Fottea, Olomouc, 14(1): 77–90, 2014
77
New species in the genus Muelleria (Bacillariophyta) from the Maritime
Antarctic Region
Bart Van de VijVer1,2, Ralitsa ZidaroVa3 & Kateřina KopaloVá4
1
Botanic Garden Meise, Department of Bryophyta & Thallophyta, Domein van Bouchout, B–1860 Meise,
Belgium; *Corresponding author e–mail: vandevijver@br.fgov.be
2
University of Antwerp, Department of Biology, ECOBE, Universiteitsplein 1, B–2610 Wilrijk, Belgium
3
Department of Botany, Faculty of Biology, St.”Kliment Ohridski” University of Soia, 8 Dragan Tzankov Blvd.,
Soia 1164, Bulgaria
4
Department of Ecology, Faculty of Science, Charles University in Prague, Viničná 7, CZ–128 44 Prague 2,
Czech Republic
Abstract: During a survey of the freshwater aquatic and limno–terrestrial diatom lora of the Maritime
Antarctic Region, six taxa belonging to the genus Muelleria that could not be identiied were observed. Based
on detailed LM and SEM observations, these six taxa have been described as new taxa: Muelleria desseiniana
sp. nov., M. levkoviana sp. nov., M. nogae sp. nov., M. spauldingiana sp. nov., M. subsabbei sp. nov. and M.
undulatoides sp. nov. Comments are made on their taxonomic position and how they can be distinguished from
other species in this genus. Brief notes on the ecology and distribution of the six taxa are added. A compiled list
of all Muelleria taxa described worldwide is included in this paper.
Key words: Antarctic Region, morphology, Muelleria, new species, taxonomy
IntroductIon
The genus Muelleria is one of the most species rich
genera in the Antarctic Region despite its rather low
total number of described species (Spaulding et al.
1999; Van de VijVer et al. 2010). Up to now, only
29 taxa are recognized worldwide of which 16 have
a distribution restricted to the Antarctic Region.
Table 1 summarizes all collated published taxonomic
information on all Muelleria species described so
far worldwide. Together with the genera Diadesmis,
Luticola and Hantzschia, the genus is one of the
major constituents of the terrestrial (soil) diatom lora,
although populations rarely reach high abundances
(Fermani et al. 2007; KopaloVá & Van de VijVer
2013). Van de VijVer et al. (2010) elaborately discuss
the success of the genus Muelleria in the Antarctic
Region which may be due to several factors such as
their strong preference for wet or semidry terrestrial
habitats which are abundantly present in this region.
But it is also likely that a comparable diversity within
this genus could be found in the Arctic Region and the
low number of recorded taxa from the Arctic could be
the result of undersampling and/or force–itting.
Muelleria taxa are easily recognizable in light
microscope (LM) based on the presence of longitudinal
ribs bordering the axial area, typically (strongly)
delected to even hooked proximal raphe endings
and central striae that are usually more distant than
the other striae in most species. Confusion with other
taxa is only possible with certain species of the genus
Neidium but the latter is very rare in the Antarctic
Region (Hamilton et al. 2013).
The highest Muelleria diversity seems to be
concentrated on the South Orkney (SOI) and South
Shetland (SSI) Islands. Spaulding et al. (1999) and Van
de VijVer et al. (2010) described nine new taxa from
Signy Island (SOI), Deception Island (SSI) and King
George Island (SSI). During an ongoing revision of the
Antarctic diatom lora of some islands in the Maritime
Antarctic Region, several very small populations
of Muelleria taxa were found on Livingston Island
(SSI) and James Ross Island. Based on LM and SEM
analysis of their structure, six of these taxa could not
be identiied using the currently available literature and
are described here as new species. The relationship of
the new taxa in comparison with other Muelleria taxa
from the Antarctic Region and notes on their ecological
preferences are presented.
MaterIals and Methods
Epilithic, sediment and moss samples were collected from
various terrestrial and freshwater habitats in the following
islands in the southern Atlantic Ocean: Livingston Island
(South Shetland Islands) and James Ross Island (Table 1).
Samples were ixed in the ield with 3% formaldehyde. More
information on sampling methods and physico–chemical
Van de VijVer et al: New species in the genus Muelleria
78
Table 1. List of samples and their characteristics used in this paper.
Sample
Collection date Locality
GPS coordinates
Short description
JRI–S1J
22/02/2007
Komárek‘s slopes below
Berry Hill, Ulu Peninsula,
James Ross Island
(not determined)
seepage area
5–1/05
08/01/2005
Hurd Peninsula, Livingston (not determined)
Island, South Shetland
Island
wet terrestrial mosses
on the edge of a pool
BYM008
9/01/2009
Byers Peninsula, Livingston (not determined)
Island (South Shetland
Islands, large plain near
large penguin rookery
wet, terrestrial mosses
on edge of large lake
BY052
15/01/2009
Byers Peninsula, Livingston 62°38‘20.1“S
Island (South Shetland
61°06‘44.2“W
Islands, between Midge &
Limnopolar Lake
large lake with
algal mats and ine
sediment/sand on
bottom
LIV–BY16A
16/12/2006
Byers Peninsula, Livingston 62°40‘11.3“S
Island (South Shetland
61°08‘45.3“W
Islands, close to the main
plateau
bioilm in a looded
area between stones
LIV–BY16C
16/12/2006
Byers Peninsula, Livingston 62°40‘11.3“S
Island (South Shetland
61°08‘45.3“W
Islands, close to the main
plateau
bioilm in a looded
area between stones
analyses can be found in KopaloVá & Van de VijVer (2013)
and KopaloVá et al. (2013).
