scieee Science in your language
[en] (orig)

Diatom assemblages distribution in catalan rivers, NE Spain, in relation to chemical and physiographical factors

Abstract

Distribution patterns of epilithic diatom assemblages in streams in northeastern Spain and their relation to different environmental gradients are presented. Thirty-five sites were sampled covering a wide range of fluvial typologies. Gradient analysis was used to analyze the community structure and the major ecological gradients underlying variation in species composition. Two major gradients were evident; the first was a complex gradient from oligotrophic, pristine, fast-flowing highland rivers to mainly eutrophic rivers of low elevation; and the second related to altitudinal and seasonal variation of temperature. Two sets of factors were evident; one was associated with water chemistry, and the other to seasonal and physiographical variation. Variance partitioning allowed the separation of the effects of the different sets of environmental parameters. The contribution of physiography and water chemistry to diatom distribution was more unclear when the level of disturbance was intermediate. Considering the relatively high proportion of variation explained by physiographical variables alone, we suggest that when using diatoms to evaluate water quality, ecoregional characteristics of river stretches should also be considered.

Read accessible full text

Diatom assemblages distribution in catalan rivers, NE Spain, in relation to chemical and physiographical factors

Author: Sabater, Sergi; Leira Campos, Antón Manoel
Publisher: Elsevier
Year: 2005
Source: https://minerva.usc.es/bitstreams/9d7af124-b604-4f77-ae1b-19a372a0fb1c/download
Dia om assemblages dis ibu ion in Ca alan i e s, NE Spain, in ela ion o chemical and
physiog aphical ac o s
Manel Lei a1* and Se gi Saba e 2
1Cen e o he En i onmen & Depa men o Geog aphy Uni e si y o Dublin, T ini y
College, Dublin 2, I eland; Tel: +353-1-6083876; Fax: +353-1-6713397; E-mail: [email p o ec ed]
2Depa amen de Ciències Ambien als, Facul a de Ciències, Campus de Mon ili i, Uni e si a
de Gi ona, E-17071 Gi ona, Spain; Tel: +34-972 418 700: Fax: +34-972 418 150; E-mail:
[email p o ec ed]
Keywo ds: dia oms, epili hon, wa e quali y, mul i a ia e me hods, communi y analyses.
Abs ac
Dis ibu ion pa e ns o epili hic dia om assemblages in s eams in no heas e n Spain and hei
ela ion o di e en en i onmen al g adien s a e p esen ed. Thi y- i e si es we e sampled
co e ing a wide ange o lu ial ypologies. G adien analysis was used o analyse he
communi y s uc u e and he majo ecological g adien s unde lying a ia ion in species
composi ion. Two majo g adien s we e e iden ; he i s was a complex g adien om
oligo ophic, p is ine, as - lowing highland i e s o mainly eu ophic i e s o low ele a ion;
and he second ela ed o al i udinal and seasonal a ia ion o empe a u e. Two se s o ac o s
we e e iden ; one was associa ed wi h wa e chemis y, and he o he o seasonal and
physiog aphical a ia ion. Va iance pa i ioning allowed he sepa a ion o he e ec s o he
di e en se s o en i onmen al pa ame e s. The con ibu ion o physiog aphy and wa e
chemis y o dia om dis ibu ion was mo e unclea when he le el o dis u bance was
in e media e. Conside ing he ela i ely high p opo ion o a ia ion explained by
physiog aphical a iables alone, we sugges ha when using dia oms o e alua e wa e quali y,
eco egional cha ac e is ics o i e s e ches should also be conside ed.
1. In oduc ion
* Co esponding au ho : Cen e o he En i onmen & Depa men o Geog aphy Uni e si y o Dublin, T ini y
College, Dublin 2, I eland; Tel: +353-1-6083876; Fax: +353-1- 6713397; E-mail: lei am@ cd.ie
1
Chemical analyses o wa e p o ide a good indica ion o he chemical quali y o he aqua ic
sys ems, bu do no in eg a e ecological ac o s such as al e ed ipa ian ege a ion o al e ed
low egime and he e o e, do no necessa ily e lec he ecological s a e o he sys em (Ka e
al. 2000). Biological assessmen is a use ul al e na i e o assessing he ecological quali y o
aqua ic ecosys ems since biological communi ies in eg a e he en i onmen al e ec s o wa e
chemis y, in addi ion o he physical and geomo phological cha ac e is ics o i e s and lakes
(S e enson and Pan 1999).
