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Journal ArticleDOI

Recuperation of nitrogen cycling in Amazonian forests following agricultural abandonment

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TLDR
The patterns of N and P cycling during secondary forest succession are similar to N- and P-cycling patterns during primary succession as soils age over thousands and millions of years, thus revealing that N availability in terrestrial ecosystems is ephemeral and can be disrupted by either natural or anthropogenic disturbances at several timescales.
Abstract
Phosphorus (P) is generally considered the most common limiting nutrient for productivity of mature tropical lowland forests growing on highly weathered soils. It is often assumed that P limitation also applies to young tropical forests, but nitrogen (N) losses during land-use change may alter the stoichiometric balance of nutrient cycling processes. In the Amazon basin, about 16% of the original forest area has been cleared, and about 30-50% of cleared land is estimated now to be in some stage of secondary forest succession following agricultural abandonment. Here we use forest age chronosequences to demonstrate that young successional forests growing after agricultural abandonment on highly weathered lowland tropical soils exhibit conservative N-cycling properties much like those of N-limited forests on younger soils in temperate latitudes. As secondary succession progresses, N-cycling properties recover and the dominance of a conservative P cycle typical of mature lowland tropical forests re-emerges. These successional shifts in N:P cycling ratios with forest age provide a mechanistic explanation for initially lower and then gradually increasing soil emissions of the greenhouse gas nitrous oxide (N(2)O). The patterns of N and P cycling during secondary forest succession, demonstrated here over decadal timescales, are similar to N- and P-cycling patterns during primary succession as soils age over thousands and millions of years, thus revealing that N availability in terrestrial ecosystems is ephemeral and can be disrupted by either natural or anthropogenic disturbances at several timescales.

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Citations
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Journal ArticleDOI

Terrestrial phosphorus limitation: mechanisms, implications, and nitrogen–phosphorus interactions

TL;DR: It is suggested that depletion, soil barriers, and low-P parent material often cause ultimate limitation because they control the ecosystem mass balance of P and cause it to be an ultimate limiting nutrient.
Journal ArticleDOI

Biomass resilience of Neotropical secondary forests

Lourens Poorter, +76 more
- 11 Feb 2016 - 
TL;DR: A biomass recovery map of Latin America is presented, which illustrates geographical and climatic variation in carbon sequestration potential during forest regrowth and will support policies to minimize forest loss in areas where biomass resilience is naturally low and promote forest regeneration and restoration in humid tropical lowland areas with high biomass resilience.
Journal ArticleDOI

A comprehensive quantification of global nitrous oxide sources and sinks

Hanquin Tian, +65 more
- 08 Oct 2020 - 
TL;DR: A global N2O inventory is presented that incorporates both natural and anthropogenic sources and accounts for the interaction between nitrogen additions and the biochemical processes that control N 2O emissions, using bottom-up, top-down and process-based model approaches.
References
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Journal ArticleDOI

The fate of phosphorus during pedogenesis

TL;DR: The fate of phosphorus during pedogenesis is considered with particular emphasis on vertical distribution within the profile Information is based on P fractionation studies involving a range of soil sequences in New Zealand forms of P in soil parent materials are discussed in relation to soil P transformations as discussed by the authors.
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Global patterns of plant leaf N and P in relation to temperature and latitude.

TL;DR: Results support the hypotheses that leaf N and P increase from the tropics to the cooler and drier midlatitudes because of temperature-related plant physiological stoichiometry and biogeographical gradients in soil substrate age and the N/P ratio increases with mean temperature and toward the equator.
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Litterfall, Nutrient Cycling, and Nutrient Limitation in Tropical Forests

Peter M. Vitousek
- 01 Feb 1984 - 
TL;DR: It is suggested that phosphorus but not nitrogen availability limits litterfall in a substantial subset of intact tropical forests, especially those in Amazonia, which appears to be particularly low in available phosphorus.
Journal ArticleDOI

Scaling of c:n:p stoichiometry in forests worldwide: implications of terrestrial redfield‐type ratios

TL;DR: Inspired by the importance of globally well-constrained carbon:nitrogen: phosphorus ratios in planktonic biomass to the understanding of nutrient cycles and biotic feedbacks in marine ecosystems, this work looked for analogous patterns in forest ecosystems worldwide and found that C:N:P ratios were as constrained as marine ratios and statistically distinct from one another.
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Global patterns of the isotopic composition of soil and plant nitrogen

TL;DR: For example, this article found that soil and plant δ15N values systematically decreased with increasing mean annual precipitation (MAP) and decreasing mean annual temperature (MAT), suggesting a systematic change in the source of plant available N (organic/NH4+ versus NO3−) with climate.
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