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古气候应属亚热带气候。The paleoclimate should belong to the subtropical one.

Paleoclimate-古气候指的是古代地质时期的气候条件。Paleoclimate The climate conditions of geologic periods in the ancient past.

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重建古气候、古环境已成为当今全球变化研究的热点。Reconstruct the paleoclimate and paleoenvironment has been the hotspot of the word.

内蒙岱海是位于东南季风区的西北边缘的内陆封闭湖泊，对气候变化十分敏感。Daihai Lake, with a closed drainage basin, is very sensitive to the paleoclimate hange.

依此对区内晚第四纪的地层及古气候环境进行了初步讨论。Then a discussion has been done on the stratigraphic division and paleoclimate in this area.

最后，结合层序地层划分分析了古气候变化。Finally, we discuss the paleoclimate change according to the sequence stratigraphical analysis.

靖远黄土剖面沉积厚度大，古气候信息分辨率高。Jingyuan loess deposition thickness, Information of paleoclimate evolution was high resolution.

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古盐度的恢复是对古环境和古气候研究的重要方法之一。Paleosalinity recovery is one of the important methods for paleoenvironment and paleoclimate study.

沙漠形成演化是第四纪古气候、古环境研究的重要内容之一。Evolution of desert is one of important aspect of Quaternary paleoclimate and paleoenvironment research.

整个侏罗纪代表了一个水体由浅-深-浅、古气候由乾燥-湿热-乾燥的演化过程。The whole Jurassic represented a complete shallow-deep-shallow palaeogeography and dry-moist-dry paleoclimate cycle.

千百年尺度全球气候快速变化是古气候研究中的一个重要内容。Rapid climate changes at millennial and centennial scales are one of the most important aspects in Paleoclimate study.

本文用粘土矿物特征来论述阳原盆地古气候演变。This paper is to discuss the paleoclimate evolution by analysing clay minerals in eight samples from the Yangyuan Basin.

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在古气候演变上，成矿作用发生在干旱气候条件下，或由潮湿向干旱的气候转变阶段。On paleoclimate evolution, the uranium metallization occur during arid climate condition or transition from humid to arid.

硅藻是湖泊沉积物的重要组成部分，沉积物硅藻硅氧同位素在重建古气候、古环境方面具有重要价值。As an important component of lake sediments, diatom is of great value for reconstructing paleoclimate and paleoenvironment.

对洞穴湖相沉积物作了地球化学特征的对比，从而获得不同的古气候环境。The geochemical characteristics of harfour deposits in the caves are compared and the paleoclimate environment is obtained.

尤其是洞穴滴石石笋为大陆气候替代指标提供了一类独特的数据源。In particular, Cave dropstones stalagmites offered us a kind of distinctive data source as continental paleoclimate archives.

生物壳体碳酸盐的稳定氧、碳同位素已经被大量地应用在古气候、古环境研究中。The oxygen and carbon isotopes in biogenic carbonate have been extensively used in paleoclimate and paleoenvironment studies.

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人地关系部分资料不足，将来还需要更多的古气候方面的研究。The chapter of human-environment interaction lacks a solid database, which calls for much more effort in the study of paleoclimate.

研究文石石笋对重建古气候环境、成岩成矿作用都有重要理论和实践意义。The study of aragonite stalagmites is important to reconstruct the paleoclimate and know mineralization in both theory and practice.

层序和体系域形成的主要控制因素有构造运动、基准面的变化和古气候的变化。The main control factors created by the sequence and the domain include tectonic movement and the changes of base level and paleoclimate.