microlunatus cavernae sp. nov., a novel actinobacterium isolated from alu ancient cave, yunnan,...
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ORIGINAL PAPER
Microlunatus cavernae sp. nov., a novel actinobacteriumisolated from Alu ancient cave, Yunnan, south-west China
Juan Cheng • Wei Chen • Bing Huo-Zhang •
Salam Nimaichand • En-Min Zhou •
Xin-Hua Lu • Hans-Peter Klenk • Wen-Jun Li
Received: 20 February 2013 / Accepted: 29 April 2013 / Published online: 8 May 2013
� Springer Science+Business Media Dordrecht 2013
Abstract A Gram-positive, coccoid, non-endo-
spore-forming actinobacterium, designated YIM
C01117T, was isolated from a soil sample collected
from Alu ancient cave, Yunnan province, south-west
China. Based on the 16S rRNA gene sequence analysis,
strain YIM C01117T was shown to belong to the genus
Microlunatus, with highest sequence similarity of
97.4 % to Microlunatus soli DSM 21800T. The whole
genomic DNA relatedness as shown by the DNA–
DNA hybridization study between YIM C01117T and
M. soli DSM 21800T had a low value (47 ± 2 %).
Strain YIM C01117T was determined to contain LL-
diaminopimelic acid with Gly, Glu and Ala amino
acids (A3c0 type) in the cell wall. Whole-cell hydrol-
ysates were found to contain glucose, galactose,
mannose and ribose. The major polar lipids were
determined to be phosphatidylglycerol and diphos-
phatidylglycerol. The predominant menaquinone sys-
tem present is MK-9(H4), while the major fatty acids
were identified to be anteiso-C15:0 (24.1 %), iso-C16:0
(22.3 %) and iso-C15:0 (11.4 %). The G?C content of
the genomic DNA was determined to be 65.9 mol%.
The chemotaxonomic and genotypic data support the
affiliation of the strain YIM C01117T to the genus
Microlunatus. The results of physiological and bio-
chemical tests allow strain YIM C01117T to be
Juan Cheng and Wei Chen contributed equally to this work.
Electronic supplementary material The online version ofthis article (doi:10.1007/s10482-013-9929-x) containssupplementary material, which is available to authorized users.
J. Cheng � B. Huo-Zhang � S. Nimaichand �E.-M. Zhou � W.-J. Li (&)
Key Laboratory of Microbial Diversity in Southwest
China, Ministry of Education, and Laboratory for
Conservation and Utilization of Bio-resources, Yunnan
Institute of Microbiology, Yunnan University, Kunming
650091, People’s Republic of China
e-mail: [email protected]; [email protected]
W. Chen
Hongyun Honghe Tobacco (Group) Co., Ltd, Kunming
650202, People’s Republic of China
S. Nimaichand
Microbial Biotechnology Research Laboratory,
Department of Biochemistry, Manipur University,
Canchipur, Imphal 795003, Manipur, India
X.-H. Lu
The National Engineering Center for Research of Microbial
Pharmaceuticals and New Drug Research and Development
Center, North China Pharmaceutical Group Corporation,
Shijiazhuang 050015, People’s Republic of China
H.-P. Klenk
Leibniz Institute—DSMZ, German Collection of
Microorganisms and Cell Cultures, Inhoffenstrasse 7B,
38124 Braunschweig, Germany
W.-J. Li
Key Laboratory of Biogeography and Bioresource in Arid
Land, Xinjiang Institute of Ecology and Geography,
Chinese Academy of Sciences, Urumqi 830011, People’s
Republic of China
123
Antonie van Leeuwenhoek (2013) 104:95–101
DOI 10.1007/s10482-013-9929-x
differentiated phenotypically from recognized Micro-
lunatus species. Strain YIM C01117T is therefore
considered to represent a novel species of the genus
Microlunatus, for which the name Microlunatus
cavernae sp. nov. is proposed. The type strain is YIM
C01117T (= DSM 26248T = JCM 18536T).
Keywords Microlunatus cavernae sp. nov.
16S rRNA gene � Polyphasic taxonomy
Alu ancient cave
Introduction
The genus Microlunatus was established by Nakamura
et al. (1995). At the time of writing, the genus contained
six validly named species isolated from different
habitats: Microlunatus phosphovorus (Nakamura et al.
