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This paper presents depth variations of dissolved O 2 , ΣCO 2 , alkalinity, and δ 13 C of ΣCO 2 in seawater off eastern Taiwan. The observed depth distributions of O 2 , ΣCO 2 , alkalinity and δ 13 C of ΣCO 2 are generally similar to those reported in the open ocean and can be attributed to O 2 utilization and CO ...
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