Short-Term Spatiotemporal Variability in Picoplankton Induced by a Submesoscale Front South of Gran Canaria (Canary Islands)

• Published in: Frontiers in Marine Science
• Main Authors: Hernández-Hernández, Nauzet, Santana Falcon, Yeray, Estrada-Allis, Sheila, Arístegui, Javier
• Other Authors: 57194425333, 56162676800, 55953934900, 7006816204, BU-BAS
• Format: Article in Journal/Newspaper
• Language: English
• Published: 2021
• Subjects: 251001 Oceanografía biológica; Canary Islands; Frontogenesis; Frontolisis; Picoplankton; Spatiotemporal Variability; Submesoscale Front; Subtropical North Atlantic; North Atlantic
• Online Access: http://hdl.handle.net/10553/106690; https://doi.org/10.3389/fmars.2021.592703

The distribution and variability of phytoplankton in the upper layers of the ocean are highly correlated with physical processes at different time and spatial scales. Model simulations have shown that submesoscale features play a pivotal role on plankton distribution, metabolism and carbon fluxes. However, there is a lack of observational studies that provide evidence for the complexity of short-term phytoplankton distribution and variability inferred from theoretical and modeling approaches. In the present study, the development and decay of a submesoscale front south of Gran Canaria Island is tracked at scales not considered in regular oceanographic samplings in order to analyze the picoplankton response to short-term variability. Likewise, the contribution of each scale of variability to the total variance of the picophytoplankton community has been quantified. We observe statistically different picophytoplankton assemblages across stations closer than 5 km, and between time periods shorter than 24 h, which were related to high physical spatiotemporal variability. Our results suggest that both temporal and spatial variability may equally contribute to the total variance of picoplankton community in the mixed layer, while time is the principal contributor to total variance in the deep chlorophyll maximum (DCM). 15 1,558 4,912 Q1 Q1 SCIE