scholarly journals Composition and distribution of macrophytobenthos near the coast of Tarkhankut Peninsula (The Black Sea, Crimea)

Algologia ◽  
2021 ◽  
Vol 31 (3) ◽  
pp. 249-270
Author(s):  
S.Yu. Sadogurskiy ◽  
◽  
S.O. Sadogurska ◽  
T.V. Belich ◽  
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
The Black Sea ◽  
Anthropogenic Pressure ◽  
Black Sea Region ◽  
High Productivity ◽  
Number Of Species ◽  
Coastal Marine ◽  
Sublittoral Zone ◽  
Marine Areas

The data on the composition and distribution of macrophytobenthos of marine and lagoon water areas of the Black Sea coastal zone in the west of the Tarkhankut Peninsula in the summer season are presented. It is shown that the occurrence and general characteristics of the vegetation cover are determined by the type of substrate. In the sea (where hydrological conditions are relatively homogeneous), the ratio of ecological-floristic groups and the species composition change with distance from the coast and along with it, depending on the depth and geomorphological features of coastal zone fragments. In the lagoon, the ratio of such groups changes along the complex gradient of environmental factors, formed by the groundwater runoff of fresh and marine waters. Within the surveyed area, 91 species of macrophytes were registered: Tracheophyta – 1 species (1.1%), Chlorophyta – 23 (25.3%), Ochrophyta (Phaeophyceae) – 21 (23.1%), and Rhodophyta – 46 (50.5%). Of these, 87 species were recorded in the sea (including 44 in the pseudolittoral zone and 81 – in the sublittoral zone). The macrophytobenthos has a pronounced marine oligosaprobic character. Short-vegetation Rhodophyta dominate by the number of species, and perennial Phaeophyceae dominate by biomass, reaching 1 kg∙m-2 in the pseudolittoral and almost 7 kg∙m-2 in the sublittoral. In the lagoon, 18 species of macrophytes were registered (4 exclusively in the lagoon). Mesosaprobic short-vegetation Rhodophyta dominate by the number of species; marine and brackish-water macrophytes are equally represented. Polysaprobic perennial Tracheophyta, which belong to the marine group, dominate by biomass, which is ranging from 0.04 to 1.2 kg∙m-2. It was found that at the time of the research, the macrophytobenthos of the surveyed area was characterized by high productivity, high species, and coenotic diversity. There were taxa and biotopes, which are subject to special protection under regional and international programs. In general, the nature of the vegetation, the composition of the flora and the ratio of the main ecological-floristic indicators corresponded to those indicated for the Tarkhankut-Sevastopol hydrobotanical region of the Black Sea. Considering the sozological value, the aquatic component of the territorial-aquatic complex was recommended for conservation and inclusion in the ecological networks (incl. the Emerald Network). The increased anthropogenic pressure and the threat of the coastal zone transformation actualize the problem of its conservation as one of the key reserves of the floristic and biotopic diversity of coastal-marine areas in the Northern Black Sea region.

scholarly journals The spatial pattern of selected extreme precipitation indices for Turkey (1975-2012)

2020 ◽  
Vol 19 (1) ◽  
pp. 19-30
Author(s):  
Faize Sarış
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
Extreme Precipitation ◽  
Precipitation Extremes ◽  
The Black Sea ◽  
The South ◽  
Black Sea Region ◽  
North East ◽  
The North ◽  
Rainy Days

AbstractThis paper analyses extreme precipitation characteristics of Turkey based on selected WMO climate change indices. The indices – monthly total rainy days (RDays); monthly maximum 1-day precipitation (Rx1day); simple precipitation intensity index (SDII); and monthly count of days when total precipitation (represented by PRCP) exceeds 10 mm (R10mm) – were calculated for 98 stations for the 38-year overlapping period (1975–2012). Cluster analysis was applied to evaluate the spatial characterisation of the annual precipitation extremes. Four extreme precipitation clusters were detected. Cluster 1 corresponds spatially to Central and Eastern Anatolia and is identified with the lowest values of the indices, except rainy days. Cluster 2 is concentrated mainly on the west and south of Anatolia, and especially the coastal zone, and can be characterised with the lowest rainy days, and high and moderate values of other indices. These two clusters are the most prominent classes throughout the country, and include a total of 82 stations. Cluster 3 is clearly located in the Black Sea coastal zone in the north, and has high and moderate index values. Two stations on the north-east coast of the Black Sea region are identified as Cluster 4, which exhibits the highest values among all indices. The overall results reveal that winter months and October have the highest proportion of precipitation extremes in Turkey. The north-east part of the Black Sea region and Mediterranean coastal area from the south-west to the south-east are prone to frequent extreme precipitation events.

