bluuebunny/crossref_metadata_2025_split huggingface dataset:
A wetland oasis at Wadi Gharandal spanning 125–70 ka on the human migration trail in southern Jordan
Authors: Al-Saqarat Bety S. , Abbas Mahmoud , Lai Zhongping , Gong Songlin , Alkuisi Mustafa M. , Abu Hamad Abdalla M.B. , Carling Paul A. , Jansen John D. 
Published: November 2020

AbstractFormer lakes and wetlands can provide valuable insights to the late Pleistocene environments encountered by the first humans to enter the Levant from Africa. Fluvial incision along Wadi Gharandal in hyperarid southern Jordan has exposed remnants of a small riverine wetland that accumulated as a sedimentary sequence up to ~20 m thick. We conducted a chronometric and sedimentological study of this wetland, including 10 optically stimulated luminescence dates. The wetland sequence accumulated during the period ~125 to 70 ka in response to a positive water balance coupled with a (possibly coseismic) landslide that dammed the outlet. The valley fill was dissected when the dam was incised shortly after ~36 ± 3 ka. Comparison of our ages with regional palaeoclimate indicates that the Gharandal oasis developed during the relatively humid Marine Isotope Stage 5. A minimum age of 74 ± 7 ka for two Levallois flakes collected from stratified sediments suggests that the oasis was visited by humans during the critical 130–90 ka time window of human migration out of Africa. Gharandal joins a growing network of freshwater sites that enabled humans to cross areas of the Levant and Arabia along corridors of human dispersal.
Bounding size of homotopy groups of Spheres
Authors: Boyde Guy 
Published: November 2020

AbstractLet p be prime. We prove that, for n odd, the p-torsion part of πq(Sn) has cardinality at most $p^{2^{{1}/({p-1})(q-n+3-2p)}}$ and hence has rank at most 21/(p−1)(q−n+3−2p). for p = 2, these results also hold for n even. The best bounds proven in the existing literature are $p^{2^{q-n+1}}$ and 2q−n+1, respectively, both due to Hans–Werner Henn. The main point of our result is therefore that the bound grows more slowly for larger primes. As a corollary of work of Henn, we obtain a similar result for the homotopy groups of a broader class of spaces.
Farmer participatory research in agricultural extension programs: A case study of fertilizer management in tropical rice
Authors: Banayo Niño P. M. C. , Kato Yoichiro 
Published: November 2020

AbstractAgricultural extension requires close communication with farmers, and researchers must consider farmers’ perspectives on crop management. Farmers tend to take into account the canopy appearance when they decide on fertilizer application, and this is often neglected in crop management recommendations by researchers. Our objectives were to dissect the growth characteristics that farmers implicitly account for in nutrient management of tropical rice. Farmer participatory trials were conducted in irrigated and rainfed lowlands in the Philippines during the wet seasons of 2014, 2015, and 2016. Each year, 30 participating farmers made decisions on fertilizer management for plots with different seedling ages and planting densities. These treatments greatly changed the canopy appearance, and affected farmer decisions on nitrogen (N) management, particularly in the first year. We found that plant height and leaf greenness were the major determinants of their decisions in irrigated lowlands. Under rainfed conditions, the risk of drought made farmers focus on tillering rather than plant elongation and leaf color during early growth stages, and on canopy cover and plant elongation during later stages. Across years and water regimes, farmers applied 78% more N than researchers without generally increasing grain yield. Since crop diagnosis is a key for successful management by farmers, guidelines for efficient nutrient management should include numerical targets for the traits emphasized by farmers. That will help farmers better understand their crops, and the guidelines will be more user-friendly than providing only a fertilizer application prescription.
The Polarising Worlds of Welfare: Political Orientations, Macroeconomic Context, and Support for Redistribution
Authors: NOUREDDINE RAJA , GRAVELLE TIMOTHY B. 
Published: November 2020

