Relevant bibliographies by topics / Deep sea ecology

Contents

  1. Journal articles
  2. Dissertations / Theses
  3. Books
  4. Book chapters
  5. Conference papers
  6. Reports

Academic literature on the topic 'Deep sea ecology'

Author: Grafiati
Published: 4 June 2021
Last updated: 15 June 2025

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Journal articles on the topic "Deep sea ecology"

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Reysenbacii, Anna-Louise, and Cindy Lee Van Dover. "Ecology of Deep-Sea Vents." Ecology 81, no. 12 (2000): 3554. http://dx.doi.org/10.2307/177518.

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FUJITA, TOSHIHIKO. "Ecology of deep-sea ophiuroids." Benthos research, no. 33-34 (1988): 61–73. http://dx.doi.org/10.5179/benthos1981.1988.61.

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Reysenbach, Anna-Louise. "Ecology of Deep-sea Vents." Ecology 81, no. 12 (2000): 3554. http://dx.doi.org/10.1890/0012-9658(2000)081[3554:eodsv]2.0.co;2.

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Barbier, Edward B., David Moreno-Mateos, Alex D. Rogers, et al. "Ecology: Protect the deep sea." Nature 505, no. 7484 (2014): 475–77. http://dx.doi.org/10.1038/505475a.

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Halfar, J., and R. M. Fujita. "ECOLOGY: Danger of Deep-Sea Mining." Science 316, no. 5827 (2007): 987. http://dx.doi.org/10.1126/science.1138289.

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Somero, G. N. "Biochemical ecology of deep-sea animals." Experientia 48, no. 6 (1992): 537–43. http://dx.doi.org/10.1007/bf01920236.

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Won, Yong-Jin. "Deep-sea Hydrothermal Vents: Ecology and Evolution." Journal of Ecology and Environment 29, no. 2 (2006): 175–83. http://dx.doi.org/10.5141/jefb.2006.29.2.175.

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Brown, Chris, and Alan Hodgson. "The Ecology of Deep-Sea Hydrothermal Vents." African Zoology 36, no. 1 (2001): 119–20. http://dx.doi.org/10.1080/15627020.2001.11657128.

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Danovaro, Roberto, Paul V. R. Snelgrove, and Paul Tyler. "Challenging the paradigms of deep-sea ecology." Trends in Ecology & Evolution 29, no. 8 (2014): 465–75. http://dx.doi.org/10.1016/j.tree.2014.06.002.

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Brandt, Angelika. "Deep-Sea Ecology: Infectious Impact on Ecosystem Function." Current Biology 18, no. 23 (2008): R1104—R1106. http://dx.doi.org/10.1016/j.cub.2008.09.035.

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Dissertations / Theses on the topic "Deep sea ecology"

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Copley, Jonathan Timothy Peter. "Ecology of deep-sea hydrothermal vents." Thesis, University of Southampton, 1998. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.246235.

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Howell, Kerry Louise. "The ecology of deep-sea asteroids." Thesis, University of Southampton, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.268842.

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Billett, David. "The ecology of deep-sea Holothurians." Thesis, University of Southampton, 1988. https://eprints.soton.ac.uk/384501/.

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MAGAGNINI, MIRKO. "Viral ecology in the deep sea." Doctoral thesis, Università Politecnica delle Marche, 2009. http://hdl.handle.net/11566/242345.

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BARONE, GIULIO. "The Ecology and Diversity of Benthic Deep-Sea Fungi." Doctoral thesis, Università Politecnica delle Marche, 2019. http://hdl.handle.net/11566/263530.