1995) from activated sludge, Microlunatus ginsengisoli
(Cui et al. 2007) and Microlunatus panaciterrae (An
et al. 2008) from soil of a ginseng field, Microlunatus
aurantiacus (Wang et al. 2008) from a rhizosphere soil,
Microlunatus soli (Kampfer et al. 2010a) from a spawn
used for growing edible mushrooms in the laboratory
and Microlunatus parietis (Kampfer et al. 2010b) from
an indoor wall. All these species are characterized
chemotaxonomically by the presence of LL-diamino-
pimelic acid (DAP) in the cell-wall, MK-9(H4) as the
predominant menaquinone and anteiso-C15:0, iso-C15:0
and iso-C16:0 as the major fatty acids.
This paper reports the taxonomic position of a novel
strain, YIM C01117T, using a polyphasic character-
ization approach. The results suggest that strain YIM
C01117T represents a novel species of the genus
Microlunatus, for which the name Microlunatus
cavernae sp. nov. is proposed here.
Materials and methods
Strain and culture conditions
Strain YIM C01117T was isolated from a soil sample
collected from Alu ancient cave (E103�45.0000,N24�33.6730), a tourism cave located in Yunnan
province, south-west China. The soil sample after
serial dilution was spread on R2A medium (BD;
Becton, Dickinson and Company) and incubated for
2 weeks at 28 �C. Colonies were selected and
repeatedly re-streaked on the same medium to obtain
pure cultures. Strain YIM C01117T was routinely
cultivated on R2A medium at 28 �C and also stored as
glycerol suspensions (20 %, v/v) at -80 �C. Biomass
for chemical and molecular studies was obtained by
cultivation on R2A medium at 28 �C for about
1 week. The reference strains M. soli DSM 21800T,
M. parietis DSM 22083T and M. phosphovorus DSM
10555T were obtained from DSMZ and cultured under
the same conditions as strain YIM C01117T.
Phenotypic characteristics
Gram staining was carried out by using the standard
Gram reaction and was confirmed by using the KOH
lysis test method (Cerny 1978). Morphology was
examined by light microscopy (BH-2; Olympus) and
scanning electron microscopy (QUANTA200; FEI).
For scanning electron microscopy, cultured cells were
harvested by centrifugation, washed and suspended in
20 mM phosphate buffer (pH 7.0). The suspended
cells were fixed with 3 % glutaraldehyde. The cells
were dehydrated in ethanol. After critical point drying,
samples were sputter coated with gold and observed
with a scanning microscope.
Growth at different temperatures (4, 10, 15, 22, 28,
37, 39, 40, 45 and 50 �C) and NaCl tolerance
(0–12.0 % w/v) were tested on tryptose soy agar
plates by incubating the cultures for 14–21 days. The
pH range (4.0–10.0, at intervals of 1.0 pH unit) for
growth was tested in tryptose soy broth medium
(28 �C, 14–21 days) using the buffer system described
by Xu et al. (2005). Carbon source utilization was
determined by the methods described by Shirling and
Gottlieb (1966) and Locci (1989). Nitrogen source
utilization was determined according to Williams et al.
(1989). Catalase activity was detected by assessing the
production of bubbles on addition of a drop of 3 % (v/
v) H2O2. Oxidase activity was determined by the
oxidation of tetramethyl-p-phenylenediamine (Kov-
acs 1956). Hydrolysis of cellulose, gelatin, tyrosine,
starch, and Tweens 20, 40, 60 and 80, milk coagulation
and peptonization, utilization of urea, hydrogen sul-
fide production and nitrate reduction were performed
as described by Gonzalez et al. (1978). Determination
of phosphate accumulation by strain YIM C01117T
was performed as described by Nakamura et al.
(1995), with M. phosphovorus DSM 10555T as the
reference strain.
96 Antonie van Leeuwenhoek (2013) 104:95–101
123
Chemotaxonomy
The isomer of amino acids in purified cell walls and
sugars of whole cell hydrolysates were determined
according to the procedures described by Hasegawa
et al. (1983), Lechevalier and Lechevalier (1970) and
Tang et al. (2009a, b). Polar lipids were extracted as
described by Minnikin et al. (1979) and identified by
two-dimensional TLC (Collins and Jones 1980).
Menaquinones were extracted (Collins et al. 1977)
and analyzed using HPLC (Kroppenstedt 1982).
Cellular fatty acid analysis was performed by using
the Microbial Identification System (Sherlock Version
6.1; MIDI database: TSBA6; Sasser 1990). Biomass
for fatty acid analysis was obtained from cell grown on
tryptose soy agar (Difco) at 28 �C for 4 days.
