Simultaneous Endocardial and Epicardial Delineation of 3D Reentrant Ventricular Tachycardia

BackgroundMechanisms of scar-related ventricular tachycardia (VT) are largely based on computational and animal models that portray a 2-dimensional view.ObjectivesThe authors sought to delineate the human VT circuit with a 3-dimensional perspective from recordings obtained by simultaneous endocardial and epicardial mapping.MethodsHigh-resolution mapping was performed during 97 procedures in 89 patients with structural heart disease. Circuits were characterized by systematic isochronal analysis to estimate the dimensions of the isthmus and extent of the exit region recorded on both myocardial surfaces.ResultsA total of 151 VT morphologies were mapped, of which 83 underwent simultaneous endocardial and epicardial mapping; 17% of circuits activated in a 2-dimensional plane, restricted to 1 myocardial surface. Three-dimensional activation patterns with nonuniform transmural propagation were observed in 61% of circuits with only 4% showing transmurally uniform activation, and 18% exhibiting focal activation patterns consistent with mid-myocardial reentry. The dimensions of the central isthmus were 17 mm (12 to 28 mm) × 10 mm (9 to 19 mm) with 55% exhibiting a minimal dimension of <1.5 cm. QRS activation was transmural in 63% and located 43 mm (34 to 52 mm) from the central isthmus. On the basis of 6 proposed definitions for epicardial VT, the prevalence of an epicardial circuit ranged from 21% to 80% in ischemic cardiomyopathy and 28% to 77% in nonischemic cardiomyopathy.ConclusionsA 2D perspective oversimplifies the electrophysiological circuit responsible for reentrant human VT and simultaneous endocardial and epicardial mapping facilitates inferences about mid-myocardial activation. Intricate activation patterns are frequently observed on both myocardial surfaces, and the epicardium is functionally involved in the majority of circuits. Human reentry may exist within isthmus dimensions smaller than 1 cm, whereas QRS activation is often transmural and remote from the critical isthmus target. A 3-dimensional perspective of the VT circuit may enhance the precision of ablative therapy and may support a greater role for adjunctive strategies and technology to address arrhythmogenic tissue harbored in the mid-myocardium and subepicardium.     

长期服用抗精神病药脑电图异常相关因素分析

〔摘 要〕 目的：观察长期服用抗精神病药物的精神疾病患者的脑电图异常检出率，对其影响因素进行分析，提出预防措施。 方法：选取 2020 年 6 月至 2020 年 12 月期间在泉州市第三医院住院的长期服用抗精神病药物患者 256 例进行脑电图检查， 统计检出异常率；并观察不同药物种类、不同年龄段、不同服药时间患者的脑电异常率，对脑电图异常的危险因素进行分析。 结果：256 例患者中 154 例（60.16 %）出现脑电图异常，其中轻度异常在临床中最常见，重度异常最少见。不同药物种类中， 氯氮平使用者脑电图异常率最高；不同年龄段中，年龄＞ 60 岁脑电图异常率较高。结论：长期服用抗精神病药物患者出现 脑电图异常的影响因素主要为年龄＞ 60 岁、长期服用氯氮平，故临床需结合患者年龄合理选择药物，尽量选择对脑电图影 响较小的药物，且密切监测患者病情变化，适当调整或优化治疗方案。     

Emotion recognition from physiological signals

Emotion recognition is one of the great challenges in human–human and human–computer interaction. Accurate emotion recognition would allow computers to recognize human emotions and therefore react accordingly. In this paper, an approach for emotion recognition based on physiological signals is proposed. Six basic emotions: joy, sadness, fear, disgust, neutrality and amusement are analysed using physiological signals. These emotions are induced through the presentation of International Affecting Picture System (IAPS) pictures to the subjects. The physiological signals of interest in this analysis are: electromyogram signal (EMG), respiratory volume (RV), skin temperature (SKT), skin conductance (SKC), blood volume pulse (BVP) and heart rate (HR). These are selected to extract characteristic parameters, which will be used for classifying the emotions. The SVM (support vector machine) technique is used for classifying these parameters. The experimental results show that the proposed methodology provides in general a recognition rate of 85% for different emotional states.     