Dia oms a e a siliceous class o algae epu ed o being e y sensi i e o chemical condi ions.
They usually accoun o he highes numbe o species among he p ima y p oduce s in aqua ic
sys ems (Pan e al. 1999). Consequen ly, hey a e equen ly used as biological indica o s o
wa e quali y and a numbe o me hods o moni o ing Eu opean i e s based on dia oms ha e
been al eady p oposed (Kelly e al. 1998, P ygiel e al. 2002). Dia om analysis ha e he e o e
been conside ed an impo an con ibu ion o he Eu opean Wa e F amewo k Di ec i e
(2000/60/EC), which aims o achie e a “good s a us” o all wa e s in he EU be o e 2015.
Despi e hei po en ial, he use o dia oms as biological indica o s o wa e quali y o lu ial
sys ems may be hampe ed because hei dis ibu ional pa e ns espond o a mul i ude o
di e en ac o s, anging om biogeog aphical o biogeochemical and human in luenced
(Po apo a and Cha les 2002). The challenge o de e mining which po ion o he dis ibu ion o
a gi en communi y is associa ed wi h human in luences and which is ela ed o he de ining
cha ac e is ics o a gi en eco egion needs o be esol ed (e.g. Hall e al. 1999). This knowledge
may be essen ial in he assessmen o biological quali y, which is based on he deg ee o
de ia ion om a e e ence biological popula ion. Biological in eg i y (Ka 1991) is measu ed
by compa ing a gi en si e wi h e e ence ecosys ems ha lie in simila geomo phological and
clima ic se ings bu a e no exposed o human impac . The sea ch o e e ence si es is o en
di icul in pa icula in egions o ex ensi e human ac i i ies, and his may hampe he
applica ion o his concep . Knowing in dep h he au oecological cha ac e is ics o species may
be ex emely help ul o make an objec i e sea ch o e e ence condi ions.
2
Mul i a ia e echniques ( e B aak and Ve donscho 1995) allow he elucida ion o ecological
ac o s, which explain mos o he a ia ion in dia om dis ibu ion. In pa icula , a iance
pa i ioning (Bo ca d e al. 1992) may help o sepa a e egional and gene al ac o s in luencing
dia om dis ibu ion. In his pape we use mul i a ia e echniques o elucida e he
physiog aphical, chemical and physical ac o s associa ed wi h dia om communi y s uc u e in
NE Spain.
2. Me hods
2.1. Dia om sampling, p epa a ion and analysis
This s udy was ca ied ou in a numbe o i e s loca ed in Ca alonia (NE Spain) (Fig. 1). These
si es we e selec ed o co e a wide ange o lu ial ypologies wi h di e en le els o human
dis u bance. Fi y-se en epili hic samples we e collec ed du ing win e (Feb ua y) and sp ing
(May) 2001. Dia oms we e p epa ed by acid oxida ion wi h concen a ed sulphu ic acid and
po assium dych oma e. Pe manen slides we e moun ed using Naph ax ( .i. 1.74). A leas 400
al es we e coun ed on each slide on andom ansec s wi h a ligh mic oscope using phase-
con as and Noma ski di e en ial in e e ence con as op ics a a magni ica ion o 1000x o
1250x. The iden i ica ion mainly ollowed K amme and Lange-Be alo (1986-1991).
