Abstract– Even in the absence of any biosphere on Mars, organic molecules, including polycyclic aromatic hydrocarbons (PAHs), are expected on its surface due to delivery by comets and meteorites of extraterrestrial organics synthesized by astrochemistry, or perhaps in situ synthesis in ancient prebiotic chemistry. Any organic compounds exposed to the unfiltered solar ultraviolet spectrum or oxidizing surface conditions would have been readily destroyed, but discoverable caches of Martian organics may remain shielded in the subsurface or within surface rocks. We have studied the stability of three representative polycyclic aromatic hydrocarbons (PAHs) in a Mars chamber, emulating the ultraviolet spectrum of unfiltered sunlight under temperature and pressure conditions of the Martian surface. Fluorescence spectroscopy is used as a sensitive indicator of remaining PAH concentration for laboratory quantification of molecular degradation rates once exposed on the Martian surface. Fluorescence-based instrumentation has also been proposed as an effective surveying method for prebiotic organics on the Martian surface. We find the representative PAHs, anthracene, pyrene, and perylene, to have persistence half-lives once exposed on the Martian surface of between 25 and 60 h of noontime summer UV irradiation, as measured by fluorescence at their peak excitation wavelength. This equates to between 4 and 9.6 sols when the diurnal cycle of UV light intensity on the Martian surface is taken into account, giving a substantial window of opportunity for detection of organic fluorescence before photodegradation. This study thus supports the use of fluorescence-based instrumentation for surveying recently exposed material (such as from cores or drill tailings) for native Martian organic molecules in rover missions.
Mars may have provided in its early history surface environmental conditions conducive for an independent origin of life. Refuges of surficial microbial life may persist today, or at least pockets of dead microbial cells and the organic compounds produced by their degradation. Even in the absence of biology on Mars, organic molecules would be expected on the surface from delivery from space.
Many organic molecules are now known to be produced by astrochemistry in the interstellar medium and circumstellar regions (Herbst and van Dishoeck 2009), and become incorporated in the planet-forming disks of new star systems (Shaw 2007). Organic compounds are common in certain kinds of meteorites, the carbonaceous chondrites, as well as comets (Ehrenfreund and Charnley 2000), and so extraterrestrial delivery aboard micrometeorites, meteorites, asteroids, and comets could have been a significant determinant of the organic inventory of the early Earth and Mars (Pierazzo and Chyba 1999), and continue to deliver organics to the Martian surface today. Carbonaceous chondrites are rich in a diverse repertoire of organic molecules of importance to life (Pizzarello 2006), including amino acids, carboxylic acids, aliphatic and aromatic hydrocarbons, alcohols, aldehydes, ketones, sugars (see reviews in Botta and Bada 2002; Sephton 2002; and Martins 2011), as well as purine and pyrimidine nucleobases (Martins et al. 2008). The total current annual arrival of unaltered organic material to the Martian surface (which has not been thermally degraded by atmospheric entry or impact) has been estimated to be around 2.4 × 105 kg/yr, and if this accretion rate were to have been constant over the history of the solar system, Mars would have received an amount of extrinsic carbon greater than the terrestrial biomass (Flynn 1996).
Despite this presumed long-term in-fall of diverse extrinsic organic molecules, no organics have yet been discovered. The Viking GC-MS experiments failed to detect organics in their samples of heated soil (Biemann et al. 1977). It has therefore been long believed that delivered organic material is destroyed on the Martian surface, probably by chemical reactivity of the soil itself (Quinn and Zent 1999; Benner et al. 2000; Yen et al. 2000; ten Kate 2010). Organics protected from oxidization chemistry and solar ultraviolet radiation, perhaps inside surface rocks, within permanently shadowed overhangs or caves, or deeper in the subsurface, may persist on Mars, and represent an enticing target for detection instrumentation on Martian lander and rover missions.
