The animal protection movement has developed an increasingly close working relationship with the criminal punishment system through lobbying and campaigning for harsher punishments for animal abuse, while at the same time showing an interest in restorative justice (RJ) as a response to harm against animals. In this article, we take a critical position aligned with anti-carceral feminists and prison abolitionists against the carceral systems that fail humans and animals in circumstances of violence. We consider the potential of RJ as an alternative approach to address and prevent harm against animals in abuse cases on an individual level while highlighting the limitations of RJ in achieving the necessary changes on a societal level to end structurally produced violence against animals, such as industrial animal exploitation. We propose that transformative justice (TJ), which involves some RJ processes, is the most promising approach that could achieve justice for both humans and nonhumans in the long term without reproducing traumas and violence for the individuals and communities involved in harm reduction and prevention. Drawing on examples of RJ and TJ as developed and practised in marginalized human communities, we apply their lessons to thinking through similar practices in the context of animal abuse and neglect.

This study aimed to examine the effect of disaster preparedness literacy on individual disaster resilience and related factors. The universe of the research consists of individuals between the ages of 18-52. Software packages AMOS 23 and SPSS 26 were used to analyze the study’s data. Mann Whitney U test and Kruskal Wallis H test were used for non-parametric variables, whereas the T test and ANOVA were used for parametric variables. The associations between variables were investigated using correlation analysis and basic linear regression analysis. According to the findings, as disaster literacy increases, individual disaster resilience increases. The individual disaster resilience level of males was higher than that of females, the individual disaster resilience level of married individuals was higher than that of single individuals, and those who have experienced a disaster before have a higher level of individual disaster resilience than those who haven’t experienced a disaster. Males have higher levels of disaster literacy than females. Married individuals have higher disaster literacy levels than singles. As the age increases, the level of individual disaster resilience and disaster literacy increases. It is considered important to develop community-based disaster awareness training programs and strategies to increase individual disaster resilience.

This research paper proposes a simple image processing technique for automatic lameness detection in dairy cows under farm conditions. Seventy-five cows were selected from a dairy farm and visually assessed for a reference/real lameness score (RLS) as they left the milking parlor, while simultaneously being video-captured. The method employed a designated walking path and video recordings processed through image analysis to derive a new computerized automatic lameness score (ALDS) based on calculated factors from back arch posture. The proposed automatic lameness detection system was calibrated using 12 cows, and the remaining 63 were used to evaluate the diagnostic characteristics of the ALDS. The agreement and correlation between ALDS and RLS were investigated. ALDS demonstrated high diagnostic accuracy with 100% sensitivity and specificity and was found to be 100% accurate with a perfect agreement (ρc = 1) and strong correlation (r = 1, P < 0.001) for lameness detection in binary scores (lame/non-lame). Moreover, the ALDS had a strong agreement (ρc = 0.885) and was highly correlated (r = 0.840; 0.796–1.000 95% confidence interval, P < 0.001) with RLS in ordinal scores (lameness severity; LS1 to LS5). Our findings suggest that the proposed method has the potential to compete with vision-based lameness detection methods in dairy cows in farm conditions.

Upper Cretaceous-Tertiary marine clayey-calcareous rocks of the Hekimhan basin contain fibrous clay minerals in significant amounts. Ophiolitic rocks in the provenance area have contributed the elements to form the clay minerals. XRD, SEM, major, trace and REE analyses were applied to samples taken from several stratigraphic sections. Diagenetic minerals such as smectite, dolomite, calcite, gypsum, celestite and quartz/chalcedony are associated with sepiolite-palygorskite group clays. Trace and rare earth elements (REE) are more abundant in palygorskite than sepiolite. REE abundances in the sepiolite-palygorskite are characterized by negative Eu and positive Nd anomalies when normalized with respect to chondrite and shale. Sepiolites with sharp XRD peaks are formed by diagenetic replacement of dolomite and diagenetic transformation of palygorskite, or by direct crystallization from solution. The average structural formula of the sepiolite is:

