Work-life Balance and Gender Regime After the Economic Transition

Work-life balance (WLB) is a key issue in our societies in which there is increasing pressure to be permanently available on demand and to work more intensively, and when due to technological change the borders between work and private life appear to be dissolving. However, the social, institutional and normative frames of a region have a huge impact on how people experience work and private life, where the borders between these spheres lie and how much control individuals have in managing these borders. Based on these arguments, this editorial to the special issue Work-life balance/imbalance: individual, organisational and social experiences in Intersections. EEJSP draws attention to the social institutions, frameworks and norms which have an effect on experience, practices and expectations about work-life balance. Concerning the time horizon, this editorial focuses on the change of regime as a reference point since socialist and post-socialist eras differ significantly, although there is still some continuity between them. The authors of this introduction offer an overview of the situation in CEE (Central and Eastern Europe) based mainly on examples of Visegrad countries.

He isotope, U/Th isotope, Calcium carbonate, biogenic opal, rare earth element concentrations, and grain size distribution measured on core-top sediments during SONNE cruise SO202 (INOPEX)

Eolian dust is a significant source of iron and other nutrients that are essential for the health of marine ecosystems and potentially a controlling factor of the high nutrient-low chlorophyll status of the Subarctic North Pacific. We map the spatial distribution of dust input using three different geochemical tracers of eolian dust, 4He, 232Th and rare earth elements, in combination with grain size distribution data, from a set of core-top sediments covering the entire Subarctic North Pacific. Using the suite of geochemical proxies to fingerprint different lithogenic components, we deconvolve eolian dust input from other lithogenic inputs such as volcanic ash, ice-rafted debris, riverine and hemipelagic input. While the open ocean sites far away from the volcanic arcs are dominantly composed of pure eolian dust, lithogenic components other than eolian dust play a more crucial role along the arcs. In sites dominated by dust, eolian dust input appears to be characterized by a nearly uniform grain size mode at ~4 µm. Applying the 230Th-normalization technique, our proxies yield a consistent pattern of uniform dust fluxes of 1-2 g/m**2/yr across the Subarctic North Pacific. Elevated eolian dust fluxes of 2-4 g/m**2/yr characterize the westernmost region off Japan and the southern Kurile Islands south of 45° N and west of 165° E along the main pathway of the westerly winds. The core-top based dust flux reconstruction is consistent with recent estimates based on dissolved thorium isotope concentrations in seawater from the Subarctic North Pacific. The dust flux pattern compares well with state-of-the-art dust model predictions in the western and central Subarctic North Pacific, but we find that dust fluxes are higher than modeled fluxes by 0.5-1 g/m**2/yr in the northwest, northeast and eastern Subarctic North Pacific. Our results provide an important benchmark for biogeochemical models and a robust approach for downcore studies testing dust-induced iron fertilization of past changes in biological productivity in the Subarctic North Pacific.