7 ‰, respectively. Pyrite samples from the three stages in the Naizhigou deposit have δ³⁴S values of 2.1 to 2.5 ‰, 3.1 to 4.3 ‰, and 3.8 to 3.9 ‰, respectively. The stable isotopes indicate that the orefluids and metals mainly originated from magma. A comparative study of regional observations reveals that the Naizhigou deposit is a magmatic-related mesothermal gold deposit, rather than a metamorphism-related orogenic gold deposit. The estimated ore-forming depths are 4.0–20.7 km, with exhumation depths of 4.1–5.5 km, which indicated that the deposit has been well preserved. Regionally, the new exploration strategies should place greater emphasis on work concerning ore-related plutons, ore-controlling faults, and hydrothermal alteration. Full article

Divine rebaptism occurs when a deity renames an entity with a proper name N*, which is pronounced differently or is orthographically distinct from the proper name N this entity previously had. Genesis 17:5 and 17:15 illustrate this phenomenon or alleged phenomenon while raising two questions not yet addressed. First, the identity question: Are those named “Abram” and “Sarai”, respectively, identical to those named “Abraham” and “Sarah” in Genesis? Second, the semantic question: What picture of the semantics of proper names best accounts for the divine rebaptisms portrayed in Genesis? This essay begins by motivating these questions; it indicates that they should—in an interdisciplinary fashion—appeal to Pentateuch specialists and philosophers interested in the semantics of proper names. Then, a case is made for the claim that though Genesis does not provide sufficient evidence to answer the identity question, it indicates a response to the semantic one: that especially in Genesis 17:5 and 17:15, this text points to gradation semantics. This is the view that proper names have the properties of being meaningful, indirect, flaccid, flexible, and lexically univocal in distinct degrees, depending on their context of use. Full article

Precambrian tropical glaciation is an enigma of Earth’s climate. Overlooking fundamental difference of land/sea icelines, it was equated with a global frozen ocean, which is at odds with the sedimentary evidence of an active hydrological cycle, and its genesis via the runaway ice–albedo feedback conflicts with the mostly ice-free Proterozoic when its trigger threshold was well exceeded by the dimmer sun. In view of these shortfalls, I put forth two key hypotheses of the tropical glaciation: first, if seeded by mountain glaciers, the land ice would advance on sea level to be halted by above-freezing summer temperature, which thus abuts an open cozonal ocean; second, a tropical supercontinent would block the brighter tropical sun to cause the required cooling. To test these hypotheses, I formulate a minimal tropical/polar box model to examine the temperature response to a varying tropical land area and show that tropical glaciation is indeed plausible when the landmass is concentrated in the tropics despite uncertain model parameters. In addition, given the chronology of paleogeography, the model may explain the observed deep time climate to provide a unified account of the faint young Sun paradox, Precambrian tropical glaciations, and Phanerozoic glacio-epochs, reinforcing, therefore, the uniformitarian principle. Full article

Uranium mineralization related to Na-metasomatism is known as Na-metasomatite or albitite-type. They represent the fourth-largest uranium resource globally and constitute fifty thousand tons of U resources. The present work gives details about well-known Na-metasomatic uranium occurrences worldwide in terms of structures, metasomatic stages, geochemical characteristics, fluid inclusions, and compositions of stable isotopes. The host rocks are granite, granitoid, and metamorphosed volcano-sedimentary rocks, and these rocks experienced two/three deformational stages. U mineralization is mainly confined to faults and characterized by granitic intrusive, cataclasis, mylonitization, and albitization. The albitized rocks exhibit two to three metasomatic and late hydrothermal stages. The first stage is marked by the replacement of pre-existing host minerals during a ductile shear regime. The second stage is related to U mineralization contemporaneous with the brittle deformation. The albitized rocks exhibit depletion in Si, K, Ba, and heavy rare-earth elements relative to the host rocks and enrichments in Na, Ca, U, Zr, P, V, Sr, and light rare-earth elements. U-enrichment is positively correlated with Na, Mo, Cu, and high-field strength elements. The pressure–temperature (P-T) conditions of U mineralization are considered to be epithermal and mesothermal. Fluid inclusion studies indicate that the mineralizing fluids were rich in Na⁺, Mg²⁺, Cl⁻, CO₂, H₂O, F⁻, and PO₄³⁻ and meteoric–magmatic derived. The geological processes responsible for the genesis of Na-metasomatic U deposits of the North Delhi Fold Belt (India) are comparable with some international examples, i.e., Australia, Ukraine, Cameroon, Brazil, Guyana, China, and the USA. Full article

