139736eo.pdf (20MB) - Japan Oceanographic Data Center
139736eo.pdf (20MB) - Japan Oceanographic Data Center 139736eo.pdf (20MB) - Japan Oceanographic Data Center
Temperature and SalinityThe effects of alterations in temperature and salinity, such as might arise from coastalconstruction work or effluent discharge, depend upon the species concerned. For example,Syringodium is reported to die at temperatures below 20°C (ZIEMAN, 1975), whilst Halophila ovaliscan tolerate seawater temperatures lower than 10°C. Conversely, Halophila stipulacea is very salinityadaptablewhilst Cymodocea serrulata is very sensitive to a decrease in salinity (DEN HARTOG,1970).OvergrazingAs already discussed, although many herbivores do not eat seagrass, a variety of species,particularly of fish and sea urchin, feed directly on the plant, and where these grazers are present invery large numbers, overgrazing and destruction of the grass bed can occur. Such overgrazing byreef-associated fish frequently results in a bare halo around patch reefs in the Caribbean (RANDALL,1965; OGDEN, 1972), and in some localities epidemic overgrazing by sea urchins is reported (CAMPet al., 1973). In the,Red Sea recently there has been loss of seagrass at Aqaba (Jordan) throughovergrazing by large numbers of the urchins Diadema setosum and Tripneustes gratilla (BENAYAHUand LOYA, 1977; MASTALLER, 1979; WAHBEH, 1980), and such population outbreaks ofechinoids may occur as a result of the loss of predators taken by man (LOWRY and PEARSE, 1973;BREEN and MANN, 1976). Thus intensification of some fisheries can indirectly result in the loss ofseagrass beds.Oil PollutionAs seagrasses are generally subtidal, they are less susceptible to damage from oil thanorganisms in the intertidal zone. However, in some regions large areas of reef flat, sometimescontaining seagrasses, are exposed at low tides and these seagrasses probably would be killed bydirect contact with oil. Also surface floating rafts of oil, if present for long enough, can affectsignificantly seagrasses by reducing light penetration, by increasing water temperature throughabsorption of light energy, and by reducing oxygen exchange at the air/oil/water interface.In addition to direct effects on the seagrass, more serious and possibly longer-term damagemay occur through interaction between the oil and the sediments in which the seagrass is growing.Much of the oil and tar from oil spills eventually sinks to the seabed, and here oil and sediment canagglomerate into more buoyant lumps and pellets which, in relatively shallow water, can be removedby wave and current action. DIAZ-PIFFERER (1962) recorded the loss of 3,000 m3 of sand from aPuerto Scan beach in less than a week due to this effect. Where oil settles over seagrass beds, loss ofsediment can lead to uprooting of the grass and damage to or destruction of the bed.In this connection it should be noted that a number of oil spill dispersants cause floating oil tosink so that seagrass beds that might otherwise be safe from oil could be directly contacted by it, orimpacted by destabilisation of sediments as just described.MetalsSeagrasses are reported to have a very high uptake of metals (e.g. PARKER et al., 1963),despite the fact that the roots are often in reducing conditions that limit the lability of metal ions. Notonly can excess metals be concentrated in the seagrass but they become available for furtheraccumulation in the food chain. This has been of particular concern in some tropical regions wkrehigh concentrations of metals have been released into the environment from desalination plants (seeCHESHER, 1975).DiseaseIn the 1930's a large-scale and so far permanent loss of beds of the temperate seagrass Zosteramarina occurred on both sides of the Atlantic (see STEVENS, 1936) that was attributed to a fungaldisease (TUTIN, 1934). So far as is known, disease has not caused extensive damage to seagrassbeds in the tropics. However, susceptibility to disease is frequently a response to increased179
