bluuebunny/crossref_metadata_2025 huggingface dataset:
EFETIVIDADE DA CIRURGIA ROBÓTICA EM PACIENTES COM CARCINOMA COLORRETAL: UMA ANÁLISE COMPARATIVA DE DESFECHOS PÓS-OPERATÓRIOS
Authors: Faria Ivan Aurélio Fortuna Kalil de , Ruiz Edwin Vilelo , Melo Arthur Lins , Dias Maria Fernanda Figueiredo Lanza , Franco Gabriel Bordalí , Barreto Sandrieler Nunes , Lustosa Jennifer Mendes , Faria Anna Beatriz Inácio Fortuna Kalil de , Ruas Anna Paula Paulino , Oliveira Ruy Sergio Sampaio Rezende de
Published: August 2024

A cirurgia robótica emergiu como uma alternativa avançada para o tratamento do carcinoma colorretal, oferecendo benefícios potenciais em comparação com as técnicas tradicionais de laparoscopia e cirurgia aberta. Esta revisão integrativa teve como objetivo avaliar a efetividade da cirurgia robótica em pacientes com carcinoma colorretal, por meio de uma análise comparativa de desfechos pós-operatórios, incluindo complicações, tempo de recuperação, margem de ressecção tumoral, e qualidade de vida. Foram incluídos 28 estudos publicados entre 2010 e 2024, abrangendo ensaios clínicos randomizados, estudos de coorte e revisões sistemáticas. Os resultados demonstraram que a cirurgia robótica está associada a uma menor taxa de complicações pós-operatórias e uma recuperação mais rápida, além de proporcionar margens de ressecção tumoral adequadas e uma melhor qualidade de vida no pós-operatório. No entanto, não foram observadas diferenças significativas nas taxas de recidiva tumoral ou sobrevida global quando comparada às técnicas convencionais. Esses achados sugerem que a cirurgia robótica é uma opção eficaz para o tratamento do carcinoma colorretal, com benefícios substanciais nos desfechos imediatos, embora seu impacto a longo prazo e a viabilidade econômica ainda precisem ser mais investigados.
Shaping the crustal structure of the SW-Alpine Foreland: Insights from 3D Geological modeling
Authors: Bienveignant Dorian , Nouibat Ahmed , Sue Christian , Rolland Yann , Schwartz Stéphane , Bernet Matthias , Dumont Thierry , Nomade Jérôme , Caritg Séverine , Walpersdorf Andrea
Published: August 2024

Reactivation processes play a significative role in the localization of deformation but still remain hard to establish at the lithospheric scale. In this work, we built a 3D structural model, which enables to bridge the gap between the main tectonic structures observed at the surface and the geometry of the major interfaces (the Moho and the top of the basement) inferred by geophysical data acquired in the external Western Alps and their foreland. The geometry of these tectonic structures is interpreted in relation to their geodynamic evolution. The main results of this study highlight: (1) a strong contribution of thick-skinned Pyrenean-Provence and Alpine tectonics, (2) a lithospheric rooting of Variscan shear zones and related faults, and (3) the regional-scale influence of these inherited structures on the post-Paleozoic strain localization of the study area. Our 3D model shows that the pattern of Variscan shear zones, that were developed at the end of the Paleozoic involved the whole crust, as emphasized by the Moho offsets. These shear zones were reactivated and localised Meso-Cenozoic deformation. The Variscan deformation pattern controlled the geometry of extensional basins, the propagation of Pyrenean-Provence deformation, and finally the Alpine deformation at crustal scale. Our 3D model shows minor crustal thickening (ca. 40 km) located below the Pelvoux External Crystalline Massif, which probably resulted from both Pyrenean and Alpine tectonic phases. In contrast, the southern part of the Alpine front shows a thinned crust (ca. 18 km) resulting from extensional Meso-Cenozoic phases between the Cevennes margin and the Durance basin.
Revealing the temporal dynamics of fault reactivation in the W-Alpine foreland using in-situ U−Pb dating on calcite
Authors: Bienveignant Dorian , Schwartz Stéphane , Rolland Yann , Bernet Matthias , Léger Julien , Vezinet Adrien , Bertauts Maxime , Boullerne Clara , Dumont Thierry
Published: August 2024

Long-term study of fault system activity is crucial for understanding the dynamics of orogeny structuring and the formation of peripheral basins, the impact of tectonic inheritance, seismic hazard assessment, and the estimating the coupling of deformation and erosion. At the junction of several orogenic domains, the foreland basin of the Western Alps exhibits a complex structural pattern inherited from the superposition of tectonic events since the late Paleozoic. Despite this knowledge, the absolute age of fault formation and reactivation remains poorly understood, primarily due to the difficulty of dating uranium-poor minerals typically found in sedimentary environments. This study proposes an integrated approach of structural analysis of deformations in the field combined to the recently developed U-Pb in-situ dating method on syn-tectonic calcite to fill this gap. By focusing on the subalpine massifs (from the Vaucluse massif to the Bornes massif), this work aims to constrain the dynamics of the Alpine foreland structuring over a wide temporal and spatial scale. Additionally, this study area presents diverse geodynamic characteristics, making it an ideal site to test the applicability of recent U-Pb in-situ dating methods.
Unveiling the Tectono-Metamorphic Framework of northern Dora-Maira Massif (Western Alps): new preliminary data from Pellice and Chisone valleys 
Authors: De Cesari Francesco , Dana Davide , Montomoli Chiara , Iaccarino Salvatore , Rubatto Daniela , Corno Albero , Carosi Rodolfo
Published: August 2024

