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.
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。
Holocene sediments contain remnants of more recent plants and animals, so it's pretty easy to differentiate geologically between these two Epochs.
全新世三角洲的形成和发育。
渡渡鸟是全新世晚期不会飞翔的鸟类。
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.
本区可能也存在着中全新世的降温事件。
There might be a cold event in the period of the Middle Holocene.
全新世地层发育基本完好。
全新世中、晚期该区继续接受砂质沉积。
Sandy materials were deposited continually during the middle and late Holocene.
最暖期不是在中全新世，而是在晚全新世。
The warmest stage was not in Middle Holocene but in Late 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。
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。
The planet's history contains many less stable and clement eras than the Holocene.
实际上，核试验并非结束全新世的唯一必要条件。
Actually, it won't necessarily be nuclear tests that ended the Holocene.
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.
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。
In an editorial published in May, the respected publication argued that the Holocene could simply be renamed the Anthropocene.
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。
A holocene paleosol-loess sediment profile and lacustrine sediment profile were found in Mengjin, Henan province.
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.
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。
Exemplified by Jingpohu Holocene volcanic rocks, this paper has discussed the relationship between melt structure and volcanic eruptive mechanism.
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。
So, it provides many new ponderations and enlightenments in understanding Holocene stratum and basement tectonics of the Hebei Plain.
所以该地区是研究第四纪以来，特别是全新世以来中国及全球环境变化的典型地区。
Therefore, the area is typical to study the environmental change of China, even of the globe since Quaternary Period, especially since the Holocene Epoch.
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。
The MIS 3 is a special period of the last glacial period and similar to the environment of Holocene on some ways.
经研究认为，该区中南部的南四湖、北五湖的湖相沉积大约形成于全新世中晚期之后。
As proved by the study, lacustrine sedimentation of Nansihu and Beiwuhu in middle and south part were formed in late period of Holecene.
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。
The soil type, cause of soil formation and soil quality changes of Holocene loess-soil sequence have been clearly distinguished.
这段稳定期也让在全新世初期也许只有几百万的智人兴旺起来；农业兴起，文明化程度也越来越高。
That stability has allowed Homo sapiens, numbering perhaps just a few million at the dawn of the Holocene, to thrive; farming has taken hold and civilizations have arisen.
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。
Study of Holocene environmental change is a focal point not only in the past but also in today.
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。
During the Holocene altithermal period, lake sediment developed extensively in the east part of China, and lake area expanded.
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。
It is consistent with the area of ancient towns distribution, loess landslides distribution, Holocene active fault and the earthquake rupture zone.
本区古地理的演变过程是：由更新世的陆地环境，经过全新世的海侵，变为现今的滨海环境。
The process of paleogeographic evolution in this area is from land of pleistocene epoch to ingression of holocene epoch, then to littoral circumstances of today.
泻湖是全新世海侵以来发育的以淤积为主的海岸地貌，其沉积地层蕴含了丰富的古环境演变信息。
Lagoon is the coastal landscape developed by the deposition mainly since Holocene transgression, and the stratigraphic of which contains a wealth of paleoenvironment evolution information.
泻湖是全新世海侵以来发育的以淤积为主的海岸地貌，其沉积地层蕴含了丰富的古环境演变信息。
Lagoon is the coastal landscape developed by the deposition mainly since Holocene transgression, and the stratigraphic of which contains a wealth of paleoenvironment evolution information.
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