Soil texture and microorganisms dominantly determine the subsoil carbonate content in the permafrost-affected area of the Tibetan Plateau
Ming Shao(Chinese Academy of Sciences), Hanbo Yun(Northwest Institute of Eco-Environment and Resources), Sen Song(Cold Spring Harbor Laboratory), Yutao Pei(Chinese Academy of Sciences), Shengyin Zhang(Chinese Academy of Sciences), Tianzhu Lei(Chinese Academy of Sciences)
Cited by 7
Related Papers
Highly Nonrandom Features of Synaptic Connectivity in Local Cortical Circuits
|PLoS Biology|2005|1.6k
Changes in active-layer thickness and near-surface permafrost between 2002 and 2012 in alpine ecosystems, Qinghai–Xizang (Tibet) Plateau, China
|Global and Planetary Change|2014|257
Improved calcium sensor GCaMP-X overcomes the calcium channel perturbations induced by the calmodulin in GCaMP
|Nature Communications|2018|200
Evaluation of the hydrological contributions of permafrost to the thermokarst lakes on the Qinghai–Tibet Plateau using stable isotopes
|Global and Planetary Change|2016|81
Potential linkages between the moisture variability in the northeastern Qaidam Basin, China, since 1800 and the East Asian summer monsoon as reflected by tree ring<i>δ</i><sup>18</sup>O
|Journal of Geophysical Research Atmospheres|2011|33