Characterization of village chicken production performance under scavenging system in Halaba district of southern Ethiopia

Village chicken production was characterized using retrospective and crosssectional methods, where 280 households rearing local chickens in Halaba district of southern Ethiopia were used for data collection. The study revealed that the average flock size was 8.5 chickens (95% CI=7.98 – 9.08). The average number of chickens added to a flock annually was 28.3 birds (95% CI=27.76 – 28.86) while 22.9 birds (95% CI=22.36 – 23.53) were leaving the flock. The majority of the households (77.7%) constructed a wooden perch for night resting of their chickens inside the main house. Scavenging was the major avenue of feeding chickens. Most of the respondents (83.6%) practiced selection in their chicken flocks for females (68.4%) and both sexes (31.6%). The average number of eggs laid by local hen was 13.3 eggs/hen/clutch (95% CI=12.81 – 13.85) and the mean annual egg production was 50.8 eggs per year with an average clutching frequency of 3.8 clutches (95% CI = 3.69 – 3.92). The average clutch length was 26 days (95% CI = 24.92 – 27.08). While the age at first lay of village chickens was 6.53 months (95% CI = 6.45 – 6.61), the average weight at first lay was 0.91 kg (95% CI = 0.87 – 0.96). The mean egg weight for the village chickens was 39.4 g (95% CI = 38.79 – 39.91). The average hatchability of eggs in this study was 83.7 % (95% CI = 81.73 – 85.72). The survival rate of chicks to 6 months of age was 52.3% (95% CI = 51.09 - 53.45). It was concluded that village chicken production was characterized by low input and output system, and scavenging was the dominant form of feeding of village chicken.Key words: Village chicken – Scavenging – Productivity – Clutc

Miocene faunal remains from the Burji-Soyama area, Amaro Horst, southern sector of the main Ethiopian Rift

The Palaeoanthropological Inventory of Ethiopia is dedicated to the discovery and documentation of palaeoanthropologically significant study areas in the Main Ethiopian Rift and Afar Depression. Fieldwork in the area at the southern end of the Amaro Horst during the 1989 field season was focused on a fossiliferous sedimentary succession with intercalated volcanic horizons. Potassium-argon dating sets a minimum age of 11.1 my for sediments bearing vertebrate remains. The partial skeleton of a fossil proboscidean recovered at Burji is described, illustrated and assessed comparatively. The remains are those of a primitive species of choerolophodont mastodon. Biochronological considerations place this specimen in the time range of 15-17 my. The presence of fossiliferous sediments in the Burji area suggest that a rift-related basin had developed in this part of Ethiopia by Middle or Early Miocene times.National Geographic Society 4134-89; National Science Foundation Anthropology Program: BSN 88-19735; Centre for Research and Conservation of the Cultural Heritage, Ethiopian Ministry of Culture and Sports Affair

In your face:A comparative field experiment on racial discrimination in Europe

We present the first large-scale comparative field experiment on appearance-based racial discrimination in hiring conducted in Europe. Using a harmonized methodology, we sent fictitious résumés to real vacancies in Germany, the Netherlands and Spain, randomly varying applicants’ ethnic ancestry (signaled foremost by name) and applicants’ racial appearance (signaled by photographs). Applicants are young-adult country nationals born to parents from over 40 different countries of ancestry (N = 12 783). We examine average differences in callback across four phenotypic groups and four regions of ancestry and present the first cross-country comparable estimates of appearance-based racial discrimination reported in the field-experimental literature. We find that applicants’ phenotype has a significant and independent effect on employers’ responses in Germany and the Netherlands, whereas in Spain we only find evidence of hiring discrimination for particular combinations of phenotype and ancestry, which suggests a less direct and more complex effect of phenotype in this country. Implications are discussed.</p

Strontium Isotopic Variations of Neoproterozoic Seawater: Implications for Crustal Evolution