Efficient responses to host and bacterial signals during Vibrio cholerae colonization

Vibrio cholerae, the microorganism responsible for the diarrheal disease cholera, is able to sense and respond to a variety of changing stimuli in both its aquatic and human gastrointestinal environments. Here we present a review of research efforts aimed toward understanding the signals this organism senses in the human host. V. cholerae’s ability to sense and respond to temperature and pH, bile, osmolarity, oxygen and catabolite levels, nitric oxide, and mucus, as well as the quorum sensing signals produced in response to these factors will be discussed. We also review the known quorum sensing regulatory pathways and discuss their importance with regard to the regulation of virulence and colonization during infection.     

婴幼儿铁缺乏症与脑发育障碍相关性研究

铁缺乏症（ID）是儿童期最为常见的微量元素缺乏症。胎儿晚期、新生儿和婴幼儿期是大脑发育的关键时期，这些阶段的铁缺乏可导致大脑发育的不可逆性损害，包括情感行为异常、认知功能下降和注意力缺陷等脑功能异常表现，并可能持续至成人阶段，必须引起足够的重视。该文就生命早期铁缺乏导致大脑发育障碍的主要机制以及干预措施等研究进展进行综述。     

Hemoglobins With High Oxygen Affinity Leading to Erythrocytosis. New Variants and New Concepts

This review brings some new insights on erythrocytosis of genetic origin related to problems of oxygen delivery by hemoglobin (Hb). A few molecular mechanisms are individualized among the about 100 Hb variants that cause compensatory erythrocytosis. The most frequently observed structural modifications are localized in the α1β2 interface, or at the C-terminal. They impair formation of a stable T state. Others mutations modify directly or indirectly the surrounding of the heme and the site where oxygen binds. A special interest is brought to the dose effect considering the possibility for formation of hybrid tetramers with altered oxygen binding properties. Homozygous cases, and patients who are compound heterozygotes for a high oxygen affinity Hb and a thalassemia (thal), are discussed. Several examples are provided, specially documented for Hb Olympia [β20(B2)Val→Met] and Hb Saint Nazaire [β103(G5)Phe→Ile]. Other mechanisms leading to erythrocytosis are discussed, and finally, an algorithm is proposed for etiological diagnosis.     

Towards a physiological signal-based access solution for a non-verbal adolescent with severe and multiple disabilities

Objective: To find physiologically arousing stimuli and labile physiological channels in a non-verbal adolescent with severe and multiple congenital disabilities, who did not have a reliable means of communication.

Methods: The client was repeatedly presented with visual and audiovisual stimuli, representing variations of six contextual factors over three sessions in a one month period. For each stimulus, reactions were detected in the client’s four peripheral autonomic nervous system signals using a rule-based classification algorithm.

Results: During the presentation of audiovisual stimuli, the number of physiological reactions significantly differed from that observed in baseline (χ²?=?3.93, p?=?0.0476). Aural stimuli articulated in an unfamiliar voice, and aural stimuli containing anticipatory patterns were also physiologically arousing. Fingertip temperature was the client’s most labile physiological signal.

Conclusions: The results of this case study suggest that physiological data may complement caregiver acumen in deciphering the reactions of non-verbal clients with severe and multiple disabilities.     

