碳酸盐岩沉积物，特别是生物礁，只有在现代海洋动物群落和植物群落生态学详细资料的帮助下才能获得有益的研究成果。
Carbonate sediments, in general, and reefs, in particular, can only be studied profitably with the aid of a detailed knowledge of the ecology of modern Marine fauna and flora.
碳酸盐岩沉积物，特别是生物礁，只有在现代海洋动物群落和植物群落生态学详细资料的帮助下才能获得有益的研究成果。
Carbonate sediments, in general, and reefs, in particular, can only be studied profitably with the aid of a detailed knowledge of the ecology of modem Marine fauna and flora.
海洋风尘沉积是一门海洋沉积学、古气候学、古海洋学的交叉学科，它在古气候、古环境和现代环境研究方面均具有重要意义。
Marine eolian deposition is a cross subject among Marine sedimentation, paleoclimate and paleoceanography, and it's important in the research of paleoclimate, paleoenvironment and modern environment.
海洋风尘沉积是一门海洋沉积学、古气候学、古海洋学的交叉学科，它在古气候、古环境和现代环境研究方面均具有重要意义。
Marine eolian deposition is a cross subject among Marine sedimentation, paleoclimate and paleoceanography, and its important in the research of paleoclimate, paleoenvironment and modern environment.
海洋风尘沉积是一门海洋沉积学、古气候学、古海洋学的交叉学科，它在古气候、古环境和现代环境研究方面均具有重要意义。
Marine eolian deposition is a cross subject among Marine sedimentation, paleoclimate and paleoceanography, and its important in the research of paleoclimate, paleoenvironment and modern environment.
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