ArticlePDF Available

Abstract and Figures

Cryptoendolithic microbial communities and epilithic lichens have been considered as appropriate candidates for the scenario of lithopanspermia, which proposes a natural interplanetary exchange of organisms by means of rocks that have been impact ejected from their planet of origin. So far, the hardiness of these terrestrial organisms in the severe and hostile conditions of space has not been tested over extended periods of time. A first long-term (1.5 years) exposure experiment in space was performed with a variety of rock-colonizing eukaryotic organisms at the International Space Station on board the European EXPOSE-E facility. Organisms were selected that are especially adapted to cope with the environmental extremes of their natural habitats. It was found that some— but not all—of those most robust microbial communities from extremely hostile regions on Earth are also partially resistant to the even more hostile environment of outer space, including high vacuum, temperature fluctuation, the full spectrum of extraterrestrial solar electromagnetic radiation, and cosmic ionizing radiation. Although the reported experimental period of 1.5 years in space is not comparable with the time spans of thousands or millions of years believed to be required for lithopanspermia, our data provide first evidence of the differential hardiness of cryptoendolithic communities in space.
Content may be subject to copyright.
Survival of Rock-Colonizing Organisms
After 1.5 Years in Outer Space
Silvano Onofri,
1
Rosa de la Torre,
2
Jean-Pierre de Vera,
3
Sieglinde Ott,
4
Laura Zucconi,
1
Laura Selbmann,
1
Giuliano Scalzi,
1,5
Kasthuri J. Venkateswaran,
5
Elke Rabbow,
6
Francisco J. Sa´ nchez In˜ igo,
2
and Gerda Horneck
6
Abstract
Cryptoendolithic microbial communities and epilithic lichens have been considered as appropriate candidates
for the scenario of lithopanspermia, which proposes a natural interplanetary exchange of organisms by means of
rocks that have been impact ejected from their planet of origin. So far, the hardiness of these terrestrial organisms
in the severe and hostile conditions of space has not been tested over extended periods of time. A first long-term
(1.5 years) exposure experiment in space was performed with a variety of rock-colonizing eukaryotic organisms
at the International Space Station on board the European EXPOSE-E facility. Organisms were selected that are
especially adapted to cope with the environmental extremes of their natural habitats. It was found that some—
but not all—of those most robust microbial communities from extremely hostile regions on Earth are also
partially resistant to the even more hostile environment of outer space, including high vacuum, temperature
fluctuation, the full spectrum of extraterrestrial solar electromagnetic radiation, and cosmic ionizing radiation.
Although the reported experimental period of 1.5 years in space is not comparable with the time spans of
thousands or millions of years believed to be required for lithopanspermia, our data provide first evidence of the
differential hardiness of cryptoendolithic communities in space. Key Words: Astrobiology—Lithopanspermia—
Radiation resistance—Survival—Vacuum. Astrobiology 12, 508–516.
1. Introduction
The lithopanspermia hypothesis suggests that impact-
ejected rocks could transfer living organisms through
space from one planet to another. This scenario implies that
rock-embedded organisms need to survive the following
three phases: first (phase-I), the ejection into space inside rock
fragments due to an impact of a cosmic projectile on one
planet (Melosh, 1984); second (phase-II), the journey through
space for a long time (hundreds, even thousands or millions,
of years) (Gladman et al., 1996); and last (phase-III), the cap-
ture by and landing on another planet (Mileikowsky et al.,
2000; Horneck et al., 2008; Nicholson, 2009). This hypothesis
dates back to Lord Kelvin’s presidential address to the British
Association in 1871 (Thomson, 1871). However, it was dis-
missed by most contemporary scientists at the time because
the general opinion was that outer space would kill any living
being exposed to it and there was no way to test the idea
experimentally. Another severe criticism was that such a hy-
pothesis just shifts the problem of the origin of life to another
planet. Only in the last decade, after the detection of several
meteorites that originated from Mars (Nyquist et al., 2001;
Fritz et al., 2005; Shuster and Weiss, 2005; The Meteoritical
Society, 2011), has lithopanspermia been seriously considered
again (Sancho et al., 2007; Sto
¨ffler et al., 2007; Horneck et al.,
2008, 2010; Nicholson, 2009; de la Torre et al., 2010).
Shock recovery experiments performed to test phase-I of
lithopanspermia showed that spores of Bacillus subtilis and
the lichen Xanthoria elegans could survive pressures up to
40 GPa, which are comparable to those experienced by the
martian meteorites (Sto
¨ffler et al., 2007; Horneck et al., 2008).
Space technology provided the opportunity to study a vari-
ety of biological specimens after exposure to space. Among
the systems tested, bacterial spores (B. subtilis) and the
1
Department of Ecological and Biological Sciences, University of Tuscia, Viterbo, Italy.
2
Department of Earth Observation, Spanish Aerospace Research Establishment-INTA, Torrejo
´n de Ardoz, Madrid, Spain.
3
Institute of Planetary Research, German Aerospace Center (DLR), Berlin, Germany.
4
Institut fu
¨r Botanik, Heinrich-Heine-Universita
¨t, Du
¨sseldorf, Germany.
5
Jet Propulsion Laboratory, California Institute of Technology, Pasadena, California, USA.
6
Institute of Aerospace Medicine, German Aerospace Center (DLR), Cologne, Germany.
ASTROBIOLOGY
Volume 12, Number 5, 2012
ªMary Ann Liebert, Inc.
DOI: 10.1089/ast.2011.0736
508
lichens Rhizocarpon geographicum and X. elegans stood out
due to their high resistance to the hostile space environment
(Sancho et al., 2007; de la Torre et al., 2010; Horneck et al.,
2010). However, eukaryotes have never been studied after
long-term exposures to space conditions.
To investigate the fate of lithic organisms and communi-
ties during long-term travel in space, we used ESA’s
EXPOSE-E facility (Rabbow et al., 2009, 2012). This facility
was attached to the balcony of the Columbus module of the
International Space Station (ISS) (Fig. 1A). EXPOSE-E was
designed to expose a variety of biological systems to selected
parameters of space over time spans of one year and more.
All biological test systems of the LIFE (Lichens and Fungi
Experiment) experiment were rock-dwelling organisms from
hostile regions: Antarctic cryptoendolithic (dwelling inside
rocks) communities in their natural sandstone, microcolonial
black cryptoendolithic fungi (Cryomyces antarcticus and
Cryomyces minteri) isolated from Antarctic sandstone, and
high mountain epilithic lichens (R. geographicum and X. ele-
gans) (de Vera et al., 2003, 2008; Selbmann et al., 2005; Sancho
et al., 2007; de la Torre et al., 2010). These lichens were se-
lected as test systems due to their high resistance to space
conditions demonstrated during short-term (10–16 days)
exposures (Lichens experiment on ESA’s Foton-M2 Mission
2005 and Lithopanspermia experiment on ESA’s Foton-M3
Mission 2007) (Sancho et al., 2007; de la Torre et al., 2010). The
biological samples were accommodated in small chambers
(1.4 cm in diameter) of the EXPOSE-E facility (Fig. 1B).
During the space mission, they were exposed either to the
full space environment (vacuum from 10
-7
to 10
-4
Pa,
fluctuations of temperature between -21.5C and +59.6C,
cosmic ionizing radiation up to 190 mGy, and solar extra-
terrestrial electromagnetic radiation up to 6.34 ·10
8
Jm
-2
)or
they were shielded from insolation. After 1.5 years in space,
the samples were retrieved and their viability investigated.
During the mission, the Sun-exposed LIFE samples were
exposed to 1879 estimated solar constant hours (Rabbow
et al., 2012).
2. Material and Methods
2.1. Experiment hardware and biological
samples of the LIFE experiment on board
the International Space Station
The EXPOSE-E facility is part of the European Technology
Exposure Facility (EuTEF) (Fig. 1A), which was designed for
testing different materials under selected parameters of
space. On 7 February 2008, EuTEF with EXPOSE-E accom-
modating the biological samples of the LIFE experiment (Fig.
1B) was launched on board Space Shuttle STS-122 for the ISS.