Molecular analysis and DNA–DNA hybridizations
Extraction of genomic DNA and PCR amplification
of the 16S rRNA gene were performed from strain
YIM C01117T as described previously (Li et al.
2007). The sequence obtained was compared
with available 16S rRNA gene sequences of
cultured species from the EzTaxon-e server
(http://eztaxon-e.ezbiocloud.net/; Kim et al. 2012).
Multiple alignments with sequences of the most
closely related taxa and calculations of levels of
sequence similarity were carried out using CLUS-
TAL_X program (Thompson et al. 1997). Phylo-
genetic analyses were performed by using three
tree-making algorithms i.e. the neighbour-joining
(Saitou and Nei 1987), maximum-likelihood (Fel-
senstein 1981) and maximum-Parsimony (Fitch
1971) methods using the software package MEGA
version 5.0 (Tamura et al. 2011). Kimura’s two
parameter model was used to calculate evolutionary
distance matrices of the neighbour-joining method
(Kimura 1980). Bootstrap analysis was performed
with 1,000 replications (Felsenstein 1985). Aeris-
cardovia aeriphila T6T (AY174107) was used as an
outgroup.
The G?C content of the genomic DNA for strain
YIM C01117T was determined by using the HPLC
method described by Mesbah et al. (1989). DNA–
DNA relatedness was studied using the fluorometric
micro-well method (Ezaki et al. 1989; Christensen
et al. 2000; He et al. 2005). The hybridizations were
performed with eight replications.
Results and discussion
Phenotypic characteristics
Strain YIM C01117T was observed to be a Gram-
positive, coccus-shaped nonmotile, nonendospore-
forming actinobacterium. The cells measured
0.6–1.0 lm in diameter and occurred either singly
or in pairs. Small irregular clusters of cells were
also found (see Supplementary Fig. S1). Growth of
strain YIM C01117T was observed at 10–37 �C,
0–9.0 % NaCl (w/v) and pH 5.0–10.0, with optimal
growth at 22–28 �C, 0–1.0 % NaCl (w/v) and pH
7.0–8.0. The strain was determined to be positive
for catalase test and negative for oxidase, gelatin-
ase, amylase and urease activities. The strain
showed negative results for milk coagulation, milk
peptonization, nitrate reduction, hydrogen sulfide
production, and hydrolysis of tyrosine, Tweens 20,
40, 60, 80 and cellulose. The differential charac-
teristics of strain YIM C01117T and the type strains
in the genus Microlunatus are shown in Table 1
while the detailed characteristics of the strain are
given in the species description. Strain YIM
C01117T was observed to accumulate phosphate
only weakly in comparison with M. phosphovorus
DSM 10555T. As shown in Fig. 1, cells of YIM
C01117T exhibited weak phosphate-accumulating
activity after incubation for 5 h in the absence of
any carbon substrate in the medium; after 13 h, the
phosphate-accumulating activity of YIM C01117T
became more stable.
Chemotaxonomic characteristics
The peptidoglycan type of strain YIM C01117T was
determined to be A3c0 based on LL-diaminopimelic
acid with Gly, Glu and Ala amino acids in its purified
cell wall (Fig. S2). The major whole-cell sugars were
identified to be glucose, galactose, mannose and
ribose. The polar lipids were found to consist of
phosphatidylglycerol and diphosphatidylglycerol with
a few unknown/uncharacterized lipids: one glycolipid,
two phospholipids and one polar lipid (see Supple-
mentary Fig. S3). The menaquinone system of strain
YIM C01117T was determined to mainly comprise of
MK-9(H4) with a small amount of MK-8(H6). The
major fatty acids ([10 %) of strain YIM C01117T
Antonie van Leeuwenhoek (2013) 104:95–101 97
123
were identified as the saturated branched-chain fatty
acids anteiso-C15:0 (24.1 %), iso-C16:0 (22.3 %) and
iso-C15:0 (11.4 %) (Table 2). The major fatty acids
profile of strain YIM C01117T were consistent with
those of three type strains, but there were also some
differences with the latter. The G?C content of
genomic DNA was determined to be 65.9 mol%,
which is consistent with the range for the genus
Microlunatus. Thus, the chemotaxonomic data for
strain YIM C01117T are consistent with its assignment
to the genus Microlunatus.