AbstractPublic support for the welfare state – and the policies constituting it – has long been a topic of research. Previous research on support for redistribution has tended to focus on how either country-level characteristics (particularly those relating to the macro-economy such as levels of economic development or income inequality) or individual-level political factors (such as left-right political orientation and sociodemographic factors) shape support for redistribution. To date, empirical research has insufficiently tested how macroeconomic context and individual political orientations interact. Research has also obscured whether the effects of macroeconomic context hold cross-sectionally (across country contexts) or longitudinally (within countries over time). Drawing on data from the International Social Survey Programme (ISSP), this article examines the cross-sectional (between-country) and longitudinal (within-country) interactive relationships involving economic development and income inequality (on one hand) and left–right political orientations (on the other) in shaping preferences for redistribution. Results indicate that there are larger left–right cleavages in attitudes in wealthier countries, more unequal countries, and countries where inequality is increasing. These findings challenge the dominant practice of focusing exclusively on additive effects of individual-level or country-level factors by showing the importance of paying attention to cross-level interactions.
Prevalence of invasive aspergillosis in suspected pulmonary tuberculosis at a referral tuberculosis hospital in Shandong, China
Authors: Wang Jun-Li , Zhou Xiao-Lin , Han Chao , Wang Mao-Shui , Hu Hua 
Published: November 2020

AbstractAlthough the progression of invasive aspergillosis (IA) shares some risk factors in the development of active pulmonary tuberculosis (PTB), however, the prevalence of IA in suspected PTB remains unclear. During a period of 1 year (from January 2016 to December 2016), consecutive patients with suspected PTB were included in a referral TB hospital. Data, including demographic information and underlying diseases, were collected from medical records. PTB were all confirmed by mycobacterial culture (Lowenstein–Jensen medium). IA were diagnosed as proven or probable according to the criteria of the 2008 EORTC/MSG definitions. A descriptive analysis was performed to estimate the corresponding prevalence. During the study year, 1507 patients have a positive mycobacterial culture, with a mean age of 45.6 (s.d.19.9) years old and a female:male ratio of 1:4. Among the 82 patients with non-tuberculous mycobacterial diseases, two patients (2.44%, 95% CI 0.67–8.46%) were diagnosed as IA (one proven and one probable); two probable IA patients (0.15%, 95% CI 0.04–0.55%) were diagnosed in PTB patients (n= 1315), and all were retreatment cases. In addition, all four IA patients (100%) exhibited cavities in both lobes on radiograph. In China, the prevalence of IA is low in active PTB patients. However, when high-risk factors for IA are encountered in PTB patients, further investigations are required and empirically treatment for IA might be warranted.
Pro-inflammatory diet is associated with a high number of cardiovascular events and ultra-processed foods consumption in patients in secondary care
Authors: da Silva Alessandra , Felício Matheus Brum , Caldas Ana Paula Silva , Miranda Hermsdorff Helen Hermana , Bersch-Ferreira Ângela Cristine , Torreglosa Camila Ragne , Shivappa Nitin , Hébert James R , Weber Bernardete , Bressan Josefina 
Published: November 2020

AbstractObjective:To evaluate the association of dietary inflammatory index (DII®) with the occurrence of cardiovascular events, cardiometabolic risk factors and with the consumption of processed, ultra-processed, unprocessed or minimally processed foods and culinary ingredients.Design:This was a cross-sectional study that analysed the baseline data from 2359 cardiac patients. Data on socio-demographic, anthropometric, clinical and food consumption were collected. Energy-adjusted food intake data were used to calculate DII, and the foods were classified according to the NOVA classification. Furthermore, the patients were grouped according to the number (1, 2 or ≥ 3) of manifested cardiovascular events. The data were analysed using linear and multinomial logistic regression.Settings:Multicentre study from Brazil.Participants:Patients with established cardiovascular events from the Brazilian Cardioprotective Nutritional Program Trial evaluated at baseline.Results:Most of the patients were male (58·8 %), older adults (64·2 %) and were overweight (68·8 %). Patients in the third tertile of DII (DII > 0·91) had were more likely to have 2 (OR 1·27, 95 % CI: 1·01–1·61) and ≥ 3 (OR 1·39, 95 % CI: 1·07–1·79) cardiovascular events, with poor cardiometabolic profile. They also were more likely to consume a higher percentage of processed, ultra-processed and culinary ingredients foods consumption compared with the patients in the first DII tertile (DII ≤ 0·91).Conclusion:A more pro-inflammatory diet is associated with a greater chance of having 2 and ≥ 3 cardiovascular events and cardiometabolic risk factors and were more likely to consume processed, ultra-processed and culinary ingredients compared to those with a more anti-inflammatory diet.
How Can Big Data Science Transform the Psychological Sciences?
Authors: Albritton Betsy H. , Tonidandel Scott 
Published: November 2020

