Affiliations 

  • 1 Institute of Marine Geology and Resources, Ocean College, Zhejiang University, Zhoushan 316021, China
  • 2 Coastal Oceanography and Climate Change Research Center, Faculty of Environmental Management, Prince of Songkla University, Songkhla 90110, Thailand. Electronic address: siriporn.pra@psu.ac.th
  • 3 Institute of Marine Geology and Resources, Ocean College, Zhejiang University, Zhoushan 316021, China. Electronic address: psloh@zju.edu.cn
  • 4 Institute of Natural Product Chemistry, Vietnam Academy of Science and Technology, Hanoi 11307, Viet Nam
  • 5 Faculty of Hydrology and Water Resources Engineering, Institute of Technology of Cambodia, Phnom Penh 12156, Cambodia
  • 6 Faculty of Science and Technology, Universiti Kebangsaan Malaysia, Bangi 43600, Malaysia
  • 7 Faculty of Science, Universiti Malaya, Kuala Lumpur 50603, Malaysia; Institute of Ocean and Earth Sciences, Universiti Malaya, Kuala Lumpur 50603, Malaysia
  • 8 Department of Geography, National University of Singapore, Singapore 119260, Singapore
  • 9 Soil Science Department, Faculty of Agriculture, Tanjungpura University, Pontianak 78124, Indonesia
  • 10 Department of Geology, School of Earth Sciences, Central University of Tamil Nadu, Neelakudi, Thiruvarur 610005, India
  • 11 Jiangsu Key Laboratory of Crop Genetics and Physiology/Jiangsu Key Laboratory of Crop Cultivation and Physiology, Agricultural College of Yangzhou University, Yangzhou 225009, China; Jiangsu Co-Innovation Centre for Modern Production Technology of Grain Crops, Yangzhou University, Yangzhou 225009, China
Mar Pollut Bull, 2024 Jan 29;200:116064.
PMID: 38290368 DOI: 10.1016/j.marpolbul.2024.116064

Abstract

Mangrove forests can help to mitigate climate change by storing a significant amount of carbon (C) in soils. Planted mangrove forests have been established to combat anthropogenic threats posed by climate change. However, the efficiency of planted forests in terms of soil organic carbon (SOC) storage and dynamics relative to that of natural forests is unclear. We assessed SOC and nutrient storage, SOC sources and drivers in a natural and a planted forest in southern Thailand. Although the planted forest stored more C and nutrients than the natural forest, the early-stage planted forest was not a strong sink relative to mudflat. Both forests were predominated by allochthonous organic C and nitrogen limited, with total nitrogen being a major driver of SOC in both cases. SOC showed a significant decline along land-to-sea and depth gradients as a result of soil texture, nutrient availability, and pH in the natural forest.

* Title and MeSH Headings from MEDLINE®/PubMed®, a database of the U.S. National Library of Medicine.