Dora-Maira (DM) Massif plays a crucial role in understanding the geodynamics that shaped the Alpine belt. Extensive studies have been mostly conducted in the southern portion of DM (e.g., Chopin et al., 1991). Recent investigations (Manzotti et al. 2022; Nosenzo et al., 2024) have renewed interest in the northern portion of the massif. These authors provided new structural and metamorphic data on the area, particularly with the discovery of a new ultra-high-pressure unit (the Chasteiran Unit). Despite these significant contributions, there are many open questions at the scale of the entire DM. In this contribution we present new data collected within the framework of the CARG mapping project (Foglio 172-Pinerolo). Our aim is to shed light on the structural and metamorphic architecture in the Val Pellice and Val Chisone areas. We present a geological map with geological cross-sections, at a scale of 1:10,000, covering the region between Colle Lazzarà and Colle Vaccera. Additionally, we conducted preliminary microtectonic, petrographic, and geochronological studies to reconstruct the structural and metamorphic evolution of the investigated area. In this relatively unexplored part of DM, three distinct tectono-metamorphic units are exposed, which are (from bottom to top): Pinerolo-Sanfront Unit; Chasteiran Unit, and the poly-cyclic basement unit of the DM massif. Particular attention has been paid to mapping the tectonic contact related to the Chasteiran Unit, which is sandwiched between the other two tectono-metamorphic units. This contact has been traced further southward, up to Colle Vaccera, compared to previous investigations. To reconstruct the metamorphic history, we present preliminary P-T data obtained from ongoing analysis of the micaschist in the Pinerolo-Sanfront Unit. At least four deformation phases have been recognized: (i) the D1 phase, associated with the development of an S1 foliation preserved only within the microlithons; (ii) a second deformation phase, associated with the development of the main foliation (S2) characterized by an E-W trending lineation, (iii) the D3 deformation phase overprinting D2 structures; (iv) a D4 deformation phase that developed during the doming of the Dora-Maira Massif; and finally, (iv) a D4 deformational phase that developed during the doming of the Dora-Maira Massif. In addition, we present preliminary geochronological data performed on Freidour-type orthogneiss in the Pinerolo-Sanfront Unit, refining the Permian age obtained from previous studies (Bussy & Cadoppi 1996).
This contribution has been performed whit the found of the CARG mapping project.
Regional Strike-Slip Structures in the Internal Dinarides: Insights from the Zvornik Fault
Authors: Mladenović Ana , Gajić Violeta , Sokol Kristijan , Prelević Dejan
Published: August 2024

The Dinarides represent a part of a double-vergent Dinaric – Carpatho – Balkan orogenic chain that formed as a response to the closure of a branch of the Tethys ocean in the latest Jurassic and subsequent convergence between the Adriatic microplate and the European continent, which is still active in the recent times. Different in convergence rates, this driving force of tectonics in the Balkans produced different kinematics of the fault structures in the central part of the Balkan Peninsula. General opinion is that from the Cretaceous times up to the Oligocene the fault kinematics in the area acted in a compressional regime, which, after the extensional episode in the Miocene, continued as a strike-slip regime in the neotectonic time. However, some regional structures seem to show evidence of oblique-slip kinematics much earlier, already in the Late Cretaceous times. Some of these pieces of evidence are related to the existence of intracontinental basalts related to the fault structures, asymmetric pull-apart sedimentary basins, tectonic structures, etc.In this contribution, we will present the most recent results of the study of one of the most prominent tectonic structures of the Internal Dinarides, the well-known Zvornik fault (suture), and its southward continuation in the area of the Jelica Mts. in western Serbia. We will show evidence of the Late Cretaceous activity of this regional fault and discuss its importance in the context of the formation of Late Cretaceous basaltic magmas and specific sedimentary basins in this area.Acknowledgement: This research was financed by the Science Fund of the Republic of Serbia through project RECON TETHYS (7744807).
Swiss Alps 3D: building a large-scale 3D underground model of the Central European Alps
Authors: Musso Piantelli Ferdinando , Ursprung Anina , Baland Pauline , Baumberger Roland
Published: August 2024

The Swiss Geological Survey (SGS) is the competence centre for the investigation of the subsurface and georesources of the Swiss Confederation. It provides up-to-date, high-quality spatial reference data for the entire country in the form of nationwide geological 2D datasets and 3D geological models. Between 2024 and 2030, the SGS is funding the Swiss Alps 3D (SA3D) project, which consists of eight research projects involving multiple universities and aims to develop a consistent large-scale underground 3D geological model of the main contacts and structures of the Central Alps.In this presentation we show the workflow that will be used to build the SA3D model and the project plan until 2030. The main challenge for 3D modelling in Alpine regions is the lack of subsurface data (seismic data, borehole data, etc.). However, the high relief, the sparse vegetation and the large number of scientific studies make these regions an excellent site for advanced surface-based 3D geological modelling. In addition, researchers from several universities in Switzerland and Europe, as well as the SGS, have a wide range of expertise in regional geology and 3D geological modelling. SA3D aims to bring all this know-how together in teams of people with diverse expertise. The result will be a large-scale 3D geological model validated by scientific arguments.Based on the new Tectonic Map of Switzerland 1:500'000 (swisstopo, 2024), the target area is divided into eight 3D modelling projects according to their paleogeographic origin and structural evolution. The resulting models will be then compiled into a single large-scale 3D model. Within each project, the target structural and lithostratigraphic contacts are modelled at the equivalent scale of 1:25’000. A network of regularly spaced (1000 m) geological cross sections and scientific concepts, discussed and reviewed by the different modelling teams, are then developed to strengthen the modelling interpolation. The workflow developed for the SA3D project offers the chance to gain validation approaches for domains only weakly constrained by/ or with no subsurface data available, by generating a 3D model that integrates multiscale geological data unified by a common dataset provided by the Tectonic Map.SA3D will generate key knowledge by establishing an experienced modelling community and 3D visualization of the main geological structures and lithostratigraphic boundaries of the Central European Alps. The development of such a project will provide a framework model of the area as a basis for higher resolution 3D geological models to be used for infrastructure planning, groundwater studies, natural hazard assessment, education and research purposes. In addition, the models will facilitate access to strategic subsurface knowledge, which is essential for the management and exploration of geo-resources and geo-energy.
Syn-collisional exhumation of the San Bernardino eclogites (Adula unit, central Alps)
Authors: Montemagni Chiara , Monti Riccardo , Malaspina Nadia , Zanchetta Stefano
Published: August 2024