For light microscope (LM) observations, diatom
samples were prepared following the method described
in Van der WerFF (1955). In total, 6 sample sites and
microhabitats were examined in this study, with all samples
listed in Table 2. Subsamples of the original material were
oxidized using 37% H2O2 and heating to 80 °C for about
1 h. The reaction was further completed by the addition of
saturated KMnO4. Following digestion and centrifugation
(three times 10 min at 3700×g), the material, free of organic
matter, was further diluted with distilled water for sample
mounting to avoid excessive concentrations of diatom valves
on the slides. A subsample from the organic–free material
was mounted in Naphrax®. The slides were analyzed using
an Olympus BX51 microscope, equipped with differential
interference contrast (DIC) optics (Nomarski) and Colorview
I Soft Imaging System. Observations on Muelleria
levkoviana sp. nov. were made using brightield optics as
images in DIC produced only overexposed images. Diatom
samples and slides are stored at BR (National Botanic Garden
of Belgium). For scanning electron microscopy (SEM),
aliquots of the oxidized suspensions were iltered through 1–
μm pore size polycarbonate ilters which were cut in small
pieces, ixed on aluminum stubs after air–drying and sputter
coated (Cressington 208HR, Watford, UK) with Au (10 nm).
Observations and photomicrographs were performed with
a Zeiss® Ultra plus SEM at 8 kV at the Natural History
Museum (London, UK). The number of observations is
quite low but can be explained by the very rare occurrence
of Muelleria taxa in the different samples as was indicated
previously in Van de VijVer et al. (2010).
Identiications and species determinations are based
primarily on Spaulding & Stoermer (1997), Spaulding et
al. (1999), eSpoSito et al. (2008) and Van de VijVer et al.
(2010). Terminology follows mostly Van de VijVer et al.
(2010) except for valve outline terminology that is based on
Hendey (1964) and raphe morphology that follows round et
al. (1990).
A compiled list of all Muelleria taxa known to date
with references to their original description, type locality and
presence in Antarctica is done (Table 2).
results and dIscussIon
A total of fourteen Muelleria taxa has been found in the
samples. Eight of them had been previously described
(Spaulding et al. 1999; Van de VijVer et al. 2010): M.
aequistriata Van de VijVer et S.a.Spaulding, M. algida
S.a.Spaulding et KocioleK, M. kristinae Van de VijVer,
M. regigeorgiensis Van de VijVer et S.a.Spaulding, M.
Fottea, Olomouc, 14(1): 77–90, 2014
rostrata Van de VijVer & S.a.Spaulding, M. sabbei Van
de VijVer et S.a.Spaulding, M. tumida Van de VijVer
et S.a.Spaulding and M. variolata S.A.Spaulding et
KocioleK. Six taxa could not be identiied using the
currently available literature. All taxa were extremely
rare in the samples making observations in LM and
SEM quite dificult. Often only one (sometimes
even damaged or broken) valve could be observed
in SEM and internal views were very hard (and even
impossible) to ind. Nevertheless, a suficient amount
of observations, both in LM and SEM could be made to
justify their description as new for science: Muelleria
desseiniana sp. nov., M. levkoviana sp. nov., M. nogae
sp. nov., M. spauldingiana sp. nov., M. subsabbei sp.
79
nov. and M. undulatoides sp.nov.
Muelleria desseiniana sp. nov. (Figs 1–10)
Light microscopy (Figs 1–8): Frustules in girdle view
rectangular (Fig. 1). Valves linear with gibbous central
part and broadly rounded ends (Figs 2–8). Valve
dimensions (n=10): length 32–40 µm, valve width
8.5–10.0 µm. Axial area rather narrow, linear, slightly
widening near the small, elliptical central area. First
row of areolae along the axial area separated from the
remaining areolae by very narrow, but distinct hyaline
line. Raphe iliform, straight with clearly unilaterally
bent, long proximal raphe endings extending almost till
Figs 1–10. Muelleria desseiniana, type population from James Ross Island (sample JRI–S1J): (1–8) LM views; (9) SEM external view; (10)
SEM internal view. Scale bar 10 µm.
80
Table 2. Compiled information on the taxa belonging to the genus Muelleria.
Taxon
Basionym
Reference
Type locality
Muelleria aequistriata Van de VijVer et
S.a.Spaulding in Van de VijVer et al. 2010
–
Van de VijVer et al. 2010
Bellingshausen, King George
Island, South Shetland Islands
X
Spaulding et al. 1999
Bladder lake, Signy Island,
South Orkney Islands
X
near Fumarole Bay, Deception
Island, South Shetland Islands
X
Muelleria algida S.a.Spaulding et KocioleK –
in Spaulding et al. 1999
Antarctic Region
Muelleria australoatlantica Van de VijVer
et S.a.Spaulding in Van de VijVer et al.
