Do behavioral observations make people catch the goal?:A meta-analysis on goal contagion

Goal contagion is a social-cognitive approach to understanding how other people's behavior influences one's goal pursuit: An observation of goal-directed behavior leads to an automatic inference and activation of the goal before it can be adopted and pursued thereafter by the observer. We conducted a meta-analysis focusing on experimental studies with a goal condition, depicting goal-directed behavior and a control condition. We searched four databases (PsychInfo, Web of Science, ScienceDirect, and JSTOR) and the citing literature on Google Scholar, and eventually included e = 48 effects from published studies, unpublished studies and registered reports based on 4751 participants. The meta-analytic summary effect was small - g = 0.30, 95%CI [0.21; 0.40], tau(2) = 0.05, 95%CI [0.03, 0.13] - implying that goal contagion might occur for some people, compared to when this goal is not perceived in behavior. However, the original effect seemed to be biased through the current publication system. As shown by several publication-bias tests, the effect could rather be half the size, for example, selection model: g = 0.15, 95%CI [-0.02; 0.32]. Further, we could not detect any potential moderator (such as the presentation of the manipulation and the contrast of the control condition). We suggest that future research on goal contagion makes use of open science practices to advance research in this domain

Saccharomyces cerevisiae single-copy plasmids for auxotrophy compensation, multiple marker selection, and for designing metabolically cooperating communities

Auxotrophic markers are useful tools in cloning and genome editing, enable a large spectrum of genetic techniques, as well as facilitate the study of metabolite exchange interactions in microbial communities. If unused background auxotrophies are left uncomplemented however, yeast cells need to be grown in nutrient supplemented or rich growth media compositions, which precludes the analysis of biosynthetic metabolism, and which leads to a profound impact on physiology and gene expression. Here we present a series of 23 centromeric plasmids designed to restore prototrophy in typical Saccharomyces cerevisiae laboratory strains. The 23 single-copy plasmids complement for deficiencies in HIS3, LEU2, URA3, MET17 or LYS2 genes and in their combinations, to match the auxotrophic background of the popular functional-genomic yeast libraries that are based on the S288c strain. The plasmids are further suitable for designing self-establishing metabolically cooperating (SeMeCo) communities, and possess a uniform multiple cloning site to exploit multiple parallel selection markers in protein expression experiments

Remote Acculturation 101: A Primer on Research, Implications, and Illustrations from Classrooms Around the World

Remote acculturation (RA) is a modern form of acculturation common among youth, which results from contact with a distant culture via the 4 Ts of globalization (trade, technology, tourism, and transnationalism). This article provides an introduction to RA by describing the what, who, how, where, and why of RA, summarizing its implications for youth development and health, and offering additional resources for student/classroom use. Utilizing our perspectives as psychology researchers and secondary school educators spanning 19 countries across Africa, Asia, Europe, North America, and South America, we supplement research findings from our lab and others with real-world illustrations from our classrooms around the globe. We conclude that the prominent role of media in RA presents cost-effective opportunities to promote its benefits (e.g., foreign media can sharpen cultural competence) and proactively buffer its risks (e.g., media literacy for inoculation against poor health habits)

Cornice dynamics and meteorological control at Gruvefjellet, Central Svalbard

Cornice fall avalanches endanger life and infrastructure in Nybyen, a part of Svalbard's main settlement Longyearbyen, located at 78° N in the High Arctic. Thus, cornice dynamics – accretion, cracking and eventual failure – and their controlling meteorological factors were studied along the ridgeline of the Gruvefjellet plateau mountain above Nybyen in the period 2008–2010. Using two automatic time-lapse cameras and hourly meteorological data in combination with intensive field observations on the Gruvefjellet plateau, cornice process dynamics were investigated in larger detail than previously possible. Cornice accretion starts directly following the first snowfall in late September and October, and proceeds throughout the entire snow season under a wide range of air temperature conditions that the maritime winter climate of Svalbard provides. Cornice accretion is particularly controlled by distinct storm events, with a prevailing wind direction perpendicular to the ridge line and average wind speeds from 12 m s<sup>−1</sup>. Particularly high wind speeds in excess of 30 m s<sup>−1</sup> towards the plateau ridgeline lead to cornice scouring and reduce the cornice mass both vertically and horizontally. Induced by pronounced air temperature fluctuations which might reach above freezing and lead to midwinter rainfall events, tension cracks develop between the cornice mass and the plateau. Our measurements indicate a linear crack opening due to snow creep and tilt of the cornice around a pivot point. Four to five weeks elapsed between the first observations of a cornice crack until cornice failure. Throughout the two snow seasons studied, 180 cornice failures were recorded, of which 70 failures were categorized as distinctive cornice fall avalanches. A clear temporal pattern with the majority of cornice failures in June was found. Thus only daily air temperature could determine avalanche from non-avalanche days. Seven large cornice fall avalanches reached the avalanche fans on which the Nybyen settlement is located. The size of the avalanches was primarily determined by the size of the cornice that detached. The improved process understanding of the cornice dynamics provides a first step towards a better predictability of this natural hazard, but also highlights that any type of warning based on meteorological factors is not an adequate measure to ensure safety of the housing at risk

The geomorphological effect of cornice fall avalanches in the Longyeardalen valley, Svalbard

The study of snow avalanches and their geomorphological effect in the periglacial parts of the cryosphere is important for enhanced geomorphological process understanding as well as hazard-related studies. Only a few field studies, and particularly few in the High Arctic, have quantified avalanche sedimentation. Snow avalanches are traditionally ranked behind rockfall in terms of their significance for mass-wasting processes of rockslopes. Cornice fall avalanches are at present the most dominant snow avalanche type at two slope systems, called Nybyen and Larsbreen, in the valley Longyeardalen in central Svalbard. Both slope systems are on northwest-facing lee slopes underneath a large summit plateau, with annual cornices forming on the top. High-frequency and magnitude cornice fall avalanching is observed by daily automatic time-lapse photography. In addition, rock debris sedimentation by cornice fall avalanches was measured directly in permanent sediment traps or by snow inventories. The results from a maximum of seven years of measurements in a total of 13 catchments show maximum mean rock debris sedimentation rates ranging from 8.2 to 38.7 kg m⁻² at Nybyen, and from 0.8 to 55.4 kg m⁻² at Larsbreen. Correspondingly, avalanche fan surfaces accreted from 2.6 to 8.8 mm yr⁻¹ at Nybyen, and from 0.2 to 13.9 mm yr⁻¹ at Larsbreen. This comparably efficient rockslope mass wasting is due to collapsing cornices producing cornice fall avalanches containing large amounts of rock debris throughout the entire winter. The rock debris of different origin stems from the plateau crests, the adjacent free rock face and the transport pathway, accumulating distinct avalanche fans at both slope systems. Cornice fall avalanche sedimentation also contributed to the development of a rock glacier at the Larsbreen site during the Holocene. We have recorded present maximum rockwall retreat rates of 0.9 mm yr⁻¹ at Nybyen, but as much as 6.7 mm yr⁻¹ at Larsbreen, while average Holocene rockwall retreat rates of 1.1 mm yr⁻¹ at Nybyen have been determined earlier. As cornice fall avalanches are the dominant type of avalanche in central Svalbard, the related geomorphological effect is assumed to be of significance at periglacial landscape scale. A climate-induced shift in prevailing winter wind direction could change the rockslope sedimentation effectively by changing the snow avalanche activity