It is proposed that carbon (C) sequestration in response to reactive nitrogen (Nr) deposition
in boreal forests accounts for a large portion of the terrestrial sink for anthropogenic CO 2 …

There is evidence that anthropogenic nitrogen (N) deposition enhances carbon (C)
sequestration in boreal forest soils. However, it is unclear how free‐living saprotrophs …

It is proposed that increases in anthropogenic reactive nitrogen (Nr) deposition may cause
temperate and boreal forests to sequester a globally significant quantity of carbon (C); …

The extent to which greater net primary productivity (NPP) will be sustained as the
atmospheric CO2 concentration increases will depend, in part, on the long‐term supply of N …

High levels of atmospheric nitrogen (N) deposition in Europe and North America were
maintained throughout the 1990s, and global N deposition is expected to increase by a …

The interaction between nitrogen cycling and carbon sequestration is critical in predicting
the consequences of anthropogenic increases in atmospheric CO2 (hereafter, Ca). The …

Forest soil carbon (C) pools may act as sinks for, or sources of, atmospheric carbon dioxide,
while nitrogen (N) fertilization may affect the net exchange of C in forest ecosystems. Since …

Ecology Letters (2010) 13: 819–828 Abstract Nitrogen (N) effects on ecosystem carbon (C)
budgets are critical to understand as C sequestration is considered as a mechanism to offset …

An estimate of net carbon (C) pool changes and long‐term C sequestration in trees and soils
was made at more than 100 intensively monitored forest plots (level II plots) and scaled up to …

Aim The continuous increase in anthropogenic nitrogen (N) may have a substantial impact
on soil carbon (C) fluxes; thus, understanding the dynamics of soil C fluxes under N …