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研究证实了中更新世微玻陨石层位于布容/松山(B/M)界线之下, 并根据南海ODP772A, 17957和17959柱状样同位素和古地磁资料推算的沉积速率, 计算出深海中更新世微玻陨石层的年龄早于B/M界线, 约为10～12 ka. 而黄土剖面中的中更新世微玻陨石层却位于B/M实测界线之上, 这是由于黄土中的B/M实测界线已向下偏离其真实位置所造成, 反映了古地磁极性事件在黄土剖面中记录的复杂性, 同时也增加了海-陆地层对比的难度.
The study confirms that the Middle Pleistocene microlite glass layer is located beneath the BJM boundary and the Pleistocene Pleistocene sediments are calculated according to the sedimentary rates derived from the pillar-like isotopes and paleomagnetic data of ODPs772A, 17957 and 17959 in the South China Sea The age of the microlite glass layer is earlier than the B / M boundary, which is about 10 ~ 12 ka, while the middle Pleistocene microlite glass layer in the loess section is above the B / M measured boundary due to the B / M measured boundaries have been deviated downward from its true position caused by the reflection of paleomagnetic events in the loess section of the complexity of the record, but also increase the difficulty of sea-land strata comparison.