Research article

Net ecosystem production and carbon dioxide fluxes in the Scheldt estuarine plume

Alberto V Borges¹ , Kevin Ruddick² , Laure-Sophie Schiettecatte¹ and Bruno Delille¹

¹  University of Liège, Chemical Oceanography Unit, Institut de Physique (B5), B-4000, Liège, Belgium

²  Management Unit of the North Sea Mathematical Models, Royal Belgian Institute for Natural Sciences, 100 Gulledelle, B-1200, Brussels, Belgium

author email corresponding author email

BMC Ecology 2008, 8:15doi:10.1186/1472-6785-8-15

Published:	8 September 2008

Abstract

Background

A time series of 4 consecutive years of measurements of the partial pressure of CO₂ (pCO₂) in the Scheldt estuarine plume is used here to estimate net ecosystem production (NEP).

Results

NEP in the Scheldt estuarine plume is estimated from the temporal changes of dissolved inorganic carbon (DIC). The strong seasonal variations of NEP are consistent with previous reports on organic carbon dynamics in the area. These variations are related to successive phytoplankton blooms that partly feed seasonally variable heterotrophy the rest of the year. On an annual time scale the Scheldt estuarine plume behaves as a net heterotrophic system sustained with organic carbon input from the Scheldt inner estuary and the Belgian coast. During one of the years of the time-series the estuarine plume behaved annually as a net autotrophic system. This anomalous ecosystem metabolic behaviour seemed to result from a combination of bottom-up factors affecting the spring phytoplankton bloom (increased nutrient delivery and more favourable incoming light conditions). This net autotrophy seemed to lead to a transient aa accumulation of organic carbon, most probably in the sediments, that fed a stronger heterotrophy the following year.

Conclusion

The present work highlights the potential of using pCO₂ data to derive detailed seasonal estimates of NEP in highly dynamic coastal environments. These can be used to determine potential inter-annual variability of NEP due to natural climatic oscillations or due to changes in anthropogenic impacts.