In the Central Alps, the Adula unit reveals (U)HP mafic and ultramafic rocks, offering insights into the subduction history of the distal European margin during the final phases of the Europe-Adria collision. The Adula unit, one of the highest basement units in the Lower Penninic nappe stack of the Lepontine Dome, is located between non-eclogitic Lower Penninic units, Simano and Lucomagno, derived from distal European margin below and non-eclogitic Middle Penninic units, Tambò and Suretta, above, composed of pre-Permian basement and Mesozoic covers of the Briançonnais terrane. The upper tectonic boundary of the Adula unit is a complex shear zone known as the Misox zone, which contains lenses of non-metamorphic sheared Mesozoic sediments and volcanics.It is widely accepted that Suretta, Tambò and Adula units were thrusted over each other during extensive mylonitic shearing directed northward. However, the current structural arrangement and the metamorphic discontinuity between the (U)HP Adula unit and the eclogite-free Tambò-Suretta complex suggest the presence of a normal-sense shear zone. This shear zone, at some point during the tectonic evolution of the central Alps, facilitated the exhumation of the Adula unit.We have documented this shear zone between the top of the Adula unit and the base of the Misox zone in the San Bernardino pass area (Switzerland). The shear zone primarily developed within Adula orthogneisses, containing lenses of paragneisses and eclogites at the top. These eclogites consistently display a mylonitic texture, with the mylonitic foliation rotated at various angles relative to the shear zone-related foliation.The P-T equilibrium conditions of the eclogites have been determined to be approximately 2.0-2.1 GPa and 520-645 °C, which are considered coeval with the development of the mylonitic texture based on microstructural evidence. The 40Ar/39Ar dating of phengite in eclogites yielded ages of 37-39 Ma. The 40Ar/39Ar age distribution across the mylonitic orthogneiss of the shear zone indicates a younging trend from the bottom to the top (eclogite-bearing zone) of the shear zone, from approximately 37 to 29 Ma. This is consistent with top-to-the-east normal shearing that started just after the HP metamorphism.
Late Cretaceous S-verging thrusting in the central Southern Alps (N Italy) proved by U-Pb syn-tectonic calcite geochronology
Authors: Zanchetta Stefano , Rocca Martina , Montemagni Chiara , Fiorini Andrea , Carminati Eugenio , Aldega Luca , Kylander-Clark Andrew , Zanchi Andrea
Published: August 2024

The central Southern Alps (cSA) form a complex S-verging polyphase fold-and-thrust belt formed in response to the Alpine convergence to the S of the Periadriatic Fault System. Despite the onset of the final continent-continent collision in the Alps is constrained in the Late Eocene, evidence of Late Cretaceous deformation occur in the northern part of the belt, along the Orobic Thrust stacking the Variscan basement onto the Permo-Triassic cover. Here, pseudotachylytes associated to faulting close to the brittle-ductile transition display radiometric ages that trace back to 80 Ma.No radiometric ages on structures in the central and southern part of the belt are until now available, with only indirect constrains (andesitic dikes and stocks cross-cutting tectonic structures) providing a pre-Late Eocene age of deformation related to the Alpine crustal shortening.We present here new U-Pb radiometric ages of calcite tectonites located along the main structures of the central and southern sectors of the cSA that consist here of a thick pile of thrust sheets deforming the Lower to Middle Triassic carbonate successions. Our new U-Pb calcite ages obtained on growth fibers along fault planes, veins and calc-mylonites sampled along some of the most important regional thrust planes mainly result in Late Cretaceous ages, suggesting that N-S to NW-SE directed compression already affected the central part of the cSA at those times. Similar ages also occur within the southern portion of the belt, where the Norian “Dolomia Principale” thrust sheets, override the Rhaetian Riva di Solto Shale immediately to the north of the frontal portion of the belt. Younger ages resulted from the Paleogene units which are involved in the exposed frontal part of the belt, which is mostly buried under the recent infilling of the Po Plain forming the Milan Belt.These data confirm that S- to SE-directed thrusting and folding affected the central Southern Alps since the Late Cretaceous, well before the onset of the Alpine collision.
The complex thermotectonic history of the eastern Southern Alps
Authors: Pomella Hannah , Klotz Thomas , Sieberer Anna-Katharina , Dunkl Istvan
Published: August 2024

Neogene to ongoing N(W)-directed continental indentation of the Adriatic microplate into Europe controls the evolution of the European eastern Southern Alps (ESA). Despite the Adriatic plate acting as a rigid indenter, it has undergone internal deformation, with predominantly Miocene shortening being accommodated within a WSW-ENE striking, S-vergent fold-and-thrust belt. This deformation overprints a compositionally heterogeneous upper crust affected by several magmatic and tectonic events. We present new (Apatite (U-Th)/He (AHe) and Fission Track (AFT) data along a N-S profile in the western ESA to better understand the thermotectonic evolution of this complex area.Time-temperature path modelling confirms the Valsugana phase as the most significant period of tectonic exhumation within the western ESA. AFT data in the research area tend to cluster within consistent distinguishable tectonic blocks, however, they are quite scattered especially in the central part of the ESA, warranting further investigation. The geodynamic history of the ESA is characterised by multiple heat pulses, which must be considered when interpreting the AFT data especially as the temperature of this pulses likely did not significantly exceed the partial annealing zone of AFT. Potential heating events are the (1) Permian magmatism, (2) Ladinian magmatism, (3) Jurassic crustal extension, (4) sedimentary superimposition (maximum thickness in Cretaceous), Middle Eocene to Lower Oligocene (5) Periadriatic intrusions and (6) Veneto Volcanic Province magmatic event.Modelled cooling paths indicate that nearly all samples experienced heating just above the AFT partial annealing zone during the Middle Triassic, preceding the Jurassic extension and Cretaceous maximum burial indicated by the stratigraphic record. Detailed analysis of AFT data reveals that only a small, single-digit percentage of analysed grains give a single grain age older than Middle Triassic. Accounting for the σ1 error, all single grain ages can be interpreted as post-Middle Triassic. This suggests that the Ladinian magmatic event caused a geothermal anomaly affecting the entire research area, not just the well-known magmatic centres (e.g. Predazzo area). During and after the subsequent relaxation of the geothermal gradient the aforementioned events (3) – (6) overprinted the geothermal field locally. Based on the modelled cooling paths, it can be assumed that most of the samples remained in the temperature range of the AFT partial annealing zone or at slightly cooler temperatures during this period. Finally, during Miocene, the entire area was affected by fast tectonic exhumation on thrusts related to the Valsugana phase. This sequence of regional and local, magmatic and tectonic events results in very complex cooling histories that can vary significantly even for closely situated samples, explaining the scattered AFT ages.
The Santa Lucia Nappe (Alpine Corsica): paleotectonic heritage and deformation history
Authors: Molli giancarlo , Zibra Ivan
Published: August 2024