On 15 February 2008, EXPOSE-E was mounted onto the
outside balcony of the Columbus module by extravehicular
activity. EXPOSE-E was decommissioned on 1 September
2009, retrieved by extravehicular activity on 2 September
2009, and returned to Earth on 12 September 2009 with STS-
128. During the 1.5 years mission, the samples were exposed
to space vacuum (10
-7
to 10
-4
Pa) (Horneck et al., 2010),
galactic cosmic radiation ( £190 mGy) (Berger et al., 2012),
and the full spectrum of solar extraterrestrial electromagnetic
radiation (k>110 nm) with fluences of 9.19 ·10
5
Jm
-2
(below
a 0.1% transmission neutral density filter) and 6.34 ·10
8
Jm
-2
(100% transmission insolated samples). All fluences were
calculated for the biologically active UV range of 200 nm <
k>400 nm, depending on the orientation of the ISS to the Sun.
Temperature varied between -21.5Cand +59.6C (Rabbow
et al., 2012).
2.2. Test systems of the LIFE experiment
The lichen Xanthoria elegans was collected from alpine
habitats between 2000 and 3000 m altitudes at Zermatt,
Switzerland (4559¢N, 748¢E) (de Vera et al., 2003, 2008);
FIG. 1. Experiment hardware and biological samples of the LIFE experiment. (A) EXPOSE-E facility (arrow) attached to the
Columbus module of the ISS during orbital flight, accommodating the LIFE samples. (B) Samples of the LIFE experi-
ment accommodated in one of the compartments of the EXPOSE-E facility (well diameter 1.4 cm). Vertical rows show
X. elegans (b1) and R. geographicum (b2) on their natural rock habitat; dried cultures of the lichen fungus (mycobiont) of X.
elegans (1
st
and 3
rd
sample from the top in b3); sandstone fragments colonized by a stratified cryptoendolithic microbial
community (2
nd
and 4
th
samples from the top in b4), and the fungi C. antarcticus and C. minteri (from the top 2
nd
and last
sample in b3, upper and 3
rd
sample in b4). Color images available online at www.liebertonline.com/ast
ROCK-COLONIZING ORGANISMS IN SPACE 509
Rhizocarpon geographicum was collected from the Plataforma
de Gredos, Spain (4017¢N, 514¢W) at an altitude of 2020 m
(de la Torre et al., 2010); sandstone fragments colonized by a
stratified cryptoendolithic microbial community were col-
lected by L. Zucconi at Battleship Promontory (7654¢37.6S,
16055¢27.5E), Southern Victoria Land, Antarctica, in Janu-
ary 2004; and the microcolonial black yeast-like fungi Cryo-
myces antarcticus CCFEE 515 and Cryomyces minteri CCFEE
5187, both dwelling cryptoendolithically, were isolated from
sandstone collected in McMurdo Antarctic Dry Valleys
(Selbmann et al., 2005). The survival of those cryptoendolithic
organisms is of special interest in terms of lithopanspermia
because rocks may supply an additional external protection
to face the impact-driven ejection into space (Horneck et al.,
2008; Meyer et al., 2011) and transfer from one planet to
another.
2.3. Viability assays of the LIFE test systems
The photosynthetic activity of the lichens X. elegans and
R. geographicum was measured after reactivating the samples
in a climatic chamber under the following controlled con-
ditions: constant temperature of 10C, 12 h light and 12 h
dark cycles for 96 h (X. elegans)or72h(R. geographicum).
Irradiation with photosynthetically active light was per-
formed by using a mercury lamp with a 100 lmol m
-2
s
-1
photosynthetic photon flux density. For rehydration, sam-
ples were sprayed twice a day with deionized water. After
reactivation, the activity of the photosystem II (PSII) of the
photobiont was measured with a Mini-PAM fluorometer
(Heinz Walz GmbH), as described previously (Sancho et al.,
2007; de Vera et al., 2010). Lichens were rewetted immedi-
ately before each measurement. The optimum quantum
yield of chlorophyll awas determined by fluorescence
measurements after 20 min of dark adaptation, according to
the equation
Fv=Fm ¼(Fm Fo)=Fm
with Fv =variable fluorescence yield, Fm =maximal fluores-
cence yield, and Fo =minimal fluorescence yield. This opti-
mum quantum yield of PSII was taken as an indication of the
PSII activity of the photobiont of the lichen system after the
exposure to space parameters. The percentage (n=2 for space
100% insolated and for space 0.1% insolated, and n=4 space
dark samples) of PSII activity was determined from the ratio
of the Fv/Fm of the same flight sample before and after
flight. Control data are given for the same sample measured
before spaceflight (preflight).
The survival of C. antarcticus and C. minteri was determined
from their colony-forming ability as percentages of colony-
forming units (CFU). Growth tests were performed by sus-
pending fungal cells from rehydrated colonies in a 0.9% NaCl
solution, inoculating them on malt agar Petri dishes (five
replicates), and incubating them at 15C for 30 days. Control
data were obtained from fresh colonies. Statistical analyses
were performed by one-way analysis of variance (ANOVA)
and pairwise multiple comparison procedure (Tukey test),
which was carried out by using the statistical software Sig-
maStat 2.0 ( Jandel, USA). The means (n=5) standard devi-
ation (s.d.) are plotted. *P=0.001; power of performed test
with a=0.050: 1.000.
The propidium monoazide (PMA) assay was used to
check the integrity of the cell membranes after spaceflight.
Fractions of DNA extracted from intact cells of cryptoendo-
lithic fungi C. antarcticus and C. minteri colonies were com-
pared with the fraction of DNA extracted from cells isolated
from the space-exposed colonized sandstone fragments. It
was performed by adding PMA (Biotium, Hayward, CA) at a
final concentration of 200 lMto the rehydrated fungal
colonies or to powdered rock suspensions in phosphate-
buffered saline solution. PMA penetrates only damaged cell
membranes, cross-links then to DNA after light exposure,
and thereby prevents polymerase chain reaction (PCR). Fol-
lowing DNA extraction and purification (Maxwell 16 auto-
mated DNA extraction instrument, Promega, Madison, WI),
quantitative PCR (Bio-Rad CFX96 real time PCR detection
system) was used to quantify the number of fungal internal
transcribed spacer (ITS) ribosomal DNA fragments present
in both PMA treated and non-treated samples. For all reac-
tions, 1 lL of purified genomic DNA was added to 23 lLof
PCR cocktail containing 1X Power Sybr-Green PCR Master
Mix (Applied Bios, Foster City, CA), as well as NS91 forward
(5¢-gtc cct gcc ctt tgt aca cac-3¢) and ITS51 reverse (5¢-acc ttg
tta cga ctt tta ctt cct c-3¢) primers, each at 0.02 Mfinal con-
centration. These primers amplify a 203 bp product spanning
the 18S/ITS1 region of rRNA-encoding genes.
A standard quantitative PCR cycling protocol consisting of a
hold at 95C for 10 min, followed by 40 cycles of denaturing at
95C for 15 s, annealing at 58C for 20 s, and elongation at 72C
for 15 s, was performed. Fluorescence measurements were re-
corded at the end of each annealing step. At the conclusion of
the 40
th
cycle, a melt curve analysis was performed by re-
cording changes in fluorescence as a function of raising the
temperature from 60Cto95Cin0.5C per 5 s increments.
These protocols were applied to the processing of both fungal
colonies and cryptoendolithic sandstone samples.
Control data were obtained for an identical sample stored on
ground in the laboratory during the mission (Control). Because
cryptoendolithic communities are not uniformly distributed
within the rocks, different quantities of total fungal DNA were
obtained from different rock samples.
Space data are given for samples shielded from extraterres-
trial UV radiation (Space Dark), exposed to k>110 nm at a
fluence of 9.19 ·10
5
Jm
-2
beneath a 0.1% transmission MgF
2
filter (Space 0.1% insolated), or at a higher fluence of 6.34·10
8
J
m
-2
(Space 100% insolated). Statistical analyses were per-
formed by one-way ANOVA and pairwise multiple compari-
son procedure (Tukey test), which was carried out by using the
statistical s oftware SigmaStat 2.0 ( Jandel, USA) *P=0.001;
**P>0.05. Power of performed test with a=0.050: 1.000. The
means (n=3) and s.d. are plotted.
