Benthic oxygen exchange in a live coralline algal bed and an adjacent sandy habitat: an eddy covariance study

Marine Ecology Progress Series

Nicholas A. Kamenos¹  Henrik Stahl¹  Heidi L. Burdett¹  Gavin Turner¹  Karl M. Attard¹  Ronnie N. Glud¹ 

关键词: Benthic oxygen exchange;    Benthic primary production;    Coastal carbon cycling;    Coralline algae;    Permeable sediment;    Eddy covariance;    Benthic chambers;   

DOI  :  10.3354/meps11413

学科分类：海洋学与技术

来源: Inter-Research

【 摘 要 】

ABSTRACT: Coralline algal (maerl) beds are widespread, slow-growing, structurally complex perennial habitats that support high biodiversity, yet are significantly understudied compared to seagrass beds or kelp forests. We present the first eddy covariance (EC) study on a live maerl bed, assessing the community benthic gross primary productivity (GPP), respiration (R), and net ecosystem metabolism (NEM) derived from diel EC time series collected during 5 seasonal measurement campaigns in temperate Loch Sween, Scotland. Measurements were also carried out at an adjacent (~20 m distant) permeable sandy habitat. The O₂ exchange rate was highly dynamic, driven by light availability and the ambient tidally-driven flow velocity. Linear relationships between the EC O₂ fluxes and available light indicate that the benthic phototrophic communities were lightlimited. Compensation irradiance (E_c) varied seasonally and was typically ~1.8-fold lower at the maerl bed compared to the sand. Substantial GPP was evident at both sites; however, the maerl bed and the sand habitat were net heterotrophic during each sampling campaign. Additional inputs of ~4 and ~7 mol m^-2 yr^-1 of carbon at the maerl bed and sand site, respectively, were required to sustain the benthic O₂ demand. Thus, the 2 benthic habitats efficiently entrap organic carbon and are sinks of organic material in the coastal zone. Parallel deployment of 0.1 m² benthic chambers during nighttime revealed O₂ uptake rates that varied by up to ~8-fold between replicate chambers (from -0.4 to -3.0 mmol O₂ m^-2 h^-1; n = 4). However, despite extensive O₂ flux variability on meter horizontal scales, mean rates of O₂ uptake as resolved in parallel by chambers and EC were typically within 20% of one another.

【 授权许可】

Unknown