discovery of the rare freshwater brown alga pleurocladia
TRANSCRIPT
Western North American Naturalist Western North American Naturalist
Volume 73 Number 2 Article 3
7-5-2013
Discovery of the rare freshwater brown alga Discovery of the rare freshwater brown alga Pleurocladia lacustris Pleurocladia lacustris
(Ectocarpales, Phaeophyceae) in California streams (Ectocarpales, Phaeophyceae) in California streams
John D. Wehr Fordham University, Armonk, NY, [email protected]
Rosalina Stancheva California State University, San Marcos, CA, [email protected]
Kam Truhn Fordham University, Armonk, NY, [email protected]
Robert G. Sheath California State University, San Marcos, CA, [email protected]
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Recommended Citation Recommended Citation Wehr, John D.; Stancheva, Rosalina; Truhn, Kam; and Sheath, Robert G. (2013) "Discovery of the rare freshwater brown alga Pleurocladia lacustris (Ectocarpales, Phaeophyceae) in California streams," Western North American Naturalist: Vol. 73 : No. 2 , Article 3. Available at: https://scholarsarchive.byu.edu/wnan/vol73/iss2/3
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It has been hypothesized that due to theirsmall size, short generation time, and ease ofdispersal, microbial and algal taxa predomi-nantly have cosmopolitan distributions (Fencheland Finlay 2004, Vanormelingen et al. 2008).But important exceptions exist. The well-rec-ognized freshwater green alga Aegagropila lin-naei Kützing is known on at least 3 continents,yet it exists in disjunct locations and is declin-ing in number due to eutrophication and avery limited potential for dispersal (Boedekeret al. 2010). Other species of freshwater algaehave very specific ecological requirements,making their biogeography similarly restricted.The benthic desmid Oocardium stratum Nägeli,a species known since 1849, is rarely observed
and is regarded as globally rare, possibly dueto its close association with CaCO3 deposi -tion (travertine) in limestone springs (Pente-cost 1991, Rott et al. 2010). In recent years,evidence has been growing that other fresh-water algae have limited distributions. Severalare regional endemics with declining popula-tions sufficient to receive conservation status(Kilroy et al. 2007, Cotterill et al. 2008). Thefactors leading to such declines are varied butinclude specialized ecological requirementsand loss of habitat, which can lead to furtherisolated and rare taxa (Sherwood et al. 2004,Coesel and Krienitz 2008). In other cases,reports of algal endemism may be the result ofeither under-sampling or taxonomic confusion
Western North American Naturalist 73(2), © 2013, pp. 148–157
DISCOVERY OF THE RARE FRESHWATER BROWN ALGA PLEUROCLADIALACUSTRIS (ECTOCARPALES, PHAEOPHYCEAE)
IN CALIFORNIA STREAMS
John D. Wehr1,3, Rosalina Stancheva2, Kam Truhn1, and Robert G. Sheath2
ABSTRACT.—Pleurocladia lacustris A. Braun is a freshwater member of the Phaeophyceae, a class of algae that occursalmost entirely in marine waters. It has previously been reported from only about 13 freshwater locations worldwide,just 2 of which are in North America. Outside of North America, P. lacustris has been listed as a threatened species onseveral European red lists. In this paper, we report the discovery of P. lacustris in 3 calcareous streams draining theSanta Lucia Mountains in coastal California, sites that are more than 1200 km from the nearest known population. Pleu-rocladia lacustris is a filamentous, benthic species that forms distinctive hemispherical colonies. It co-occurs with thegreen alga Cladophora glomerata and species of cyanobacteria (Rivularia, Nostoc, Schizothrix spp.). Detailed color illus-trations of the diagnostic macroscopic and microscopic features are provided and appear identical to those features ofEuropean populations. In the California streams, P. lacustris and other associated algae co-precipitate CaCO3 to formcarbonate crusts on rocks. Preliminary ecological data are consistent with other streams and lakes in Europe where P.lacustris has also been reported (pH > 8.0, calcareous substrata, travertine). The global distribution of this presumedrare alga is also described and examined with respect to a specialized ecological niche.
