The paleoclimate should belong to the subtropical one.
古气候应属亚热带气候。
Pollen analysis helped to find out the paleoclimate information.
以孢粉分析了解古气候方面的信息。
Paleoclimate the climate conditions of geologic periods in the ancient past.
Paleoclimate -古气候指的是古代地质时期的气候条件。
Carbon isotope in soil carbonates is an important paleoclimate data carrier.
土壤碳酸盐中碳稳定同位素是记录古气候变化信息的重要载体。
Then a discussion has been done on the stratigraphic division and paleoclimate in this area.
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。
Pollen grains and spores are important index to reconstruct paleoclimate and paleoenvironment.
孢粉是恢复古植被、古气候的重要代用指标。
Finally, we discuss the paleoclimate change according to the sequence stratigraphical analysis.
最后，结合层序地层划分分析了古气候变化。
Paleosalinity recovery is one of the important methods for paleoenvironment and paleoclimate study.
古盐度的恢复是对古环境和古气候研究的重要方法之一。
Evolution of desert is one of important aspect of Quaternary paleoclimate and paleoenvironment research.
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。
The mixing could be more or less influenced by the former topography and carbonate production in moderate paleoclimate.
先期地形、气候变化(含碳酸盐生产速率影响)或多或少对体系域的混合沉积作用有影响。
Therefore, the change of Earth orbital parameters is just one of factors, which could lead to the paleoclimate variation.
因此，地球轨道参数变化影响气候长期变化只是其中一种因素。
On paleoclimate evolution, the uranium metallization occur during arid climate condition or transition from humid to arid.
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。
As an important component of lake sediments, diatom is of great value for reconstructing paleoclimate and paleoenvironment.
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。
In particular, Cave dropstones stalagmites offered us a kind of distinctive data source as continental paleoclimate archives.
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。
Obviously, the Lunan stone forest was developed in tropical paleoclimate, when the region of lower latitude was at a lower altitude.
纬度较低的路南石林是处在低海拔时古热带环境下形成的。
Present use of biomarkers to reconstruct paleoclimate and ancient human activities has become an important part of molecular stratigraphy.
应用生物标志化合物恢复古气候、探索古人类活动已成为古气候研究中的重要内容。
The sediments in the cave are of not only the value for tourism development, but also rich information of paleoclimate and paleoenvironment.
洞穴沉积物不仅具有旅游开发价值，而且蕴含了丰富的古气候环境信息。
The carbon and oxygen stable isotopes have been considered to be the most effectual proxy indexes in reconstructing the paleoclimate of Quaternary.
利用洞穴次生化学沉积物进行古环境重建是第四纪全球变化研究的一个热点，而碳氧稳定同位素是最重要的气候替代性指标。
Ice core study, providing much information for "a study of global change", is an effective approach to the study of paleoclimate and paleoenvironment.
冰岩芯研究是古气候、古环境研究的有力手段，它将为“全球变化研究”提供多方面的气候、环境信息。
Comparison with the historical climate changes shows a good correlation between the Marine and continental records of the East Asian paleoclimate changes.
结合历史气候变化，得到东亚古气候变化的海陆记录具有很好的可比性。
There were three times of sea-level fluctuation corresponding to the paleoclimate evolution, which had formed the sediments of alternative sea and river facies.
晚更新世以来的三次海平面升降变化造成了潍河下游地区海陆沉积环境交替，形成了巨厚的海陆交互相沉积层。
The paleoclimate records of the vermicular red earth in the Middle-Lower Yangtze Region is of great significance to the study of the global changes in Quaternary.
长江中下游地区网纹红土中的古气候记录，在第四纪全球变化研究中具有十分重要的意义。
The factors affecting the property of reservoir were as follows. (1) environment of sedimentary, (2) paleoclimate, (3) diagenesis, (4) tectonic movement, (5) clay minerals.
影响储层储集性能的主要因素：(1)沉积环境，(2)古气候，(3)成岩作用，(4)构造运动，(5)粘土矿物。
Schmittner notes that many previous studies only looked at periods spanning from 1850 to today, thus not taking into account a fully integrated paleoclimate data on a global scale.
齐弥特纳注解说很多以前的研究只研究了从1850年至今这段时期的变化，因此从全球的规模上来说，没有考虑到古气候这个属于整体的数据。
The Late Quaternary paleoclimate environment in Ninghua was not suitable for the development of a glacier, and it was kept under the influence of the global temperature variation.
结果表明，宁化地区晚第四纪古气候环境没有形成冰川的条件，但明显受到全球气温变化的控制。
The aeolian silty sand in shale can provide good guide to study of paleoclimate about lacustrine shale and varve, and to reconstruct sedimentary environment of paleolake accurately.
页岩中风成粉砂沉积的发现，可以进一步为研究有关湖相页岩和第四纪纹泥的古气候变化、正确恢复古湖泊沉积环境提供良好的指标。
This paper deals with the present situation, prospect and significance of the research for continental Cretaceous red beds to reconstruction of paleoclimate in the Cretaceous period.
介绍了白垩纪陆相红层研究的现状及前景，特别是其在白垩纪陆相古气候恢复方面所具有的重要意义。
P. the Late Quaternary paleoclimate environment in Ninghua was not suitable for the development of a glacier, and it was kept under the influence of the global temperature variation.
结果表明，宁化地区晚第四纪古气候环境没有形成冰川的条件，但明显受到全球气温变化的控制。
Results show that the quantitative reconstruction of the paleoclimate on the Chinese Loess Plateau is still on the preliminary stage, though lots of positive results have been achieved.
相关的研究结果表明，黄土高原地区的古气候定量化研究取得了积极的成果，但还仍处在初步阶段。
Results show that the quantitative reconstruction of the paleoclimate on the Chinese Loess Plateau is still on the preliminary stage, though lots of positive results have been achieved.
相关的研究结果表明，黄土高原地区的古气候定量化研究取得了积极的成果，但还仍处在初步阶段。
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