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I funghi sono ovunque sulla Terra e contano oltre 2 milioni di specie, di cui solo il 10% è stato descritto. Il contributo fungino ai processi ecologici in ecosistemi terrestri è nodale. Tuttavia, la diversità e l’ecologia fungina negli ecosistemi bentonici di acque profonde sono ancora sconosciute. Questa tesi propone un’analisi dettagliata della letteratura corrente sull’ecologia dei funghi e fornisce nuove informazioni sulla loro abbondanza e diversità in campioni di sedimenti di acque profonde raccolti in tutto il mondo. Negli ultimi decenni, la diversità fungina è stata descritta da in numerosi habitat bentonici di acque profonde, ma le informazioni quantitative sul loro ruolo ecologico sono carenti. Questa tesi mostra che l'abbondanza fungina non diminuisce all'aumentare della profondità dell'acqua, contrariamente ad altri eucarioti. Piuttosto, l’abbondanza fungina è generalmente alta e correlata alla disponibilità di risorse trofiche ed in particolare alle concentrazioni di carboidrati, che in questi ecosistemi includono la frazione più refrattaria. Questo studio rivela anche una ricchezza relativamente elevata di OTU fungine, in gran parte assenti nelle banche dati pubbliche, suggerendo che i sedimenti bentonici ospitano nuovi taxa anche ad alto livello tassonomico. Infine, la composizione delle comunità fungine varia nei diversi ecosistemi bentonici profondi in funzione di fattori biologici e ambientali. In particolare, le condizioni termoaline e l'ossigeno disciolto spiegano significativamente le variazioni osservate ad ampia scala spaziale. Nel complesso, questo studio suggerisce che i funghi possono essere responsabili della degradazione di quelle risorse inaccessibili ad altri gruppi microbici e che i funghi sono una componente significativa, anche se largamente trascurata, delle comunità microbiche bentoniche di profondità. Pertanto, i funghi dovrebbero essere inclusi nei modelli per lo studio di reti trofiche e cicli biogeochimici.<br>Fungi occur in every environment of Earth and account for more than 2 million species of which we only roughly described the 10%. Fungal contribution to ecological processes in terrestrial and aquatic ecosystems is pivotal and well recognised. However, fungal diversity and ecology are yet largely unknown in benthic deep-sea ecosystems. Thus, this thesis provides a deep analysis of the current literature about fungal ecology along with laboratory analyses on fungal abundance and diversity in deep-sea sediment samples collected worldwide. In the last few decades, fungi have been described from numerous benthic deep-sea habitats accounting for substantial diversity. However, quantitative information is missing hampering conclusions regarding their ecological role. The results of this thesis indicate that fungal abundance does not decline with increasing water depth, conversely to other eukaryotes. Rather, fungal abundance is generally high and strongly correlated to trophic resource availability and in particular with carbohydrate concentrations, which in deep-sea sediments include the less bioavailable fraction. This study also reveals that benthic deep-sea ecosystems host a relatively high fungal OTUs richness, whose majority did not match public databases, suggesting that benthic deep-sea sediments host novel taxa even at high taxonomic level. Also, assemblage composition considerably varies across benthic deep-sea ecosystems in function of biological and environmental factors such as thermohaline conditions and dissolved oxygen which significantly explain patterns of fungal assemblage composition over a wide spatial scale. Overall, this study suggests that fungi can be responsible for the degradation of those resources inaccessible to other microbial groups and that fungi are a significant, although largely overlooked, component of the benthic deep-sea assemblages which should be included in food-web and biogeochemical cycle models.
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Premke, Katrin. "Aggregations of Arctic deep-sea scavenging amphipods at large food falls = Ökologische Untersuchungen nekrophager Amphipoden in der arktischen Tiefsee /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2006. http://www.loc.gov/catdir/toc/fy0706/2006506722.html.

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Ashford, Oliver Simon. "Illuminating the deep : an exploration of deep-sea benthic macrofaunal ecology in the Northwest Atlantic Ocean." Thesis, University of Oxford, 2017. https://ora.ox.ac.uk/objects/uuid:228c4d19-56a8-41e1-a1da-9ca13fe2eef1.

