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DEUSER, W.G., ROSS, E.H. and MLODZINSKA, Z.J. (1978). Evidence for the rate ofdenitrification in the Arabian Sea. Deep-sea Res., 25,431-455.DHARGALKAR, V.K., KUREISHY, T.W. and BHANDARE, M.V. (1977). Deposition of tarballs (oil residue) on beaches along the west coast of India. Mahasagar-Bulletin of theNational Institute of Oceanography, 10, 103- 108.DIETRICH, G. (1963). General Oceanography. Interscience, New York, 588 pp, 13.DIETRICH, G. (1973). The unique situation in the environment of the Indian Ocean. In: B.Zeizschel, B. (ed.), The biology of the Indian Ocean. Springer-Verlag, Berlin, 1-6.DIETRICH, G. and ULRICH, J. (1968). Atlas Zur Ozeanographie. Bibliographisches Institut,Mannheim, 76 pp.DUING, W. (1970). The Monsoon regime of the currents in the Indian Ocean. International IndianOcean Expedition. Oceanogr., Monogr., East-West Centre Press, Honolulu, 1, 1-68.DUING, W. and SCHWILL, W.D. (1967). Ansbreitung und vermischung des salzreichen wassersaus dem Roten Meer und aus dem Persischen Golf. Meteor Forschungsergebnisse, A3,1-43.EAMFRO (1973). Annual report-EastEast African Community.African Marine Fisheries Research Organization, Zanzibar,EMERY, KO., ORR, W.L. and RITTENBERG, S.C. (1955). Nutrient budgets in the ocean. In:Essays in the natural sciences in honour of Captain Allan Hancock, University of SouthernCalifornia Press, 299-309.EWING, M., EITTREIM, S., TRUCHAN, M. and EWING, J.I. (1969). Sediment distribution inthe Indian Ocean. Deep-sea Res., 16,231-248.FAO (1978). Yearbook of Fishery Statistics. FAO, Rome, 45.FONDEKAR, S.P. and TOPGI, R.S. (1979). Trace analysis of pollutants in rainwater at Goa.Mahasagar-Bulletin of the National Institute of Oceanography, 12,49-51.FONDEKAR, S.P. TOPGI, R.S. and NORONHA, R.J. (1980). Dissolved, absorbed and adsorbedpetroleum hydrocarbons from the central west coast of India. Indian Journal of Marine Sci.,9, 286-289.GANESAN, R., SHAH, P.K., TUREL, Z.R. and HALDAR, B.C. (1980). Study of heavyelements (Cd, H g and Se) in the environment around Bombay by radiochemical neutronactivation analysis. Transaction 4th International Conference on Nuclear Methods inEnvironment and Environmental Research, Univ. Missouri, Columbia, USA.HARKANTRA, S.N., NAIR, A. ANSARI, Z.A. and PARULEKAR, A.H. (1980). Benthos of theshelf region along the west coast of India. Indian Journal of Marine Sci., 9, 106-1 10.HARTMANN, M. LANGE, H. SEIBOLD, S. and WALGER, E. (1971). Oberflachen-sedimenteim Persischen Golf und Golf von Oman, I. Geologisch-Hydrologischer rahmen und erstesedimentologiche ergebnisse, Meteor Forschungsergebnisse, C4, 1-76, GebruderBorn trae ger, Berlin .HEEZEN, B.C. and THARP, M. (1964). Physiograhic diagram of the Indian Ocean, the Red Sea,the South China Sea, the Sulu Sea and Celebes Sea. Geol. Soc. Amer.22
HOLEMAN, J.N. (1968). The sediment yield of major rivers of the world. Water Resources Res.,4, 787-797.INDIAN OCEAN BIOLOGICAL CENTRE (1968a). Maps on total zooplankton biomass in theArabian Sea and the Bay of Bengal. In: N.K. Pannikar (ed.), International Indian OceanExpedition Plankton Atlas, NIO, CSIR, New Delhi, l(1).INDIAN OCEAN BIOLOGICAL CENTRE (1968b). Maps on total zooplankton biomass in theArabian Sea and the Bay of Bengal. In: N.K. Pannikar (ed.), International Indian OceanExpedition Plankton Atlas, NIO, CSIR, New Delhi, l(2).IVANENKOV, V.N. and GUBIN, F.T. (1960). Water masses and hydrochemistry of the westernand southern parts of the Indian Ocean. Trudy Morskii Gidrofiz. Inst., Mad. Nauk SSSR,22, 33-1 15.KANNAN, S.T. and SEN GUPTA, R. (1987). Organochlorine residues in zooplankton off theSaurashtra Coast, India. Mar. Poll. Bull., 18,92-94.KREY, J. and BABENERD, B. (1976). Phytoplankton production, Atlas of the International IndianOcean Expedition, IOC/UNESCO, 70 pp.KUREISHY, T.W., GEORGE, M.D. and SEN GUPTA, R. (1978). DDT concentration inzooplankton from the Arabian Sea. Indian Journal of Marine Sci., 7,54-55.KUREISHY, T.W., GEORGE, M.D. and SEN GUPTA, S. (1979). Total mercury content in somemarine fish from the Indian Ocean. Mar. Pollut. Bull., 10,357-360.KUREISHY, T.W., SANZGIRI, S. and