Fluorescence-Based Instrumentation for Detecting Martian Organics
One category of molecules that is of particular interest to the possibility of detecting organics on Mars is the polycyclic aromatic hydrocarbons (PAHs). PAHs are common in the interstellar medium and star-forming regions, as well as comets and carbonaceous chondrite meteorites (Herbst and van Dishoeck 2009). Botta and Bada (2002) summarize the abundance of different meteoritic organic compounds, and report concentrations of over 1000 ppm of aromatic hydrocarbons in carbonaceous chondrites. PAHs have also already been detected in Martian material; in the shergottite meteorites EETA79001 and ALH 84001 (Botta et al. 2008), rocks which formed on Mars before being ejected by an impact. PAHs are also commonly formed by biological degradation, such as found in terrestrial oil deposits, and the debate continues as to whether the PAH deposits within ALH 84001 (Clemett et al. 1998) represent decay products of Martian organisms (McKay et al. 1996; Becker et al. 1999; Gibson et al. 2001). Aliphatic hydrocarbons and PAHs may also have been synthesized in situ on Mars by Fischer-Tropsch type reactions of hydrogen- and carbon-monoxide-rich volcanic and impact gasses or hydrothermal fluids (Zolotov and Shock 1999). However, the expected PAHs, or indeed any organic molecules, have not yet been detected in situ on the Martian surface.
In addition to representing a promising molecular target from prebiotic chemistry or even microbial decay, PAHs are highly fluorescent. PAHs exhibit such intrinsic fluorescence because the delocalized pi-orbital electrons within the aromatic rings are readily excited, and this energy is reemitted as fluorescence with a high quantum efficiency, as the rigid molecular structure does not allow for efficient vibrational relaxation. The fluorescent emission spectra can also be distinctively characteristic of particular PAHs, depending upon the number and arrangement of aromatic rings (Howerton et al. 2002). This sensitivity combined with discriminatory power has allowed the development of fluorescence-based instrumentation for applications such as detecting low levels of oil-derived PAH pollutants in seawater (Rudnick and Chen 1998) or PAH-contaminants in soil (Ko et al. 2003).
If a Mars exploration mission is to detect localizations of organics, they must have been protected from solar UV. Whilst protection from direct insolation is provided by shadowed overhangs, calculated by Moores et al. (2007) to offer UV flux reduction down to around 2 × 10−5 that of exposed regions, atmospheric scattering of UV radiation means that even permanently shadowed areas accumulate large doses of UV over geological periods. Detection of Martian organics can be optimized by examining previously shielded material freshly uncovered by the probe. A rock abrasion tool (RAT) such as carried by the Mars Exploration Rovers Spirit and Opportunity (Gorevan et al. 2003), the rock coring drill on Mars Science Laboratory (Okon 2010) and the 2 m subsurface drill proposed for ExoMars-C (Vago et al. 2006) are all appropriate devices for this. Once exposed to the unfiltered solar UV spectrum on the Martian surface, however, any PAHs will be readily photodegraded and their fluorescence signal lost. So the key question for the detection of PAHs and other aromatic prebiotic organic molecules is: on what time scale are they destroyed by solar UV once uncovered? What is the window of opportunity for detection by instrumentation aboard a rover?
Previous exposure experiments under Martian surface conditions have been conducted on simple organic molecules to assess ultraviolet photostability (ten Kate et al. 2005, 2006; Garry et al. 2006; Peeters et al. 2009; Stalport et al. 2009). Here, we conduct an assessment of the photostability of three PAHs, anthracene, pyrene, and perylene; representative of PAHs with three, four, and five aromatic rings, respectively (see molecular structures shown in Fig. 1). These compounds are significant both due to their expected prevalence on Mars and possibility for detection through fluorescence.