RESUMEN.—Pleurocladia lacustris A. Braun es un organismo de agua dulce perteneciente a Phaeophyceae, una clasede algas que habita casi exclusivamente aguas marinas. Ha sido reportada solo en aproximadamente trece sitios de aguadulce en todo el mundo y sólo dos sitios en los Estados Unidos. Fuera de Norteamérica, está incluida en varias listasrojas de Europa como especie amenazada. En este trabajo presentamos el hallazgo de P. lacustris en 3 arroyos con mate-rial calcáreo que confluyen en las Montañas de Santa Lucía en la costa de California y se encuentran a más de 1200 kmde la población conocida más cercana. Es una especie filamentosa, bentónica, que forma colonias hemisféricas distinti-vas y coexiste con el alga verde Cladophora glomerata y especies de cianobacterias (Rivularia, Nostoc, Schizothrix spp.).Mostramos ilustraciones detalladas en color de las características macroscópicas y microscópicas, donde se puede apre-ciar que son idénticas a las poblaciones europeas. En los arroyos de California, P. lacustris y otras algas asociadas precip-itan CaCO3 y forman cortezas de carbono sobre las rocas. La información ecológica preliminar coincide con la de otrosarroyos y lagos de Europa donde se registró la presencia de esta alga (pH > 8.0, sustrato calcáreo, travertino). Además,se describe y se estudia la distribución global de esta alga aparentemente poco frecuente en relación con un nichoecológico específico.
1Louis Calder Center–Biological Field Station and Department of Biological Sciences, Fordham University, Armonk, NY 10504.2Department of Biological Sciences, California State University, San Marcos, CA 92096.3E-mail: [email protected]
148
(Whitford 1983, Vanormelingen et al. 2008).The discovery of new populations of a pre-sumed rare algal species may help to informthis discussion.
The Phaeophyceae is a large and diverseclass of algae with roughly 270 genera and up -wards of 2000 taxa, of which more than 99%occur in marine waters (Wehr 2003). They rangein size from microscopic filaments to largekelps that form huge underwater for ests. Thefreshwater members of this class are modestin size, ranging from small filamentous tufts topseudoparenchymatous crusts (united prostratefilaments), which may form macroscopicallyrecognizable forms in streams and rivers (Kusel-Fetzmann 1996). Few freshwater species arecommonly observed. The crust-forming Herib-audiella fluviatilis (Areschoug) Svedelius is themost widely recognized spe cies, with a fewhundred populations identified from many coun -tries, although thus far only in the northernhemisphere (Wehr 2003). One of the lesser-known freshwater representatives is Pleuro-cladia lacustris A. Braun, a fila mentous speciesdescribed more than 150 years ago (Braun1855), yet observed only from few locations.Interestingly, P. lacustris has been reportedfrom widely separated calcareous freshwaterenvironments (lakes and streams) and also sev-
eral intermittently marine or brack ish loca-tions (Eloranta et al. 2011). Some freshwaterpopulations have apparently been extirpateddue to habitat degradation and urbanization(Sukopp 2003, Täuscher 2011, Wehr 2011),causing some European countries to list thisspecies on their conservation red lists (Sie -mińska 2006, Täuscher 2010). In this paper,we report the recent discovery of P. lacustrisin 3 streams in California. These streams con-stitute the fourth location for North America(third freshwater location), more than 1200 kmfrom the nearest known population. We alsoexamine the distribution of this species globallyand discuss the presumed rarity of its occur-rence (e.g., Siemińska 2006, Täuscher 2011).
STUDY AREA
The study was conducted along the Big Surcoast in central California (Fig. 1). A previouscollection of periphyton taken from a streamin this area on 23 June 2010 by the SurfaceWater Ambient Monitoring Program (SWAMP)of the California State Water Resources ControlBoard included material that was thought tobe P. lacustris. In the present study, we sur-veyed 12 streams that drain the Santa LuciaMountains between Pfeiffer Big Sur State Parkand San Simeon, California. Most are first- orsecond-order streams and typically have verysteep gradients with a calcareous geology (Hen -son and Usner 1993); CaCO3 precipitationand travertine formation are apparent at manylocations. The region has a cool-Mediterraneanclimate, and riparian vegetation is composedmainly of white alder (Alnus rhom bifolia), big -leaf maple (Acer macrophyllum), arroyo willow(Salix laseolepis), black cottonwood (Populustrichocarpa), California bay (Umbellularia cali-fornica), and in some locations, coast redwood(Sequoia sempervirens). The streambed at mostsites had variable canopy cover, with areasranging from open sun to heavy shade. Fur-ther details of the physical conditions of thesestreams are described by Rundio (2009).
