New data on sedimentation and biostratigraphy of ancient and New Azov Deposits (Sea of Azov)

Matishov, G. G.; Dyuzhova, K.V.; Ковалева, Галина; Polshin, V. V.

doi:10.1134/s1028334x16040048

Cited by 12 publications

(3 citation statements)

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“…It was revealed that the smallest values of sedimentation rate are confined to the transit zones and weak accumulation of sedimentary material and coincide with the directions of the main currents in the Taganrog Bay [29]. It is shown that the Azov Sea level variation occurs with a delay compared with the landscape-climatic phases [30]. The obtained data confirm the interconnection of marine and terrestrial processes occurring in the Azov Sea basin, while the transgressive phases are preceded by general moistening of the adjacent territories and the regressive ones, on the contrary, are associated with aridization of the climate [30].…”

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“…It is shown that the Azov Sea level variation occurs with a delay compared with the landscape-climatic phases [30]. The obtained data confirm the interconnection of marine and terrestrial processes occurring in the Azov Sea basin, while the transgressive phases are preceded by general moistening of the adjacent territories and the regressive ones, on the contrary, are associated with aridization of the climate [30]. Based on the analysis of the archaeological research results in conjunction with the paleogeography, geomorphology and biostratigraphy data, landscapes of the Lower Don region in the Late Holocene era were reconstructed.…”

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confidence: 99%

“…Based on the analysis of the archaeological research results in conjunction with the paleogeography, geomorphology and biostratigraphy data, landscapes of the Lower Don region in the Late Holocene era were reconstructed. The factors controlling the migration of the population in this region were climate and the Azov Sea level variations [30,31].…”

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R/V “Professor Panov”: 15 Years of Marine Scientific Research

Matishov¹,

Stepanyan²

2018

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The Taganrog Bay of the Azov Sea has attracted attention of scientists for more than 100 years. In different periods intensity of research sometimes increased, sometimes decreased; and in 2003 alone, when the Southern scientific center of RAS (SSC RAS) was formed, it became possible to perform the year-round, large-scale and comprehensive studies of the marine environment and biota both in the Bay and in the river Don which is the most important river-way of the southern Russia. The investigations carried out in course of the past 15 years have permitted to solve many riddles existing in the Taganrog Bay paleo-history, to study formation of its bioproductivity and the features of its hydrological and hydro-biological regimes, to perform large-scale assessment of anthropogenic activity (pollution, fishing, poaching, shipping, etc.). Such a marine scientific research would be impossible but for the research vessel (R/V) "Professor Panov" named in honor of the outstanding Russian marine geologist and geo-morphologist, professor of the Leningrad and the Rostov universities D. G. Panov. During 15 years, due to the R/V "Professor Panov" more than 150 expeditions were performed that permitted to collect a significant amount of modern information which significantly expanded our notions on the Taganrog Bay and the Sea of Azov. The expeditions on board the R/V "Professor Panov" are complex and answer the purposes and problems of modern oceanology in the fields of hydrology, hydro-biology, hydro-chemistry, lithology, paleogeography, ornithology, etc.

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confidence: 99%