2019
DOI: 10.1016/j.envres.2019.108536
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Effect of the conversion of mangroves into shrimp farms on carbon stock in the sediment along the southern Red Sea coast, Saudi Arabia

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Cited by 46 publications
(27 citation statements)
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References 53 publications
(85 reference statements)
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“…Therefore, carbon storage of mangrove ecosystem in Sirik region was estimated 302 (Mg ha -1 ), which is signi cant and can play an important role in reducing global climate changes by carbon capture and storage. Our results point to a consideration in agreement with Eid et al (2019), that highlighted how the capacity to stored OC in arid areas is not as low as previously presented, thus enriching present available data will be of interest to draw a more reliable picture of this peculiar ecosystem.…”
Section: Total Biomass and Soil Carbon Storagesupporting
confidence: 91%
“…Therefore, carbon storage of mangrove ecosystem in Sirik region was estimated 302 (Mg ha -1 ), which is signi cant and can play an important role in reducing global climate changes by carbon capture and storage. Our results point to a consideration in agreement with Eid et al (2019), that highlighted how the capacity to stored OC in arid areas is not as low as previously presented, thus enriching present available data will be of interest to draw a more reliable picture of this peculiar ecosystem.…”
Section: Total Biomass and Soil Carbon Storagesupporting
confidence: 91%
“…Similar to other studies [40], we found that land use change from mangrove to aquaculture use represented the decrease of more than 50% of soil carbon stocks. This confirms that anthropogenic activities contribute enormously to soil carbon losses from conversion [58]. The loss of soil C stocks occurs when mangrove trees are cut down and large quantities of soil is removed for construction of ponds.…”
Section: Soil Carbonsupporting
confidence: 54%
“…With northerly winds in the winter and southerly winds in the summer [51], most of the limited rainfall for Saudi Arabia's south-western regions is due to monsoons in the Indian Ocean; a further gradient from north to south is produced by this environment, with substantially greater rainfall in the south [18]. In addition to the environmental factors, many human activities (such as camel and livestock grazing, depositing waste along the beaches and in the sea, and shrimp farming) increase the pressure on the ecosystems here [52,53]. The result of the combination of these factors, as discussed by Shaltout et al [54], is that the northern region is much less hospitable to plant life than the south.…”
Section: Study Areamentioning
confidence: 99%