The Santa Lucia Nappe is a continental-derived unit exposed East of Corte, in central Alpine Corsica (Durand Delga 1984; Rossi et al., 1996).  The unit includes a peculiar lower- to mid-crustal section, exposing mafic and felsic granulites, with an overall structure, Permian age of tectono-metamorphic and magmatic history (Caby et al., 2002; Zibra et al, 2010, 2012), like that of the Ivrea Zone (northwestern Alps), and of the Sila-Stilo unit in the Calabria terrane (Molli et al., 2020). Moreover, the Santa Lucia Nappe includes a Cretaceous metasedimentary cover, with a basal conglomerate transitioning to a calcareous flysch, which shows affinities with calcareous-marly Ligurian Flysch (Amaudric Du Chaffaut 1972; Rieuf 1980). The Santa Lucia Nappe recorded a polyphase Alpine tectonic evolution, developed under greenschist-facies conditions (Zibra, 2006; Vitale-Brovarone et al., 2013)Because of its unique lithological association, the structural position, significance, and paleotectonic attribution of the Santa Lucia Nappe are  the subject of a long-standing debate. These topics are here re-discussed, based on our data collected in the last two decades of field work.Our observations allow: (i) to document the Alpine deformation structures affecting both basement and cover sequence, their styles and distribution; (ii) to analyze the structural characters and kinematics of its basal tectonic contacts; (iii) to confirm its tectonic position with respect to the “Schistes Lustres”- composite Nappe system; and, finally, (iv) to propose an original interpretation of its internal architecture. The latter results from the tectonic inversion of pre-Cretaceous high-angle faults, which were originally arranged in an east-dipping, domino-like system, which affected the already exhumed and exposed basement, formerly part of a Permian regional-scale transtensional shear zone.
Deep structure and collisional processes in the Western and Central European Alps
Authors: Bellahsen Nicolas , Rosenberg Claudio , Paul Anne , Nouibat Ahmed , Girault Jean Baptiste , Huet Bastien , Sonnet Manon , Labrousse Loic , Jolivet Laurent , Agard Philippe , Marquer Didier , Bernet Matthias , Pik Raphael
Published: August 2024

We investigate both the deep crustal structure of the Western and Central Alps orogenic wedge and the timing and amount of convergence accommodated since 32 Ma. The new structural interpretations are based on the most recent geophysical models (Vs and Vp tomography mainly) coupled to geological surface information. We show that first-order similarities in collision kinematics can be described from the Western to the Central Alps. After the subduction-collision transition (37-32 Ma), from around 32 Ma and until 22-20 Ma, the shortening consists of distributed deformation throughout the doubly verging orogenic wedge. From around 20 Ma until recent times, the orogen was controlled by localized west- or northwest-verging thrusts below the External Crystalline Massifs. This probably witnesses localization processes in the proximal European crust (i.e., below the Penninic Frontal Thrust) on a 10 Myr timescale. These structures (both distributed and localized ones) root in middle- to lower crustal low velocity (Vs) zones interpreted as a thick shear zone acting as a deep, crustal decollement. The low seismic velocity is most probably controlled by active fluid circulations, structural anisotropy, and/or metamorphic Alpine paragenesis (amphibolite facies). Thus, the 10 Myr timescale may correspond to characteristic time for the localization processes within the deep, ductile decollement.Along-strike significant differences from Western to Central Alps can also be highlighted. Beyond collisional magmatism and amphibolite facies metamorphism only present in the Central Alps, kinematical differences can be quantified. In the Western Alps, after the first phase of collision, at around 20 Ma, the orogenic wedge consisted in a West-verging wedge while in the Central Alps, North- and South verging structures remained active. These differences imply significant contrasts in terms of convergence rates that can be quantified through balanced cross sections with realistic inherited Mesozoic structures. In Central Alps, convergence rates were about 1.2 +/- 0.2 cm/yr from 32 to 22 Ma and about 0.3 +/- 0.1 cm/yr from 22 to 0 Ma. This strongly suggests that before collision s.s., i.e. before 32 Ma, the convergence rate was higher than 1.2 cm/yr.While similarities in terms of structural styles and kinematics in both parts of the orogen most likely reflect crustal rheology and localization processes, the differences allow discussing the influence of both the inherited Mesozoic structure and the kinematics of Adria after the subduction phase.
Assessing multivariate bias corrections of climate simulations on various impact models under climate change
Authors: Allard Denis , Vrac Mathieu , François Bastien , García de Cortázar-Atauri Iñaki
Published: August 2024

