The distribution of Pacific Ocean tuna populationsappears to change during the years when El Niño isin effect (Hunt 2002). This change in distribution islikely a result of changes in tuna prey such as krill. Inan El Niño year the pressure gradient between theeast <strong>and</strong> west Pacific Ocean lessens <strong>and</strong> thereforecauses the equatorial waters of the Central <strong>and</strong>Western Pacific to become cooler. Lehodey (2001)note that tuna catches are highest in the westernequatorial Pacific warm pool but can be displaced byas much as 50° of longitude eastward (which mayalter the jurisdiction of these catches from nationalwaters to the high seas) during El Niño episodes.During La Niña years when the westerly trades blowmore strongly, tuna catches tend to move westward(Hunt 2002). These changes in the marine ecosystemobviously have both direct <strong>and</strong> run-on effects tocetacean populations in the region.Decline in the health of coral reef systems in areasof the Pacific Ocean has also raised serious concerns(Crosby et al. 2002, Hoegh-Guldberg et al. 2000).Notably, the reduction of calcification rates coupledwith higher sea temperatures has intensified coralbleaching events. Many are particularly concernedabout the implications of changes in ocean pHresulting from increased atmospheric carbon dioxide,or ocean acidification (Pörtner et al. 2004, Basset al. 2006). An increase in CO 2concentrationwill act to reduce the availability of carbonatesnecessary for the growth of corals <strong>and</strong> molluscs.The physiological effects are also implicated toadversely influence the metabolic function insensitive creatures such as the ommastrephid squid(Pörtner et al. 2004). Increases in atmospheric CO2concentrations due to greenhouse gas emissions arepartly to blame (Hunt 2002), although it has beennoted that coral degradation is most aggravatedin urban areas (Hoegh-Guldberg et al. 2000).Additional factors contributing to coral habitatdecline include: soil erosion <strong>and</strong> sedimentation ofvolcanic <strong>isl<strong>and</strong>s</strong>, coastal construction, sewage <strong>and</strong>industrial discharges, overfishing of subsistenceresources <strong>and</strong> excessive commercial exploitation ofother fisheries, increased flooding <strong>and</strong> discharge offertilizers <strong>and</strong> toxic chemicals, <strong>and</strong> destructive fishingtechniques, especially explosives. In addition, thecorals themselves are being extracted for the marineaquarium <strong>and</strong> curio trade (Lovell <strong>and</strong> Tumuri 1999).In response to these imminent ecological problemsmany monitoring programs have been established inlocations including American Samoa (Craig <strong>and</strong> Basch2001), <strong>and</strong> Fiji (Harborne et al. 2001). It is probablethat fish production will suffer as these reef habitatscontinue to be degraded or are lost (Hunt 2002).Once again the impact on the surrounding marineecosystem is undetermined.The Antarctic is the feeding ground of many ofthe great whale species that migrate to the PacificIsl<strong>and</strong>s Region during their breeding season inthe austral winter, however, these ecosystems arealso undergoing significant changes as a result ofglobal warming (Moline et al. 2004). Clapham et al.(1999) note that the blue whales’ nearly exclusivedependence upon euphausiids, especially krill(Euphausia superba) in the Antarctic, could make bluewhales vulnerable to large-scale changes in oceanproductivity. Specifically, if the extent of sea icedecreases larval krill may not be able to endure theextended periods in which they do not have accessto under-ice algae for feeding. Accordingly, krillabundance has decreased in the northern westernAntarctic Peninsula during the last decade (Fraser<strong>and</strong> Hofmann 2003). Glacial melt-water runoff <strong>and</strong>reduced surface water salinities have also resultedin shifts in phytoplankton community structurealong the Antarctic Peninsula (Moline et al. 2004).Changes in the spatial <strong>and</strong> temporal distribution<strong>and</strong> abundance of krill will have severe implicationsfor marine species such as baleen whales that relyon krill as their main prey, or are important in theirrespective food webs.The fate of cetaceans as a result of climate change islargely speculative, but the Intergovernmental Panelon Climate Change (IPCC) (2001) asserts that: “Wildspecies have three possible responses to climatechange: (i) change geographical distribution to trackenvironmental changes; (ii) remain in the same20 CURRENT STATE OF KNOWLEDGE OF CETACEAN THREATS, DIVERSITY, AND HABITATS IN THE PACIFIC ISLANDS REGION
