a multimetric diatom index to assess the ecological status of coastal galician rivers (nw spain)
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PRIMARY RESEARCH PAPER
A multimetric diatom index to assess the ecological statusof coastal Galician rivers (NW Spain)
Cristina Delgado • Isabel Pardo • Liliana Garcıa
Received: 3 September 2009 / Revised: 24 February 2010 / Accepted: 1 March 2010 / Published online: 17 March 2010
� Springer Science+Business Media B.V. 2010
Abstract There are many rivers in northwest Spain
as a consequence of the mountainous landscape and
the granitic geology subjected to Atlantic influences.
Water and epilithic diatoms samples were collected
at 72 sites in Galicia flowing into the Atlantic Ocean
and Cantabrian Sea in summer 2002–2003 and
spring 2004. These sites included minimally dis-
turbed sites, defined as reference sites, and impacted
sites which were influenced by different human
pressures. We used the diatom assemblages to
calculate diatom indices using the Omnidia software,
but we also developed new metrics based on the
similarity of species composition in reference sites.
The response of the metrics was tested in relation to
physicochemical variables. We developed a diatom
multimetric index (MDIAT) as a combination of
metric values. The sensitivity of the MDIAT to
organic and nutrient stressors supports the use of this
index to classify the ecological status of Galician
rivers. The MDIAT showed higher correlations with
some variables and nutrients than the individual
metrics. According to the MDIAT, 69% of the sites
sampled in Galician coastal rivers achieve good
ecological status. The MDIAT has been developed
specifically for Galician granitic rivers (NW Spain),
and has been intercalibrated at the European level in
the Central Baltic Rivers GIG. Our study validates
the application of this multimetric index to evaluate
the water quality in coastal Galician rivers.
Keywords Coastal Galician rivers � Ecological
status � Diatoms � Multimetric index � Water
Framework Directive
Introduction
The degradation of freshwater ecosystems has been a
cause of concern for several decades. Since the
implementation of the European Water Framework
Directive (WFD; European Union, 2000) has encour-
aged different applied ecological studies for under-
standing the impact caused to freshwater ecosystems
by anthropogenic pressures (Hering et al., 2006a;
Muxika et al., 2007). The WFD requires that
ecological status assessments of rivers and lakes are
based on evaluations of phytoplankton, macrophytes
and phytobenthos, benthic invertebrates and fish.
Methods to assess the phytobenthos have tended to
focus on diatoms which often form a large part of the
algal diversity in freshwaters (King et al., 2000).
Although, macroinvertebrates and fishes have been
frequently used in the evaluation of the ecological
status in rivers (Oberdorff & Hughes, 1992; Morais
et al., 2004; Hering et al., 2006a), the diatoms are
Handling editor: P. Noges
C. Delgado (&) � I. Pardo � L. Garcıa
Department of Ecology and Animal Biology,
University of Vigo, 36330 Vigo, Spain
e-mail: [email protected]
123
Hydrobiologia (2010) 644:371–384
DOI 10.1007/s10750-010-0206-y
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very sensitive organisms to sudden and minor
changes occurring in water chemistry (Leira &
Sabater, 2005). Benthic diatoms are traditionally
considered to be regulated mainly by local rather than
large scale factors (Pan et al., 1999) although large-
scale spatial factors, such as climate, geology and
vegetation also influence the structure of the diatom
community (Leland, 1995). Benthic diatoms seem not
only to respond to hydromorphological modification
(Hering et al., 2006a) but also have been used
extensively in rivers for assessing nutrient enrichment
(e.g. Coring et al., 1999; Rott et al., 1999). In Latvia,
the relationship between diversity indices and envi-
ronmental variables is stronger in the case of
small*bodied organisms, such as diatoms and macr-
oinvertebrates, compared to macrophytes and fishes
(Springe et al., 2006).
The response of the community to a pressure
gradient can be converted into a continuous variable
using diatom metrics (Kelly et al., 2008). This
simplifies the complicated ecology of rivers in a way
that permits the rapid assessment of the overall
condition in a manner that is easily understood
(Atazadeh et al., 2007). Some studies show that diatom
metrics detect eutrophication effects better than met-
rics calculated using fishes, macroinvertebrates and
macrophytes, and they respond most strongly to land-
use gradients (Hering et al., 2006a; Johnson et al.,
2006). For all these reasons, the use of diatom indices
has undergone an increase in recent years as a tool to
provide a reflection of water quality (Prygiel & Coste,
1993; Kelly, 1998, 2002; Wu, 1999; Gomez & Licursi,
2001; Wu & Kow, 2002). Moreover, the appearance of
software packages, such as Omnidia, which facilitates
the calculation of indices, has intensified its use in
Europe (Kwandrans et al., 1998; Eloranta & Soininen,
2002; Pardo et al., 2005; Garcıa et al., 2008). Mean-
while, in North America, the use of metrics based on
sensitive and tolerant species is more developed (Fore
& Grafe, 2002; Passy & Bode, 2004).
