Root exudates in mangrove forests accelerate bicarbonate production in the soil environment
Abstract Mangrove forests are increasingly recognized as vital blue carbon ecosystems due to their high carbon sequestration capacity, primarily through the accumulation of soil organic carbon (SOC). Recent research highlights that, in addition to SOC, dissolved inorganic carbon (DIC), particularly...
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2024-12-01
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author | Norihiro Kato Ken’ichi Osaka Toshiyuki Ohtsuka Yasuo Iimura |
author_facet | Norihiro Kato Ken’ichi Osaka Toshiyuki Ohtsuka Yasuo Iimura |
author_sort | Norihiro Kato |
collection | DOAJ |
description | Abstract Mangrove forests are increasingly recognized as vital blue carbon ecosystems due to their high carbon sequestration capacity, primarily through the accumulation of soil organic carbon (SOC). Recent research highlights that, in addition to SOC, dissolved inorganic carbon (DIC), particularly in the form of bicarbonate (HCO₃⁻), plays a crucial role in carbon sequestration by being exported from these ecosystems to adjacent coastal waters. This study aims to investigate the previously unexamined mechanisms behind bicarbonate production in mangrove soils. We test the hypothesis that root exudates, specifically sugars and organic acids, induce a priming effect that enhances DIC production. We conducted a month-long incubation experiment using soil samples from an estuarine mangrove forest in Japan, under varying salinity levels and root exudate treatments. During the incubation period, the total amounts of DIC, HCO₃⁻, and carbonic acid (H₂CO₃) detected per vial in each treatment ranged from 30.0 to 43.9 mg C, 26.6 to 39.7 mg C, and 1.9 to 4.4 mg C, respectively, with HCO₃⁻ accounting for approximately 90% of the DIC. These values tended to be higher under high salinity conditions resembling seawater levels. In particular, the treatment with a complex solution of root exudates and high salinity (h-ASW + c-REC) showed the highest average values for all forms of DIC. Furthermore, in the h-ASW + c-REC treatment, HCO₃⁻ increased significantly (P < 0.005) by approximately 20% compared to the control without added root exudates. Additionally, changes in water quality parameters—including increased NH₄⁺ levels and decreased dissolved oxygen and oxidation-reduction potential—provided further support for the priming effect hypothesis. This study is the first to demonstrate that root exudates promote bicarbonate production in mangrove soils, offering new insights into the complex carbon and nutrient dynamics in these ecosystems. |
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institution | Kabale University |
issn | 2045-2322 |
language | English |
publishDate | 2024-12-01 |
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spelling | doaj-art-18f3beb401644344967a968f7a6b515e2025-01-05T12:26:06ZengNature PortfolioScientific Reports2045-23222024-12-0114111410.1038/s41598-024-82873-yRoot exudates in mangrove forests accelerate bicarbonate production in the soil environmentNorihiro Kato0Ken’ichi Osaka1Toshiyuki Ohtsuka2Yasuo Iimura3Gradutate School of Environmental Science, The University of Shiga PrefectureSchool of Environmental Science, The University of Shiga PrefectureInstitute for Advanced Study, Gifu UniversitySchool of Environmental Science, The University of Shiga PrefectureAbstract Mangrove forests are increasingly recognized as vital blue carbon ecosystems due to their high carbon sequestration capacity, primarily through the accumulation of soil organic carbon (SOC). Recent research highlights that, in addition to SOC, dissolved inorganic carbon (DIC), particularly in the form of bicarbonate (HCO₃⁻), plays a crucial role in carbon sequestration by being exported from these ecosystems to adjacent coastal waters. This study aims to investigate the previously unexamined mechanisms behind bicarbonate production in mangrove soils. We test the hypothesis that root exudates, specifically sugars and organic acids, induce a priming effect that enhances DIC production. We conducted a month-long incubation experiment using soil samples from an estuarine mangrove forest in Japan, under varying salinity levels and root exudate treatments. During the incubation period, the total amounts of DIC, HCO₃⁻, and carbonic acid (H₂CO₃) detected per vial in each treatment ranged from 30.0 to 43.9 mg C, 26.6 to 39.7 mg C, and 1.9 to 4.4 mg C, respectively, with HCO₃⁻ accounting for approximately 90% of the DIC. These values tended to be higher under high salinity conditions resembling seawater levels. In particular, the treatment with a complex solution of root exudates and high salinity (h-ASW + c-REC) showed the highest average values for all forms of DIC. Furthermore, in the h-ASW + c-REC treatment, HCO₃⁻ increased significantly (P < 0.005) by approximately 20% compared to the control without added root exudates. Additionally, changes in water quality parameters—including increased NH₄⁺ levels and decreased dissolved oxygen and oxidation-reduction potential—provided further support for the priming effect hypothesis. This study is the first to demonstrate that root exudates promote bicarbonate production in mangrove soils, offering new insights into the complex carbon and nutrient dynamics in these ecosystems.https://doi.org/10.1038/s41598-024-82873-yMangrove forestsDissolved inorganic carbon (DIC)Bicarbonate (HCO₃⁻)Root exudateSoil organic carbon (SOC)Priming effect |
spellingShingle | Norihiro Kato Ken’ichi Osaka Toshiyuki Ohtsuka Yasuo Iimura Root exudates in mangrove forests accelerate bicarbonate production in the soil environment Scientific Reports Mangrove forests Dissolved inorganic carbon (DIC) Bicarbonate (HCO₃⁻) Root exudate Soil organic carbon (SOC) Priming effect |
title | Root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
title_full | Root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
title_fullStr | Root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
title_full_unstemmed | Root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
title_short | Root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
title_sort | root exudates in mangrove forests accelerate bicarbonate production in the soil environment |
topic | Mangrove forests Dissolved inorganic carbon (DIC) Bicarbonate (HCO₃⁻) Root exudate Soil organic carbon (SOC) Priming effect |
url | https://doi.org/10.1038/s41598-024-82873-y |
work_keys_str_mv | AT norihirokato rootexudatesinmangroveforestsacceleratebicarbonateproductioninthesoilenvironment AT kenichiosaka rootexudatesinmangroveforestsacceleratebicarbonateproductioninthesoilenvironment AT toshiyukiohtsuka rootexudatesinmangroveforestsacceleratebicarbonateproductioninthesoilenvironment AT yasuoiimura rootexudatesinmangroveforestsacceleratebicarbonateproductioninthesoilenvironment |