This study meticulously examines the influence of aluminum (Al) and titanium (Ti) on the genesis of self-generated ordered phases in high-entropy alloys (HEAs), a class of materials that has garnered considerable attention due to their exceptional multifunctionality and versatile compositional palette. By meticulously tuning the concentrations of Al and Ti, this research delves into the modulation of the in situ self-generated ordered phases’ quantity and distribution within the alloy matrix. The annealing heat treatment outcomes revealed that the strategic incorporation of Al and Ti elements facilitates a phase transformation in the Cr-Fe-Ni medium-entropy alloy, transitioning from a BCC (body-centered cubic) phase to a BCC + FCC (face-centered cubic) phase. Concurrently, this manipulation precipitates the emergence of novel phases, including B2, L2₁, and σ. This orchestrated phase evolution enacts a synergistic enhancement in mechanical properties through second-phase strengthening and solid solution strengthening, culminating in a marked improvement in the compressive properties of the HEA. Full article

Digital solutions in the field of restorative neurology offer significant assistance, enabling patients to engage in rehabilitation activities remotely. This research introduces ReMoVES, an Internet of Medical Things (IoMT) system delivering telemedicine services specifically tailored for multiple sclerosis rehabilitation, within the overarching framework of the STORMS project. The ReMoVES platform facilitates the provision of a rehabilitative exercise protocol, seamlessly integrated into the Individual Rehabilitation Project, curated by a multidimensional medical team operating remotely. This manuscript delves into the second phase of the STORMS pilot feasibility study, elucidating the technology employed, the outcomes achieved, and the practical, professional, and academic implications. The STORMS initiative, as the genesis of digital telerehabilitation solutions, aims to enhance the quality of life for multiple sclerosis patients. Full article

In this article, I develop a critique of Chantal Mouffe’s leftist populism and its construction of ‘the people’ against an opposed ‘them’, from a perspective informed by the thought of Didier Eribon. I draw on both his public interventions and his theoretical work, employing his concepts of return, society as verdict, and his two principles of critical thinking to question the desirability of crafting ‘the people’ in the first place. I contend that Eribon’s critique renders Mouffe’s proposal problematic on three accounts. First, her approach is too politically volatile; its instability leaves it devoid of a critical analysis of the differences between concrete social positions, struggles, and subjectivities within ‘the people’. Consequently, the political becomes merely a function of the social. Yet, the social and its determining power remain mostly unaddressed by her framework. Second, its simplistic opposition of an overly generalised ‘the people’ against ‘the oligarchy’ is susceptible to right-wing populist appropriations. Third, for a shot at hegemony and a general appeal, it eclipses plurality and dissensus within ‘the people’. In contrast, Eribon encourages a connection between the social and the political by suggesting that a self-critical analysis be mutually intertwined with social analysis. Instead of merely mobilising affects, they must be critically interrogated. Instead of summoning ‘the people’, a return to their respective genesis must be attempted. Unless both principles of critical thinking, the insights of return, and societal verdicts are deployed to come to terms with the social determinisms at hand, the ‘people’s’ mobilisation against an opposed ‘them’ risks sacrificing pluralism and equality alike and neglecting the criteria of the desirability of specific changes in favour of a “whatever it costs” attempt at hegemony. Full article

Gendered criticism of Eve and general criticism of Eve and Adam are rooted in the idea of their moral failing when they disobey Yahweh. Two lenses bring a more ancient understanding of the text into focus. The first lens is reading the story in the context of the J source of the Pentateuch. The second lens is that of natural law as understood by Greco-Roman philosophers. These lenses provide new clarity, showing how Eve and Adam’s decision to eat from the tree of knowledge violates a non-moral norm: they transgress the boundary between humanity and divinity. It is this ontological transgression to which Yahweh responds. Mortality, many labors, and many pregnancies reflect the natural consequences of this ontological violation, not an arbitrary punishment for a moral failing. This alternative understanding of Genesis 2–3 allows us to understand that Eve and Adam are neither cursed nor punished. Full article

