Dynamics of Calcium, Magnesium, and Manganese During Litter Decomposition in Alpine Forest Aquatic and Terrestrial Ecosystems

Plant litter decomposition is one of the most important ecosystem processes influencing elemental biogeochemistry across terrestrial and aquatic environments. Calcium (Ca), magnesium (Mg), and manganese (Mn) are essential nutrients, which play a key role in plant energy metabolism, photosynthesis, a...

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Published inEcosystems (New York) Vol. 24; no. 3; pp. 516 - 529
Main Authors Yue, Kai, Ni, Xiangyin, Fornara, Dario A., Peng, Yan, Liao, Shu, Tan, Siyi, Wang, Dingyi, Wu, Fuzhong, Yang, Yusheng
Format Journal Article
LanguageEnglish
Published New York Springer Science + Business Media 01.04.2021
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Abstract Plant litter decomposition is one of the most important ecosystem processes influencing elemental biogeochemistry across terrestrial and aquatic environments. Calcium (Ca), magnesium (Mg), and manganese (Mn) are essential nutrients, which play a key role in plant energy metabolism, photosynthesis, and membrane transport of plants, and the major source of these nutrients is litter decomposition. Although litter decomposition has been subject to extensive research over the last several decades, the dynamics of Ca, Mg, and Mn in decomposing litter has been poorly assessed. Also, very few decomposition studies have been simultaneously carried out across aquatic and terrestrial ecosystems. Here, we conducted a two-year litterbag experiment across alpine forest aquatic (stream and riparian zone) and terrestrial (forest floor) ecosystems to address the dynamics of Ca, Mg, and Mn during litter decomposition. We found that (1) in general concentrations of Ca, Mg, and Mn all increased (that is, high immobilization) during the period of decomposition; (2) Ca and Mn immobilized in decomposing litter regardless of ecosystem type or litter species identity, while Mg showed release (mineralization) or immobilization depending on litter species identity; (3) a common hierarchy of drivers for Ca, Mg, or Mn release rate was found across all ecosystem types; and (4) Ca, Mg, and Mn concentrations all showed positive relationships with litter decomposition. Our results provide evidence of general patterns of Ca, Mg, and Mn dynamics in decomposing litter and significant positive effects of these nutrients on litter decomposition across terrestrial and aquatic environments associated with a forest ecosystem. We suggest that addressing nutrient dynamics across contrasting environments is crucial for predicting how biogeochemical cycling of different nutrients is modulated by litter mass decomposition.
AbstractList Plant litter decomposition is one of the most important ecosystem processes influencing elemental biogeochemistry across terrestrial and aquatic environments. Calcium (Ca), magnesium (Mg), and manganese (Mn) are essential nutrients, which play a key role in plant energy metabolism, photosynthesis, and membrane transport of plants, and the major source of these nutrients is litter decomposition. Although litter decomposition has been subject to extensive research over the last several decades, the dynamics of Ca, Mg, and Mn in decomposing litter has been poorly assessed. Also, very few decomposition studies have been simultaneously carried out across aquatic and terrestrial ecosystems. Here, we conducted a two-year litterbag experiment across alpine forest aquatic (stream and riparian zone) and terrestrial (forest floor) ecosystems to address the dynamics of Ca, Mg, and Mn during litter decomposition. We found that (1) in general concentrations of Ca, Mg, and Mn all increased (that is, high immobilization) during the period of decomposition; (2) Ca and Mn immobilized in decomposing litter regardless of ecosystem type or litter species identity, while Mg showed release (mineralization) or immobilization depending on litter species identity; (3) a common hierarchy of drivers for Ca, Mg, or Mn release rate was found across all ecosystem types; and (4) Ca, Mg, and Mn concentrations all showed positive relationships with litter decomposition. Our results provide evidence of general patterns of Ca, Mg, and Mn dynamics in decomposing litter and significant positive effects of these nutrients on litter decomposition across terrestrial and aquatic environments associated with a forest ecosystem. We suggest that addressing nutrient dynamics across contrasting environments is crucial for predicting how biogeochemical cycling of different nutrients is modulated by litter mass decomposition.
Audience Academic
Author Yue, Kai
Ni, Xiangyin
Peng, Yan
Yang, Yusheng
Fornara, Dario A.
Tan, Siyi
Wang, Dingyi
Wu, Fuzhong
Liao, Shu
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  givenname: Kai
  surname: Yue
  fullname: Yue, Kai
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  givenname: Xiangyin
  surname: Ni
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  givenname: Dario A.
  surname: Fornara
  fullname: Fornara, Dario A.
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  givenname: Yan
  surname: Peng
  fullname: Peng, Yan
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  givenname: Shu
  surname: Liao
  fullname: Liao, Shu
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  surname: Wu
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Keywords Litter species
Microbe
Concentration
Ecosystem type
Release rate
Structural equation modeling
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Snippet Plant litter decomposition is one of the most important ecosystem processes influencing elemental biogeochemistry across terrestrial and aquatic environments....
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Index Database
Publisher
StartPage 516
SubjectTerms Aquatic ecosystems
Aquatic environment
Aquatic plants
Biogeochemical cycles
Biogeochemistry
Biomedical and Life Sciences
Calcium
Calcium signalling
Decomposition
Dynamics
Ecology
Ecosystems
Energy metabolism
Environmental Management
Essential nutrients
Forest ecology
Forest ecosystems
Forest floor
forest litter
Forests
Geoecology/Natural Processes
Hydrology/Water Resources
Immobilization
Life Sciences
Litter
Magnesium
Manganese
Mineralization
Nutrient cycles
Nutrient dynamics
Nutrients
Original Articles
Photosynthesis
Physiological aspects
Plant Sciences
riparian areas
Riparian forests
Riparian land
streams
Structural equation modeling
Terrestrial ecosystems
Terrestrial environments
Zoology
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Title Dynamics of Calcium, Magnesium, and Manganese During Litter Decomposition in Alpine Forest Aquatic and Terrestrial Ecosystems
URI https://www.jstor.org/stable/48761992
https://link.springer.com/article/10.1007/s10021-020-00532-5
https://www.proquest.com/docview/2517102133
https://www.proquest.com/docview/2551932426
Volume 24
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