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We describe the first recorded occurrence of oolite in the main Hawaiian Islands. Well-cemented oolite was recovered at several locations at −140 to −150m depth south of Lana'i. The ooids contain foraminiferal, skeletal, and peloidal nuclei, coated by thin to moderately thick (20–50% of ooid radius) tangential cortices, and are cemented by fibrous aragonite needles. The extent of amino acid racemization...
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