environmental stress, and subsequent loss of Zostera beds in Japan was linked to industrialisation andincreasing water pollution along the coast (NAIKAI REG. FISH. RES. LAB., 1967; NASEI REG.FISH. RES. LAB., 1974).SMALL ISLANDSOTHER CRITICAL HABITATSSmall islands, offshore of the mainland coast or oceanic islands in deeper water, are numerousin many parts of the Indian Ocean. For example there are 200 or more small coral cays and islandsalong the eastern seaboard of the Red Sea alone. Island groups of the Indian Ocean, the Maldives,Seychelles, Lakshadweep, Nocibars and Andamans, include many small coralline or volcanic islets,besides the larger islands that support human population.The smaller islands constitute significant critical habitats. Not only are they generallysurrounded by shallow water marine habitats, coral reefs, seagrass beds and mangrove stands, whichare considered critical in their own right, but the islands themselves are vital breeding and nurseryareas for animals that are of significant economic value and particular scientific and popular interest- namely seabirds and turtles.Forty-two species of seabirds breed in the Indian Ocean, almost all of these invariably onsmall offshore or oceanic islands. Of these 42, fourteen are endemic to the region (UNEP, 1985);these are:Mascarene petrelPterodroma aterriinaBarau's petrelPterodroma baru'Jouanin's petrelBuiweria fallaxAbbott's boobySula abbottiIndian cormorantPhulacrocorm fuscicollisSocotra cormorantPhulacrocorax nigrogularisJavanese cormorantHalietor nigerChristmas Island frigatebird Fregata andravsiWhite-eyed gullLams leucophthalmusSooty gullLarus hemprichiiWhite-cheeked ternStem repressaSaunder's ternSterna saundersiLesser crested ternSterna bengalensisLesser noddyAnous tenuirostrisIn the Indian Ocean the breeding of all seabirds has become increasingly impacted by man'sactivities, largely by general disturbance and habitat changes (linked to the spread of villages, holidayhomes, navigational and military installations to offshore islands), by accidental introduction ofpredators (e.g. cats and rats), and also by egg collection and taking of chicks. In the past eggs havebeen collected in small quantities by fishermen and coastal villages, and generally in a sustainablemanner; but in recent years, as a result of human population expansion and the increase in range ofmotorised fishing craft, taking of eggs and chicks has greatly intensified. The Pelicaniformes(boobies, frigatebirds, etc.) appear to have been most affected and to be in serious decline: They andtheir young are taken for food; they are especially vulnerable to human disturbance because gulls taketheir eggs when they leave the nest; and they have been excluded either by the destruction of trees usedfor nesting, or by the planting of previously treeless islands with coconuts. In Indonesia (DEKORTE, 1983) and in the centraVwestern Indian Ocean (FEARE, 1984), many islands that supportedbreeding colonies earlier in this century now either lack any breeding birds or support only greatlyreduced numbers.Smalloffshore and oceanic islands also provide important nesting grounds for all five speciesof marine turtles found in the Indian Ocean: the Green turtle (Chelonia mydas), the Hawksbill(Eretmochelys imbricata), the Loggerhead (Caretta caretta), the Leatherback (Dermochefys coriacea),and the Olive Ridley (Lepidochelys olivacea). Of these, the Loggerhead may nest predominantly onmainland beaches, but the others nest frequently, and the Hawksbill almost exclusively, on smallislands. Green and Hawksbill are the most widespread species and are the only ones breeding in180
- Page 124 and 125: Madagascar and the Red Sea. Within
- Page 126 and 127: South Australian Basin: (Figs. 10-1
- Page 128 and 129: Offshore placers are likely to occu
- Page 130 and 131: MILLIMAN, J.D. (1974). Marine Carbo
- Page 132 and 133: Thailand Tin 5560 (1980) NA 4.2 (19
- Page 134 and 135: Table 2. The range (in percent) of
- Page 136 and 137: Table 4. Chemical composition of po
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- Page 148 and 149: IFigure 17. Marine mineral explorat
- Page 150 and 151: central are corals to the integrity
- Page 152 and 153: Very little information is availabl
- Page 154 and 155: leaving little trace of their exist
- Page 156 and 157: REFERENCESAGASSIZ, A. (1903). The c
- Page 158 and 159: PILLAI, C.S.G. (1969b). Studies on
- Page 160 and 161: Table 1.Extent of damage to coral r
- Page 162 and 163: STATUS OF CRITICAL MARINE HABITATS
- Page 164 and 165: OCCURRENCEThe distribution of reefs
- Page 166 and 167: Mining of Reef RockMining of reef r
- Page 168 and 169: -resource. Their significance deriv
- Page 170 and 171: Coating of Aerial Roots by Fine Sed
- Page 172 and 173: associated with the roots (e.g. GOE
- Page 176 and 177: significant numbers in the Red Sea,
- Page 178 and 179: mersas are known to serve as nurser
- Page 180 and 181: BURCHARD, J.E. (1979). Coral fauna
- Page 182 and 183: HIRTH, H.F., KLIKOFF, L.G. and HARP
- Page 184 and 185: MacNAE, W. (1974). Mangrove forests
- Page 186 and 187: RINKEVITCH, B. and LOYA, Y. (1977).