2010
–
Van de VijVer et al. 2010
Muelleria bachmannii (HuStedt)
S.a.Spaulding et Stoermer 1997
Navicula bachmannii HuStedt
1961
HuStedt 1961, Spaulding & Stoermer Advent Bay,
1997, Spaulding et al. 1999
Spitsbergen
Muelleria cryonicola StaniSH et
S.A.Spaulding in Van de VijVer et al. 2010
–
Van de VijVer et al. 2010
Commonwealth Glacier, Taylor
Valley, Antarctica
X
Muelleria desseiniana sp. nov.
–
this study
Ulu Peninsula, James Ross
Island
X
Muelleria dubitanda (HuStedt et Kolbe)
S.a.Spaulding et Stoermer 1997
Navicula dubitanda HuStedt & HuStedt 1961, Spaulding & Stoermer Ale, Norrbottens, Sweden
1997, Spaulding et al. 1999
Kolbe in HuStedt 1961
Muelleria gibbula (cleVe) S.a.Spaulding et
Stoermer 1997
Navicula gibbula cleVe 1894
cleVe 1894, Spaulding & Stoermer Spitsbergen
1997, Spaulding et al. 1999
Muelleria holmenii (Foged) S.a.Spaulding
et Kociolek in Spaulding et al. 1999
Navicula holmenii Foged 1955
Foged 1955, Spaulding et al. 1999
Muelleria islandica (ØStrup) H. lange–
bertalot in lange–bertalot & genKal
1999
Navicula islandica ØStrup
1910
ØStrup 1910, lange–bertalot & Iceland
genKal 1999
Van de VijVer et al. 2010
Island,
Pearyland, Greenland
near Irizar lake, Deception
Island, South Shetland Islands
X
Van de VijVer et al: New species in the genus Muelleria
Muelleria kristinae Van de VijVer in Van de –
VijVer et al. 2010
Bear
Taxon
Basionym
Reference
Muelleria linearis (O.müller) Frenguelli
1945
Diploneis linearis O.müller
1909
müller 1909, Frenguelli
Spaulding et al. 1999
Muelleria levkoviana sp. nov.
–
this study
Muelleria lototskaya Van de VijVer in Van
de VijVer et al. 2010
–
Van de VijVer et al. 2010
Crater southwest of Corinth
Head, Heard Island
X
Muelleria luculenta S.A.Spaulding &
Stoermer 1997
–
Spaulding et al. 1999
Lake
Marie–Nicole,
Kerguelen
Iles
X
Muelleria meridionalis S.A.Spaulding &
Stoermer 1997
–
Spaulding & Stoermer 1997
Lake Hoare, Taylor valley,
Antarctica
X
Muelleria nogae sp. nov.
–
this study
Muelleria patagonica (O.muller)
Frenguelli 1945
Diploneis patagonica
O.müller 1909
müller 1909, Frenguelli
Spaulding et al. 1999
Muelleria peraustralis (W.&g.S.WeSt)
S.a.Spaulding & Stoermer 1997
Navicula peraustralis
W.&g.S.WeSt 1911
WeSt & WeSt 1911, Spaulding & Lake Deposit, Cape Royds,
Stoermer 1997, Spaulding et al. 1999, Ross Island, Antarctica
Van de VijVer et al. 2012
Muelleria portomontana (cleVe) Frenguelli Navicula portomontana cleVe
1945
1894
Muelleria regigeorgiensis Van de VijVer et
S.a.Spaulding in Van de VijVer et al. 2010
–
Muelleria relicta (mccall) reicHardt 2004 Navicula relicta mccall 1933
cleVe 1894, Frenguelli
Spaulding et al. 1999
Type locality
Antarctic Region
1945, Kark, South Patagonia
X
Fottea, Olomouc, 14(1): 77–90, 2014
Table 2 Cont.
X
1945, Lago Moor Fontana, Chubut
Province, Argentina
X
1945, Puerto Montt, Chile
Van de VijVer et al. 2010
Bellingshausen, King George
Island, South Shetland Islands
mccall 1933, reicHardt 2004
Invergowrie
House,
District, Scotland
X
Tay
Muelleria rostrata Van de VijVer et
S.a.Spaulding in Van de VijVer et al. 2010
–
Van de VijVer et al. 2010
near Crater lake, Deception
Island, South Shetland Islands
X
Muelleria sabbei Van de VijVer et
S.a.Spaulding in Van de VijVer et al. 2010
–
Van de VijVer et al. 2010
Bellingshausen, King George
Island, South Shetland Islands
X
81
82
Table 2 Cont.
Taxon
Basionym
Reference
Muelleria spauldingiana sp. nov.
–
this study
Muelleria splendidula (HuStedt & KraSSKe) Navicula splendidula HuStedt
S.a.Spaulding & Stoermer 1997
& KraSSKe in KraSSKe 1949
Type locality
Antarctic Region
X
KraSSKe 1949, Spaulding & Stoermer Lago Moor Fontana, Chubut
1997, Spaulding et al. 1999
Province, Argentina
Muelleria subsabbei sp. nov.