2.2. Si e cha ac e iza ion
The mo phological and clima ic di e si y o NE Spain de e mine an impo an spa ial
he e ogenei y in he egion. The Py enees and nea by a eas ha e clima es ypical o high
moun ainous egions, wi h minimum empe a u es below 0ºC, annual ain all o abo e 1,000
mm and hea y snow all in he win e . Coas al a eas ha e mild, empe a e wea he , wi h
empe a u es ha ise and ain all ha dec eases as one mo es om no h o sou h. Inland, a
om he sea, he clima e is ypical o con inen al Medi e anean egions, wi h cold win e s and
e y ho summe s. The si es we e selec ed o co e a la ge g adien anging om p is ine o
pollu ed wi h di e en le els o human dis u bance, co e ing he majo ypes o
geomo phological and physiog aphical condi ions.
Chemical da a (conduc i i y, suspended ma e , dissol ed oxygen, pH, BOD5, NH s up 7(+ )-N,
Ca2+, PO
Com
b i n
–P, Mg2+, NO s up 7(- ) -N, NO s up 7(- )-N, K+, Na+, SO
Com
b i n
, Cl-) o he si es we e ob ained
3
om he Ca alan Wa e Agency (ACA) which moni o s hem ou inely. Wa e samples we e
analysed ollowing s anda d p ocedu es (APHA 1989). The ollowing physical desc ip o s o
he si es we e used o his s udy: wa e empe a u e, al i ude, slope, s eam o de , ca chmen
a ea, dis ance o sou ce, and bi u ca ion a io (i.e. he quan i a i e a io de e mined be ween
he numbe o s eam segmen s in one o de and he nex ). Pa s o hese da a we e de i ed
om maps and ield obse a ions, while o he s we e p o ided by he ACA.
2.3. Da a analysis
Dia om da a we e analysed wi h de ended co espondence analysis (DCA) (Hill and Gauch
1980) o de e mine he leng h o he g adien o he i s wo axes. DCA indica ed ha he
g adien leng h was g ea e han 2 s anda d de ia ion uni s (3.191); he e o e, he use o
unimodal o dina ion echniques would be app op ia e ( e B aak 1987). Consequen ly,
co espondence analysis (CA), an indi ec –g adien o dina ion, was used o de e mine he majo
pa e ns o a ia ion in species composi ion da a wi hou inco po a ing da a on en i onmen al
a iables. Cons ained o dina ion (canonical co espondence analysis, CCA) was used o ela e
dia om assemblage s uc u e o all p edic o en i onmen al a iables and o explo e he
ela ionships among and be ween species and he en i onmen ( e B aak and Ve donscho
1995). Acco ding o his p elimina y CCA, we iden i ied collinea a iables and selec ed a
subse o a iables based on inspec ion o a iance in la ion ac o s (VIF<20) ( e B aak and
Šmilaue 1998). S ep-wise o wa d selec ion and Mon e Ca lo pe mu a ion es we e used o
educe u he he en i onmen al a iables o hose co ela ed signi ican ly wi h he de i ed
axes ( e B aak and Šmilaue 1998), a a cu -o poin o P=0.05. P obabili ies o mul iple
compa isons we e co ec ed using he Bon e oni co ec ion. Pa ial CCA was used o sepa a e
and examine he ela i e impo ance o he species da a o se e al se s o explana o y a iables
on he dia om assemblages (Bo ca d e al. 1992). We we e in e es ed in sepa a ing he e ec s o
he wa e chemis y om all he o he a iables and hen es ing whe he hese wo di e en
g oups o a iables we e edundan o each o he , o whe he hey each explained unique
aspec s o species composi ion.
4
Only hose axa ha we e obse ed in mo e han 5% o he samples we e included in analyses
o axa abundances o minimize he in luence o a e axa. Taxa abundance was squa e oo
ans o med in all analyses o educe he e ec o highly a iable popula ion densi ies on
o dina ion sco es. En i onmen al da a (excep pH and pe cen age slope) we e loga i hmically
ans o med be o e analysis o educe skewed dis ibu ions. All o dina ions we e pe o med
using CANOCO e sion 4.1 ( e B aak and Šmilaue 1998).