METHODS
Stream sites were accessed from along a40-km stretch of California State Route 1, northfrom Cambria, California, 12–14 March 2012.All sampling reaches were located at least 150m upstream of any marine water. We collectedalgae by using knives and razor blades to
2013] FRESHWATER PLEUROCLADIA IN CALIFORNIA 149
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Fig. 1. Location of 3 stream populations of Pleurocladialacustris (solid circles), with map of study area in westcentral California (inset).
sample rocks, and we inspected the materialwith a Swift FM-31 field microscope. At siteswhere P. lacustris was present, samples werecollected into bags or tubes (at least 10 repli-cates per site) and separated for future use inmi crophotography, lab cultures, DNA extrac-tion, and preserved samples. Live materialwas placed in sterile, 120-mL Whirl-Pak® bagsand stored on ice. Water temperature and spe-cific conductance were measured in situ byusing a YSI EC300 meter, and pH was mea-sured by using a YSI pH10A meter. A portablelaboratory microscope (Nikon 50i with LEDillumination) was later used after each sam-pling day to confirm identifications conductedin the field.
Samples were shipped overnight to ourlaboratories for further observations and mi -crophotography. In the laboratory, live algalsamples were prepared for wet-mount micro -scopy by using sterile probes to separate colo -nies prior to observation. Occasionally, diluteacid (1% HCl) was added to heavily calcifiedcolonies to improve clarity. Specimens wereobserved using a Nikon Eclipse E600 micro-scope with Nomarski (DIC) optics (200X, 400X,and 1000X total magnification), photographedusing a Nikon DS-Fi1 digital camera, andprocessed and measured using NIS-Elementssoftware. Identifications were based on Kusel-Fetzmann (1996), Wehr (2003), and Elorantaet al. (2011). Georeferenced voucher specimenswere submitted to the William and LyndaSteere Herbarium at the New York BotanicalGarden (NYBG), and DNA samples werestored frozen (–40 °C) at the NYBG MolecularSystematics Laboratory for a later study. Smallportions of live material were placed in algalgrowth media and maintained at FordhamUniversity and the NYBG.
Past records of Pleurocladia lacustris werecollected from published literature, personalcommunications with authors, and herbariumrecords. Where precise georeferenced records
were not available, latitude and longitude val-ues for the names or nearest water body wereused. Geographic data for all populations werecompiled and mapped using ArcGIS v. 10.
RESULTS
Of 7 streams sampled, we located 3 thatcontained populations of Pleurocladia lacustris(Table 1). Water at all sites was alkaline (pH>8.0) and had moderate specific conductance(average ~250 mS ⋅ cm–1). When present, thisalga was among the most common and macro-scopically recognizable species in the stream.Along with Pleurocladia, the filamentous greenalga Cladophora glomerata and colonial cyano -bacteria Nostoc, Rivularia, and Schizothrixspecies were also common. Macroscopically,the morphology of Pleurocladia appeared tohave 2 distinct forms: small irregular, flatbrown spots on rocks (Fig 2A) and brown totan-colored hemispherical tufts (Fig. 2B). Bothforms occurred in running water, but thehemispherical form was more common in low-current microhabitats, whereas the spreading(flat-form) was more common in riffles. In thefield, colonies of both forms ranged in sizefrom about 1 to 5 mm in diameter and ap -peared dark brown or reddish brown in color.Where colonies were heavily calcified, theyappeared light tan in color. Those that pro-duced large quantities of elongate hyaline hairs(narrow, unpigmented filaments), grayish mats,or tufts were also apparent.
Microscopically, basal filaments were alluniaxial and ranged in diameter from 12 to 20mm, whereas upright filaments were 9–14 mmwide (Figs. 2C–D). Branching frequency wasirregular, although filaments in larger cush -ion-like colonies tended to be more elongateand have fewer side branches. In smaller oryounger colonies, the typical comb-like ap -pearance was common. In both forms, cells inthe main axes ranged from 10 to 35 mm in
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TABLE 1. Locations and ecological conditions of California streams from which Pleurocladia lacustris was collected in2012.
