With a pace of about twice the observed rate of global warming, the temperature on the
Qinghai‐Tibetan Plateau (Earth's 'third pole') has increased by 0.2° C per decade over the …

Contents Summary 35 I. Introduction 36 II. Tree CH4 fluxes 36 III. Tree emissions of soil‐
produced CH4 40 IV. Tree‐produced CH4 42 V. Trees in forest CH4 budgets 44 VI …

Currently, the global annual flux of methane (CH 4) to the atmosphere is fairly well
constrained at ca. 645 Tg CH 4 year− 1. However, the relative magnitudes of the fluxes …

While determining the response of soil microbes to grazer exclosure duration is critical to
understanding ecosystem restoration processes, few studies have focused on this issue …

Efforts to enhance food, fibre, and forage yields and achieve global food security have
included the conversion of natural grasslands to cultivated grasslands. The quantitative …

Plant-mediated CH 4 transport (PMT) is the dominant pathway through which soil-produced
CH 4 can escape into the atmosphere and thus plays an important role in controlling …

In this minireview, we evaluate all experimental work published on the phenomenon of
aerobic methane (CH4) generation in terrestrial plants and plant. Clearly, despite much …

Ultraviolet (UV) radiation has recently been demonstrated to drive an aerobic production of
methane (CH4) from plant tissues and pectins, as do agents that generate reactive oxygen …

Our knowledge on permafrost carbon (C) cycle is crucial for understanding its feedback to
climate warming and developing nature-based solutions for mitigating climate change. To …

The limited number of in situ measurements of greenhouse gas (GHG) flux during soil freeze-
thaw cycles in permafrost regions limits our ability to accurately predict how the alpine …