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晚上新世全球性海平面波动振幅的控制因素：新西兰浅海沉积记录的新证据ＴｉｍＮａｉｓｈ目前我们对上－更新世全球性海平面变化的认识大部分来自深海气候代替物的记录，特别是来自钙质有孔虫贝壳的氧同位素比值。冰席在陆上形成时，１６Ｏ率先与大陆冰席结合，这个过程使...
GLOBAL SEA-LEVEL FLUCTUATION CONTROL IN THE NEW PALEOZOE: NEW EVIDENCE OF SHALLOW SEA-SHELF RECORD IN NEW ZEALAND TimNaish Much of our understanding of the global-Pleistocene global sea-level changes at the present time comes from the record of deep-sea climatic alternatives, especially from calcareous Oxygen isotope ratio of foraminifer shells. When the ice mat is formed on land, 16O takes the lead in combining with the Chinese ice mat, and this process makes ...