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Nomination for a World Heritage Site 2009 - Phoenix Islands ...

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Jamie Gove in Maragos et al (2008) provided a sketch of the equatorial current system in the<br />

central Pacific shown in the figure below. The <strong>Phoenix</strong> <strong>Islands</strong> were in an area of unique<br />

subsurface water currents. This may have great significance <strong>for</strong> dispersing larvae originating<br />

from the <strong>Phoenix</strong> <strong>Islands</strong>.<br />

Sketch of equatorial current system in the central Pacific Ocean (170 0 W) including the Equatorial Intermediate<br />

Current (EIC), the North and South Subsurface Countercurrents (NSCC and SECC). (Source: Maragos et al<br />

Coral Reefs of the USA, 2008). Cross-sectional sketch of the equatorial current system in the central Pacific<br />

Ocean (170° W). Shown in crosshatch are the North and South Equatorial Countercurrent (NECC and SECC),<br />

subsurface Equatorial Intermediate Current (EIC), North and South Subsurface Countercurrents (NSCC and<br />

SSCC), and Equatorial Undercurrent (EUC ). Eastward flow is colored green or brown, and all westward flow is<br />

white, including the North Equatorial Current (NEC) north of 5° N and the South Equatorial current (SEC )<br />

south of 5° N and outside the EIC. Black numbers in italics were observations from January 1984 to June 1986<br />

(latitude 165° E), and bold red numbers were observations from April 1979 to March 1980 (latitude 155° W),<br />

with both representing transports in Sverdrups (Sv = 106 m3/s) (Modified from Tomczak and Godfrey (2003).<br />

MARINE ECOSYSTEMS<br />

The marine environment of the PIPA is extremely diverse. It varies from the spectacular<br />

turquoise lagoons with huge coral heads and clams to pristine and colorful coral reefs that<br />

<strong>for</strong>m and surround the atoll, low reef islands and submerged reefs down the slopes of the<br />

massive volcanoes to the ocean floor to over 6,000 meters deep. The marine environment of<br />

the PIPA is known to support a number of globally endangered and endemic species and<br />

hosts interesting and unique species assemblages not found elsewhere in the world.<br />

From a marine science perspective the PIPA is extremely important because of the minimal<br />

human impacts and hence it’s near pristine state. In addition PIPA is biogeographically<br />

uniquely situated in the center of the equatorial Pacific. PIPA plays a significant role in<br />

movements and dispersal of marine animals and larvae. Little is still known about the full<br />

effect of these islands on the surrounding pelagic marine species and systems, which in turn<br />

support internationally important seabird populations and numerous migratory birds.<br />

Signs (prolific algae growth) of unusually high nutrient levels <strong>for</strong> oceanic atolls have been<br />

observed in the <strong>Phoenix</strong> <strong>Islands</strong>. This effect could be caused by a combination of lagoon<br />

enrichment, leaching of guano deposits or oceanic upwelling caused by deep currents striking<br />

the massive seamounts underlying each of the <strong>Phoenix</strong> <strong>Islands</strong>. Pierce et al (2006) suggested<br />

35

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