Soil and Vegetative Carbon Sequestration in Khuran Estuary Mangroves, Strait of Hormoz, During the Last 18 Centuries

The present paper, for the first time, estimates the amount of soil and vegetative blue carbon (C) sequestered in Khuran mangrove, Iran’s largest mangrove forest along the Persian Gulf coasts. Cores were retrieved down to parental materials in 32 stations to achieve whole-soil C stock. A radiocarbon...

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Veröffentlicht in:Estuaries and coasts 2022-09, Vol.45 (6), p.1583-1595
Hauptverfasser: Hamzeh, M. A., Lahijani, H. A. K.
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description The present paper, for the first time, estimates the amount of soil and vegetative blue carbon (C) sequestered in Khuran mangrove, Iran’s largest mangrove forest along the Persian Gulf coasts. Cores were retrieved down to parental materials in 32 stations to achieve whole-soil C stock. A radiocarbon dating was also used to estimate sediment accretion and C sequestration rates during the last 18 centuries. Results indicated that soils and mangrove trees of the Khuran store a total of 16.79 Tg C (equivalent to ~ 60 Tg of CO 2 ), 98.8% of which (16.59 Tg C) is sequestered in mangrove soils. During the last couple of thousand years, 8967 Mg C year −1 (one Mg C ha −1  year −1 ) has been stored in mangrove soils of the area. Mean whole-soil C stock in Khamir and Qeshm is 1076 and 2134 Mg C ha −1 , respectively. A total of 5181 Gg C and 201 Gg C is stored in the top 1 m of soil and mangrove trees, respectively, 76% of which is sequestered in QM. Our results also indicate that mangroves located in desert and dryland coasts can store comparable quantities of belowground C than their tropical counterparts. High phytoplankton concentration and accreting mangrove high organic C content soils on their own accumulated peat in response to sea-level rise have possibly caused Khuran desert mangroves to store large amounts of C in their sediments. Our estimates suggest that probable complete deforestation of Khuran mangrove could lead to 8.14 Tg CO 2 equivalent emissions.
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A total of 5181 Gg C and 201 Gg C is stored in the top 1 m of soil and mangrove trees, respectively, 76% of which is sequestered in QM. Our results also indicate that mangroves located in desert and dryland coasts can store comparable quantities of belowground C than their tropical counterparts. High phytoplankton concentration and accreting mangrove high organic C content soils on their own accumulated peat in response to sea-level rise have possibly caused Khuran desert mangroves to store large amounts of C in their sediments. 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A.</au><au>Lahijani, H. A. K.</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Soil and Vegetative Carbon Sequestration in Khuran Estuary Mangroves, Strait of Hormoz, During the Last 18 Centuries</atitle><jtitle>Estuaries and coasts</jtitle><stitle>Estuaries and Coasts</stitle><date>2022-09-01</date><risdate>2022</risdate><volume>45</volume><issue>6</issue><spage>1583</spage><epage>1595</epage><pages>1583-1595</pages><issn>1559-2723</issn><eissn>1559-2731</eissn><abstract>The present paper, for the first time, estimates the amount of soil and vegetative blue carbon (C) sequestered in Khuran mangrove, Iran’s largest mangrove forest along the Persian Gulf coasts. Cores were retrieved down to parental materials in 32 stations to achieve whole-soil C stock. A radiocarbon dating was also used to estimate sediment accretion and C sequestration rates during the last 18 centuries. 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subjects Accretion
Arid zones
Blue carbon
Carbon dioxide
Carbon sequestration
Coastal Sciences
Coasts
Deforestation
Deposition
Deserts
Earth and Environmental Science
Ecology
Ecosystems
Emissions
Environment
Environmental Management
Equivalence
Estimates
Estuaries
Estuarine dynamics
Forests
Freshwater & Marine Ecology
Mangrove swamps
Mangrove trees
Mangroves
Ocean currents
Organic soils
Peat
Phytoplankton
Radiocarbon dating
Radiometric dating
Sea level changes
Sediment
Sediments
Soil
Soils
Trees
Tropical climate
Water and Health
title Soil and Vegetative Carbon Sequestration in Khuran Estuary Mangroves, Strait of Hormoz, During the Last 18 Centuries
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