2.4. Confocal laser scanning microscopy (CLSM)
imaging: viability of X. elegans analyzed by LIVE/
DEAD staining kit FUN 1
Adult lichen thallus, young thallus, and the isolated my-
cobiont of X. elegans were stained by FUN 1 to determine
their viability. A green and yellow color of the cells indicates
that they still maintain vitality. A change from green to
yellow in the cytoplasm and from green to red in the vacu-
oles is an indication of physiological activity expressed by
accumulation of the dye in the vacuoles. Dead cells cannot
510 ONOFRI ET AL.
be stained; therefore, red crystals are not formed in the
vacuoles.
Instruments used for imaging are as follows: LSM 510
META of Carl Zeiss Mikroskopsysteme Jena GmbH with
objective lenses 10 ·and 40 ·/oil immersion, scanning res-
olution 1024 ·1024 pixels and time 64 ls to 1.76 ls, scan
zoom 0.7 ·-2.8, image bit depth 12 bit, experimental tem-
perature condition 22C, UV-laser with emission wavelength
488/561/633 nm and VIS-laser HeNe with 633 nm excitation
and 5 mW power, filters with ChS1 679–754; Ch2 BP 505–550;
Ch3 BP 575–615. For operation of the instrument, the Carl
Zeiss Jena GmbH software system at the Institute of Genetics
of the Heinrich-Heine-Universita
¨tDu
¨sseldorf was used.
3. Results
First visual inspections assured that the ‘‘space samples’’
had not changed in shape and color compared to their pre-
flight appearances. Tailored to each test system, different
viability assays were applied: (i) photosynthetic activity of
the lichenized alga (photobiont) of X. elegans and R. geo-
graphicum (Fig. 2); (ii) colony-forming ability of C. antarcticus
and C. minteri (Fig. 3A and 3B); (iii) fraction of DNA am-
plified from intact cells of C. antarcticus and C. minteri and of
cryptoendolithic communities inside sandstone fragments
(Fig. 3C, 3D, and 3E); and (iv) viability of X. elegans and the
fungus of the lichen (mycobiont, cultured without the algal
symbiont and dried) by means of vital staining (Fig. 4).
Among those space samples that were shielded from ex-
traterrestrial insolation but exposed to space vacuum, cosmic
radiation, and temperature fluctuations (Space Dark in Figs.
2 and 3), the lichen X. elegans excelled by a PSII activity of
99.35 0.59% compared to the preflight data of the same
samples (Fig. 2A). This high viability was not reached by the
other space test systems kept in the dark during the mission:
2.46 1.39% for the PSII activity of the lichen R. geographicum
(Fig. 2B), and 8.04 3.05% and 0.13 0.07% surviving cells for
C. antarcticus and C. minteri, respectively (Fig. 3A and 3B).
PMA assay showed 98 4.67% and 8.14 0.35% of DNA
amplified from intact cells from colonies of C. antarcticus and
C. minteri, respectively (Fig. 3C and 3D), in comparison to
total extracted DNA; the percentage of DNA amplified from
intact fungal cells in sandstone fragments was 18 0.18%
(Fig. 3E).
The viability of culturable cells was not further decreased
in the black fungi (12.5 4.11% for C. antarcticus and
0.46 0.24% for C. minteri) that were insolated with the full
extraterrestrial spectrum (k>110 nm) of the Sun, having
AB
FIG. 2. Viability of the lichens (A)X. elegans and (B)R. geographicum, determined by fluorescence measurements of the
photosynthetic activity of the photobiont. Control data are given for the same sample measured before spaceflight (preflight), as
100% viability. Space data are given for samples shielded from extraterrestrial UV radiation (Space Dark), and insolated
(k>110 nm) at a fluence of 6.34 ·10
8
Jm
-2
(Space 100% insolated). Color images available online at www.liebertonline.com/ast
ROCK-COLONIZING ORGANISMS IN SPACE 511
*
*
*
*
AB
FIG. 3. Viability of the fungi (A)C. antarcticus and (B)C. minteri, as percentage of survival, determined as CFU. Control data
were obtained from fresh colonies. No CFU were obtained from the samples ‘‘Space 100% insolated.’’ The meanss.d. are
plotted. *P=0.001. Power of performed test with a=0.050: 1.000. ITS rDNA fragments amplified from intact cells of C.
antarcticus and C. minteri (Cand D) colonies and from sandstone fragments (E) after different space conditions, compared to
total extracted DNA. PMA penetrates only damaged cells’ membranes, cross-linking to DNA after light exposure and thereby
preventing PCR amplification. Following DNA extraction and purification, quantitative PCR was used to quantify the
number of fungal ITS rDNA fragments (203 bp) amplifiable in samples treated and non-treated with PMA. The means (n=3)
and s.d. are plotted. Statistical significance was calculated by using the Tukey test. *P=0.001. **P>0.05. Power of performed
test with a=0.050: 1.000. Color images available online at www.liebertonline.com/ast
512 ONOFRI ET AL.
received an UV irradiation of 9.19 ·10
5
Jm
-2
(Space 0.1%
insolated, Fig. 3A and 3B). The highest fraction of intact
fungal cells (35 0.15%) occurred in a sandstone sample that
had received the full influx of solar electromagnetic radiation
of 6.34 ·10
8
Jm
-2
(Space 100% insolated, Fig. 3E). When
comparing all test systems exposed to outer space, including
the high influx of full solar extraterrestrial radiation
(6.34 ·10
8
Jm
-2
), again the lichen X. elegans, with a PSII
activity of 45 2.50% (Fig. 2A) and C. antarcticus with
80 0.82% of DNA from intact cells (Fig. 3C), were the most
resistant test systems of LIFE. However, black Antarctic
cryptoendolithic fungi lost colony-forming ability after ex-
posure to full insolation; no survivors were detected in the
space 100% insolated samples. Resistance of X. elegans and
its mycobiont after exposure to the combined action of all
space parameters tested, including full insolation, was con-
firmed by vital staining and CLSM. Figure 4 shows the high
capacity of the lichenized fungus (part of the symbiotic li-
chen association) in a young thallus (B), and of the lichen
fungus of X. elegans in pure culture (C), to resist space ex-
posure. The fungal cells in the cortex (Cx) of the young
thallus were still vital, although a protecting mucilage layer
had not been formed, and the parietin layer appeared to be
very thin. The same features appeared to (C), the fungal cells
of the mycelium.
4. Discussion
The LIFE experiment provided for the first time data on
the viability of rock-dwelling organisms and microbial
communities after a long-term exposure to space parameters.
These conditions cannot easily be simulated in the labora-
tory, if at all. The test systems collected from hostile condi-
tions, such as Antarctica and high mountain regions, are
FIG. 3. Continued.
ROCK-COLONIZING ORGANISMS IN SPACE 513
adapted to cope with high radiation intensities, arid phases,
and extreme temperature fluctuations that are in some ways
similar to those experienced in space. In C. antarcticus, for
example, globular cells are enveloped in a thick melanized
cell wall, which protects them from radiation and desicca-
tion. Their meristematic way of producing colonies (i.e., di-
viding in all directions) further supports their resistance
(Onofri et al., 2008, 2009; Selbmann et al., 2005; Sterflinger,
2005). Special protection against environmental extremes is
also granted for the photobiont, the green alga Trebouxia sp.
of the lichen X. elegans. In this symbiotic organization, the
fungus forms a cortex with an upper layer encrusted with
parietin and a mucilage layer that envelopes the algal cells in
a medulla matrix (Fig. 4A and 4B) (de Vera et al., 2003, 2008).
All organisms selected for the LIFE experiment are poi-
kilohydric, that is, they are able to dehydrate till most bio-
chemical activities stop. In this state, they are highly tolerant
to stresses and may resume their metabolism once water
becomes available again. Specifically, exposure to vacuum
should inhibit any oxidative process related to their metab-
olism; this particular effect could protect against other
damaging effects induced, for example, by solar UV radia-
tion, cosmic ray ions, and temperature extremes.
The LIFE experiment has demonstrated that some, but not
all, of those most robust microbial communities from ex-
tremely hostile regions on Earth are also partially resistant
against the even more hostile environment of outer space. In
this experiment, the following species stood out as the most
persistent survivors after 1.5 years in outer space: the black
fungus C. antarcticus (as determined from PMA assay) and
the symbiotic X. elegans (as determined from PSII activity)
and its mycobiont (as determined by LIVE/DEAD staining).