–
this study
Muelleria supra S.A.Spaulding et eSpoSito
in eSpoSito et al. 2008
–
eSpoSito et al. 2008
Canada Stream, Taylor valley,
Antarctica
X
Muelleria taylorii Van de VijVer et cocquyt –
in Van de VijVer et al. 2010
Van de VijVer et al. 2010
Sentinel Peak Hiking Trail,
Drakensburg,
Freestate
province, South Africa
X
Muelleria terrestris (peterSen)
S.a.Spaulding & Stoermer 1997
Navicula terrestris peterSen
1915
peterSen 1915, Spaulding & Stoermer Garden
soil,
Copenhagen
1997, Spaulding et al. 1999
Botanical garden, Denmark
Muelleria tumida Van de VijVer et
S.a.Spaulding in Van de VijVer et al. 2010
–
Van de VijVer et al. 2010
Muelleria undulatoides sp. nov.
–
this study
cHolnoKy 1955, Van
2010
Bellingshausen, King George
Island, South Shetland Islands
X
X
de
VijVer et al. Eastern Transvaal, South Africa
X
Muelleria variolata S.A.Spaulding et
KocioleK in Spaulding et al. 1999
–
Spaulding et al. 1999
Bladder lake, Signy Island,
South Orkney Islands
X
Muelleria varipunctata S.a.Spaulding et
KocioleK in Spaulding et al. 1999
–
Spaulding et al. 1999
Lake
Marie–Nicole,
Kerguelen
X
Iles
Van de VijVer et al: New species in the genus Muelleria
Diploneis vandermerwei
Muelleria vandermerwei (cHolnoKy) Van
de VijVer et cocquyt in Van de VijVer et al. Cholnoky 1955
2010
X
Fottea, Olomouc, 14(1): 77–90, 2014
83
Figs 11–22. Muelleria levkoviana, type population from Livingston Island (sample BYM008): (11–21) LM views; (22) SEM external view.
Scale bar 10 µm.
Isotypes (designated here): PLP–244 (University
of Antwerp, Belgium), BRM–ZU9/37 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Ulu Peninsula, James Ross Island,
sample JRI–S1J (Leg. J. Komárek; coll. date
22/02/2007).
Etymology: The species is named after our colleague
Dr. Steven Dessein, director of the National Botanic
Garden of Belgium in recognition of his scientiic
achievements in botany.
and even beyond the irst row of areolae. Distal raphe
endings are weakly delected to the same side of the
valve as the proximal raphe ends. Striae near the central
area (6–9 striae) more spaced than the other striae and
clearly radiate whereas other striae more distant from
the central area only slightly radiate, becoming almost
entirely parallel near the apices. Central striae 13–15
in 10 µm, distal striae 27–29 in 10 µm. Areolae hardly
discernible in LM.
Scanning electron microscopy (Figs 9–10): Striae
composed of usually transapically elongated, short,
slitlike areolae. First row of areolae bordering the axial
area however appearing as short wavy slits, separated
from the rest of the striae by a narrow hyaline area
and gradually becoming longer towards the apices
(Fig. 9). Near the distal raphe ends, one or two large,
rounded canal punctae present. Proximal raphe endings
unilaterally bent, long, extending into the irst row of
areolae. Distal raphe endings delected onto the valve
mantle, not bifurcated (Fig. 9). Internally, clear but short
rectelevatum present between proximal raphe endings.
Longitudinal canals forming narrow ribs running from
central area towards the apices, clearly perforated on
both sides by irst row of areolae (Fig. 10). Distal raphe
endings terminating on short helictoglossae (Fig. 10).
Ecology and distribution: So far the species was
only observed in very small numbers in samples
obtained from Livingston Island (SSI) and James
Ross Island. The largest population was found in one
sample, collected from a seepage area near Berry Hill
on Ulu Peninsula on James Ross Island. The sample
was dominated by several Luticola and Hantzschia
species clearly indicating its aerophilic nature. Due to
confusion with other similar taxa such as M. luculenta
(as it was earlier reported in Zidarova 2008, Pl. III, ig.
26) or the larger and coarser M. algida, its geographic
distribution is still unclear but it is not excluded that
the new species is more widespread on the Maritime
Antarctic islands.
Holotype (designated here): BR–4350 (National
Botanic Garden, Meise, Belgium)
Taxonomical remarks: Muelleria desseiniana has
a unique combination of features that separates it
84
Van de VijVer et al: New species in the genus Muelleria
Figs 23–30. Muelleria nogae, type population from Livingston Island (sample LIV–BY16A): (23–29) LM views; (30) SEM external view.
Scale bar 10 µm.
well from all other known Muelleria taxa. The raphe
is not bifurcated in its distal part, a feature rarely
seen within the genus Muelleria. Muelleria sabbei
shows comparable, though shorter, raphe endings but
has a clearly elliptic–lanceolate valve outline with
broad, convex margins (Van de VijVer et al. 2010).