The objectives of this study are (i) to test the
response, in Galician rivers, of different diatom
indices and metrics (some newly developed for the
area) that taken into account the composition and
abundance of reference species assemblages, (ii) to
build a multimetric diatom index by a combination of
different types of response metrics (taxonomic,
organic, trophic, and sensitivity of taxa) to fulfil the
normative definitions of the WFD, and finally (iii) to
assess, using this multimetric, the ecological status of
Galician rivers.
Materials and methods
Study area
The Northwest of the Iberian Peninsula is influenced by
the Atlantic climate, and it is characterized by rainy
weather with mild temperatures throughout the year,
similar to the rest of Western Europe. The region of
Galicia lies in this area of Spain with the Cantabrian
Sea to the north and the Atlantic Ocean to the west
(Fig. 1). The geology is dominated by siliceous rocks:
granite in the west and metamorphic rocks in the east.
The region can be divided into two areas: Inland
Galicia and Coastal Galicia which are separated by a
mountain range known colloquially as ‘Galicia0sbackbone’. Coastal Galicia has mild winters and cool
summers with precipitation exceeding 1,500 mm per
year. The mountainous geomorphology and regular
precipitation influences the occurrence and perma-
nence of many small- and medium-sized rivers with
regular discharge throughout the year. This study
focuses on these systems within the area of Coastal
Galicia that includes all Galician river basins that flow
into the Cantabrian Sea and to the Atlantic Ocean
(Fig. 1).
Sampling design
Initially, we differentiated river types using ‘system A’
of the WFD, which uses geology, altitude and catch-
ment area as descriptors (WFD, Annex II). Galician
coastal rivers have granitic geology and they were thus
divided into three categories according to the catchment
area: small, medium and large at different altitudes
(Table 1). Most of the rivers were small to medium
sized and only the downstream parts of the rivers Ulla,
Umia and Tambre were considered to be large rivers.
These, however, were not included in this study.
Selecting reference and non-reference sites
Candidate reference sites had to satisfy a series of
a priori selection criteria based on the absence of
significant pressures (dams, water treatment plants, fish
farms and percentage of agricultural land\30%). We
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used local information on pressures in the Galician
coastal area and data from CoORdination of INforma-
tion of the Environment (CORINE) Land Cover 1990
(Bossard et al., 2000) to calculate the percentage of land
used for different purposes. The reference condition
criteria used to select the reference sites were those of
the Central/Baltic Geographical Intercalibration Group
(C/B GIG; van de Bund, 2009; Kelly et al., 2009).
Field sampling and laboratory processing
During this study, we sampled a total of 72 small and
medium rivers from 27 river basins in Coastal Galicia.
Sampling was conducted in two seasons: summer
2002–2003 and spring 2004, giving a total of 144
samples. Environmental factors, such as water temper-
ature (�C), pH, dissolved oxygen (mg l-1) and electri-
cal conductivity (lS cm-1) were measured in situ using
portable meters. Temperature and oxygen were
measured with a WTW Oxi 197 oxymeter, conductiv-
ity with an Orion Model 115 corrected for 25�C, and
pH with a Thermo Orion 290?. Water samples for
chemical analyses were collected into polypropylene
bottles and transported chilled to the laboratory.
Standard methods for chemical water analysis were
carried out following American Public Health Asso-
ciation (APHA) (1989): BOD5 with oxitop WTW
after incubation for 5 days at 20�C; alkalinity by the
potentiometric method, nitrates (NO3-), silica (SiO2),
phosphates (PO43-) using an auto-analyzer for nutri-
ents (Auto-Analyzer 3, Bran ? Luebbe, Germany),
ions, such as calcium (Ca2?), iron (Fe2?), magnesium
(Mg2?), potassium (K?), sodium (Na?) with a
spectrophotometer of masses, and chlorides (Cl-)
and sulphates (SO42-) with Inductively Coupled
Plasma-Mass Spectrophotometry (ICP-MS).