- Page 188 and 189: WALKER, D.I. and ORMOND, R.F.G. (19
- Page 190 and 191: DAMMING AND DIVERSION OF RIVERSIn d
- Page 192 and 193: FUTURE STUDIESWhat can marine scien
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- Page 198 and 199: STORM SURGES IN THE BAY OF BENGAL*T
- Page 200 and 201: low pressure centres over the Bay i
- Page 202 and 203: ACKNOWLEDGEMENTSThe writers wish to
- Page 204 and 205: Table 1.Latitude and longitude of p
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- Page 214 and 215: 221
- Page 216 and 217: Table 3. Nomenclature used by India
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environmental stress, and subsequent loss of Zostera beds in <strong>Japan</strong> was linked to industrialisation andincreasing water pollution along the coast (NAIKAI REG. FISH. RES. LAB., 1967; NASEI REG.FISH. RES. LAB., 1974).SMALL ISLANDSOTHER CRITICAL HABITATSSmall islands, offshore of the mainland coast or oceanic islands in deeper water, are numerousin many parts of the Indian Ocean. For example there are 200 or more small coral cays and islandsalong the eastern seaboard of the Red Sea alone. Island groups of the Indian Ocean, the Maldives,Seychelles, Lakshadweep, Nocibars and Andamans, include many small coralline or volcanic islets,besides the larger islands that support human population.The smaller islands constitute significant critical habitats. Not only are they generallysurrounded by shallow water marine habitats, coral reefs, seagrass beds and mangrove stands, whichare considered critical in their own right, but the islands themselves are vital breeding and nurseryareas for animals that are of significant economic value and particular scientific and popular interest- namely seabirds and turtles.Forty-two species of seabirds breed in the Indian Ocean, almost all of these invariably onsmall offshore or oceanic islands. Of these 42, fourteen are endemic to the region (UNEP, 1985);these are:Mascarene petrelPterodroma aterriinaBarau's petrelPterodroma baru'Jouanin's petrelBuiweria fallaxAbbott's boobySula abbottiIndian cormorantPhulacrocorm fuscicollisSocotra cormorantPhulacrocorax nigrogularisJavanese cormorantHalietor nigerChristmas Island frigatebird Fregata andravsiWhite-eyed gullLams leucophthalmusSooty gullLarus hemprichiiWhite-cheeked ternStem repressaSaunder's ternSterna saundersiLesser crested ternSterna bengalensisLesser noddyAnous tenuirostrisIn the Indian Ocean the breeding of all seabirds has become increasingly impacted by man'sactivities, largely by general disturbance and habitat changes (linked to the spread of villages, holidayhomes, navigational and military installations to offshore islands), by accidental introduction ofpredators (e.g. cats and rats), and also by egg collection and taking of chicks. In the past eggs havebeen collected in small quantities by fishermen and coastal villages, and generally in a sustainablemanner; but in recent years, as a result of human population expansion and the increase in range ofmotorised fishing craft, taking of eggs and chicks has greatly intensified. The Pelicaniformes(boobies, frigatebirds, etc.) appear to have been most affected and to be in serious decline: They andtheir young are taken for food; they are especially vulnerable to human disturbance because gulls taketheir eggs when they leave the nest; and they have been excluded either by the destruction of trees usedfor nesting, or by the planting of previously treeless islands with coconuts. In Indonesia (DEKORTE, 1983) and in the centraVwestern Indian Ocean (FEARE, 1984), many islands that supportedbreeding colonies earlier in this century now either lack any breeding birds or support only greatlyreduced numbers.Smalloffshore and oceanic islands also provide important nesting grounds for all five speciesof marine turtles found in the Indian Ocean: the Green turtle (Chelonia mydas), the Hawksbill(Eretmochelys imbricata), the Loggerhead (Caretta caretta), the Leatherback (Dermochefys coriacea),and the Olive Ridley (Lepidochelys olivacea). Of these, the Loggerhead may nest predominantly onmainland beaches, but the others nest frequently, and the Hawksbill almost exclusively, on smallislands. Green and Hawksbill are the most widespread species and are the only ones breeding in180