Stream Salmon Creek Willow Creek Villa Creek
Latitude (N) 35°48�56.80� 35°53�37.23� 35°50�59.24�Longitude (W) 121°21�31.82� 121°27�40.71� 121°24�28.23�Date 12 Mar 2012 12 Mar 2012 13 Mar 2012Temperature (°C) 9.3 11.4 10.9pH 8.22 8.45 8.50Specific conductance (mS ⋅ cm−1) 220.9 253.2 271.2
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Fig. 2. Morphology of field populations of Pleurocladia lacustris from California streams: A, macroscopic appearanceof dark brown, spreading (flat-form) colonies on rocks; B, macroscopic appearance of cushion-forming colonies (grayishmaterial is a network of elongate hyaline cells); C, microscopic appearance of cushion-forming colonies with terminalhyaline cells (arrows); D, microscopic appearance of spreading colonies, with unilocular sporangia (arrows) and CaCO3encrusting the colony base (brackets); E, detail of filaments with single parietal chloroplast and numerous oil bodies;F, detail of unilocular sporangium (left) on lateral side branch.
length. Chloroplasts were single and parietal,usually filling one-half to three-quarters of thecell diameter (Fig. 2E). In older cells, somechloroplasts appeared twisted or lobed. Nu -merous spherical bodies, assumed to be oildroplets, were scattered throughout the cells.When present, terminal hyaline hair cells (Fig.2C) often would exceed 200 mm in length.Macroscopically, some appeared to extend morethan 1 mm. Large, ovoid, or clavate unilocularsporangia (20–40 × 30–85 mm) were frequentlyformed on short side branches (Fig. 2F). Pluri -locular sporangia were not observed.
Following the discoveries in California, theglobal distribution of Pleurocladia lacustrisnow includes 8 countries, and 4 locations inNorth America, totaling 27 separate freshwa-ter stream or lake sites. Most sites are concen-trated in western and northern Europe (Fig. 3,Appendix), and many of these are located ineastern Sweden, including several rivers inthe eastern Uppland province north of Stock-holm and various standing waters in the Öre-grund Archipelago area (Israelsson 1938, Waern1952). Ecological information from these re -ports is spotty, but many researchers commenton the calcareous nature of P. lacustris. Of allthe freshwater populations currently known,the California sites are nearest to a populationin the Green River, Utah, downstream ofFlaming Gorge Dam (Ekenstam et al. 1996,Wehr 2003). These 2 locations are more than
1200 km apart, but the macroscopic morphol-ogy of the 2 populations is indistinguishable interms of cell dimensions, branching pattern,and sporangia. Both occur in calcareous river-ine habitats and commonly have CaCO3 en -crusting at the base of the colonies (Fig. 2D).One recent collection has also been madefrom a deep limestone pool in South Australia(deposited in the National Herbarium of NewSouth Wales; listed as Pleurocladia sp. nov.but without verification; #NSW 486949), asite which is ~13,000 km from the Californiapopulations and ~15,000 km from the nearestfreshwater population in Europe.
DISCUSSION
The evidence for the existence of rare spe -cies of freshwater algae and other protists hasbeen regarded somewhat skeptically by someresearchers (Whitford 1983, Fenchel and Fin-lay 2004). Reports of restricted distributions infreshwater algae may simply be the result ofundersampling (Foissner 2008). Some speciesare seasonally ephemeral and missed by spotsampling. Others have cryptic life stages thatroutine surveys may miss. However, studiesof freshwater algae in North America havespanned more than 150 years, and certain spe -cies are still rarely seen. Evidence from multi-ple studies in Europe suggest that there arerare, threatened, and endangered species of
152 WESTERN NORTH AMERICAN NATURALIST [Volume 73
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Fig. 3. Geographic locations of all known populations of Pleurocladia lacustris (solid circles). Details of individualsites, including designations of freshwater, brackish, and marine locations, are given in the Appendix.
algae that require conservation efforts (Brodieet al. 2007, Cotterill et al. 2008, Ros et al.2009). This idea has been raised specificallyfor Pleurocladia lacustris in the United King-dom, where the only known habitats havebeen altered through nutrient pollution (Brodieet al. 2007) and the species may have beenregionally extirpated (Wehr 2011). Similarly,Friedrich et al. (1984) documented that all 4species of freshwater brown algae known fromGermany are listed as endangered to differentdegrees. This includes the population of Pleu-rocladia lacustris from its type location in Ger-many, where it was first described by Braun in1855 and where it is now listed as threatenedwith local extinction (Geissler 1988). As of thisdate, it is not known if this important popula-tion still exists.