Three rocks were selected at random from each site
and their upper surface divided into two halves,
Fig. 1 Localization and
distribution of the 72 sites
sampled in this study
Table 1 Types of rivers found in Galicia coastal area in the system A and B classification and the number of reference sites and total
sites
System A Number of sites System B
Size catchment area Altitude (m) Total References Size catchment area Altitude (m)
Small \200 16 0 Small and Medium (10–1000 km2) \200; 200–800; [800
Small 200–800 31 5
Small [800 4 4
Medium 200–800 11 0
Medium \200 10 0
Large \200 0 0 Large (1000–10000 km2) \200
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providing a total of six replicate samples of approx-
imately 20–60 cm2 each. Samples of periphyton were
taken from the upper surfaces of each rock removed
by brushing with a toothbrush and rinsing with
distilled water. They were stored in ice, kept in
darkness and transported to the laboratory. Three
samples were used for analysis of chlorophyll a (chl a)
and the other three were used to estimate periphyton
biomass as ash-free dry mass (AFDM). The periph-
yton samples were filtered through Watman GF/C
glass fibber-filters, and the chl a concentration was
extracted with acetone (90%) for 48 h at 4�C, kept in
the dark and measured using a Hitachi Model U-2001
UV/Visible Spectrophotometer. Values were cor-
rected for degradation products using the equations
given by Lorenzen (1967). Samples for AFDM were
filtered through pre-ashed and weighed glass-fiber
filters, dried to constant mass at 105�C for 24 h, and
reweighed. Filters were then placed in a muffle
furnace at 505�C for 1.5 h to estimate the AFDM.
Organic mass lost during combustion was determined
as the difference between initial and ash masses
(American Public Health Association (APHA) 1989).
Epilithic diatoms were collected from stones
following the European standard (CEN, 2003) with
a small toothbrush. Immediately after collection,
the diatom samples were fixed with formaldehyde
(4% v). Diatom samples were digested by following
the procedure of Renberg (1990), and permanent
slide mounts were prepared for each sample using the
high-resolution mountant Naphrax�. Diatoms were
observed and identified at the lowest taxonomic level
possible using a light microscope (Olympus BX40);
and a minimum of 400 diatom valves were counted
on each slide. The identification and the nomencla-
ture were based on Krammer & Lange-Bertalot
(1986–1991).
Analysis of the diatom communities
Diatom abundance data in this study was log-
transformed (x ? 1), to give more weight to large
species that are often found at low relative abundance
in benthic diatom communities and which can be
important for defining assemblages (ter Braak &
Verdonschot, 1995; Snoeijs et al., 2002; Tison et al.,
2005). The data were analyzed using the program
Primer 6 (Plymouth Marine Laboratory, UK, 2001).
Two analyses were performed: (i) a SIMPER analysis
(SIMilarity PERcentage) to estimate the degree of
similarity between the reference and non-reference
samples, and (ii) a Non-metric MultiDimensional
Scaling (NMDS), based in the Bray–Curtis similarity
index to examine patterns of community composi-
tion. The SIMPER indicated the individual contribu-
tion and the importance of each taxon to the global
similarity between sites by considering the frequency
and the abundance of each taxon. This analysis
allowed us to identify the reference taxa that char-
acterized the community of reference sites.
Candidate indices and metrics
Calculation
The diatom abundance data was used to calculate 17
biological indices and metrics (Table 2). The soft-
ware OMNIDIA v.3.6 (Lecointe et al., 1993) was
used to calculate the first 13 diatom indices listed in
Table 2. Each index differed in the number of species
that were used and in the constant values (tolerance
values) that have been evaluated for ecological
relevance from the compiled literature information
(Prygiel & Coste, 1993, van Dam et al., 1994).
The other four metrics were calculated for each
sample in an excel spreadsheet: (a) relative abun-
dance (ABSS) and richness (FSS) of reference taxa
and (b) the ratio of reference taxa to the total taxa
expressed as percentages of abundance (PABSS) and
richness (PFSS).
Selection
Diatom indices and metrics representing ecologically
relevant aspects of the assemblage, and responding to
the targeted stressors tested were considered as
potential metrics to combine in a multimetric index.
The selection of indices and metrics followed the
procedure described by Barbour et al. (1999) with
some modifications as follows:
(i) Assessing redundancy: this method identifies
pairs of metrics with significant Spearman rank
correlations. If a pair had a correlation coeffi-
cient greater than [0.7, one of the two metrics
was excluded from further analyses. We used
r = 0.77 as a limit following Ofenbock et al.
(2004).
