Environmental Engineering Reference
In-Depth Information
[10]
Friedl G., Dinkel C. and Wehrli B. Benthic fluxes of nutrients in the northwestern Black
Sea. Mar Chem 1998; 62:77-88.
[11]
Friedrich J., Dinkel C., Friedl G., Pimenov N., Wijsman J., Gomoiu M. T., Cociasu A.,
Popa L. and Wehrli B. Benthic nutrient cycling and diagenetic pathways in the north-
western Black Sea. Estuar Coast Shelf S 2002; 54:369-83.
[12]
Gal'chenko V.F., Abranochkina F.N., Bezrukova L.V., Sokolova E.N. and Ivanov M.V.
Species composition of aerobic methanotrophic microflora in the Black Sea. Mikrobi-
ologiya 1988; 57:305-11.
[13]
Gorur N., Cagatay M.N., Emre O., Alpar B., Sakinc M., Islamoglu Y., Algan O., Erkal
T., Kecer M., Akkok R. and Karlik G. Is the abrupt drowning of the Black Sea shelf at
7150 yr BP a myth? Mar Geol 2001; 176:65-73.
[14]
Hinrichs K.-U., Hayes J.M., Sylva S.P., Brewer P.G. and DeLong E.F. Methane-consuming
archaebacteria in marine sediments. Nature 1999; 398:802-05.
[15]
IPPC. Climate Change 2001: The Scientific Basis. Contribution of the Intergovernmental
Panel on Climate Change, Greenhouse Gases (pp. 241-287).
[16]
Ivanov M.K., Limonov A.F. and Woodside J.M. “Extensive deep fluid flux through the
sea floor on the Crimean continental margin (Black Sea).” In
Gas Hydrates: Relevance to
World Margin Stability and Climate Change
, Henriet J.-P. and Mienert J. eds., Geological
Society London, 1998.
[17]
Ivanov M.V., Pimenov N.V., Rusanov, II and Lein A.Y. Microbial processes of the methane
cycle at the north-western shelf of the Black Sea. Estuar Coast Shelf S 2002; 54:589-99.
[18]
Ivanov M.V., Polikarpov G.G., Lein A.Y., Galchenko V.F., Egorov V.N., Gulin M.B.,
Rusanov I.I., Miller Y.M. and Kupzov V.I. Biogeochemistry of carbon cycle on the Black
Sea region of CH
4
gas seeps. Dokladi Academy Nauk USSR, 1989; 320:1235-40.
[19]
Ivanov M.V., Rusanov I.I., Lein A.Y., Pimenov N.V., Yusupov S.K. and Galchenko V.F.
Biogeochemistry of methane cycle in the anaerobic zone of the Black Sea,
Past and
present water column anoxia. NATO Advanced Research Workshop
Crimea, Ukraine:
NATO, 2003.
[20]
Jones G.A. Constraining the initiation and evolution of anoxia in the Black Sea by AMS
radiocarbon dating. Radiocarbon 1991; 33:211-12.
[21]
Jørgensen B.B., Weber A. and Zopfi J. Sulfate reduction and anaerobic methane oxidation
in Black Sea. Deep-Sea Res Pt I 2001; 48:2097-120.
[22]
Kipfer R., Aeschbach-Hertig W., Peeters F. and Stute M. “Noble gases in lakes and ground
waters.” In
Noble gases in geochemistry and cosmochemistry.
Porcelli D., Ballentine C.
and Wieler R. eds., Mineralogical Society of America, Geochemical Society, 2002.
[23]
Koga Y., Morii H., Akagawa-Matsushita M. and Ohga M. Correlation of polar lipid com-
position with 16S rRNA phylogeny in methanogens. Further analysis of lipid component
parts. Biosci Biotech Biochem 1998; 62(2):230-36.
[24]
Konovalov S.K., Ivanov L.I. and Samodurov A.S. Fluxes and budget of sulphide and
ammonia in the Black Sea anoxic layer. J Marine Syst 2001; 31:203-16.
[25]
Kvenvolden K.A. Methane hydrates and global climate. Global Biogeochem Cy 1988;
2:221-29.
[26]
Kvenvolden K.A., Ginsburg G. and Soloviev V. Worldwide distribution of subaquatic gas
hydrates. Geo-Mar Lett 1993; 13:32-40.
[27]
Lammers S. and Suess E. An improved head-space analysis method for methane in
seawater. Mar Chem 1994; 47:115-25.
