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Smithsonian at the Poles: Contributions to International Polar

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354 SMITHSONIAN AT THE POLES / RUIZ AND HEWITT<br />

found on such artifi cial substr<strong>at</strong>es (Cohen and Carl<strong>to</strong>n,<br />

1995; Hewitt et al., 2004; Glasby et al., 2007), which<br />

may be especially important focal areas for coloniz<strong>at</strong>ion.<br />

If local export of oil occurs by shipping, this could gre<strong>at</strong>ly<br />

increase <strong>the</strong> scale of port development as well as propagule<br />

supply, as exemplifi ed by oil export from Port Valdez<br />

(see above).<br />

2. The scope of shoreline development, and especially<br />

associ<strong>at</strong>ed habit<strong>at</strong> alter<strong>at</strong>ion and disturbance (as outlined<br />

above), is likely <strong>to</strong> exceed th<strong>at</strong> for commercial shipping<br />

alone. Specifi cally, we expect some level of development <strong>to</strong><br />

support oversight of terri<strong>to</strong>rial jurisdiction among Arctic<br />

countries, shore-based mineral extraction, <strong>to</strong>urism, and<br />

fi sheries. It is diffi cult <strong>to</strong> gauge <strong>the</strong> potential scale of such<br />

development, although it is noteworthy th<strong>at</strong> several countries<br />

have recently increased <strong>the</strong>ir presence in <strong>the</strong> Arctic<br />

(including military and surveying activities) in support<br />

of claims <strong>to</strong> Arctic terri<strong>to</strong>ry and underlying mineral resources.<br />

3. Offshore mineral extraction itself will also cre<strong>at</strong>e<br />

opportunities for increased dispersal of propagules as well<br />

as some disturbance. It is not uncommon <strong>to</strong> use mobile<br />

drilling pl<strong>at</strong>forms for oil explor<strong>at</strong>ion, where <strong>the</strong> pl<strong>at</strong>forms<br />

are <strong>to</strong>wed among sites <strong>at</strong> slow speeds. Although little<br />

studied, this movement can occur over gre<strong>at</strong> distances<br />

(i.e., across ocean basins) and may result in <strong>the</strong> transport<br />

organisms <strong>at</strong> much gre<strong>at</strong>er densities than found on oper<strong>at</strong>ing<br />

ships because (1) <strong>the</strong> pl<strong>at</strong>forms sometimes reside<br />

<strong>at</strong> previous sites for long periods, accumul<strong>at</strong>ing dense assemblages<br />

of organisms, and (2) <strong>the</strong> speed of transport is<br />

rel<strong>at</strong>ively slow, increasing <strong>the</strong> chance th<strong>at</strong> organisms will<br />

remain associ<strong>at</strong>ed. To our knowledge, str<strong>at</strong>egies <strong>to</strong> assess<br />

or <strong>to</strong> reduce <strong>the</strong> associ<strong>at</strong>ed risk of species transfers have<br />

not been explored for mobile drilling pl<strong>at</strong>forms. As with<br />

port development, offshore oil pl<strong>at</strong>forms, when fi xed, cre<strong>at</strong>e<br />

artifi cial (novel) habit<strong>at</strong>s and have some risk of chemical<br />

discharge, and both types of disturbance may affect<br />

susceptibility <strong>to</strong> invasion.<br />

For <strong>the</strong> Antarctic, we do not expect commercial shipping<br />

or shoreline development <strong>to</strong> occur <strong>to</strong> any gre<strong>at</strong> extent,<br />

simply because <strong>the</strong> same economic drivers do not exist<br />

<strong>the</strong>re <strong>at</strong> this point in time. There are not major shipping<br />

routes th<strong>at</strong> would benefi t from transiting near Antarctica,<br />

and access <strong>to</strong> mineral and o<strong>the</strong>r resources is restricted under<br />

<strong>the</strong> Antarctic Tre<strong>at</strong>y System.<br />

The potential exists for fi sheries <strong>to</strong> expand much more<br />

rapidly in <strong>the</strong> Arctic than in <strong>the</strong> Antarctic. This difference<br />

results in large part from access. The Arctic is in rel<strong>at</strong>ively<br />

close proximity <strong>to</strong> current centers of popul<strong>at</strong>ion and human<br />

activity, and a considerable his<strong>to</strong>ry of fi sheries <strong>at</strong> nor<strong>the</strong>rn<br />

high l<strong>at</strong>itudes already exists in <strong>the</strong> Arctic. In contrast, access<br />

