大连市海洋旅游文化发展研究

大连是著名的海滨旅游城市,其丰富的海洋文化遗存为海洋旅游文化资源开发提供了有利条件。文章对大连市海洋旅游文化资源现状及存在问题进行分析,提出了大连市海洋旅游文化的发展对策。     

海洋文化在大连城市发展中的战略考量

大连市在率先基本实现现代化的进程中,提出"建设东北亚重要国际航运中心"的目标,根据大连的历史和现实,在该目标实践过程中,应当建设以海洋文化为特色的城市文化.在海洋科技方面,大连已凸显实力,在依据海洋事业的传统和优势的基础之上,把建设"现代海洋文化名城"当作重要任务来抓,从而推动城市的和谐及创新发展.     

海洋文化与大连海洋旅游开发

海洋文化是人类社会历史实践过程中受海洋影响所创造的物质财富和精神财富的总和。大连是著名的海滨旅游城市,其丰富的海洋文化遗存给海洋文化旅游资源开发提供了有利条件。文中在对大连市海洋文化旅游资源现状进行详尽分析的基础上．提出了如何借助大连市海洋文化的优势．实现旅游业可持续发展的具体对策。     

青岛海洋文化产业发展战略研究

文章论述了海洋文化与海洋文化产业的关系,分析了深圳、舟山和连云港等沿海城市发展海洋文化产业的主要经验,并提出:立足青岛海洋文化和齐鲁文化实际,以市场经济和政府引导为双翼,以企业文化、大众文化为体魄,以各项文化产业要素为羽毛,以世界文化潮流和打造知名品牌为龙头,以人才培养和科技创新为动力,全面发展青岛海洋文化产业的战略思考。     

海洋文化与青岛旅游开发

海洋文化是人类社会历史实践过程中受海洋影响所创造的物质财富和精神财富的总和.青岛是中国海洋文化的核心区域之一,其丰富的海洋文化遗存给海洋文化旅游资源开发提供了有利条件,预示着海洋文化内涵丰富的海洋旅游将成为青岛新世纪旅游的热点,同时也推动青岛旅游业的发展,发挥海洋旅游产业在青岛市建设现代化国际城市中的作用.     

我国南海海洋国家公园建设

为进一步保护我国南海海洋生态环境和海洋历史文化,促进南海地区社会经济的可持续发展,同时完善我国国家公园制度建设,文章在概述我国国家公园和国内外海洋公园建设情况的基础上,分析建设我国南海海洋国家公园的必要性和面临的挑战,并提出政策建议。研究结果表明:我国相继建设国家级风景名胜区和国家公园,其中国家公园规模更大,且以生态环境保护为主;美国等海洋国家公园的建设实践较完善;我国具有海洋公园建设和管理优势,但也存在不足,尤其尚未建立海洋国家公园;我国南海海洋国家公园建设在保护生态环境、传承传统文化、管理旅游活动和恢复渔业资源等方面的意义重大,但面临体制机制创新、管理技术突破以及人与自然和谐相处等方面的挑战;建设我国南海海洋国家公园应以珊瑚礁保护区为基础、以国家公园体制改革为契机、生态环境保护与社会经济发展并行、发扬海洋历史文化以及建立海洋科研基地。     

加强海洋文化建设 保护海洋生态环境

海洋文化,作为人类文化的重要组成,是人类认识、把握、开发、利用海洋,调整人和海洋的关系,在开发利用海洋的社会实践中形成的精神成果和物质成果的总和.历史证明,海洋文化在任何时代都代表着一种先进文化,它具有强烈的开创意识和冒险意识,含有不畏艰险和勇于拼搏的精神.     

海洋文化的学科主体性困境与建构

中国对于海洋文化的理论探索与建构已有数十年的积淀,然而目前学术界对其学科主体性依然缺乏共识。为增强中国海洋强国建设的文化软实力,文章解答海洋文化学科主体性的基本问题,分析海洋文化学科主体性建构面临的挑战,并提出具有针对性的建议。研究结果表明：海洋文化属于知识门类意义上的学科,是独特的知识集合和自成系统的理论体系;由于传统学术思维的惯性、经世致用思想的影响、研究对象范畴模糊和研究方法特性缺失等因素,海洋文化的学科主体性尚未真正确立;海洋文化的学科主体性建构应坚持“人 海主体”的理论建构、“人 海和谐”的价值取向、“人 海依存”的研究范畴和“人 海互动”的研究方法。     

