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ROYAL SOCIETY (1963). International Indian Ocean Expedition RRS “Discovery”, Cruise 1. SouthEast Arabian Upwelling Region. Cruise Report, Royal Society, London, 24 p.ROYAL SOCIETY (1965). International Indian Ocean Expedition RRS “Discovery”, Cruise 3Report. Oceanographic work in the western Indian Ocean 1964. Royal Society, London, 55P.ROCHFORD, D.J. (1966). Source regions of oxygen maxima in intermediate depths of the ArabianSea. Aust. J. Mar. Freshw. Res., 17, 1-30.RYTHER, J.H. and YENTSCH, C.S. (1957). The estimation of phytoplankton production in theocean from chlorophyll and light data. Limnol. Oceanogr., 2,281-286.RYTHER, J.H. and MENZEL, D.W. (1965). On production, composition and distribution of organicmatter in the western Arabian Sea. Deep-sea Res., 12, 199-209.RYTHER, J.H. et a1..(1966). Primary production in relation to the chemistry and hydrography of thewestern Indian Ocean. Limnol. Oceanogr., 11,371-380.SANDERS, M.J. (1981). Revised stock assessment for the cuttlefish Sepia pharaonis taken off thecoast of FDR of Yemen. FAO, Rome. Fish. Tech. Pap. 77/008,43 p.SANDERS, M.J. and BOUHLEL (1982). Preliminary estimates of some stock assemssmentparameters for the mesopelagic speices Benthosoma pterotum inhabiting the western andnorthern Arabian Sea. FAO, Rome. Fish. Tech. Pap. RAB 77/008,23 p.SANDERS, M.J. and BOUHLEL, M. (1984). Stock assessment for the Indian oil sardine Sardinellalongiceps inhabiting the eastern waters of the People’s Democratic Republic of Yemen. FAO,Rome. Fish. Tech. Pap. RAB/81/002/18,62 p.SAVICH, M.S. (1968). Phytoplankton of the Gulf of Aden and the Arabian Sea during winter (1)and summer monsoon (2). Trudy VNIRO 64 - AZCHERNIRO 28,243 p.SAVICH, M.S. (1969). Seasonal dynamics of phytoplankton of the Gulf of Aden in 1963.Okeanol., 9, 1056-1062.SAVICH, M.S. (1979). Phytoplankton of the Gulf of Aden. Ph.D. Thesis. Kerch. 188 p.SCHOTT, F. (1983). Monsoon response of the Somali current and associated upwelling. Prog.Oceanogr., 12, 357-381.SERIY, V.V. (1968). Pecularities of seasonal variations in hydrological conditions in the Gulf ofAden. Trudy VNIRO 64 - AZCHERNIRO 28,117-129.SERIY, V.V. and KHIMITSA, V.A. (1963). The hydrology and chemistry of the Gulf of Aden andthe Arabian Sea. Okeanol., 6,994- 1003.SEN GUPTA R. and NAQVI, S.W.A. (1984). Chemical Oceanography of the Indian Ocean, north ofthe equator. Deep-sea Res., 31,671-706.SEWELL, R.B.S. and FAGE, L. (1948). Minimum oxygen layer in the ocean. Nature, 162,949-951.SHINDO, S. (1972). General review of the trawl fishery and the demersal fish stocks of the SouthChina Sea. FAO, Rome. Fish. Tech. Pap. 120,49 p.SMITH, R.L. (1968). Upwelling. Oceanogr. Mar. Biol. Ann. Rev., 6, 11-46.275
SMITH, S.L. (1982). The northwestern Indian Ocean during the monsoons of 1979: distribution,abundance, and feeding of zooplankton. Deep-sea Res., 29, 1331- 1353.SMITH, S.L. (1984). Biological indication of active upwelling in the northwestern Indian Ocean in1964 and 1979, and a comparison with Peru and NW Africa. Deep-sea Res., 31,951-968.STROMME, T. (1984). Second fisheries resource survey in F.D.R. Yemen. Cruise Report R/V “Dr.FridtjofNansen”, Institute of Marine Research, Bergen, 13 p.SUKHANOVA, I.N. (1969). Some data on the phytoplankton of the Red Sea and the western Gulfof Aden. Okeanol., 9,243-247.SWALLOW, J.C. (1984). Some aspects of the physical oceanography of the Indian Ocean.Deep-sea Res., 3 1 , 639-650.SWALLOW, J.C. and BRUCE, J.G. (1966). Current measurements off the Somali Coast during thesouthwest monsoon of 1964. Deep-sea Res., 13, 861-888.SZEKIELDA, K.H. (1970). The development of upwelling along the Somali Coast as detected withthe Nimbus 2 and Nimbus 3 satellites. Goddard Space Flight Center, GreenbeltX-651-70-419, 52 p. (Cit. Dietrich, 1973).THIEL, H. (1978). Benthos in upwelling regions. In: R. Boje and M. Tomczak (eds.), Upwellingecosystems, Springer-Verlag, Berlin, 124- 138.VENEMA, S.C. (1984). Fishery