中文版 | English

在结果中检索

CCPortal
（本次检索基于用户作品认领结果）

浏览/检索结果: 共5条，第1-5条 帮助

限定条件                    
已选(0)清除 条数/页：   排序方式：
Provenance and Climatic Implications of the Middle-Pleistocene Loess Deposit, Southern China 期刊论文
FRONTIERS IN EARTH SCIENCE, 2021, 卷号: 9
作者:  Fan, Qingbin;  Liao, Jie;  Li, Yan;  Ye, Wei;  Wang, Tao;  Feng, Xiao
收藏  |  浏览/下载：25/0  |  提交时间：2022/04/28
SCANNING-ELECTRON-MICROSCOPY  ASIAN WINTER MONSOON  XIASHU LOESS  QUARTZ GRAINS  MICROTEXTURAL ANALYSIS  SOIL SEQUENCES  ICE-VOLUME  SEM  INTENSITY  EXTREMES  
Plant community changes determine the vegetation and soil delta C-13 and delta N-15 enrichment in degraded alpine grassland 期刊论文
LAND DEGRADATION & DEVELOPMENT, 2021, 卷号: 32, 期号: 7
作者:  Li, Chengyang;  Peng, Fei;  Lai, Chimin;  Xue, Xian;  You, Quangang;  Chen, Xiaojie;  Liao, Jie;  Ma, Shaoxiu;  Wang, Tao
收藏  |  浏览/下载：37/0  |  提交时间：2022/04/28
Spatial and Temporal Differences in Alpine Meadow, Alpine Steppe and All Vegetation of the Qinghai-Tibetan Plateau and Their Responses to Climate Change 期刊论文
REMOTE SENSING, 2021, 卷号: 13, 期号: 4
作者:  Duan, Hanchen;  Xue, Xia;  Wang, Tao;  Kang, Wenping;  Liao, Jie;  Liu, Shulin
收藏  |  浏览/下载：25/0  |  提交时间：2022/04/28
Origin and Paleoenvironmental Significance of the Old Red Sand Along the Southeast Coast of China 期刊论文
FRONTIERS IN EARTH SCIENCE, 2021, 卷号: 9
作者:  Fan, Qingbin;  Liao, Jie;  Li, Yan;  Ye, Wei;  Wang, Tao;  Feng, Xiao
收藏  |  浏览/下载：24/0  |  提交时间：2022/04/28
SCANNING-ELECTRON-MICROSCOPY  QUARTZ GRAINS  SEM  MICROTEXTURES  DEPOSITS  ACCUMULATION  CHRONOLOGY  INDIA  
Dominant Plant Functional Group Determine the Response of the Temporal Stability of Plant Community Biomass to 9-Year Warming on the Qinghai-Tibetan Plateau 期刊论文
FRONTIERS IN PLANT SCIENCE, 2021, 卷号: 12
作者:  Li, Chengyang;  Lai, Chimin;  Peng, Fei;  Xue, Xian;  You, Quangang;  Liu, Feiyao;  Guo, Pinglin;  Liao, Jie;  Wang, Tao
收藏  |  浏览/下载：30/0  |  提交时间：2022/04/28
CLIMATE-CHANGE  ALPINE MEADOW  ECOSYSTEM STABILITY  SPECIES COMPOSITION  BIODIVERSITY  DIVERSITY  AVAILABILITY  PRODUCTIVITY  ASYNCHRONY