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1 UMR INRA-Université de Bourgogne, Microbiologie
du Sol et de l'Environment, BP 86510, 21065 Dijon Cedex, France
2 Instituto de Recursos Naturales y Agrobiologia, CSIC,
Apartado 1052, 41080 Sevilla, Spain
3 Institute of Soil Biology, Na Sádkách
7, 37005
eské Bud
jovice, Czech Republic
Correspondence
C. Saiz-Jimenez
saiz{at}irnase.csic.es
| ABSTRACT |
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| Introduction |
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The Cave of Lascaux was discovered in 1940. The importance of its paintings
was recognized shortly after their discovery and they are now considered one
of the finest examples of rock art paintings (Fig. 1
). As soon as it was open to the public
the cave attracted a large audience, which amounted to 1800 every day in the
1960s (Sire, 2006
).
This seriously disturbed the microclimate and had a strong impact on the cave
ecosystem.
|
Sire (2006)
, in
an historical report on Lascaux Cave management, stated that the treatments
for defeating la maladie verte in 1963 included a combined spray
application of streptomycin and penicillin for bacteria and a subsequent treatment
with formaldehyde for algae. These applications were effective until 1969
when it was necessary to start again and a programme of periodic maintenance
and cleaning was adopted.
In July 2001 the first evidence appeared of an outbreak of the fungus Fusarium solani, and its associated bacterium Pseudomonas fluorescens (Allemand, 2003
; Orial & Mertz, 2006
), which can
be considered the second major microbial crisis. This growth appeared in the
form of long white mycelia, with a fluffy appearance. The rapid extension
of the outbreak promoted an intensive treatment in September 2001 based on
benzalkonium chloride solutions (Vitalub QC 50) plus streptomycin
and polymyxin. The sediments were treated with quicklime (Sire, 2006
). In 2004 benzalkonium
chloride treatments were replaced by mechanical cleaning, air extraction and
recovery of cleaning debris. However, in 2006, the dispersion of black stains
on the ceiling and passage banks became apparent. This constituted the third
major microbial crisis (Fig. 2
),
although some of these stains were already present in 2003 (Geneste, 2008
). Dematiaceous hyphomycetes,
producing olivaceous to black colonies, and species of the genera Verticillium and Scolecobasidium were isolated from the stains (Bastian & Alabouvette, 2009
). Mechanical
cleaning as well as new biocide treatments have been used since January 2008.
|
| Cave ecology |
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|
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| Fungal outbreaks |
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Fusarium solani is considered a natural cave mycobiont. We found
this fungus in different Spanish caves (unpublished data) and in
cave sediments from Slovakia (Nováková,
2009
), and other authors have reported its presence in caves
from the UK (Mason-Williams & Holland,
1967
), the USA (Cunningham et al., 1995
) and India (Koilraj et al., 1999
).
Dupont et al. (2007)
found, in addition, representatives of six fungal genera in the
cave: Chrysosporium, Gliocladium, Gliomastix, Paecilomyces, Trichoderma and Verticillium. However,
no species identification was provided. The data reported by these authors
suggest a strong correlation between cave fungi and arthropods because these
fungal genera contain many entomopathogenic species (Samson et al., 1988
). Species of Chrysosporium, Gliocladium, Paecilomyces and Verticillium have been isolated from larval and adult cadavers of cave crickets (Gunde-Cimerman et al., 1998
),
and an association between fungi and insects in caves was recently reported (Kubátová & Dvorák, 2005
; Jurado et al., 2008
).
| Molecular microbiology |
|---|
|
|
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|
|
Although unfortunately no report on the bacteria present in Lascaux Cave
before benzalkonium chloride treatments is available, and therefore the composition
of pristine microbial communities is unknown, the data suggest that years
of benzalkonium chloride treatments in Lascaux Cave might have selected a
population of Ralstonia and Pseudomonas highly resistant
to the biocide (Bastian et al.,
2009c
).
The study of the fungal population (607 clones) revealed that
the 10 most abundant phylotypes represented 59.2 % of the total
clones (Bastian et al., 2009b
). Only two of these 10 phylotypes can be labelled as soil
fungi, while the rest can be classified as entomophilous fungi, including
the well-known entomopathogen Isaria farinosa (Table 2
) (Bastian et al., 2009b
). Only seven clones of Fusarium solani were found in the samples, which suggests that after
prolonged biocide treatment the F. solani population decreased drastically,
but in turn, this was replaced by an abundant population of entomophilous
and other fungi.
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| The black stains |
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Previous reports on Scolecobasidium species indicated that they
constitute a very small proportion of the fungal biota in natural habitats,
including soil and decaying leaves, and are particularly active in oil-contaminated
soils (Pinholt et al., 1979
). In addition, S. tshawytschae is a known fish
pathogen (Doty & Slater, 1946
).
We can hypothesize that the reason why S. tshawytschae appeared
in the cave is linked to the availability of carbon sources, and benzalkonium
chloride or their degradation products might be a possible carbon source.