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(ii) Relation with the physicochemical variables:
correlations were used to establish the relation-
ship of the different indices and metrics with the
physicochemical variables. Those that did not
correlate with the physicochemical variables,
and did not sufficiently discriminate among
sites of different condition were eliminated. The
remaining metrics, which were used in further
analysis, were termed ‘candidate metrics’.
(iii) Estimating discrimination efficiency: as the
percentage of samples with metric values lower
than the P25 of reference values for decreasing
metrics, and higher than the P75 for increasing
metrics, respectively (Ofenbock et al., 2004).
Discriminatory efficiencies were calculated to
evaluate the most suitable indices by visualis-
ing each metric’s distribution between the
reference and the non-reference group.
Results
Typology and reference community
The geology in the Galician coastal area is homoge-
neously siliceous, thus, the a priori ‘system A’
provided six types of rivers based on catchment area
and altitude (Table 1). A total of 51 small rivers and
21 medium rivers were sampled in this study. The
most abundant were the small rivers at mid-altitudes
(Table 1), but only nine sites were designated as
‘reference sites’ according to the criteria established
by CB-GIG. These reference sites were located in
mountainous areas of coastal Galicia area, and
corresponded to small rivers: four of these were
located at an altitude greater than 800 m, and five at
mid-altitudes from 200 to 800 m (Table 1). We could
not find sites that achieved these criteria in medium
rivers and in small rivers at low altitudes.
Diatom samples from these reference sites, along
with sites not influenced by pressures (having less
than 50% of agriculture in their basin), a total of 56
samples, were analyzed for two purposes:
(i) The SIMPER routine compared both groups
‘reference’ and ‘non-reference’ groups. The
within-group percentage of similarity in the
references was 50.14, and in the non-references,
was 35.57%. Indeed, the reference group was
characterized by nine species that contributed
[90% to characterize the diatom reference
assemblage (Tables 3 and 4). This group was
dominated by the genus Eunotia with five taxa:
Eunotia exigua, E. minor, E. subarcuatoides,
E. intermedia and E. paludosa Grunow var.
Table 2 Diatom indices
and metrics tested in this
study
Metrics
CEE Commission for Economical Community metric (Descy & Coste, 1991)
DESCY Descy’s pollution metric (1979)
EPID Pollution metric based on diatoms (Dell’Uomo, 1996)
IBD Biological Diatom Index (Prygiel & Coste, 1999)
IDG Generic Diatom Index (Coste & Ayphassorho, 1991)
IDAP Indice Diatomique Artois Pircardie (Prygiel et al., 1996; Lecointe et al., 2003)
IPS Specific pollution sensitivity index (Cemagref, 1982)
L&M Leclercq & Maquet‘s pollution index (1987)
ROOT Trophic metric (Rott et al., 1999)
SHE Steinber & Schiefele trophic metric (1988)
SLAD Sladecek’s pollution index (Sladecek, 1986)
TDI Trophic Diatom Index (Kelly & Whitton, 1995)
WAT Watanabe et al. pollution metric (Watanabe et al., 1986; Lecointe et al., 2003)
ABSS Abundance of reference taxa (Present study)
PSS Richness of reference taxa (Present study)
PABSS Percentage abundance of reference taxa (Present study)
PFSS Percentage of richness of reference taxa (Present study)
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paludosa, together with Achnanthidium minu-
tissimum, Navicula angusta, Peronia fibula and
Surirella roba. These nine species plus other
nine taxa, more abundant in reference sites than
in non-reference sites (Table 4), were considered
to be the core of the reference assemblage and
their presence and abundance (Table 2) were
used to build the new metrics based on the
reference community. Although, the dissimilar-
ity of two groups had a value of 60.62%, the
nine taxa of the reference community appeared
as well in the non-reference group, but at lower
percentages (Table 3).
(ii) Non-metric MultiDimensional Scaling (NMDS)
ordination plot (stress 0.17), based on the
samples of diatom communities, revealed spa-
tially the similarity between reference samples
in relation with some of the non-reference
samples (Fig. 2).
Metric selection
We compared indices/metrics based on their correla-
tions, discriminatory efficiency and response to the
physicochemical variables: (1) The indices EPID and
CEE were excluded due to their high correlation
coefficient with other indices, such as IPS and SLAD;
(2) IDAP and WAT were excluded because they
were not significantly correlated with the physical–
chemical variables (Table 5); (3) For the rest of indices,
we selected those with discrimination efficiencies higher
than 50%: IDG, IPS, L&M, SHE, SLAD and TDI
(Table 5); (4) From the four metrics based on
reference taxa, PFSS and PABSS were selected due
to their higher discriminatory efficiency, 77.78 and
84.13%, respectively (Table 5).
