Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere glaciation
Oxygen isotope and palaeomagnetic evidence for early Northern Hemisphere glaciation
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DOI：
10.1038/270216a0
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发表时间：
1977-11
期刊：
影响因子：
64.8
通讯作者：
N. Shackleton;N. Opdyke
中科院分区：
文献类型：
--
作者：
N. Shackleton;N. Opdyke
对LDGO活塞芯V28-179下半部分的氧同位素和古地磁分析表明，冰川-间冰期波动是过去320万年地球气候的特征，在此之前有一段稳定的“间冰期”或“前冰期”气候。冰川的规模在250万年前增加。
Oxygen isotope and palaeomagnetic analysis of the lower half of LDGO piston core V28–179 shows that glacial–interglacial fluctuations have characterised Earth's climate for the past 3.2 Myr, before which there was a period of stable ‘interglacial’ or ‘preglacial’ climate. The scale of glaciations increased about 2.5 Myr ago.