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Article

Spatiotemporal Heterogeneity of Mangrove Root Sphere under a Tropical Monsoon Climate in Eastern Thailand

by
Sarawan Hongwiset
1,
Chadtip Rodtassana
1,*,
Sasitorn Poungparn
1,
Suthathip Umnouysin
2 and
Akira Komiyama
3,†
1
Department of Botany, Faculty of Science, Chulalongkorn University, Bangkok 10330, Thailand
2
Department of Biology, Faculty of Science, Silpakorn University, Nakhon Pathom 73000, Thailand
3
Faculty of Applied Biological Sciences, Gifu University, Gifu 501-1193, Japan
*
Author to whom correspondence should be addressed.
Fellow in 2019, the Emeritus Professor.
Forests 2021, 12(8), 966; https://doi.org/10.3390/f12080966
Submission received: 13 June 2021 / Revised: 14 July 2021 / Accepted: 20 July 2021 / Published: 21 July 2021
(This article belongs to the Special Issue Mangrove Wetland Restoration and Rehabilitation)

Abstract

Mangrove ecosystems under tropical monsoon climates experience changes in environmental factors, especially seasonal variations in salinity. These changes might have direct influences on the mangrove root sphere, which plays an important role in carbon dynamics and supports mangrove growth. We aimed to elucidate how the soil properties including salinity and nutrient budget affect the mangrove roots in the wet and dry seasons across the mangrove zonation (Avicennia, Rhizophora, and Xylocarpus zones). This area is in a secondary forest at the Trat River estuary, eastern Thailand. Root mass was observed at 0–10 and 10–20 cm depths across all zones and the living roots were separated into diameter classes. The soil water salinity was measured at a 10 cm depth. We analyzed the nitrogen, phosphorus, and carbon contents in the roots and soil. Spatiotemporal changes occurred due to the vegetation zonation and the variations in salinity and the content of soil available phosphorus that caused different root sphere conditions along the distance from the river. The highest root biomass was found in the riverward Avicennia zone, which was 4.8 times higher than that of the inland Xylocarpus zone in the wet season. The root necromass distribution along the zonation showed an opposite trend to that of biomass. Among seasons, the root size-class proportion differed, with high fine roots observed during the wet season. We confirmed that the root sphere showed both spatial and temporal heterogeneity. Mangrove roots, especially fine roots, interacted with changing salinity, inundation regime, and biological processes evoked by microtopographic gradients as a consequence of mangrove zonation and seasonal rainfall. Our findings indicate how the root sphere differed by specific vegetation structure in this mangrove forest. Therefore, these might provide an ecological perspective for the mangrove rehabilitation plans to facilitate below-ground carbon stock.
Keywords: root biomass; necromass; salinity; seasonality; zonation; tropical mangrove; secondary mangrove root biomass; necromass; salinity; seasonality; zonation; tropical mangrove; secondary mangrove

Share and Cite

MDPI and ACS Style

Hongwiset, S.; Rodtassana, C.; Poungparn, S.; Umnouysin, S.; Komiyama, A. Spatiotemporal Heterogeneity of Mangrove Root Sphere under a Tropical Monsoon Climate in Eastern Thailand. Forests 2021, 12, 966. https://doi.org/10.3390/f12080966

AMA Style

Hongwiset S, Rodtassana C, Poungparn S, Umnouysin S, Komiyama A. Spatiotemporal Heterogeneity of Mangrove Root Sphere under a Tropical Monsoon Climate in Eastern Thailand. Forests. 2021; 12(8):966. https://doi.org/10.3390/f12080966

Chicago/Turabian Style

Hongwiset, Sarawan, Chadtip Rodtassana, Sasitorn Poungparn, Suthathip Umnouysin, and Akira Komiyama. 2021. "Spatiotemporal Heterogeneity of Mangrove Root Sphere under a Tropical Monsoon Climate in Eastern Thailand" Forests 12, no. 8: 966. https://doi.org/10.3390/f12080966

APA Style

Hongwiset, S., Rodtassana, C., Poungparn, S., Umnouysin, S., & Komiyama, A. (2021). Spatiotemporal Heterogeneity of Mangrove Root Sphere under a Tropical Monsoon Climate in Eastern Thailand. Forests, 12(8), 966. https://doi.org/10.3390/f12080966

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