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Understanding of the fundamental ecology of deep-sea ecosystems remains immature relative to more familiar shallow-water and terrestrial habitats, despite more than two hundred years of scientific investigation. This thesis aims to progress knowledge of deep-sea benthic ecology by the analysis of over three hundred box core samples collected from the Northwest Atlantic continental slope as part of the international NEREIDA programme. Aspects of the ecology of Peracarida (Crustacea) are studied, and this is facilitated by the coupling of a large faunal dataset with extensive environmental information. To further enhance the power of this dataset, phylogenetic and functional characteristics of assemblages are investigated. Using community phylogenetic methodology, it is demonstrated that the peracarid assemblages studied are structured more strongly by variation in environmental parameters than they are by competitive interactions. Analyses demonstrate that the intensity of bottom trawling, seafloor temperature, current speed, food availability, sediment characteristics and physical habitat heterogeneity all influence deep-sea peracarid assemblage biodiversity metrics. Further, the importance of high poriferan biomass for the promotion of peracarid assemblages of high density, biomass, richness and diversity is highlighted. Of relevance to the management of deep-sea ecosystems, the results of this thesis suggest that caution should be exercised when applying species distribution models to data-deficient environments, whilst the location of spatial closures in the NAFO Regulatory Area may not be fully optimal for the protection of all components of diverse benthic assemblages against the impacts of bottom trawling. The importance of deep-sea diversity is demonstrated by the finding of positive biodiversity – ecosystem functioning relationships. However, the form of these relationships is found to be dependent on the biodiversity and ecosystem functioning metrics employed, and a hypothesis for a generalised form of biodiversity – ecosystem functioning relationships is proposed. Finally, this thesis calls for more ambitious deep-sea ecological investigations, and it is hoped that its findings will encourage future research initiatives, helping to further illuminate this enigmatic and fascinating environment.
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Davies, Gareth John. "Aspects of the biology and ecology of deep-sea Scaphopoda (Mollusca)." Thesis, Heriot-Watt University, 1987. http://hdl.handle.net/10399/1005.

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Durkin, Alanna G. "The ecology of deep-sea chemosynthetic habitats, from populations to metacommunities." Diss., Temple University Libraries, 2018. http://cdm16002.contentdm.oclc.org/cdm/ref/collection/p245801coll10/id/488249.

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Biology<br>Ph.D.<br>Chemosynthetic ecosystems are habitats whose food webs rely on chemosynthesis, a process by which bacteria fix carbon using energy from chemicals, rather than sunlight-driven photosynthesis for primary production, and they are found all over the world on the ocean floor. Although these deep-sea habitats are remote, they are increasingly being impacted by human activities such as oil and gas exploration and the imminent threat of deep-sea mining. My dissertation examines deep-sea chemosynthetic ecosystems at several ecological scales to answer basic biology questions and lay a foundation for future researchers studying these habitats. There are two major varieties of chemosynthetic ecosystems, hydrothermal vents and cold seeps, and my dissertation studies both. My first chapter begins at cold seeps and at the population level by modeling the population dynamics and lifespan of a single species of tubeworm, Escarpia laminata, found in the Gulf of Mexico. I found that this tubeworm, a foundation species that forms biogenic habitat for other seep animals, can reach ages over 300 years old, making it one of the longest-lived animals known to science. According to longevity theory, its extreme lifespan is made possible by the stable seep environment and lack of extrinsic mortality threats such as predation. My second chapter expands the scope of my research from this single species to the entire cold seep community and surrounding deep-sea animals common to the Gulf of Mexico. The chemicals released at cold seeps are necessary for chemosynthesis but toxic to non-adapted species such as cold-water corals. Community studies in this area have previously shown that seeps shape community assembly through niche processes. Using fine-scale water chemistry samples and photographic mapping of the seafloor, I found that depressed dissolved oxygen levels and the presence of hydrogen sulfide from seepage affect foundation taxa distributions, but the concentrations of hydrocarbons released from these seeps did not predict the distributions of corals or seep species. In my third chapter I examine seep community assembly drivers in the Costa Rica Margin and compare the macrofaunal composition at the family level to both hydrothermal vents and methane seeps around the world. The Costa Rica seep communities have not previously been described, and I found that depth was the primary driver behind community composition in this region. Although this margin is also home to a hybrid “hydrothermal seep” feature, this localized habitat did not have any discernible influence on the community samples analyzed. When vent and seep communities worldwide were compared at the family-level, geographic region was the greatest determinant of community similarity, accounting for more variation than depth and habitat type. Hydrothermal vent and methane seeps are two chemosynthetic ecosystems are created through completely different geological processes, leading to extremely different habitat conditions and distinct sets of related species. However, at the broadest spatial scale and family-level taxonomic resolution, neutral processes and dispersal limitation are the primary drivers behind community structure, moreso than whether the habitat is a seep or a vent. At more local spatial scales, the abiotic environment of seeps still has a significant influence on the ecology of deep-sea organisms. The millennial scale persistence of seeps in the Gulf of Mexico shapes the life history of vestimentiferan tubeworms, and the sulfide and oxygen concentrations at those seeps determine seep and non-seep species’ distributions across the deep seafloor.<br>Temple University--Theses
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Cornelius, Nils. "Biodiversity and ecology of benthic foraminiferans from the Antarctic deep sea." Thesis, University of Southampton, 2005. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.416476.