Dydrogesterone treatment for menstrual-cycle regularization in routine clinical practice: a multicenter observational study

Dydrogesterone is an oral retroprogesterone widely used to treat progesterone deficiencies, including irregular menstrual cycles (MCs). This prospective, non-interventional, single-arm, post-marketing, observational study evaluated the effects of dydrogesterone on MC regularization. Women aged 18–40 years who had been prescribed dydrogesterone to treat irregular MCs due to progesterone deficiency were enrolled across 64 centers in Russia, Ukraine, Kazakhstan and Uzbekistan. Study objectives included: patients reporting ≥1 regular MC during treatment; the number of regular MCs after the end of treatment over a 6-month follow-up (FU) period. In total, 996 women were enrolled. Of those who completed treatment, 946/955 patients (99.1%) achieved ≥1 regular MC. During FU, 680/860 patients (79.1%) maintained ≥6 regular MCs. Patient grading of menstrual pain and anxiety decreased significantly during treatment (p?≤?0.0001 versus baseline); this persisted during FU. Dydrogesterone was associated with high or very high patient satisfaction (856/955; 89.6%); the clinical response was considered good or excellent in 819/955 patients (85.8%). In total, 16/986 patients (1.6%) reported an adverse event (AE); two had serious AEs (SAEs) (unrelated to treatment) and three discontinued treatment due to non-SAEs. Dydrogesterone therapy was effective in achieving MC regularization and reducing menstrual pain and anxiety, during both treatment and 6-month FU.     

Critical slowing down suggests that the western Greenland Ice Sheet is close to a tipping point

The Greenland Ice Sheet (GrIS) is a potentially unstable component of the Earth system and may exhibit a critical transition under ongoing global warming. Mass reductions of the GrIS have substantial impacts on global sea level and the speed of the Atlantic Meridional Overturning Circulation, due to the additional freshwater caused by increased meltwater runoff into the northern Atlantic. The stability of the GrIS depends crucially on the positive melt-elevation feedback (MEF), by which melt rates increase as the overall ice sheet height decreases under rising temperatures. Melting rates across Greenland have accelerated nonlinearly in recent decades, and models predict a critical temperature threshold beyond which the current ice sheet state is not maintainable. Here, we investigate long-term melt rate and ice sheet height reconstructions from the central-western GrIS in combination with model simulations to quantify the stability of this part of the GrIS. We reveal significant early-warning signals (EWS) indicating that the central-western GrIS is close to a critical transition. By relating the statistical EWS to underlying physical processes, our results suggest that the MEF plays a dominant role in the observed, ongoing destabilization of the central-western GrIS. Our results suggest substantial further GrIS mass loss in the near future and call for urgent, observation-constrained stability assessments of other parts of the GrIS.