3. Resul s
3.1. En i onmen al cha ac e is ics o si es
Ri e s o he s udy a ea a ied widely in wa e quali y and habi a cha ac e is ics. Conduc i i y
inc eased downs eam and he highes alues o suspended solids we e ound a he lowe mos
si es. Nu ien concen a ions also inc eased downs eam bu a ied mo e spa ially han did
o he majo a iables because he ex ensi e applica ion o chemical e ilize s in ag icul u e and
di e se sewage inpu s (Table 1 & 2). Some s udy si es we e loca ed in densely popula ed,
hea ily indus ialized o in ensi e ag icul u al a eas, hus ecei ing high inpu s o o ganic
ma e and indus ial sewage. O he si es we e less dis u bed, as - lowing and wi h a s ony o
s ony-g a el bo om, cha ac e is ic o moun ainous a eas. Finally, o he s ha e a lowland
cha ac e , being slow- lowing.
3.2. Species composi ion o dia om assemblages
A o al o 195 axa we e ound. Only 33 axa we e obse ed in mo e han 5% o he samples.
Ampho a pediculus (Kü zing) G unow was he mos abundan axon and occu ed in up o 78%
o all samples. The second mos abundan species we e Achnan hes minu issima Kü zing and
Na icula g ega ia Donkin. CA o dina ion esul s showed ha 15.2% o dia om assemblages
a iance was explained on axis 1, and a u he 13% on axis 2. Si es on he le side o he i s
CA axis (Fig. 2) lay in densely popula ed, indus ialized o ag icul u al a eas, ecei ing high
inpu s o o ganic ma e and indus ial discha ge. Dia om axa showing maximum abundance in
samples om si es si ua ed on he le side o he diag am included Ni zschia capi ella a
Hus ed , Ni zschia us ulum (Kü zing) G unow and Na icula subminuscula Manguin. Si es less
in luenced by human ac i i ies had highe alues on CA axis 1 and a e clus e ed on he igh
5

hand side o he diag am. Dia oms abundan in hese samples included Achnan hes minu issima
Kü zing, Achnan hes biasole iana G unow and Gomphonema pumilum (G unow) Reicha d &
Lange-Be alo . The second axis is mos p obably e lec ing seasonal di e ences in he dia om
communi ies, since he win e samples had highe alues, while hose aken du ing sp ing ime
had lowe alues on CA axis 2.
3.3. Impo an en i onmen al a iables
The 21 en i onmen al a iables al oge he explained 52.0% (2.067 s.d. uni s) o he o al
a ia ion wi hin he species da a. The i s wo axes explained a signi ican po ion o a iance
in he dia om axa da a (P<0.01). The la ge a iance in la ion ac o s (>20) o he explo a o y
CCA indica ed edundancy among dis ance o sou ce, sulpha es, po assium, sodium,
magnesium, chlo ides, calcium and ca chmen ’s a ea, and we e subsequen ly excluded om he
en i onmen al da a se .
CCA wi h o wa d selec ion o species da a indica ed ha conduc i i y, wa e empe a u e,
BOD5, al i ude, s eam o de and ni a e ni ogen we e he en i onmen al a iables ha
accoun ed o signi ican (P<0.05) po ions o he o al a iance in dia om species composi ion
(Table 3). Conduc i i y explained he la ges po ion (7.3%) o he o al uncons ained a iance.
CCA o dina ion plo s (Fig. 3a, b) p ima ily exp essed wo majo g adien s. The i s one
a anged si es om oligo ophic, p is ine, as - lowing highland i e s o p edominan ly
eu ophic i e s o low ele a ion. The second g adien is likely in eg a ing a seasonal and
al i udinal a ia ion o empe a u e. Cyclo ella meneghiniana Kü zing, Na icula subminuscula,
Ni zschia us ulum and Ni zschia capi ella a ha we e mainly obse ed a si es wi h high
conduc i i y and BOD5, usually a lowe al i udes. Achnan hes minu issima and Ni zschia
on icola G unow we e ins ead associa ed wi h mo e p is ine wa e s and high al i ude si es.
