Yanhong Zheng

TL;DR: In this article, a multi-proxy analysis of a radiocarbon-dated peat core that records the history of paleoclimate change dating from 18ka in the Dingnan region of southern China was carried out.

TL;DR: In this article, the authors extracted from a peat core obtained from the northeast edge of the Tibetan Plateau have provided a 13 kyr record of regional climate change, showing that a period of warmer climate corresponding to the Holocene Optimum between 9-ka and 5-ka is evident in greater alteration of nalkanoic acids and n-alkanols and in the appearance of biomarkers indicative of greater microbial activity.

TL;DR: The peat sequence at Hani in northeastern China accumulated over the past 16cal kyr in a percolation mire in which rain water and ground water seeped through the peat system as mentioned in this paper.

TL;DR: In this paper, the authors determined molecular compositions of individual plant wax hydrocarbons and their hydrogen isotope compositions ( δD values) in a radiocarbon-dated peat core recovered from the Hani marsh in Jilin Province (China) and confirmed that the temperaturedependent effective precipitation in northeast China decreased during the Holocene Climate Optimum.

TL;DR: In this article, the authors reconstruct changes in mean annual air temperature and peat soil moisture across the last ∼13,000 year BP using samples from the Gushantun and Hani peat, located in NE China.