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Books on the topic "Deep sea ecology"

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Hyde, Natalie. Deep sea extremes. Crabtree Pub. Co., 2008.

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Lindop, Laurie. Venturing the deep sea. Twenty-First Century Books, 2006.

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Koslow, J. Anthony. The silent deep: The discovery, ecology and conservation of the deep sea. UNSW Press, 2007.

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Consalvey, Mireille, Malcolm R. Clark, and A. A. Rowden. Biological sampling in the deep sea. Wiley-Blackwell, 2016.

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Barnard, J. Laurens. Lysianassoid Amphipoda (Crustacea) from deep-sea thermal vents. Smithsonian Institution Press, 1990.

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Sokolova, M. N. Feeding and trophic structure of the deep-sea macrobenthos. Smithsonian Institution Press, 2000.

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Koslow, Julian Anthony. The silent deep: The discovery, ecology, and conservation of the deep sea. University of Chicago Press, 2007.

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Shinkai, 2000 (Ship). Sensui chōsasen Shinkai, 2000: 500-kai senkō kiroku : 2000 mētoru no shinkai o hiraku. Kaiyō Kagaku Gijutsu Sentā, 1991.

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Etnoyer, Peter J. Deep Coral and Associated Species Taxonomy and Ecology (DeepCAST) II Expedition report. U.S. Dept. of Commerce, National Oceanic and Atmospheric Administration, National Ocean Service, 2011.

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A, Ott Jörg, Stachowitsch Michael, and Uiblein Franz, eds. Deep-sea and extreme shallow-water habitats: Affinities and adaptations. Österreichische Akademie der Wissenschaften, 1996.

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Book chapters on the topic "Deep sea ecology"

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Prieur, Daniel, Mary Voytek, Christian Jeanthon, and Anna-Louise Reysenbach. "Deep-Sea Thermophilic Prokaryotes." In Thermophiles Biodiversity, Ecology, and Evolution. Springer US, 2001. http://dx.doi.org/10.1007/978-1-4615-1197-7_2.

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Fujiwara, Yoshihiro, and Koetsu Kon. "Marine Ecology: Continental Shelf to Deep Sea." In Japanese Marine Life. Springer Singapore, 2020. http://dx.doi.org/10.1007/978-981-15-1326-8_21.

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Hawkins, S. J., H. B. S. M. Corte-Real, F. G. Pannacciulli, L. C. Weber, and J. D. D. Bisbop. "Thoughts on the ecology and evolution of the intertidal biota of the Azores and other Atlantic islands." In Island, Ocean and Deep-Sea Biology. Springer Netherlands, 2000. http://dx.doi.org/10.1007/978-94-017-1982-7_1.

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Carney, Robert S. "Examining Relationships Between Organic Carbon Flux and Deep-Sea Deposit Feeding." In Ecology of Marine Deposit Feeders. Springer New York, 1989. http://dx.doi.org/10.1007/978-1-4684-7671-2_2.

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Carney, Robert S. "Examining Relationships Between Organic Carbon Flux and Deep-Sea Deposit Feeding." In Ecology of Marine Deposit Feeders. Springer-Verlag, 2013. http://dx.doi.org/10.1029/ln031p0024.

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Thistle, David. "Harpacticoid copepods are successful in the soft-bottom deep sea." In Copepoda: Developments in Ecology, Biology and Systematics. Springer Netherlands, 2001. http://dx.doi.org/10.1007/0-306-47537-5_20.

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Welch, David B. Mark, and Susan M. Huse. "Microbial Diversity in the Deep Sea and the Underexplored “Rare Biosphere”." In Handbook of Molecular Microbial Ecology II. John Wiley & Sons, Inc., 2011. http://dx.doi.org/10.1002/9781118010549.ch24.

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Montroso, Alan S. "Ocean is the New East." In Sea Monsters. punctum books, 2017. https://doi.org/10.21983/p3.0182.1.03.

