[1] Liu, L., Tian, J., Wang, H., Xue, D., Huang, X., Wu, N., Wang, M., Xu, X., Peng, C., Wang, Y., Chen, H., 2023. Stable oxic-anoxic transitional interface is beneficial to retard soil carbon loss in drained peatland. Soil Biology and Biochemistry 181, 109024.

[2] Liu, L., Chen, H., Tian, J., 2022. Varied response of carbon dioxide emissions to warming in oxic, anoxic and transitional soil layers in a drained peatland. Communications Earth & Environment 3(1), 313.

[3] Liu, L., Chen, H., He, Y., Liu, J., Dan, X., Jiang, L., Zhan, W., 2022. Carbon stock stability in drained peatland after simulated plant carbon addition: Strong dependence on deeper soil. The Science of the total environment 848, 157539.

[4] Liu, L., Chen, H., Jiang, L., Zhan, W., Hu, J., He, Y., Liu, J., Xue, D., Zhu, D., Zhao, C., Yang, G., 2019. Response of anaerobic mineralization of different depths peat carbon to warming on Zoige plateau. Geoderma 337, 1218-1226.

[5] Liu, L., Chen, H., Jiang, L., Hu, J., Zhan, W., He, Y., Zhu, D., Zhong, Q., Yang, G., 2018. Water table drawdown reshapes soil physicochemical characteristics in Zoige peatlands. Catena 170, 119-128.

[6] Liu, L., Chen, H., Zhu, Q., Yang, G., Zhu, E., Hu, J., Peng, C., Jiang, L., Zhan, W., Ma, T., He, Y., Zhu, D., 2016. Responses of peat carbon at different depths to simulated warming and oxidizing. The Science of the total environment 548-549, 429-440.

[7] Tian, J^#., Liu, L^#., Chen, H., Zhong, L., Zhou, X., Jiang, L., Zhan, W., Wang, Y., 2022. Aerobic environments in combination with substrate additions to soil significantly reshape depth-dependent microbial distribution patterns in Zoige peatlands, China. Applied Soil Ecology 170, 104252.