BEHAIRY, AKA. (1983). Marine transgression in the west coast of Saudi Arabia (Red Sea),between Mid-Pleistocene and Present. Mar. Geol., 52, M25-M31.BEHAIRY, A.K.A., AL-KLOLY, A.A., HASHEM, M.T. and EL-SAYED, MKH. (1983).Preliminary study on the geology and fisheries of the coastal area between Jeddah andYanbu. J. Fac. Mar. Sci., Jeddah, 3, 1-47. (in Arabic).BEHAIRY, A.K.A., DURGAPRASSADA RAO, N.V., EL-ABD, Y ., EL-SAYED, M.KH. andYUSUF, N. (1985). Investigations on the metalliferous sediments from some deeps in theRed Sea. Report, KAUFMS, Jeddah, 119 p.BOUCHON, C., JAUBERT, J., MONTAGGIONI, L and PICHON, M. (1981). Morphology andevolution of the coral reefs of the Jordanian coast of the Gulf of Aqaba. 4* Int. Coral ReefSymp. Manila,Philippines, May, 1981, Abs: 8.CHERIF, O.H., EL-DEEB, W.Z.and HASSAN, M.Y. (1983). Statistical studies on the distributionof dead foraminiferal tests in recent sediments of the northern Red Sea. Bull. Inst.Oceanogr. Fish., 9, (in press).COLEMAN, R.G. (1977). Geologic background of the Red Sea. Min. Res. Bull., DGMR, Jeddah,22, 1-9.CROSSLAND, C. (1939). Some coral formations. In: Report on the preliminary expedition for theexploration of the Red Sea in the RRS "Mabahith". Publ. Mar. Biol., St. Ghardaqa, 1,21-35.DEGENS, E.T. and ROSS, D.A. (1969). Hot brines and Recent heavy metal deposits in the RedSea. Springer-Verlag, New York, 600 p.EL-DEEB, W.Z.M. (1978). Ecological studies on foraminifera in Recent marine sediments of thenorthern Red Sea. M.Sc. Ain-Shams University.EL-SAYED, M.KH. (1983). Trace metals as possible descriminating tool amongst the differentreefal depositional sedimentary environments. Unpubl. Report, Jeddah, KAU/FMS, 8-25.EL-SAYED, M.KH. (1984). Reefal sediments of Al-Ghardaqa, northern Red Sea, Egypt. Mar.Geol., 56, 259-271.EL-SAYED, M.KH. and HOSNY, CH.F. (1980). Sediments of the intertidal zone off Ghardaqa,Red Sea, Egypt. Prw. Symp. Coastal. Mar. Environ. Red Sea, Khartoum 1980,2,3-15.EL-WAKEEL, S.K., EL-SAYED, M.KH. and HUSSEIN, S.A. (1984). Relative abundance ofcarbonate minerals in common reef building corals at Al-Ghardaqa, Red Sea, Egypt. Symp.Coral Reef Environ. Red Sea, Jeddah, Jan. 1984 (in press).FRIEDMAN, G.M. (1965). A fossil shoreline reef in the Gulf of Aqaba. Isr. J. Earth Sci., 14,86-90.FRIEDMAN, G.M. (1968). Geology and geochemistry of reefs, carbonate sediments and waters,Gulf of Aqaba, Red Sea. J. Sed. Petrol., 38, 895-913.GABRIE, C., and MONTAGGIONI, L. (1982). Sedimentary facies from the modem coral reef,Jordan, Gulf of Aqaba, Red Sea. Coral Reefs, 1, 115-124.GEVIRTZ, J.L. and FRIEDMAN, G.M. (1966). Deep sea carbonate sediments of the Red Sea andtheir implications on marine lithification. J. Sed. Petrol., 36, 143-152.347
GUILCHER, A. (1979). Les rivages coraliens de l'est et du sud de la presqu'ile du Sinai. Ann. deGeogr., 88, 394-418.GVIRTZMAN, G., BUCHBINDER, B., SNEH, A, NIR, Y. and FRIEDMAN, G.M. (1977).Morphology of the Red Sea fringing reefs, a result of the erosional pattern of the last glaciallow stand sea level and following Holocene recolonization. 2nd Symp. Int. Coral et RacifsCoral. Fossils., Paris, Sept. Mem. BRGM., 89, 480-491.HALL, S.A. (1976). A total intensity magnetic anomaly map of the Red Sea and its interpretation.Ph.D. thesis, Newcastle Upon Tyne University.HUME, W.F. (1906). The topography and geology of the Peninsula of Sinai (Southern portion).Cairo, Survey, Dept. of Egypt. Nat'l. Printing Dept., 280 p.MERGNER, H. (1984). The ecological research on coral reefs of the Red Sea. Deep-sea Res.,68A, 855-900.MERGNER, H. and SCHUMACHER, H. (1974). Morphlogie, Okologie und Zonierung vonKorallenriffen bei Aqaba (Golf von Aqaba). Rotes Meer. Helgolander Wissensch.Meeresinst., 26, 238-358.MILLIMAN, J.D. (1974). Recent marine sedimentary carbonates. Springer-Verlag, Heidelberg,375 p.MILLIMAN, J.D., ROSS, D.A. and KU, T.-L. (1969). Precipitation and lithification of deep-seacarbonates in the Red Sea. J. Sed. Petrol., 39,724-736.MOHAMED, A.F. (1949). The distribution of organic matter in sediments from the northern RedSea. Amer. J. Sci., 247, 1 16- 127.MOHAMED, M.A. (1979). The Recent bottom sediments of the Gulf of Suez, Red Sea. J. Univ.Kuwait (Sci.), 6, 209-228.MOHAMED, M.A. (1980). The distribution of carbonate in the Recent bottom sediments of the Gulfof Suez (Red Sea). Roc. Symp. Coast. Mar. Environ. Red Sea, Khartoum, 2,37-51.MORCOS, S.A. (1970). Physical and chemical oceanography of the Red Sea. Oceanogr. Mar.Biol., Annual Rev., 8, 73-203.NAWAR, A.H. (1983). Mineralogy and bottom topography of the Gulf of Suez. Bull. Inst.Oceanogr. Fish., 8, 31 p.RUPPELL, E. (1829). Reisen in Nubien, Kordofan und dem petraischen Arabien vorzuglisch.Geogr. Statist. Hinsicht. Wilmans, Frankfurt, 141 p.SAID, R. (1949). Foraminifera of the northern Red Sea. Cushman Lab. Foram. Res. Sp. Publ.SAID, R. (1950a). The distribution of foraminifera in the northern Red Sea. Contrib. Cushman.Found. Foram. Res., 1, 9-29.SAID. R. (1950b). Foraminifera of the northern Red Sea. Ph.D. thesis, Harvard University.SAID, R. (1951). Organic origin of some calcareous sediments from the Red Sea. Science, 113,518-5 19.SAID, R. (1969). General stratigraphy of the adjacent land areas of the Red Sea. In: E.T. Degensand D.A. Ross (eds.), Springer-Verlag, New York Inc., 71-81.348