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On a recent visit to the Smithsonian’s National Museum of Natural History, I lingered a little while longer than usual in my favorite exhibit: the Sant Ocean Hall (see oppo-site page). Wandering with no telos in mind, I let myself bask before bioluminescent beings, tremble in awe at the improbability of the extremophiles, and gaze up like a supplicant at the model of Phoenix, a North Atlantic right whale. Deeply affected by these strange strangers,1 I stretched my imagination towards the inconceivable and wondered at the sheer breadth of possibilities for ways of living in the still-occult thalassic regions of Earth’s oceans. I found solace in the evidence that so many vast and heterogeneous lives can flourish without the intrusive light of the sun or human reason, and that such animacy is possible in the darkness, which is, according to Stacy Alaimo, a “world where the Copernican revolution is irrelevant.”2 I then with some discomfort imagined myself embodying an oceanic form, imagined breathing without oxygen, thriving at thermal vents, and manifesting light with my own body. I imagined myself as an aqueous and somewhat amorphous body squeezed and strangled by the just bearable pressures of the deep sea. I attempted a posthumanist thought project similar to what Alaimo describes in “Violet-Black,” her contribution to Prismatic Ecology, in which she insists that “thinking with and through the elec-tronic jellyfish, seeing through the prosthetic eye, playing open-ended, improvisa-tional language games with deep-sea creatures, being transformed by astonishment and desire enact a posthumanist practice.”
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Baker, Maria C., Eva Z. Ramirez-Llodra, Paul A. Tyler, et al. "Biogeography, Ecology, and Vulnerability of Chemosynthetic Ecosystems in the Deep Sea." In Life in the World's Oceans. Wiley-Blackwell, 2010. http://dx.doi.org/10.1002/9781444325508.ch9.

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Ward, Peter, and Rachael S. Shreeve. "The deep-sea copepod fauna of the Southern Ocean: patterns and processes." In Copepoda: Developments in Ecology, Biology and Systematics. Springer Netherlands, 2001. http://dx.doi.org/10.1007/0-306-47537-5_4.

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Conference papers on the topic "Deep sea ecology"

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Перерайс, Р., and R. Pererays. "SEA-PORT CONSTRUCTION IMPACT ON LIMAN NATURE ALONG THE BLACK SEA COASTAL ENVIRONMENT." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3b99793c8.27322405.

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Construction of sea-ports in limanic aquathory along the Northern Black Sea coast have prefer impact on the coastal environment. Especially deep impact have liman bottom artificial deepening, liman slopes artificial reconstruction, navigate canals, jetties of different sizes, ground dumps etc. Typical examples are Odessa, Ill'ichevsk, Yuzhniy commercial sea-ports in northern sector of the Black Sea. On shores nearest Port Yuzhniy jetties was firstly employed new construction against sea wave erosion. This new artificial shore terrace, that consist of natural matherials, expressed as shore protection, purification of sea water, needless ground depot, new shore territory and squire for recreants simultaneous.
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Есина, Л., L. Esina, А. Хворощ, et al. "THE ROLE OF THE SUBMARINE LANDSLIDE PROCESSES IN EVOLUTION OF THE BLACK SEA CONTINENTAL SLOPE AND SHELF. THE INFLUENCE OF LANDSLIDES ON MODERN COASTAL PROCESSES." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3a0b6c337.05323429.

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Detailed studies of landslide formation on the continental slope of Near Caucasus part of Black Sea, we have made in the area between the Pshada– Olginka settlements allowed to explore the distribution of landslide formations on the continental slope and to establish their influence on the retreat of the shelf edge. The intensive destruction of shelf edge leads to a reduction in its width, the intense movement of sediments from the shelf and transporting them to the continental slope and deep-sea part in large quantities. The evolution and distribution of landslides are influenced by the geological structure of the navigation area, the width of the shelf, the rate of shoreline destruction and sediment transport from the shelf to the continental slope, underwater topography and slope declination, tectonic and seismic factors. Landslide processes on the coast and continental slope affect the modern coast changes, the bottom topography, the formation of Black Sea deep basins and the expansion of Black Sea. Coastal landslides pose a threat to coastal communities and national economic objects located in areas of high abrasion scarps of terraces, as well as for engineering structures on the continental shelf, continental slope and the seabed.
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Гущин, О., O. Guschin, Ж. Спонт, and Zh Spont. "TO A QUESTION ABOUT THERMAL CONVECTION IN THE COASTAL ZONE OF THE CURONIAN LAGOON." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce3964a36b5.65544812.