<strong>to</strong> fi sheries resources in Sou<strong>the</strong>rn Ocean w<strong>at</strong>ers �60°S<br />

is managed under <strong>the</strong> Antarctic Tre<strong>at</strong>y System, specifi cally<br />

<strong>the</strong> Convention on <strong>the</strong> Conserv<strong>at</strong>ion of Antarctic Marine<br />

Living Resources. It is diffi cult <strong>to</strong> say whe<strong>the</strong>r aquaculture<br />

would occur <strong>to</strong> any extent in high-l<strong>at</strong>itude systems; however,<br />

current aquaculture trends indic<strong>at</strong>e th<strong>at</strong> it is highly<br />

likely. As discussed for commercial shipping, fi sheries activities<br />

can increase <strong>the</strong> levels of propagule supply and disturbance,<br />

with <strong>the</strong> l<strong>at</strong>ter resulting from oper<strong>at</strong>ion of ships<br />

(and discharges), removing pred<strong>at</strong>ors and competi<strong>to</strong>rs, and<br />

cre<strong>at</strong>ing physical disturbance with fi shing gear (especially<br />

bot<strong>to</strong>m trawls; Thrush et al., 1995).<br />

Tourism is already a growing industry <strong>to</strong> both <strong>the</strong> Arctic<br />

and Antarctic, and we expect this trend <strong>to</strong> continue. As<br />

with fi shing, <strong>the</strong> scope for growth appears gre<strong>at</strong>er in <strong>the</strong><br />

Arctic, simply because of distance and access (including<br />

cost). As most <strong>to</strong>urism occurs by ships, <strong>the</strong> potential consequences<br />

for invasions are as outlined previously.<br />

Finally, we predict an increase in <strong>the</strong> quantity of human-derived<br />

fl o<strong>at</strong>ing debris <strong>to</strong> occur in <strong>the</strong> Arctic and<br />

surrounding high l<strong>at</strong>itudes in <strong>the</strong> Nor<strong>the</strong>rn Hemisphere,<br />

coincident with increased levels of shipping, shoreline development,<br />

fi sheries, and <strong>to</strong>urism, as <strong>the</strong>se are all potential<br />

sources for fl o<strong>at</strong>ing debris. While Barnes (2002) reported<br />

rel<strong>at</strong>ively few organisms colonizing fl o<strong>at</strong>ing debris <strong>at</strong> high<br />

l<strong>at</strong>itudes, <strong>the</strong> number may also increase under warmer<br />

temper<strong>at</strong>ures. Fur<strong>the</strong>r, in <strong>the</strong> absence of sea ice in <strong>the</strong> summer,<br />

<strong>the</strong> potential for longer-distance transport of fl o<strong>at</strong>ing<br />

m<strong>at</strong>erial across <strong>the</strong> Arctic exists. Thus, we surmise th<strong>at</strong><br />

fl o<strong>at</strong>ing debris may play an important future role in <strong>the</strong><br />

inocul<strong>at</strong>ion and, especially, regional spread of species in<br />

<strong>the</strong> Arctic, in contrast <strong>to</strong> much smaller changes expected<br />

in <strong>the</strong> Antarctic.<br />

CONCLUSIONS<br />

At <strong>the</strong> present time, very few introduced species are<br />

known from marine ecosystems <strong>at</strong> high l<strong>at</strong>itudes in ei<strong>the</strong>r<br />

hemisphere, especially for polar regions. This low number<br />

most likely results from a combin<strong>at</strong>ion of low propagule<br />

supply of nonn<strong>at</strong>ive species and environmental resistance<br />

<strong>to</strong> invasion due <strong>to</strong> cold w<strong>at</strong>er temper<strong>at</strong>ures and seasonal<br />

fl uctu<strong>at</strong>ions in resources. The rel<strong>at</strong>ive lack of anthropogenic<br />

disturbance may also serve <strong>to</strong> limit invasion opportunity.<br />

With projected increases in temper<strong>at</strong>ure and <strong>the</strong> disappearance<br />

of Arctic sea ice in summer, we should expect<br />

invasions <strong>to</strong> increase as (1) temper<strong>at</strong>ures fall within <strong>the</strong><br />

<strong>the</strong>rmal <strong>to</strong>lerance limits of organisms th<strong>at</strong> are arriving

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