Sort by
When rhinosinusitis is not just rhinosinusitis: Clinical characteristics and phenotypes of patients with type 2 chronic rhinosinusitis with nasal polyps.

Background and aim:Chronic rhinosinusitis (CRS) is a chronic and recurrent disease that negatively affects patients’ quality of life. CRS has two main phenotypes: CRS with nasal polyps (CRSwNP) and CRS without polyps (CRSsNP). Minimal research has been conducted to study the variability in patients’ characteristics. Therefore, we conducted this study to examine these differences.Methods:A retrospective cohort study included patients with both CRSwNP and CRSsNP. Outcomes included symptom severity, radiographic severity, and number of sinus surgeries. Symptom severity was assessed using the Sino-nasal Outcome Test and the Lund-Mackay CT score was used to determine radiographic severity. Further subgroup analysis was done based on the presence or absence of comorbid asthma.Results:A total of 110 and 106 patients were included in the CRSwNP and CRSsNP groups, respectively. The mean age in the CRSwNP and CRSsNP groups was 50.2 and 48.7, and the proportion of female patients was 40.9% and 58.5%, respectively. No significant difference in symptom severity was noted between CRSwNP and CRSsNP group (68.1±18.6 vs. 73.2±21.27; P=0.097), while the Lund-Mackay score was significantly lower in the CRSsNP group (7.4±2.3 vs. 11.9±3.6; P=0.016). Also, the number of surgeries was significantly lower in the CRSsNP group as compared to the CRSwNP group (P=0.023). Subgroup analysis revealed statistically significant differences between those with and without asthma in patients with CRSwNP in terms of Lund-Mackay scores and number of surgeries (P=0.038 and 0.043), respectively. However, no significant differences were noted in the CRSsNP group (P>0.05).Conclusions:There is a clear variability in the characteristics of patients with CRSsNP and CRSwNP. A similar difference was noted in the CRSwNP group when patients were stratified based on the presence of absence of asthma. This warrants further investigation of potential correlation with the prognosis and optimum treatment strategies of this patient population (www.actabiomedica.it)

Open Access
Relevant
A simple prognostic score based on troponin and presepsin for COVID-19 patients admitted to the emergency department: a single-center pilot study.

Background:The need to determine prognostic factors that can predict a particularly severe or, conversely, the benign course of COVID-19 is particularly perceived in the Emergency Department (ED), considering the scarcity of resources for a conspicuous mass of patients. The aim of our study was to identify some predictors for 30-day mortality among some clinical, laboratory, and ultrasound variables in a COVID-19 patients population.Methods:Prospective single-center pilot study conducted in an ED of an University Hospital. A consecutive sample of confirmed COVID-19 patients with acute respiratory failure was enrolled from March 8th, to April 15th, 2020.Results:143 patients were enrolled. Deceased patients (n = 65) were older (81 vs. 61 years, p <0.001), and they had more frequently a history of heart disease, neurological disease, or chronic obstructive pulmonary disease (p-values = 0.026, 0.025, and 0.034, respectively) than survived patients. Troponin I and presepsin had a significant correlation with a worse outcome. Troponin achieved a sensitivity of 77% and a specificity of 82% for a cut-off value of 27.6 ng/L. The presepsin achieved a sensitivity of 54% and a specificity of 92% for a cut-off value of 871 pg/mL.Conclusion:In a population of COVID-19 patients with acute respiratory failure in an ED, presepsin and troponin I are accurate predictors of 30-day mortality. Presepsin is highly specific and could permit the early identification of patients who could benefit from more intensive care as soon as they enter the ED. Further validation studies are needed to confirm this result. (www.actabiomedica.it)

Open Access
Relevant
The stratigraphic response to the Oligo-Miocene extension in the western Mediterranean from observations on the Sardinia graben system (Italy)

Abstract The Sardinian Cainozoic rifted basin is a useful model for studying the stratigraphic response to the Oligo-Miocene structural extension in the western Mediterranean because it allows precise observations on the relationship between sedimentation and normal faulting based on outcrops and seismic reflection data. The purpose of this paper, essentially of stratigraphic nature is to propose a chronology as precise as possible of the tectonic events and of the sedimentary formations. Indeed the tectono-sedimentary framework is complex, characterized by an extreme facies variability, from continental to marginal transitional and to marine environments (shallow-water, hemipelagic). Rifting, active calc-alkaline volcanism and sea-level changes caused rapid physiographical evolution, which controlled progressive marine ingression. New chronobiostratigraphical data presented in this paper allow correlating the sequences, defining their environment and depth of deposition and specifying precisely the timing of pre-, syn-, and post-rift stages in the Oligo-Miocene graben system. In southwestern Sardinia during the middle-late Eocene, after the Pyrenean phase, a continental graben (Cixerri), W-E oriented, preceded the Oligo-Miocene extension, which reactivated inherited Eocene and Palaeozoic faults. The calc-alkaline volcanic activity ranging from 32 to 13 Ma, provides a good estimate for the time span of the west-dipping Apenninic subduction responsible for the continental extension and the oceanic accretion in the western Mediterranean. In Sardinia the Oligo-Miocene extensional tectonics started in a continental environment, preceding the earliest calc-alkaline volcanic products (32 Ma). The marine ingression is dated to the late Chattian-Aquitanian interval and corresponds to a rapid deepening of the Oligo-Miocene graben system of tectonic origin. The end of the rifting i.e. the end of normal faulting activity is pre-middle Burdigalian in age. When Sardinia was in the post-rift stage, extension continued until late Burdigalian – Langhian in the Algero-Provençal basin with oceanic accretion and rotation of the Corsica-Sardinia block (CSB).

Relevant