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In the given work the circulation caused in the various speed of warming up (cooling) of shallow and deep-water zones of pool (the phenomenon of the thermal bar) is simulated. The thermal bar is formed in the spring at heating a coastal part of a reservoir above +4 °C and in the autumn during cooling below\ +4 °C. Conditions of the thermal bar occurrence and dependence of circulation on specificity of warming up above underwater slopes with different biases are shown. Influence of the thermal bar on ecology system of large lagoons as it divides two zones with different characteristics of water that defines spatial distinctions of plankton populations is considered. It is supposed to analyse in the further influence of parameters on arising circulation and to compare results to experimental data.
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Горячкин, Ю., and Yu Goryachkin. "VARIABILITY OF SEA LEVEL AND DYNAMICS THE ACCUMULATIVE COASTS OF WESTERN CRIMEA." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce394b37220.57460895.

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Influence of the sea level changes on the dynamics of accumulative coasts (in the region of the western Crimea) is considered. The data of observations shows that the greatest change of the beaches under the influence of the level changes by 1 cm can be 1, 3 m. However, the period for which it is determined (1989–2001) was characterized, firstly, by amplification of storm activity, and secondly, by substantial growth of deficiency in deposits. It has been caused by the new deep-water mooring in Eupatoria trading port, which has changed the local migration of deposits. The regular deepening of the waterway has resulted in change of their balance, adaptation of the coast to the changed conditions and, consequently, to acceleration of the coastal line abrasion. The weakest change of beaches under the influence of changes of the level by 1 cm, which is determined for the period 2006–2010, is 0,2–0,3 m. This period was characterized by relatively little changeability of storm activity and relative stabilization of anthropogenic influence, thus such figure seems to be more trustworthy.
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Aguzzi, J., C. Costa, J. B. Company, et al. "The new synthesis of cabled observatory science: Technology meets deep-sea ecology." In 2013 IEEE International Underwater Technology Symposium (UT 2013). IEEE, 2013. http://dx.doi.org/10.1109/ut.2013.6519817.

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Voronin, V. P., D. V. Artemenkov, A. M. Orlov, and S. A. Murzina. "DEEP-SEA FISH OF THE STOMIIDAE FAMILY OF THE IRMINGER SEA: ECOLOGICAL AND BIOCHEMICAL ADAPTATION WITH THE PARTICIPATION OF LIPID TO DEPTH." In NOVEL TECHNOLOGIES IN MEDICINE, BIOLOGY, PHARMACOLOGY AND ECOLOGY. LLC Institute Information Technologies, 2023. http://dx.doi.org/10.47501/978-5-6044060-3-8.142-147.

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Lipid and fatty acid profiling of some representatives of mesopelagic fish species of the Stomiidae family, inhabiting the depth gradient of the Irminger Sea (North Atlantic) and be-ing the main predators of the "twilight" zone, was carried out. For the first time, changes in the qualitative and quantitative composition of lipids, phospholipids and fatty acids in mus-cle tissue have been established, which determine the specifics of the adaptive response strat-egy when living at depth.
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Дзагания, Е., and E. Dzaganiya. "FEATURES OF DETERMINATION OF SEA WAVE PARAMETERS FOR CONSTRUCTION OF HYDRAULIC ENGINEERING CONSTRUCTIONS TO FROM REVER TUAPSE TO RIVER PSOU." In Sea Coasts – Evolution ecology, economy. Academus Publishing, 2018. http://dx.doi.org/10.31519/conferencearticle_5b5ce39bdaaa38.41181927.

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East coast is the most storm part of the Black Sea because extent of the water area of the Black Sea more than 800 km. In a year there are about 17 days strong storm. Almost rectilinear outlines of the coast on a site from the river Tuapse to river Psou testify to destructive force of storm at low durability of the rocks composing the coast. The wave mode in the high sea can be determined by standard fields of a wind which build with use of weather maps. For a basis of typification take the direction and gradation of speed of a wind for that part of the water area within which it is required to define elements of waves. The main lack of a method is a short row – 10 years therefore the forecast for 25, 50 and 100 years on this row is estimated. Besides, for the district of Sochi the considerable share of excitements of a ripple (50–75 %) which are formed in different areas of the sea is characteristic. Therefore for this region any settlement method for wind excitement in the high sea won't reflect the actual mode of excitement and parameters of waves at the coast. Therefore in this case it is necessary to use all available actual data on excitement at probably bigger depth of supervision and all data on impact of the maximum storm on the coast in similar to the area of research conditions. The most qualitative for the considered coast are materials of supervision in Pitsunda. For application of these data for other sites of the coast taking into account a refraction recalculation of these supervision from shallow water is made for excitement of the deep sea. These data can be used for calculation of elements of waves on the Sochi coast. For the accounting of features of a wave mode at construction of such responsible and expensive constructions as ports, creation of new wave posts for long-term supervision is necessary. Especially it is actual in the Adler district of the city of Sochi where parameters of extreme storm are estimated generally on the put damage, instead of on series of observations over excitement. Tool supervision over excitement were carried out on northern to a pier of the Sochi port after the completion of its construction and allowed to define instrumentalno&#x0D; wave loads of a hydraulic engineering construction during a storm. Again created constructions of Mzymta seaport on the coast of the Imeretinsky bay and created during reconstruction of the Sochi seaport a new northern pier could form base for the organization of tool supervision over excitement on rather big depths near 15–20 M that it is quite enough for supervision of the maximum waves to their collapse.
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8

