139736eo.pdf (20MB) - Japan Oceanographic Data Center

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STATION : VISHAKHAPATANAM-200-E 100.-Wz02a -100 -IWv)-200--3Od800-600-40&200-< 0-; I I I I I IFigure 9. Same as in 3, but for Vishakhapatnam.102
STATION : CALCUTTA, J l F , M , A , M , J , J , A , S , O , N , D ,-Ec.W9J>WJa -400-60020-0-20-1 II I I800 -5 4oaaLLZ2alLa[y:Q-I1J I F I M I A M ' J I J I A I SI 0 ' N I 0'Figure 10. Same as in 3, but for Calcutta.103
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
Page 9 and 10:
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
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
Page 91 and 92: Table 1.MarmagaoCochin1969-781958-7
Page 93 and 94: tFigure 2. An idealized coastal cur
Page 95 and 96: STATION : BOMBAY~ J , F I M .- , A
Page 97 and 98: STATION : COCHIN, J , F , M , A , M
Page 99: 3007STATION : MADRASI J I F , M I A
Page 103 and 104: RED TIDE§ IN THE INDO-WEST PACIFIC
Page 105 and 106: were observed as early as 1770 duri
Page 107 and 108: diarrhetic shellfish poisoning (DSP
Page 109 and 110: GACUTAN, R.Q., TABBU, M.Y., AUJERO,
Page 111 and 112: Table 1.Clinical symptoms of variou
Page 113 and 114: Table 3. Fish species implicated in
Page 115 and 116: FIGURE CAPTIONSFigure la. Trichodes
Page 118 and 119: (*14aEE15aHH15c120
Page 120 and 121: MINERAL RESOURCES OF THE INDIAN OCE
Page 122 and 123: tonnes of monazite. Similar deposit
Page 124 and 125: Madagascar and the Red Sea. Within
Page 126 and 127: South Australian Basin: (Figs. 10-1
Page 128 and 129: Offshore placers are likely to occu
Page 130 and 131: MILLIMAN, J.D. (1974). Marine Carbo
Page 132 and 133: Thailand Tin 5560 (1980) NA 4.2 (19
Page 134 and 135: Table 2. The range (in percent) of
Page 136 and 137: Table 4. Chemical composition of po
Page 138 and 139: 141FIGURE - 1
Page 140 and 141: ~IT 73qw p' le' IS IFigure 4. Map s
Page 142 and 143: @A5 3 9 93 3 s 3 m4P 8O C ' . .' ,
Page 144 and 145: Figure 10. Map showng the abundance
Page 146 and 147: Figure 14. Map showing the distribu
Page 148 and 149: IFigure 17. Marine mineral explorat
Page 150 and 151:
central are corals to the integrity
Page 152 and 153:
Very little information is availabl
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leaving little trace of their exist
Page 156 and 157:
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
Page 174 and 175:
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
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
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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
Page 214 and 215:
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
Page 220 and 221:
INDIABAY OF-Point CalirnereLanka L-
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pressure in the South Pacific and l
Page 224 and 225:
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-
Page 238 and 239:
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
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
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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
Page 284 and 285:
I I I I I10 Ic L0U0mI(dw -rlo u0w m
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III I I I0. 1....w'3...-0U-J..,....
Page 288 and 289:
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
Page 298 and 299:
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
Page 320 and 321:
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
Page 330 and 331:
SUPERFICIAL SEDIMENTS OF NORTHERN R
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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
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Figure 4. Distribution of minerals
Page 346 and 347:
ARAGONITEHIGH HG-CALCITEFigure 6. T
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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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