The fluorescence response from a target can be quantitatively described by the generation of an excitation-emission matrix (EEM). Briefly, an EEM is created by recording the fluorescent emission spectrum from an experimental sample across a range of excitation wavelengths, and plotting the fluorescence intensity produced at each excitation-emission wavelength combination as a contour map. Figure 1 displays EEMs of the three PAHs considered here. For further details on the production of EEMs, see the fluorescence spectroscopy methodology presented in Dartnell et al. (2010). Figure 1 shows the peak excitation wavelengths thus determined for each PAH (indicated with horizontal solid lines), as used in this study to track the UV-induced degradation of PAHs under Martian surface conditions. Dashed horizontal lines in Fig. 1 indicate other wavelengths available from commercial laser diode and LED (which can have full width at half maximum spectral spreads of around ±10 nm) light sources, as explained further in the Discussion section.
In this study, three representative polycyclic aromatic hydrocarbons (PAHs) are doped onto mineral grains and exposed to ultraviolet radiation simulating the unfiltered Martian sunlight, under temperature and pressure conditions emulating the Martian surface environment, to quantify their photostability once uncovered on the Martian surface. Fluorescence spectroscopy is used as a sensitive indicator of the degree of PAH photodestruction over time, and emulation of fluorescence-based instrumentation for detection of Martian aromatic organics.
Samples of mineral grains were experimentally doped with PAH as follows. Glass microscope slides were cleaned with 70% ethanol. Peridotite mineral grains of the size fraction 250–500 μm were fixed onto the glass slides in dense circles 1 cm in diameter using UN1133 all purpose clear adhesive (Everbuild, Leeds, UK), 3 spots per slide. The grains were fixed atop the patch of adhesive so UV-shielding by the glue itself is not an issue. Prior blanks tests had determined that neither peridotite grains nor the glue used to fix them to the glass slides, nor the solvents methanol or methylene chloride, exhibited any detectable fluorescence of their own (data not shown here).
Analytical standard samples of three PAHs, anthracene, pyrene, and perylene, had been purchased in 1 mL ampoules (Sigma-Aldrich). Working in a fume hood, PAHs were diluted to a concentration of 40 μg/mL using the same organic solvent that the PAHs had been supplied in (anthracene: methanol; pyrene and perylene: methylene chloride). Twenty microliters of PAH was pipetted uniformly onto each of the three mineral grain spots on a glass slide, with one PAH type per slide. The solvent was allowed to rapidly evaporate in the fume hood to leave the PAH samples adhered to the surface of the peridotite grains. Each PAH was subjected to a series of five increasing exposures (see below), and in addition, a control slide of three doped grain spots was prepared, but not exposed to the Mars chamber or UV irradiation. In total, therefore, six sample slides (eighteen doped mineral spots) were prepared for each of the three PAHs.
Thus, sample preparation deposited 0.8 μg (20 μL of 40 μg/mL solution) of PAH uniformly across the peridotite grain spots. This quantity of PAH was selected for doping because pilot experimentation had determined that it produced a strong fluorescence, and without any of the three PAHs saturating the detector (see the Fluorescence Spectroscopy section). Doped mineral samples were stored overnight at room temperature before being transported to the exposure facility.
UV exposures were conducted in the Mars chamber operated by the Open University, Milton Keynes, UK. Sample slides were placed two at a time onto a packed bed of dry ice (−79 °C) within the chamber, which was then sealed and evacuated to a pressure of 6 mbar. This exposed the samples to a temperature and pressure regime representative of the Martian surface. Sublimation of the dry ice occurred in the evacuated chamber, but the low pressure was maintained by the pump and the packed bed refreshed between sample runs. Illumination by a xenon lamp through a quartz top window provided the UV flux. On each glass slide, two PAH-doped mineral spots were exposed to the UV source above. The third spot was designated as control and shielded from the UV flux with aluminum foil, whilst still exposed to the low temperature and pressure regime within the chamber. The experimental set-up is shown in Fig. 2.
