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https://hdl.handle.net/20.500.14094/0100495841
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2025-05-23
14:35 集計
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0100495841 (fulltext)
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4.25 MB
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メタデータID
0100495841
アクセス権
open access
出版タイプ
Version of Record
タイトル
Organo-metal coprecipitation contributes to stable organic carbon fraction in mangrove soil
著者
Hamada, Kota ; Yimatsa, Nada ; Ohtsuka, Toshiyuki ; Fujitake, Nobuhide ; Miyajima, Toshihiro ; Yokoyama, Yusuke ; Miyairi, Yosuke ; Kida, Morimaru
著者名
Hamada, Kota
著者名
Yimatsa, Nada
著者名
Ohtsuka, Toshiyuki
著者ID
A1193
研究者ID
1000050243332
ORCID
0000-0002-4089-1579
KUID
https://kuid-rm-web.ofc.kobe-u.ac.jp/search/detail.html?systemId=ca5ed552c91130b5520e17560c007669
著者名
Fujitake, Nobuhide
藤嶽, 暢英
フジタケ, ノブヒデ
所属機関名
農学研究科
著者名
Miyajima, Toshihiro
著者名
Yokoyama, Yusuke
著者名
Miyairi, Yosuke
著者ID
A2972
研究者ID
1000070903730
ORCID
0000-0002-9908-2012
KUID
https://kuid-rm-web.ofc.kobe-u.ac.jp/search/detail.html?systemId=0de2b24ca0c466ec520e17560c007669
著者名
Kida, Morimaru
木田, 森丸
キダ, モリマル
所属機関名
農学研究科
言語
English (英語)
収録物名
CATENA
巻(号)
256
ページ
109075
出版者
Elsevier B.V.
刊行日
2025-08
公開日
2025-05-13
抄録
Prediction of the impact of anthropogenic disturbances and global change on Organic Carbon (OC) pools in mangrove soils requires a detailed understanding of the mechanisms underlying OC stabilization. Using density fractionation to physically separate OC fractions with varying degrees of mineral association and protection, this study aimed to assess distributions of these fractions and the geochemical factors influencing the most dominant and refractory mineral-associated, High-density Fraction (HF). We conducted forest-wide soil sampling in the Gaburumata mangrove forest on Ishigaki Island, Japan, along three transects (upstream, midstream, downstream) and at five depths (until 100 cm). The OC in HF (OCHF) was the oldest (median Δ14C value of −13.81 ‰) and contributed most significantly to bulk soil OC (43 %-63 %) and total nitrogen (64 %-85 %). Among the extractable metals analyzed (aluminum [Al], iron [Fe], calcium [Ca], and magnesium [Mg]) with different crystallinity, only organically complexed Al and Fe showed strong positive correlations with OCHF. Together with high OCHF:Fe ratios that surpassed the maximum sorptive capacity of Fe oxides, these results indicate that co-precipitation of OC and Fe was the dominant mode of organo-mineral associations. The low clay content reduced the importance of Ca and Mg on OCHF, as these divalent cations typically facilitate OC stabilization through cation bridging between negatively charged clay surfaces and organic matter. Furthermore, the Δ14C–OC relationship suggested efficient incorporation of mangrove-derived modern C into HF, in addition to the pre-existing old C. Thus, mangrove expansion may enhance stable soil OC pools as well as increase plant biomass and litter. Overall, this study proposes a biogeochemical mechanism for how stable mangrove OC is newly formed, as well as maintained, with ramifications for global mangrove expansion and plantation efforts.
キーワード
Blue carbon
Coastal vegetated ecosystem
Physico-chemical protection
Radiocarbon
Reactive mineral
Stabilization mechanism
Stable isotope
カテゴリ
農学研究科
学術雑誌論文
権利
© 2025 The Authors. Published by Elsevier B.V.
This is an open access article under the Creative Commons Attribution-NonCommercial 4.0 International license
関連情報
DOI
https://doi.org/10.1016/j.catena.2025.109075
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資源タイプ
journal article
ISSN
0341-8162
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eISSN
1872-6887
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