The ecological data for P. lacustris assem-bled so far indicate that the species is re -stricted to fairly nutrient-rich, alkaline, cal-careous environments (Israelsson 1938, Waern1952, Kusel-Fetzmann 1996) and that it isabsent from softwater or humic-stained sys-tems (Kann 1940, Eloranta et al. 2011). A sin-gle sample in June 2010 taken from one of oursites (Salmon Creek) by the Surface WaterAmbient Monitoring Program of the CaliforniaState Water Resources Control Board indi-cated moderately high specific conductance(372 mS ⋅ cm–1), very low TDP (9.5 mg ⋅ L–1),TDN 63.6 mg ⋅ L–1, and alkaline pH (8.5) butclearly nonsaline. These data collectively indi-cate that the alga occurs in systems with pH>7.5 and specific conductivity >200 mS ⋅cm–1. No extensive analyses of water chem-istry requirements exist yet for this species.However, preliminary lab experiments suggestthat P. lacustris may tolerate a wide range ofphosphorus conditions through the productionof hyaline hairs (Wehr 2003). Hyaline hairs inother species have been documented to utilizeorganic-P sources (Gibson and Whitton 1987).Pleurocladia lacus tris has been collected fromsmall ponds to very large lakes (e.g., Klebahn1895, Kirkby et al. 1972, Kahlert et al. 2002,Young et al. 2010), as well as from streams andrivers (Eken stam et al. 1996, Kusel-Fetzmann1996, this study).
Interestingly, in addition to occurring in anumber of fully freshwater systems, P. lacus-tris has been reported from brackish environ-ments, often in areas where limestone is pres -ent (Waern 1952, Wilce 1966, Konan-Brou and
Guiral 1994, Aysel et al. 2008). The specificconductance data from the 3 California sites(220–270 mS ⋅ cm–1) indicate that these popu-lations have little or no marine influence. Thespecies is strictly benthic in habit but growson a variety of substrata, with several reportsof occurrence on stones (Kann 1993, Kusel-Fetzmann 1996, Kahlert et al. 2002), as an epi-phyte on higher plants or other algae (Kirkbyet al. 1972, Szymanska and Zakrys 1990, Younget al. 2010), and even as an endophyte in a fewinstances (Waern 1952). Kann and Tschamler(1976) demonstrated that the alga also colo-nizes artificial substrata (plastic and glassslides) in suitable habitats. Given these eco-logical limitations, this species may be geo-graphically limited by a restriction to calcare-ous habitats.
Pleurocladia lacustris was the first freshwa-ter species of brown algae described; yet it isan enigma with regard to its ecological re -quirements and geographic distribution. Withfreshwater and brackish water populations,and relatively few known locations, the dis-covery of new populations is noteworthy.Further biodiversity surveys may clarify theextent to which P. lacustris may be a rarespecies. But, given its widespread locationsseparated by long distances, 4 broad questionsemerge: (1) Is “Pleurocladia lacustris,” as re -ported, one species or several? It may be thatwhile its morphological characteristics arehighly consistent among populations, isola -tion and divergence may have resulted in sev-eral cryptic species, as demonstrated in otherfreshwater and marine taxa (Casamatta et al.2003, Saunders 2008). Future genetic analyseswill shed light on this question. (2) If its distri-bution is restricted, is P. lacustris limited by itsecological requirements or perhaps by disper-sal? Field data suggest that this species pre -fers calcareous conditions, but detailed experi-ments are needed to confirm either factor as acause of its ecological and geographic restric-tion (e.g., Telford et al. 2006, Boedeker et al.2010). (3) Is P. lacustris a rare species or eco-logically restricted? Though habitat destruc-tion has reduced its distribution in some areas,P. lacustris could still be undersampled ormissed in biodiversity surveys. New surveyscan employ molecular methods, such as ge -nome shotgun sequencing and DNA bar-coding, to reveal hidden biological diversityand the presence of underreported taxa (e.g.,
2013] FRESHWATER PLEUROCLADIA IN CALIFORNIA 153
Eisen 2007). (4) What is the relationship be -tween freshwater and brackish (intermittentlymarine) populations of P. lacustris, both interms of ecological adaptations and evolution?Laboratory studies can elucidate the ability ofnear-coastal and inland populations to adapt toa range of salinities (e.g., Dittami et al. 2012),whereas population genetics studies may ex -plain the evolutionary route this species mayhave taken from marine to freshwater habitats(e.g., Müller et al. 1998).