The xenon lamp produces a UV emission spectrum closely matching that modeled for the unfiltered sunlight incident on the Martian equatorial surface at noon during northern summer (Ls = 90°) and nominal atmospheric dust loading (Patel et al. 2002), and at a flux rate calibrated to be ten times greater, as shown in Fig. 3. This experimental protocol thus provided a faithful reproduction of both the physical conditions of the Martian surface and spectrally matched solar irradiance, while allowing accelerated experimental exposure times. One sample slide, consisting of two experimental doped grain spots and one control spot, of each PAH type was exposed within the Mars chamber for a given period of time. The experimental UV exposure times used (and their Martian equivalent exposure times) were: 6 min (1 h Mars surface equivalent), 30 min (5 Mars hours), 1 h (10 Mars hours), 2 h (20 Mars hours), and 3 h (30 h equivalent).
After timed exposure, samples were analyzed for their fluorescence response.
The fluorescent emission of samples was measured using a Perkin Elmer LS55 Fluorescence Spectrometer (Perkin Elmer, Cambridge, UK; L2250107). This instrument consists of a pulsed xenon arc lamp light source, excitation and emission scanning monochromators, and a photomultiplier tube (PMT) detector.
A remote fiber-optic accessory (Perkin Elmer; L2250144) was used to measure fluorescence from the solid surface of the doped mineral samples. This attachment uses bifurcated fused silica fiber optics to pass excitation light from the xenon source to the sample surface, and also fluorescent emission from the sample to the detector, down two halves of the same cable. The head of the fiber-optic cable was positioned 8 mm above the surface of the mineral grains; the distance that had been found to be optimal for surface fluorescence measurements. A blackout curtain was used to isolate the sample and fiber-optic head from ambient light in the laboratory. Precise targeting of the fiber-optic attachment onto the mineral spot was achieved with the selection of the visible wavelength of 500 nm (green), before changing to the short wavelength excitation light.
FL WinLab software (Perkin Elmer; B8011050) was used to control the spectrometer, setting the desired excitation wavelength and recording the emission spectrum over a set wavelength range. Emission spectra between 240 and 600 nm were recorded at 50 nm/min scan speed with an excitation slit width of 8 nm and emission slit width of 5 nm. Raw data were processed using analysis code written by the first author in Mathematica 8 (Wolfram).
The fluorescent response from each doped sample was measured at two peak excitation wavelengths appropriate to the PAH. Figure 1 shows the EEM generated for each of the three PAHs, with the corresponding peak excitation wavelengths indicated with dashed lines. In addition, fluorescence was measured from excitation wavelengths relevant to available LEDs or laser diodes that could provide excitation light for a fluorescence-based instrument. The available wavelengths relevant to excitation of anthracene, pyrene, or perylene are 266 nm (achieved by frequency-doubling a green 532 nm laser), 365, 375, and 405 nm. The excitation wavelengths selected for the three PAHs are listed in Table 1.
Table 1. Excitation wavelengths used for the three PAH samples.
Wavelengths listed in bold correspond to the peak excitation, as determined from the EEMs shown in Fig. 1. Other wavelengths correspond to those available from commercial LED and laser diode sources.
Each PAH-doped peridotite grain spot was measured three times with repositioning of the fiber-optic head in a triangular pattern over the spot, as described above. Thus, for each excitation wavelength of interest, both independent experimental samples were measured in triplicate, and the control sample was also measured in triplicate.
The time between deposition of the PAH samples, UV exposure, and fluorescence analysis was no longer than 72 h. Pilot experimentation had verified that loss of PAHs to volatilization at room temperature and pressure did not occur over this time frame.
Figure 4, left column, shows the fluorescence emission spectra of the three PAHs considered here, anthracene (top row), pyrene (middle), and perylene (bottom). All spectra have been plotted on the same emission wavelength and intensity scale to allow comparison. Each spectrum has been cropped to exclude the scattered excitation light and its harmonics, and represents an average over the three unexposed control samples, each measured in triplicate. In each case, the blue emission spectrum corresponds to the shorter wavelength excitation maximum, and the red spectrum that induced by the longer wavelength excitation used. These two peak excitation wavelengths for each PAH are indicated with solid horizontal lines in the EEMs displayed in Fig. 1, and are listed in bold in Table 1. The vertical shaded bars in Fig. 4 indicate the peak emission wavelength, ±1 nm, and are the range of values over which the fluorescent emission is averaged.
