Regulation of desiccation-immersion cycle on the rate and fate of dissolved organic carbon release by Ulva pertusa.

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Auteurs principaux: Wang, Luyao, Peng, Chengxiang, Liu, Zhengyi, Zhang, Xiaoli, Xu, Zhaokun, Liu, Zhiyuan, Hu, Jinhuan, Qin, Song, Zhong, Zhihai
Format: Artículo científico
Langue:en
Publié: Marine environmental research 2025
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author Wang, Luyao
Peng, Chengxiang
Liu, Zhengyi
Zhang, Xiaoli
Xu, Zhaokun
Liu, Zhiyuan
Hu, Jinhuan
Qin, Song
Zhong, Zhihai
author_facet Wang, Luyao
Peng, Chengxiang
Liu, Zhengyi
Zhang, Xiaoli
Xu, Zhaokun
Liu, Zhiyuan
Hu, Jinhuan
Qin, Song
Zhong, Zhihai
Wang, Luyao
Peng, Chengxiang
Liu, Zhengyi
Zhang, Xiaoli
Xu, Zhaokun
Liu, Zhiyuan
Hu, Jinhuan
Qin, Song
Zhong, Zhihai
collection PubMed - marine biology
contents Regulation of desiccation-immersion cycle on the rate and fate of dissolved organic carbon release by Ulva pertusa. Wang, Luyao Peng, Chengxiang Liu, Zhengyi Zhang, Xiaoli Xu, Zhaokun Liu, Zhiyuan Hu, Jinhuan Qin, Song Zhong, Zhihai Ulva Carbon Desiccation Carbon Sequestration Seaweed Macroalgae widely distribute in intertidal zones, one of blue carbon organisms. However, the regulatory mechanisms of tide on the carbon sequestration of macroalgae are still unclear. This study explored the effects of desiccation-rewetting cycles induced by tide on dissolved organic carbon (DOC) release from Ulva pertusa, which is prevalent from high to low tidal zones. Results showed that during desiccation stage, the DOC release of U. pertusa varied with desiccation levels, releasing 0.082, 0.22, and 0.35 mg g FW at 0%, 40%, and 80% water loss, respectively, DOC accumulated on the surface of U. pertusa at a rate of about 0.52 mg g FW h. Following 4 h of rewetting, DOC released surges to 0.99, 2.51, and 2.10 mg g FW h. Using a stable isotope (C) tracer method, we found that most DOC released by U. pertusa come from early fixed carbon. At 40% water loss, partial DOC stemmed from newly fixed carbon. DOC composition varied with desiccation level, affecting its bioavailability. After 16 days of degradation, DOC concentrations from U. pertusa at 0%, 40%, and 80% desiccation were 1.99, 3.22, and 2.54 mg g FW, respectively. The 80% water loss showed the highest degradation rate, while the non-water-loss treatment group had the most potential to form refractory DOC. This study underlines the complex relationship between tide and the dynamics of DOC release in U. pertusa, highlighting their role in coastal carbon cycling.
format Artículo científico
id pubmed_39753009
institution PubMed
language en
publishDate 2025
publisher Marine environmental research
record_format pubmed
spellingShingle Regulation of desiccation-immersion cycle on the rate and fate of dissolved organic carbon release by Ulva pertusa.
Wang, Luyao
Peng, Chengxiang
Liu, Zhengyi
Zhang, Xiaoli
Xu, Zhaokun
Liu, Zhiyuan
Hu, Jinhuan
Qin, Song
Zhong, Zhihai
Ulva
Carbon
Desiccation
Carbon Sequestration
Seaweed
Regulation of desiccation-immersion cycle on the rate and fate of dissolved organic carbon release by Ulva pertusa. Wang, Luyao Peng, Chengxiang Liu, Zhengyi Zhang, Xiaoli Xu, Zhaokun Liu, Zhiyuan Hu, Jinhuan Qin, Song Zhong, Zhihai Ulva Carbon Desiccation Carbon Sequestration Seaweed Macroalgae widely distribute in intertidal zones, one of blue carbon organisms. However, the regulatory mechanisms of tide on the carbon sequestration of macroalgae are still unclear. This study explored the effects of desiccation-rewetting cycles induced by tide on dissolved organic carbon (DOC) release from Ulva pertusa, which is prevalent from high to low tidal zones. Results showed that during desiccation stage, the DOC release of U. pertusa varied with desiccation levels, releasing 0.082, 0.22, and 0.35 mg g FW at 0%, 40%, and 80% water loss, respectively, DOC accumulated on the surface of U. pertusa at a rate of about 0.52 mg g FW h. Following 4 h of rewetting, DOC released surges to 0.99, 2.51, and 2.10 mg g FW h. Using a stable isotope (C) tracer method, we found that most DOC released by U. pertusa come from early fixed carbon. At 40% water loss, partial DOC stemmed from newly fixed carbon. DOC composition varied with desiccation level, affecting its bioavailability. After 16 days of degradation, DOC concentrations from U. pertusa at 0%, 40%, and 80% desiccation were 1.99, 3.22, and 2.54 mg g FW, respectively. The 80% water loss showed the highest degradation rate, while the non-water-loss treatment group had the most potential to form refractory DOC. This study underlines the complex relationship between tide and the dynamics of DOC release in U. pertusa, highlighting their role in coastal carbon cycling.
title Regulation of desiccation-immersion cycle on the rate and fate of dissolved organic carbon release by Ulva pertusa.
topic Ulva
Carbon
Desiccation
Carbon Sequestration
Seaweed
url https://pubmed.ncbi.nlm.nih.gov/39753009/