Surface elevation changes in an estuarine mangrove forest in Vanga, Kenya: Implications for management and mitigation of sea-level rise

被引:2
|
作者
Kimeli, Amon Kibiwot [1 ,2 ,3 ]
Cherono, Shawlet [3 ]
Baya, Patience [3 ]
Mathinji, Margaret [3 ]
Okello, Judith Auma [3 ]
Koedam, Nico [4 ]
Westphal, Hildegard [1 ,2 ,5 ]
Kairo, James Gitundu [3 ]
机构
[1] Univ Bremen, Fac Geosci, Bremen, Germany
[2] Leibniz Ctr Trop Marine Res ZMT, Biogeochem & Geol Dept, Bremen, Germany
[3] Kenya Marine & Fisheries Res Inst, Oceanog & Hydrog Dept, Mombasa, Kenya
[4] Vrije Univ Brussels, Fac Biol, Brussels, Belgium
[5] King Abdullah Univ Sci & Technol KAUST, Phys Sci & Engn PSE, Thuwal, Saudi Arabia
关键词
sediments; accretion; mangroves; Vanga; Kenya; sea-level rise; elevation; shallow subsidence; CLIMATE-CHANGE; RATES; ACCRETION; SEDIMENTATION; VULNERABILITY; ACCUMULATION; RESTORATION; DEGRADATION; RESILIENCE; RESPONSES;
D O I
10.3389/fmars.2022.932963
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
Mangrove ecosystems are often called "makers of land" due to their ability to promote deposition, trap, and augment sediments. Accurate location- and region-specific elevation information is required to assess and mitigate threats to mangroves caused by their vulnerability to sea-level rise. The provision of land building services by mangroves is primarily sediment-dependent. It is therefore influenced by local factors, including sediment availability and supply. In the present study from Kenya, we measured and examined the variations in surface elevation in mangroves at variable distances from the creek channel using a combination of surface-elevation tables and horizon markers for three years. Elevation changes varied with distance from the creek channel (p < 0.05), with both surface loss and gains recorded. Elevation changes varied between -80 mm (most significant subsidence) and 42 mm (highest accretion) in stations closer to the creek, while farther from the creek (similar to 200 m away), elevation changes ranged between -68 mm (most significant subsidence) and 29 mm (highest accretion). However, net surface elevation changes over the three years showed that shallow subsidence occurred in both stations closer to the creek (-45 +/- 7.2 mm) and those farthest from the creek (-20 +/- 7.1 mm). At the same time, an average of 18 mm of sediments were accreted above the horizon markers translating to similar to 9 mm yr(-1) of accretion, a rate larger than both the current global rates of sea-level rise (similar to 3.1 mm yr(-1)) and local measured rates of sea-level rise (3.8 mm yr(-1)) in Mombasa, a tide-gauge station nearest (similar to 100 km) to the study site. Cumulatively, sediment elevation changes in Vanga indicate that they are outpacing the current rates of sea-level rise. However, they could be vulnerable to predicted and accelerated rates. It, therefore, calls for more holistic management and monitoring of the dynamics within the mangrove forests and adjacent terrestrial hinterlands.
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页数:14
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