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KARBE, L., THIEL, H., WEIKERT, H. and MILL, A.J.B. (Eds.) (1981). Mining of metalliferoussediments from the Atlantis I1 Deep, Red Sea: Pre-mining environmental conditions andevaluation of the risk to the environment. Environmental Impact Study presented to theSaudi Sudanese Red Sea Joint Commission, Jeddah. Hamburg, 352 pp.KHMELEVA, N.N. (1970). On the primary production in the Red Sea and Gulf of Aden (Russ.).Biol. Morya (Kiev), 21, 107-133.KHIMITSA, V.A. and BIBIK, V.A. (1979). Seasonal exchange in dissolved oxygen andphosphates between the Red Sea and the Gulf of Aden. Oceanology, 19,544-546.LEVANON-SPANIER, I., PADAN, E. and REISS, 2. (1979). Primary production in adesert-enclosed sea - the Gulf of Elat (Aqaba), Red Sea. Deep-sea Res., 26,673-685.MURINA, W.W. (1971). Characterization of the Red Sea macrobenthos. In: The Benthos of theRed Sea shelfs. Akad. Nauk. SSSR. Verlag Naukova Dumka, Kiev, 3-22.PFANNKUCHE, O., THEEG, R. and THIEL, H. (1983). Benthos activity, abundance andbiomass under an area of low upwelling off Morocco, Northwest Africa. Meteor. Forsch.Ergebnisse D, 36, 85-96.PFANNKUCHE, 0. and THIEL, H. (1983). Meiobenthic stocks and benthic activity on theNE-Svalbard shelf and in the Nansen Basin. Polar Biol., 7,253-266.POISSON, A., MORCOS, S., SOUVERMEZOGLOUj E., PAPAUD, A. and IVANOFF, A.(1984). Some aspects of biogeochemical cycles in the Red Sea with special reference to newobservations made in summer 1982. Deep-sea Res., 31,707-718.SUKHANOVA, J.N. (1969). Some data on the phytoplankton of the Red Sea and the western Gulfof Aden. Oceanology, 9,243-247.THEEG, R. (1985). Die Aktivitat des Elektronen-Transport-Systems benthischerLebensgemeinschaften. Diss. Univ. Hamburg, 195 pp.THIEL, H. (1979). First quantitative data on the Red Sea deep benthos. Mar. Ecol. Prog. Ser., 1,347-350.THIEL, H. (1983). Meiobenthos and nanobenthos of the deep sea. In: G.T. Rowe (ed.), The Sea,8, 176-230.THIEL, H. (in press). Benthos of the deep Red Sea. In: A. Edwards and S.M. Head (eds.), TheRed Sea. Key Environment Series. Pergamon Press, Oxford, 112-127.THIEL, H. and WEIKERT, H. (1984). Biological oceanography of the Red Sea oceanic system(Abst.). Deep-sea Res., 31, 829-831.THIEL, H., WEIKERT, H. and KARBE, L. (1986). Risk assessment for mining metalliferousmuds in the deep Red Sea. Ambio, 15,34-41.THIEL, H., PFANNKUCHE, O., THEEG, R. and SCHRIEVER, G. (1987). Benthic metabolismand standing stock in the central and northern deep Red Sea. P.S.Z.N.I. Mar. Ecol., 8,1-20.WEIKERT, H. (1981). The pelagic communities. In: L. Karbe, H. Thiel, H. Weikert and A.J.B.Mill (eds.), Mining of metalliferous sediments from the Atlantis I1 Deep, Red Sea:Re-mining environmental conditions and evaluation of the risk to the environment.Environmental Impact Study presented to the Saudi Sudanese Red Sea Joint Commission,Jeddah. Hamburg, 100-154 pp.302
WEIKERT, H. (1982). The vertical distribution of zooplankton in relation to habitat 'zones in thearea of the Atlantis I1 Deep, central Red Sea. Mar. Ecol. hog. Ser., 8, 129-143.WEIKERT, H. (in press). Plankton and the pelagic environment. In: A Edwards and S.M. Head(eds.), The Red Sea. Key Environment Series. Pergamon Press, Oxford, 90-111.Table , A comparison of meiofauna dens_,les (individuals 10 cm-*; valuesrounded, omitting Foraminifera) from different areas. Summarizedfrom various sources (THIEL, 1983).Regionapproximate water depth in meters500 1000 2000303
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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
Page 242 and 243: Age of Semi-Diurnal Tide (hrs)28".+
Page 244 and 245: ! 5"BOTTOMFigure 13. Predicted mode
Page 246 and 247: OCEANOGRAPHIC CONDITIONS PELAGIC PR
Page 248 and 249: Low oxygen content in subsurface wa
Page 250 and 251: R/V Dr. F. Nansen trawl of 41 m hea
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Page 254 and 255: 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
Page 266 and 267: ROYAL SOCIETY (1963). International
Page 268 and 269: APPENDIX:REGIONAL COOPERATIVE INVES
Page 270 and 271: 20 015 20 25FEBOC015 20 25 30 35M A
Page 272 and 273: W0-8w0-Inww[r3a+eW281
Page 274 and 275: B35 36 a7 XlO+ 35 36 a7- Mar--- Fob
Page 276 and 277: a, A
Page 278 and 279: ...... :'I. .. ,... .. 8.*.. ... ._
Page 280 and 281: 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
Page 286 and 287: III I I I0. 1....w'3...-0U-J..,....
Page 288 and 289: 297
Page 290 and 291: clearly is too low. Because of low
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
Page 302 and 303: 1969; SEARLE and ROSS, 1975). This
Page 304 and 305: y normal faulting. This is most int
Page 306 and 307: South of 19"N, the McKENZIE pole no
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
Page 324 and 325: 5 b'o w-Y EO'i Ii04!I 0I0I334
Page 326 and 327: II,'{34/,'0SOMALIAND: N. DANAKILFig
Page 328 and 329: spreadingvulcanismmblock faultingII
Page 330 and 331: SUPERFICIAL SEDIMENTS OF NORTHERN R
Page 332 and 333: 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
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EGYPTEl-Morgan 1Bargan IBargan 2Yub
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Figure 4. Distribution of minerals
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ARAGONITEHIGH HG-CALCITEFigure 6. T
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MARINE LIVING RESOURCES OF THE RED
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This elevated productivity may resu
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REVELLE (1981) mentioned that the p
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FISHELSON, L. (1964). Observation o
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