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 …

Peatlands contain one-third of soil carbon (C), mostly buried in deep, saturated anoxic
zones (catotelm). The response of catotelm C to climate forcing is uncertain, because prior …

Understand the current concept of wetland and methods for identifying, describing,
classifying, and delineating wetlands in the United States with Wetland Indicators-capturing …

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

Background Peatlands are expected to experience sustained yet fluctuating higher
temperatures due to climate change, leading to increased microbial activity and greenhouse …

Peatlands contain one-third of the world's soil carbon (C). If destabilized, decomposition of
this vast C bank could accelerate climate warming; however, the likelihood of this outcome …

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 …

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 …