Neuroactive hormones and interpersonal trust: International evidence

Social attachment is vital for human health and welfare. Recent experimental evidence in humans has identified the role of neuroactive hormones, especially the peptide oxytocin, in mediating trusting behaviors. Herein, we test if the endocrinological basis for trust between humans scales up to the country level. Trust pervades nearly every aspect of our daily lives, yet survey data on trust show substantial variation across countries. Using 31 measures of biological, social, and environmental factors associated with hormone levels for a sample of 41 countries, we find that two classes of factors are related to trust: consumption of plant-based estrogens (phytoestrogens), and the presence of environmental conditions that include measures of estrogen-like molecules. Our findings provide preliminary evidence that interpersonal trust at the country level may be related to the intake of neuroactive hormones.     

The effect of anions on spectral properties of iodopsin and native cones in the frog retina (microspectrophotometric study)

Absorption spectra of single outer segments of the frog Rana temporaria photoreceptors were registered. Effects of nitrate and chloride ions on spectral properties of cone and rod pigments were compared. These pigments proved to differ in structure of the native photoreceptor membrane and, therefore, in effect of hydrophile environment on the chromophore centrum. Substitution of chloride by nitrate ions led to the hypochromic shift of the cone absorption spectrum (20-25 nm) but does not affect the spectrum on case of rod pigment. The ionochromic behaviour of cone pigments resembles that of the light-sensitive halobacterium protein halorhodopsin, in native membrane. We suppose that the effect of anions on the chromophore centrum may be the cause of bathochromic shifts of absorption spectra of longwave-length retinal-containing pigments.     

A myosin isoform repressed in hypertrophied ALD muscle of the chicken reappears during regeneration following cold injury

A library of monoclonal antibodies specific for myosin heavy chain (HC) was used to study myosin expression in regenerating fibers. The response to cold injury of slow skeletal ALD muscle previously induced to eliminate SM1 myosin by weight overload was compared to that of its contralateral control. Native gel electrophoresis combined with immunoblotting demonstrated that slow SM1 myosin HC eliminated from hypertrophic muscle reappeared both at the site of active regeneration and unexpectedly, also distal to the site of injury. The regeneration response of hypertrophied muscles was similar to that of the controls. In addition to SM1 myosin HC, ventricular-like and embryonic/fast isoforms were also expressed in both muscles during the early stages of regeneration and disappeared as the muscle fibers matured. These observations demonstrate that regenerating slow muscle fibers reexpress myosins' characteristic of developing muscle irrespective of the myosin phenotype prior to injury. The reappearance of repressed myosin HC in the hypertrophied ALD muscle is consistent with the presence of newly differentiated myonuclei.     

The unexpected long period of elevated CH4 emissions from an inundated fen meadow ended only with the occurrence of cattail (Typha latifolia)

Drainage and agricultural use transform natural peatlands from a net carbon (C) sink to a net C source. Rewetting of peatlands, despite of high methane (CH₄) emissions, holds the potential to mitigate climate change by greatly reducing CO₂ emissions. However, the time span for this transition is unknown because most studies are limited to a few years. Especially, nonpermanent open water areas often created after rewetting, are highly productive. Here, we present 14 consecutive years of CH₄ flux measurements following rewetting of a formerly long-term drained peatland in the Peene valley. Measurements were made at two rewetted sites (non-inundated vs. inundated) using manual chambers. During the study period, significant differences in measured CH₄ emissions occurred. In general, these differences overlapped with stages of ecosystem transition from a cultivated grassland to a polytrophic lake dominated by emergent helophytes, but could also be additionally explained by other variables. This transition started with a rapid vegetation shift from dying cultivated grasses to open water floating and submerged hydrophytes and significantly increased CH₄ emissions. Since 2008, helophytes have gradually spread from the shoreline into the open water area, especially in drier years. This process was periodically delayed by exceptional inundation and eventually resulted in the inundated site being covered by emergent helophytes. While the period between 2009 and 2015 showed exceptionally high CH₄ emissions, these decreased significantly after cattail and other emergent helophytes became dominant at the inundated site. Therefore, CH₄ emissions declined only after 10 years of transition following rewetting, potentially reaching a new steady state. Overall, this study highlights the importance of an integrative approach to understand the shallow lakes CH₄ biogeochemistry, encompassing the entire area with its mosaic of different vegetation forms. This should be ideally done through a study design including proper measurement site allocation as well as long-term measurements.