

FOLLOWUS
1.School of Atmospheric Sciences, Sun Yat-sen University, Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
2.School of Ecology, Shenzhen Campus of Sun Yat-sen University, Shenzhen 518107, China
3.Hainan International Blue Carbon Research Center, Hainan Research Academy of Environmental Sciences, Haikou 571126, China
4.School of Marine Sciences, Sun Yat-sen University, Southern Marine Science and Engineering Guangdong Laboratory (Zhuhai), Zhuhai 519082, China
5.State Key Laboratory of Isotope Geochemistry, Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, Guangzhou 510640, China
6.Climate Center of Hainan Province, Key Laboratory of Meteorological Disaster Prevention and Reduction in South China Sea, Haikou 570203, China
lhxie@gig.ac.cn
wangfan25@mail.sysu.edu.cn
Received:25 September 2024,
Accepted:06 January 2025,
Online First:12 March 2025,
Published:01 January 2026
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SU Juan,LIN Yaobei,LI Penghui,et al.The centennial legacy of disturbances on sedimentation and carbon burial in an estuarine mangrove ecosystem, South China[J].Journal of Oceanology and Limnology,2026,44(01):109-124.
SU Juan,LIN Yaobei,LI Penghui,et al.The centennial legacy of disturbances on sedimentation and carbon burial in an estuarine mangrove ecosystem, South China[J].Journal of Oceanology and Limnology,2026,44(01):109-124. DOI: 10.1007/s00343-025-4258-2.
Both natural and human-induced disturbances affect the normal functioning and services of mangrove ecosystems. To address the consequences of intense human and climatic disturbances on sedimentation and carbon burial
sediment cores from the last remaining mangrove
Kandelia
obovata
forest and an adjacent mudflat in the densely populated and typhoon-prone Zhujiang (Pearl) River estuary of China
were analyzed using methods including
210
Pb dating and δ
13
C analysis. Results indicate that after damming in the 1950s
during 1960–1980
the natural establishment of
K
.
obovata
forests initiated the in-situ sedimentation. As these forests matured during 1980–1990
they significantly boosted siltation in the region on mudflat. During 1990–2015
the invasion of
Spartina
alterniflora
and land reclamation for aquaculture caused infiltration of coarse sediments and the impacts of typhoons were recorded within the
K
.
obovata
forest
while no clear typhoon record was observed on the mudflat. Since 2015
reforestation efforts with
S
.
apetala
that began in 1999 have reversed the effects of earlier deforestation. Over time
mangroves established a rapid autochthonous carbon burial that grew as the forests age
potentially surpassing the influx of allochthonous carbon due to deforestation. The reforestation also immediately improved carbon burial on the mudflat
which stabilized after a decade due to the rapid growth and high biomass of
S
.
apetala
. Overall
the
K
.
obovata
forest demonstrated a stronger sedimentation and carbon burial capabilities than the mudflat
with a surplus of 35.2 Mg C/hm
2
in soil organic carbon stock and 1.0 Mg C/(hm
2
·a
) in burial rate. Organic matter dissolved in soil was mainly humus-like components
and mangrove inputs likely increased the degree of humification. This study offered direct evidence regarding the impact of multiple disturbances on local and regional sedimentation and carbon burial
and future management strategies.
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