BRAGANCA, A.M. (1981). Some heavy metals in fishesfrom the Andaman Sea. Indian Journal of Marine Sci., 10,303-307.LEVY, E.M. and WALTON, A. (1976). High seas oil pollution-particulate petroleum residues in theNorth Atlantic. Journal of the Fisheries Research Board of Canada, 33,2781-2791.LISITZIN, A.P. (1971). Distribution of carbonate microfossils in suspension and in bottomsediments. In: B.M. Funnel and W.R. Riedel (eds.), The micropaleontology of the oceans,Cambridge University Press, London, 197-21 8.McGILL, D.A. (1973). Light and nutrients in the Indian Ocean. In: B. Zeitzschel (ed.), TheBiology of the Indian Ocean, Springer-Verlag, Berlin, 53-102.McKENZIE, D. and SCLATER, J.G. (1971). The evolution of the Indian Ocean since the lateCretaceous, Geophys. J. Royal Astron. Soc., London, 25,437-528.MOORE, W.S. and KRISHNASWAMI, S. (1972). Coral growth rates using 228Ra and 210Pb.Earth Planet. Sci. Lett., 15, 187-195.NATIONAL INSTITUTE OF OCEANOGRAPHY (1976). Report on the Marine EnvironmentalMonitoring and Marine Living Resources Assessment Programme for the Indian OceanRegion, Phase I-Survey of Institutional Capabilities, Report submitted to UNEP (mimeo).NATIONAL INSTITUTE OF OCEANOGRAPHY (1980). Status report on IOC/WMO MAPMOPPof IGOSS for the Indian Ocean region. Technical Report 04/80,19 pp.NAQVI, S.W.A., DE SOUSA, S.N. and REDDY, C.V.G. (1978). Relationship between nutrientsand dissolved oxygen with special reference to water masses in western Bay of Bengal.Indian Journal of Marine Sci., 7, 15-17.23
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: Localized problems, both short-term
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 38 and 39: Table 2.Ranges of Dissolved heavy m
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
Page 89 and 90:
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
Page 105 and 106:
were observed as early as 1770 duri
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diarrhetic shellfish poisoning (DSP
Page 109 and 110:
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
Page 138 and 139:
141FIGURE - 1
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~IT 73qw p' le' IS IFigure 4. Map s
Page 142 and 143:
@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
Page 154 and 155:
leaving little trace of their exist
Page 156 and 157:
REFERENCESAGASSIZ, A. (1903). The c
Page 158 and 159:
PILLAI, C.S.G. (1969b). Studies on
Page 160 and 161:
Table 1.Extent of damage to coral r
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STATUS OF CRITICAL MARINE HABITATS
Page 164 and 165:
OCCURRENCEThe distribution of reefs
Page 166 and 167:
Mining of Reef RockMining of reef r
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-resource. Their significance deriv
Page 170 and 171:
Coating of Aerial Roots by Fine Sed
Page 172 and 173:
associated with the roots (e.g. GOE
Page 174 and 175:
Temperature and SalinityThe effects
Page 176 and 177:
significant numbers in the Red Sea,
Page 178 and 179:
mersas are known to serve as nurser
Page 180 and 181:
BURCHARD, J.E. (1979). Coral fauna
Page 182 and 183:
HIRTH, H.F., KLIKOFF, L.G. and HARP
Page 184 and 185:
MacNAE, W. (1974). Mangrove forests
Page 186 and 187:
RINKEVITCH, B. and LOYA, Y. (1977).
Page 188 and 189:
WALKER, D.I. and ORMOND, R.F.G. (19
Page 190 and 191:
DAMMING AND DIVERSION OF RIVERSIn d
Page 192 and 193:
FUTURE STUDIESWhat can marine scien
Page 194 and 195:
!0OD9 -8 Nc80,a,u-3(dcab(Dbrr)8brr)
Page 196 and 197:
0 0-0 00 O0O 0% LD d- m cu 0 0202
Page 198 and 199:
STORM SURGES IN THE BAY OF BENGAL*T
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low pressure centres over the Bay i
Page 202 and 203:
ACKNOWLEDGEMENTSThe writers wish to
Page 204 and 205:
Table 1.Latitude and longitude of p
Page 207 and 208:
214
Page 209 and 210:
0Poa9nU0m0Yan-I2li7mYUVQk?401mc0mYm
Page 211 and 212:
0In218
Page 214 and 215:
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 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 316 and 317:
mC- 1000- 2000- 3000E0Figure 2.Sche
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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