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Impact of Chronic and Massive Resuspension Mechanisms on the Microphytobenthos Dynamics in a Temperate Intertidal Mudflat

Authors :
Savelli, Raphael
Bertin, X.
Orvain, Francis
Gernez, P.
Dale, A.
Coulombier, T.
Pineau, P.
Lachaussée, N.
Polsenaere, Pierre
Dupuy, C.
Le fouest, V.
Savelli, Raphael
Bertin, X.
Orvain, Francis
Gernez, P.
Dale, A.
Coulombier, T.
Pineau, P.
Lachaussée, N.
Polsenaere, Pierre
Dupuy, C.
Le fouest, V.
Source :
Journal Of Geophysical Research-biogeosciences (2169-8953) (American Geophysical Union (AGU)), 2019-12 , Vol. 124 , N. 12 , P. 3752-3777
Publication Year :
2019

Abstract

Microphytobenthos (MPB) resuspension is a key mechanism in the transfer of organic matter from productive intertidal mudflats to terrestrial and marine systems. In this study, we infer on the contribution of physical and biological factors involved in the MPB resuspension. We use a physical‐biological coupled model forced by realistic meteorological and hydrodynamical forcings to simulate chronic (without any concomitant sediment resuspension) and massive (driven by bed failure) resuspension over a year. The model simulates mud surface temperature, MPB growth, and grazing by the gastropod Peringia ulvae. The model suggests that MPB resuspension is the highest in spring tides and at the flood beginning due to high current velocity and low water heights that promote waves‐sea bottom interactions. The seasonal export of MPB biomass is the highest in spring, up to threefold higher than in summer when the export is the lowest. The simulated seasonal dynamics of MPB resuspension results from the MPB biomass concentration in the sediment, physical disturbances, and the bioturbation activity by P. ulvae. Annually, 43% of the simulated MPB primary production is resuspended. The MPB resuspension (60.8 g C·m−2·yr−1) exceeds the loss by P. ulvae grazing (41.1 g C·m−2·yr−1). The model suggests that chronic and massive resuspension events are important in the synoptic to seasonal MPB dynamics in temperate intertidal mudflats. Accounting for such processes in the carbon budget assessment in the land‐ocean interface could bring new insights to our understanding of the role played by MPB in the coastal carbon cycle. Plain Language Summary Intertidal mudflats support a high biological productivity sustained mainly by microalgae living in the sediment. Microalgae form a dense biofilm at the surface of the mud during daytime low tides and fix a high quantity of inorganic carbon into organic carbon through photosynthesis. Microalgae can be resuspended along with the sediment into the se

Details

Database :
OAIster
Journal :
Journal Of Geophysical Research-biogeosciences (2169-8953) (American Geophysical Union (AGU)), 2019-12 , Vol. 124 , N. 12 , P. 3752-3777
Notes :
application/pdf, English
Publication Type :
Electronic Resource
Accession number :
edsoai.on1286174532
Document Type :
Electronic Resource
Full Text :
https://doi.org/10.1029.2019JG005369