Abstract
Big data and related technologies are radically altering our society. In a similar way, these approaches can transform the psychological sciences. The goal of this commentary is to motivate psychologists to embrace big data science for the betterment of the field. Big data sources, algorithmic methods, and a culture that embraces prediction has the potential to advance our science, improve the robustness and replicability of our research, and allow us to focus more centrally on actual behaviors. We highlight these key transformations, acknowledge criticisms of big data approaches, and emphasize specific ways psychologists can contribute to the big data science revolution.
Erfassung von mathematischen Kompetenzen im Vorschulalter mit MARKO-D
Authors: Garrote Ariana , Opitz Elisabeth Moser 
Published: November 2020

Zusammenfassung. In dieser Studie wurde der Test MARKO-D (Mathematik- und Rechenkonzepte im Vorschulalter–Diagnose) mit einer Stichprobe von Kindern aus der deutschsprachigen Schweiz ( N = 555) im ersten und zweiten Kindergartenjahr erprobt und es wurde analysiert, ob sich die Altersnormen der deutschen Stichprobe auf die Schweiz übertragen lassen. Zudem wurde der Test mit einer Teilstichprobe ( n = 87) hinsichtlich Messinvarianz über die Zeit untersucht. Die Ergebnisse des eindimensionalen Rasch-Modells zeigen, dass das Instrument für die Schweiz geeignet ist. Die Testleistungen hängen jedoch vom Kindergartenbesuch ab. Für die Schweiz müssten deshalb nebst Altersnormen auch Normen pro Kindergartenhalbjahr verwendet werden. Die Analyse mittels Differential Item Functioning ergab, dass 17 von 55 Items von großer Messvarianz über die Zeit betroffen sind. Um das Instrument für Längsschnittuntersuchungen einsetzen zu können, müsste es weiterentwickelt werden.
On the Three‐Dimensional Scattering of Waves by Flexible Marginal Ice Floes
Authors: Meylan Michael H. , Perrie Will , Toulany Bechara , Hu Yongcun , Casey Michael P. 
Published: November 2020

AbstractWe reformulate a three‐dimensional theory for wave‐ice interactions for flexible ice floes and present a comparison of this new formulation with selected recent parameterizations for the scattering of ocean surface waves due to individual ice floes. The formulation is based on single flow scattering and a transport equation for energy, which fits with the paradigm used in wave prediction code. These parameterizations are implemented as source terms in the action balance equation for a modern version of the phase‐averaging wave model WAVEWATCH III® (denoted WW3). In this comparison, a simple experiment is performed with regularly distributed ice floes in a marginal ice zone. With the new wave‐ice formulation, results show that attenuation in the direction of propagation is less intense than for the other considered formulations, scattering is more isotropic, and the wave energy is attenuated in the region of the original spectral peak. Thus, a new spectral peak is developed, which is shifted to higher frequencies. The wave scattering and subsequent attenuation are related to the floe response amplitude and the dimensions of the ice floes.
Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite
Authors: Cawood T. K. , Platt J. P. 
Published: November 2020