resources in the North Arabian Sea and adjacent waters. Deep-seaRes., 31, 1001-1018.VINOGRADOV, M.D. and VORONINA, N.M. (1961). On the influence of oxygen deficiency on thedistribution of plankton in the Arabian Sea. Okeanol., 1,670-678.VNXO & AZCHERNIRO (Moiseev, P.A. ed.) (1968). Soviet fisheries investigation in the IndianOcean and adjacent waters. Trudy VNIRO 64 - AZCHERNIRO 28, Moscow, 445 p.VOYTOV, V.I. and DEMENTYEVA, M.G. (1970). The relative transparency of the Indian Oceanwater. Okeanol., 10, 48-50.WARREN, B., STOMMEL, H. and SWALLOW, J.C. (1966). Water masses and patterns of flow inthe Somali Basin during the southwest monsoon of 1964. Deep-sea Res., 13,825-860.WHITLEDGE, T.E. (1978). Regeneration of nitrogen by zooplankton and fish in the NW Africa andPeru upwelling. In: R. Boje and M. Tomczak (eds.), Upwelling ecosystems,Springer-Verlag, Berlin, 90- 100.WOOSTER, W.S., SCHAEFER, M.K. and ROBINSON, M.K. (1967). Atlas of the Arabian Sea forfishery oceanography. Univ. Calif. IMR Ref. 67-12, 35 p., 140 pls.WYRTKI, K. (1971).Oceanographic Atlas of the International Indian Ocean Expedition. NationalScience Foundation, U.S. Govt. Printing Office, Washington, DC, 53 1 p.WYRTKI, K. (1973). Physical oceanography of the Indian Ocean. In: B. Zeitzschel (ed.), Thebiology of the Indian Ocean, Springer-Verlag, Berlin-Heidelberg-New York, 18-36.276
Page 1 and 2:
Intergovernmental Oceanographic Com
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of the IOC Marine Pollution Monitor
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PageMARGINAL SEASSTORM SURGES IN TH
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Marine PollutionAt present, marine
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THE INDIAN OCEAN --- AN ENVIRONMENT
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The subtropical anticyclonic gyre i
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GEOLOGICALBecause of its asymmetric
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RADIOACTIVE AND THERMAL WASTESIn co
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RESEARCH AND MONITORING ACTIVITIESM
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2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
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Localized problems, both short-term
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HOLEMAN, J.N. (1968). The sediment
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UNEP/UNIDO (1982a). Industrial sour
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0-5-24 -I I I I I I I I I 11--25- A
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I*in '0( U N '0- '0 '0 N , p d'0I I
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C'EO IIFigure 6. Observations of oi
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Table 2.Ranges of Dissolved heavy m
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d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
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Table 6. Population and related dat
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PROBLEMS IN THE PHYSICAL OCEANOGRAP
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B2: How does the Agulhas Current in
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0Q0mbWbvx(U49
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Figure 6 Average wind stress curl f
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THE DESTRUCTION OF THE TETHYS AND P
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part of the Seychelles-Mascarene bl
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Much of the old Tethys seafloor has
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when there was little or no movemen
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scouring of the sediments by cold b
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CANDE, S.C. and MUTTER, J.C. (1982)
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SHACKLETON, N.J. and KENNETT, J.P.
