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0EYNz 10c2XaYWeKB20LuUz a5 cl300 10 20 30 40 SO 60 70 80TIME IN M.Y.B.P.Figure 5. A comparison of half spreadingrates for the latest Cretaceousand Cenozoic (magnetic anomalies33 base to 5) in three majoroceans. Notice the exceptionallyfast rates in the central IndianOcean up to anomaly 21. Pacificmagnetic anomaly profile afterPITTMAN -- et al. (1968), SouthAtlantic profile after DICKSONet al. (19681, and centralL-Indian Ocean profile after MCKENZIEand SCLATER (1971).72
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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
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 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 72: a9zI I I I I I I I0 0 0 0 0 0 0O Z
Page 78 and 79: 2M.r(LL79
Page 80 and 81: oundaries between regions completed
Page 82 and 83: FISHER, R.L. SCLATER, J.G. and McKE
Page 84 and 85: UDINTSEV, G.B. and KORENEVA, E.V. (
Page 86 and 87: PRELIMINARY DISCUSSIONPATULLO, MUNK
Page 88 and 89: KNMI Atlas (1952) gives the monthly
Page 90 and 91: PERMANENT SERVICE FOR MEAN SEA LEVE
Page 92 and 93: 26lo'Figure 1.Area of interest, sho
Page 94 and 95: STATION : VERAVALL , J , F , M , A
Page 96 and 97: 3001STATION : MARMAGAOJ . F . M , A
Page 98 and 99: 300~STATION : NAGAPATTINAM, J.,F M
Page 100 and 101: STATION : VISHAKHAPATANAM-200-E 100
Page 102 and 103: Xrn0 iO QD0 2jIxM+X00QQ ma00 0 m++0
Page 104 and 105: caused by eating shellfish, and cig
Page 106 and 107: (TANGEN, 1983), where its coffee-br
Page 108 and 109: ACKNOWLEDGMENTSI am greatly indebte
Page 110 and 111: SUBRAHMANYAN, R. (1954b). A new mem
Page 112 and 113: Ta ble 2.Shellfish species implicat
Page 114 and 115: IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII
Page 116: laIC
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ECONOMICANDPOLLUTIONASPECTS121
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of equipment and larger vessels, on
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Southeast Asia: Southeast Asia is t
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to 32.5 percent of P205) and limest
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studies would not only provide data
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COOLEY, N., CRONAN, D.S. and MOORBY
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South Africa Titanium sand ,NA NA 4
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Table 1. (continued)Country Mineral
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South AfricaTanzaniaKenya (Guano)Em
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Table 4. Chemical composition of po
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142
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115’ 739 1(‘ 117’ I 1I’Figu
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IFigure 8. Map showing the occurren
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Figure 12. Map showing the distribu
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CENTRAL INDIAN BASINP, N cuWHARTON
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RESEARCH NEEDS FOR THE CORAL REEF E
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NATURAL CAUSES OF REEF DEGRADATIONA
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INDIAThe coral reef formations in I
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BANGLADESHThe only known coral reef
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GARDINER, J.S. (1904). Madreporaria
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SOROKIN, Y.I. (1973). In O.A. Jones
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Figure 1. The major types of coral
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1954) and 7,300 g C m-2 yrl (GORDON
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upstream land and soil erosion. Inc
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However, corals that become coated
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island nations and groups of the In
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ecognised, as is common with many m
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Along the coasts of the Indian sub-
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environmental stress, and subsequen
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acteria, zooplankton and filter fee
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REFERENCESALEEM, A.A. (1984). Seagr
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DIAZ-PIFFERER, M. (1962). The effec
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JOKIEL, P.L. and COLES, S.L. (1974)
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O'GOWER, A.K. and WACASEY, J.W. (19
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SNEDAKER, S.C. (1984). The mangrove
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RISING SEA LEVEL AND CHANGING SEDIM
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of unconsolidated sediment (assumin
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Table 1. Ranking of the world's maj
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01601402 400ro0 hL 350Q2 300625025
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MARGINALSEAS203
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FACTORS RELATING TO SURGE GENERATIO
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(3) A short C-type belt occurs Niza
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RAO, N.S.B. (1968). On some aspects
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3;7354aM8F9a00I-dd.212
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215
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Wd217
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n E219
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IIIIIIIIIIIIIIIIIIIIII3rFIIojoa222
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Table 4. Maximum possible storm sur
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Figure 2.Frequency of severe cyclon
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CIRCULATION AND PHYSICAL PROCESSES
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In the Arabian Sea dissolved oxygen
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Table 1.Distribution of the depth o
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61' 63' 65' 67'25'I I I I I61' 63O
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A REVIEW OF THE PHYSICAL OCEANOGRAP
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PHYSICAL OCEANOGRAPHIC PROPERTIESTh
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This current is weaker and narrower
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IIFigure 1.Geography and bathymetry
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4l 2-4 1 .1. 4- ---- --.2./*--I,0°
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I R A NARABIA26"-24'-INNER GULF, KA
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K:Diutide. ....... ....._ ..... ..