We mainly considered indices and metrics for the
multimetric construction, but values of Chl a were
also analyzed and related to indices/metrics
(Table 5). The Chl a was inversely related to diatom
multimetric index (MDIAT) indicating a significant
increase in biomass with lower values of MDIAT and
consequently higher in nutrients.
Generating a multimetric index
Finally, these six indices and two metrics were
combined in a multimetric, the MDIAT. All selected
indices, calculated with the Omnidia software, had
values from 0 to 20, while the metrics PFSS and
PABSS ranged from 0 to more than 1 with values
decreasing with increased degradation (Table 5). The
TDI index is an exception, with values 0–100 and
positive correlations in pressure variables, for this
reason, this index had to be inverted. We rescaled each
of the eight metrics, transforming them by dividing
each individual value by the median value of the
reference population, so that each index ranged from
0 to [1. The eight rescaled values were summed to
the MDIAT. Subsequently, the Ecological ratio
(EQR_MDIAT) was calculated by dividing each value
of the multimetric by the MDIAT median value of the
reference data, the expected value without significant
human influence. The ranges of values obtained for the
selected indices/metrics, MDIAT and EQR_MDIAT
in reference sites and the rest of samples from Galician
coastal area are summarized in Table 6. The values of
the MDIAT ranged from 2.804 to 8.819 and EQRs
from 0.349 to 1.096 (Table 6).
Classification system of the ecological status
Diatom multimetric index (MDIAT) had the highest
discriminatory efficiency and highest correlations
with the physical–chemical variables of all indices
and metrics tested (Table 5). Initially, the EQR values
were subdivided into five classifications according to
its status: High, Good, Moderate, Poor and Bad, using
the P25 of the reference values as the limit between
High and Good. The remaining EQR values from the
Fig. 2 Ordination (MDS) of the diatom community of
reference (ref) and some of no reference sites (no ref), all of
them with percentages of agriculture \50%
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P25 EQR to 0 were divided into four equal intervals
corresponding to the remaining classifications
(Table 7). Minor adjustments to these boundary
values were made during the European Intercalibra-
tion Exercise, and the final values were 0.93, 0.70,
0.50 and 0.25, respectively (Table 7). Figure 3 shows
the ranges of the measured physicochemical variables,
percentage of agriculture, MDIAT and EQR_MDIAT
for each of the status classifications (High, Good,
Moderate and Poor) defined by MDIAT.
The relationship between the EQR_MDIAT and
some of its component metrics is shown in Fig. 4.
The other component metrics have similar curves in
relation to the EQR_MDIAT, but the IDG had the
highest correlation with the MDIAT (R2 [ 0.7).
Figure 4 represents the metrics tendency within the
EQR_MDIAT. All metrics tend to decrease with
increasing degradation, except for the TDI that
diminishes with higher values. According to the
shape of the curves, the two metrics built from the
reference community are more sensitive to low levels
of pressures than the other indices with a more
conservative tendency, such as the NIDG. NPFSS
had the same tendency as NPABSS, but only the
Table 3 Percentage of
contribution and
accumulative percentage of
the diatom species that
characterized reference and
no reference groups
(resulted by SIMPER)
Species Reference group No Reference group
% Contribution %A Contribution % Contribution %A Contribution
ADMI 34.38 34.38 25.55 25.55
ESUB 21.24 55.61 14.6 40.14
SRBA 14.71 70.32 9.79 49.93
EUIN 8.87 79.19 6.58 56.51
EEXI 3.28 82.46 2.07
PFIB 2.95 85.41 1.99
NAAN 2.36 87.77 2.44
EPAL 2.09 89.86 1.52
EMIN 1.95 91.81 3.13
Table 4 Codes and names
of the 18 reference taxa for
coastal Galician rivers
* Taxa that characterized
the reference community
until 90%
Code Reference taxa
ADMI *Achnanthidium minutissimum (Kutzing) Czarnecki
BBRE Brachysira brebissonii Ross spp. brebissonii
DLAE Diadesmis laevissima (Cleve) Mann
EAQL Encyonopsis aequalis (W.Smith) Krammer
EBIL Eunotia bilunaris (Ehrenberg) Mills var. bilunaris
EEXI *Eunotia exigua (Brebisson ex Kutzing) Rabenhorst
EINC Eunotia incisa Gregory var. incisa
EMIN *Eunotia minor (Kutzing) Grunow
EPUN Eunotia pectinalis (Kutzing) Rabenhorst var. undulata (Ralfs) Rabenhorst
ESUB *Eunotia subarcuatoides Alles, Norpell & Lange-Bertalot
EUIN *Eunotia intermedia (Krasske ex Hustedt) Norpel & Lange-Bertalot
EUPA *Eunotia paludosa Grunow var. paludosa
GGRA Gomphonema gracile Ehrenberg
NAAN *Navicula angusta Grunow
PFIB *Peronia fibula (Brebisson ex Kutzing) Ross
PCHL Psammothidium chlidanos (Hohn & Hellerman) Lange-Bertalot
SLIN Surirella linearis W. M. Smith
SRBA *Surirella roba Leclercq
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former was represented in the figure. We defined the
centre of good status as the point at which the NPFSS
and TDI crossed, whilst the TDI and NIDG crossed
on the moderate class. The NIDG and NPFSS
crossing near the value of one represent the centre
of the high classification (Fig. 4).
