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mC- 1000- 2000- 3000E0Figure 2.Schematic transverse .topographic profilesacross the Red Sea, showing the main trough,the axial trough, and the transition fromshelf to coastal plain. After ALLEN (1970).Location of profiles shown in Fig. 1.326
QA.7 o 2.7*oPlia‘PlrihPlia 7c tMiocrnoMioctnrb20 mynl l0O0 1Synthetics-215 235I 1a- 59 Mia Mio. 59 68Ucrel. Pal.Pal. CretCanomaly No.1.Ocmlyr.0.75 cmtyclb 100 !k $6 si, 100 1%.....1’5 io b o 10 210m.y.dFigure 3. a) Composite magnetic profile of the central Red Sea reducedto the pole and its interpretation in terms of a two-stagespreading model,b) Alternative model for the interpretation of the profile ina) YC) Magnetic profile in the western Gulf of Aden reduced to thepole and its interpretation in terms of two-stage spreadingmodel similar to a),d) Alternative model for the interpretation of the profile inc) (see text). Magnetic profiles not reduced to the pole.After GIRDLER (1978),-NOY (19781, GIRDLER -- et al. (1980) andCOCHRAN (1981).3 27
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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
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Table 3. Nomenclature used by India
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ANDHRAB A Y OFB E N G A L ,.16'LO 4
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INDIABAY OF-Point CalirnereLanka L-
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pressure in the South Pacific and l
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SWALLOW, J.C. (1983). Arabian Sea c
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234
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236
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scale wind phenomenon that occurs w
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Several two-dimensional models of t
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HARTMANN, M., LANGE, H., SEIBOLD, E
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Y-Model Domaint=6hrs.b-250 0 59 Xw-
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UELEVATIONS (m) ai 18 HOURS L2:-+EL
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HARMONIC CONSTITUENT K,Figure 8. Ob
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Age of Semi-Diurnal Tide (hrs)28".+
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! 5"BOTTOMFigure 13. Predicted mode
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OCEANOGRAPHIC CONDITIONS PELAGIC PR
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Low oxygen content in subsurface wa
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R/V Dr. F. Nansen trawl of 41 m hea
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thermocline temperature decreases s
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Nitrate - NitrogenSimilarly to phos
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The maximum standing stocks in the
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By April/May the demersal stocks ha
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in 6 months when spawning occurs. T
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REFERENCES3BANSE, K. (1968). Hydrog
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GILSON, H.C., (1937). The nitrogen
Page 266 and 267: ROYAL SOCIETY (1963). International
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
Page 318 and 319: -20b-0,20wFigure 4. Seismicity and
Page 320 and 321: kmaFigure 6. Summary of seismic ref
Page 322 and 323: kQ)Um 5U0c04 3N 4COQ)k3M*rlk332
Page 324 and 325: 5 b'o w-Y EO'i Ii04!I 0I0I334
Page 326 and 327: II,'{34/,'0SOMALIAND: N. DANAKILFig
Page 328 and 329: spreadingvulcanismmblock faultingII
Page 330 and 331: SUPERFICIAL SEDIMENTS OF NORTHERN R
Page 332 and 333: normally sorted, with median diamet
Page 334 and 335: EL-SAYED (1983) used the trace meta
Page 336 and 337: BEHAIRY, AKA. (1983). Marine transg
Page 338 and 339: SHUKRI, N.M. (1953). Bottom deposit
Page 340 and 341: Table 2 Heavy metal concentrations
Page 342 and 343: EGYPTEl-Morgan 1Bargan IBargan 2Yub
Page 344 and 345: Figure 4. Distribution of minerals
Page 346 and 347: ARAGONITEHIGH HG-CALCITEFigure 6. T
Page 348 and 349: MARINE LIVING RESOURCES OF THE RED
Page 350 and 351: This elevated productivity may resu
Page 352 and 353: REVELLE (1981) mentioned that the p
Page 354 and 355: FISHELSON, L. (1964). Observation o
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