参考文献:1.Bityukov, E.P., Rybasov, V.P., and Shaida, V.G., Annual variations in the intensity of bioluminescence field in the neritic zone of the Black Sea, Okeanologiya, 1967, Vol. 7, No. 6, pp. 1089–1099.<br>2.Borovikov, V.P., Populyarnoe vvedenie v programmu STATISTICA (Simplified Introduction to STATISTICA Software Package), Moscow: Komp’yuterPress, 1998.<br>3.Gitel’zon, I.I., Levin, L.A., Utyushev, R.N., et al., Biolyuminestsentsiya v okeane (Bioluminescence in the Ocean), St. Petersburg: Gidrometeoizdat, 1992.<br>4.Zuev, G.V. and Mel’nikova, E.B., Intraspecies heterogeneity of sprat Sprattus sprattus phalericus Risso (Pisces: Clupeidae) in the western Black Sea, Mor. Ekol. Zhurn., 2007, vol. VI, No. 4, pp. 31–41.<br>5.Ivanov, V.A. and Belokopytov, V.N., Okeanografiya Chernogo morya (Black Sea Oceanography), Sevastopol: EKOSI-Gidrofizika, 2011.<br>6.Il’in, Yu.P., Anticyclonic vortices at denting in the northwestern Black Sea: the formation of surface images and satellite IR-observations in spring and summer, in Issledovaniya shel’fovoi zony Azovo-Chernomorskogo basseina: Sb. nauchn. Tr. MGI NANU (Studying the Shelf Zone of Azov–Black Sea Basin: Coll. Sci. Papers MGI NANU), Sevastopol, 1995, pp. 22–31.<br>7.Mandel’, I.D., Klasternyi analiz (Cluster Analysis), Moscow: Finansy i statistika, 1988.<br>8.Mel’nikova, E.B. and Burmistrova, N.V., Application of cluster analysis for the structuring of communities of bioluminescent aquatic organisms, Uch. Zap. TNU, Ser. Biol., Chem., Simferopol, 2011, Vol. 24(63), No. 4, pp. 156–165.<br>9.Senicheva, M.I., Species diversity, seasonal and yearto-year variations of microalgae in plankton at Crimean shores, Mikrovodorosli Chernogo morya: problemy sokhraneniya bioraznoobraziya i biotekhnologicheskogo ispol’zovaniya (Black Sea Microalgae: Problems of Biodiversity Preservation and Biotechnological Utilization), Tokarev, Yu.N., Finenko, Z.Z., Shadri, N.V., Eds., Sevastopol: EKOSI-Gidrofizika, 2008, pp. 5–17.<br>10.Tokarev, Yu.N., Bityukov, E.P., Vasilenko, V.I., et al., Species diversity of planktonic bioluminescents in the Black Sea and the characteristics of the bioluminescence field they form in the neritic zone of Crimea, Sovremennoe sostoyanie bioraznoobraziya pribrezhnykh vod Kryma (chernomorskii sektor) (Current State of the Biodiversity in Crimean Coastal Waters: Black Sea Sector), Eremeev, V.N., Ed., Sevastopol: EKOSIGidrofizika, 2003, pp. 121–151.<br>11.Tokarev, Yu.N., Bityukov, E.P., Vasilenko, V.I., and Sokolov, B.G., Bioluminescence field as a characteristic index of planktonic community structure in the Black Sea, Ekol. Morya, 2000, No. 53, pp. 20–25.<br>12.Tokarev, Yu.N. and Mel’nikova, E.B., The effect of hydrophysical characteristics on the intensity of bioluminescence field in the Black Sea, Gidrobiol. Zh., 2012, Vol. 48, No. 2, pp. 97–104.<br>13.Tokarev, Yu.N. and Sokolov, B.G., Effect of physical and biological factors on the formation of small-scale structure of bioluminescence and acoustic fields in the Black and Mediterranean Seas, Gidrobiol. Zh., 2001, Vol. 37, No. 2, pp. 3–13.<br>14.Cherepanov, O.A., Levin, L.A., and Utyushev, R.N., Relationship between bioluminescence and the biomass and abundance of luminescent and entire plankton: the Barents and Norwegian seas, Mor. Ekol. Zhurn., 2007, Vol. 6, No. 1, pp. 55–65.<br>15.Melnikova, E.B., Tokarev, Yu.N., and Burmistrova, N.V., Regularities of changes of the bioluminescence field in the Black Sea coastal waters, Hydrobiol. J., 2013, Vol. 49, No. 3, pp. 105–111.CrossRef <br>
作者单位:E. B. Mel’nikova (1) <br><br>1. Kovalevsky Institute of Biology of the Southern Seas, prosp. Nakhimova 2, Sevastopol, 299011, Russia <br>
刊物类别:Earth and Environmental Science
刊物主题:Earth sciences<br>Hydrogeology<br>Waste Water Technology, Water Pollution Control, Water Management and Aquatic Pollution<br>Russian Library of Science<br>
出版者:MAIK Nauka/Interperiodica distributed exclusively by Springer Science+Business Media LLC.
ISSN:1608-344X
文摘
The regional features of the vertical structure of bioluminescence field have been studied in summer along Crimean coast. Six regions, which differ in bioluminescence vertical distribution were identified. The position of the layer of the maximal intensity of bioluminescence field is determined for each region and its correlation with the hydrodynamic and hydrological characteristics of Crimean coastal waters is demonstrated.