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Figure 11. The probable circulation
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FISHERY RESOURCES IN THE NORTH ARAB
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BASIC OCEANOGRAPHIC FEATURES OF THE
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Simultaneously, rather extensive fi
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~~Table 1 Physical chemical propert
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position in time and according to c
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OXYGENThe spatial distribution of d
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EXPLOITABLE LIVING RESOURCESThe fir
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Table 3. Seasonal variations in sta
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It is logical to expect that such h
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DHULKED, M.H. (1962). Observations
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KREY, J. and BABENARD (1976). Phyto
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SMITH, S.L. (1982). The northwester
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c0*rlUaUII)hU.rl?.rlUU3a0.4a0‘rlP
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GmEakU0U0Cn I4: aUkm .u u-aw nLU0,t
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282
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1984 -1985 AIMu kalla---- Nov-- Feb
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aIVI030cH \'YNlEO 08'000 0 0dOJ286
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na288
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-mE-*’=0 c>0zmNt0c0nWU0Iv)2It33aU
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d............... . ..LL '..,.. . I.
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W0-5:izU0v,PIIMI I I I0InIn(UO/o 3n
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WEATHER IMONSOONSJ I SOLAR RADIATIO
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RED SEA BIOLOGICAL OCEANOGRAPHY AND
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Benthic studies in the deep waters
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WEIKERT, H. (1982). The vertical di
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SiO4(,urnoi/I)0 5 10 15 20 25 30PO4
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THE CRUST BENEATH THE RED SEA - GUL
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generally weak or lacking, the only
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the Bouguer gravity reaches only 90
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Such an isotopic composition has le
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Since no major shear, spreading, or
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~5) continued thinning and rifting
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BURKE, R.A. JR., BROOKS, J.M. and S
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GIRDLER, R.S. and STYLES, P. (1982)
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QUENNELL, A.M. (1958). The structur
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Figure 1.Simplified morphology and
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QA.7 o 2.7*oPlia‘PlrihPlia 7c tMi
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v)CdQIE-30LIYiJr0,dQ,rnUQIaT dIIT I
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37.19'vv22'06'N01 37.36' EJ 2.522 '
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N-c-0-c.I333
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Figure 11.Isochrons in m.y. deduced
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337c&!C0
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SEDIMENTARY STRUCTURE OF THE NORTHE
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On the African side, Precambrian sh
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length the Red Sea is characterized
Page 335 and 336:
SUGGESTIONS FOR FUTURE RESEARCH IN
Page 337 and 338:
GUILCHER, A. (1979). Les rivages co
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Concentration96Aqaba*AI-Ghardaqa**3
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Figure 1. Geologic map of the north
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35 O 34O 33O 32' 3 l o30°SINAI?go!
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356
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1 In 35" 4003I4 50Oceanographer dee
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only a partial inflow of Indian Oce
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wind reef margins, are required. Th
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4.5.6.7.8.9.10.11.F12.13.14.What is
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SMITH, J.J.B. (1950). The sea fishe
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