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综合分析和研究了采自布兰斯菲尔德海峡主体海槽中ＰＣ１０孔（７５３ｃｍ长）的全部室内外资料：岩芯、粒度特征、矿物组分、生物尸体群和年代学等，指出了整个岩芯柱代表了区内１１２．５ｋａ以来冰－海环境的沉积。沉积作用包括生物硅质沉积，火山碎屑沉积和浊流沉积等。其中生物硅质沉积作用，不论在高水位／间冰期或低水位／冰期均占主导地位，不同的是低水位／冰期沉积物中陆源碎屑物含量低且矿物成分和岩屑成分较单一，而高水位／间冰期则相反，且前者沉积速率低于后一时期，这一沉积特点与中低纬度情况有所不同
A comprehensive analysis and study of all indoor and outdoor data collected from PC10 wells (753 cm long) in the main channel of the Bransfield Strait: core, grain size characteristics, mineralogical composition, biological cadaver and chronology, The stem represents the deposition of the ice-sea environment since 112.5 ka in the area. Sedimentations include biosilica deposition, volcaniclastic sedimentation and turbidite deposition. Among them, biosilica sedimentation plays a dominant role in both high water level / interglacial period or low water level / ice age, except that the content of terrestrial detrital substances in low water level / glacial sediments is low and the composition of mineral components and cuttings are relatively single, While the high water level / interglacial period is the opposite, and the deposition rate of the former is lower than that of the latter period. The depositional characteristics are different from those in the middle and low latitudes