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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
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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
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0Q0mbWbvx(U49
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Figure 6 Average wind stress curl f
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THE DESTRUCTION OF THE TETHYS AND P
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part of the Seychelles-Mascarene bl
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Much of the old Tethys seafloor has
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when there was little or no movemen
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scouring of the sediments by cold b
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CANDE, S.C. and MUTTER, J.C. (1982)
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SHACKLETON, N.J. and KENNETT, J.P.
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0EYNz 10c2XaYWeKB20LuUz a5 cl300 10
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CALCAREOUS FORAMINIFERANANNOFOSSIL
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GEOLOGICAL-GEOPHYSICAL MAPPING OF T
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The latest tectonic generalization
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LE PICHON, X. and HEIRTZLER, J.R. (
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AN EXAMINATION OF THE FACTORS THAT
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is the specific volume anomaly. Po
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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
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were observed as early as 1770 duri
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diarrhetic shellfish poisoning (DSP
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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
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141FIGURE - 1
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~IT 73qw p' le' IS IFigure 4. Map s
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@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
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leaving little trace of their exist
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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
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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
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BURCHARD, J.E. (1979). Coral fauna
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HIRTH, H.F., KLIKOFF, L.G. and HARP
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MacNAE, W. (1974). Mangrove forests
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RINKEVITCH, B. and LOYA, Y. (1977).
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WALKER, D.I. and ORMOND, R.F.G. (19
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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
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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
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INDIABAY OF-Point CalirnereLanka L-
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pressure in the South Pacific and l
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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
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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-
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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
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The maximum standing stocks in the
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By April/May the demersal stocks ha
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in 6 months when spawning occurs. T
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REFERENCES3BANSE, K. (1968). Hydrog
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GILSON, H.C., (1937). The nitrogen
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ROYAL SOCIETY (1963). International
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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 -
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YU0IwYY->02(33-1 II 1amLyY>02(33amL
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I I I I I10 Ic L0U0mI(dw -rlo u0w m
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- 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
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- Page 304 and 305: y normal faulting. This is most int
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- 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
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- Page 326 and 327: II,'{34/,'0SOMALIAND: N. DANAKILFig
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- Page 334 and 335: EL-SAYED (1983) used the trace meta
- 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
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- Page 354 and 355: FISHELSON, L. (1964). Observation o