Arantza Iriarte

Primary plankton production, respiration and nitrification in a shallow temperate estuary during summer

Abstract Patterns of longitudinal and temporal variation in rates of primary production, respiration and nitrification were investigated in the Urdaibai estuary during August 1994. Rates of primary production, as measured with the 14C technique, varied between 0.002 and 2.828 mg C l−1 d−1. 14C and oxygen based rates of primary production showed a good correlation, but photosynthetic quotients (mean PQ of 2.2) were higher than expected from considerations of the N source used by the algae. Chlorophyll a biomass showed an inverse correlation with salinity and tidal flushing is hypothesized to be a major controlling factor of its spatial variability. Temporal variations in chlorophyll a concentration were associated primarily to changes in the lunar cycle and following rain events. Rates of community respiration varied between 0.154 and 6.857 mg O2 l−1 d−1 and were significantly and positively correlated with both bacterial abundance and chlorophyll a concentration. The relationship between respiration and primary production suggested that respiration rates based on substrates not associated with the autochthonous pelagic primary production increased greatly from the outer to the inner estuary and that the consumption of autotrophic production by heterotrophs in the water column was higher in the less productive outer estuary than in highly productive intermediate and inner areas. Except at the innermost station, temporal variations in respiration rates followed variations in temperature. The ratio of gross primary production to respiration ( GP R ) showed marked spatial and temporal variations, ranging from 0.24 to 17.94. Rates of nitrification, measured as allylthiourea sensitive rates of CO2 fixation, varied from undetectable levels to 9.3 μg C l−1 d−1.In general, highest rates of nitrification were observed at the inner estuary under conditions of elevated ammonia concentration, high bacterial abundance and high turbidity. Rates of nitrification were frequently associated with the > 3 μm size fraction. Oxygen consumed in nitrification was estimated to account on average for 4.7 ± 8.3% of total oxygen consumption.

Phytoplankton blooms in the Urdaibai estuary during summer: Physico-chemical conditions and taxa involved

In the Urdaibai estuary, despite its small volume in relation to the tidal prism, phytoplankton grows massively in the upper and intermediate zones of the estuary during summer when rainfall is low to moderate. Data obtained in 23 sampling transects along the longitudinal axis of the estuary, undertaken in July 1993 and August 1994, showed three distinct zones in terms of the phytoplankton species composition: in the upper zone the phytoplankton assemblage was dominated by the diatoms Cyclotella spp., the dinoflagellate Glenodinium foliaceum, cryptophytes and euglenophytes; in the intermediate zone the diatom Chaetoceros ceratosporus, the dinoflagellates Peridinium quinquecorne and Prorocentrum minimum and cryptophytes were the most abundant; in the lower zone diatoms such as Leptocylindricus danicus and Skeletonema costatum together with the dinoflagellates Prorocentrum spp. were dominant. The distribution and abundance of these phytoplankton forms is discussed in relation to variations in salinity, water column stratification, nutrients and temperature, which in turn vary mainly as a function of meteorological conditions (i.e. rainfall, irradiance) and tidal amplitude. The longitudinal distribution of phytoplankton cells suggests that the diatoms Cyclotella spp. and Chaetoceros ceratosporus undergo a greater dispersion along the estuary during rain events than the flagellates, thus contributing to the transport of silica to the outer areas of the estuary.

Seasonal variation of nitrification along a salinity gradient in an urban estuary

The rates of water column nitrification measured as nitrapyrin-sensitive rates of bicarbonate assimilation were monitoredalong the salinity gradient of the estuary of the RiverNervión (Bay of Biscay) from January to November 1993.Highest nitrapyrin-sensitive rates of bicarbonate assimilationwere found in the deep layer at stations located in the innerestuary during summer and autumn, coinciding with dissolvedoxygen concentrations generally lower than 1 mg O2 l−1. Possible explanation for this spatial distributionpattern are discussed. Axial and depth distribution of ammonia,nitrite and nitrate suggests that in the deep layer of theinner zone of the estuary nitrification and nitrate and nitritereduction are occurring concurrently. Nitrification showed asignificant positive correlation with temperature, but thiscorrelation was not very strong. It is argued that the wash outof nitrifying bacteria by rainfalls also plays a role in theseasonal variation of nitrification rates.