place but change to match the new environment,through either plastic response, such as shifts inphenology (for example timing of growth, breedingetc.), or, genetic response, such as an increase inthe proportion of heat tolerant individuals; or (iii)extinction.” It is therefore critical that projectedimpacts of climate change are taken into accountwhen addressing conservation <strong>and</strong> managementplans for cetaceans (Simmonds <strong>and</strong> Isaac In press).Chemical pollution <strong>and</strong> diseaseBetween June 1946 <strong>and</strong> October 1958, the Enewetak<strong>and</strong> Bikini Atolls of the Marshall Isl<strong>and</strong>s were usedas testing grounds for 66 nuclear devices (Reeveset al. 1999). This testing produced close-in falloutdebris that was contaminated with quantities ofradioactive fission <strong>and</strong> particle activated products,<strong>and</strong> unspent radioactive nuclear fuel that enteredthe aquatic environment of the atolls (Robinson etal. 1998). Today, the sediments in the lagoons arereservoirs for transuranics <strong>and</strong> some long-lived fission<strong>and</strong> activation products, although the larger amountsof contamination are associated with fine <strong>and</strong>coarse sediment material adjacent to the locationsof the high yield explosions. Radionuclides are alsodistributed vertically in the sediment column tovarious depths in all regions of the lagoons (Robinsonet al. 1998). Concentrations greater than falloutbackground levels are found in filtered water sampledover several decades from all locations <strong>and</strong> depthsin the lagoons. Of particular importance is the factthat the long-lived radionuclides are accumulatedto different levels by indigenous aquatic plants <strong>and</strong>organisms that are used as food by resident people<strong>and</strong> quite possibly animals. Various isotopes ofplutonium have been found in reef fish includingmullet, convict surgeonfish <strong>and</strong> goatfish (Robinsonet al. 1998, Noshkin et al.1998). The resultant longtermimplications for the marine ecosystems <strong>and</strong>marine mammals in this area are unknown.A comprehensive study of water quality of theU.S. Pacific Isl<strong>and</strong> territories revealed levels ofcontaminants in vacation beaches that have causedmany beach closures (Dorfman 2004). Examplesfrom Guam beaches indicate elevated levels ofenterococcus while estuarine areas are subject toorganic enrichment, pathogens, increased salinity<strong>and</strong> nutrients, <strong>and</strong> high pH from municipal pointsources <strong>and</strong> urban runoff. Information fromNorthern Mariana beaches indicates that runoff, <strong>and</strong>,faulty septic <strong>and</strong> sewage systems are part of thereason for beach-water contamination. In addition,sedimentation from unpaved roads <strong>and</strong> development,stormwater <strong>and</strong> urban runoff, reverse osmosisdischarges, <strong>and</strong> nutrients from golf courses <strong>and</strong>agriculture were cited as problematic in this area. Inaddition, l<strong>and</strong>fills are believed to leach metals <strong>and</strong>synthetic organic compounds (Dorfman 2004).High nutrient levels of phosphate <strong>and</strong> nitrate havebeen noted proximal to human activities alongthe Coral Coast of Vitu Levu in Fiji (Mosley <strong>and</strong>Aalsbersberg 2003) in quantities believed to beharmful to coral reef ecosystems. Coupled withoverfishing of herbivore species these elevatednutrient levels are believed to be a contributor to therecent widespread