Environmental Engineering Reference
In-Depth Information
[14]
Emeis K.-C., Br uchert V., Currie B., Endler R., Ferdelman T.G., Kiessling A., Leipe T.,
Noli-Peard K., Struck U. and Vogt T. Shallow gas in shelf sediments of the Namibian
coastal upwelling ecosystem. Cont Shelf Res 2004; 24:627-42.
[15]
Hamukuaya H., O'Toole M. and Woodhead P.M.J. Observations of severe hypoxia and
offshore displacements of Cape Hake over the Namibian Shelf in 1994. S Afr J Marine
Sci 1998; 19:41-57.
[16]
Hardman-Mountford N.J., Richardson A.J., Agenbag J.J., Hagen E., Nykjaer L., Shilling-
ton F.A. and Villacastin C. Ocean climate of the South East Atlantic observed from
satellite data and wind models. Prog Oceanogr 2003; 59:181-221.
[17]
Helly J.J. and Levin L.A. Global distribution of naturally occurring marine hypoxia on
continental margins. Deep-Sea Res 2004; 51:1159-68.
[18]
Jørgensen B.B. Bacteria and biogeochemistry, In
Marine Geochemistry
, H.D. Schulz and
M. Zabel, eds. Berlin: Springer Verlag, 2000.
[19]
Kiørboe T. and Jackson G.A. Marine snow, organic solute plumes, and optimal chemosen-
sory behaviour of bacteria. Limnol Oceanogr 2001; 46:1309-18.
[20]
Kiørboe T., Tiselius P., Mitchell-Innes B., Hansen J.L.S., Visser A.W. and Mari X. In-
tensive aggregate formation with low vertical flux during an upwelling-induced diatom
bloom. Limnol Oceanogr 1998; 43:104-16.
[21]
Kuypers M.M.M., Lavik G., Woebken D., Schmid M., Fuchs B.M., Amann R., Jørgensen
B.B. and Jetten M.S.M. Massive nitrogen loss from the Benguela upwelling system
through anaerobic ammonium oxidation. PNAS 2005; 102:6478-83.
[22]
Martens C.S., Albert D.B. and Alperin M.J. Biogeochemical processes controlling
methane in gassy coastal sediments-part 1. A model coupling organic matter flux to
gas production, oxidation, and transport. Cont Shelf Res 1998; 18:1741-70.
[23]
Martens C.S. and Klump J.V. Biogeochemical cycling in an organic-rich coastal marine
basin-I. Methane sediment-water exchange processes. Geochim Cosmochim Ac 1980;
44:471-90.
[24]
McHatton S.C., Barry J.P., Jannasch H.W. and Nelson D.C. High nitrate concentrations
in vacuolate, autotrophic marine
Beggiatoa
spp. Appl Environ Microb 1996; 62:954-58.
[25]
Mohrholz V., Schmidt M. and Lutjeharms J.R.E. The hydrography and dynamics of the
Angola-Benguela frontal zone and environment in 1999. S Afr J Sci 2001; 97:199-208.
[26]
Naqvi S.W.A., Jayakumar D.A., Narvekar P.V., Nalk H., Sarma V.V.S.S., D'Souza W.,
Joseph S. and George M.D. Increased marine production of N
2
O due to intensifying
anoxia on the Indian continental shelf. Nature 2000; 408:346-49.
[27]
Nelson D.C., Jørgensen B.B. and Revsbech N.P. Growth pattern and yield of a chemoau-
totrophic
Beggiatoa
spp. in oxygen-sulfide microgradients. Appl Environ Microb 1986;
52:225-33.
[28]
O'Hara S.C.M., Dando P.R., Schuster U., Bennis A., Boyle J.D., Chui F.T.W., Hatherell
T.V.J., Niven S.J. and Taylor L.J. Gas seep induced interstitial water circulation: observa-
tions and environmental applications. Cont Shelf Res 1995; 15:931-48.
[29]
Otte S., Kuenen J.G., Nielsen L.P., Paerl H.W., Zopfi J., Schulz H.N., Teske A., Strotmann
B., Gallardo V.A. and Jørgensen B.B. Nitrogen, carbon, and sulfur metabolism in natural
Thioploca
samples. Appl Environ Microb 1999; 65:3148-57.
[30]
Ploug H., Hietanen S. and Kuparinen J. Diffusion and advection within and around
sinking, porous diatom aggregates. Limnol Oceanogr 2002; 47:1129-36.