Additionally, the areolae bordering the central area
are small and rounded whereas in M. desseiniana, the
areolae form long wavy slits. Muelleria varipunctata
S.a.Spaulding et KocioleK shows a similar valve
outline but has a much coarser striation pattern,
large round areolae near the axial area and different
(=bifurcating) distal raphe endings. Muelleria
lototskayae Van de VijVer, M. luculenta and M.
algida are larger with longer valves and a different
raphe course, usually showing a terminal bifurcation
(Spaulding et al. 1999; Van de VijVer et al. 2010). All
three taxa have small, rounded to short slitlike areolae,
never showing the elongated, wavy areolae typical for
M. desseiniana.
Muelleria levkoviana sp. nov. (Figs 11–22)
Light microscopy (Figs 11–21): Frustules in girdle
view rectangular (Fig. 11). Valves linear with
clearly undulating margins, a gibbous central part
and cuneately rounded ends (Figs 12–21). Valve
dimensions (n=15): length 24–38 µm, valve width
Fottea, Olomouc, 14(1): 77–90, 2014
85
Figs 31–40. Muelleria spauldingiana, images from various population from Livingston Island: (31, 32, 36) are from the type population
(sample BY052); (31–38) LM views; (39) SEM external view of an entire (broken) valve; (40) SEM external detail of the valve apex in girdle
view showing distal raphe issures, mantle areolae and canal puncta. Scale bar 10 µm except for igure 1 where scale bar = 1 µm.
6.0–7.8 µm. Axial area rather narrow, linear, widening
near the small central area. First row of areolae not
separated from the rest of the striae. Raphe iliform,
straight with clearly unilaterally bent, long proximal
raphe endings extending almost till and even beyond
the irst row of areolae. Distal raphe endings not well
visible in LM, apparently delected. Striae near the
central area (5–7 striae) only slightly more spaced than
the other striae and clearly radiate whereas other striae
more distant from the central area only slightly radiate,
gradually becoming parallel near the apices. Central
striae 16–18 in 10 µm, distal striae 20–22 in 10 µm.
Areolae moderately discernible in LM.
Scanning electron microscopy (Fig. 22): Striae
composed of two types of areolae: near the axial
area usually 1–3 rows of apically elongated areolae,
gradually becoming transapically elongated. Central
striae composed of only transapically elongated
areolae. Proximal raphe endings clearly bent, almost
reaching each other at the end, extending till the irst
86
Van de VijVer et al: New species in the genus Muelleria
Figs 41–51. Muelleria subsabbei, type population from Livingston Island (sample LIV–BY16C): (41–50) LM views; (51) SEM external view.
Scale bar 10 µm.
Figs 52–61. Muelleria undulatoides, type population from Livingston Island (sample 5–1/05): (52–60) LM views; (61) SEM external view.
Scale bar 10 µm.
row of areolae. Distal raphe endings delected, clearly
bifurcating due to siliceous lap. Canal puncta not
observed. No observations of the valve interior could
be made due to the rarity of the taxon.
Holotype (designated here): BR–4351 (National
Botanic Garden, Meise, Belgium)
Isotypes (designated here): PLP–245 (University
of Antwerp, Belgium), BRM–ZU9/38 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Byers Peninsula, Livingston Island,
South Shetland Islands, sample BYM008 (Leg. B. Van
de Vijver; coll. date 09/01/2009).
Etymology: The species is named after our colleague
Fottea, Olomouc, 14(1): 77–90, 2014
Dr. Zlatko Levkov (University of Skopje, Macedonia)
in recognition of his important contributions in diatom
research.
Ecology and distribution: Muelleria levkoviana
was only found so far in small numbers in one moss
sample on Byers Peninsula (Livingston Island). The
mosses were sampled near the shore of a very large
lake close to a large penguin rookery. Remains of
penguins, such as feathers and partly decomposed
body parts, were visible in and around the lake.
The sample was dominated by Chamaepinnularia
australomediocris (lange–bertalot et ScHmidt) Van
de VijVer and various Psammothidium taxa such as P.
papilio (Kellogg et al.) KopaloVá et Van de VijVer,
P. germainii (manguin) Sabbe and P. incognitum
(KraSSKe) Van de VijVer et beyenS.
Taxonomical remarks: Despite the single SEM
observation of the M. levkoviana so far, it is
possible to justify its separation from all other
Muelleria taxa known so far. Similar taxa include M.
terrestris (peterSen) S.a.Spaulding et Stoermer, M.
meridionalis S.a.Spaulding et Stoermer, M. supra
S.A.Spaulding et eSpoSito, M. australoatlantica and
M. relicta (mccall) reicHardt. Muelleria relicta
is probably the most similar species based on the
structure of the central striae which are only weakly
more distant in comparison with the rest of the striae.
A similar pattern is found in M. levkoviana. Both taxa
have a comparable raphe structure but differ in the
valve outline with M. relicta having less undulating
valve margins and more broadly rounded apices
(mccall 1933; reicHardt 2004). Moreover, based on
the illustration in reicHardt (2004, plate 4, ig. 7) it is
obvious that the irst row of areolae is separated from
the rest of the striae contrary to M. levkoviana. It is
however unfortunate that no SEM illustrations exist of
M. relicta to allow comparison of the areola shape and
the structure and the presence of canal puncta, absent
in M. levkoviana. Muelleria supra has more undulating
valve margins, a larger central valve part, more distantly
spaced central striae and typically large canal puncta
(eSpoSito et al. 2008). Muelleria terrestris is smaller
with parallel valve margins while M. meridionalis has
non–bifurcating distal raphe endings and two large
canal puncta. Moreover, the areolae are large and
rounded and never present the typical direction shift
as is typical for M. levkoviana (Spaulding et al. 1999).