Phylogenetic analysis and DNA–DNA relatedness
Sequence analysis of the almost complete 16S rRNA
gene sequence of strain YIM C01117T (1,480 bp;
GenBank accession no. KC693588) using the EzTax-
on-e server showed highest similarity to sequences of
strains belonging to the genus Microlunatus: M. soli
DSM 21800T (97.4 %), M. parietis DSM 22083T
(96.6 %), M. panaciterrae Gsoil 954T (95.1 %), M.
phosphovorus DSM 10555T (94.6 %), M. ginsengisoli
Gsoil 633T (94.6 %) and M. aurantiacus YIM 45721T
Table 1 Physiological characteristics of strain YIM C01117T and the type strains of the genus Microlunatus
Characteristics 1 2 3 4 5 6 7
Temperature range for growth (�C) 20–37 20–30 20–30
NaCl range (%) 0–9.0 0–9.0 0–6.0 0–7.0 7.0–7.5 5.5–8.5 5.0–9.0
pH range 5.0–10.0 6.0–10.0 5.0–10.0 5.0–9.0 0 0–5.0 0–5.0
Oxidase – ? – ? – – ?
Nitrate reduction – ? ? ? ? – –
Hydrolysis of cellulose – – – – – ? –
Gelatin – – – – ND ? ?
H2S – – – – – – –
Starch – – – – ND – ?
Tween 20 – – – – ? ND ND
Tween 60 – – – ? – ND ND
Tyrosine – – – ? ND ND ND
Urea – – – – ? – –
Utilization of sole carbon source sources
L-arabinose – ? ? – ? ? ?
Cellobiose ? ? – ? ? ? –
D-fructose – – ? ? ? ? –
Galactose ? – ? ? ? ? –
Raffinose ? ? ? ? ? ? –
L-rhamnose ? – ? ? – ? ?
Xylitol ? ? – ? ? ? –
D-xylose ? ? – ? ? ? –
Utilization of sole nitrogen source
L-histidine ? ? – ? – ? –
L-lysine ? – ? ? – – –
L-glycine ? ? ? ? ND – ND
L-methionine ? ? ? ? ND – ND
Strains: 1 YIM C01117T; 2 M. soli DSM 21800T; 3 M. parietis DSM 22083T; 4 M. phosphovorus DSM 10555T; 5 M. aurantiacusYIM 45721T (Wang et al. 2008); 6 M. ginsengisoli DSM 17942 T (Cui et al. 2007); 7 M. panaciterrae Gsoil 954 T (An et al. 2008).
All the data for strains YIM C01117T, M. soli DSM 21800T, M. parietis DSM 22083T and M. phosphovorus DSM 10555T are from
the present study
? Positive, - negative, ND not determined
98 Antonie van Leeuwenhoek (2013) 104:95–101
123
(94.4 %). The phylogenetic tree based on the neigh-
bour-joining (NJ) method showed the formation of
clade with M. soli DSM 21800T with a bootstrap
support of 62 % (Fig. 2), which indicates the affiliation
of the strain YIM C01117T to the genus Microlunatus.
Based on the sequence analysis from EzTaxon-e and the
NJ tree, the strain M. soli DSM 21800T was the closely
related phylogenetic neighbor, and thus it was selected
for DNA–DNA hybridization studies with strain YIM
C01117T. The determined DNA–DNA relatedness
value of 47 ± 2 %, which is well below the 70 %
cut-off point for the recognition of genomic species
(Wayne et al. 1987). Additionally, the differences in the
phenotypic characters of YIM C01117T from the
reference type strain M. soli DSM 21800T (including
utilization of galactose and L-lysine as sole C/N sources
but not arabinose, along with negative results in the
oxidase and nitrate reduction tests) support the place-
ment of strain YIM C01117T as representative of a
novel species within the genus Microlunatus, for which
the name M. cavernae sp. nov. is proposed.
Description of Microlunatus cavernae sp. nov.
Microlunatus cavernae (ca.ver’na.e. L. gen. n. caver-
nae, of a cave; M. L. gen. fem. n. cavernae of a cave,
referring to the habitat of the organism) Gram-positive,
coccus-shaped nonmotile, non-endospore-forming.
Cells measure 0.6–1.0 lm in diameter and occur either
singly or in pairs. Irregular clusters of cells are also
observed. Growth occurs at 10–37 �C, pH 5.0–10.0 and
in the presence of up to 9.0 % NaCl (w/v). Utilizes
cellobiose, galactose, maltose, D-mannose, raffinose,
rhamnose, sodium malate, xylitol and D-xylose as sole
carbon sources, but not L-arabinose and D-fructose.
