The Holocene Epoch is characterized by different sediments, ones that form when the climate is warmer.
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。
Holocene sediments contain remnants of more recent plants and animals, so it's pretty easy to differentiate geologically between these two Epochs.
全新世的沉积物中含有较新的动植物遗迹，因此很容易从地质学上区分这两个时期。
Formation and development of the Holocene delta.
全新世三角洲的形成和发育。
Dodos are flightless birds from the late Holocene.
渡渡鸟是全新世晚期不会飞翔的鸟类。
Development of the Holocene strata roughly is well.
全新世地层发育基本完好。
There might be a cold event in the period of the Middle Holocene.
本区可能也存在着中全新世的降温事件。
The warmest stage was not in Middle Holocene but in Late Holocene.
最暖期不是在中全新世，而是在晚全新世。
This article has a brief review on Holocene climate changes in Mongolia.
简要地回顾了蒙古全新世气候变化研究。
Actually, it won't necessarily be nuclear tests that ended the Holocene.
实际上，核试验并非结束全新世的唯一必要条件。
The planet’s history contains many less stable and clement eras than the Holocene.
地球的历史是包含了许多不如全新世稳定温和的时期的。
Sandy materials were deposited continually during the middle and late Holocene.
全新世中、晚期该区继续接受砂质沉积。
The planet's history contains many less stable and clement eras than the Holocene.
地球历史包含许多没有全新世稳定和温和的时期。
This time interval can be considered as the climatic optimum of the Holocene in this region.
这段时间可以认为是本地区全新世的气候最适宜期。
Study of Holocene environmental change is a focal point not only in the past but also in today.
全新世环境演变研究是过去全球变化研究的重点，也是当今全球变化研究的重点和热点。
Sequence I can be distinguished from the northwest slope to trough basin and is Holocene softy sediments.
层序I，由海槽西北部陆坡可以连续追踪至海槽区域，为全新世松软沉积物。
One strategy of Holocene climatic changes research is the select of key area to different time resolution.
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。
A holocene paleosol-loess sediment profile and lacustrine sediment profile were found in Mengjin, Henan province.
在河南孟津地区发现全新世古土壤-黄土沉积剖面和湖沼相沉积剖面。
The MIS 3 is a special period of the last glacial period and similar to the environment of Holocene on some ways.
深海氧同位素第3阶段是末次冰期中的一段特殊时期，与全新世存在一定的相似性。
Es Safa contains numerous vents that have been active during the holocene epoch (beginning approximately 12, 000 years ago).
Essafa那儿有许许多多的火山口，在全新世时期就已经很活跃了(差不多始于1万2千年前)。
In an editorial published in May, the respected publication argued that the Holocene could simply be renamed the Anthropocene.
在五月发表的社论中，这份权威刊物认为这仅仅是将全新世更名为人类世而已。
During the Holocene altithermal period, lake sediment developed extensively in the east part of China, and lake area expanded.
在全新世高温期，我国东部地区湖泊沉积广泛发育，西部地区湖泊扩张和高湖面记录普遍。
The soil type, cause of soil formation and soil quality changes of Holocene loess-soil sequence have been clearly distinguished.
通过本文各指标的研究，进一步认识了汾渭平原全新世土壤的类型、成因与质量演变。
So it provides many new ponderations and enlightenments in understanding holocene stratum and basement tectonics of the hebei plain.
因此，它对全面认识河北平原的全新世地层和新构造运动形迹会有许多新的启示。
So, it provides many new ponderations and enlightenments in understanding Holocene stratum and basement tectonics of the Hebei Plain.
因此，它对全面认识河北平原的全新世地层和新构造运动形迹会有许多新的启示。
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.
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。
During the investigation of the Weishui River valley, we found many palaeoflood slack-water deposits sandwiched in Holocene loess-soil profiles.
在湋水河谷多个地点发现全新世古洪水平流沉积层赋存于黄土—古土壤剖面中。
Exemplified by Jingpohu Holocene volcanic rocks, this paper has discussed the relationship between melt structure and volcanic eruptive mechanism.
本文以镜泊湖全新世火山为例，讨论了熔体结构和某些火山喷发机制的关系。
It is consistent with the area of ancient towns distribution, loess landslides distribution, Holocene active fault and the earthquake rupture zone.
这与本区黄土地震滑坡的分布范围、全新世活动断裂的展布及地震破裂带遗迹的分布相吻合。
The sea level changes of Holocene in Shanghai region are discussed in this paper based on the spore - pollen and microfossil analysis of Zhaoxiang core.
本文通过对位于上海同身西侧的赵巷孔进行孢粉和微古分析，论述上海地区全新世海平面变化。
The sea level changes of Holocene in Shanghai region are discussed in this paper based on the spore - pollen and microfossil analysis of Zhaoxiang core.
本文通过对位于上海同身西侧的赵巷孔进行孢粉和微古分析，论述上海地区全新世海平面变化。
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