ACKNOWLEDGMENTS
We thank the Surface Water Ambient Moni -toring Program (SWAMP)–California State Wa -ter Resources Control Board for providing theinitial periphyton sample containing Pleuro-cladia. We also thank Christina Vanderwerkenfor her enthusiastic and capable assistancewith fieldwork, as well as Professor RobertWilce (University of Massachusetts) for adviceon the biology and distribution of Pleurocla-dia. JDW was supported in part by a FacultyResearch Grant from Fordham University. RGSand RS were supported by the California StateWater Resources Control Board–SWAMP.
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156 WESTERN NORTH AMERICAN NATURALIST [Volume 73A
PPE
ND
IX. L
istin
g of
all
know
n po
pula
tions
of P
leur
ocla
dia
lacu
stri
s w
orld
wid
e. M
any
earl
y re
port
s la
ck p
reci
se la
titud
e an
d lo
ngitu
de u
nles
s sp
ecifi
c pl
ace
nam
es w
ere
prov
ided
(neg
ativ
e la
titud
e =
sou
ther
n he
mis
pher
e; n
egat
ive
long
itude
= v
alue
s w
est o
f the
pri
me
mer
idia
n). S
ourc
es a
re li
sted
in n
umer
ical
ord
er a
t the
end
of t
he a
ppen
dix;
* =
pre
sent
stu
dy.
Cou
ntry
Site
loca
tion
desc
ript
ion
Lat
itude
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gitu
deH
abita
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urce
Aus
tral
iaPi
ccan
inni
e Po
nds,
Por
t Mac
Don
nell
−38
.046
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0.93
6332
° EFr
eshw
ater
25
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tria
Was
enbr
uck
(str
eam
)47
.986
840°
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.555
300°
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eshw
ater
16A
ustr
iaFi
scha
-Dag
nitz
(str
eam
)48
.025
307°
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.498
241°
EFr
eshw
ater
16A
ustr
iaH
asch
endo
rf (s
trea
m)
47.8
8657
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16.3
4425
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hwat
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tria
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e Tr
auns
ee47
.861
839°
N13
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835°
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rack
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9B
elgi
umA
ntw
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regi
on51
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8053
84° E
Bra
ckis
h17
, 27
Can
ada
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alitt
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, Dev
on I
slan
d75
.699
993°
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4.43
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° EM
arin
e30
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mar
kL
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sø55
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eshw
ater
29D
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slan
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669°
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mar
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147°
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ater
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e Fu
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8422
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onia
/ Fin
land
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f of F
inla
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altic
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3319
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ceSt
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of t
he B
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man
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e, N
. Ber
lin52
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/ Pol
and
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tern
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tic S
ea54
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ish
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, Upe
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. Gre
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72.7
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18G
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land
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alitt
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, Hol
stei
nbor
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. Gre
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66.9
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19G
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land
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k (W
. Gre
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ine
18G
reen
land
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alitt
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, Qaa
naaq
(W. G
reen
land
)77
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9.27
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° EM
arin
e30
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enla
ndSu
pral
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al, V
estr
e H
avne
naes
(E. G
reen
land
)76
.750
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N–1
8.76
6667
° EM
arin
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y C
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5.26
5194
° N–4
.023
402°
EB
rack
ish
14L
atvi
aB
altic
Sea
56.7
9727
1° N
24.9
4778
5° E
Bra
ckis
h21
, 22
Lat
via
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tern
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land
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in, B
altic
Sea
56.8
3347
6° N
20.3
3118
8° E
Bra
ckis
h15
Nor
way
Isfjo
den
78.2
2925
3° N
15.4
4253
6° E
Mar
ine
12Po
land
Wig
ry L
ake
54.0
3056
2° N
23.1
1294
2° E
Fres
hwat
er23
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sia
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aya
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lya
70.8
1896
2° N
53.6
9890
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ine
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ussi
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h Is
land
69.9
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9777
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ine
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ussi
a / K
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nN
. Cas
pian
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45.5
3422
6° N
50.2
5589
2° E
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h22
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nG
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43.5
3506
4° N
–5.6
5782
4° E
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ine
26Sw
eden
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e M
alar
en59
.514
982°
N17
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460°
EFr
eshw
ater
29Sw
eden
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e E
rken
59.8
4504
0° N
18.5
7564
6° E
Fres
hwat
er7,
10
Swed
enSt
ream
in L
unda
kvar
n59
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536°
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eshw
ater
6Sw
eden
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am in
Söd
erby
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l, R
issl
ingb
y59
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306°
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eshw
ater
6Sw
eden
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am in
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sbol
59.8
2501
8° N
18.6
1504
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hwat
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enN
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o, in
flow
str
eam
to L
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ater
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am in
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una,
Nor
rmal
ma,
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59.8
3731
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18.6
5490
3° E
Fres
hwat
er6
2013] FRESHWATER PLEUROCLADIA IN CALIFORNIA 157A
PPE
ND
IX1.
