Peatlands in the Earth's 21st century climate system
Peatlands occupy a relatively small fraction of the Earth's land area, but they are a globally
important carbon store because of their high carbon density. Undisturbed peatlands are …
important carbon store because of their high carbon density. Undisturbed peatlands are …
Terrestrial biogeochemical feedbacks in the climate system
The terrestrial biosphere is a key regulator of atmospheric chemistry and climate. During
past periods of climate change, vegetation cover and interactions between the terrestrial …
past periods of climate change, vegetation cover and interactions between the terrestrial …
A database and synthesis of northern peatland soil properties and Holocene carbon and nitrogen accumulation
Here, we present results from the most comprehensive compilation of Holocene peat soil
properties with associated carbon and nitrogen accumulation rates for northern peatlands …
properties with associated carbon and nitrogen accumulation rates for northern peatlands …
Global peatland dynamics since the Last Glacial Maximum
Here we present a new data synthesis of global peatland ages, area changes, and carbon
(C) pool changes since the Last Glacial Maximum, along with a new peatland map and total …
(C) pool changes since the Last Glacial Maximum, along with a new peatland map and total …
Northern peatland carbon stocks and dynamics: a review
ZC Yu - Biogeosciences, 2012 - bg.copernicus.org
Peatlands contain a large belowground carbon (C) stock in the biosphere, and their
dynamics have important implications for the global carbon cycle. However, there are still …
dynamics have important implications for the global carbon cycle. However, there are still …
Climate-related changes in peatland carbon accumulation during the last millennium
Peatlands are a major terrestrial carbon store and a persistent natural carbon sink during the
Holocene, but there is considerable uncertainty over the fate of peatland carbon in a …
Holocene, but there is considerable uncertainty over the fate of peatland carbon in a …
Holocene carbon flux histories of the world's peatlands: Global carbon-cycle implications
Z Yu - The Holocene, 2011 - journals.sagepub.com
This paper proposes a novel approach using basal peat ages and carbon (C) accumulation
profiles from the world's major peatland regions to decompose C flux terms from time …
profiles from the world's major peatland regions to decompose C flux terms from time …
[HTML][HTML] Natural gas as a key alternative energy source in sustainable renewable energy transition: a mini review
N Mohammad, WW Mohamad Ishak… - Frontiers in Energy …, 2021 - frontiersin.org
Energy security and sustainability are undeniably the main concerns in combatting climate
change. While an immediate call for all-green and renewable energy seems to be …
change. While an immediate call for all-green and renewable energy seems to be …
[HTML][HTML] 全新世年代框架约束下的东北地区土壤有机碳储库时空格局
陈雨露, 郭利成, 崔静怡, 熊尚发 - 第四纪研究, 2022 - dzkx.org
陈雨露, 郭利成, 崔静怡, 熊尚发. 全新世年代框架约束下的东北地区土壤有机碳储库时空格局[J].
第四纪研究, 2022, 42 (5): 1311-1327. doi: 10.11928/j. issn. 1001-7410.2022. 05.07引用本文 …
第四纪研究, 2022, 42 (5): 1311-1327. doi: 10.11928/j. issn. 1001-7410.2022. 05.07引用本文 …
Holocene vegetation and climate histories in the eastern Tibetan Plateau: controls by insolation-driven temperature or monsoon-derived precipitation changes?
Y Zhao, Z Yu, W Zhao - Quaternary Science Reviews, 2011 - Elsevier
The climates on the eastern Tibetan Plateau are strongly influenced by direct insolation
heating as well as monsoon-derived precipitation change. However, the moisture and …
heating as well as monsoon-derived precipitation change. However, the moisture and …