However, the CFU test did not yield any survivors of C.
antarcticus flight samples that were exposed to the un-
attenuated solar extraterrestrial spectrum (space 100% in-
solated) and less than 10% survivors for the space dark
samples. This means that even if the cell membrane seemed
to be intact, as indicated by the PMA test, the cells had lost
their ability to grow and divide.
Earlier studies have shown that the circumpolar and al-
pine red lichen X. elegans was able to retain its photosyn-
thetic activity almost completely after 14 days in space
(Sancho et al., 2007; de la Torre et al., 2010). This observation
was confirmed in the present study for a much longer ex-
posure time of 565 days in space, although this high viability
was only observed for the lichen that had been shielded from
solar electromagnetic irradiation, maintaining 45% PSII ac-
tivity after 100% insolation exposure. CLSM, in combination
with the use of specific fluorescent probes, allowed for the
assessment of the physiological state of the cells. Particularly,
the mycobiont seemed to play a fundamental role in main-
taining the viability of the entire lichen system, because 565
days in space appeared not to have any effect on its physio-
logical activity, even after 100% insolation (Fig. 4C). These
observations are in agreement with earlier ones from short-
term space exposures (de la Torre et al., 2010); in those studies
the spores also maintained a high germination capacity, even
after exposure to the full spectrum of solar UV radiation.
However, so far, the ability of X. elegans to reproduce after this
long-term space exposure remains an open question.
Interestingly, it has been earlier shown that X. elegans also
resisted shock pressures comparable to those experienced by
the martian meteorites during impact ejection (Horneck et al.,
2008; Meyer et al., 2011), as required for phase-I of litho-
panspermia.
Although we have demonstrated that some rock-dwelling
species are capable of partially withstanding the harsh en-
vironment of outer space, or certain parameters of it, for at
least 1.5 years, the data are insufficient for drawing any
consequences for the likelihood of lithopanspermia. The
possibility of surviving a much longer journey in space, as
would be required for natural travel from Mars to Earth or
vice versa, still remains an open question. This especially
applies to organisms that dwell at the surface of rocks, like
the lichen X. elegans, which would be fully exposed to the
lethal spectrum of solar extraterrestrial UV radiation during
a hypothetical interplanetary transfer. The only one data point
at an exposure time of 1.5 years, resulting in a viability of
45 2.50%, as determined by PSII activity, does not allow any
extrapolation over hundreds, thousands, or even millions of
years, as would be required for lithopanspermia (Gladman
et al., 1996). The situation would be much more favorable for
FIG. 4. CLSM imaging: viability of X. elegans analyzed by LIVE/DEAD staining kit FUN I. (A) Adult lichen thallus, (B)
young thallus, and (C) lichen fungus isolated in pure culture (mycobiont) of X. elegans, all dried and exposed to 100%
insolation and space vacuum. Green to yellow cells are stained by FUN 1, indicating vital cells. Turning from green to yellow
and finally to red indicates physiological activity expressed by the accumulation of the dye in the vacuoles. The high degree
of maintained viability is due to a cortex Cx, a mucilage layer Mc, and crystal deposits of parietin P on the surface of the
lichen. These layers are able to protect interior cells of the algal layer A and the medulla M.
514 ONOFRI ET AL.
endolithic organisms, because they would be shielded from
solar UV radiation by the surrounding rock material. How-
ever, the cryptoendolithic organisms tested in this study did
not show a high survival rate in space, even if shielded from
solar UV radiation. Our experiments also demonstrate that
outer space can act as a selection pressure on the composition
of microbial communities (Cockell et al., 2011). Further studies
are needed with more resistant communities. An example is
the vagrant lichen species Aspicilia fruticulosa that, after 10
days in space, showed a complete recovery of space-induced
damage after 72 h of reactivation (Raggio et al., 2011).
Natural transfer of microorganisms between planets via
lithopanspermia could have occurred over the course of
billions of years (Gladman et al., 1996; Nicholson, 2009). In
the last 50 years, human activities in space exploration have
become another potential source of spreading microorgan-
isms between planets. Nearly 40 robotic missions have been
launched with Mars as their destination (Horneck et al.,
2007). To prevent the introduction of microbes from Earth to
another celestial body or vice versa, a concept of contami-
nation control has been elaborated by the Committee on
Space Research (COSPAR) under consideration of specific
classes of mission/target combinations, which have been
recommended to be followed by each space-faring organi-
zation (COSPAR, 2011). Lander missions to Mars require
especially strict measures of cleanliness and partial sterility
of the spacecraft (COSPAR, 2011). The test systems that have
been used in the LIFE experiment, though unlikely to be
found on spacecraft, can be considered as models for dem-
onstrating how life, if accidentally transferred from Earth to
outer space, may resist and contaminate other celestial
bodies and planets (i.e., Mars) and thereby interfere with
future life-detection missions.
Acknowledgments
We thank the staff at the European Space Agency for the
provision and operations of the EXPOSE-E facility and
Thomas Berger for the cosmic ray dosimetry data. We also
thank the Italian National Program of Antarctic Research
and National Antarctic Museum for funding the collection of
Antarctic samples, strains, and sample analyses, as well as
the European Coordination Action for Research Activities on
life in Extreme Environments (CAREX) for one ToK Grant to
G.S. Collection and preparation of samples, and CLSM and
photosynthetic activity analyses of X. elegans have been
supported partly by the Helmholtz Association through the
research alliance ‘‘Planetary Evolution and Life’’ and the
BMWi, 50WB0614; the selection and preparation of the Rhi-
zocarpon geographicum samples have been financed by the
Space Program of the Spanish Ministry of Science and Edu-
cation (ESP2005-25292-E) and INTA. We thank Philipp
Holzwig, Isabella Halezki, Eva-Maria Posthoff, and the In-
stitute of Genetics at the Heinrich-Heine-Universita
¨tDu
¨s-
seldorf for skillful technical assistance. Special thanks also go
to Prof. Giovanni Bignami for his scientific advice.
Author Disclosure Statement
No competing financial interests exist for Silvano Onofri,
Rosa de la Torre, Jean-Pierre de Vera, Sieglinde Ott, Laura
Zucconi, Laura Selbmann, Giuliano Scalzi, Kasthuri J. Ven-
kateswaran, Elke Rabbow, Francisco Javier Sa
´nchez In
˜igo, or
Gerda Horneck.
Abbreviations
ANOVA, analysis of variance; CFU, colony-forming units;
CLSM, confocal laser scanning microscopy; COSPAR, Com-
mittee on Space Research; EuTEF, European Technology
Exposure Facility; ISS, International Space Station; ITS, in-
ternal transcribed spacer; PCR, polymerase chain reaction;
PMA, propidium monoazide; PSII, photosystem II; s.d.,
standard deviation.
References
Berger, T., Hajek, M., Bilski, P., Ko
¨rner, C., Vanhavere, F., and
Reitz, G. (2012) Cosmic radiation exposure of biological test
systems during the EXPOSE-E mission. Astrobiology 12:387–
392.
Cockell, C.S., Rettberg, P., Rabbow, E., and Olsson-Francis, K.
(2011) Exposure of phototrophs to 438 days in low Earth orbit:
microbial selection pressures in outer space and on early
Earth. ISME J 10:1671–1682.
