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Chapter I Intro & Objectives - SPREP

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PHOENIX ISLANDS PROTECTED AREA MANAGEMENT PLAN<br />

<strong>Chapter</strong> III. Background, 1. Physical Setting of the Islands<br />

Draft 1 March 2007<br />

zero. Most of the carbon produced remained in the lagoon. Phosphorus utilization in<br />

Abariringa’s (Canton’s) lagoon was estimated at 0.027 m moles m -2 day -1 (Smith and Jokiel<br />

1978). Nitrogen utilization was 8.5 higher. Net excess organic carbon production was<br />

estimated to be about 3 m moles m -2 day -1 , or 35 mg C m -2 day -1 . Gross carbon production<br />

was estimated to be 6 g C m -2 day -1 . CaCO3 production was estimated to be 13 m moles m -2<br />

day -1 , or 1.4 g CaCO3 m -2 day -1 .<br />

Jokiel and Maragos (1978) analyzed sediment composition and water quality in Abariringa’s<br />

(Canton’s) lagoon, based on distance from the lagoon passage. Results are provided here in<br />

Tables III-1.2 and III-1.3. Sediment closer to the lagoon passage had hard substrata or larger<br />

median grain size, while sediments far from the lagoon passage consisted of calcareous mud<br />

(smaller median grain size).<br />

Table III-1.2. Sediment composition in Abariringa’s (Canton’s) lagoon<br />

(source: Jokiel and Maragos 1978).<br />

Table III-1.3. Water quality in Abariringa’s (Canton’s) lagoon.<br />

(source: Jokiel and Maragos 1978).<br />

3

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