But, low sedimentary rate in many profiles, especially in S1, and following strong pedogenesis and eluviation would have effect on those climate records.

 
  • 然而,黄土高原中部大多数剖面由于沉积速率较低(特别是S1地层),加上后期强烈的成壤作用和淋溶作用可能影响其气候记录。
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