1) penultimate deglaciation
倒数第二次冰消期
1.
7‰ was discovered in a planktonic foraminifera of the penultimate deglaciation age from core NS93-5 in the South China Sea.
南海地区NS93- 5柱样在倒数第二次冰消期出现浮游有孔虫壳体δ13C值快速负偏 (幅度达 1 。
3) Penultimate interglacial
倒数第二次间冰期
1.
The global tendency and regional characteristic of palaeoclimate change were received through comparing the paleovegetation and paleoclimate among Luochuan and other places profile during the Penultimate interglacial.
本文选取洛川地区黑木沟剖面S2地层为研究对象,以高分辨率的孢粉资料分析,重建S2时期的植被发展演化序列,进而推断其气候演化规律;同时测定剖面的磁化率与粒度,来揭示这一阶段冬夏季风的进退规律,从而揭示我国干旱、半干旱区在S2时期古气候演化规律;将不同指标所揭示的气候规律进行对比,验证孢粉研究方法在古气候恢复中的可信度;另外将倒数第二次间冰期阶段洛川地区古植被、古气候变化规律与其它地区揭示的气候变化规律进行比较,得出S2时期气候变化的全球性趋势与存在的区域性特点。
5) penultimate stage
次末级，倒数第二级
6) last deglaciation
末次冰消期
1.
Paleoenvironmental Evolution in the Inner Shelf of the East China Sea Since the Last Deglaciation
末次冰消期以来东海内陆架古环境演化
2.
A typical borehole P5 was examined for lithology, dating, spore-pollen and microfossil to reveal the phases of climate and sea level fluctuation and the associated sedimentary facies recorded in the paleo-incised valley sediments in the southeastern Changjiang Delta Plain since the last deglaciation.
利用典型钻孔P5孔沉积物的岩性、测年、孢粉和有孔虫的分析结果,探讨了末次冰消期以来长江三角洲东南部古河谷区记录的气候波动和海平面阶段性上升过程及其控制下的古河谷沉积模式。
3.
The rapid climatic changes occurred at the northwest margin of East Asia monsoon region during the last deglaciation were divided into six climatic periods, namely Oldest Dryas, Exiling, Older Dryas, Allerd, IACP and Young Dryas periods.
通过对中卫剖面和米浪沟湾剖面的年代学与高分辨率气候地层记录的研究,认为末次冰消期东亚季风区西北缘发生气候快速变化事件,它可分辨出古仙女木、波令、老仙女木、阿勒鲁德、IACP 和新仙女木等6个气候阶段,并可与格陵兰冰心(GISP2)检出的6个气候阶段相对比。
补充资料：冰消
1.亦作"冰销"。 2.冰冻消融。 3.比喻事物消释涣解。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条