AbstractDeformation in crustal‐scale shear zones occurs over a range of pressure‐temperature‐time (P‐T‐t) conditions, both because they may be vertically extensive structures that simultaneously affect material from the lower crust to the surface, and because the conditions at which any specific volume of rock is deformed evolve over time, as that material is advected by fault activity. Extracting such P‐T‐t records is challenging, because structures may be overprinted by progressive deformation. In addition, granitic rocks, in particular, may lack syn‐kinematic mineral assemblages amenable to traditional metamorphic petrology and petrochronology. We overcome these challenges by studying the normal‐sense Simplon Shear Zone (SSZ) in the central Alps, where strain localization in the exhuming footwall caused progressive narrowing of the shear zone, resulting in a zonation from high‐T shearing preserved far into the footwall, to low‐T shearing adjacent to the hanging wall. The Ti‐in‐quartz and Si‐in‐phengite thermobarometers yield deformation P‐T conditions, as both were reset syn‐kinematically, and although the sheared metagranites lack typical petrochronometers, we estimate the timing of deformation by comparing our calculated deformation temperatures to published thermochronological ages. The exposed SSZ footwall preserves evidence for retrograde deformation during exhumation, from just below amphibolite‐facies conditions (∼490°C, 6.7 kbar) at ∼24.5 Ma, to lower greenschist‐facies conditions (∼305°C, 1.5 kbar) at ∼11.5 Ma, with subsequent slip taken up by brittle faulting. Our estimates fall within the P‐T‐t brackets provided by independent constraints on the maximum and minimum conditions of retrograde ductile deformation, and compare reasonably well to alternative approaches for estimating P‐T.
An Abrupt Aging of Dissolved Organic Carbon in Large Arctic Rivers
Authors: Schwab Melissa S. , Hilton Robert G. , Raymond Peter A. , Haghipour Negar , Amos Edwin , Tank Suzanne E. , Holmes Robert M. , Tipper Edward T. , Eglinton Timothy I. 
Published: November 2020

AbstractPermafrost thaw in Arctic watersheds threatens to mobilize hitherto sequestered carbon. We examine the radiocarbon activity (F14C) of dissolved organic carbon (DOC) in the northern Mackenzie River basin. From 2003–2017, DOC‐F14C signatures (1.00 ± 0.04; n = 39) tracked atmospheric 14CO2, indicating export of “modern” carbon. This trend was interrupted in June 2018 by the widespread release of aged DOC (0.85 ± 0.16, n = 28) measured across three separate catchment areas. Increased nitrate concentrations in June 2018 lead us to attribute this pulse of 14C‐depleted DOC to mobilization of previously frozen soil organic matter. We propose export through lateral perennial thaw zones that occurred at the base of the active layer weakened by preceding warm summer and winter seasons. Although we are not yet able to ascertain the broader significance of this “anomalous” mobilization event, it highlights the potential for rapid and large‐scale release of aged carbon from permafrost.
Après Nous, le Déluge: A Human‐Triggered Jökulhlaup From a Subglacial Lake
Authors: Gaidos E. , Jóhannesson T. , Einarsson B. , Thorsteinsson Th. , Amend J. P. , Skidmore M. 
Published: November 2020

AbstractGlacial floods (jökulhlaups) are a phenomenon of some temperate ice masses; they are a significant natural hazard, but their complex hydrology is incompletely understood. We document a jökulhlaup from a subglacial lake in Iceland that was inadvertently triggered by a borehole drilled through the overlying ice. We propose that this borehole allowed an englacial water body to drain into the lake, inducing a transient rise in pressure that overwhelmed the lake's subglacial seal 5 days later. Runaway melting of a subglacial conduit by 4°C lake water then initiated a flood to the outlet glacier margin. This incident suggests that draining of englacial water bodies via hydrofracturing crevasses and flooding of moulins by precipitation events are potential natural triggers of jökulhlaups and explains a correlation between surface melting and jökulhlaups. This hydraulic trigger could have wider implications for relations between meteorological conditions, drainage, and dynamics of some glaciers.
Pseudotachylyte Alteration and the Rapid Fade of Earthquake Scars From the Geological Record
Authors: Fondriest M. , Mecklenburgh J. , Passelegue F. X. , Artioli G. , Nestola F. , Spagnuolo E. , Rempe M. , Di Toro G. 
Published: November 2020

AbstractTectonic pseudotachylytes are solidified frictional melts produced on faults during earthquakes and are robust markers of seismic slip events. Nonetheless, pseudotachylytes are apparently uncommon fault rocks, because they are either rarely produced or are easily lost from the geological record. To solve this conundrum, long‐lasting (18–35 days) hydrothermal alteration tests were performed on fresh pseudotachylytes produced by sliding solid rock samples at seismic slip rates in the laboratory. After all tests, the pseudotachylytes were heavily altered with dissolution of the matrix and neo‐formation of clay aggregates. Post‐alteration products closely resemble natural altered pseudotachylytes and associated ultracataclasites (i.e., fault rocks affected by fracturing in the absence of melting), demonstrating that the preservation potential of original pseudotachylyte microstructures is very short, days to months, in the presence of hydrothermal fluids. As a consequence, pseudotachylytes might be significantly underrepresented in the geological record, and on‐fault frictional melting during earthquakes is likely to occur more commonly than generally believed.
Large Atmospheric Waves Will Get Stronger, While Small Waves Will Get Weaker by the End of the 21st Century
Authors: Chemke R. , Ming Y. 
Published: November 2020