Microplankton metabolism along a trophic gradient in a shallow-temperate estuary

Microplankton metabolism was studied in the Urdaibai estuary from June 1996 to May 1997 to investigate the factors that control the autotrophic-heterotrophic balance in three zones of contrasting trophic status. Gross primary production (GPP) and dark oxygen consumption (R) were measured from the upper eutrophic reaches to the lower marine segment for unfractionated samples as well as for nanoplankton (<20 μm) and ultraplankton (<5 μm). Microplankton composition differed in the three segments and the peaks of abundance were uncoupled. Microplankton biomass both as carbon content and chlorophylla concentration decreased seaward. Size-fractionated metabolism was to a great extent conducted by the dominant species in the upper and middle reaches, where GPP and R rates were frequently coupled. In the lower marine estuary GPP experienced marked seasonal changes while R rates were rather constant and uncoupled to GPP. In the upper and lower estuary the gross primary production:respiration (P:R) ratio of the nonfractionated samples were >1 only during peak values of production, whilst in the middle estuary they were almost always ≥1. Ultraplankton was generally heterotrophic in the three zones. The relative importance of the <5 μm fraction increased seaward for both GPP and R rates. This size class was responsible for most of the oxygen consumption in the middle and lower estuary, while in the upper estuary the 5–20 μm size fraction was also relevant. During periods of enhanced phytoplankton growth, less than 20% of the total GPP was instantaneously respired in the three segments. In periods between peaks, only in the middle estuary was some percentage of the GPP not instantaneously processed. The percentage of the fractionated primary production respired in each size fraction was highly variable, although the highest values were found in the <5 μm for all stations.

Dissolved oxygen in the rehabilitation phase of an estuary: influence of sewage pollution abatement and hydro-climatic factors.

Seasonal and inter-annual variations of dissolved oxygen (DO) along the estuary of Bilbao were investigated from 1998 to 2008, during its rehabilitation phase from pollution, to determine whether anthropogenic or natural forcings or both govern DO dynamics and hypoxia. Both seasonal and inter-annual variations of DO were best explained by hydro-climatic factors, sewage pollution and phytoplankton dynamics in the inner, intermediate and outer estuary respectively. The most remarkable intra-decadal improvement in DO occurred in the halocline layer of the intermediate estuary, where the factor that best explained these changes was sewage pollution abatement. However, in the estuarine hotspot for hypoxia, i.e. inner estuary bottom waters, no parallel response to sewage pollution abatement was observed and hydro-climatic factors were the main drivers of inter-annual DO variations. Differences in the degree of stratification and flushing accounted for this differential response of DO to anthropogenic and climate-related forcings at both axial and vertical scales.

Insights on the origin of invasive copepods colonizing Basque estuaries; a DNA barcoding approach

BackgroundThe introduction of NIS to estuaries and coastal embayment is of great concern. Commercial ships’ ballast water discharge and the northwards progression of species due to the ongoing climate change arise as the main factors explaining the rising occurrence of NIS species in Northern Atlantic waters. In this regard, regular monitoring of the plankton communities is paramount as to be able to respond properly to this potential issue.ResultsWhile monitoring the invasive copepod Acartia tonsa populations in the estuaries of Bilbao and Urdaibai (Basque country, Spain), we report here the Asian copepod Pseudodiaptomus marinus for the first time in the Iberian Peninsula waters. Individuals from both species were collected from July to October, 2013 for DNA sequencing of mitochondrial cytochrome c oxidase subunit I gene (MT-CO1). Phylogenetic analysis of MT-CO1 confirmed P. marinus identity.ConclusionsPhylogeographic distribution of A. tonsa haplotypes in Europe along with the Bilbao port traffic patterns suggested a secondary invasion from an European source to Basque estuaries. The successful establishment of the A. tonsa population and the appearance of Pseudodiaptomus marinus confirm the need for regular plankton monitoring of estuarine and port waters. This applies also to nearby systems as these populations could represent a source of future dispersal.

