中文摘要：

晚新生代地球环境演化的重要事件包括冰期气候和人类起源等,其中,冰期及其旋回问题受到广泛关注,但迄今没有被广泛接受的理论解释.地球构造活动诱发的地表风化强度和大洋环流变化,改变了大气CO2含量和地表热量传输过程,其与地球运动轨道变化调制的太阳辐射量变化周期,包括地球轨道偏心率、黄赤夹角和岁差等,共同驱动了第四纪大冰期降临及旋回变化.其中,太阳辐射量变化起主导作用.在包括海陆配置、大气CO2、洋流变化、岩石风化等达到临界点的背景下,太阳辐射量变化驱动着第四纪冰期气候旋回变化.在晚上新世,由于地表化学风化加强、深海沉积埋藏碳增多,使得大气中CO2含量减少,温室气体效应减弱;加上高纬地区接受太阳辐射量降到临界值,高纬地区冰川发育并形成强大的反馈机制,北半球冰期来临并在之后发生了中更新世冰期气候转型.在上新世-更新世的古气候变化中,存在~400,100,41和23ka等周期,这是太阳辐射量变化驱动的结果;其中,大气CO2和冰冻圈反馈起到重要的放大作用.近200年以来,人类急剧向大气中排放CO2气体,增强了温室气体效应,可能改变冰期气候的趋向.

英文摘要：

For more than a century, two families of ice age theories have been proposed： insolation based theories proposed by Adhémar, and atmospheric CO2 ones proposed by Tyndall. The major technique advance of deep-sea sediment drilling, as well as new interpretations of stable oxygen isotopic composition of the deep-sea fossil foraminifera, which is regarded as a proxy index of continental ice volume and sea water temperature, established the now well recognized glacial-interglacial variations in climate over the late Pliocene and Pleistocene, e.g. ~3 Ma. A landmark progress came from Hays et al.（1976） who unambiguously demonstrated that the change in insolation induced by the Earth＇s axial tilt（obliquity）, the wobble of this tilt（precession）, and the degree of circularity of the Earth＇s orbit around the sun（eccentricity） brings on ice ages（glaciations） every hundred thousand years or so during the Pleistocene. Many subsequent observations, from the deep-sea to continental records, confirmed the co-variation between insolation and the alternation of glacial ice age phases, and warmer interglacial phases, at least in terms of frequency domains. However, these findings cannot explain the so called ~100 ka conundrum, where the size of 100 ka insolation forcing is relatively small yet the apparent ice sheet response is large, as well as the bi-polar symmetry in climate changes at precessional frequency of ~23 ka, despite the fact that the precession cycle drives insolation changes in antiphase between the two hemispheres. As such, other factors may be considered in the driving of Northern Hemisphere Glaciation（NHG） global glacial-interglacial variations. Several hypotheses have been put forward, such as：（1） the gradual decreasing CO2 drove global cooling through to a threshold value where insolation changes may force the ice age cycles;（2） the effect of local insolation that modulated the East Antarctica Ice Sheet after the gradual CO2 decline that drove its growth to maximal extent;