SPATIAL CHARACTER RECONSTRUCTION OF DIFFERENT PERIODS IN OLIGOCENE AND MIOCENE
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摘要: 已有工作对地质环境指标空间分布特征的研究揭示出,我国的环境在新生代期间经历了从近于东西向的带状格局向与现今相似的非带状格局的转变,代表了东亚地区重大的环境变化,但对这一转变的时间、空间变化的详细过程还缺少深入的认识。越来越多的证据显示,渐新世/中新世之交和中新世可能是这一环境变化最为关键的时期,因而有必要对渐新世和中新世内部不同时期的环境格局进行更详细的研究。近十年来,大量新的研究工作积累了更多的资料和证据,为进一步研究上述问题提供了新的可能。文章根据已有文献资料,对有明确环境意义和较可靠年代控制的地质记录进行了重新整理和分类,对渐新世和中新世不同时期的环境格局进行了详细的考察。研究显示,以内陆干旱为基本特征的非带状环境格局至少出现于中新世早期,与我国北方风尘堆积出现的时代具有一致性。Abstract: Previous studies illustrated that the Tertiary paleoenvironmental pattern in China was dominated by roughly zonal climates resulted from the planetary wind systems. Conspicuous changes had occurred for the Neogene when the originally arid south-western and south-eastern part of the country became much more humid and the geographic location of arid region in the north China was further close to the present-day status, indicating the initiation of the East Asian monsoon and inland-type aridity. More geological evidences indicated that the boundary of Oligocene and Miocene was the key time of the change. It is necessary to reconstruct the environmental patterns of different periods in Oligocene and Miocene. Here, we attempt to compile a series of paleogeographical maps based on newly collected climate indicators from the literature and age-controllable evidence of geological maps in order to re-examine the temporal and spatial evolution of climate belts in China during the Oligocene and Miocene with special emphasis on the changes of the arid belt.
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Key words:
- Oligocene /
- Miocene /
- environmental patterns /
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