在南海北部陆架，这一孢粉组合可与WS1-3-1井流沙港组三段孢粉组合对比，时代为早始新世。
On the northern shelf of South China Sea, the latter assemblage can only be compared with the third member of Liushagang Formation in the WS1-3-1 well, Beibu Gulf Basin.
在南海北部陆架，这一孢粉组合可与WS1-3-1井流沙港组三段孢粉组合对比，时代为早始新世。
On the northern shelf of South China Sea, the latter assemblage can only be compared with the third member of Liushagang Formation in the WS1-3-1 well, Beibu Gulf Basin.
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