Belowground climate change responses remain a key unknown in the Earth system. Plant
fine-root response is especially important to understand because fine roots respond quickly …

In this study, a suite of complementary environmental geochemical analyses, including NMR
and gas chromatography-mass spectrometry (GC-MS) analyses of central metabolites …

Sphagnum mosses are keystone components of peatland ecosystems. They facilitate the
accumulation of carbon in peat deposits, but climate change is predicted to expose peatland …

Managed forests generally produce high water quality, but degradation is possible via
sedimentation if proper management is not implemented during forest harvesting. To …

We characterized peat decomposition at the Marcell Experimental Forest (MEF), Minnesota,
USA, to a depth of 2 m to ascertain the underlying chemical changes using Fourier transform …

This paper describes the operational methods to achieve and measure both deep-soil
heating (0–3 m) and whole-ecosystem warming (WEW) appropriate to the scale of tall …

Sphagnum‐dominated peatlands comprise a globally important pool of soil carbon (C) and
are vulnerable to climate change. While peat mosses of the genus Sphagnum are known to …

We compared carbon (C), nitrogen (N), and phosphorus (P) concentrations in atmospheric
deposition, runoff, and soils with microbial respiration [dehydrogenase (DHA)] and …

Despite being a significant input into soil carbon pools of many high‐latitude ecosystems,
little is known about the effects of climate change on the turnover of mycorrhizal fungal …

Warming is expected to increase the net release of carbon from peatland soils, contributing
to future warming. This positive feedback may be moderated by the response of peatland …