Abstract

The analysis of a 28-year-long (1989–2016) series of monthly measurements of chlorophyll concentrations and primary production rates at a shelf station off A Coruña (NW Spain) provided evidence of changes at several time scales that were only partly related to upwelling intensity. Chlorophyll determinations were made in acetonic extracts and primary production rates by the measurement of 14C-uptake by natural phytoplankton populations in simulated in situ conditions. Wavelet analysis revealed multiple modes of variation in both series, particularly at high frequencies, but some were only significant for part of the series. For instance, the seasonal cycle was not uniform through the series despite the annual repetition of maxima and minima. At multiannual time scales, both series were divided in three quasi-decadal periods characterized by significant increases in mean values. Fluctuations in chlorophyll and primary production covaried with changes in upwelling intensity at annual scales, but annual means showed low correlation. Changes in dissolved nutrient concentrations from continental sources were the likely drivers of the observed changes in productivity at large time scales. Increases in the decadal mean rates of production and concentrations of chlorophyll were driven by increased intensity of spring blooms associated to increased nutrients and low salinity water in the surface. In contrast, blooms caused by upwelling nutrients remained unchanged along the series. This study illustrates the complexity of interactions in coastal upwelling areas at large time scales, where changes in continental nutrient inputs may affect phytoplankton production more than variations in upwelling intensity.

Highlights

  • The primary production of the global ocean is expected to change in future climate scenarios

  • The objective of this study is to analyze periodic and longterm changes in the series of phytoplankton chlorophyll and primary production rates measured off A Coruña (Galicia, NW Spain) between 1989 and 2016 in relation to changes in upwelling intensity and nutrient inputs

  • The analysis of a series spanning 28 years showed significant quasi-decadal variability in primary production in a coastal site affected by upwelling

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Summary

Introduction

The primary production of the global ocean is expected to change in future climate scenarios. 30% of the values observed for the period between 1980 and 1990, mainly due to the expansion of oligotrophic areas in the subtropical and equatorial biomes (Behrenfeld et al 2006; Polovina et al 2008; Cabré et al 2015). Such a reduction in production will translate in decreasing fisheries and mariculture production and will affect the global use of marine resources even beyond the direct demands for seafood (Chassot et al 2010; Watson et al 2015). Even when some of these changes can be attributed to photoacclimation (Behrenfeld et al 2016), the

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