间冰期

论中国第四纪冰期与间冰期

On the glacial and interglacial stages in Quaternary of China

末次间冰期以来地球气候系统的突变

Abrupt changes in earth 's climate system since last interglacial

在从冰期向间冰期的过渡期间，CO2和CH4浓度分别增加40%和100%。

CO2 and CH4 concentrations respectively increase bv about 40 % and 100 % during glacial-interglacial transitions .

在早于上一个间冰期的等效时期的CO2下降趋势的较为流行的解释对于自然因素驱动晚全新世以来的CO2浓度升高提出了一个主要的问题。

The prevalence of downward CO2 trends during equivalent intervals early in previous interglaciations poses a major problem for natural explanations of the late-Holocene CO2 increase .

综合考虑这些因素，利用有孔虫Mg/Ca比值重建表层海水温度（SST）记录时，获得的温度结果的误差在±0.5℃之内，可以满足冰期/间冰期气候变化过程中SST变化研究的要求。

Considering all the factors that may contribute to the errors of the Mg / Ca SST records , the overall errors for the temperature reconstructing from the foraminifer shells should be ± 0.5 ℃ . This precision meets the requirement of studying SST changes within glacial-interglacial cycles .

我国南方末元古代间冰期的锰矿层（大塘坡期）出现了普遍超过+40‰的异常高δ34S值的沉积黄铁矿，这是全球性的雪球事件的响应。

The ultra-high δ 34S values of sedimentary pyrite , exceeded + 40 ‰, occurring in interglacial manganese mineralization beds ( Datangpo Stage ) of terminal Proterozoic in southern China are response to global snowball Earth .

与Bc-1孔相同，研究区沉积地层与冰期旋回具有明显的对应关系，冰期时形成陆相地层，间冰期时形成海相地层。

Similar to those in Core Bc-1 , the depositional strata in the area have obvious corresponding relation to the glacial-interglacial cycles , that is , the continental facies strata were formed during the glacial periods , and the marine facies strata were formed during the interglacial periods .

黄土高原末次间冰期气候的不稳定性特征

Climatic instability characteristic in Loess Plateau during the last interglacial age

浅析末次间冰期以来柴达木盆地东南部古气候环境演化

Paleoclimate evolution in southeast of Qaidam Basin since the last interglacial

末次间冰期以来会宁黄土剖面的热释光测年

Thermoluminescence Dating of the Late Quaternary Loess Sequence along the Huining Section

三门峡王官与武威沙沟黄土记录中的末次间冰期向末次冰期转换期的暖性回返事件

A warm-return event during the transition of last interglacial-glacial cycle

末次间冰期以来陆地生态系统的碳储量与气候变化

Changes in terrestrial carbon storage with global climate changes since the last interglacial

从展示到纪录甘肃环县剖面记录的末次间冰期地磁场

A detailed palaeomagnetic record for the last interglacial period from Huanxian loess section

末次间冰期东亚季风百年&十年际分辨率洞穴石笋记录

Decadal-to Century-scale High Resolution Stalagmites Record of Asian Monsoon during the Last Interglacial

大塘坡组为间冰期海陆过渡相沉积。

Datangpo Formation deposited in transitional facies during interglaciation .

洛川地区倒数第二次间冰期气候变化研究

Climate Change during the Penultimate Interglacial in Luochuan Area

全新世与末次间冰期对比，总体气候变化较平缓。

Comparing with last interglacial , the climate change in Holocene is more gently .

嗯，这一次间冰期和之前的间冰期，有什么不同呢？

Um ... What was different about this interglacial period than the other ones ?

山西临汾盆地末次间冰期以来古气候变化研究

The Research on Paleoclimate Changes Since Last Interglacial Stage in Linfen Basin , Shanxi

整个全新世虽存在着干旱与湿润、冰期与间冰期的变化，但总的趋势向着更为干旱的方向发展。这些结果为未来气候预测和生产投资提供了重要的信息。

These results provide an important information for predicting future climate and production investments .

此外在半深海地区无论是冰期还是间冰期陆坡都是陆源物质的主要沉积区，槽底区的沉积速率远低于陆坡区，但二者沉积速率的差异在冰期相对减小。

In the semi-abyssal area continental slope is the major accumulation site of terrestrial material ;

间冰期的发生于冰河时代之间的这条河曾短期结冰。

Occurring between glacial epochs . The river was covered with ice for a space .

末次间冰期以来源自中亚的粉尘记录的对比

A Comparison of the Records of Dust Originated from Central Asia since the Last Interglacial

中纬度亚洲现代间冰期气候变化的西风模式讨论

A discussion on the westerly-dominated climate model in mid-latitude Asia during the modern interglacial period

冰期-间冰期旋回过程中，大气温度可随之作大幅度的波动。

In the glacial-interglacial cycle process , the air temperature can be followed for large fluctuations .

孟加拉湾晚第四纪冰期和间冰期古生产力演变研究

The study of the glacial interglacial paleoproductivity evolution during late Quaternary in the bay of Bengal

我们不知道自己是生活在后冰川期还是生活于间冰期。

We do not know whether we live in a postglacial period or an interglacial period .

末次冰期-间冰期蒙古高原与黄土高原对全球变化的重要贡献

Contribution to Global Change of Mongolian Plateau and Loess Plateau in the Last Glaciation and Interglacial Periods

末次间冰期以来黄河中游黄土高原沟谷侵蚀-堆积过程初探

Processes of Gully Erosion and Accumulation in the Central Loess Plateau of China Since the Last Interglacial

结果同时表明，间冰期时黄土高原地区风化成壤强度和南北气候梯度不具严格的对应关系。

Our results also reveal two distinct combinations of climate gradient and weathering intensity for interglacial periods .