COSPAR. (2011) COSPAR Planetary Protection Policy (20 October
2002, as amended 24 March 2011), COSPAR, Paris. Available
online at http://cosparhq.cnes.fr/Scistr/PPPolicy%20%2824-
Mar2011%29.pdf.
de la Torre, R., Sancho, L., Horneck, G., de los Rı
´os, A., Wierz-
chos, J., Olsson-Francis, K., Cockell, C.S., Rettberg, P., Berger,
T., de Vera, J.-P.P., Ott, S., Martinez Frı
´as, J., Melendi, P.G.,
Lucas, M.M., Reina, M., Pintado, A., and Demets, R. (2010)
Survival of lichens and bacteria exposed to outer space con-
ditions—results of the Lithopanspermia experiments. Icarus
208:735–748.
de Vera, J.P., Horneck, G., Rettberg, P., and Ott, S. (2003) The
potential of lichen symbiosis to cope with extreme conditions
of outer space.—I. Influence of UV radiation and space vac-
uum on the vitality of lichen symbiosis and germination ca-
pacity. International Journal of Astrobiology 1:285–293.
de Vera, J.P., Rettberg, P., and Ott, S. (2008) Life at the limits:
capacities of isolated and cultured lichen symbionts to resist
extreme environmental stresses. Orig Life Evol Biosph 38:457–
468.
de Vera, J.P., Mo
¨hlmann, D., Butina, F., Lorek, A., Wernecke, R.,
and Ott, S. (2010) Survival potential and photosynthetic ac-
tivity of lichens under Mars-like conditions: a laboratory
study. Astrobiology 10:215–227.
Fritz, J., Artemieva, N.A., and Greshake, A. (2005) Ejection of
martian meteorites. Meteorit Planet Sci 40:1393–1411.
Gladman, B.J., Burns, J.A., Duncan, M., Lee, P., and Levison,
H.F. (1996) The exchange of impact ejecta between terrestrial
planets. Science 271:1387–1392.
Horneck, G., Debus, A., Mani P., and Spry J.A. (2007) Astro-
biology exploratory missions and planetary protection re-
quirements. In Complete Course in Astrobiology, edited by G.
Horneck and P. Rettberg, Wiley-VCH, Berlin, pp 353–397.
Horneck, G., Sto
¨ffler, D., Ott, S., Hornemann, U., Cockell,
C.S., Moeller, R., Meyer, C., de Vera, J.-P., Fritz, J., Schade,
S., and Artemieva, N.A. (2008) Microbial rock inhabitants
survive impact and ejection from host planet: first phase
of lithopanspermia experimentally tested. Astrobiology 8:
17–44.
Horneck, G., Klaus, D.M., and Mancinelli, R.L. (2010) Space
microbiology. Microbiol Mol Biol Rev 74:121–156.
ROCK-COLONIZING ORGANISMS IN SPACE 515
Melosh, H.J. (1984) Impact ejection, spallation, and the origin of
meteorites. Icarus 59:234–260.
Meyer, C., Fritz, J., Misgaiski, M., Sto
¨ffler, D., Artemieva, N.A.,
Hornemann, U., Moeller, R., de Vera, J.-P., Cockell, C., Hor-
neck, G., Ott, S., and Rabbow, E. (2011) Shock experiments in
support of the lithopanspermia theory: the influence of host
rock composition, temperature, and shock pressure on the
survival rate of endolithic and epilithic microorganisms. Me-
teorit Planet Sci 46:701–718.
Mileikowsky, C., Cucinotta, F., Wilson, J.W., Gladman, B.,
Horneck, G., Lindegren, L., Melosh, J., Rickman, H., Valtonen,
M., and Zheng, J.Q. (2000) Natural transfer of viable microbes
in space: 1. From Mars to Earth and Earth to Mars. Icarus
145:391–427.
Nicholson, W.L. (2009) Ancient micronauts: interplanetary
transport of microbes by cosmic impacts. Trends Microbiol
17:243–250.
Nyquist, L.E., Bogard, D.D., Shih, C.-Y., Greshake, A., Sto
¨ffler,
D., and Eugster O. (2001) Ages and geological histories of
martian meteorites. Space Sci Rev 96:105–164.
Onofri, S., Barreca, D., Selbmann, L., Isola, D., Rabbow, E.,
Horneck, G., de Vera, J.P.P., Hatton, J., and Zucconi, L. (2008)
Resistance of Antarctic black fungi and cryptoendolithic
communities to simulated space and martian conditions. Stud
Mycol 61:99–109.
Onofri, S., Selbmann, L., Barreca, D., Isola, D., and Zucconi, L.
(2009) Fungal survival in space conditions, new insights for
lithopanspermia. Plant Biosyst 143:S85–S87.
Rabbow, E., Horneck, G., Rettberg, P., Schott, J.-U., Panitz, C.,
L’Afflitto, A., von Heise-Rotenburg, R., Willnecker, R., Ba-
glioni, P., Hatton, J., Dettmann, J., Demets, R., and Reitz, G.
(2009) EXPOSE, an astrobiological exposure facility on the
International Space Station—from proposal to flight. Orig Life
Evol Biosph 39:581–598.
Rabbow, E., Rettberg, P., Barczyk, S., Bohmeier, M., Parpart, A.,
Panitz, C., Horneck, G., von Heise-Rotenburg, R., Hoppen-
brouwers, T., Willnecker, R., Baglioni, P., Demets, R., Dett-
mann, J., and Reitz, G. (2012) EXPOSE-E: an ESA astrobiology
mission 1.5 years in space. Astrobiology 12:374–386.
Raggio, J., Pintado, A., Ascaso, C., de la Torre, R., de los Rı
´os, A.,
Wierzchos, J., Horneck, G., and Sancho, L.G. (2011) Whole
lichen thalli survive exposure to space conditions: results of
Lithopanspermia experiment with Aspicilia fruticulosa.Astro-
biology 11:281–292.
Sancho, L.G., de la Torre, R., Horneck, G., Ascaso, C., de los
Rios, A., Pintado, A., Wierzchos, J., and Schuster, M. (2007)
Lichens survive in space: results from the 2005 LICHENS
experiment. Astrobiology 7:443–454.
Selbmann, L., de Hoog, G.S., Mazzaglia, A., Friedmann, E.I., and
Onofri, S. (2005) Fungi at the edge of life, cryptoendolithic
black fungi from Antarctic deserts. Stud Mycol 51:1–32.
Shuster, D.L. and Weiss, B.P. (2005) Martian surface paleo-
temperatures from thermochronology of meteorites. Science
309:594–597.
Sterflinger, K. (2005) Black yeasts and meristematic fungi: ecol-
ogy, diversity and identification. In Yeast Handbook: Biodi-
versity and Ecophysiology of Yeasts, edited by C. Rosa and P.
Gabor, Springer, New York, pp 505–518.
Sto
¨ffler, D., Horneck, G., Ott, S., Hornemann, U., Cockell, C.S.,
Moeller, R., Meyer, C., de Vera, J.-P., Fritz, J., and Artemieva,
N.A. (2007) Experimental evidence for the potential impact
ejection of viable microorganisms from Mars and Mars-like
planets. Icarus 186:585–588.
The Meteoritical Society. (2011) Meteoritical Bulletin Database, The
Meteoritical Society. Available on line at http://www.lpi
.usra.edu/meteor/metbull.php.
Thomson, W. (Lord Kelvin). (1871) The British Association
meeting at Edinburgh. Inaugural address of Sir William
Thomson, LL.D., F.R.S., President. Nature 4:262–270.
Address correspondence to:
Professor Silvano Onofri
Department of Ecological and Biological Sciences (DEB)
Largo dell’Universita
`snc
01100 Viterbo (Italy)
E-mail: onofri@unitus.it
Submitted 30 September 2011
Accepted 1 April 2012
516 ONOFRI ET AL.
This article has been cited by:
1. Elke Rabbow , Petra Rettberg , Simon Barczyk , Maria Bohmeier , André Parpart , Corinna Panitz , Gerda Horneck , Ralf
von Heise-Rotenburg , Tom Hoppenbrouwers , Rainer Willnecker , Pietro Baglioni , René Demets , Jan Dettmann , Guenther
Reitz . 2012. EXPOSE-E: An ESA Astrobiology Mission 1.5 Years in Space. Astrobiology 12:5, 374-386. [Abstract] [Full
Text HTML] [Full Text PDF] [Full Text PDF with Links]
2. Martin Schuster , Tsvetan Dachev , Peter Richter , Donat-Peter Häder . 2012. R3DE: Radiation Risk Radiometer-Dosimeter
on the International Space Station—Optical Radiation Data Recorded During 18 Months of EXPOSE-E Exposure to Open
Space. Astrobiology 12:5, 393-402. [Abstract] [Full Text HTML] [Full Text PDF] [Full Text PDF with Links]
... There is a need for studies that focus on elucidating microbial survival mechanisms in extreme habitats, as a primary goal of the planetary protection policy is to prevent forward and backward contamination of any celestial bodies and the Earth (Rummel et al., 2002). So far, the majority of such studies have focused on investigating extremophilic bacteria, mainly spore-formers ( Nicholson et al., 2012;Tirumalai et al., 2013), and rocks containing fungi ( Onofri et al., 2012;Zakharova et al., 2014) however, monolayers of fungal conidia have not been studied. ...
