C and N Functioning in Forest Ecosystems

A special issue of Forests (ISSN 1999-4907). This special issue belongs to the section "Forest Ecology and Management".

Deadline for manuscript submissions: closed (15 March 2022) | Viewed by 2106

Special Issue Editor


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Guest Editor
Ecology Systematic Evolution, Vegetal Ecophysiology department, Paris Saclay University, CNRS, Agropasparistech, 91400 Orsay, France
Interests: forest and grassland ecosystems; C and N reserve; plant soil interaction; rhizosphere; soil organic matter; soil biodiversity; climate change; forest management

Special Issue Information

Dear Colleagues,

Understanding and predicting the future role of forest ecosystems in the context of global change constitutes an important scientific challenge. The ecological and economic services (preservation of biodiversity, wood production) provided by forest ecosystems and their roles in biogeochemical cycles are considerable. Forests largely contribute to biosphere carbon exchange and the carbon stock. Ecosystem respiration almost balances photosynthetic carbon assimilation in forest ecosystems. The net ecosystem exchange is one order of magnitude lower than the two gross fluxes. Small variations in one of these two fluxes due to climatic changes would indeed strongly affect the carbon budget of the ecosystem and its ability to sequester carbon, possibly leading to positive or negative feedback. Moreover, nitrogen is a limiting factor in carbon sequestration in many forest ecosystems. In a context where carbon fixation by temperate forest ecosystems increases due to the increase in CO2 and the lengthening of the vegetation cycle, we can only speculate about the influence of nitrogen on the capacity of carbon sequestration by these forests in the near future. Deepening our knowledge on C and N functioning in forest ecosystems is crucial and must be explored on different scales, from the soil–tree system to forest ecosystems.

In this Special Issue of Forests, we propose to aggregate innovative new research on the characterization of C and N functioning in temperate, boreal, and tropical forest ecosystems. It will notably concern research on C and N cycling in forests, trees, and all the plant and soil processes involved in these cycles: internal C and N allocation, assimilation, storage, fruiting, interaction between tree and soil, tree–soil C and N transfer, forest soil organic matter dynamics, and more globally, forest ecosystems fluxes. It will include both experimental approaches and soil–vegetation–atmosphere transfer models. Indeed, these models are a key tool for predicting the response of carbon and nitrogen exchange between the biosphere and the atmosphere in response to climate change, as well as for studying the feedback between the climate and ecosystem functions. However, there is still a lack of mechanistic description concerning the carbon and nitrogen cycle and, therefore, these models are unable to accurately predict carbon residence time or the importance of the N cycle in each of the ecosystem compartments. The influence of biotic (pests) and abiotic (climate, forest management) factors on the C and N cycles can be included in the proposed studies

Dr. Stéphane Bazot
Guest Editor

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Keywords

  • C and N cycles
  • tree–soil system
  • forest ecosystem
  • allocation
  • organic matter
  • climate
  • forest management pests
  • models

Published Papers (1 paper)

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Research

13 pages, 2286 KiB  
Article
Elevation Alone Alters Leaf N and Leaf C to N Ratio of Picea crassifolia Kom. in China’s Qilian Mountains
by Yalin Niu, Jianfang Kang, Haohai Su, Jan F. Adamowski, Asim Biswas, Chunfang Liu and Jianjun Cao
Forests 2021, 12(10), 1325; https://doi.org/10.3390/f12101325 - 28 Sep 2021
Cited by 4 | Viewed by 1542
Abstract
Leaf stoichiometry of plants can respond to variation in environments such as elevation ranging from low to high and success in establishing itself in a given montane ecosystem. An evaluation of the leaf stoichiometry of Qinghai Spruce (Picea crassifolia Kom.) growing at [...] Read more.
Leaf stoichiometry of plants can respond to variation in environments such as elevation ranging from low to high and success in establishing itself in a given montane ecosystem. An evaluation of the leaf stoichiometry of Qinghai Spruce (Picea crassifolia Kom.) growing at different elevations (2400 m, 2600 m, 2800 m, 3000 m, and 3200 m) in eastern China’s Qilian Mountains, showed that leaf carbon (LC) and leaf phosphorus (LP) were similar among elevations, with ranges of 502.76–518.02 g·kg−1, and 1.00–1.43 g·kg−1, respectively. Leaf nitrogen (LN) varied with changes of elevation, with a maxima of 12.82 g·kg−1 at 2600 m and a minima of 10.74 g·kg−1 at 2800 m. The LC:LN under 2400 m and 2600 m was lower than that under other elevations, while LC:LP and LN:LP were not different among these elevations. Except for LN and LC:LN, P. crassifolia’s other leaf stoichiometries remained relatively stable across elevations, partly supporting the homeostasis hypothesis. Variations in leaf stoichiometry across elevations were mainly linked to mean annual precipitation, mean annual temperature, soil pH, and the soil organic C to soil total N ratio. P. crassifolia growth within the study area was more susceptible to P limitation. Full article
(This article belongs to the Special Issue C and N Functioning in Forest Ecosystems)
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