The right column of Fig. 4 shows the peak fluorescence intensity measured for the control samples after increasing periods exposed to Martian surface temperature and pressure (but not UV irradiation), normalized to the mean of the three control samples unexposed to simulated Martian conditions, and plotted on a log scale (i.e., log[N/N0]). Errors bars, calculated as plus and minus the standard error of the measurements, are plotted but on the log scale are generally obscured by the data points themselves. Fluorescence measurements from both short and long wavelength excitation (see left column) are indicated with blue and red color-coded data points, respectively. These controls have been exposed to the simulated temperature and pressure regime of the Martian surface for the indicated period, but not the ultraviolet illumination (shielded beneath aluminum foil). It can be seen that, as expected, the anthracene and pyrene deposited samples show no detectable reduction after up to 3 h exposure to 6 mbar pressure at −79°C. The perylene control samples do, however, exhibit a slight decrease. The gradient of this trend, fitted to fluorescence measurements from both excitation wavelengths, is −0.00445 (SE = 0.00114). This trend is accounted for in the analysis of the UV-exposed experimental samples of perylene, as explained below.
Figure 5 displays the change in fluorescence emission intensity as a function of the Martian-equivalent hours of UV exposure under simulated Martian conditions. These Martian-equivalent exposure times are calculated for an equatorial region at local noon during northern summer, with a nominal atmospheric dust loading (using the model reported in Patel et al. 2002), and will be covered further in the Discussion section. As with Fig. 4, the log fluorescence scale is normalized to the averaged emission recorded from the three controls (each measured in triplicate) unexposed to UV or Martian environmental conditions. Data are presented for two independent experimental samples, each measured in triplicate, and each analyzed at two peak excitation wavelengths (see Fig. 4). Samples and excitation wavelengths are coded as explained in the figure caption. A best-fit trend line is calculated for each of the four data sets measured for each PAH. The mean of these fitted trend lines is displayed in Fig. 5, along with the range defined by the standard error of these estimates. Table 2 summarizes the parameters of these fitted trend lines of PAH degradation. As explained above, the perylene control samples show a slight decrease in fluorescence signal with duration exposed to the low pressure and low temperature experimental conditions. The fitted exponent for perylene degradation with UV exposure shown in Table 2 has had this control exponent subtracted, and the standard errors have been summed.
Table 2. The calculated UV-degradation rates of PAH fluorescence, listing the mean exponent of the fitted trends to the four data sets and the standard error of this measure.
Half-life (Mars-equivalent hours)
Time to 10% remaining signal (hours)
Also shown are calculations of the half-life of decreasing PAH fluorescence, and the total duration of exposure required to diminish fluorescent emission to 10% of the initial intensity. These times are based on the modeled equatorial noontime flux during northern summer, and so actual persistence times will be longer, as explained in the Discussion section. *The fitted exponent displayed here for perylene has already had the decreasing trend observed in the control samples (Fig. 4) removed, and the standard errors summed.
Measurements of the decrease in fluorescence intensity were also made at wavelengths other than the peak excitations for the different PAHs, appropriate to the emission wavelengths of available LED and laser diode light sources. These additional wavelengths were 365 nm for anthracene and 266, 265, 375 nm for perylene (the excitation peak of pyrene fortuitously lies on the available laser diode wavelength of 266 nm), as illustrated in Fig. 1 with dashed lines. Figure 6 displays the results of degrading fluorescence signal with period of UV exposure on the Martian surface for these excitation wavelengths. As with Fig. 4, the mean trend line fitted to the data is shown, along with the region defined by the standard error of the results.