Con
tinue
d.
Cou
ntry
Site
loca
tion
desc
ript
ion
Lat
itude
Lon
gitu
deH
abita
tSo
urce
Swed
enSt
ream
in V
ende
l, K
leri
nge
60.1
4992
9° N
17.6
1261
7° E
Fres
hwat
er6
Swed
enÖ
regr
und
Arc
hipe
lago
60.3
5694
2° N
18.5
1571
5° E
Bra
ckis
h29
Swed
en / E
ston
iaN
orth
ern
Bal
tic S
ea p
rope
r58
.694
637°
N20
.522
091°
EB
rack
ish
15Sw
eden
/ Fin
land
Ala
nd S
ea, B
altic
60
.100
433°
N19
.253
617°
EB
rack
ish
15Sw
eden
/ Fin
land
Bot
hnia
n Se
a &
The
Qua
rk, B
altic
62.7
9399
7° N
19.8
8010
9° E
Bra
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h15
Turk
eyIn
fral
ittor
al B
osph
orus
, nea
r Is
tanb
ul41
.175
102°
N29
.113
328°
EB
rack
ish
1U
krai
neR
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s, C
rim
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588°
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ater
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ater
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eshw
ater
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er*
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ted
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er*
1 AYS
EL, V
., H
. ER
DU
GA
N, B
. DU
RA
L, A
ND
E.S
. OK
UD
AN
. 200
8. A
sur
-ve
y of
mar
ine
alga
e an
d se
agra
sses
of
Ista
nbul
, (Tu
rkey
). Jo
urna
lof
the
Bla
ck S
ea / M
edite
rran
ean
Env
iron
men
t 14:
129–
144.
2 BA
CK
HA
US,
D. 2
006.
Lito
rale
Auf
wuc
hsal
gen
im H
och-
und
Obe
r-rh
ein.
Car
olin
ea 6
4:5–
68.
3 BR
AU
N, A
. 185
5. A
lgar
um u
nice
llula
rium
gen
era
nova
et m
inus
cog
-ni
ta
prae
mis
sis
obse
rvat
ioni
bus
de
algi
s un
icel
lula
ribu
s in
gene
re. p
p. [1
]−11
4, 6
pla
tes.
Lei
pzig
, Ger
man
y.4 C
AR
TE
R, R
.L.,
AN
DR
.L. L
OW
E. 2
001.
Dis
trib
utio
n an
d ab
unda
nce
ofa
prev
ious
ly u
nrep
orte
d br
own
alga
, Ple
uroc
ladi
a la
cust
ris,
in th
elit
tora
l zo
ne o
f no
rthe
aste
rn L
ake
Mic
higa
n [a
bstr
act].
Pro
ceed
-in
gs o
f the
Nor
th A
mer
ican
Ben
thol
ogic
al S
ocie
ty, L
a C
ross
e, W
I.5 E
KE
NST
AM
, D
., E
.G.
BO
ZN
IAK
, A
ND
M.R
. SO
MM
ER
FE
LD
. 19
96.
Fres
hwat
er P
leur
ocla
dia
(Pha
eoph
yta)
in N
orth
Am
eric
a. J
ourn
alof
Phy
colo
gy S
uppl
emen
t 32:
15.
6 ISR
AE
LSS
ON
, G
. 19
38.
Übe
r di
e Sü
ßwas
serp
haeo
phyc
een
Schw
e-de
ns. B
otan
isk
Not
iser
193
8:11
3–12
8.7 K
AH
LE
RT,
M.,
A.T
. HA
SSE
LR
OT,
H. H
ILL
EB
RA
ND
, AN
DK
. PE
TT
ER
SON
.20
02. S
patia
l and
tem
pora
l var
iatio
n in
the
bio
mas
s an
d nu
trie
ntst
atus
of e
pilit
hic
alga
e in
Lak
e E
rken
, Sw
eden
. Fre
shw
ater
Bio
l-og
y 47
:119
1–12
15.
