Abstract
Intensified coastal eutrophication can result in an overgrowth of seagrass leaves by epiphytes, which is a major threat to seagrass habitats worldwide, but little is known about how epiphytic biofilms affect the seagrass phyllosphere. The physico-chemical microenvironment of Zostera marina L. leaves with and without epiphytes was mapped with electrochemical, thermocouple and scalar irradiance microsensors as a function of four irradiance conditions (dark, low, saturating and high light) and two water flow velocities (approx. 0.5 and 5 cm s -1), which resemble field conditions. The presence of epiphytes led to the build up of a diffusive boundary layer and a thermal boundary layer which impeded O 2 and heat transfer between the leaf surface and the surrounding water, resulting in a maximum increase of 0.8°C relative to leaves with no epiphytes. Epiphytes also reduced the quantity and quality of light reaching the leaf, decreasing plant photosynthesis. In darkness, epiphyte respiration exacerbated hypoxic conditions, which can lead to anoxia and the production of potential phytotoxic nitric oxide in the seagrass phyllosphere. Epiphytic biofilm affects the local phyllosphere physico-chemistry both because of its metabolic activity (i.e. photosynthesis/respiration) and its physical properties (i.e. thickness, roughness, density and back-scattering properties). Leaf tissue warming can lead to thermal stress in seagrasses living close to their thermal stress threshold, and thus potentially aggravate negative effects of global warming.
Originalsprog | Engelsk |
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Artikelnummer | 20200485 |
Tidsskrift | Journal of the Royal Society Interface |
Vol/bind | 17 |
Udgave nummer | 171 |
ISSN | 1742-5689 |
DOI | |
Status | Udgivet - 1 okt. 2020 |
Udgivet eksternt | Ja |
Bibliografisk note
Funding Information:The study was funded by a grant from the Carlsberg Foundation (CF16-0899; K.E.B.), the Villum Foundation (grant no. 00028156; K.E.B.) and by a grant from the Independent Research Fund Denmark (grant no. DFF-1323-00065B; M.K.). F.N. was supported by the European Union’s Horizon 2020 research and innovation programme under the Marie Skłodowska-Curie grant agreement (no. 701366), as well as, the IMAP network from the Future Ocean Cluster. A.D. was supported by the Swiss National Science Foundation.