Nine years of warming and nitrogen addition in the Tibetan grassland promoted loss of soil organic carbon but did not alter the bulk change in chemical structure
Huimin Sun,Michael W. I. Schmidt,Jintao Li,Jinquan Li,Xiang Liu,Nicholas O. E. Ofiti,Shurong Zhou,and Ming Nie
Huimin Sun
Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai 200433, China
Department of Geography, University of Zurich, Zurich, Switzerland
Department of Geography, University of Zurich, Zurich, Switzerland
Jintao Li
Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai 200433, China
Jinquan Li
Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai 200433, China
Xiang Liu
State Key Laboratory of Grassland Agro-Ecosystem, Institute of Innovation Ecology, Lanzhou University, 222 Tianshui South Road, Lanzhou 730000, China
Department of Geography, University of Zurich, Zurich, Switzerland
Shurong Zhou
Key Laboratory of Genetics and Germplasm Innovation of Tropical Special Forest Trees and Ornamental Plants, Ministry of Education, College of Forestry, Hainan University, Haikou 570228, China
Ministry of Education Key Laboratory for Biodiversity Science and Ecological Engineering, National Observations and Research Station for Wetland Ecosystems of the Yangtze Estuary, Institute of Biodiversity Science and Institute of Eco-Chongming, School of Life Sciences, Fudan University, Shanghai 200433, China
Viewed
Total article views: 2,918 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,178
609
131
2,918
231
114
150
HTML: 2,178
PDF: 609
XML: 131
Total: 2,918
Supplement: 231
BibTeX: 114
EndNote: 150
Views and downloads (calculated since 01 Sep 2023)
Cumulative views and downloads
(calculated since 01 Sep 2023)
Total article views: 2,160 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,693
363
104
2,160
122
98
133
HTML: 1,693
PDF: 363
XML: 104
Total: 2,160
Supplement: 122
BibTeX: 98
EndNote: 133
Views and downloads (calculated since 26 Jan 2024)
Cumulative views and downloads
(calculated since 26 Jan 2024)
Total article views: 758 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
485
246
27
758
109
16
17
HTML: 485
PDF: 246
XML: 27
Total: 758
Supplement: 109
BibTeX: 16
EndNote: 17
Views and downloads (calculated since 01 Sep 2023)
Cumulative views and downloads
(calculated since 01 Sep 2023)
Viewed (geographical distribution)
Total article views: 2,918 (including HTML, PDF, and XML)
Thereof 2,914 with geography defined
and 4 with unknown origin.
Total article views: 2,160 (including HTML, PDF, and XML)
Thereof 2,151 with geography defined
and 9 with unknown origin.
Total article views: 758 (including HTML, PDF, and XML)
Thereof 758 with geography defined
and 0 with unknown origin.
A soil organic carbon (SOC) molecular structure suggested that the easily decomposable and stabilized SOC is similarly affected after 9-year warming and N treatments despite large changes in SOC stocks. Given the long residence time of some SOC, the similar loss of all measurable chemical forms of SOC under global change treatments could have important climate consequences.
A soil organic carbon (SOC) molecular structure suggested that the easily decomposable and...