(Mg7.15Al0.13Fe0.31Cr0.06Ni0.04)(Si11.98Al0.02)O30(OH)4(OH2)4Ca0.03Na0.02K0.02.8H2O

Palygorskite appears to be authigenic by direct precipitation from solution. It exists in both monoclinic and orthorhombic forms with the mean structural formula given below

(Mg2.22Al1.00Ti0.04Fe0.77Cr0.01Ni0.02)(Si7.68Al0.32)O20(OH)2(OH2)4Ca0.07Na0.05K0.10.4H2O

Hydrous Al-silicate deposits are found to the south of Pütürge in Malatya city, Turkey. The surrounding rocks consist of mylonitic granitic gneiss overlain by muscovite gneiss with kyanite-bearing metabasic schist lenses on top which are cut by silica veins containing prismatic tourmaline and speculante. Pyrophyllite is found within kyanite gneisses overlying the granitic gneisses. Fibrous, platy pyrophyllite is developed along the edges and cleavage planes of kyanite, whereas platy bunches of dickite occur as replacements of the relict kyanites as well as crack- and pore-fillings. Rocks forming the hydrous Al-silicate deposit contain 2M1 pyrophyllite, alunite, topaz, paragonite, dravite, dumortierite, chlorite and epidote as early hypogene minerals, and 2M1 dickite, diaspore, gibbsite, speculante, goethite and crandallite/goyazite as late hypogene minerals. On the basis of fluid inclusion and stable isotope data, it is estimated alterations to pyrophyllite and kaolinite occurred at temperatures are of 150 and 100°C, respectively, the minerals being formed by meteoric waters interacting with metamorphic rocks. Trace and REE variations are highly distinctive in terms of enrichment of most trace elements in pyrophyllite, whereas REEs are clearly abundant in dickite, indicating different conditions during formation such as early and late hypogene processes. The pyrophyllitic alteration took place in the late Cretaceous (69–71 Ma), whereas kaolinization occurred later.

Talc deposits, located mainly in three areas of north-central Turkey, are present in the ophiolitic series of the Cretaceous and in siliciclastic rocks of the Paleocene. Talc deposits related to ophiolites are between tectonite and cumulate occurring as beds and/or lenses and 0.1–3 cm thick fracture fillings within a 5 m brecciated zone with a vein-type bedding. Sedimentary-hosted talc beds and semi-rounded to angular talc grains (0.1–2 cm) range in thickness from 0.1 to 30 cm within marls and conglomerates. Talc veins form lenses (a few meters long) and spheroidal and/or ellipsoidal nodules (1–10 cm). Calcite, dolomite, serpentine and/or mixed-layered illite-smectite (I-S) minerals are encountered in the talc samples. Serpentine with positive U and Hf anomalies, and talc with positive Nb and Zr anomalies, and negative Ta and Ce anomalies are typically depleted in P and Ti, based on chondrite-normalized trace element patterns. The light rare earth element content of sedimentary-hosted talc with a negative Gd anomaly is richer than those of ultramafic-hosted talc with a negative anomaly for Eu as well as serpentine. Significantly, talc with a uniquely sedimentary origin tends to be the principal source of Nb, Hf, Zr, La, Ce, Pr and Nd with respect to serpentine. δ18O and δD values for talc range from +13.8 to +17.5‰ and −60 to −36‰, and those of serpentine are +9.4 and −88‰, indicating supergene conditions for sedimentary-hosted talc and hypogene for ultramafic-hosted talc. When compared with seawater, δ18O data indicate temperatures of 68°C and 80–98°C for the sedimentary- and ultramafic-hosted talc formations, respectively, and 100°C for serpentine, suggesting that talcification and serpentinization of ultramafic rocks both occurred at nearly the same time with various stages. All data show that the talc occurrences are divided into two types based on their mode of formation. The first corresponds to a serpentinization stage within the ophiolites. The others are the neoformation products of sedimentary deposition, diagenetic and post-diagenetic processes, respectively. Sedimentary-hosted talc also seems to have inherited trace element and isotopic compositions from the parent ultramafic rocks.