scholarly journals River sediment transport and coastal erosion in the southeastern Black Sea rivers / Transport riečnych sedimentov a erózia pobrežia riek krajiny v juhovýchodnej časti čierneho mora

2012 ◽  
Vol 60 (4) ◽  
pp. 299-308 ◽  
Author(s):  
Mehmet Berkun ◽  
Egemen Aras
Keyword(s):  
Sediment Transport ◽  
Black Sea ◽  
Coastal Erosion ◽  
The Black Sea ◽  
Coastal Protection ◽  
Anthropogenic Pressure ◽  
Hydroelectric Power ◽  
Protection Measures ◽  
Black Sea Region ◽  
Bed Material

In the Southeastern Black Sea Region, rivers are dammed for hydroelectric power and irrigation. The natural course of fluvial alluvium transport is almost completely altered because of planned and constructed dams and coastal protection measures. Decreasing volume of sediment carried to the sea cause intensification of the shore erosion. The Black Sea Rivers and coastal areas of Turkey and Georgia are under heavy anthropogenic pressure because of the bed material extraction and coastal erosion rate. In this study, environmental effects of dams and related effects of sediment transport on coastal erosion in the Eastern Black Sea region are discussed.

Tsunami vulnerability along the western Bulgarian Black Sea coast - from the historical review towards multidisciplinary assessment approach

2021 ◽  
Author(s):  
Lyubka Pashova ◽  
Liliya Dimitrova ◽  
Emil Oynakov ◽  
Vasko Galabov
Keyword(s):  
Risk Assessment ◽  
Coastal Zone ◽  
Black Sea ◽  
Tsunami Hazard ◽  
The Black Sea ◽  
Black Sea Region ◽  
Tsunami Modelling ◽  
Black Sea Coast ◽  
Hazard And Risk ◽  
Sea Coast

<p>Over the last two decades, in line with the global trend of expanding research into natural hazards and disaster risk reduction, the tsunami hazard and risk assessment along the coast of Europe has become a hot topic of research. In all its aspects, tsunami research includes the study of tsunami documentary evidence, historical data collection, field experiments, laboratory research, theoretical numerical and analytical modelling, and in-depth analysis of recent tsunami events. Tsunami modelling research methodologies and holistic approaches to risk assessment are continually being improved. Researches are directed to develop conventional standardised methods to analyse tsunami hazard and risk with associated uncertainties, aiming to reduce possible adverse effects on potentially vulnerable coastal settlements, coastal and marine infrastructures and natural ecosystems.</p><p>In the Black Sea, dangerous tsunami waves are a relatively rare phenomenon that cannot be forecast. Multidisciplinary studies focused on mapping and dating past events on the Black Sea coast, determining the causes, frequency of recurrence, and current prospects for tsunamis occurrence (risk) are not yet fully clarified or are in their infancy. Moreover, tsunami hazard along the Bulgarian coast is poorly understood and not considered in the National methodology for flood hazards and risk in the coastal zone. Numerical tsunami modelling performed in recent years for the region still needs to be improved. These events are relatively rare, few such cases have been documented, and validation data are scarce or missing.</p><p>This study provides a comprehensive inventory of tsunami sources from scientific publications, model studies of tsunami generated waves carried out during the recent years and an analysis of the results from recently established early warning systems in the Black Sea region. For the Bulgarian coastal zone, the results of studies of active faults with tsunamigenic potential in and around vulnerable coastal zones, available registrations at sea level during seismic events and some extreme meteorological events for the last century are summarized. A near-field and far-field tsunami sources that can generate tsunamis and affect the Bulgarian coastline are briefly reviewed. High-resolution data are needed for more credible tsunami numerical modelling for the western Black Sea region. Preliminary studies of the available datasets regarding Digital Elevation Model (DEM) and bathymetry for specific locations along the coastal zone are presented as well the needed accuracy and completeness of the data. Some consideration regarding the available and newly establish research infrastructure in the western Black Sea are also discussed.</p><p><strong>Acknowledgements:</strong><strong> </strong>The authors would like to thank the Bulgarian National Science Fund for co-funding the research under the Contract КП-СЕ-КОСТ/8, 25.09.2020, which is carried out within the framework of COST Action 18109 “Accelerating Global science In Tsunami HAzard and Risk analysis” (AGITHAR; https://www.agithar.uni-hamburg.de/).</p>

