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Table 2.Ranges of Dissolved heavy metal concentrations (pg 1-I) in the IndianOcean.Topping (1 969) 0.549.1 - 0.1-61.8 0.1-4.6 3.9-19.5 - - - -Chester & Stoner(1974)Surface 0.2- 1.2 0.024.14 0.5-3.1 0.07-0.37 0.3-3.0 - 0.3-2.6 - -OdYSen Gupta et al. 1.7-7.9 - 7.2-66.9 - 0.542.4 - 0-11.5 0-6.6 -(1978b)Singbal et al. - - - - - - - - 13-187(1978)Sanzgiri & Moraes 1.9-19.9 - 8.5-96 1.8-80 1.2-29.7 - 0-16.3 0-6.7 -(1979)Danielsson (1980) 0.08-0.48 0.014.16 0.15-10 - 0.613.8 0.02--0.180.18--O.95o--O.02 -Braganca & 22-37.2 - 6.2-131.5 1.84.8 2.620 - 0-12.2 0-7.9 -Sanzgiri (1980)Sanzgiri & 1-5 0.15-1.9 2-21.7 1.5-24.7 1.2-12.8 0.25-7.5 0-1 0-1 -Braganca (1 981)36
I80U)'9-00c!IIIIIIr42U)c?-9VIIIIIzd-8s-VIIIII-tdwrd\d8n42U)c?62cVIIIII$0Ev)e2vl2-VIIIIII-8ms-VIIIIII37
Page 1 and 2: Intergovernmental Oceanographic Com
Page 3 and 4: of the IOC Marine Pollution Monitor
Page 5: PageMARGINAL SEASSTORM SURGES IN TH
Page 9 and 10: Marine PollutionAt present, marine
Page 11 and 12: THE INDIAN OCEAN --- AN ENVIRONMENT
Page 13 and 14: The subtropical anticyclonic gyre i
Page 15 and 16: GEOLOGICALBecause of its asymmetric
Page 17 and 18: RADIOACTIVE AND THERMAL WASTESIn co
Page 19 and 20: RESEARCH AND MONITORING ACTIVITIESM
Page 21 and 22: 2-5, Mn 3-7, Zn 8-31, Fe 35-94, Pb
Page 23 and 24: Localized problems, both short-term
Page 25 and 26: HOLEMAN, J.N. (1968). The sediment
Page 28 and 29: UNEP/UNIDO (1982a). Industrial sour
Page 30 and 31: 0-5-24 -I I I I I I I I I 11--25- A
Page 32 and 33: I*in '0( U N '0- '0 '0 N , p d'0I I
Page 34: C'EO IIFigure 6. Observations of oi
Page 40 and 41: d.2 W2n2 n z0U.IzIO N m mENmIYEE*Ed
Page 42 and 43: Table 6. Population and related dat
Page 44 and 45: PROBLEMS IN THE PHYSICAL OCEANOGRAP
Page 46: B2: How does the Agulhas Current in
Page 50 and 51: 0Q0mbWbvx(U49
Page 52 and 53: Figure 6 Average wind stress curl f
Page 54 and 55: THE DESTRUCTION OF THE TETHYS AND P
Page 56 and 57: part of the Seychelles-Mascarene bl
Page 58 and 59: Much of the old Tethys seafloor has
Page 60 and 61: when there was little or no movemen
Page 62 and 63: scouring of the sediments by cold b
Page 64 and 65: CANDE, S.C. and MUTTER, J.C. (1982)
Page 66: SHACKLETON, N.J. and KENNETT, J.P.
Page 71 and 72: 0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
Page 75: CALCAREOUS FORAMINIFERANANNOFOSSIL
Page 79 and 80: GEOLOGICAL-GEOPHYSICAL MAPPING OF T
Page 81 and 82: The latest tectonic generalization
Page 83 and 84: LE PICHON, X. and HEIRTZLER, J.R. (
Page 85 and 86: AN EXAMINATION OF THE FACTORS THAT
Page 87 and 88:
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
Page 232 and 233:
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
Page 256 and 257:
The maximum standing stocks in the
Page 258 and 259:
By April/May the demersal stocks ha
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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 266 and 267:
ROYAL SOCIETY (1963). International
Page 268 and 269:
APPENDIX:REGIONAL COOPERATIVE INVES
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20 015 20 25FEBOC015 20 25 30 35M A
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W0-8w0-Inww[r3a+eW281
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B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
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a, A
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...... :'I. .. ,... .. 8.*.. ... ._
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ASTAT.Si -Si (OH14 in p M - d ~ n -
Page 282 and 283:
YU0IwYY->02(33-1 II 1amLyY>02(33amL
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I I I I I10 Ic L0U0mI(dw -rlo u0w m
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III I I I0. 1....w'3...-0U-J..,....
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297
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clearly is too low. Because of low
Page 292 and 293:
KARBE, L., THIEL, H., WEIKERT, H. a
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50010001 scoOxygen (rnl/l)0I1I2I3I4
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c1 oc50C10001500_j_///.///II:I? 0:3
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THE RED SEAPHYSIOGRAPHYThe Red Sea
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intensity of magnetization which co
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1969; SEARLE and ROSS, 1975). This
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y normal faulting. This is most int
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South of 19"N, the McKENZIE pole no
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BAUMANN, A., RICHTER, H. and SCHOEL
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EYAL, M., EYAL, Y., BARTOV, Y. and
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LEWIS, B.T.R. (1983). The process o
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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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