Benzalkonium chloride, a cationic surfactant, is rapidly and strongly sorbed
onto sediments, clays and minerals. Benzalkonium chloride is transformed into
alkyl dimethylamines through a nucleophilic substitution at low temperatures (0–40 °C)
in an abiotic reaction in the presence of nitrites (Tezel & Pavlostathis, 2009
). Nitrates and
ammonium are abundant in Lascaux Cave (Lastennet et al., 2009
), and it is expected that
nitrites are as well; however, the last was not analysed. When benzalkonium
chloride is degraded by bacteria, formation of benzyldimethylamine, benzylmethylamine,
benzylamine, benzaldehyde and benzoic acid occurs (Patrauchan & Oriel, 2003
). Nobuo (2005)
found that a Scolecobasidium sp. was dominant in washing machines using synthetic detergent. Laundry
detergents typically contain cationic surfactants. It is possible that S. tshawytschae utilizes some of the benzalkonium chloride intermediates
as nitrogen and carbon sources. This is a hypothesis to be tested.
| Arthropod ecology |
|---|
|
|
|---|
|
Collembolae are largely mycophagous, and numerous Fol. candida
specimens were observed feeding on black stains (Fig. 4
). Fol. candida prefers melanized
fungal species (Scheu & Simmerling,
2004
) over hyaline fungi as food, but Fusarium hyphae (Sabatini & Innocenti, 2000
), several Pseudomonas spp., including P. fluorescens (Thimm et al., 1998
) and nematodes (Lee & Widden, 1996
), have also
been shown to be eaten.
We used the collembolan Fol. candida and the two fungi from Lascaux outbreaks (Fusarium solani and S. tshawytschae) to answer the following questions: Does Fol. candida show feeding preferences for these fungi? Can the feeding preferences be responsible for the fungal dispersion? Live specimens of Fol. candida from Gombasecka Cave in Slovakia were collected. Thirty specimens were placed in Petri dishes containing either a fresh culture of F. solani (4-day-old colonies) isolated from Domica Cave, Slovakia, or a culture of S. tshawytschae, isolated from black stains in Lascaux Cave. Both were deposited onto a cave sediment or plaster of Paris (gypsum). After 24 h, all specimens in the gypsum dishes were feeding on Fusarium or in the immediate vicinity and they were eating mycelia, while in cave sediment dishes most specimens were in the environs of Fusarium although visible signs of feeding were observed.
After 10 days, strong grazing of Fol. candida on the fungi
was observed, especially on Fusarium, where the mycelium was eaten
off and Folsomia eggs were present (Fig. 5A
). Even further more evident changes
were found after 20 days of the experiment and more than one-third
of Fusarium mycelia on both substrata (cave sediment and gypsum)
were eaten off (Fig. 5B
). Scolecobasidium was also attacked and the mycelia on gypsum were completely
eaten while on the cave sediment distinct parts were eaten off (Fig. 5C
). These results show that the two
fungal species which caused the most serious outbreaks in Lascaux Cave were
a very suitable food for Fol. candida.
|
On the other hand, Fol. candida is a vector for micro-organisms. Dromph (2003)
reported that collembolae
are vectors of entomopathogenic fungi, and Greif & Currah (2007)
isolated species of the fungal
genera Acremonium, Beauveria, Cladosporium, Cryptendoxyla, Geomyces, Gliocladium, Hormiactis, Leptographium, Oidiodendron, Penicillium
and Verticillium from collembolae.
The high density of collembolae in contact with bacterial cells, mycelial
fragments and conidia suggests that these arthropods significantly increase
the dispersal rate of bacteria (Scheu &
Simmerling, 2004
) and fungi (Thimm et al., 1998
) by carrying conidia on their
bodies. In addition, the gut of Fol. candida is a selective habitat
and a vector for micro-organisms (Thimm et al., 1998
).
The Fol. candida population in Lascaux Cave is related to its
feeding preferences, which explains the presence of this collembola species
after the first fungal outbreak. Fungi produce volatile compounds that are
potentially attractive to collembolae (Bengtsson et al., 1988
). At present, grazing on
the black stains might be a consequence of the presence of melanized fungi
and, particularly, of S. tshawytschae in the last 2 years.
This fungus is probably disseminated through the cave by the collembolae and
their faecal pellets, thus contributing to the appearance of black stains.
Interestingly, unidentified members of the family Campodeidae (Diplura)
were also observed feeding on the black stains. Most diplurae are predators
and their diet includes collembolae and mites (Lock et al., 2009
). They may also survive
on vegetable debris and fungal mycelia. Indeed melanized fungi are also the
most palatable fungi for mites (Schneider &
Maraun, 2005
). A detailed survey on different classes of
arthropods should be carried out to confirm the presence of other cavernicole
populations in the cave.
| Conclusions and perspectives |
|---|
|
|
|---|
The composition of the fungal community is largely influenced by the colonization and activity of arthropods, with collembolae considered to be of primary significance. Other arthropods, such as coleoptera, could play a role in fungal community structure; however, further studies are needed to verify this and to determine the degree of association of some of the fungal species identified in the cave with coleoptera.
The appearance of black stains in Lascaux Cave might be related to the presence of S. tshawytschae, probably promoted by biocide applications, and the grazing effects of the cavernicole population. How can we explain the fast development of black stains in the last 2 years, if not by the presence of abundant organic matter in the cave and the imbalance produced by antifungal treatments, which were revealed not to be fully effective? Are the black stains due to the production of melanin by S. tshawytschae? What are the carbon sources for this fungus? The utilization of benzalkonium chloride as a probable carbon and nitrogen source for cave micro-organisms has to be assessed.
There are still many unanswered questions on the microbial ecology of this cave that research should clarify in the coming years. A careful study on the arthropods, the ecology of foreign fungi and their dispersion patterns is needed in order to complete the food web and to control the black stains.
| ACKNOWLEDGEMENTS |
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