The Antalya Unit, one of the allochthonous units of the Tauride belt, is of critical, regional tectonic importance because of the presence of rifting remnants related to the break-up of the northern margin of Gondwana during Triassic time. Paleozoic — Mesozoic sedimentary rocks of the Antalya Unit consist mainly of calcite, dolomite, quartz, feldspar, and phyllosilicate (illite-smectite, smectite, kaolinite, chlorite, illite, chlorite-smectite, and chlorite-vermiculite) minerals. Illite-smectite (I-S) was found in all of the sequences from Cambrian to Cretaceous, but smectite was only identified in Late Triassic-Cretaceous sediments. R0 I-S occurs exclusively in early-diagenetic Triassic—Cretaceous units of the Alakırçay Nappe (rift sediments), whereas R3 I-S is present in late-diagenetic to low-anchimetamorphic Cambrian—Early Triassic units of the Tahtalıdağ Nappe (pre-rift sediments). Kübler Index (KI) values and the illite content of I-S reflect increasing diagenetic grades along with increasing depth. Major-element, trace-element, rare-earth-element (REE), and stable-isotope (O and H) compositions were investigated in dioctahedral and trioctahedral smectites and I-S samples from the pre-rift and rift-related formations. Both total layer charge and interlayer K increase, whereas tetrahedral Si and interlayer Ca decrease from smectite to R3 I-S. Trace-element and REE concentrations of the I-S are greater in pre-rift sediments than in rift sediments, except for P, Eu, Ni, Cu, Zn, and Bi. On the basis of North American Shale Composite (NASC)-normalized values, the REE patterns of I-S in the pre-rift and rift sediments are clearly separate and distinct. Oxygen (δ18O) and hydrogen (δD) values relative to SMOW (Standard Mean Oceanic Water) of smectite and I-S reflect supergene conditions, with decreasing δ18O but increasing δD values with increasing diagenetic grade. Lower dD values for these I-S samples are characteristic of rift sediments, and pre-rift sediments have greater values. On the basis of isotopic data from these I-S samples, the diagenesis of the Antalya Unit possibly occurred under a high geothermal gradient (>35ºC/km), perhaps originating under typical extensional-basin conditions with high heat flow. The geochemical findings from I-S and smectites were controlled by diagenetic grade and can be used as an additional tool for understanding the basin maturity along with mineralogical data.

A 2 m thick brecciated zone containing magnesian minerals is present at the contact of tectonites and cumulates. Tectonites below this zone comprise serpentinized orthopyroxenite and serpentinite. An alteration zone with vein-type bedding comprises four different levels; from bottom to top they are: (1) green-brown serpentinite with dolomite (0.9 m), (2) light greenish-white dolomite with serpentine (0.5 m), (3) white dolomite with sepiolite (0.4 m), and (4) greenish-white dolomite with smectite-chlorite (0.2 m). The first level has a mineral association of serpentine + dolomite ± calcite ± aragonite, the second level consists of dolomite + serpentine ± calcite or dolomite + magnesite + serpentine, the third level comprises dolomite + sepiolite, and the fourth level is made up of dolomite + chlorite + smectite + serpentine. Dolomite, the main mineral of the alteration zone, occurs as coarse crystals (microsparitic-sparitic) in fractures and as small crystals (microsparitic-micritic) in the matrix, which includes serpentine and gabbro relics. Sepiolite developed at the edges and surfaces of dolomite and as fibrous forms in voids. Cumulate rocks above this zone comprise uralitic gabbros. The occurrences of magnesian minerals developed in three stages: the first stage was the serpentinization of olivine; the second stage was the dissolution of serpentine by groundwater and/or meteoric water containing carbon dioxide; and the last stage was the synthesis of neoformed minerals.