基于文化生态理论的山东海洋文化产业创新发展

文化生态理论是建立在马克思主义方法论之上的关于文化的生态学理论。与其他文化生态相比,海洋文化生态具有开放性、多样性、丰富性、主体性等特征,强调人类整体利益、人与自然和谐以及经济平衡发展。山东海洋文化资源丰富,海洋文化产业开发应秉持生态化原则,建设海洋文化生态保护区,加强海洋文化旅游基础设施建设,重点开发滨海文化旅游、海岛休闲旅游、海洋艺术等产业项目,促进“双碳”和“海洋强省”目标的达成以及经济社会发展的全面绿色转型。     

中国可以走不称霸的海洋强国之路

<正>中国建设海洋强国的思想和原则受民族精神和宪法的制约,是能够走上不称霸发展道路的。中国文化中有丰富的优良传统。例如:宽容大度的精神,是中华民族的优秀文化传统和独特的民族精神。     

Model of the post-Cenozoic evolution of the cryolithozone of the shelf of the western part of the Laptev Sea

The analysis of the structure of the cryolithozone, facies, and thicknesses of the Quaternary sediments and the results of the physicochemical mathematical modeling of the modern shelf of the western part of the Laptev Sea support the influence of the Late Pleistocene glaciations on the heat conditions and the distribution of the permafrost in the area. A ～200-m thick glacier formed under aerial conditions from atmospheric precipitation represented the metamorphosed snow cover. According to the modeling, the long-living (from 60?50 to 10?4 ky) glacier reduced the thickness of the permafrost rocks in the reviewed shelf area for 280–360 m. The Holocene marine transgression additionally decreased the thickness from 50–140 m on the inner shelf to 220–350 m on the outer shelf. The modern submarine cryolithozone 450-0 m thick is wide-spread in the studied region from the coast to the shelf boundary (isobaths of 130–140 m), where it pinches out at a distance of ～380 km from the coast at a depth of ～250 m above the sea level.     

Investigation of the mechanism of the long-term evolution of the carbon cycle in the ecosystem of the Sevastopol bay

We analyze the components of the carbon system of the Sevastopol bay waters and the balance of main sediment-forming substances using the data of field investigations in 1998–2008. The interannual variations of total inorganic carbon and the equilibrium partial pressure of carbon dioxide in the bay water are noted. An increase in the flux of carbon dioxide into the bay and in the content of organic carbon in bottom sediments is revealed, and an explanation of this phenomenon is given. The priority accumulation of organic carbon in the sediments of the bay is established. We assess the interannual variation in the relative abundances of organic and inorganic carbon as an index of the carbon cycle stability.     

Contemporary state of the investigation of the influence of the discharge of rivers on the hydrologic structure of the Black Sea

We generalize and analyze the state of investigations of the influence of river waters on the hydrologic structure of the Black Sea. Specific features of the water, regime and hydrography of rivers flowing into the sea, data on the discharge of rivers, and intrayear and interyear variability of the discharge are presented. We discuss and analyze works studying the transformation of river waters, routes of desalinized sea waters, and their influence on the thermohaline structure and dynamic regime of the sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Modelling of the ecosystem of the Black-Sea shelf zone near the estuary of the Danube

We analyze the results of numerical calculations performed according to the three-dimensional interdisciplinary model of an ecological system of the Black-Sea shelf zone near the estuary of the Danube. The complete system of equations of hydrothermodynamics is solved together with transport equations of the advection-diffusion-reaction type used to describe the transformation of a substance (nitrogen) between the components of the characteristic vectors of the ecosystem: plankton, detritus, and biogenic elements (nitrates). We describe the distinctive features of the circumcontinental distribution of components obtained as a result of numerical experiments and present arguments for the conclusion that the ecosystem of the Danube estuary water area plays the role of a buffer zone between the press of the Danubian biogenic pollutions and the neighbouring areas of the shelf zone and open sea. Translated by Peter V. Malyshev and Dmitry V. Malyshev     

Dynamics of the ice cover and peculiarities of the ice transportation of the sediments at the tidal flats of the Kandalaksha Gulf of the White Sea

