Topic Editors

Prof. Dr. Xiaoming Zou
Department of Environmental Sciences, College of Natural Sciences, University of Puerto Rico, P.O. Box 70377, San Juan, PR 00936-8377, USA
College of Biology and the Environment, Nanjing Forestry University, Nanjing 210037, China

Climate and Substrate Control on Decomposition across Temperate and Tropical Forests

Abstract submission deadline
closed (1 September 2023)
Manuscript submission deadline
closed (1 November 2023)
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1643

Topic Information

Dear Colleagues,

Climate and substrate quality together influence soil biological activity and control plant litter decomposition. While global temperature rises, substrate quality is expected to decrease. How the increased temperature and decreased substrate quality may jointly affect the decomposition of plant and soil organic carbon has become a new challenge for ecologists and forest managers. Furthermore, biological interactions are hypothesized to play a more important role in decomposition in tropical ecosystems than in temperate ecosystems. Will global temperature warming and substrate quality reduction alter biological interactions in litter decomposition across temperate and tropical forests? The aims of this Topic issue of Forests is to bring together studies disentangling the relative role of climate/microclimate and substrate on litter decomposition in forest ecosystems and to elucidate differences in biological interactions between temperate and tropical forests. Potential topics for papers include but are not limited to:

  • Litter decomposition addressing substrate quality and climate/microclimate controls in all forest ecosystems;
  • Soil heterotrophic respiration addressing substrate quality and climate/microclimate controls in all forest ecosystems;
  • Climate control emphasizing either temperature or precipitation and their annual dynamics;
  • Microclimate controls related to land-use changes and alteration of forest communities;
  • Data on soil biota and biological interactions.

Prof. Dr. Xiaoming Zou
Prof. Dr. Honghua Ruan
Topic Editors

Keywords

  • litter decomposition
  • Q10
  • soil biota
  • soil heterotrophic respiration
  • soil fauna
  • soil microbes
  • temperate forest
  • tropical forest

Participating Journals

Journal Name Impact Factor CiteScore Launched Year First Decision (median) APC
Forests
forests
2.4 4.4 2010 16.9 Days CHF 2600
Microorganisms
microorganisms
4.1 7.4 2013 13.4 Days CHF 2700
Sustainability
sustainability
3.3 6.8 2009 20 Days CHF 2400

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Published Papers (1 paper)

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11 pages, 2907 KiB  
Article
Bedrock Type Mediates the Response of Vegetation Activity to Seasonal Precipitation in the Karst Forest
by Xiguang Yang, Xuebing Guan and Zihan Jiang
Sustainability 2024, 16(3), 1281; https://doi.org/10.3390/su16031281 - 2 Feb 2024
Viewed by 789
Abstract
Global warming is expected to enhance the severity and frequency of drought in subtropical areas; thus, understanding how vegetation growth responds to precipitation is crucial to comprehending the impact of these changes on ecosystem services, such as carbon storage. However, vegetation activity in [...] Read more.
Global warming is expected to enhance the severity and frequency of drought in subtropical areas; thus, understanding how vegetation growth responds to precipitation is crucial to comprehending the impact of these changes on ecosystem services, such as carbon storage. However, vegetation activity in subtropical karst regions in Southwest China is hard to explain when we merely consider the influence of climate and soil factors. In this study, we extended traditional research by combining bedrock data we aim to investigate the role of bedrock and its interaction with precipitation on plant growth in the Guizhou Province of China. We analyzed the differences in the precipitation–vegetation growth relationship in noncarbonate and carbonate rock regions, assessing the sensitivity of vegetation from two lithological types to drought. The results reveal that although there are no significant differences in climate and soil parameters between carbonate and noncarbonate regions, the normalized difference vegetation index (NDVI) in carbonate regions is more strongly related to precipitation (carbonate region: R2 = 0.67; noncarbonate region: R2 = 0.37), while the spring greenness–precipitation relationship show is more stable in the carbonate region. Our results show that the vegetation activity in the carbonate region is more vulnerable during the drought period, highlighting that the vegetation dynamic was not only regulated by climatic factors, and bedrock-caused water stress should be taken into account. Full article
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