growth of macro-algae speciesalong this coast. The authors noted that nutrientlevels were highest at sites located near hotels <strong>and</strong>other populated sites (Mosley <strong>and</strong> Aalsbersberg 2003).Mining operations in the Pacific Isl<strong>and</strong>s Regionpresently (or have historically) exist in Papua NewGuinea, Fiji, Nauru, Solomon Isl<strong>and</strong>s <strong>and</strong>, NewCaledonia <strong>and</strong> are feared to be placing a heavyenvironmental toll on the l<strong>and</strong>scape (SPREP 2004).Dumping of mine tailings into submarine canyonsoccurs very close to the Pacific Isl<strong>and</strong>s Region.Of concern is that several large mines in nearbySulawesi, Indonesia dispose of their tailings in deepocean canyons known to support populations ofsperm whales <strong>and</strong> various beaked whales (Kahn2000). In addition to point-source pollution, theatmospheric transport of contaminants from theseoperations also represents a danger.The input of such toxins into the marine environmentlikely has grave consequences for cetaceans. ACURRENT STATE OF KNOWLEDGE OF CETACEAN THREATS, DIVERSITY, AND HABITATS IN THE PACIFIC ISLANDS REGION 21
- Page 1 and 2: Current State of Knowledge ofCetace
- Page 3: Current State of Knowledge of Cetac
- Page 7 and 8: Chapter 4: Cetacean checklists by c
- Page 9 and 10: Executive SummaryThis report provid
- Page 12 and 13: The limited land base of the 22 Pac
- Page 14 and 15: “Pacific Island Countries and Ter
- Page 16 and 17: Land degradationDue to the limited
- Page 18 and 19: identified as marine and coastal ec
- Page 22 and 23: ecent global survey of toxicity lev
- Page 24 and 25: and Orams 2005). Hector’s dolphin
- Page 26 and 27: pilot whale (4), sperm whale (2), s
- Page 28 and 29: al. 2003). In January 2004 a humpba
- Page 30 and 31: Stranded Cuvier’s beaked whale, A
- Page 32 and 33: Reeves et al. (1999) also refer to
- Page 34 and 35: “... the limited research efforts
- Page 36 and 37: were made to ensure that classifica
- Page 38 and 39: Scientific NameCommon NameBalaenopt
- Page 40 and 41: their presence in the region. Distr
- Page 42 and 43: Over the austral summer of 1998-199
- Page 44 and 45: 7. KiribatiLand Area (km 2 ): 811Se
- Page 46 and 47: Scientific NameCommon NameBalaenopt
- Page 48 and 49: Scientific NameCommon NameBalaenopt
- Page 50 and 51: Northern Marianas Islands (D. Johns
- Page 52 and 53: Scientific NameCommon NameBalaenopt
- Page 54 and 55: within the Pitcairn group reported
- Page 56 and 57: short-finned pilot whales have been
- Page 58 and 59: Scientific NameCommon NameBalaenopt
- Page 60 and 61: Scientific NameCommon NameMegaptera
- Page 62 and 63: Table 1American SamoaCook IslandsFe
- Page 64 and 65: “The diverse and expansive Pacifi
- Page 66 and 67: feeding occurs in summer to warmer,
- Page 68 and 69: ID: At sea identification between l
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FAMILY PhocoenidaePhocoena dioptric
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“... the subtleties and extent of
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Palumbi. 1993. Abundant mitochondri
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Coan, A. L., G. T. Sakagawa, D. Pre
- Page 78 and 79:
Forestell, P.H. and G. D. Kaufman.
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Halliday I., J. Ley, A. Tobin, R. G
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grouping and population structure.
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Moller, L. M. and R. G. Harcourt. 1
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Paterson, R., P. Paterson and D. H.
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Samuels, A., L. Bejder and S. Heinr
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Trianni, M. S. and C. C. Kessler. 2
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“The conservation status of amigr
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TAXONVERNACULAR NAMESUBORDER ODONTO
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taxon, threatened status may well b
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WDCS CMS ProgrammeCoordinating Offi