Macroalgae and cyanobacteria of supra- and pseudolittoral zones on the Southern coast of Crimea

2020 ◽  
pp. 63-68
Author(s):  
Tatiana V. Belich ◽  
Svetlana A. Sadogurskaya ◽  
Sergei Ye. Sadogurskiy
Keyword(s):  
Coastal Zone ◽  
Geographical Area ◽  
The Black Sea ◽  
Southern Coast ◽  
Crimean Peninsula ◽  
Marine Area ◽  
Coastal Marine ◽  
Black Sea Coast ◽  
Protected Natural Area ◽  
Marine Areas

The Southern coast of Crimea (SCC) forms a separate physical and geographical area located in the extreme South of the Crimean Peninsula, between the Main range of the Crimean Mountains and the Black Sea coast. Currently, the coast of the SCC is mostly concreted (65%). Therefore, fragments of the coastal zone with preserved natural vegetation have a special environmental value, one of such sites is the Kuchuk-Lambatsky stone chaos. Kuchuk-Lambatsky stone chaos is a Specially Protected Natural Area (SPNA), but the coastal-marine area does not have any protected status. In the coastal zone of the sea, it is very important that protected areas include both land areas and coastal–marine areas. Information about the species composition and the structure of phytobenthos of the supra – and pseudolittoral zones in the marine area of the Kuchuk-Lambatsky stone chaos is presented. In total 43 species of phytobenthos have been identified: Rhodophyta – 10 species, Chlorophyta – 7, Ochrophyta – 3, Cyanobacteria – 23. Altogether 23 species were found in the supralitoral zone. During the observation period, the vegetation cover of the supralittoral zone was formed exclusively by Cyanobacteria, represented by one class, 5 orders, 10 families and 15 genera. The community, dominated by Calothrix scopulorum, Gloeocapsopsis crepidinum and Aphanocapsa incerta was found. The community is mainly formed by typical benthic, marine, and cosmopolitan species. In total 20 species of macrophyte algae were observed in the pseudolittoral zone. The Rhodophyta division is represented by one class, 5 orders, 6 families, and 8 genera. The Ochrophyta division has one class, 2 orders, 3 families, and 3 genera. The division Chlorophyta is represented by one class, 2 orders, 3 families, and 4 genera. In the pseudolittoral zone the community dominated by Ulva kylinii and U. intestinalis has been registered. It is formed mainly by annual, marine and brackish-marine, mesosaprobic species.

DISTRIBUTION OF DISSOLVED METHANE IN SURFACE COASTAL WATERS OF THE NORTHEASTERN PART OF THE BLACK SEA

2017 ◽  
Author(s):  
Elena Kovaleva ◽  
Elena Kovaleva ◽  
Alexander Izhitskiy ◽  
Alexander Izhitskiy ◽  
Alexander Egorov ◽  
...  
Keyword(s):  
Black Sea ◽  
Natural Waters ◽  
Sea Water ◽  
The Black Sea ◽  
Methane Formation ◽  
Anthropogenic Pressure ◽  
Russian Science ◽  
Southeastern Part ◽  
Dissolved Methane ◽  
Continental Runoff

