Янко-Хомбах, Валентина ВенедиктівнаШнюков, Євген ФедоровичІноземцев, Ю. І.Паришев, О. О.Коніков, Євген ГеоргійовичКадурін, Сергій ВолодимировичПедан, Галина СергіївнаСминтина, Олена ВалентинівнаЯнко-Хомбах, Валентина ВенедиктовнаШнюков, Евгений ФедоровичИноземцев, Ю. И.Парышев, A. А.Коников, Евгений ГеоргиевичКадурин, Сергей ВладимировичПедан, Галина СергеевнаСмынтына, Елена ВалентиновнаInozemtsev, Yu.Paryshev, A.Konikov, Yevhenii G.Yanko-Hombach, Valentyna V.Kadurin, Serhii V.Pedan, Halyna S.Smyntyna, Olena V.Shniukov, Yevhen F.2012-04-182012-04-182008Black sea-mediterranean corridor during the last 30 ky: sea level change and human adaptation (2005–2009) : IV plenary meeting and field trip IGCP 521 (Bucharest ; Varna, 4–16 Oct. 2008). – Bucharest, 2008https://dspace.onu.edu.ua/handle/123456789/2362Caspian-Black Sea mediterranean corridor during last 30 ky: sea level change and human adaptive strategies (2008-2010), plenary meeting and fild trip INQUA 0501, (4, 2008);4-16, Oct., 2008Mud volcanoes at the bottom of the Black Sea and Sea of Azov have been studied for more than 20 years. The priority in investigating mud volcanoes belongs to a group of researchers under the guidance of one of the authors, E. Shnyukov. Data on their lithological structure, gSochemistry of deposits, water chemistry, and thermal condition of the deposits are available in many publications (Konyukhov et al., 1990; Shnyukov et al., 2003; Shnyukov and Kobolev, 2004; Stadnitskaya and Belen'kaya, 2000; and others).enpseudovolcanismabyssal plaingenesismethaneArticle