Abstract

Oceanic physics at fine scale; e.g. eddies, fronts, filaments; are notoriously difficult to sample. However, an increasing number of theoretical approaches hypothesize that these processes affect phytoplankton diversity which have cascading effects on regional ecosystems. In 2015, we targeted the Iroise Sea (France) and evidenced the setting up of the Ushant tidal front from the beginning of spring to late summer. Seawater samples were taken during three sampling cruises and DNA-barcoding allowed us to investigate patterns of eukaryotic phytoplankton diversity across this front. First focusing on patterns of taxonomic richness, we evidenced that the front harbored a hotspot of eukaryotic phytoplankton diversity sustained throughout summer. We then detail the ecological processes leading to the formation of this hotspot by studying shifts in community composition across the Iroise Sea. Physical mixing mingled the communities surrounding the front, allowing the formation of a local ecotone, but it was cycles of disturbances and nutrient inputs over the front that allowed a decrease in competitive exclusion, which maintained a higher diversity of rare phytoplankton taxa. These processes did not select a specific ecological strategy as inferred by a trait approach coupled to our taxonomic approach. Instead the front favored higher richness within widespread strategies, resulting in functional redundancy. We detail how fine-scale ocean physics affect phytoplankton diversity and suppose that this interplay is a major control on regional ecosystems.

Highlights

  • Oceanic physics at fine scale; e.g. eddies, fronts, filaments; are notoriously difficult to sample

  • We propose to investigate the drivers of phytoplankton diversity over a coastal tidal front

  • A sampling rosette equipped with Niskin bottles (10 L), a conductivity–temperature–depth probe (CTD) and a fluorescence sensor were used for profiling water temperature stratification, the chlorophyll a concentration and the Photosynthetically Active Radiation (PAR) over the water column (Fig. 1b,c)

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Summary

Introduction

Oceanic physics at fine scale; e.g. eddies, fronts, filaments; are notoriously difficult to sample. If previous studies have focused on phytoplankton diversity patterns at larger s­ cale[7,8,9], observations at the meso- and submeso-scale, of 100–0.1 km spatial and days to months temporal r­ anges[10], remain scarce These studies showed that oceanic phytoplankton can be strongly affected by mesoscale (i.e. large eddies, fronts)[11,12,13] and sub-mesoscale physical processes (i.e. smaller eddies, fronts, filaments)[14]. Tidal fronts in coastal areas, ranging in between the sub-mesoscale and mesoscale, are r­ ecurrent[22] and easier to target They provide a great opportunity to investigate the in-situ interplay between small-scale ocean physics and the ecological processes driving phytoplankton diversity patterns. We propose to investigate the drivers of phytoplankton diversity over a coastal tidal front

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