... Other studies have investigated molecular adaptations of selected species to space conditions, revealing changes in metabolome, and proteome of ISS-isolated strains ( Knox et al., 2016;Romsdahl et al., 2018;Blachowicz et al., 2019). In other investigations, several multilayered or embedded cryptoendolithic fungal communities were exposed to space conditions (Billi et al., 2011;Onofri et al., 2012Onofri et al., , 2015Scalzi et al., 2012;Pacelli et al., 2018). Tested isolates that adapted to environmental extremes of their habitats survived SMC for extended periods and revealed high stability of the DNA in the surviving cells (Billi et al., 2011;Onofri et al., 2015;Pacelli et al., 2018). ...
... In this study, recovery of fungal conidia exposed in monolayers from aluminum coupons was possible for both ISSFT-021 and IMV 00236 even after 30 min exposure, suggesting an enhanced ability of fungal conidia to withstand such environments. The results from this study, combined with those revealing that cryptoendolithic fungal communities embedded in rocks can withstand SMC for an extended period of time ( Onofri et al., 2012Onofri et al., , 2015Pacelli et al., 2018), imply that fungi should be considered as a possible forward contamination source. This is further supported by the fact that the omnipresence of filamentous fungi has been documented in spacecraft assembly facilities (La Duc et al., 2012;Weinmaier et al., 2015). ...
Article
Full-text available
Filamentous fungi have been associated with extreme habitats, including nuclear power plant accident sites and the International Space Station (ISS). Due to their immense adaptation and phenotypic plasticity capacities, fungi may thrive in what seems like uninhabitable niches. This study is the first report of fungal survival after exposure of monolayers of conidia to simulated Mars conditions (SMC). Conidia of several Chernobyl nuclear accident-associated and ISS-isolated strains were tested for UV-C and SMC sensitivity, which resulted in strain-dependent survival. Strains surviving exposure to SMC for 30 min, ISSFT-021-30 and IMV 00236-30, were further characterized for proteomic, and metabolomic changes. Differential expression of proteins involved in ribosome biogenesis, translation, and carbohydrate metabolic processes was observed. No significant metabolome alterations were revealed. Lastly, ISSFT-021-30 conidia re-exposed to UV-C exhibited enhanced UV-C resistance when compared to the conidia of unexposed ISSFT-021.
... A crucial issue on the Lithopanspermia theory consists in testing that microbes situated on or within rocky bodies could survive hypervelocity entry through the Earth's atmosphere (Cockell 2008) since some meteorites do not show signals of great heating (Mileikowsky et al. 2000;Weiss et al. 2000;Meyer et al. 2008;Nichoson 2009). For that purpose, the European Space Agency (ESA) has developed experiments to prove the endurance of terrestrial organisms against environmental conditions prevailing in space, particularly harmful radiation, vacuum and extreme temperatures, such as BIOPAN (effect of space environmental conditions on biological material), STONE 6 (survival of microfossils in artificial Martian meteorites to the Terrestrial atmospheric entry), LITHOPANSPERMIA (survival of organisms inside rocks to space conditions and atmospheric entry) and EXPOSE (study of survival of different terrestrial organisms to space environmental conditions) Horneck et al. 2008;de la Torre et al. 2010;Cockell et al. 2011;Meyer et al. 2011;Bertrand et al. 2012;Onofri et al. 2012;Parnell et al. 2012). The results of some of these experiments demonstrated the survival of some biomarkers linked unambiguously to biological activity. ...
... Although microorganisms, such as bacteria, are the main candidate in those studies, lichens have assumed an important role in Exobiology since numerous experiments, as LICHENS II on BIOPAN 5/FOTONM2; LITHOPANSPERMIA and STONE on BIOPAN6/FOTONM3; and LIFE on EXPOSE-E/EuTEF de la Torre et al. 2010;Raggio et al. 2011;de Vera 2012;Onofri et al. 2012;Scalzi et al. 2012), have demonstrated that lichens are viable after exposition to space conditions. Lichens can survive the outdoor space which exposes them to low and high temperatures in a short time period (e.g. ...
Article
Lithopanspermia Theory has suggested that life was transferred among planets by meteorites and other rocky bodies. If the planet had an atmosphere, this transfer of life had to survive drastic temperature changes in a very short time in its entry or exit. Only organisms able to endure such a temperature range could colonize a planet from outer space. Many experiments are being carried out by NASA and European Space Agency to understand which organisms were able to survive and how. Among the suite of instruments designed for extraplanetary exploration, particularly for Mars surface exploration, a Raman spectrometer was selected with the main objective of looking for life signals. Among all attributes, Raman spectroscopy is able to identify organic and inorganic compounds, either pure or in admixture, without requiring sample manipulation. In this study, we used Raman spectroscopy to examine the lichen Squamarina lentigera biomarkers. We analyse spectral signature changes after sample heating under different experimental situations, such as (a) laser, (b) analysis accumulations over the same spot and (c) environmental temperature increase. Our goal is to evaluate the capability of Raman spectroscopy to identify unambiguously life markers even if heating has induced spectral changes, reflecting biomolecular transformations. Usnic acid, chlorophyll, carotene and calcium oxalates were identified by the Raman spectra. From our experiments, we have seen that usnic acid, carotene and calcium oxalates (the last two have been suggested to be good biomarkers) respond in a different way to environmental heating. Our main conclusion is that despite their abundance in nature or their inorganic composition the resistance to heat makes some molecules more suitable than others as biomarkers.
... Cryo. antarcticus strains have withstood ground simulated space and Mars conditions ( Pacelli et al., 2017) and 18 months of real Space exposure and Mars-simulated exposure outside the International Space Station ( Onofri et al., 2012Onofri et al., , 2015Onofri et al., , 2018. Based on this resilience, Cryo. ...
Article
Full-text available
Endolithic growth is one of the most spectacular microbial adaptations to extreme environmental constraints and the predominant life-form in the ice-free areas of Continental Antarctica. Although Antarctic endolithic microbial communities are known to host among the most resistant and extreme-adapted organisms, our knowledge on microbial diversity and composition in this peculiar niche is still limited. In this study, we investigated the diversity and structure of the fungal assemblage in the cryptoendolithic communities inhabiting sandstone using a meta-barcoding approach targeting the fungal Internal Transcribed Sequence region 1 (ITS1). Samples were collected from 14 sites in the Victoria Land, along an altitudinal gradient ranging from 1,000 to 3,300 m a.s.l. and from 29 to 96 km distance to coast. Our study revealed a clear dominance of a ‘core’ group of fungal taxa consistently present across all the samples, mainly composed of lichen-forming and Dothideomycetous fungi. Pareto-Lorenz curves indicated a very high degree of specialization (F0 approximately 95%), suggesting these communities are highly adapted but have limited ability to recover after perturbations. Overall, both fungal community biodiversity and composition did not show any correlation with the considered abiotic parameters, potentially due to strong fluctuations of environmental conditions at local scales.
... Furthermore, virulence properties exhibited by fungal population need to be tested after exposing them beyond LEO orbit (12,13). Once these OSR extremophiles exhibit survival (14,15), their proliferation inside the DSG spacecraft would enable developing biofilms and such phenomenon should be tested under beyond LEO environment. Subsequently, there is a need to develop countermeasures to eradicate or contain these OSR extremophiles without human intervention for long duration missions. ...
Conference Paper
Full-text available
Early integration of science and exploration concerns into the design of the Deep Space Gateway (DSG) is essential to maximizing its science and exploration potential. The proposed concept, characterization of outer space radiation induced changes in microbial extremophiles, requires the DSG as infrastructure supplying power, communications, etc. to otherwise autonomous systems. Survival and proliferation of life beyond low earth orbit (LBLEO) can be accomplished by exposing extremophilic microorganisms in outer space radiation (OSR) conditions using DSG system. Extremophilic microbial survival, adaptation, biological functions, and molecular mechanisms associated with outer space radiation can be tested by exposing them onto DSG hardware (inside/outside) utilizing the traditional microbiology methods and state-of-the-art molecular biology techniques.