Abstract. Atmospheric variables simulated from climate models often present biases relative to the same variables calculated by reanalysis in the past. In order to use these models to assess the impact of climate change on processes of interest, it is necessary to correct these biases. Currently, the bias correction methods used operationally correct one-dimensional time series and are therefore applied separately, physical variable by physical variable and site by site. Multivariate bias correction methods have been developed to better take into account dependencies between variables and in space. Although the performance of multivariate bias correction methods for adjusting the statistical properties of simulated climate variables has already been evaluated, their effectiveness for different impact models has been little investigated. In this work, we propose a comparison between two multivariate bias correction methods (R2D2 and dOTC) in three different configurations (intervariable, spatial and spatial-intervariable) and a univariate correction (CDF-t) through several highly multivariate impact models (phenological stage, reference evapotranspiration, soil water content, fire weather index) integrating the weather conditions over a whole season. Our results show that CDF-t does a fair job in most situations and that there is no single best MBC method. The performances of multivariate bias correction methods depend both on some characteristics of the studied process and on the configuration of the chosen bias correction method. When all characteristics are important (multivariate, time cumulative and spatial) it is found that dOTC in its spatial-intervariable configuration brings improvements in most cases and no significant improvement in some rare cases. We did not find any multivariate cases where the spatial-intervariable configuration for dOTC performs less well than CDF-t.
Effect of Differences in the Composition of Growing Media on the Growth of White Oyster Mushroom Mycelium (Pleurotus ostreatus)
Authors: Herawati Elisa , Dwi Septi Amalia  , Malaysia Emi , Murniyati Agustina , Fathiah
Published: August 2024

The use of the main growth medium in the form of wood sawdust in mushroom domestication is still higher than that of other organic materials, even though its availability is limited, so efforts need to be made to find a growth medium composition that minimizes the percentage of sawdust use. The purpose of this study was to determine the comparison of treatment 1 (80% teak sawdust, 10% bran, 5% tapioca flour, and 5% agricultural lime) with treatment 2 (70% teak sawdust, 15% bran, 10% tapioca flour, and 5% agricultural lime) on the percentage of growth and mycelium growth of white oyster mushrooms.  Composting of growing media was carried out for 5 days, then baglog making was carried out, after which the baglog was sterilized for 4 hours. After sterilization, the baglog was cooled and inoculated. After inoculation, the baglog is incubated to grow mycelium. Then, after 15 days, data collection and calculation were carried out. The parameters measured were the percentage of growth and mycelium growth of white oyster mushrooms in baglogs. Results showed that the percentage of growth and mycelial growth of white oyster mushrooms in treatment 1 is better than in treatment 2. Reducing the percentage of the main growing medium of teak sawdust and adding the percentage of additional growing media of bran and tapioca flour has a negative impact on the number of baglogs that grow mycelium (percentage of growth) and the growth of white oyster mushroom mycelium. This means that reducing the main media of teak sawdust and adding additional media is not the right growing media composition for domestication of white oyster mushrooms, so it cannot be used as an alternative growing media composition to reduce the use of wood sawdust.
Liquid Smoke Yield Grade 3, Grade 2 and Grade 1 from Five Different Types of Plants
Authors: Merni Ita , Aldo Kurniawan  , Andi Yusuf
Published: August 2024

This research was motivated by the lack of optimal use of leaves in forest plants, while there are many types of leaves in the forest. One use of leaves is to use them as raw material for making liquid smoke. This research was conducted to determine the yield of liquid smoke on forest plant species from their leaves. The research method used is the pyrolysis method with indirect combustion. This research was carried out by treating forest plant raw materials, namely kerai paying leaves (Filicium decipiens L.), bungur leaves (Lagerstroemia speciosa), mahogany leaves (Swietenia macrophylla King), teak leaves (Tectona grandis) and sungkai leaves (Peronema canecens Jack). The results of the research showed that the results of liquid smoke from the 5 types of plant leaves, namely sungkai leaves, had the highest grade 3 yield of 23.83% and the lowest grade 3 yield, namely mahogany leaves, of 17.81%. In grade 2 sungkai leaves the highest percentage was 21.12% and mahogany leaves had the lowest yield with a percentage of 16.18%. Meanwhile, in grade 1, sungkai leaves have the highest yield percentage of 19.33% and mahogany leaves have the lowest yield, namely 15.03%.
Prediabetes, ¿cómo abordarla en el 2024?
Authors: Cebrián Cuenca Ana María
Published: August 2024

La prediabetes afecta a aproximadamente el 14,8 % de la población adulta en España, aumentando el riesgo de desarrollar diabetes mellitus tipo 2 (DM2) y enfermedades cardiovasculares. La detección temprana es crucial para implementar medidas preventivas y evitar complicaciones. La Asociación Americana de Diabetes (ADA) define la prediabetes por niveles de glucosa o hemoglobina glicosilada A1c (HbA1c) elevados, con un riesgo proporcionalmente mayor a medida que aumentan los valores. Se recomienda el cribado en adultos a partir de los 35 años, especialmente en aquellos con sobrepeso u obesidad y otros factores de riesgo cardiovascular. El manejo se enfoca en cambios en el estilo de vida, como la dieta y el ejercicio, siendo programas de prevención de diabetes coste-efectivos. La metformina puede considerarse en ciertos grupos de alto riesgo. Es fundamental controlar los factores de riesgo cardiovascular y personalizar el tratamiento para cada individuo, con el objetivo de prevenir la progresión a DM2 y reducir la morbimortalidad cardiovascular
Aplicaciones básicas de la ecografía en el abordaje del paciente
con diabetes en Atención Primaria
Authors: Conangla Ferrin Laura , Guirado Vila Pere , Ortega Vila Yolanda , Ródenas Aguilar José Luís , Leceaga Gaztambide Eva
Published: August 2024

