A significant interrelation between heavy metal exposure and metabolic syndrome (MetS) development has been demonstrated earlier. Despite the presence of a number of works aimed at the investigation of the role of Hg in MetS development, the existing data remain contradictory. Therefore, the primary objective of the current work is to review the existing data regarding the influence of mercury on universal mechanisms involved in the pathogenesis of the development of MetS and its components. The brief chemical characterization of mercury is provided. The role of mercury in induction of oxidative stress has been discussed. In particular, Hg-induced oxidative stress may occur due to both prooxidant action of the metal and decrease in antioxidant enzymes. Despite the absence of direct indications, it can be proposed that mercury may induce endoplasmic reticulum stress. As it is seen from both in vivo and in vitro studies, mercury is capable of inducing inflammation. The reviewed data demonstrate that mercury affects universal pathogenetic mechanisms of MetS development. Moreover, multiple investigations have indicated the role of mercury in pathogenesis of MetS components: dyslipidemia, hypertension, insulin resistance, and obesity to a lesser extent. The present state of data regarding the interrelation between mercury and MetS denotes the following perspectives: (1) Further clinic-epidemiologic and experimental studies are required to estimate the association between mercury exposure and the development of MetS components, especially obesity; (2) Additional investigations of the possible effect of organism's mercury content modulation on MetS pathogenesis should be undertaken.

Methane is a powerful greenhouse gas, and the abrupt degassing events that recently have formed large craters on the Russian Arctic Yamal and Gydan Peninsulas have caused major concern. Here we present field data on cover sediments and evolution of a gas-emission crater discovered in the Erkuta–Yakha River valley in the southern Yamal Peninsula in June 2017. The crater is located south of other similar craters discovered over the past decade in northern West Siberia. Data were collected during a field trip to the Erkuta crater in December 2017 which included field observations and sampling of permafrost soil and ground ice from the rim of the crater. All soil and ice samples were measured for contents of methane and its homologs (ethane and propane) and carbon dioxide. The contents of carbon dioxide in some samples are notably higher than methane. The strongly negative δ13С of methane from ground ice samples (−72‰) is typical of biogenic hydrocarbons. The ratio of methane to the total amount of its homologs indicate a component of gases that have migrated from a deeper, thermogenic source. Based on obtained results, a potential formation model for Erkuta gas-emission crater is proposed, which considers the combined effect of deep-seated (deep gas migration) and shallow (oxbow lake evolution and closed talik freezing) causes. This model includes several stages from geological prerequisites to the lake formation.

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