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0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
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CALCAREOUS FORAMINIFERANANNOFOSSIL
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GEOLOGICAL-GEOPHYSICAL MAPPING OF T
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The latest tectonic generalization
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LE PICHON, X. and HEIRTZLER, J.R. (
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AN EXAMINATION OF THE FACTORS THAT
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is the specific volume anomaly. Po
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circulation. At Nagappattinam, Madr
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Table 1.MarmagaoCochin1969-781958-7
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tFigure 2. An idealized coastal cur
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STATION : BOMBAY~ J , F I M .- , A
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STATION : COCHIN, J , F , M , A , M
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3007STATION : MADRASI J I F , M I A
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STATION : CALCUTTA, J l F , M , A ,
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RED TIDE§ IN THE INDO-WEST PACIFIC
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were observed as early as 1770 duri
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diarrhetic shellfish poisoning (DSP
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GACUTAN, R.Q., TABBU, M.Y., AUJERO,
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Table 1.Clinical symptoms of variou
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Table 3. Fish species implicated in
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FIGURE CAPTIONSFigure la. Trichodes
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(*14aEE15aHH15c120
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MINERAL RESOURCES OF THE INDIAN OCE
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tonnes of monazite. Similar deposit
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Madagascar and the Red Sea. Within
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South Australian Basin: (Figs. 10-1
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Offshore placers are likely to occu
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MILLIMAN, J.D. (1974). Marine Carbo
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Thailand Tin 5560 (1980) NA 4.2 (19
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Table 2. The range (in percent) of
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Table 4. Chemical composition of po
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141FIGURE - 1
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~IT 73qw p' le' IS IFigure 4. Map s
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@A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
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Figure 10. Map showng the abundance
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Figure 14. Map showing the distribu
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IFigure 17. Marine mineral explorat
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central are corals to the integrity
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Very little information is availabl
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leaving little trace of their exist
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REFERENCESAGASSIZ, A. (1903). The c
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PILLAI, C.S.G. (1969b). Studies on
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Table 1.Extent of damage to coral r
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STATUS OF CRITICAL MARINE HABITATS
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OCCURRENCEThe distribution of reefs
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Mining of Reef RockMining of reef r
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-resource. Their significance deriv
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Coating of Aerial Roots by Fine Sed
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associated with the roots (e.g. GOE
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Temperature and SalinityThe effects
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significant numbers in the Red Sea,
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mersas are known to serve as nurser
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BURCHARD, J.E. (1979). Coral fauna
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HIRTH, H.F., KLIKOFF, L.G. and HARP
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MacNAE, W. (1974). Mangrove forests
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RINKEVITCH, B. and LOYA, Y. (1977).