Finally, M. australoatlantica has larger central striae,
longer proximal raphe endings and a high number of
canal puncta and non–bifurcating raphe endings (Van
de VijVer et al. 2010).
Muelleria nogae sp. nov. (Figs 23–30)
Light microscopy (Figs 23–29): Larger valves linear
with a clearly widened, gibbous central part and
87
broadly rounded apices (Figs 23–24). Smaller valves
more elliptic–lanceolate with almost convex, less
gibbous margins and broadly rounded ends (Figs 25–
29). Valve dimensions (n=10): length 24–50 µm, valve
width 10.0–14.0 µm. Axial area rather broad, linear
throughout most of its length, clearly widening to form
a large, elliptic central area. First row of areolae not
markedly separated from the rest of the striae. Raphe
iliform, straight with clearly unilaterally bent to even
hooked, long proximal raphe, completing their course
entirely within the large central area, even within
the smallest specimens. Distal raphe endings clearly
delected. Striae near the central area almost not more
spaced than the other striae and clearly radiate whereas
the other striae more distant from the central area only
slightly radiate, gradually becoming parallel near the
apices, 18–20 in 10 µm. Areolae clearly discernible in
LM, ca. 15–20 in 10 µm.
Scanning electron microscopy (Fig. 30): Striae
composed of large, rounded to transapically elongated,
oval areolae. The smallest areolae present near the
central area. Proximal raphe endings sometimes
asymmetrically bent with one hooked and one simply
bent. Distal raphe endings delected, bifurcated due to
the presence of a large siliceous lap. Presence of canal
puncta unclear due to possible confusion with normal
areolae.
Holotype (designated here): BR–4352 (National
Botanic Garden, Meise, Belgium)
Isotypes (designated here): PLP–246 (University
of Antwerp, Belgium), BRM–ZU9/39 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Byers Peninsula, Livingston Island,
South Shetland Islands, sample LIV–BY16A (Leg. M.
Toro; coll. date 16/12/2006).
Etymology: The species is named after Dr. Teresa
Noga (Institute of Botany, Krakow, Poland) who found
the species also on King George Island.
Ecology and distribution: Muelleria nogae is a rare
species found so far only on Livingston Island and on
King George Island (tereSa noga, pers. comm.). The
largest population was found in sample LIV–BY16A,
taken from a bioilm in an area looded by fresh water
between stones on Byers Peninsula close to the main
plateau. The sample is dominated by various taxa of
Luticola, Hantzschia, Pinnularia and Diadesmis.
Taxonomic remarks: Muelleria nogae can hardly be
confused with any other Muelleria species known so
far, based on the unique, large central area. Muelleria
bachmannii (HuStedt) S.a.Spaulding et Stoermer
shows a somewhat similar valve outline with a
somewhat enlarged central area but the latter area
never reaches the same size and shape as in M. nogae
(Spaulding et al. 1999, Fig. 67). Other Muelleria taxa
with a comparable gibbous valve center such as the
88
more narrow M. meridionalis differ suficiently not to
be mistaken for M. nogae.
Muelleria spauldingiana sp. nov. (Figs 31–40)
Light microscopy (Figs 31–38): Valves linear–
lanceolate with convex margins and clearly capitate,
broadly rounded apices. Valve dimensions (n=8):
length 38–50 µm, width 8.5–9.5 µm. Axial area rather
narrow, linear, only very slightly widening towards
the very small central area. First row of areolae
bordering the axial area separated from the striae by
a narrow hyaline line. Raphe iliform and straight.
Proximal raphe endings unilaterally bent, relatively
long, terminating before the irst row of areolae, never
extending into the irst row. Distal raphe endings
delected to the same side as the proximal endings.
Striae near the central area (4–5 striae) more spaced
than the other striae and clearly radiate whereas other
striae more distant from the central area only slightly
radiate, gradually becoming parallel and even weakly
convergent near the apices. Central striae 13–15 in 10
µm, distal striae 19–21 in 10 µm. Striae rather coarse,
areolae discernible in LM, 18–20 in 10 µm.
Scanning electron microscopy (Figs 39–40):
Striae composed of irregularly (c– and e–) shaped
areolae throughout the entire valve. Largest and most
complex areolae present near the axial area, gradually
becoming smaller and more rounded towards the valve
margins (Fig. 39). Areolae on mantle showing similar
irregular shape (Fig. 40). Proximal raphe endings bent,
terminating before the irst row of areolae. Distal raphe
endings bifurcating due to a large siliceous lap. One
large canal punctum present near distal raphe endings
(Fig. 40). Due to the rarity of this taxon, no observations
of the valve interior could be made.
