冰芯记录 meaning in English

ice core records

Correlation of environmental and climatic change between qaidam basin gamma ray logging curve and guliya ice core 18o record since the last interglacial cycle
柴达木盆地自然伽玛曲线与古里雅冰芯记录的末次间冰期以来气候环境变化过程的对比
The climate of this period is almost as warm and wet as the stage 5e of the last interglacial . the mean temperature is 2 - 4 c higher and the precipitation is much larger than that of the today , the holocene which we live in . while in the climatic records of deep ocean , antarctic and greenland ice - core , marine isotope stage ( mis ) 3 is a weakly warm period , though a little warmer than marine isotope stage ( mis ) 2 and marine isotope stage ( mis ) 4 , evidently colder than the last interglacial and holocene favorable period
末次冰期中期，即深海氧同位素第3阶段的气候在我国，尤其是青藏高原地区表现出明显不同于深海沉积物和极地冰芯记录的特征：青藏高原古里雅冰芯的~ ( 18 ) o曲线表明3阶段存在特强夏季风事件，其气温和降水接近于末次间冰期5e阶段，超过全新世，其暖湿程度已经达到间冰期的程度；而深海氧同位素3阶段在深海、南极、格陵兰冰芯的氧同位素记录中均为弱暖期，虽较2阶段、 4阶段温暖，但显著低于全新世大暖期和末次间冰期。