... So far, lichens are the only organisms that were able to survive under space conditions, which included solar extraterrestrial UV radiation as tested during the 2-week flight of BIOPAN- 5 and -6 ( Sancho et al., 2007;De los Ríos et al., 2009;De la Torre et al., 2010). Other studies were performed to concurrently test the response of lichen species under space and Mars-simulated conditions on board two space missions, EXPOSE-E and -R2 ( Onofri et al., 2012;, on the International Space Station. Laboratory studies using a simulated Mars environment and space-relevant ionizing radiation have also been conducted ( Sánchez et al., 2012;De la Torre et al., 2017;Meeßen et al., 2017). ...
Article
Full-text available
Lichens are extremely resistant organisms that colonize harsh climatic areas, some of them defined as “Mars-analog sites.” There still remain many unsolved questions as to how lichens survive under such extreme conditions. Several studies have been performed to test the resistance of various lichen species under space and in simulated Mars-like conditions. The results led to the proposal that Circinaria gyrosa (Lecanoromycetes, Ascomycota) is one of the most durable astrobiological model lichens. However, although C. gyrosa has been exposed to Mars-like environmental conditions while in a latent state, it has not been exposed in its physiologically active mode. We hypothesize that the astrobiological test system “Circinaria gyrosa,” could be able to be physiologically active and to survive under Mars-like conditions in a simulation chamber, based on previous studies performed at dessicated-dormant stage under simulated Mars-like conditions, that showed a complete recover of the PSII activity (Sánchez et al., 2012). Epifluorescence and confocal laser scanning microscopy (CLSM) showed that living algal cells were more abundant in samples exposed to niche conditions, which simulated the conditions in micro-fissures and micro-caves close to the surface that have limited scattered or time-dependent light exposure, than in samples exposed to full UV radiation. The medulla was not structurally affected, suggesting that the niche exposure conditions did not disturb the lichen thalli structure and morphology as revealed by field emission scanning electron microscopy (FESEM). In addition, changes in the lichen thalli chemical composition were determined by analytical pyrolysis. The chromatograms resulting from analytical pyrolysis at 500°C revealed that lichen samples exposed to niche conditions and full UV radiation consisted primarily of glycosidic compounds, lipids, and sterols, which are typical constituents of the cell walls. However, specific differences could be detected and used as markers of the UV-induced damage to the lichen membranes. Based on its viability responses after rehydration, our study shows that the test lichen survived the 30-day incubation in the Mars chamber particularly under niche conditions. However, the photobiont was not able to photosynthesize under the Mars-like conditions, which indicates that the surface of Mars is not a habitable place for C. gyrosa.
... As a consequence, organisms using these putative metabolic pathways would need to cope with additional sources of stress, including high radiation and, in the case of icy worlds, low temperatures. The low pressures and potential drastic pressure changes of near-surface environments could be resisted by terrestrial microorganisms, whose tolerance spans the minute pressures outside the International Space Station (Horneck, 1999;Cox and Battista, 2005;de la Torre et al., 2010;Onofri et al., 2012;Vaishampayan et al., 2012) to 100 MPa at the Challenger Deep (Kato et al., 1998). ...
Article
Life on Earth is found in a wide range of environments as long as the basic requirements of a liquid solvent, a nutrient source, and free energy are met. Previous hypotheses have speculated how extraterrestrial microbial life may function, among them that particle radiation might power living cells indirectly through radiolytic products. On Earth, so-called electrophilic organisms can harness electron flow from an extracellular cathode to build biomolecules. Here, we describe two hypothetical mechanisms, termed "direct electrophy" and "indirect electrophy" or "fluorosynthesis," by which organisms could harness extracellular free electrons to synthesize organic matter, thus expanding the ensemble of potential habitats in which extraterrestrial organisms might be found in the Solar System and beyond. The first mechanism involves the direct flow of secondary electrons from particle radiation to a microbial cell to power the organism. The second involves the indirect utilization of impinging secondary electrons and a fluorescing molecule, either biotic or abiotic in origin, to drive photosynthesis. Both mechanisms involve the attenuation of an incoming particle's energy to create low-energy secondary electrons. The validity of the hypotheses is assessed through simple calculations showing the biomass density attainable from the energy supplied. Also discussed are potential survival strategies that could be used by organisms living in possible habitats with a plentiful supply of secondary electrons, such as near the surface of an icy moon. While we acknowledge that the only definitive test for the hypothesis is to collect specimens, we also describe experiments or terrestrial observations that could support or nullify the hypotheses. Key Words: Radiation-Electrophiles-Subsurface life. Astrobiology 18, xxx-xxx.
... Stone colonization is a multi-step process leading to the establishment of complex microbial communities responsible for stone deterioration [3,12,45]. Some microorganisms, particularly adapted to extreme conditions such as rock black fungi and cyanobacteria, represent a serious challenge for restorers due to their ability to grow inside the rock and cope with several physical and chemical stresses when desiccated [12,25,27,45,[60][61][62]. Therefore, the control of rock settlers and their complete removal are the primary goals in restoration of outdoor cultural and historical heritages. ...
Article
In restoration and conservation practices, biocide treatments are considered one of the most practical approaches to remove biological colonization on artworks, including stone. Numerous studies have focused on the short- and long-term effects of these treatments and recently many alternative methods to reduce their potential hazards to human health and the environment have been proposed. In this study, a solvent gel containing dimethyl sulfoxide (DMSO), already used to clean paintings, was applied on colonized marble artifacts at the monumental cemetery of Bonaria (Cagliari - Italy) to remove biological patinas. The protocol efficiency was evaluated by scanning electronic microscopy, rugosimetric and colorimetric measurements and growth tests. A comparative study also was performed to validate the method using biocides currently used in conservation. The results demonstrate that DMSO solvent gel is efficient at removing patinas on stone, of low impact, easy to use, inexpensive and can be considered a more practical alternative to biocide treatments.
... Analogous to the tanning of human skin, fungal melanogenesis is also stimulated by exposure to ionizing radiation and resulting in pigmented yeasts which are more resistant to radiotoxicity than their albino counterparts ( Bultler, 1987;Durrell and Shields, 1960;Ellis and Griffiths, 1975;Gauslaa and Solhaug, 2001;Selbmann et al., 2011;Wang and Casadevall, 1994;Zhdanova et al., 1978). It is important to note that black fungi are able to survive ionizing radiation levels that are lethal to any other eukaryote ( Dighton et al., 2008;Mironenko et al., 2000;Onofri et al., 2012;Selbmann et al., 2015;Zhdanova et al., 1991) which yields its own interesting implications with regards to the limits of life. The mechanism by which fungal melanin protects a cell from radiation damage likely involves a combination of several processes for absorption-dissipation of radiation energy, including: changes in melanin's chemical composition and structure, inelastic scattering of photons by protons or electrons (or Compton scattering), non-radiative dissipation of absorbed photons (a process that results in energy decay in the form of heat), and antioxidant or free-radical scavenging ( Khajo et al., 2011;Revskaya et al., 2012). ...
Article
Melanins are ancient biological pigments found in all kingdoms of life. In fungi, their role in microbial pathogenesis is well established; however, these complex biomolecules also confer upon fungal microorganisms the faculty to tolerate extreme environments such as the Earth's poles, the International Space Station and places contaminated by toxic metals and ionizing radiation. A remarkable property of melanin is its capacity to interact with a wide range of electromagnetic radiation frequencies, functioning as a protecting and energy harvesting pigment. Other roles of fungal melanin include scavenging of free radical, thermo-tolerance, metal ion sequestration, cell development, and mechanical-chemical cellular strength. In this review, we explore the various functions ascribed to this biological pigment in fungi and its remarkable physicochemical properties.