El uso de la ecografía clínica se ha extendido en Atención Primaria, y muchos médicos de familia disponen de ecógrafo en consulta o en el centro, a menudo equipado con sonda lineal y convexa. En el paciente con diabetes, la ecografía tiene múltiples aplicaciones, que van desde las técnicamente más simples (como la valoración de la grasa subcutánea o la medición del grosor de la íntima-media carotídea) hasta las más complejas (como la ecocardiografía). Mediante la ecografía, se podrán valorar alteraciones potencialmente causantes de la patología, comorbilidades acompañantes y complicaciones de la diabetes o de algunos de sus tratamientos. El médico de familia debe conocer aquellas aplicaciones básicas, con una curva de aprendizaje asequible, que aporten gran información en consulta, en un tiempo razonable.
Entre los usos de la ecografía en la diabetes destacan el estudio abdominal (hígado, riñones, páncreas...), vascular (específicamente la determinación del grosor de la íntima-media carotídea por su relación con el riesgo y daño cardiovascular), y el estudio ecográfico del tejido celular graso subcutáneo. Otras aplicaciones más específicas incluirán la valoración muscular en el estudio de sarcopenia, la ecografía cardiaca, la ecografía vascular de extremidades inferiores, el estudio ecográfico de la neuropatía diabética, y muchas más.
Actualización en factores de riesgo cardiovascular y diabetes mellitus
Authors: Ávila Lachica Luis , Gómez García María del Carmen
Published: August 2024

El tratamiento de la diabetes mellitus no debe basarse en el control glucémico exclusivamente, sino que es fundamental controlar todos los factores de riesgo cardiovascular de forma conjunta. Como los pacientes con diabetes tienen un mayor riesgo de desarrollar enfermedades cardiovasculares es clave un enfoque multifactorial que aborde los diferentes factores de riesgo cardiovascular.
Por este motivo es fundamental la evaluación detallada del riesgo cardiovascular del paciente con diabetes. Una vez calculado, este riesgo cardiovascular lo debemos considerar al iniciar el tratamiento con fármacos antihiperglucemiantes que hayan demostrado eficacia en la reducción del riesgo cardiovascular.
استشراف الأزمات في عالم الفوكا (التحديات والفرص)
Authors:   دكتوراه في استشراف المستقبل والابتكار والدراسات المستقبلية، المملكة العربية السعودية, المنصور أحمد
Published: August 2024

في عصر يتميز بالتغيرات السريعة والمفاجئة، أصبحت إدارة الأزمات ضرورة حيوية لنجاح المؤسسات واستمراريتها. تعيش المنظمات اليوم في بيئة متقلبة ومعقدة، تتسم بعدم اليقين والتحديات الكبيرة، وهذا ما يُعرف بمصطلح فوكا. يتطلب هذا السياق من القادة والمديرين التفكير المستقبلي والاستعداد الفعال لمواجهة أي أزمة قد تنشأ بشكل مفاجئ. تتناول الدراسة موضوع استشراف الأزمات في عالم فوكا، مع التركيز على تحليل العوامل والاتجاهات المحتملة التي قد تؤدي إلى نشوء أزمات مستقبلية. تهدف هذه الدراسة إلى استكشاف أدوات وتقنيات استشراف الأزمات في عالم الفوكا، وتحليل كيفية تطبيقها بشكل فعّال لتعزيز قدرة المؤسسات على الاستجابة السريعة والمتجاوبة في مواجهة التحديات الطارئة. من خلال دراسة تجارب سابقة واستعراض أفضل الممارسات. تم استخدام منهجية البحث النوعي لتحليل البيانات والمصادر المعتمدة، بما في ذلك الدراسات السابقة والتقارير العلمية. تم شرح مفهوم الاستشراف والأزمات وإدارة الأزمة في عالم فوكا والتحديات في عالم فوكا والفرص في عالم فوكا وتم شرح أدوات وتقنيات للاستشراف في عالم فوكا. تساهم نتائج الدراسة في توجيه السياسات العامة والاستراتيجيات العالمية للتصدي للأزمات المستقبلية وتحسين قدرة المنظمات والمجتمعات على التكيف والاستجابة. يأتي هذا البحث في سياق الحاجة الملحة لفهم عميق لكيفية تأمين المنظمات وتعزيز قدرتها على البقاء في ظل التحديات المعقدة والمتغيرات السريعة للسوق والبيئة الاقتصادية العالمية، ويوصي الباحث بتعزيز الاستثمار في البحث والابتكار في مجال استشراف الأزمات لتحسين قدرة المؤسسات على التنبؤ بالأزمات والاستعداد لها.
UPAYA MENGEMBANGKAN KREATIVITAS ANAK MELALUI BERMAIN BAHAN ALAM DI KELOMPOK A TK JAYA BOGOBABADAN KARANGBINANGUN
Authors: Munif Moh. Vito Miftahul , Shoimah Retno Nuzilatus , Yunara Nora Yulia
Published: August 2024

Penelitian ini mengkaji 1) untuk mengetahui penerapan media pelepah pisang yang digunakan dalam meningkatkan kreativitas anak, 2) untuk meningkatkan kreativitas anak melalui media pelepah pisang. Penelitian ini merupakan penelitian tindakan kelas (classroom reseach) dengan pendekatan kuantitatif dan penelitian ini dilakukan untuk membuktikan tingkat kreativitas anak melalui penerapan media pasir ajaib dengan indikator keberhasilan ≥ 75.Hasil dari penelitian ini menunjukkan bahwa, terjadi peningkatan kreativitas anak yang mencapai kualifikasi berkembang sangat baik (BSH), hal itu dibuktikan dengan mendapat nilai pada rata-rata pra siklus kelas sebanyak 64,9, kemudian meningkat pada siklus I sebanyak 72,2 dan pada siklus II terjadi peningkatan sebanyak 81,9.
UPAYA MENINGKATKAN KEMAMPUAN MEMBACA PERMULAAN MELALUI MEDIA SNADER GAME PADA ANAK KELOMPOK B DI RA AL ISLAM KARANGREJO SUKOLILO SUKODADI TAHUN PELAJARAN 2021/2022
Authors: Fitriana Anis , Sun'iyah Siti Latifatus
Published: August 2024

