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NAQVI, S.W.A., NORONHA, R.J. and REDDY, C.V.G. (1982). On denitrification in the ArabianSea. Deep-sea Res., 29,459-469.PARULEKAR, A.H. and ANSARI, Z.A. (1981).Journal of Marine Sci., 10,280-284.Benthic macrofauna of the Andaman Sea. IndianPRASAD, R.R., BANNERJEE, S.K. and NAIR, P.V.R. (1970). A quantitative assessment of thepotential fishery resources of the Indian Ocean and adjoining seas. Indian Journal of AnimalSci., 48, 78-98.QASIM, S.Z. (1977). Biological productivity of the Indian Ocean. Indian Journal of Marine Sci., 6,122- 1 37.QASIM, S.Z. (1982). Oceanography of the Northern Arabian Sea. Deep-sea Res., 29, 1041-1068.QASIM, S.Z. and SEN GUPTA, R. (1980). Recent status of marine pollution studies in India. In:B. Pate1 (ed.), Management of Environment, Wiley Eastern, New Delhi, 310-329.RAMA and SOMAYAJULU, B.L.K. (1972). Mercury in the sea food from the coast off Bombay.Current Sci., 41, 207-208.ROCHFORD, D.J. (1964). Salinity maxima in the upper 1000 m of the North Indian Ocean.Australian Journal of Marine and Freshwater Res., 15, 1-24.RYTHER, J.H. and MENZEL, D.W. (1965). On production, composition and distribution oforganic matter in the western Arabian Sea. Deep-sea Res., 12,199-209.SANO, A. SATOH, N. and KUBO, N. (1979). Particulate petroleum residues, tar balls, in thewestern Pacific. <strong>Oceanographic</strong> Magazine, <strong>Japan</strong>, 30,47-54.SANZGIRI, S and MORAES, C. (1979). Trace metals in the Laccadive Sea. Indian Journal ofMarine Sci., 10,238-240.SANZGIRI, S., SEN GUPTA, R. and SINGBAL, S.Y.S. (1979). Total mercury concentrations inwaters of the Laccadive Sea. Indian Journal of Marine Sci., 8,252-254.SANZGIRI, S. and BRAGANCA, A. (1981). Trace metals in the Andaman Sea. Indian Journal ofMarine Science, 10,238-240.SARKAR, A. and SEN GUPTA, R. Studies on organochlorine pesticide residues in marinesediments along the east coast of India. Mar. Pollut. Bull., in press.SEN GUPTA, R., FONDEKAR, S.P., SANKARANARAYANAN, V.N. and DE SOUSA, S.N.(1975). Chemical Oceanography of the Arabian Sea, Part I, Hydrochemical andhydrographical features of the northern basin. Indian Journal of Marine Sci., 4, 136-140.SEN GUPTA, R., SANKARANARAYANAN, V.N., DE SOUSA, S.N. and FONDEKAR, S.P.(1976a). Chemical oceanography of the Arabian Sea, Part 111, Studies on nutrient fractionsand stoichiometric relationships in the northern and the eastern basins. Indian Journal ofMarine Sci., 5, 58-71.SEN GUPTA, R. RAJAGOPAL, M.D. and QASIM, S.Z. (1976b). Relationship between dissolvedoxygen and nutrients in northwestern Indian Ocean. Indian Journal of Marine Sci., 5,201 -21 2.SEN GUPTA, R., DE SOUSA, S.N. and JOSEPH, T. (1977). On nitrogen and phosphorus inWestern Bay of Bengal. Indian Journal of Marine Sci., 6, 107-110.24
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: HOLEMAN, J.N. (1968). The sediment
Page 29 and 30: tP t\ P9 hc.r(27
Page 31 and 32: STAT I ON222 223 224 225 226 227DIS
Page 33 and 34: 30' 60' goo I 20°Figure 5. The Ind
Page 36: L2WE.- LEUEc0At-0ae-0cI2p.a:0AWE._L
Page 39 and 40: I80U)'9-00c!IIIIIIr42U)c?-9VIIIIIzd
Page 41 and 42: Body Parts Mercurv LeadRange Averag
Page 43 and 44: Table 1A. Relation between the diss
Page 45 and 46: (9) PIOLA and GORDON (1984) estimat
Page 48: wfhcu2L53drNHlNOrJ47
Page 51 and 52: 4015 SO€ 60E 70E 80E 90E IOOE 114
Page 53 and 54: PHYSICAL OCEANOGRAPHY OF THE NORTHE
Page 55 and 56: helped in the piecing-together of t
Page 57 and 58: high opal and biogenic siliceous co
Page 59 and 60: MESOZOIC OCEANOGRAPHY AND CLIMATESM
Page 61 and 62: The ophiolite suite along the Indus
Page 63 and 64: associated with the development of
Page 65 and 66: LUYENDYK, B.P. and RENNICK, W. (197
Page 68: v)z_Um9nzWU0!-IJU520nQ,40v)wn:-an84
Page 72: a9zI I I I I I I I0 0 0 0 0 0 0O Z
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2M.r(LL79
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oundaries between regions completed
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FISHER, R.L. SCLATER, J.G. and McKE
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UDINTSEV, G.B. and KORENEVA, E.V. (
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PRELIMINARY DISCUSSIONPATULLO, MUNK
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KNMI Atlas (1952) gives the monthly
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PERMANENT SERVICE FOR MEAN SEA LEVE
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26lo'Figure 1.Area of interest, sho
Page 94 and 95:
STATION : VERAVALL , J , F , M , A
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3001STATION : MARMAGAOJ . F . M , A
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300~STATION : NAGAPATTINAM, J.,F M
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STATION : VISHAKHAPATANAM-200-E 100
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Xrn0 iO QD0 2jIxM+X00QQ ma00 0 m++0
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caused by eating shellfish, and cig
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(TANGEN, 1983), where its coffee-br
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ACKNOWLEDGMENTSI am greatly indebte
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SUBRAHMANYAN, R. (1954b). A new mem
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Ta ble 2.Shellfish species implicat
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IIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIIII
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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
Page 205:
3;7354aM8F9a00I-dd.212
Page 208 and 209:
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
Page 221 and 222:
CIRCULATION AND PHYSICAL PROCESSES
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In the Arabian Sea dissolved oxygen
Page 225 and 226:
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
Page 247 and 248:
BASIC OCEANOGRAPHIC FEATURES OF THE
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Simultaneously, rather extensive fi
Page 251 and 252:
~~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
Page 281 and 282:
-mE-*’=0 c>0zmNt0c0nWU0Iv)2It33aU
Page 283 and 284:
d............... . ..LL '..,.. . I.
Page 285 and 286:
W0-5:izU0v,PIIMI I I I0InIn(UO/o 3n
Page 287 and 288:
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
Page 295 and 296:
SiO4(,urnoi/I)0 5 10 15 20 25 30PO4
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THE CRUST BENEATH THE RED SEA - GUL
Page 299 and 300:
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
Page 307 and 308:
~5) continued thinning and rifting
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BURKE, R.A. JR., BROOKS, J.M. and S
Page 311 and 312:
GIRDLER, R.S. and STYLES, P. (1982)
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QUENNELL, A.M. (1958). The structur
Page 315 and 316:
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
Page 331 and 332:
On the African side, Precambrian sh
Page 333 and 334:
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
Page 355:
SMITH, J.J.B. (1950). The sea fishe
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