Philip Camill

TL;DR: In this article, the authors presented revised estimates of permafrost organic carbon stocks, including quantitative uncertainty estimates, in the 0-3 m depth range in soils as well as for sediments deeper than 3 m in deltaic deposits of major rivers and in the Yedoma region of Siberia and Alaska.

TL;DR: This article synthesized sedimentary charcoal records of biomass burning since the last glacial maximum (LGM) and present global maps showing changes in fire activity for time slices during the past 21,000 years.

TL;DR: In this article, the vulnerability of the North American high-latitude soil organic carbon (SOC) pool to climate change has been discussed, where the authors divide the current northern highlatitude organic carbon pools into near-surface soils where SOC is affected by seasonal freeze-thaw processes and changes in moisture status, and deeper permafrost and peatland strata down to several tens of meters depth where organic carbon is usually not affected by short-term changes.

TL;DR: It is concluded that greater attention to spatially extensive and longer duration sampling for early life history stages is needed to assess the role of recruitment limitation in forests.

TL;DR: In this paper, the authors present results from the most comprehensive compilation of Holocene peat soil properties with associated carbon and nitrogen accumulation rates for northern peatlands, which consists of 268 peat cores from 215 sites located north of 45°N.