Summary: Human activities have increased reactive nitrogen (Nr) input to terrestrial ecosystems compared with the pre-industrial era. However, the fate of such Nr input remains uncertain, leading to missing sink of the global nitrogen budget. By synthesizing records of Nr burial in sediments from 303 lakes worldwide, here we show that 9.6 ± 1.1 Tg N year−1 (Tg = 1012 g) accumulated in inland water sediments from 2000 to 2010, accounting for 3%–5% of global Nr input to the land from combined natural and anthropogenic pathways. The recent Nr burial flux doubles pre-industrial estimates, and Nr burial rate significantly increases with global increases in human population and air temperature. Sediment ratios of C:N decrease after 1950 while N:P...
Human activity has fundamentally altered the global phosphorus (P) cycle. Yet our understanding of w...
Several national-scale studies have shown that reactive N is accumulating in developed countries eve...
International audience[1] Atmospheric O 2 trend measurements are used to partition global oceanic an...
Human activities have increased reactive nitrogen (Nr) input to terrestrial ecosystems compared with...
Human activities have doubled the pre-industrial supply of reactive nitrogen on Earth, and future ra...
Human activities have doubled the pre-Industrial supply of reactive nitrogen on Earth, and future ra...
Lakes have a disproportionate effect on the global carbon (C) cycle relative to their area, mediatin...
Declining atmospheric nitrogen (N) deposition in northern Europe and parts of North America, coupled...
Atmospheric deposition is a primary source of reactive nitrogen (Nr) to undisturbed watersheds of th...
<p>To fully understand coupling between P and other macronutrients it is nece...
The south?east margin of Tibet is highly sensitive to global environmental change pressures, in part...
Lakes are a crucial component of the global carbon and nitrogen cycle. As a trend of enhanced human ...
To feed an increasingly affluent population, the nitrogen input into global food production systems ...
Human activity has fundamentally altered the global phosphorus (P) cycle. Yet our understanding of w...
Several national-scale studies have shown that reactive N is accumulating in developed countries eve...
International audience[1] Atmospheric O 2 trend measurements are used to partition global oceanic an...
Human activities have increased reactive nitrogen (Nr) input to terrestrial ecosystems compared with...
Human activities have doubled the pre-industrial supply of reactive nitrogen on Earth, and future ra...
Human activities have doubled the pre-Industrial supply of reactive nitrogen on Earth, and future ra...
Lakes have a disproportionate effect on the global carbon (C) cycle relative to their area, mediatin...
Declining atmospheric nitrogen (N) deposition in northern Europe and parts of North America, coupled...
Atmospheric deposition is a primary source of reactive nitrogen (Nr) to undisturbed watersheds of th...
<p>To fully understand coupling between P and other macronutrients it is nece...
The south?east margin of Tibet is highly sensitive to global environmental change pressures, in part...
Lakes are a crucial component of the global carbon and nitrogen cycle. As a trend of enhanced human ...
To feed an increasingly affluent population, the nitrogen input into global food production systems ...
Human activity has fundamentally altered the global phosphorus (P) cycle. Yet our understanding of w...
Several national-scale studies have shown that reactive N is accumulating in developed countries eve...
International audience[1] Atmospheric O 2 trend measurements are used to partition global oceanic an...