Holotype (designated here): BR–4353 (National
Botanic Garden, Meise, Belgium)
Isotypes (designated here): PLP–247 (University
of Antwerp, Belgium), BRM–ZU9/40 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Byers Peninsula, Livingston Island,
South Shetland Islands, sample BY052 (Leg. B. Van
de Vijver; coll. date 15/01/2009).
Etymology: The species is named after our colleague
Dr. Sarah A. Spaulding (INSTAAR, Boulder, Colorado,
USA) in recognition of her contributions to Antarctic
diatom research in general and the genus Muelleria
more speciically.
Ecology and distribution: Muelleria spauldingiana
is a very rare species, occasionally observed in very
low numbers in some lakes of Livingston Island (South
Shetland Islands). The largest population was found in
a large lake between Midge and Limnopolar Lake on
the central plateau of Byers Peninsula (although only
a few valves were found). The lake is characterized
by a slightly alkaline pH (7.35) and low speciic
Van de VijVer et al: New species in the genus Muelleria
conductance values (< 100 µS.cm–1).
Taxonomic remarks: There are hardly any Muelleria
species that show a similar valve outline as present in
M. spauldingiana. The most similar taxon seems to
be M. peraustralis (W. et g.S.WeSt) S.a.Spaulding
et Stoermer, described in 1911 from the Antarctic
Continent (WeSt & WeSt 1911, Spaulding & Stoermer
1997; Van de VijVer et al. 2012). Both species can
however be separated based on the shape of the areolae,
being slit–like in M. peraustralis but very irregular,
even e–shaped in M. spauldingiana. Moreover, M.
spauldingiana has more capitate apices compared to
the subcapitate apices in M. peraustralis. Muelleria
bachmannii also shows a comparable valve outline
but has very small, rounded areolae (Van de VijVer,
pers. obs.). Muelleria meridionalis is smaller with less
elongated valves, non–bifurcating distal raphe endings
and small, slit–like areolae. All other Muelleria
species lack the typical capitate apices, coarse striation
pattern and irregularly shaped areolae, justifying the
description of M. spauldingiana as a new species.
Muelleria subsabbei sp. nov. (Figs 41–51)
Light microscopy (Figs 41–50): Valves strictly
lanceolate with non–protracted, broadly rounded,
apices. Valve dimensions (n=20): length 18–27 µm,
width 5.5–6.9 µm. Axial area moderately broad, linear,
widening to form a small, elliptic central area. First
row of areolae bordering the axial area separated from
the striae by a narrow hyaline line. Raphe iliform and
straight. Proximal raphe endings short, unilaterally
bent, terminating before the irst row of areolae. Distal
raphe endings delected to the same side as the proximal
endings. Striae near the central area (4–5 striae) more
spaced than the other striae and clearly radiate whereas
other striae more distant from the central area only
slightly radiate, gradually becoming parallel and even
weakly convergent near the apices. Central striae ca.
18 in 10 µm, distal striae 26–28 in 10 µm. Striae rather
coarse, areolae usually but not always discernible in
LM.
Scanning electron microscopy (Fig. 51): Striae
composed of very ine, transapically elongated slit–like
areolae throughout the entire valve. Areolae bordering
the axial area sometimes irregularly shaped, separated
by hyaline zone from the rest of the striae. Proximal
raphe endings bent, terminating before the irst row of
areolae. Distal raphe endings not bifurcating, strongly
hooked onto the valve face extending into the irst row
of areolae, never continuing onto the mantle. One large
canal punctum present near distal raphe endings. Due
to the rarity of this taxon, no observations of the valve
interior could be made.
Holotype (designated here): BR–4354 (National
Botanic Garden, Meise, Belgium)
Fottea, Olomouc, 14(1): 77–90, 2014
Isotypes (designated here): PLP–248 (University
of Antwerp, Belgium), BRM–ZU9/41 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Byers Peninsula, Livingston Island,
South Shetland Islands, sample LIV–BY16C (Leg. M.
Toro; coll. date 16/12/2006).
Etymology: The speciic epithet refers to the
resemblance to Muelleria sabbei Van de VijVer et
S.a.Spaulding but showing lower valve dimensions.
Ecology and distribution: Muelleria subsabbei is
a rare species found so far only in two samples on
Livingston Island. The largest population was found
in sample LIV–BY16C, taken between stones from
a bioilm in a seepage area looded by fresh water on
Byers Peninsula close to the main plateau. The sample
is dominated by various taxa of Luticola, Hantzschia,
Pinnularia and Diadesmis.
Taxonomic remarks: Muelleria subsabbei is up to
now the smallest Muelleria species observed. Other
small Muelleria species such as M. kristinae Van de
VijVer show a different pattern of the central striae
(lacking any differentiation with the rest of the striae,
different distal raphe endings (never continuing onto
the valve face) and different valve outlines (linear–
lanceolate with acutely rounded ends compared to the
strictly lanceolate valves with broadly rounded ends in
M. subsabbei) (Van de VijVer et al. 2010). Muelleria
terrestris (peterSen) S.a.Spaulding et Stoermer
has more linear valves with longer proximal raphe
endings. Unfortunately, SEM images for the latter
species are lacking making a comparison on the distal
raphe endings and the shape of the areolae impossible.