3.4. Rela i e impo ance o chemical s. physiog aphical ac o s
Pa ial CCA analyses showed ha 25.5% (0.526) o he o al a ia ion in he species da a could
be explained by bo h se s o a iables oge he . Wa e chemis y explained a conside ably high
p opo ion (12.9%, 0.266) o he o al a iabili y in species da a. The ac ion o he o al
a iance a ibu ed o physiog aphical a iables was 11.6% (0.239). Since he alue o he
6
in e sec ion (0.021, 1.0%) was much smalle han he ac ion o he a ia ion explained
independen ly by bo h se s o a iables, we can conclude ha he wo se s o a iables we e
p ima ily explaining unique aspec s o species composi ion.
The summa y o he o dina ion gi es an o e all measu emen o how much a ia ion can be
ela ed o bo h explana o y a iables. Bu no all species a e equally well explained by he same
se o en i onmen al a iables. The i o species can be used as a measu emen o ind ou
which species a e well ep esen ed and he pe cen age o a iance i by each se o explana o y
a iables. The pe cen age o a iance explained by wa e chemis y and he physiog aphical
ac o s wi h espec o he uncons ained a iance di e s among he di e en species (Table 4).
Na icula a omus (Kü zing) G unow a . pe mi is (Hus ed ) Lange-Be alo , Ni zschia
capi ella a, N. us ulum and Cyclo ella meneghiniana had hei dis ibu ions mos ly explained
by he wa e chemis y. Cocconeis pediculus Eh enbe g and C. placen ula Eh enbe g,
Gomphonema oli aceum (Ho nemann) B ébisson and Ni zschia inconspicua G unow we e
amongs he mos ela ed o he physiog aphical g oup o a iables. Finally, Melosi a a ians
Aga dh, Na icula subminuscula, Cymbella minu a Hilse ex Rabenho s and Ni zschia on icola
we e bo h explained by he physiog aphical and chemical a iables.
4. Discussion
App oaches o he use o dia om communi ies as biological indica o s di e ge om he di ec
applica ion o dia om indices, which ha e been de eloped and widely used in Eu opean wa e s
(Descy and Cos e 1991, Kelly and Whi on 1995) o mul ime ics o mul i a ia e app oaches
(e.g. IBI o index o biological in eg i y), which a e p e e ed in he Uni ed S a es (Hill e al.
2000, Ka 1991). I espec i e o he me hod used, unce ain ies s ill exis conce ning he
uniqueness o gene al applicabili y o a gi en diagnosis p o ided by he dia om communi ies.
This is especially he case when pollu ion o nu ien en ichmen is no d i ing communi y
composi ion. Leland and Po e (2000) obse ed ha incomple e p edic ion o phospho us
loading by dia om communi ies occu ed sys ema ically a lowe phospho us concen a ions.
Saba e (2000) showed ha dia om indices success ully indica ed he e ec o a ca as ophic
hea y me al spill on a i e sys em, bu ailed o eliably de ec he eco e y. Thus in cases
7
whe e dis u bance is no ex eme, eco egional cha ac e is ics (e.g. geochemical ea u es,
empe a u e, wa e low) and esponses o en i onmen al s esso s (e.g.: nu ien en ichmen ,
habi a al e a ion, oxic inpu s) may combine o p oduce a con using pic u e.
The use o mul i a ia e analyses in he p esen s udy showed he g adien om p is ine o
pollu ed i e s as being he mos impo an in s uc u ing i e ine dia om assemblages o i e
wa e s in NE Spain. A esponse o dia om communi ies o nu ien en ichmen appea ed o be
e iden , al hough he CCA showed ha he e ec o nu ien s and conduc i i y on species
composi ion was simila . Many s udies ha e shown ha dia om communi ies a y along
g adien s o ionic concen a ion (Saba e and Roca 1992). Mos o en he inc ease in ionic
con en is accompanied by nu ien en ichmen (Saba e and Saba e 1988, Leland and Po e
2000). The downs eam en ichmen wi h dissol ed sal s, and nu ien s in pa icula , is
pa icula ly clea in his s udy. The o e iding e ec o conduc i i y and nu ien s on he
composi ion o dia om communi ies has been ecognized ecen ly h ough he analysis o la ge
da a se s (Po apo a and Cha les 2003). In hese ci cums ances ca e mus be aken no o con use
he e ec o ionic con en wi h ha o nu ien en ichmen .