Table 3 summarizes the parameters of these fitted trend lines of PAH fluorescent signal loss, when excited at these alternative wavelengths. Again, the decrease in signal from perylene control samples has been removed from these perylene fitted exponents, and the standard errors summed.
Table 3. The calculated UV-degradation rates of PAH fluorescence, as measured at the indicated excitation wavelength of relevance to commercially available LED and laser diode light sources.
Half-life (Mars-equivalent hours)
Time to 10% remaining signal (hours)
The table lists the mean exponent fitted to the data recorded from both experimental samples, and the standard error of this measure. Also shown are calculations of the half-life of decreasing PAH fluorescence, and the total duration of exposure required to diminish fluorescent emission to 10% of the initial intensity. These times are based on the modeled equatorial noontime flux during northern summer, and so actual persistence times will be longer, as explained in the Discussion section. *The fitted exponents displayed here for perylene have already had the decreasing trend observed in the control samples (Fig. 4) removed, and the standard errors summed.
Anthracene; 365 nm
Perylene; 266 nm*
Perylene; 365 nms*
Perylene; 375 nm*
Organic molecules are expected on the Martian surface, even in the absence of biology, through compounds synthesized by astrochemistry and delivered by meteoritic and cometary infall, as well as remnants of in situ Martian prebiotic chemistry. Many of these prebiotic molecular targets contain aromatic moieties and so exhibit fluorescent emission when excited. A large class of such compounds are the polycyclic aromatic hydrocarbons, PAHs, which are found in abundance in the interstellar medium, within carbonaceous chondrite meteorites, and also in meteorite samples of the Martian surface such as ALH 84001.
Organic compounds are yet to be detected on the Martian surface, and it has been proposed to exploit the fluorescence emission from molecules with aromatic moieties as a means to survey for assemblages of organic molecules on Mars. Such a fluorescence-based surveying instrument would identify promising target locations for the first detection of organics with other more discriminatory instruments, and possibly also reveal niches of relic life.
The intense ultraviolet component of unfiltered Martian sunlight, however, would be expected to photobleach fluorescence and ultimately photolyse and destroy exposed target compounds (Cockell et al. 2005; ten Kate et al. 2005, 2006; Garry et al. 2006; Peeters et al. 2009; Stalport et al. 2009). Organic molecules may persist on Mars, shielded from solar UV inside rocks or in the subsurface, but will face degradation as soon as they become exposed to the unfiltered sunlight. After uncovering fresh Martian samples, with a rock abrasion tool or subsurface drill, for example, there is therefore a limited window of opportunity to survey for the presence of fluorescent organic compounds and decide whether to employ more discriminatory, but resource-limited, instruments. The crucial question, therefore, is what is the photostability of these PAH target molecules—what is the rate of loss of the fluorescence signal once exposed to Martian sunlight?
The study reported here addresses this key unknown. Three representative PAH compounds, anthracene, pyrene, and perylene (3-, 4-, and 5-ring PAHs, respectively, as shown in Fig. 1), were selected and the remaining fluorescence signal quantified at a variety of excitation wavelengths after increasing periods of exposure to simulated Martian UV flux under emulated surface conditions of cold and low pressure atmosphere. These particular PAH compounds were chosen because they are common components of the organic inventory within carbonaceous chondrites and are also fluorescent, making them promising targets for detection on Mars.
The fluorescence spectra taken of the control samples (three samples of each PAH, each measured in triplicate) shown in Fig. 4 were used to normalize the remaining signal plotted in Figs. 5 and 6. From the intensity of the fluorescence peaks shown in Fig. 4, left column, it can be seen that perylene adhered onto peridotite grains is approximately 3.5 times more intrinsically fluorescent than anthracene, and 30% more intense than pyrene, as measured at their peak excitation and emission. It is also worth noting that perylene, the largest PAH considered here, comprised of 5 aromatic rings (see Fig. 1), exhibits both the longest peak excitation and emission wavelength.