During the last century, the Greenland Ice Sheet (GrIS) has lost mass at an accelerating rate (1, 2). The mass loss is caused by solid ice discharge into the North Atlantic and surface melting due to increasing temperatures. The relative contribution of the latter has increased from 42% before 2005 to 68% between 2009 and 2012, and surface runoff caused 84% of the increase in mass reduction since 2009 (3). The complete melting of the GrIS would cause a global sea level rise of more than 7 m (4, 5). Continued melting of the GrIS has been suggested to potentially lead to a collapse of the Atlantic Meridional Overturning Circulation via increased freshwater flux into the North Atlantic (6, 7), which may, in turn, trigger a cascade of transitions in additional tipping elements such as the Amazon rainforest and the tropical monsoon systems (6, 8–10).In addition to the centennial-scale variability associated with the increasing trend in mean temperatures related to anthropogenic climate change, the pace of mass loss has decadal-scale fluctuations caused by natural variations in external oceanic and atmospheric forcing. The imprints of these natural, decadal-scale fluctuations are spatially heterogeneous across the GrIS. Since the early 2000s, periods of persistently negative phases of the North Atlantic Oscillation (NAO) and a positive phase of the East Atlantic Pattern (11) have led to a weakening and southward shift of the jet stream, and more persistent blocking (12) over Greenland during summer, resulting in overall increased mass reduction rates (2, 13). On the other hand, a slowing down of mass loss since 2013—which inverted again in 2019—was caused by more periods with a persistent positive NAO (14). Moreover, recent observations show that the Jakobshavn glacier has been advancing again since 2016 due to anomalous wintertime heat loss in the boundary current around southern Greenland (15). However, these natural fluctuations do not have a sustained impact on melt rates comparable to the longer-term trend toward overall increasing melt rates caused by anthropogenic global warming (Fig. 1A).Open in a separate windowFig. 1.(A) Summer sea level temperatures from the Ilulissat station in CWG (25) (blue curves) and Arctic temperature anomalies (26) (red curves). The linear trend of the station data (dashed blue curve) corresponds to 1.3 °C warming per century. Arctic temperature anomalies are shown only for comparison; only the station data (blue curves) are used for our analysis. (B) Melt rates from the CWG ice core stack (blue curve) and the NU peninsula core (red curve), given as z scores with respect to a normal distribution (18). (C) Detrended logarithmic CWG (blue curve) and NU (red curve) melt rates. A Gaussian filter with bandwidth σ=30 y was used for detrending. The runoff and melt time series are preprocessed in this way before computing the EWS indicators to exclude potential biases by underlying trends; in particular, we take the logarithm of the melt rates in order to account for skewed data distributions. (D) The variance of the CWG (blue curves) and NU (red curves) melt rates. (E) The AC1 of the CWG (blue curves) and NU (red curves) melt rates. Note that the AC1, despite a significantly positive trend, appears to have at least temporarily stabilized in the last few decades. It should be noted, however, that the AC1 is generally influenced by (multi)decadal variability (27). The window size for computing the variance and the AC1 is w=70 y, and values are plotted at the windows’ endpoints. Data for the first w=70 y are omitted to ensure that all windows contain the same number of data points. The dashed lines in D and E indicate linear trends of the variance and AC1, and P values for positive slopes as determined from a phase surrogate test are indicated in the legend (see Materials and Methods). The statistical significance of the positive trends is robust across wide ranges of the bandwidth σ and the sliding window size (SI Appendix, Fig. S1).Early model simulations suggest that melting of the GrIS is inevitable beyond a critical global mean temperature threshold of 0.8 °C to 3.2 °C above preindustrial levels, with a best estimate of 1.6 °C (16). More recent comprehensive modeling results show that, for the representative concentration pathway 8.5 (RCP8.5), the GrIS melts entirely until AD 3000 (5). Arctic temperatures have increased more than the global average (17) (Fig. 1A), and the nonlinear increase in GrIS melt rates and runoff that have recently been detected (18) (Fig. 1B) suggests that the critical temperature threshold may be closer than previously thought. We emphasize that the surface mass balance turning negative is not a necessary condition for stability loss, and the temperature may reach a critical threshold years before a turning point in the mass balance (16).Idealized models of critical transitions in natural systems suggest that the loss of stability of an equilibrium (fixed point) is observable before the abrupt transition (19). In dynamical systems with random forcing, one can show that, if a system approaches a bifurcation where an equilibrium point loses its stability, the variance of the fluctuations around the equilibrium will increase, as will the characteristic decay time of the autocorrelation function of these fluctuations. The change in dynamics that occurs as stability is lost is often called critical slowing down, and the associated statistical precursor signs in terms of rising variance and lag-one autocorrelation (AC1) are called early-warning signals (EWS) (19). Such statistical EWS associated with critical slowing down are, for example, detectable in the temperature proxy from the North Greenland Ice Core Project before several of the Dansgaard–Oeschger events of the last glacial interval (20, 21), as well as before other abrupt transitions in past climates (22). In the context of anthropogenic global warming, EWS are expected to precede potential abrupt transitions in the Earth system’s major tipping elements, such as the polar ice sheets, the Atlantic Meridional Overturning Circulation, or the tropical monsoon systems (23). We investigate here a possible tipping point for the GrIS based on the theory of critical slowing down.In the following, we will first show that central-western Greenland (CWG) melt rates exhibit robust and significant EWS. We then reconstruct the corresponding CWG ice sheet height changes and show that they can be captured well by a simple model focusing on the melt elevation feedback (MEF). We then demonstrate that pronounced EWS can also be found in the fluctuations of the reconstructed ice sheet height around the equilibrium of the model and show that these EWS are consistent with the theoretical expectations provided by the MEF model.