AbstractAtmospheric waves control the weather and climate variability, by affecting winds, temperature, and precipitation. It is thus critical to assess their future response to anthropogenic emissions. Most previous studies investigated the projected regional changes in the intensity of atmospheric waves, by pooling across waves with different scales. However, the waves' projected changes might vary with their scale, and thus, their future climate impacts might also be scale dependent. Here we show that both in the tropics and midlatitudes while large waves will get stronger, small waves will get weaker by the end of this century. Thus, investigating the response of atmospheric waves to human activity by pooling across all wave scales masks the future climate impacts of large waves. We further reveal that the opposite response of large and small waves stems from the opposite effect of static stability and zonal wind on the growth rate of the different waves.
Geomorphological Analysis of the Southwestern Margin of Xanadu, Titan: Insights on Tectonics
Authors: Matteoni Pietro , Mitri Giuseppe , Poggiali Valerio , Mastrogiuseppe Marco 
Published: November 2020

AbstractEvidence for tectonic activity on Titan is provided by the presence of eroded mountain ranges. Xanadu is an equatorial region of Titan characterized by a complex topography, even though, overall, it has a lower average elevation compared to its surroundings. We investigated Xanadu's southwestern margin, a part of the region composed of heavily eroded and rugged terrains to the north and east, and of smoother, more uniform terrains to the west and south. The central portions of southwestern Xanadu (SW Xanadu) are characterized by an extensive fluvial network. The presence of such a distinctive feature was the main reason motivating the study of this area, given its potential to provide tectonic indications. Through detailed geomorphological mapping (map scale 1:700,000) on Synthetic Aperture Radar data and analysis of both fluvial drainage patterns and Digital Terrain Models, we identified several putative tectonic structures in this area: normal faulting to the west and east, thrust faulting to the north, and small‐scale strike‐slip faulting in its central parts. Pull‐apart basins are depressions bounded by both dip‐slip faults and by (overlapping and/or bending) segments of a major transcurrent fault, i.e., they are basins generated in transtensional tectonic settings. We propose that central SW Xanadu is a pull‐apart basin, bordered by both normal and thrust faults and formed by transtensional tectonics, which we consider to be the most recent tectonic phase active in this area. This basin is characterized by small‐scale strike‐slip faulting within it, on which a fluvial network has subsequently imposed.
Ionospheric Horizontal Correlation Distances: Estimation, Analysis, and Implications for Ionospheric Data Assimilation
Authors: Forsythe Victoriya V. , Azeem Irfan , Crowley Geoff 
Published: November 2020

AbstractThe background covariance matrix establishes the transition from the data‐ to model‐driven regions in the ionospheric data assimilation algorithms. To construct the background covariance matrix, the information about the spatial ionospheric correlations of model errors is required. This paper focuses on the horizontal component of the covariance matrix. It is the first study that presents global maps of zonal and meridional ionospheric correlation lengths derived for IRI‐2016 model errors. The model errors were calculated using 20 years of GPS total electron content (TEC) values from the Jet Propulsion Laboratory Global Ionospheric Maps (GIMs) for different seasons, geomagnetic conditions, and universal times. The correlation lengths derived from IRI model errors were analyzed and compared to correlation lengths derived from day‐to‐day ionospheric variability calculated from GIM. It was found that the global distributions of the zonal and meridional correlation lengths between the two approaches are very different and that the correlation lengths derived from day‐to‐day TEC variability cannot be used as a proxy for the construction of covariance matrix for ionospheric data assimilation. A new method is proposed for the modeling of azimuthal distribution of the correlation distances that considers the nonisotropic nature of the distribution of correlations around the reference point.