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1. The southward migration of the Antarctic Circumpolar Current enhanced oceanic degassing of carbon dioxide during the last two deglaciations

2. The southward migration of the Antarctic Circumpolar Current enhanced oceanic degassing of carbon dioxide during the last two deglaciations

3. Analytical improvements and assessment of long‐term performance of the oxidation–denitrifier method.

4. Preface: Special Issue on Probing the Open Ocean With the Research Sailing Yacht Eugen Seiboldfor Climate Geochemistry

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