Dissolved Oxygen in a Temperate Estuary: the Influence of Hydro-climatic Factors and Eutrophication at Seasonal and Inter-annual Time Scales

Dissolved oxygen dynamics in estuarine and coastal environments are complex and highly variable, which highlight the need to compile information from many different types of estuaries. Small estuaries where euhaline habitats dominate are particularly ill represented in the literature. As a contribution to fill this gap, a study on dissolved oxygen dynamics was conducted in the small estuary of Urdaibai (inner Bay of Biscay). Spatial and temporal variations in the percentage saturation of dissolved oxygen (DO-saturation) along the salinity gradient of the estuary and the role of hydro-climatic factors and eutrophication as drivers of those variations at seasonal and inter-annual time scales were analyzed (period 1998–2008). DO-saturation showed an inner to outer estuary increasing gradient. DO-saturation below the salinity gradient layer was either significantly higher than or not significantly different from that in the salinity gradient layer. DO-saturation showed summer minima, but hypoxia was rarely observed. At the outermost estuary, seasonal variations of DO were small and it is hypothesized that DO dynamics were governed mainly by tidal exchange and turbulence. In the intermediate and inner estuary, seasonal variations of DO-saturation were best explained by river discharge, and to a lesser extent by chlorophyll a and temperature, each factor gaining relevance in different periods of the year. In intermediate and inner zones, river discharge exerted a positive effect on DO-saturation, likely via an increase in the renewal rate of DO. At the inter-annual time scale, unlike at the seasonal scale, temperature did not show a significant negative relationship with DO-saturation.

Zooplankton variability at four monitoring sites of the Northeast Atlantic shelves differing in latitude and trophic status

Zooplankton abundance series (1999–2013) from the coastal sites of Bilbao 35 (B35), Urdaibai 35 (U35), Plymouth L4 (L4) and Stonehaven (SH), in the Northeast Atlantic were compared to assess differences in the magnitude of seasonal, interannual and residual scales of variability, and in patterns of seasonal and interannual variation in relation to latitudinal location and trophic status. Results showed highest seasonal variability at SH consistent with its northernmost location, highest interannual variability at U35 associated to an atypical event identified in 2012 in the Bay of Biscay, and highest residual variability at U35 and B35 likely related to lower sampling frequency and higher natural and anthropogenic stress. Interannual zooplankton variations were not coherent across sites, suggesting the dominance of local influences over large scale environmental drivers. For most taxa the seasonal pattern showed coherent differences across sites, the northward delay of the annual peak being the most common feature. The between-site seasonal differences in spring–summer zooplankton taxa were related mainly to phytoplankton biomass, in turn, related to differences in latitude or anthropogenic nutrient enrichment. The northward delay in water cooling likely accounted for between-site seasonal differences in taxa that increase in the second half of the year.

Assessment of the climate and human impact on estuarine water environments in two estuaries of the Bay of Biscay

Abstract The effect of climate variability on estuarine water environments was assessed in two systems of the Bay of Biscay, the estuaries of Bilbao and Urdaibai, with contrasting morphology, hydrodynamic features and anthropogenic influence. To that purpose, the main time scales of variability in relevant environmental factors were established along spatial salinity gradients and, using a combination of multivariate and regression analyses, the contribution of each factor to the total variability, as well as the influence of climate factors in the seasonal and inter-annual estuarine environment variations were assessed. The major seasonal modes of variability in the water environments of both estuaries were accounted for by water temperature together with salinity stratification and/or chlorophyll a. This seasonal variability was associated with climate variability, as shown by the relationship with air temperature and river flow. The major inter-annual modes of variability were also accounted for by water temperature, along with dissolved oxygen and/or chlorophyll a in Bilbao, and chlorophyll a and/or transparency in Urdaibai. These were also associated with climate variability, in this case summer air temperatures. Water quality variables, such as dissolved oxygen and transparency, were found to be sensitive to reveal the effect of long term anthropogenic activities.