Article
With the discovery of rocky planets in the temperate habitable zone (HZ) of the close-by cool star TRAPPIST-1 the question of whether such planets could also harbour life arises. Potentially habitable planets around red dwarf stars can orbit in radiation environments that could cause life-sterilizing surface radiation events. UV flares from these stars are more frequent and intense than solar flares. In addition, their temperate HZs are at closer separations from the star. Here we show UV surface environment models for planets in the HZ of TRAPPIST-1 and explore the implications for life. TRAPPIST-1 has high X-ray/EUV activity, placing planetary atmospheres at risk from erosion over time. If a dense Earth-like atmosphere with a protective ozone layer exists on planets in the HZ of TRAPPIST-1, UV surface environments would be similar to Earth. However an anoxic atmosphere, or an eroded thinner atmosphere, would allow more UV to reach the surface, making surface environments hostile even to highly UV-tolerant terrestrial extremophiles. If future observations detect ozone in the atmospheres of any of the planets in the HZ of TRAPPIST-1, these would be interesting targets for the search for life. We anticipate our assay to be a starting point for in-depth exploration of stellar and atmospheric observations of the TRAPPIST-1 planets to constrain their UV-surface-habitability.
Article
Astrobiology strives to increase our knowledge on the origin, evolution and distribution of life, on Earth and beyond. In the past centuries, life has been found on Earth in environments with extreme conditions that were expected to be uninhabitable. Scientific investigations of the underlying metabolic mechanisms and strategies that lead to the high adaptability of these extremophile organisms increase our understanding of evolution and distribution of life on Earth. Life as we know it depends on the availability of liquid water. Exposure of organisms to defined and complex extreme environmental conditions, in particular those that limit the water availability, allows the investigation of the survival mechanisms as well as an estimation of the possibility of the distribution to and survivability on other celestial bodies of selected organisms. Space missions in low Earth orbit (LEO) provide access for experiments to complex environmental conditions not available on Earth, but studies on the molecular and cellular mechanisms of adaption to these hostile conditions and on the limits of life cannot be performed exclusively in space experiments. Experimental space is limited and allows only the investigation of selected endpoints. An additional intensive ground based program is required, with easy to access facilities capable to simulate space and planetary environments, in particular with focus on temperature, pressure, atmospheric composition and short wavelength solar ultraviolet radiation (UV). DLR Cologne operates a number of Planetary and Space Simulation facilities (PSI) where microorganisms from extreme terrestrial environments or known for their high adaptability are exposed for mechanistic studies. Space or planetary parameters are simulated individually or in combination in temperature controlled vacuum facilities equipped with a variety of defined and calibrated irradiation sources. The PSI support basic research and were recurrently used for pre-flight test programs for several astrobiological space missions. Parallel experiments on ground provided essential complementary data supporting the scientific interpretation of the data received from the space missions.
Article
Full-text available
Twenty-six strains of black, mostly meristematic fungi isolated from cryptoendolithic lichen dominated communi-ties in the Antarctic were described by light and Scanning Electron Microscopy and sequencing of the ITS rDNA region. In addition, cultural and temperature preferences were investigated. The phylogenetic positions of species recognised were determined by SSU rDNA sequencing. Most species showed affinity to the Dothideomycetidae and constitute two main groups referred to under the generic names Friedmanniomyces and Cryomyces (gen. nov.), each characterised by a clearly distinct morphology. Two species could be distinguished in each of these genera. Six strains could not be assigned to any taxonomic group; among them strain CCFEE 457 belongs to the Hysteriales, clustering together with Mediterranean marble-inhabiting Coniosporium species in an approximate group with low bootstrap support. All strains proved to be psychrophiles with the only exception for the strain CCFEE 507 that seems to be mesophilic-psychrotolerant. All had very thick melanised cell walls, the ability to produce exopolysaccharides and to grow meristematically. They are thought to be well adapted to the harsh environment of the Antarctic cold Desert. Hypotheses concerning their origin and evolution are put forward. Taxonomic novelties: Cryomyces antarcticus Selbmann, de Hoog, Mazzaglia, Friedmann & Onofri gen. sp. nov., C. minteri Selbmann, de Hoog, Mazzaglia, Friedmann & Onofri sp. nov., Friedmanniomyces simplex Selbmann, de Hoog, Mazzaglia, Friedmann & Onofri sp. nov.
Article
Full-text available
We review the radiometric ages of the 16 currently known Martian meteorites, classified as 11 shergottites (8 basaltic and 3 lherzolitic), 3 nakhlites (clinopyroxenites), Chassigny (a dunite), and the orthopyroxenite ALH84001. The basaltic shergottites represent surface lava flows, the others magmas that solidified at depth. Shock effects correlate with these compositional types, and, in each case, they can be attributed to a single shock event, most likely the meteorite’s ejection from Mars. Peak pressures in the range 15 – 45 GPa appear to be a “launch window”: shergottites experienced ~ 30 – 45 GPa, nakhlites ~ 20 ± 5 GPa, Chassigny ~35 GPa, and ALH84001 ~35 – 40 GPa. Two meteorites, lherzolitic shergottite Y-793605 and orthopyroxenite ALH84001, are monomict breccias, indicating a two-phase shock history in toto: monomict brecciation at depth in a first impact and later shock metamorphism in a second impact, probably the ejection event.
Article
The possibility and probability of natural transfer of viable microbes from Mars to Earth and Earth to Mars traveling in meteoroids during the first 0.5 Ga and the following 4 Ga are investigated, including:
Article
Orbital histories of ejecta from the terrestrial planets were numerically integrated to study their transfer to Earth. The properties of the lunar and martian meteorites are consistent with a recurrent ejection of small meteoroids as a result of impacts on their parent bodies. Long-range gravitational effects, especially secular resonances, strongly influence the orbits of many meteoroids, increasing their collision rates with other planets and the sun. These effects and collisional destruction in the asteroid belt result in shortened time scales and higher fluxes than previously believed, especially for martian meteorites. A small flux of mercurian ejecta appears possible; recovery of meteorites from the Earth and Venus is less likely.
Article
Shock recovery experiments were performed with an explosive set-up in which three types of microorganisms embedded in various types of host rocks were exposed to strong shock waves with pressure pulse lengths of lower than 0.5 ls: spores of the bacterium Bacillus subtilis, Xanthoria elegans lichens, and cells of the cyanobacterium Chroococcidiopsis sp. 029. In these experiments, three fundamental parameters were systematically varied (1) shock pressures ranging from 5 to 50 GPa, (2) preshock ambient temperature of 293, 233 and 193 K, and (3) the type of host rock, including nonporous igneous rocks (gabbro and dunite as analogs for the Martian shergottites and chassignites, respectively), porous sandstone, rock salt (halite), and a clay-rich mineral mixture as porous analogs for dry and water-saturated Martian regolith. The results show that the three parameters have a strong influence on the survival rates of the microorganisms. The most favorable conditions for the impact ejection from Mars for microorganisms would be (1) low porosity host rocks, (2) pressures <10–20 GPa, and (3) low ambient temperature of target rocks during impact. All tested microorganisms were capable of surviving to a certain extent impact ejection in different geological materials under distinct conditions.
Article
Abstract— We investigated the transfer of meteorites from Mars to Earth with a combined mineralogical and numerical approach. We used quantitative shock pressure barometry and thermodynamic calculations of post-shock temperatures to constrain the pressure/temperature conditions for the ejection of Martian meteorites. The results show that shock pressures allowing the ejection of Martian meteorites range from 5 to 55 GPa, with corresponding post-shock temperature elevations of 10 to about 1000 °C. With respect to shock pressures and post-shock temperatures, an ejection of potentially viable organisms in Martian surface rocks seems possible. A calculation of the cooling time in space for the most highly shocked Martian meteorite Allan Hills (ALH) 77005 was performed and yielded a best-fit for a post-shock temperature of 1000 °C and a meteoroid size of 0.4 to 0.6 m. The final burial depths of the sub-volcanic to volcanic Martian rocks as indicated by textures and mineral compositions of meteorites are in good agreement with the postulated size of the potential source region for Martian meteorites during the impact of a small projectile (200 m), as defined by numerical modeling (Artemieva and Ivanov 2004). A comparison of shock pressures and ejection and terrestrial ages indicates that, on average, highly shocked fragments reach Earth-crossing orbits faster than weakly shocked fragments. If climatic changes on Mars have a significant influence on the atmospheric pressure, they could account for the increase of recorded ejection events of Martian meteorites in the last 5 Ma.