简要地回顾了蒙古全新世气候变化研究。
This article has a brief review on Holocene climate changes in Mongolia.
全新世气候变化研究的策略之一就是不同时间分辨率的关键地点的选择。
One strategy of Holocene climatic changes research is the select of key area to different time resolution.
蒙古全新世气候变化研究侧重于对树轮、风成沉积和湖泊沉积物的研究。
The studies of Mongolian Holocene climate changes mainly focused on the records of tree-rings, eolian sediments and lacustrine sediments.
公元前9000年到5000年这段时期被称为全新世气候暖期(Holocene ClimateOptimum)，这种气候就像地中海海滨的温暖午后一样惬意。
The time from 9, 000 to 5, 000 BC is called the Holocene Climate Optimum, which makes it sound like a nice afternoon on a Mediterranean beach.
全新世时期的特征为不同的沉积物，它们在气候变暖时形成。
The Holocene Epoch is characterized by different sediments, ones that form when the climate is warmer.
地球历史上有很多尚未揭示的奥秘，例如距今约350 ~ 250万年前的全新世中期地球气候变化的根本原因一直都是个谜。
09051903 One of the mysteries of the Earth's history is the fundamental climate change in the Mid Pliocene, about 3.5-2.5 million years ago.
这段时间可以认为是本地区全新世的气候最适宜期。
This time interval can be considered as the climatic optimum of the Holocene in this region.
进入全新世晚期，由于气候相对于全新世中期变得较为干燥，也较为温凉，流域来水减少，故流量减小，河床宽度变小。
In late Holocene, climate is dryer and cooler than that in middle Holocene, the precipitation of drainage area decreases. So runoff deceases, the width of riverbed becomes narrow.
宁晋泊沉积物的环境指标高分辨率分析，揭示了全新世温暖期以来气候变化规律和湖泊演化过程。
Climatic fluctuation and process of lake changes were revealed through high resolution analysis on environmental indices based on sediments of Ningjin lake.
结果表明，全新世以来，中国西部干旱区的气候变化经历了多次的相对暖干和相对冷湿交替变化，变化历程较为复杂。
The results showed that the climate changing patterns had gone through several complex cycles of "warm and dry" and "cold and moist" periods.
虽然未来年降水总量的变幅没有超过过去50年器测记录变幅，更不及全新世的降水变化量，但湖泊水量对气候变化的反映变率较变幅要大。
Although the future changes in precipitation are equivalent to the last 50-yr gauges and lower than changes in the Holocene, the speed of lake water change was much high.
本文据古生物学和古生态学资料，论述了建湖地区全新世生物群的演替、海平面波动、古地理变迁和古气候变化。
The purpose of this paper is to study the Holocene biotic variance and to discuss the sea level fluctuation and the palaeoclimatic change in Jianhu area, northern Jiangsu.
到全新世晚期，由于全球气候的变化和优势的北北东方向风力的逐渐增强，河谷洼地与海湾相联结的地区长时间受风沙的堆积而形成岚湖。
Due to the change of the global climate and gradually strengthened predominant NNE wind in Late Holocene, the eolian sand had been accumulated for a long time in the area b…
关中平原全新世l 0发育时的气候与西北荒漠区的气候也存在遥相关关系。
There was the remote correlation of the climate between Guanzhong Plain and the northwest desert area during development of L0.
该海底古森林生长于全新世长乐组冲洪积层中，生长时代为距今约7000—7500 a，为湿热气候环境；
Ancient submarine forest grew in alluvial-pluvial deposit in Holocene Changle group, and the growing era is damp and hot climate environment as about 7000 ~ 7500 years ago;
晚全新世植被为森林草原或疏林草原，气候干旱偏暖—温凉干旱。
The vegetation of the middle Holocene was forest grassland and aciculignosa and aeslilignosa grassland, and the climate was warm and wet.
晚全新世植被为森林草原或疏林草原，气候干旱偏暖—温凉干旱。
The vegetation of the middle Holocene was forest grassland and aciculignosa and aeslilignosa grassland, and the climate was warm and wet.
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