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CALCAREOUS FORAMINIFERANANNOFOSSIL SITE 253SITE 2170 SITE 237o PLANKTONIC0 BENTHIC& 6 LATE I M.1 EARLY LATE [EARLYE smA dMIOCENEOLIGOCENELATElMlDDLEl EARLY I L. I E. LATEEOCENE PALEO- CRETA,ICENE CEOUS0 10 20 30 40 50 60 70TIME IN MILLION YEARS B.P.B K2w tK3FQ:Kw:r0w4Q:ncs0Figure 9.Cenozoic oxygen-isotopic record from DSDP sites in the Indian Ocean. The majorclimatic trends in the Indian Ocean follow global trends. (After OBERHANSLI,1986).76
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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
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 71 and 72: 0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
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
Page 119 and 120: ECONOMICANDPOLLUTIONASPECTS121
Page 121 and 122: 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
Page 179 and 180:
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
Page 187 and 188:
SNEDAKER, S.C. (1984). The mangrove
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RISING SEA LEVEL AND CHANGING SEDIM
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of unconsolidated sediment (assumin
Page 193 and 194:
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
Page 205:
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
Page 259 and 260:
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.
Page 285 and 286:
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
Page 291 and 292:
Benthic studies in the deep waters
Page 293 and 294:
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
Page 317 and 318:
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!
Page 345 and 346:
356
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1 In 35" 4003I4 50Oceanographer dee
Page 349 and 350:
only a partial inflow of Indian Oce
Page 351 and 352:
wind reef margins, are required. Th
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4.5.6.7.8.9.10.11.F12.13.14.What is
Page 355:
SMITH, J.J.B. (1950). The sea fishe
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