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Authorities cracked down on online resources that have been used to mobilize civic activism. As major antigovernment protests were held in dozens of cities across Russia in 2017, authorities focused on censoring online sources of information on upcoming demonstrations. The prosecutor general asked Roskomnadzor to initiate the blocking of websites that were allegedly inciting public disorder. One of the pages targeted was a group on the social networking site VKontakte called \"We Demand Systemic Changes in the Country.\"[19]
However, while Russians are still able to access a wide variety of outside sources, many independent online media outlets within Russia have been forced to shut down over the past two years due to increasing government pressure. Self-censorship is encouraged by the vague wording of restrictive legislation, the seemingly arbitrary manner in which these laws are enforced, and the near-total ineffectiveness of judicial remedies.[50] Laws prohibiting \"extremist\" content and the government's crackdown on certain media outlets have had a chilling effect on free speech, particularly with regard to such sensitive topics as governance failures, corruption, the war with Ukraine, the annexation of Crimea, violations of civil rights, religion, and the LGBTI community. The new \"Information Society Development Strategy\" adopted in May 2017 directs officials to ensure that Russian \"spiritual and cultural values\" are represented in internet governance policy,[51] potentially foreshadowing further censorship.
Cave geometry also determines how surface conditions will influence the cave environment (de Freitas & Littlejohn, 1987; Tuttle & Stevenson, 1978; Williams & McKay, 2015; Williams et al., 2017). Acquiring a data set with adequate statistical power to model how temperature and humidity varies by structure will enable a robotic platform to both identify the most stable and buffered locations within a cave (Q11), which, in most cases, will represent the regions of optimal habitability and thus the best locations to sample for evidence of life (Q12). Moreover, Q10 highlights the importance of cave ice. Airflow, which is also influenced by cave geometry as well as surface temperature and barometric pressure shifts governs cave temperature and humidity regimes and water/water ice stability (Perșoiu & Onac, 2019; Williams & McKay, 2015; Williams et al., 2017).
Another important topic is how to identify, measure, and quantitatively examine paleoclimate records from planetary cave deposits (Q19). For Earth, paleoclimatic research involves examining the carbon and oxygen isotope composition of cave minerals and speleothems in both volcanic (Ulloa et al., 2013) and dissolution (both carbonate and evaporite) caves (De Waele et al., 2017; Fairchild & Baker, 2012). On the Moon, Mars, and other planetary bodies, the presence of secondary minerals is likely related to local geochemical processes, possibly due to the presence of volatiles, which has direct implications in the search of life on Mars. Importantly, could we apply the same terrestrial techniques to extract paleoclimatic and/or paleoenvironmental information from speleothems on another planetary body Terrestrial caves are typically characterized by stable climatic conditions where evidence of past climates (mainly within sediments and chemical precipitates) can be preserved much better than on the surface. By comparing similar deposits on Earth (e.g., Fairchild & Baker, 2012), Martian cave deposits may represent key proxies for further characterizing the climatic history of Mars. However, until we can conduct a robotic mission to explore a Martian cave interior, this remains speculative.
Alexopoulos, Theocharis and Packianather, Michael ORCID: -0002-9436-8206 2017. A monitoring