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WALKER, D.I. and ORMOND, R.F.G. (19
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DAMMING AND DIVERSION OF RIVERSIn d
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FUTURE STUDIESWhat can marine scien
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!0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
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0 0-0 00 O0O 0% LD d- m cu 0 0202
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STORM SURGES IN THE BAY OF BENGAL*T
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low pressure centres over the Bay i
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ACKNOWLEDGEMENTSThe writers wish to
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Table 1.Latitude and longitude of p
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214
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0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
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0In218
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221
Page 216 and 217: Table 3. Nomenclature used by India
Page 218 and 219: ANDHRAB A Y OFB E N G A L ,.16'LO 4
Page 220 and 221: INDIABAY OF-Point CalirnereLanka L-
Page 222 and 223: pressure in the South Pacific and l
Page 224 and 225: SWALLOW, J.C. (1983). Arabian Sea c
Page 226 and 227: 234
Page 228 and 229: 236
Page 230 and 231: scale wind phenomenon that occurs w
Page 232 and 233: Several two-dimensional models of t
Page 234 and 235: HARTMANN, M., LANGE, H., SEIBOLD, E
Page 236 and 237: Y-Model Domaint=6hrs.b-250 0 59 Xw-
Page 238 and 239: UELEVATIONS (m) ai 18 HOURS L2:-+EL
Page 240 and 241: HARMONIC CONSTITUENT K,Figure 8. Ob
Page 242 and 243: Age of Semi-Diurnal Tide (hrs)28".+
Page 244 and 245: ! 5"BOTTOMFigure 13. Predicted mode
Page 246 and 247: OCEANOGRAPHIC CONDITIONS PELAGIC PR
Page 248 and 249: Low oxygen content in subsurface wa
Page 250 and 251: R/V Dr. F. Nansen trawl of 41 m hea
Page 252 and 253: thermocline temperature decreases s
Page 254 and 255: Nitrate - NitrogenSimilarly to phos
Page 256 and 257: The maximum standing stocks in the
Page 258 and 259: By April/May the demersal stocks ha
Page 260 and 261: in 6 months when spawning occurs. T
Page 262 and 263: REFERENCES3BANSE, K. (1968). Hydrog
Page 264 and 265: GILSON, H.C., (1937). The nitrogen
Page 268 and 269: APPENDIX:REGIONAL COOPERATIVE INVES
Page 270 and 271: 20 015 20 25FEBOC015 20 25 30 35M A
Page 272 and 273: W0-8w0-Inww[r3a+eW281
Page 274 and 275: B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
Page 276 and 277: a, A
Page 278 and 279: ...... :'I. .. ,... .. 8.*.. ... ._
Page 280 and 281: ASTAT.Si -Si (OH14 in p M - d ~ n -
Page 282 and 283: YU0IwYY->02(33-1 II 1amLyY>02(33amL
Page 284 and 285: I I I I I10 Ic L0U0mI(dw -rlo u0w m
Page 286 and 287: III I I I0. 1....w'3...-0U-J..,....
Page 288 and 289: 297
Page 290 and 291: clearly is too low. Because of low
Page 292 and 293: KARBE, L., THIEL, H., WEIKERT, H. a
Page 294 and 295: 50010001 scoOxygen (rnl/l)0I1I2I3I4
Page 296 and 297: c1 oc50C10001500_j_///.///II:I? 0:3
Page 298 and 299: THE RED SEAPHYSIOGRAPHYThe Red Sea
Page 300 and 301: intensity of magnetization which co
Page 302 and 303: 1969; SEARLE and ROSS, 1975). This
Page 304 and 305: y normal faulting. This is most int
Page 306 and 307: South of 19"N, the McKENZIE pole no
Page 308 and 309: BAUMANN, A., RICHTER, H. and SCHOEL
Page 310 and 311: EYAL, M., EYAL, Y., BARTOV, Y. and
Page 312 and 313: LEWIS, B.T.R. (1983). The process o
Page 314 and 315: TARLING, D.H. and MITCHELL, J.G. (1
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mC- 1000- 2000- 3000E0Figure 2.Sche
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-20b-0,20wFigure 4. Seismicity and
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kmaFigure 6. Summary of seismic ref
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kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
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5 b'o w-Y EO'i Ii04!I 0I0I334
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II,'{34/,'0SOMALIAND: N. DANAKILFig
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spreadingvulcanismmblock faultingII
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SUPERFICIAL SEDIMENTS OF NORTHERN R
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normally sorted, with median diamet
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EL-SAYED (1983) used the trace meta
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BEHAIRY, AKA. (1983). Marine transg
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SHUKRI, N.M. (1953). Bottom deposit
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Table 2 Heavy metal concentrations
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EGYPTEl-Morgan 1Bargan IBargan 2Yub
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Figure 4. Distribution of minerals
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ARAGONITEHIGH HG-CALCITEFigure 6. T
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MARINE LIVING RESOURCES OF THE RED
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This elevated productivity may resu
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REVELLE (1981) mentioned that the p
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FISHELSON, L. (1964). Observation o
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