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.
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.
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.
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.
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