We report high precision Sr isotopic data on carbonates from the Neoproterozoic Shaler Group, Victoria Island, Northwest Territories, Canada. Lithostratigraphic correlations with the relatively well-dated Mackenzie Mountains Supergroup constrain Shaler deposition to approximately 770-880 Ma, a range corroborated by 723 +/- 3 Ma lavas that disconformably overlie Shaler carbonates and by Late Riphean microfossils within the section. Samples with low Rb-87/Sr-86 ratios (< 0.01) were selected for Sr isotopic analysis. delta-O-18, Mn, Ca, Mg, and Sr data were used to recognize altered samples. The altered samples are characterized by high Mn/Sr (greater-than-or-equal-to 2) and variable delta-O-18; most are dolomites. The data indicate that between ca. 790-850 Ma the Sr-87/Sr-86 ratio of seawater varued between 0.70676 and 0.70561. The samples show smooth and systematic variation, with the lowest Sr-87/Sr-86 value of 0.70561 at ca. 830 Ma. The low Sr-87/Sr-86 ratio of carbonates from the lower parts of our section is similar to a value reported for one sample from the Adrar of Mauritania (almost-equal-to 900 Ma), West African Craton. Isotopic ratios from the upper part of the Shaler section are identical to values from the lower part of the Neoproterozoic Akademikerbreen Group, Spitsbergen. Although a paucity of absolute age determinations hinders attempts at the precise correlation of Neoproterozoic successions, it is possible to draw a broad outline of the Sr isotopic composition of seawater for this period. Indeed, the Sr isotope data themselves provide a stratigraphic tool of considerable potential. Data from this study and the literature are used to construct a curve of the Sr-87/Sr-86 ratio of Neoproterozoic seawater. The new data reported in this study substantially improve the isotopic record of Sr in seawater for the period 790-850 Ma. The Sr isotope composition of seawater reflects primarily the balance between continental Sr input through river input and mantle input via hydrothermal circulation of seawater through mid-ocean ridges. Coupling of Nd and Sr isotopic systems allows us to model changes in seafloor spreading rates (or hydrothermal flux) and continental erosion. The Sr hydrothermal flux and the erosion rate (relative to present-day value) are modeled for the period 500-900 Ma. The results indicate that the hydrothermal flux reached a maximum value at ca. 830 Ma. In contrast, a large peak in erosion rate is indicated at ca. 570 Ma. The peaks in hydrothermal flux and erosion rate are most likely related to developments in the Pan-African and related orogenic events, whose initial development is characterized by production of juvenile crust during supercontinental break up and rifting. The time ca. 570 Ma is characterized by continent-continent collision and production of recycled crust. Sr isotope data from Proterozoic carbonates offer a valuable resource for understanding large-scale crust dynamics.Earth and Planetary SciencesOrganismic and Evolutionary Biolog

Gender Discrimination in Hiring: Evidence from a Cross-National Harmonized Field Experiment

© The Author(s) 2021. Published by Oxford University Press. This is an Open Access article distributed under the terms of the Creative Commons Attribution License (https://creativecommons.org/licenses/by/4.0/), which permits unrestricted reuse, distribution, and reproduction in any medium, provided the original work is properly citedGender discrimination is often regarded as an important driver of women’s disadvantage in the labour market, yet earlier studies show mixed results. However, because different studies employ different research designs, the estimates of discrimination cannot be compared across countries. By utilizing data from the first harmonized comparative field experiment on gender discrimination in hiring in six countries, we can directly compare employers’ callbacks to fictitious male and female applicants. The countries included vary in a number of key institutional, economic, and cultural dimensions, yet we found no sign of discrimination against women. This cross-national finding constitutes an important and robust piece of evidence. Second, we found discrimination against men in Germany, the Netherlands, Spain, and the UK, and no discrimination against men in Norway and the United States. However, in the pooled data the gender gradient hardly differs across countries. Our findings suggest that although employers operate in quite different institutional contexts, they regard female applicants as more suitable for jobs in female-dominated occupations, ceteris paribus, while we find no evidence that they regard male applicants as more suitable anywhere.This project received funding from the European Union’s Horizon 2020 research and innovation program under grant agreement No 649255; the Research Council of Norway, grant number 287016; The Netherlands Organization for Scientific Research (NWO), (016.Vidi.185.041)Peer reviewe