Ten years of semistationary studies of the interaction of the ice cover and the coastal relief of the Kandalakhsa Gulf in the White Sea allowed us to reveal the peculiarities of these processes in the warm and cold years and the mechanisms of the origination of ice forms, including ice tents, which govern the character of the tidal flats. Three dynamic fast ice zones are distinguished by their geomorphological location, morphology, and ice dynamics. The dependence of the mechanisms and volumes of the enrichment of the fast ice in the sediments on the coastal zone??s relief was established. At the coast of the Kindo Peninsula (Velikaya Salma Strait), the ice mostly contains fine-sandy sediments. Coarser sediments, including boulders, are occasional and frozen into the ice at the contact of the fast ice and the bottom. At the expense of the ice??s spreading by 4?C6 times in the warm years and 2?C4 times in the cold years, several thousand tons of sediments mostly from the tidal flat??s surface (100?C700 m³ from 1 km of coast in the wide tidal flats and <50 m³ on the steep coasts) are delivered to the water area.     

Relationship between the path of the Kuroshio in the south of Japan and the path of the Kuroshio Extension in the east

A relationship between paths of the Kuroshio and Kuroshio Extension (KE) is investigated, using the satellite-derived altimetry dataset of 1993–2008. When the Kuroshio takes the nearshore nonlarge meander path or typical large meander path and resultantly goes through the deeper channel (about 2500 m) of the Izu-Ogasawara Ridge, the KE path adopts a relatively stable state with the two quasi-stationary meanders. On the other hand, when the Kuroshio takes the offshore nonlarge meander path and then passes over the shallower part of the Ridge (about 1000 m), the KE path tends to be convoluted, i.e., an unstable state.     

Modelling of the ecosystem on the shelf of the Republic of Guinea

Three mathematical models are considered: a two-dimensional model for calculating the concentration fields of the ecosystem components on the shelf of the Republic of Guinea, a pointwise model for the annual variation of the components, and a two predators-prey model. These models are used to study the effect of hydrodynamic conditions on the state of the shelf ecosystem and for research into the causes which distort the balance between marketable and unmarketable fish.Translated by Mikhail M. Trufanov.     

Evolution of the slope of the buried depression of the Black Sea

The first data on the temporal evolution of the slope of the buried depression of the Black Sea are obtained. The sharp change in the rate of the decrease in the slope steepness that occurred in the Late Miocene-Pliocene time reflects a reorientation of the vector of mutual movement and a related intensification of the collision between the Arabian and Eurasian lithospheric plates.     

The stages of the development of the basin of the Bransfield Strait

The study of the sedimentary body of the Bransfield Strait has made it possible to identify several sedimentary complexes, to construct the first electronic charts for the acoustic basement, and to establish four stages of the evolution of its floor, which updates the previous knowledge about the formation of the strait. At the first stage, there was an increase in tension stresses that were accompanied by the local splits of the continental crust at the periphery of the Antarctic Peninsula. At the second stage, a graben-like structure filled with the Lower stratigraphic complex was formed northward of the Antarctic Peninsula. At the third stage, the continuing processes of extension led to intensive explosive activity of the growing volcanic structures and filling of the graben with sediments of the Middle seismostratigraphic complex. The fourth stage, which has continued until recently, is characterized by quasi-linear localization of the major centers of volcanic activity in the band closer to the South-Shetland Islands and the formation of the Upper seismostratigraphic sedimentary complex. The evolution of the floor of the Bransfield Strait reflects the process of penetration of the American-Antarctic ridge to the continental lithosphere of the Antarctic Peninsula for the last million years.     

Influence of the dynamics of currents on the hydrophysical structure of the waters and the vertical exchange in the active layer of the Black Sea

An analysis of the data of measurements of the fine structure and microstructure fluctuations of hydrophysical fields in the upper 200-m layer of the Black Sea carried out using CTD profilers and a Baklan free falling microstructure and turbulence profiler revealed the existence of a positive correlation between the intensity of the fine structure and microstructure fluctuations and the dynamics of the currents. On the other hand, the level of the fine structure and microstructure fluctuations reflects the rate of the vertical turbulent exchange. It was shown that, in the case of the absence of the Black Sea Rim Current (BSRC) jet or clearly manifested mesoscale eddy structures, the vertical turbulent exchange in the pycnocline is weak, while, in the opposite case, it is stronger. The results obtained support the supposition that the interbasin dynamics play an important role in the maintenance of the rate of small-scale mixing in the pycnocline and halocline and provide the vertical transport of dissolved oxygen from the cold intermediate layer into the deeper layers of the sea.