Studying of methane formation and distribution in natural waters is important for understanding of biogeochemical processes of carbon cycle, searching for oil and gas sections and evaluation of CH4 emissions for investigations of greenhouse effect. The Black Sea is the largest methane water body on our planet. However, relatively low values of methane concentration (closed to equilibrium with the atmospheric air) are typical of the upper aerobic layer. At the same time, the distribution pattern of CH4 in surface waters of coastal areas is complicated by the influence of coastal biological productivity, continental runoff, bottom sources, hydrodynamic processes and anthropogenic effect. The investigation is focused on the spatial variability of dissolved methane in the surface layer of the sea in coastal regions affected by the continental runoff and anthropogenic pressure. Unique in situ data on methane concentrations were collected along the ship track on 2 sections between Sochi and Gelendzhik (2013, 2014) and 2 sections between Gelendzhik and Feodosia (2015). Overall 170 samples were obtained. Gas-chromatographic analysis of the samples revealed increase of CH4 saturation in the southeastern part of the Crimean shelf and the Kerch Strait area. Such a pattern was apparently caused by the influence of the Azov Sea water spread westward along the Crimean shore from the strait. This work was supported by the Russian Science Foundation, Project 14-50-00095 and the Russian Foundation for Basic Research, Project 16-35-00156 mol_a.

SPECIALIZED OCEANOGRAPHIC DATABASE FOR INFORMATION SUPPORT OF THE BLACK SEA COASTAL ZONE STUDY

2017 ◽  
Author(s):  
Alexey Khaliulin ◽  
Alexey Khaliulin ◽  
Andrey Ingerov ◽  
Andrey Ingerov ◽  
Elena Zhuk ◽  
...  
Keyword(s):  
Coastal Zone ◽  
Black Sea ◽  
Data Bank ◽  
Information Support ◽  
The Black Sea ◽  
Federal State ◽  
Short Term ◽  
Marine Hydrophysical Institute ◽  
State Budget ◽  
Oceanographic Data

The information resources of the Federal State Budget Scientific Institution “Marine Hydrophysical Institute of RAS” (FSBSI MHI) oceanographic data bank (MHI BOD), which contains about 115,000 oceanographic and more than 27,000 hydrochemical stations accomplished in the Black Sea coastal zone, as well as experience accumulated while providing information support of the coastal zone research, main directions of activities, and short-term plans are considered.

Obsidian Exchange Networks in Prehistoric Anatolia: New Data from the Black Sea Region

Paléorient ◽  
2013 ◽  
Vol 39 (2) ◽  
pp. 173-182
Author(s):  
Bleda S. Düring ◽  
Bernard Gratuze
Keyword(s):  
Black Sea ◽  
The Black Sea ◽  
Exchange Networks ◽  
Black Sea Region

The referendum as an institution in the Black Sea Region: Does it signal the rise or collapse of democracy?

2019 ◽  
Vol 17 (4) ◽  
pp. 161-185
Author(s):  
Małgorzata Podolak
Keyword(s):  
Black Sea ◽  
Direct Democracy ◽  
The Black Sea ◽  
Moral Issues ◽  
Black Sea Region ◽  
Positive Effects ◽  
The Subject ◽  
Democratic Systems ◽  
Important State ◽  
Constitutional Changes

Views on the institution of direct democracy have changed during the period of democratic transition. The various advantages and positive effects of direct democracy have been confirmed by the practice of some democratic countries. Its educational and political activation value for society was also noted, without which civil society cannot form. The referendum is especially treated as the purest form of correlation between the views of society and the decisions of its representatives. In a situation where two representative bodies are present – the parliament and the president – a referendum is considered a means of resolving disputes between them in important state affairs. The referendum is nowadays becoming more than just a binding or consultative opinion on a legislative act, especially a constitution. First and foremost, it is important to see the extension of the type and scope of issues that are subject to direct voting. Apart from the traditional, i.e., constitutional changes, polarising issues that raise considerable emotion have become the subject of referenda. Problems of this type include, in particular, moral issues, membership in international organisations, and so-called ‘New Policy’. This article presents the role and importance of the referendum as an institution shaping the democratic systems of the Black Sea Region.

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