Petrological, geochronological, and geochemical analyses of mafic rocks in northern Liaoning were conducted to constrain the formation age of the Proterozoic strata, and to further study the source characteristics, genesis, and tectonic setting. The mafic rocks in northern Liaoning primarily consist of basalt, diabase, gabbro, and amphibolite. Results of zircon U-Pb chronology reveal four stages of mafic magma activities in northern Liaoning: the first stage of basalt (2209 ± 12 Ma), the second stage of diabase (2154 ± 15 Ma), the third stage of gabbro (2063 ± 7 Ma), and the fourth stage of magmatic protolith of amphibolite (2018 ± 13 Ma). Combined with the unconformity overlying Neoproterozoic granite, the formation age of the Proterozoic strata in northern Liaoning was found to be Paleoproterozoic rather than Middle Neoproterozoic by the geochronology of these mafic rocks. A chronological framework of mafic magmatic activities in the eastern segment of the North China Craton (NCC) is proposed. The mafic rocks in northern Liaoning exhibit compositional ranges of 46.39–50.33 wt% for SiO₂, 2.95–5.08 wt% for total alkalis (K₂O + Na₂O), 6.17–7.50 wt% for MgO, and 43.32–52.02 for the Mg number. TiO₂ contents lie between 1.61 and 2.39 wt%, and those of MnO between 0.17 and 0.21 wt%. The first basalt and the fourth amphibolite show low total rare earth element contents. Normalized against primitive mantle, they are enriched in large ion lithophile elements (Rb, Ba, K), depleted in high field strength elements (Th, U, Nb, Ta, Zr, Ti), and exhibit negative anomalies in Sr and P, as well as slight positive anomalies in Zr and Hf. The second diabase and the third gabbro have similar average total rare earth element contents. The diabase shows slight negative Eu anomalies (Eu/Eu* = 0.72–0.88), enrichment in large ion lithophile elements (Ba), depletion in Rb, and slight positive anomalies in high field strength elements (Th, U, Nb, Ta, Zr, Hf, Ti), with negative anomalies in K, Sr, and P. The gabbro is enriched in large ion lithophile elements (Rb, Ba, K), depleted in high field strength elements (Th, U, Nb, Ta, Zr, Hf), and exhibits positive anomalies in Eu (Eu/Eu* = 1.31–1.37). The contents of Cr, Co, and Ni of these four stages of mafic rocks are higher than those of N-MORB. The characteristics of trace element ratios indicate that the mafic rocks belong to the calc-alkaline series and originate from the transitional mantle. During the process of magma ascent and emplacement, it is contaminated by continental crustal materials. There are residual hornblende and spinel in the magma source of the first basalt. The other three magma sources contain residual garnet and spinel. The third gabbro was formed in an island arc environment, and the other three stages of mafic rocks originated from the Dupal OIB and were formed in an oceanic island environment. The discovery of mafic rocks in northern Liaoning suggests that the Longgang Block underwent oceanic subduction and extinction in both the north and south in the Paleoproterozoic, indicating the possibility of being in two different tectonic domains. Full article

Botanic gardens are increasingly important agents of plant research and conservation. A large number of botanic gardens have been established throughout the globe since the mid-20th century to pursue new socio-environmental missions. Others, with histories that span centuries, have also undergone a deep transformation in the context of growing attention to matters of sustainability. Bridging key aspects of the scholarly literature on the genesis of the botanical garden institution in Europe and its legacy, this article presents the re-invention of these gardens as institutions of conservation, sustainability, and social engagement as they renew their relevance in the contemporary world. This article proceeds by covering three focal points. First, it summarizes the scholarly literature on the emergence of botanical gardens in Europe and their association with the rise of modern science, the nation-state, colonialism, and empire-building. Second, it presents accounts of current scientific and biodiversity conservation endeavours as reflexive engagements with these historical legacies, decolonization initiatives, and new socio-environmental missions. Third, this article points beyond its focus on the historical transformation of the European botanical garden institution, by identifying a more widely encompassing body of scholarship that puts forth frameworks for understanding the current role of botanic gardens on a global scale. Full article