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A strong negative anomaly of seismic wave velocities at the core-mantle boundary (the Perm Anomaly) beneath the East European platform is attributed to the remnant of a deep mantle upwelling. The interaction between the upwelling and the East European lithosphere in the geological past and its resulting surface manifestations are still poorly understood. Using mantle plume modelling and global plate motion reconstructions, we show here that the East European lithosphere is likely to have been situated over the weakening Perm Anomaly upwelling for about 150–200 million years. As the East European platform moved above the Perm Anomaly in post-Jurassic times, the vertical tectonic movements recorded in sedimentary hydrocarbon-rich basins show either hiatus/uplift or insignificant subsidence. Analytical modelling of heat conduction through the lithosphere demonstrates that the basins have been slowly heated for a long time by the Perm Anomaly upwelling, creating suitable conditions for hydrocarbon maturation. This suggests a profound relationship between mantle plume dynamics, basin evolution, and hydrocarbon generation. Since the Jurassic, East European basins have likely been situated over a weakening mantle upwelling, which heated the basins and created suitable conditions for hydrocarbon maturation, according to geodata combined with modelling. [ABSTRACT FROM AUTHOR]

This study aims to detect residual thermal anomalies along the path of a hotspot beneath the continental lithosphere using gradiometry data. We calculate perturbations in gravity vectors and gradients by employing a simple thermal anomaly model. The results highlight that the horizontal components of Bouguer gravity gradients, sensitive to source structure and elongation, exhibit substantial magnitudes, exceeding current detection levels. To improve signals from sources of different sizes and orientations, we apply a filtering approach involving wavelet transforms and rotated local frames. We also assess the impact of lateral crustal variations on the gravity field by introducing random density anomalies and a seismic crustal model, testing the method's ability to distinguish between these anomalies and thermal sources. Using Gravity field and steady‐state Ocean Circulation Explorer satellite data, we generated scale‐orientation diagrams aiming to identify signals aligned with the direction of plate movement and with a spatial scale of a few hundred kilometers (scale of the plumes). Maps of filtered Bouguer gravity gradients aligned with hotspot trajectories are generated for all continental hot plumes, with the position and the age of the intraplate volcanism to support the interpretation. While we do not show a clear signal in regions that are too tectonically complex or with lateral variations in the crust or at the lithospheric boundary correlated with the hotspot trace, we found observed signals with expected sign and amplitude over Hoggar, Tibesti, Darfour and Cameroon tracks in Africa and over Iceland and Jan Mayen in Greenland. However, determining corresponding mass source depths remains a complex task. Plain Language Summary: This study aims to detect residual heat patterns from hotspots beneath the continental lithosphere by analyzing gravity changes using gradiometry data. The results reveal significant gravity variations, particularly horizontally, suggesting the presence of heat sources beyond current detection capabilities. To improve signal detection for varied heat source sizes, we employ a filtering approach with wavelet transforms and rotated frames. The impact of crustal gravity variations is also considered, testing the ability to distinguish between different anomalies. Utilizing Gravity field and steady‐state Ocean Circulation Explorer satellite data, we create diagrams identifying signals linked to plate movement and heat source size, and we generate maps displaying filtered gravity gradients changes along hotspot paths on continents. While complex tectonic regions show no clear signal, expected signals are observed over specific tracks in Africa and Greenland. Determining the depth of corresponding mass sources remains a challenging aspect of the study. Key Points: We reconstruct hotspots trajectories on the continental lithosphere and we superimpose the position of the age of intraplate volcanismWe build maps of Bouguer gravity gradients filtered at the spatial scale of a few hundred kilometers and oriented along the trajectoriesWe show that gradiometry data have the potential to track hotspots in the continental lithosphere for tens of millions years [ABSTRACT FROM AUTHOR]