Penelitian ini membahas mengenai upaya meningkatkan kemampuan membaca permulaan melalui media snader game pada anak kelompok B di RA Al Islam Karangrejo Sukolilo Sukodadi Tahun Pelajaran 2021/2022. Tujuan penelitian ini adalah untuk mengetahui penerapan dan peningkatan media snader game dalam upaya meningkatkan kemampuan membaca permulaan anak. Adapun metode yang digunakan dalam penelitian ini adalah Penelitian Tindakan Kelas (classroom reseach) dan teknik pengumpulan data yang digunakan adalah observasi, wawancara, dokumentasi dan tes. Hasil dari penelitian ini menunjukkan bahwa, terjadi peningkatan kemampuan membaca permulaan anak yang mencapai kualifikasi berkembang sesuai harapan (BSH), hal itu dibuktikan dengan mendapat nilai pada rata-rata kelas pra siklus kelas sebanyak 61,4, kemudian meningkat pada siklus I sebanyak 67,7 dan pada siklus II terjadi peningkatan sebanyak 76,9. Dapat disimpulkan bahwa penerapan media snader game dapat meningkatkan kemampuan membaca permulaan pada anak kelompok B di RA Al Islam Karangrejo Sukolilo Sukodadi Tahun Ajaran 2021/2022. Penerapan media snader game mampu meningkatkan kemampuan membaca permulaan anak dan penelitian ini dikatakan meningkat dan berhasil. bahwa ada peningkatan pada setiap tahap, dari Pra siklus 27,2% menjadi 45,4% pada siklus I, dan meningkat menjadi 100% pada siklus II. Hal ini menunjukkan bahwa peningkatan dalam menggunakan media snader game dapat meningkatkan kemampuan membaca permulaan pada anak.
UPAYA MENINGKATKAN KEMAMPUAN MOTORIK HALUS ANAK MELALUI KEGIATAN PRAMENULIS MENGGUNAKAN MEDIA YANG BERVARIASI DI TK TUNAS PERTIWI
Authors: Setyaningrum Herawati , Machmudah Machmudah , Sa'adah Hurin Innihayatus
Published: August 2024

Penelitian ini bertujuan untuk meningkatkan kemampuan motorik halus anak melalui kegiatan pra menulis yang menggunakan media yang bervariasi di TK TUNAS PERTIWI di Kecamatan Tanjung Priok, Kota Administrasi Jakarta Utara. Siklus I dan Siklus II, masing-masing terdiri dari empat tahap yaitu : Perencanaan, pelaksanaan, pengamatan, dan refleksi. Bentuk penelitian ini dikenal sebagai Penelitian Tindakan Kelas (PTK). Penelitian ini melibatkan 16 anak yang berusia antara 5 dan 6 tahun di kelompok B TK Tunas Pertiwi, yang terdiri dari 9 anak laki-laki dan 7 anak perempuan. Lembar Pengamatan dan Observasi digunakan untuk mengumpulkan data. Penelitian perbaikan pembelajaran ini menemukan bahwa kompetensi bidang pengembangan motorik halus anak yang belum berkembang sebesar lima puluh persen pada kegiatan pra siklus, tetapi turun menjadi 0 % pada kegiatan siklus I dan siklus II. Anak yang Berkembang Sesuai Harapan meningkat dari kegiatan pra siklus sebesar 25%, menjadi 62% pada siklus I, dan 40% pada siklus II. Anak yang Berkembang Sangat Baik meningkat dari kegiatan pra siklus sebesar 0% menjadi 19% pada siklus I dan 50% pada siklus II. Dalam penelitian tindakan perbaikan ini, diharapkan kemampuan motorik halus anak dapat lebih meningkat lagi jika metode pembelajaran menggunakan media yang  bervariasi.
DETERMINAN KEJADIAN ANEMIA PADA IBU HAMIL TRIMESTER I DI WILAYAH KERJA PUSKESMAS BUNTOK
Authors: Uswatun Hafizhah  , Greiny Arisani  , Yena Wineini Migang  , Seri Wahyuni
Published: August 2024

Latar Belakang : Ibu hamil yang mengalami anemia (Hb<11 gr/dl) akan dengan cepat terganggu kondisinya bila terjadi kehilangan darah saat persalinan meskipun hanya sedikit. Ada beberapa faktor yang menjadi perhatian khusus karena merupakan penyebab yang sangat mendominasi terjadinya anemia pada kehamilan seperti umur ibu, jarak kehamilan, Indeks Massa Tubuh (IMT) dan paritas.
Tujuan : Untuk menganalisis determinan atau faktor yang menentukan kejadian anemia pada ibu hamil trimester I di wilayah kerja Puskesmas Buntok.
Metode : Penelitian ini menggunakan metode observasional analitik dengan pendekatan cross sectional study. Teknik pengambilan sampel menggunakan purposive sampling. Populasi seluruh ibu hamil trimester I  yang aktif ANC di Puskesmas Buntok dengan total sampel 106 ibu hamil. Penelitian ini dianalisis menggunakan uji Chi-Square.
Hasil : Hasil uji Chi-Square pada variabel paritas  didapatkan nilai p value = 0,000 (p < 0,05) yang berarti ada hubungan paritas dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok. Hasil uji Chi-Square pada variabel umur ibu didapatkan nilai p value = 0,043 (p < 0,05) yang berarti ada hubungan umur ibu dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok. Pada variabel jarak kehamilan didapatkan nilai p value = 0,502 (p > 0,05) yang berarti tidak ada hubungan jarak kehamilan dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok. Kemudian pada variabel Indeks Massa Tubuh (IMT) didapatkan nilai p value = 0,117 (p > 0,05) yang berarti tidak ada hubungan IMT dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok.
Kesimpulan : Terdapat hubungan paritas dan umur ibu dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok. Tidak terdapat hubungan jarak kehamilan  dan Indeks Massa Tubuh (IMT) dengan kejadian anemia pada ibu hamil trimester I di Puskesmas Buntok.
Application of Apriori Algorithm in Determining Behavioral Patterns and Lifestyle of GERD Patients
Authors: Pramudhita Chika , Buaton Relita , Sitompul Melda Pita Uli
Published: August 2024