Utilizes L-alanine, L-glycine, L-histidine, L-lysine, L-
methionine, L-phenylalanine and L-valine as sole nitro-
gen sources. Positive in the catalase test and negative in
oxidase, milk coagulation, milk peptonization, nitrate
reduction and hydrogen sulfide production tests. Does
not hydrolyze cellulose, gelatin, starch, tyrosine,
Tweens 20, 40, 60, 80 and urea. The peptidoglycan
type is A3c0 based on LL-diaminopimelic acid. The
0
50
100
150
200
250
0 5 10 15 20 25 30
Time (h)
Pho
spha
te c
once
ntra
tion
(mg
P-1
)
Fig. 1 Phosphate uptake profiles of strain YIM C01117T and
M. phosphovorus DSM 10555T under aerobic conditions. Both
strains were grown on R2A medium (removed KH2PO4 and
MgSO4�7H2O) and harvested in the late exponential phase. The
amount of phosphate was determined by the molybdenum blue
method. Filled square YIM C01117T, filled diamond M.phosphovorus DSM 10555T (reference strain)
Table 2 Fatty acid profiles ([1 %) of strains YIM C01117T,
M. soli DSM 21800T, M. parietis DSM 22083T and M. phos-phovorus DSM 10555T
Fatty acids YIM
C01117TDSM
21800TDSM
22083TDSM
10555T
C16:0 1.1 – – 1.5
C14:1x5c 2.4 1.4 2.7 –
C17:1x9c – 2.2 – –
C17:1x6c – 11.5 – –
Iso-C14:0 2.4 2.2 2.5 16.1
Iso-C15:0 11.4 7.5 30.5 13.7
Iso-C15:1 3.7 – – –
Iso-C16:0 22.3 21.2 6.0 22.7
Iso-C16:1 9.5 – – –
Iso-C17:0 3.1 – – 2.5
Anteiso-C15:0 24.1 18.0 44.3 32.9
Anteiso-C15:1 1.2 – – –
Anteiso-C17:0 8.9 2.6 1.4 1.1
C8:0 3OH 1.0 – 1.2 –
Iso-C14:0 3OH – 4.1 3.1 2.0
C14:0 2OH – 1.8 1.2 –
Summed feature 3a – – – 1.5
Summed feature 4a – – 3.0 –
Summed feature 8a – 20.6 – –
Summed feature 3 consisted of C16:1x6c and/or C16:1x7c
Summed feature 4 consisted of anteiso-C17:1 and/or iso-C17:1
Summed feature 8 consisted of C18:1x7c.and/or C18:1x6c
- Negative or absenta Summed features are groups of two or three fatty acids that
cannot be separated by GLC with the MIDI system
Antonie van Leeuwenhoek (2013) 104:95–101 99
123
major whole cell sugars are glucose, galactose, man-
nose and ribose. The polar lipids consist of phosphat-
idylglycerol, diphosphatidylglycerol, an unknown
glycolipid, two unknown phospholipids and an unchar-
acterized polar lipid. The menaquinone system com-
prises of MK-9(H4) and MK-8(H6). The fatty acid
profile includes anteiso-C15:0, iso-C16:0 and iso-C15:0 as
major components. The G?C content of the genomic
DNA of the type strain is 65.9 mol %.
The GenBank accession number for the 16S rRNA
gene sequence of strain YIM C01117T is KC693588.
The type strain YIM C01117T (= DSM 26248T =
JCM 18536T) was isolated from a soil sample
collected at Alu Ancient cave (E103�45.0000,N24�33.6730), Yunnan province, south-west China.
Acknowledgments The authors are grateful to Prof. Jean P.
Euzeby for construction of the Latin name of the new taxon.
This work was funded jointly by National New Drug Research
and Development Project (No. 2010ZX09401-403) and project
of China tobacco Yunnan industrial Co. Lid. (Nos. 2012JC07
and 2012FL02). W-J Li was also supported by ‘Hundred Talents
Program’ of the Chinese Academy of Sciences.
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Microlunatus cavernae YIM C01117T (KC693588)
Microlunatus soli DSM 21800T (FJ807672) Microlunatus parietis DSM 22083T (FN556016)
Microlunatus ginsengisoli Gsoil 633T (AB245389) Microlunatus phosphovorus DSM 10555T (AP012204)Microlunatus aurantiacus YIM 45721T (EF601828)
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99*98*
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7163*
53*
0.02
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