Introduction: In patients with haemophilia, repeated bleeding in large joints leads to chronic haemophilic arthropathy, a rare disease that can be managed surgically with ankle arthrodesis or with total ankle replacement (TAR). TAR has been reported to provide good surgical results in the medium/long‐term and allow preservation of joint mobility but the medical therapeutic management of the patients has not been described. Aim: To describe the medical therapeutic management of TAR. Methods: All patients with haemophilia A/B, with haemophilic ankle arthropathy, and who underwent TAR between April 2006 and October 2019 were retrospectively included. Factor consumption, perioperative and early complications, volume of blood lost, and orthopaedic data were collected. Results: A total of 25 patients underwent 29 TAR (mean age was 44.7 years [range: 26–65]). In the 17 patients with HA without history of anti‐FVIII inhibitor, the mean ± SD consumption the day of surgery was 116 ± 16 UI/kg when clotting factors were administered by continuous infusion, 106 ± 13 UI/kg when SHL factors were administered by bolus infusion, and 75 ± 22 UI/kg when EHL factors were administered by bolus infusion. During hospitalisation, the mean factor cost was €38,073 (83.7% of the total cost of surgery). Mean blood loss was significantly lower in patients treated with tranexamic acid (164 mL, range: 40–300) than in those not (300 mL, range: 70–800; p =.01). Six patients had haematoma. The 10‐year survival free of any prosthesis removal/arthrodesis was estimated to be 92.2% (95% CI [83; 100]). Conclusion: The medical therapeutic management of TAR is complex, carried out by a multidisciplinary team but effective in avoiding the occurrence of complications. [ABSTRACT FROM AUTHOR]

Background: Previous studies have examined the effect of concomitant triceps surae lengthening on ankle dorsiflexion motion at the time of total ankle arthroplasty (TAA). As plantarflexor muscle-tendon structures are important for producing positive ankle work during the propulsive phase of gait, caution should be exercised when lengthening triceps surae, as it may decrease plantarflexion strength. In order to develop an understanding of the work of the anatomical structures crossing the ankle during propulsion, joint work must be measured. The aim of this explorative study was to assess the effect of concomitant triceps surae lengthening with TAA on the resultant ankle joint work. Methods: Thirty-three patients were recruited to the study and divided into 3 groups of 11. The first group underwent both triceps surae lengthening (Strayer and TendoAchilles) and TAA (Achilles group), the second group underwent only TAA (Non-Achilles group), and the third group underwent only TAA, but had a greater radiographic prosthesis range of motion (Control group) compared to the first 2 groups. The 3 groups were matched in terms of demographic variables and walking speed. All patients underwent a 3D gait analysis 1 year after surgery to measure intersegmental joint work using a 4-segmented kinetic foot model. An analysis of variance (ANOVA) or Kruskal-Wallis test was used to compare the 3 groups. Results: The ANOVA showed significant differences between the 3 groups. Post hoc analyses suggested that (1) the Achilles group had less positive work at the ankle joint than the Non-Achilles and Control groups; (2) the Achilles group produced less positive work performed by all foot and ankle joints than the Control group; and (3) the Achilles and Non-Achilles groups absorbed less energy across all foot and ankle joints during the stance phase than the Control group. Conclusion: Concomitant triceps surae lengthening in TAA may reduce the positive work at the ankle joint. Level of Evidence: Level III, retrospective comparative study. [ABSTRACT FROM AUTHOR]

The so-called Croatian Orthodox Church was an ephemeral creation of the Ustachi regime founded in 1942 in Croatia. The analysis of its founder Malsinov, an archbishop of the Russian Orthodox Church in exile, doubtlessly reveals his anti-communist motives, which were also behind his cooperation with the Romanian Orthodox Church through Metropolitan Bessarion. The two prelates ordained Spyridon Mifka as bishop of Sarajevo, an extension of the same Croatian Orthodox Church. The anti-communist aspect of this cooperation continued in exile following the establishment of Soviet rule in Eastern Europe. The climate and reasons that led Maslinov to become the head of this phantom institution, however, cannot be fully elucidated at present.