The objective of this study is to show how contract-intensive economic institutions can promote diversity and inclusion of social and political groups in economic and business opportunities provided by governments. Building on the interdisciplinary political economy and governance literatures, two types of economic institutions are identified: rent-seeking and contract-intensive. It is argued that rent-seeking economic activities can reinforce in-group norms, gift-giving practices, and governments' discrimination of groups. However, when contract-intensive activities increase in an economy, they can enhance diversity and inclusion of groups in the marketplace creating opportunity structures outside the state and as businesses press governments toward greater impartiality. Analyses of 165 countries from 1961 to 2011 show that a one standard deviation increase in contract-intensive economic activity is associated with a substantial 18 percent increase in the equality of access to state business opportunities for both social and political groups in the long run.

A prosocial action typically provides a more sizable benefit when directed at those who have less as opposed to those who have more. However, not all prosocial acts have a direct bearing on socioeconomic disadvantage, nor does disadvantage necessarily imply a greater need for the prosocial outcome. Of interest here, welfare impact may depend on the number of beneficiaries but not on their socioeconomic status. Across four preregistered studies of life-saving decisions, we demonstrate that when allocating resources, many people are benevolently partial. That is, they choose to help the disadvantaged even when this transparently implies sacrificing lives. We suggest that people construct prosocial aid as an opportunity to correct morally aversive inequalities, thus making relatively more disadvantaged recipients a more justifiable target of help. Benevolent partiality is reduced when people reflect beforehand on what aspects they will prioritize in their donation decision.

The aim of this study is to evaluate the changes in myocardial functions in children who underwent haematopoietic stem cell transplantation along with associated chemotherapy. Additionally, we evaluated the effect of baseline echocardiographic parameters on mortality. We evaluated 39 patients (mean age 7.4 years) who underwent haematopoietic stem cell transplantation owing to non-malignant disease. The control group included 39 healthy children who had normal cardiac findings. The myocardial functions were evaluated in all subjects by conventional echocardiography and tissue Doppler echocardiography before haematopoietic stem cell transplantation and in the 1st, 3rd, 6th, and 12th month after haematopoietic stem cell transplantation. All patients had normal left ventricular ejection fraction before haematopoietic stem cell transplantation, except one case. Before haematopoietic stem cell transplantation, the patient group had significantly greater mean pulmonary artery pressure and lower tricuspid valve annular plane excursion rate. Baseline E’ velocities for mitral lateral annuli, septum, and tricuspid lateral annuli were lower in the patient group than the control group. The E’ velocities for the left ventricle decreased in the patient group after haematopoietic stem cell transplantation, and then returned to baseline levels at the 6 months. E’ and S’ velocities for tricuspid lateral annuli also decreased after haematopoietic stem cell transplantation and were still depressed in the first year after haematopoietic stem cell transplantation. Baseline E’ velocity for septum was significantly lower in patients who died after haematopoietic stem cell transplantation than patients who survived (p = 0.009). Subclinical impairment in both ventricular functions was observed after haematopoietic stem cell transplantation and the right ventricular functions were affected for longer periods than left ventricle after haematopoietic stem cell transplantation. The myocardial functions should be monitored after the first year of haematopoietic stem cell transplantation.

In the event of a work-related death, Turkish law directs the victim’s family to see the death as accidental and understand monetary compensation as a primary vehicle for justice. Based on interview data from a group of victims’ survivors, I examine how the bereaved make sense of accepting money for their losses. Despite the compliance of these families with monetized justice, the interviews suggest that they also have resentments against it. I show that pressing economic needs, a sense of disenfranchisement, and the limited nature of legal counsel lead the survivors to suppress their frustrations. In turn, many come to narrow their expectations of justice to getting what they think of as a fair sum of money. This situated framework, I argue, works to trivialize concerns about workplace safety. Insofar as the families see monetary compensation through a frame of justice, structural factors behind their losses remain unaddressed. Viviana Zelizer has long treated money as being grounded in meanings and moralities. In the tradition of legal consciousness literature, this article extends Zelizer’s fundamental approach by providing a framework to address how the moral underpinning of money can emerge from and reinforce power imbalances and systemic bias in the legal system.