Factors driving epilithic algal colonization in show caves and new
insights into combating biofilm development with UV-C treatments
Fabien Borderie
a
, Nicolas Tête
a
, Didier Cailhol
c
, Laurence Alaoui-Sehmer
a
, Faisl Bousta
b
, Dominique Rieffel
a
,
Lotfi Aleya
a,
⁎, Badr Alaoui-Sossé
a
a
Laboratoire Chrono-Environnement (LCE), UMR CNRS 6249, Université de Franche-Comté, Place Leclerc, F-25030 Besançon, France
b
Laboratoire de Recherche des Monuments Historiques (LRMH), USR 3224, 29 rue de Paris, F-77420 Champs-sur-Marne, France
c
Laboratoire Environnement, Dynamique et Territoires de Montagne (EDYTEM), UMR CNRS 5204, Université de Savoie, F-73376 Le Bourget du Lac, France
HIGHLIGHTS
• Growth-influencing factors of epilithic algae in a show cave were studied.
• Not one but a combination of factors explained the presence of algae.
• Colorimetric measurements are a good diagnosis of colonization state.
• Effects of UV-C treatments were investigated on several green biofilms.
• Treated biofilms are bleached but re-colonization occurs after 16 months.
abstract article info
Article history:
Received 7 January 2014
Received in revised form 7 March 2014
Accepted 11 March 2014
Available online xxxx
Editor: C.E.W. Steinberg
Keywords:
Epilithic algae
Biofilms
Cave
Growth-influencing factors
Colorimetric measurements
UV-C treatment
The proliferation of epilithic algae that form biofilms in subterranean environments, such as show caves, is a
major problem for conservators. In an effort to reduce the use of chemical cleansers when addressing this
problem, we proposed investigating the effects of UV-C on combating algal biofilm expansion in a cave located
in northeastern France (Moidons Cave). First, the biofilms and cavity were studied in terms of their algal
growth-influencing factors to understand the dynamics of colonization in these very harsh environments.
Next, colorimetric measurements were used both to diagnose the initial colonization state and monitor the
UV-C-treated biofilms for several months after irradiation. The results indicated that passive dispersal vectors
of the viable spores and cells were the primary factors involved in the cave's algae repartition. The illumination
time during visits appeared to be responsible for greater colonization in some parts of the cave. We also showed
that colorimetric measurements could be used for the detection of both thin and thick biofilms, regardless of the
type of colonized surface. Finally, our results showed that UV-C treatment led to bleaching of the treated biofilm
due to chlorophyll degradation even one year after UV-C treatment. However, a re-colonization phenomenon
was colorimetrically and visually detected 16 months later, suggesting that the colonization dynamics had not
been fully halted.
© 2014 Elsevier B.V. All rights reserved.
1. Introduction
Caves are probably the most particular ecosystem, as they harbor life
despite their lack of sunlight and reminding us of how life on earth may
have first begun. While light-driven photosynthetic production by
plants is the key source of energy in outdoor ecosystems, chemical-
driven microbial production can support food webs in caves (Simon,
2012). However, the discovery of a given cave and its opening to the
public give irremediable rise to a combination of structural changes
that greatly affect its relatively stable microclimate (Groth et al.,
1999). The installation of a lighting system to make cave formations vis-
ible to visiting tourists may, over time, lead to the appearance of green-
ish biofilms due to the growth of prototrophs such as algae and
cyanobacteria, which are considered a major source of biodeterioration
on rock surfaces (Albertano, 2012; Cutler et al., 2013). These colonists,
or “r-selected species,” possess invasive, fast-growing and prolific prop-
agule production and are later joined by more varied, larger and more
slowly growing species, and eventually by species that, through the ex-
clusion of their competitors, achieve complete dominance over an eco-
logical climax (Aleya, 1991).
The Moidons Cave (Jura, France), discovered in 1966 and open to
tourists for 6 months a year since 1989, may constitute a plausible ex-
ample of this phenomenon. Each year, approximately 25,000 people
Science of the Total Environment 484 (2014) 43–52
⁎ Corresponding author. Tel.: +33 3 81 66 57 64; fax: +33 3 81 66 57 97.
E-mail address: lotfi.aleya@univ-fcomte.fr (L. Aleya).
http://dx.doi.org/10.1016/j.scitotenv.2014.03.043
0048-9697/© 2014 Elsevier B.V. All rights reserved.
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