8 KA
NN
, E. 1
940.
Öko
logi
sche
Unt
ersu
chun
gen
an L
itora
lalg
en o
stho
l -st
eini
sche
r Se
en. A
rchi
v fü
r H
ydro
biol
ogie
37:
177–
269.
9 KA
NN
, E
. 19
78.
Syst
emat
ik u
nd Ö
kolo
gie
der
Alg
en Ö
ster
reic
h -is
cher
Ber
gbiic
he. A
rch.
Hyd
robi
ol. S
uppl
. 53:
405–
643.
10K
AN
N, E
. 199
3. D
er li
tora
le A
lgen
aufw
uchs
in S
ee E
rken
und
inse
inem
Abf
luß
(Upp
land
, Sch
wed
en).
Alg
olog
ical
Stu
dies
69:
91–1
12.
11K
IRK
BY,
S.M
., D
.J. H
IBB
ER
D, A
ND
B.A
. WH
ITT
ON
. 197
2. P
leur
ocla
dia
lacu
stri
sA
. Bra
un (P
haeo
phyt
a)—
a ne
w B
ritis
h re
cord
. Vas
culu
m57
:51–
56.
12K
JEL
LM
AN
, F.
R.
1877
. O
m S
pets
berg
ens
mar
ina,
klo
rofy
llfor
ande
Tha
lloph
yter
. II
. B
ihan
g ti
ll K
ongl
. Sv
ensk
a Ve
tens
kaps
–Aka
de -
mie
ns H
andl
inga
r 4:
51–5
2.13
KL
EB
AH
N,
H.
1895
. B
eoba
chtu
ngen
übe
r Pl
euro
clad
ia l
acus
tris
A.
Br.
Ber
icht
e de
r D
euts
chen
Bot
anis
chen
Ges
ells
chaf
t 13
:93
–106
.14
KO
NA
N-B
RO
U, A
.A.,
AN
DD
. GU
IRA
L19
94. A
vaila
ble
alga
l bi
omas
sin
tro
pica
l br
acki
sh w
ater
art
ifici
al h
abit
ats.
Aqu
acul
ture
119
:17
5–19
0.15
KO
NT
UL
A,
T.,
AN
DJ.
HA
LD
IN,
edit
ors.
201
2. H
EL
CO
M 2
012
Che
cklis
t of
Bal
tic
Sea
mac
ro-s
peci
es.
Bal
tic
Sea
Env
iron
men
tPr
ocee
d ing
s N
o. 1
30, H
elsi
nki C
omm
issi
on, H
elsi
nki,
Finl
and.
16K
USE
L-F
ET
ZM
AN
, E
.L.
1996
. N
ew r
ecor
ds o
f fr
eshw
ater
Pha
eo-
phyc
eae
from
low
er A
ustr
ia. N
ova
Hed
wig
ia 6
2:79
–89.
17PA
SCH
ER
, A.,
J. SC
HIL
LE
R, A
ND
W. M
IGU
LA. 1
925.
Die
Suß
was
ser-
Flo
ra D
euts
chla
nds,
Öst
erre
ichs
und
der
Sch
wei
z. H
eft 1
1, H
eter
o -ko
ntae
, Pha
eoph
yta,
Rho
doph
yta,
Cha
roph
yta.
G. F
isch
er, J
ena.
18R
OSE
NV
ING
E,
L.K
.18
93.
Grø
nlan
ds h
aval
ger.
Med
dele
lser
om
Grø
nlan
d 3:
763–
981,
57
figs.
+ 2
pla
tes.
19R
OSE
NV
ING
E,
L.K
. 19
10.
On
the
mar
ine
alga
e fr
om n
orth
-eas
tG
reen
land
(N. o
f 76
N. L
at.)
colle
cted
by
the
“Dan
mar
ks E
xped
i-tio
n.”
Med
dele
lser
om
Grø
nlan
d 43
:122
–123
.20
SCH
OR
IES,
D.,
U.
SEL
IG,
AN
DH
. SC
HU
BE
RT.
2009
. Sp
ecie
s an
dsy
nony
m li
st o
f the
Ger
man
mar
ine
mac
roal
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base
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