The ecological improvement of the MDIAT
Having established the MDIAT using existing con-
cepts for classification systems, we aimed subse-
quently to develop and simplify this. In particular, an
important variable that we had estimated, Chl a, was
Table 5 Significative Spearman correlations among indices/
metrics and physico-chemical variables and percentage of
discriminatory efficiency and the Spearman correlation
coefficients (n = 144) with some of physicochemical variables
(** significative correlation at the level 0.01; * significative
correlation at the level 0.05)
NO3- SiO2 SO4
2- PO43- BDO5 Chl a AFDM PH Alkalinity % Discriminatory
efficiency
IDAP -0.073 -0.098 -0.153 -0.102 -0.006 -0.173 -0.169 0.095 -0.103 15.38
EPID -0.172* -0.494** -0.203* -0.134 -0.380** -0.235** -0.183* -0.252** -0.103 59.52
ROTT -0.237** -0.469** 0.018 -0.351** -0.148 0.099 -0.014 -0.537 -0.231** 33.33
IBD -0.210* -0.569** -0.326** -0.261** -0.380** -0.207* -0.338** -0.338** -0.190* 47.62
WAT -0.099 0.173* -0.081 -0.023 -0.122 0.013 -0.106 0.293** 0.058 42.86
DES -0.199* -0.516** -0.154 -0.290** -0.353** -0.179* -0.164* -0.472** -0.192* 44.44
CEE -0.265** -0.607** -0.364** -0.365** -0.425** -0.337** -0.380** -0.256** -0.226* 72.73
IDG -0.323** -0.530** -0.170* -0.319** -0.360** -0.362** -0.321** -0.412** -0.252** 78.57
IPS -0.242** -0.515** -0.239** -0.232** -0.461** -0.285** -0.349** -0.237** -0.101 57.94
L&M -0.335** -0.594** -0.263** -0.364** -0.393** -0.195* -0.286** -0.474** -0.281** 59.52
SHE -0.372** -0.551** -0.265** -0.483** -0.288** -0.267** -0.288** -0.288** -0.274** 77.78
SLAD -0.233** -0.684** -0.260** -0.265** -0.466** -0.341** -0.378** -0.459** -0.195* 65.87
TDI 0.381** 0.741** 0.201* 0.440** 0.440** 0.384** 0.413** 0.560** 0.336** 90.48
PABSS -0.388** -0.673** -0.297** -0.447** -0.386** -0.316** -0.390** -0.511** -0.287** 84.13
PFSS -0.413** -0.734** -0.279** -0.481** -0.419** -0.194* -0.373** -0.595** 0.322** 77.78
MDIAT -0.411** -0.722** -0.292** -0.478** -0.474** -0.302** -0.411** -0.527** -0.315** 93.65
Nitrates (NO3-), silicon dioxide (SiO2), sulphates (SO4
2-), phosphates (PO43-), biological demand of oxygen (BDO5), chlorophyll a
(chl a), biomass as ash-free dry mass (AFDM), pH and alkalinity
Table 6 Minimum, maximum, mean and standard error (SE) of the selected metrics, MDIAT and EQR_MDIAT of reference sites
and the rest of samples
Reference sites All sites
Minimum Maximum Mean SE Minimum Maximum Mean SE
MDIAT 7.250 8.600 7.920 0.091 2.804 8.819 5.811 0.110
EQR_MDIAT 0.900 1.070 0.980 0.011 0.349 1.096 0.722 0.010
SHE 16.50 17.20 16.85 0.03 4.20 17.80 11.00 0.22
SLAD 14.90 16.90 15.90 0.14 11.20 18.50 14.85 0.14
IDG 16.10 18.10 17.10 0.12 9.60 19.00 14.30 1.15
TDI 1.90 30.40 16.15 2.29 0.10 96.90 48.50 2.21
IPS 17.70 20.00 18.85 0.15 7.30 20.00 13.65 0.21
L&M 15.10 16.50 15.80 0.10 1.50 17.60 9.55 1.16
PABSS 0.57 1.00 0.78 0.02 0.00 1.00 0.50 0.03
PFSS 0.36 1.00 0.68 0.05 0.00 1.00 0.50 0.02
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missing from the classification. For this reason, we
decided to build a new, simpler multimetric, MDIATa
that included Chl a along with a trophic index (TDI),
and PABSS, one of the new metrics calculated with
the reference community. We then compared the
results from the MDIAT and the MDIATa. The Chl a
had to be inverted due to its increase with stream
nutrients/organic degradation. The three metrics were
averaged to produce the MDIATa. The interpretation
of the change of the metrics along a degradation
gradient evaluated by the MDIATa can be seen in
Fig. 5. The crossing between metrics is an indicator of
the consistency with the limits already established, 0.7
for the High/Good, and 0.5 for the Good/Moderate. It
is interesting to note that Chl a only increases below
the moderate class boundary. The lineal regression
between the MDIAT_EQR and the MDIATa_EQR
was significant (P \ 0.01) with R2 = 0.90.