I is impo an o s ess ha dia om dis ibu ion was no only a ec ed by chemical
cha ac e is ics. CCA showed ha dia om communi y s uc u e could also be ela ed o
empe a u e, al i ude and s eam o de . Gene al desc ip o s summa izing physical habi a (e.g.:
s eam size and s eam o de ) ha e been associa ed wi h dia om dis ibu ion (Molloy 1992).
Physiog aphical a iables, especially al i ude and s eam o de , may p o ide in o ma ion on
how i e basins a e s uc u ed and, analogously, on how dis u bances occu ing a he basin
scale (human ac i i ies, changes in land use o in ege a ion) may a ec dia om communi ies.
A smalle spa ial scales i has been also shown ha subs a um ype and habi a he e ogenei y
a e ela ed o species composi ion and p e e en ial mo phological g ow h o ms o dia om
communi ies (Leland 1995). A he basin scale used in his s udy, al i udinal g adien may be
pa ly ela ed o he ionic en ichmen o i e wa e s. Ma gale (1960) sugges ed ha algal
assemblages (including dia oms) we e ela ed o he geochemical and nu ien composi ion o
wa e , as well as o he hyd aulics and geomo phology o he i e sys em. This p edic ion
8
ad anced he indings based on he use o mul i a ia e analysis, as well as he p edic ions o he
Ri e Con inuum Concep (Vanno e e al. 1980). Ou analyses showed ha pa e ns o dia om
dis ibu ion could be a ibu ed no only o wa e quali y a ia ion, bu also o physiog aphical
p ocesses. The dis ibu ion o some common and abundan axa in ou da a se is la gely
in luenced by physiog aphical pa ame e s. Th ee di e en g oups o axa can be iden i ied wi h
ega d o hei link o he chemical, physiog aphical o mixed (o e lapped) in luences (Table 4).
Al hough mos o hese axa ha e widesp ead dis ibu ion elsewhe e, p e ious s udies sugges ed
ha hei occu ence is ela ed o speci ic ype o en i onmen s. Fo example, Gomphonema
oli aceum has a dis ibu ion es ic ed o low-o de s eams wi h high alkalini y and low
nu ien inpu (Pa ick 1977), indica ing s ong physiog aphical in luence. Na icula a omus a .
pe mi is and Ni zschia capi ella a occupied highly pollu ed sec ions o i e s, and we e
he e o e amongs he mos in luenced by he wa e chemical cha ac e is ics o he i e s. Thei
occu ence was i espec i e o he s eam o de o loca ion (Lange-Be alo 1979). Melosi a
a ians was ound mainly in downs eam sec ions o he s udied wa e cou ses, occupying
nu ien -en iched, mine alised wa e s (Ma gale 1951). This species is he e o e an exp ession
o he o e lapping in luence be ween he chemical and he physiog aphical ac o s.
5. Conclusions
A p esen he in luence o small-scale ac o s on dia om communi y s uc u e is poo ly
unde s ood. This makes i di icul o es ablish any s anda d me hodology o assess wa e
quali y in a wide geog aphical a ea, pa icula ly in hose si es wi h in e media e dis u bance.
Se ing e e ence s anda ds o biological quali y will equi e he ca e ul de elopmen o da a
se s along majo en i onmen al g adien s unde lying species composi ion, in o de o
unde s and he p ocesses ha a e s uc u ing dia om assemblages. We ha e demons a ed ha a
conside able p opo ion o a ia ion in he dia om assemblages can be explained by
physiog aphical ac o s; i would he e o e be mo e eliable o de elop dia om-based
app oaches o wa e quali y es ima ion ha a e applied a he eco egional le el o in
homogeneous geog aphical a eas, hus a oiding unwan ed e ec s on da a se s.
9