李文宝, 王汝建. 近100 Ma以来海平面变化机制[J]. 海洋地质与第四纪地质, 2014, 34(1): 117-127. DOI: 10.3724/SP.J.1140.2014.01117
引用本文: 李文宝, 王汝建. 近100 Ma以来海平面变化机制[J]. 海洋地质与第四纪地质, 2014, 34(1): 117-127. DOI: 10.3724/SP.J.1140.2014.01117
LI Wenbao, WANG Rujian. RESEARCH OF THE MECHANISM OF SEA LEVEL CHANGE DURING THE LAST 100 MA[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 117-127. DOI: 10.3724/SP.J.1140.2014.01117
Citation: LI Wenbao, WANG Rujian. RESEARCH OF THE MECHANISM OF SEA LEVEL CHANGE DURING THE LAST 100 MA[J]. Marine Geology & Quaternary Geology, 2014, 34(1): 117-127. DOI: 10.3724/SP.J.1140.2014.01117

近100 Ma以来海平面变化机制

RESEARCH OF THE MECHANISM OF SEA LEVEL CHANGE DURING THE LAST 100 MA

  • 摘要: 海平面变化不仅关系到全球环境的演变,而且与人类社会的发展有着极其密切的关系。关于海平面变化的机制研究与精确估算则一直以来是海洋学研究的重点方向之一。通过分析晚中生代以来全球海平面变化记录,在行星尺度和地球轨道尺度上,分析讨论了海平面变化的主要影响机制。结果显示:虽然近100 Ma以来,海平面记录中构造和大洋碳储库周期连续小波分析信号显著,其滤波振幅强度变化也对应了全球性的构造、气候及生物演变事件,反映了由构造运动引起的海-陆格局变化、气候突变以及相应的生物演变事件等全球性变化对海平面变化的影响。但在南极冰盖形成之后,构造周期与大洋碳储库周期的影响对海平面变化的影响出现不同,特别是近5 Ma以来两者出现相反的变化趋势;近10 Ma以来,偏心率周期、斜率周期和岁差周期分别在约0.8、5.3及6.2 Ma之后对海平面变化的影响开始增强,显示出不同地球轨道参数周期对海平面变化影响存在一定的时间差异。而在这一阶段,虽然极地冰盖体积变化与海平面变化的相关性最为显著,但是,海平面变化可能受到地球轨道参数变化引起的高纬度地区冰盖体积变化与低纬度季风演化引起的大洋碳储库变化等因素的共同影响。

     

    Abstract: The development of human society and evolution of the global environment is influenced markedly by sea level change (SLC). So it is important to know the mechanism and its primarily driving factors of the SLC. To this end, based on the reconstructed record of the SLC during the last 100 Ma, the mechanism of the SLC responding to the tectonically variations and the orbit cycles had been researched. During the last 100 Ma, the signal of 1 Ma tectonically period and 0.4~0.5 Ma oceanic carbon reservoir cycle were obvious, and the change in amplitude intensity of the 1 Ma tectonically period and 0.4~0.5 Ma oceanic carbon reservoir cycle responded well to the global tectonics, climate and biological evolution events. That is to say that the long-term eustatic changes had been influenced by the tectonically controlled sea-land distribution, changing of the global climate and biological events at the Planetary-scale period. Here, we should pay attention to that the effect of 1 Ma tectonically period had become weaker and weaker and 0.4~0.5 Ma oceanic carbon cycle become stronger and stronger after the appearance of south polar ice sheet, especially since the last 5 Ma. On the other hand, the orbit cycles, such as 100 ka eccentricity period, 40 ka obliquity period and 23 ka (and 19 ka) precession period, had different effect on the SLC. For example, these three periods had increased impact on SLC since about 0.8 Ma, 5.3 Ma and 6.2 Ma, respectively. Otherwise, the SLC and δ18OBenthic have very high coherency at orbital cycles, which show that the SLC was influenced directly by ice volume change during the last 10 Ma. Anyway, the SLC is not only influenced by the ice volume change in high-latitude area, but also affected by the evolution of the monsoon and the change in oceanic carbon reservoir cycle in low-latitude area.

     

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