Discussion
The main objective of this study was to analyze
different diatom metrics, to check their response to
organic/nutrient pressures, and to develop a classifi-
cation system for the evaluation of ecological status,
based on diatoms, for small and medium rivers. For
these rivers, we identified a spatial network of
reference sites [minimally disturbed according to
Stoddard et al. (2006)], that fulfilled the reference
criteria that has been widely applied across Europe in
the intercalibration exercise (Wallin et al., 2005; van
de Bund, 2009). Defining reference sites is a very
important step in this study (WFD, Annex V). The
reference criteria applied in Galicia has been agreed
to and intercalibrated (Central/Baltic Rivers GIG),
and it has been included in the first phase of
intercalibration (van de Bund, 2009).
The diatom reference assemblages found in small
and medium Galician rivers showed that a high
degree of similarity independent of altitude. The
reference group showed more than 50% similarity,
whilst the non-reference group was more diverse. The
nine taxa that characterized the reference assemblage
also appeared in sites with low levels of disturbance,
but at lower relative abundances. This assemblage
characterizes sites under minimally disturbed condi-
tions, but some species can appear in disturbed sites
in this area. We considered this assemblage to be very
sensitive because they tend to disappear with increas-
ing levels of human disturbance. The reference
community was dominated by five species of the
genus Eunotia: E. exigua, E. minor, E. subarcuato-
ides, E. intermedia and E. paludosa var. paludosa, a
genus that is usually well-represented and character-
istic of acidic waters (van Dam et al., 1994; De
Nicola, 2000; Sala et al., 2002), such as the waters of
Galician rivers.
The existing differences in the water quality of the
studied Galician rivers corresponded to changes in the
diatom assemblages and consequently to the values of
diatom indices and metrics. Diatom indices have been
shown to be one of the most effective tools for
evaluating ecological status in European rivers
(Eloranta & Soininen, 2002; Kelly et al., 2008). The
response to pressures that the diatom indices provided
when applied to small and medium Galician rivers was
very weak and not able to discriminate low enrichment
levels, and for this reason, it was necessary to develop
new metrics, using the conceptual framework pro-
posed by the WFD of characterizing the reference
community. The new metrics based on the diatom
reference community for Galician rivers were more
sensitive indicators than the diatom indices used and
developed for other geographical areas of Europe
(Kelly, 1998; Kelly & Whitton, 1998; Prygiel et al.,
2002). Even though diatoms species are widely
distributed across regions, there is a regional constraint
as local test datasets may not include the whole
spectrum of the taxa’s autoecology that exist across
regions. Our observations are consistent with findings
from studies that show that some diatom indices
developed in certain parts of Europe are not effective
when they are used in other areas of the same continent
(Pipp, 2002; Rott et al., 2003); for this reason, we also
used the new metrics based in the reference commu-
nity. Galician coastal rivers are, in general, systems
Table 7 Boundaries between the different status classes in the
EQR_MDIAT sensu P25 of our values and sensu the Intercal-
ibration European Exercise
Boundaries P25 EQR_MDIAT Intercalibration
European Exercise
High/Good 0.960 0.930
Good/Moderate 0.720 0.700
Moderate/Poor 0.480 0.500
Poor/Bad 0.240 0.250
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characterized by low levels of nutrients and low
conductivity. This oligotrophic character may be the
reason for the absence of significant responses from
indices derived in other, more nutrient-rich regions.