Gastroesophageal Reflux Disease (GERD) is a condition of reflux of stomach contents into the esophagus which can cause typical symptoms such as heartburn (burning in the epigastric region), acid regurgitation (bitter taste in the mouth), nausea, and dysphagia which can result in damage to the esophageal mucosa and in the long term can cause complications such as Barrett's esophagus.  Based on data on patients with GERD disease in 2020-2023, there were 521 patients obtained at Bidadari Binjai General Hospital, with differences in prevalence caused by socioeconomic and lifestyle changes that can increase the incidence of GERD. The purpose of this study is to obtain the results of the combination between item-sets on the behavior patterns and lifestyles of GERD sufferers which are expected to help the agency in processing data on GERD sufferers into more effective information to determine the behavior patterns and lifestyles of GERD sufferers with the Apriori Algorithm method. From the research conducted, the results obtained rules that meet the value of 30% support and 100% confidence, if unhealthy eating patterns are often late eating, then unhealthy lifestyles are often done sleeping after eating and smoking.
ANALISIS INCREASE TAX DAN TAX AMNESTY TERHADAP TAX ASSURANCE DALAM PROBABILITAS PEMERIKSAAN PAJAK
Authors: Angelina Natalia , Kurniawan Rudy , Haryono Haryono
Published: August 2024

Charge is a required commitment owed by people or substances. In this context, the SAMSAT office participates in public services, contributing to fiscal monitoring and supervision of tax amnesty implementation. It was found that individuals tend to disagree more than agree with tax amnesty, but tax amnesty tends to improve tax compliance. The research method used was qualitative, involving interview sessions at the SAMSAT office. The goal was to gather detailed information about various aspects of public services, with the main objective of providing constructive suggestions to enhance service standards. Interviews were conducted at the Samsat UPT Wilayah I Kota Pontianak, covering the overall profile and structure of the institution, as well as documents related to tax regulations. The research results indicate that increased taxes impact tax assurance, affecting both expenditures and central taxes. Tax rates in daily collections are subject to change, and tax assurance plays a crucial role in handling and overseeing local taxpayers. The government ensures compliance with existing tax regulations, monitored by the Regional Revenue Agency and the State Audit Board, with annual routines to engage the general public in a timely manner.
KAJIAN LITERATUR : DIFUSI INOVASI TERHADAP APLIKASI CARI TEMU BAZNAS
Authors: Hadi Abdul , Ardianto Reno , Arpenta Shady
Published: August 2024

Dalam penelitian ini, dilakukan kajian literatur mengenai difusi inovasi dan aplikasinya terhadap Aplikasi Cari Temu yang dikelola oleh Badan Amil Zakat Nasional (BAZNAS). Aplikasi Cari Temu adalah aplikasi yang disediakan BAZNAS untuk mencari korban pasca bencana yang terkadang masih menjadi kendala bagi keluarga korban dalam mencari informasi yang valid dari sumber yang  terpercaya. Difusi inovasi ini merupakan proses di mana inovasi baru disebarkan melalui komunikasi formal atau informal di antara anggota suatu sistem. Analisis difusi inovasi untuk aplikasi Cari Temu diharapkan dapat meningkatkan sistem informasi yang efektif dan mudah digunakan dalam penanganan suatu kebencanaan oleh masyarakat. Dalam penelitian ini metode yang digunakan adalah literatur sistematis dimana pencarian tentang literatur mengenai difusi inovasi, teknologi dan mengaitkannya dengan aplikasi Cari Temu BAZNAS. Dalam penelitian ini, peneliti masih mendapatkan kurangnya data setelah tahun 2022 dikarenakan adanya proses internal BAZNAS yang berdampak pada sistem aplikasi Cari Temu sedang tidak dapat diakses sampai saat ini. Memberikan rekomendasi untuk peneliti selanjutnya untuk penelitian mendalam terhadap sistem-sistem informasi kebencanaan yang sudah diperbaiki oleh BAZNAS, sejauh mana kebermanfaatan dan dapat diakses dengan mudah oleh masyarakat.
PROYEK SISTEM INFORMASI MANAJEMEN PELAYANAN TERPADU PADA POSYANDU TUNAS HARAPAN JATIMAKMUR BEKASI
Authors: Ramadhan Muhammad Rafi , Sari Diana , Nurmalasari Nurmalasari
Published: August 2024

Posyandu yang merupakan singkatan dari “Pos Pelayanan Terpadu” adalah program pelayanan kesehatan berbasis masyarakat di Indonesia yang bertujuan untuk memberikan pelayanan kesehatan dasar dan gizi, khususnya bagi ibu dan anak balita. Penekanan diberikan pada urgensi pengembangan aplikasi web sebagai solusi untuk mengatasi tantangan administratif yang dihadapi oleh Posyandu. Dengan demikian, penelitian ini diharapkan dapat memberikan kontribusi dalam meningkatkan efisiensi dan efektivitas program Posyandu serta memberikan dampak positif bagi kesehatan masyarakat di tingkat lokal. pihak posyandu lebih mudah untuk memonitor  balita yang sudah di imunisasi karena setelah mendata bayi dan balita, kader posyandu hanya tinggal menginput data berat badan, vaksin dan lain-lain nantinya data dibulan sebelumnya pun bisa di gabungkan  dan terintegrasi dengan baik sehingga pihak puskesmas pun juga menjadi lebih mudah untuk melihat informasi di website tersebut.