Murzina, S. A., V. P. Voronin, D. V. Artemenkov, and A. M. Orlov. "ECOLOGICAL AND BIOCHEMICAL ADAPTATIONS OF LIPIDS AND FATTY ACIDS CERTAIN FISH SPECIES FROM THE IRMINGER SEA TO DEEPWATER HABBIT." In NOVEL TECHNOLOGIES IN MEDICINE, BIOLOGY, PHARMACOLOGY AND ECOLOGY. Institute of information technology, 2022. http://dx.doi.org/10.47501/978-5-6044060-2-1.196-203.

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Lipid profiling and identification of lipid status were carried out in certain species of meso-pelagic fish species - Lampanyctus macdonaldi and Bathylagus euryops of the Irminger Sea, which are manifested as integral components of the aquatic ecosystem and prevail in habitat, life cycle, specific development, intraspecific degree and the presence of specialization. For the first time, changes in the lipid profiles and the contents, observed by the specific adaptive sensitivity of fish to a deep-sea lifestyle, have been revealed.
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Reports on the topic "Deep sea ecology"

1

Kropp, Roy K. Review of Deep-Sea Ecology and Monitoring as They Relate to Deep-Sea Oil and Gas Operations. Office of Scientific and Technical Information (OSTI), 2004. http://dx.doi.org/10.2172/15010486.

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2

Stone, Robert P., Stephen D. Cairns, Dennis M. Opresko, Gary C. Williams, and Michele M. Masuda. A guide to the corals of Alaska. US Department of Commerce, NOAA, NMFS Scientific Publications Office, 2024. http://dx.doi.org/10.7755/pp.23.

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The Magnuson-Stevens Fishery Conservation and Management Reauthorization Act of 2006 mandat¬ed the research and management of the nation’s deep-sea coral resources through establishment of the National Oceanic and Atmospheric Administra¬tion’s Deep Sea Coral Research and Technology Program. The challenge for Alaska was daunting, where expansive, world-class fisheries often coincided with extraordinarily rich coral habitats for a high-latitude region. The first chal¬lenge was to inventory known locations of deep-sea corals. Many coral records and some museum collections existed from Alaska, but the taxonomy of cor¬als was little studied and field iden¬tification of corals was problematic. Formal bycatch programs and research activities in recent decades provided many more specimens for taxonomic study, but guides to species were largely incomplete, inaccurate, and outdated given the fast pace of species discovery in Alaska. We provide a comprehen¬sive, up-to-date guide, detailing 161 coral taxa identified from museum collections, primary literature, and video records. Each profile includes a description, images for each taxon, taxonomic history, biology, ecology, geographical distribution, and habitat, including depth distribution. Corals are found in the six regions of Alaska but the coral fauna of the Aleutian Islands is by far the most species rich. The state of taxonomy for some coral groups is ex¬cellent, while others require additional collections and more taxonomic work. Construction of this guide resulted in descriptions of several antipatharian species, published separately from this guide (Alternatipathes mirabilis, Bathypathes alaskensis, B. ptiloides, B. tiburonae, and Parantipathes pluma) and the scleractinian Flabellum (Flabel¬lum) oclairi Cairns, sp. nov. described herein. The guide provides informa¬tion for targeting new collections and identifying areas of high abundance and indicator species of vulnerable marine ecosystems. Stakeholders can now more adequately assess Alaska’s coral resources and risks from natural and anthropogenic stressors.
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