Multimetric Indices can be easily interpreted, a
fact which is regarded as a main advantage of this
type of classification systems, but European countries
have little experiences with these multimetrics
(Hering et al., 2006b). We demonstrated that the
metrics selected for the multimetric satisfied three
important requirements: (i) They were not strongly
correlated with other metrics (Fore & Grafe, 2002);
(ii) They responded to disturbance in the predicted
ecological direction and magnitude; and (iii) They
Fig. 3 Box and whisker
plots of different
physicochemical variables
and percentages of
agriculture, for the different
class that we found in
Coastal Galician Rivers
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were significantly associated with water physico-
chemical variables. Therefore, the MDIAT consti-
tutes a good tool to evaluate the ecological status of
Galician coastal rivers. The multimetric values were
better correlated with the physicochemical variables
than with the individual indices, integrating the
effects of the pressures studied (organic pollution
enrichment and eutrophication). The values of MDI-
AT have been converted into EQR values, computed
from the observed and the expected status value
(Kelly et al., 2008) giving a value for each river in
terms of their deviation from the biota expected at
the reference state. We used the limits of the last
intercalibration exercise, and checked that the limits
between the different status classifications that arose
in this exercise corresponded with significant rele-
vant metric crossing and ecological interpretation.
The crossing between the trophic index (TDI) and
the normalized metric that represented the reference
community (NPFSS) indicates that community
changes due to nutrient enrichment decreased the
abundance and richness of sensitive species, the
crossing of their curves representing the middle of
the Good classification. We confirmed that the
crossing between NIDG and TDI was on the
Moderate classification. The evaluation resulting
from our multimetric indicates that none of the study
sites were under the Bad classification, and that 69%
of the studied sites achieved the Good ecological
status according to the diatoms in this area.
The classification provided by the MDIAT in
Galician rivers has been intercalibrated at the Euro-
pean level under the first phase of the exercise of
intercalibration with other countries (Kelly et al.,
2009), showing a good correlation with the intercal-
ibration common metric (composed of IPS and Rott’s
TI). However, the MDIAT has a complex composi-
tion that includes newly developed metrics which are
more sensitive and specific for Galician oligotrophic
waters than the intercalibration indices. The EQR
provided by the MDIATa is highly related to the
MDIAT, indicating a high agreement of classification
results between both multimetrics.
The new MDIATa also includes Chl a, a good
indicator of the trophic status of streams (Dodds,
2006). Granitic rivers are known to be poor in
nutrients, and they usually have developed riparian
areas that shade the channel, conditions that increase
the probability for nutrient and light limitation of
diatom communities (Pardo & Alvarez, 2006). The
fact that we only perceive an increase in Chl a from
values prevailing under reference sites after the
moderate classification seems indicative of a diffi-
culty to build biomass even though nutrient levels
increase.
Previous studies have applied diatom indices to
Galician rivers (Ector, 1992; Penalta & Lopez, 2007)
without an analysis of pressures or suitability to
Galician waters. This study represents the first
extensive research on the application of diatom
indices and composition metrics to Galician rivers.
Fig. 4 Bivariate graphic between normalized IDG (NIDG),
normalized PFSS (NPFSS), inverted TDI (TDI/100) and the
EQR_MDIAT
Fig. 5 Bivariate graphic between standardized Chl a (SChl a),
normalized PABSS (NPABSS), inverted TDI (TDI/100) and
the EQR_MDIATa
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However, further studies should be done when more
data are available to ascertain whether MDIAT may
be improved and, ideally, further simplified. Our
research has confirmed that the application of the
multimetric diatom indicator system is a valuable tool
to classify the ecological status in Galician rivers
because it integrates the effects of stressors on
different indicators and components of the diatom
community.
Acknowledgements This article complemented some of the
results obtained by a project dealing with the application of
the Water Framework Directive in Galician coastal area. The
financial support for this study has been provided by Augas de
Galicia (Xunta de Galicia, Spain), and this also included the
support of the University of Vigo (Spain). We are grateful to
the editor and the reviewers for their criticism and comments
that improved the final manuscript. We thank M. Kelly for
improving the language and content of the article, M.H. Novais
for their commentaries, M. Dominguez for the help with the
chemical analysis and L.M. Gonzalez for the help with figures.
We also thank C. Veiga, A. Nebra, M. Arndal and Sofia for
their assistance with sample collection and for their friendship.
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