Muelleria sabbei is much larger with clearly convex,
rounded margins but shows comparable distal raphe
endings terminating on the valve face, hence the
nomenclatural connection between both species.
Muelleria undulatoides sp. nov. (Figs 52–61)
Light microscopy (Figs 52–60): Valves strictly linear
with parallel but clearly undulated margins and almost
non–protracted to weakly subcapitate (never rostrate),
broadly rounded apices. Valve dimensions (n=10):
length 23–29 µm, width 6.0–7.5 µm. Axial area narrow,
linear, slightly widening forming a small, elliptic
central area. First row of areolae bordering the axial
area usually not separated from the striae by a narrow
hyaline line, although valves with larger areolae near
the axial area were observed. Raphe iliform, straight.
Proximal raphe endings short, unilaterally bent,
terminating before the irst row of areolae. Distal raphe
endings delected to the same side as the proximal
endings. Striae near the central area (6–8 striae) very
slightly more spaced than the other striae and clearly
radiate whereas other striae more distant from the
central area only slightly radiate, parallel in the lower
89
1/3 of the valve and even weakly convergent near the
apices. Central striae 18–20 in 10 µm, distal striae
23–26 in 10 µm. Striae rather coarse, areolae usually
discernible in LM.
Scanning electron microscopy (Fig. 61): Only one
eroded valve observed. Striae composed of small,
rounded areolae. Areolae of the central striae smaller.
Presence of canal puncta unclear. Proximal raphe
endings clearly delected, terminating before the irst
row of areolae. Distal raphe endings not bifurcating,
continuing onto the valve mantle.
Holotype (designated here): BR–4355 (National
Botanic Garden, Meise, Belgium)
Isotypes (designated here): PLP–249 (University
of Antwerp, Belgium), BRM–ZU9/42 (Hustedt
Collection, Bremerhaven, Germany)
Type locality: Hurd Peninsula, Livingston Island,
sample 5–1/05 (Leg. R. Zidarova; coll. date
08/01/2005).
Etymology: The speciic epithet refers to the undulated
valve outline of the valves. It was deliberately chosen
not to use the epithet ‘undulata’ to avoid confusion
with Navicula gibbula var. undulata KraSSKe.
Ecology and distribution: So far the species has only
been found in very low numbers in between mosses
covered with thin cyanobacterial mats, collected on the
shore of a small pool on Hurd Peninsula, Livingston
Island, South Shetland Islands.
Taxonomic remarks: Actually, there is only a handful
of Muelleria species showing an undulated valve
outline. Kolbe (1959) discusses the morphology of
Navicula lagerstedtii cleVe but shows valves that
represented a different taxon, later described as N.
dubitanda. Therefore, several years later, HuStedt &
Kolbe described in 1961 Navicula dubitanda (in 1997
later transferred to Muelleria by Spaulding et Stoermer)
but the illustrated valves show a species which is much
bigger (up to 52 µm) with very narrow apices contrary
to M. undulatoides that is smaller and has broadly
rounded apices (HuStedt 1961). Navicula gibbula var.
undulata, described in 1938 from Iceland, has a similar
valve outline with undulated margins (KraSSKe 1938).
Only 2 specimens could be identiied from this species
(lange–bertalot et al. 1996, plate 17, igs. 25, 25).
Based on the illustrations, the latter taxon apparently
has a iner striation pattern, compared to the coarse
striae in M. undulatoides. Moreover, the overall valve
shape appears more slender and less compacted as is
the case in M. undulatoides. Therefore, we exclude
conspeciicity between both taxa despite the lack of a
detailed SEM analysis between both taxa. Muelleria
holmenii (Foged) S.a.Spaulding et Stoermer,
described from Peary Land, Greenland (Foged 1955),
is also only known from a few specimens (Spaulding et
al. 1999). Based on the illustrated valves in Spaulding
90
et al. (1999, igs 4, 5), the latter can be separated
from M. undulatoides by the narrower rostrate apices,
compared to the more subcapitate, broadly rounded
apices in the new species. Other taxa showing a similar
valve outline are up to now not known. Taxa such as
M. supra or M. meridionalis are suficiently different
based on their gibbous central part and the differences
in the raphe structure to avoid all confusion (Spaulding
et al. 1999; eSpoSito et al. 2008).
acknowledgeMents
Samples on Byers Peninsula (Livingston Island) were taken in
the framework of the IPY–Limnopolar Project POL2006–06635
(Ministerio de Ciencia y Tecnología, Spain). Samples on Hurd
Peninsula (Livingston Island) were taken with the logistic support
of the Bulgarian Antarctic Institute. The authors would also like
to thank the members of expeditions to the Czech J.G. Mendel
Antarctic Station for their support and help in the ield. This study
has been supported as a long–term research development project
no. RVO 67985939. Mrs. K. Kopalová beneitted from an Erasmus
grant during her stay in Belgium and GA UK grant nr. 394211. Part
of the research was funded within the BELSPO CCAMBIO project
(Belgium) and by L’Oréal–Unesco For Women in Science Program
(Bulgaria).
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© Czech Phycological Society (2014)
Received November 11, 2013
Accepted December 13, 2013