Sea salt sulfate in the upper part of sediment column was dominantly reduced by AOM, and the remained sulfate involving reduction would probably cause positive sulfur isotopic excursion of pyrites.

 
  • 海水源為主的硫酸鹽參與了沉積物上部的AOM過(guò)程,黃鐵礦硫穩定同位素正偏的原因可能與較強的AOM作用和較多的殘余硫酸鹽參與有關(guān)。
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