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: 3,023 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
2,250
636
137
3,023
238
118
162
HTML: 2,250
PDF: 636
XML: 137
Total: 3,023
Supplement: 238
BibTeX: 118
EndNote: 162
Views and downloads (calculated since 01 Sep 2023)
Cumulative views and downloads
(calculated since 01 Sep 2023)
Total article views: 2,257 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
1,759
388
110
2,257
124
101
145
HTML: 1,759
PDF: 388
XML: 110
Total: 2,257
Supplement: 124
BibTeX: 101
EndNote: 145
Views and downloads (calculated since 26 Jan 2024)
Cumulative views and downloads
(calculated since 26 Jan 2024)
Total article views: 766 (including HTML, PDF, and XML)
HTML
PDF
XML
Total
Supplement
BibTeX
EndNote
491
248
27
766
114
17
17
HTML: 491
PDF: 248
XML: 27
Total: 766
Supplement: 114
BibTeX: 17
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: 3,023 (including HTML, PDF, and XML)
Thereof 3,022 with geography defined
and 1 with unknown origin.
Total article views: 2,257 (including HTML, PDF, and XML)
Thereof 2,251 with geography defined
and 6 with unknown origin.
Total article views: 766 (including HTML, PDF, and XML)
Thereof 766 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...
