末次间冰期（氧同位素５ｅ亚期）两次高海平面的新证据Ｃ．Ｅ．Ｓｈｅｒｍａｎ等解释晚更新世海平面变化的两个主要出处是：（１）深海沉积物岩心的氧同位素记录，（２）对海相沉积物露头的研究。这两种解释都需要根据说明某些问题的以前海平面做出一些假设，因此，对海平... New evidence of two high sea levels in the last interglacial (oxygen isotope 5e). E. Sherman et al. Explain two main sources of late Pleistocene sea level changes: (1) oxygen isotope records of deep-sea sediment cores, and (2) studies of marine sediment outcrops. Both interpretations need to make some assumptions based on previous sea levels that account for some issues, and therefore, for sea level ...