The plots in the right-hand column of Fig. 4 track the fluorescence signal over 3 h of exposure to the simulated Martian surface conditions of 6 mbar atmospheric pressure at −79 °C, but shielded from UV radiation. Whilst anthracene and pyrene samples are very stable over this period, perylene does show a slight loss in signal. The effect of this decrease over time is simple to remove from the UV-exposed experimental perylene sample data, as described in the Results section. Whilst this control correction does increase the standard error of the estimate, it is still clear that the perylene fluorescent signal can persist for a significant duration once exposed on the Martian surface, as discussed in greater depth below.
This observed fluorescence signal decrease in the perylene control samples unexposed to UV is believed to be due to the slow volatilization of the small organic molecules off the surface of the mineral grains under low atmospheric pressure. The fact that out of all the UV shielded control samples perylene shows the most reduction is a surprise. Perylene has the highest molecular weight of the three representative PAHs tested here, and so would be expected to be the least volatile. However, such low molecular weight aromatics are found in abundance in carbonaceous chondrite meteorites, after very long-term exposure to the vacuum of space, and so their long-term stability in the environmental conditions of the Martian surface is not under question. Inside carbonaceous meteorites, the prevalence of intramolecular bonds within the complex assemblage of organics, including much larger and refractory molecules and a cross-linked matrix of macromolecules making up the “kerogen-like” material (Botta and Bada 2002), would thus serve to stabilize the lower molecular weight species against volatilization. In this experimental set-up, PAHs were adhered onto mineral grains from pure solution; a necessary simplification to allow quantification of the degradation rate of each compound. In the Martian environment, aromatic prebiotic compounds, either synthesized in situ or the products of astrochemistry delivered aboard meteorites, would be present in much more complex, mixed assemblages, and so be much less susceptible to volatilization than the pure samples considered here.
In any case, the UV degradation rates quantified by excitation at the peak wavelengths, plotted in Fig. 5 and the fitted exponents summarized numerically in Table 2, show a clear result. All three representative PAH compounds considered here are demonstrated to exhibit a detectable degradation in fluorescent signal over the 30 h of simulated Martian surface UV exposure. The half-life of this declining fluorescence ranges from about 25 to 60 h. The photostabilities of anthracene and pyrene are measured here to be very similar, and this result is corroborated by Jochims et al. (1999) who experimentally determined a photostability index for a range of PAHs under conditions of the interstellar medium, and also found anthracene and pyrene to exhibit near-identical rates. By way of comparison, Ram and Anastasio (2009) experimentally determined the photostability of PAHs exposed to simulated sunlight in arctic snow. They calculated that in surface snow at midday on the summer solstice at Summit, Greenland, the photodegradation half-life of pyrene is just over 40 min. Whilst the UV flux at Greenland is less than on the Martian surface, Ram and Anastasio (2009) irradiated at warmer temperatures (−2.4 to −11 °C) and with the PAH molecules within water ice (not adhered on dry mineral grains, as with this current study) and so they were additionally subject to degradation from hydroxyl radicals.
Multiple samples were irradiated to ensure a high degree of accuracy on these fitted trend lines. If these measured trends do continue to higher total UV doses, pyrene emission is down to only 10% of its initial value after around 90 h of Martian sunlight, and perylene after around 200 h.
These results on degradation rates of PAHs under UV irradiation and simulated Martian surface environmental conditions are comparable to similar previous studies on the photostability of organic molecules on Mars. ten Kate et al. (2005) subjected thin films of amino acids to Mars-like UV flux levels and discovered that the photodecomposition half-life of glycine is 22 ± 5 h and that of D-alanine is 3 ± 1 h. The difference between the degradation of these two amino acids is believed to be due to the rate-limiting step of the free radical chemistry driven by absorption of a UV photon (ten Kate et al. 2005). However, when these room-temperature experiments were repeated simulating a Martian surface temperature of 210 K (−63 °C), as this current study has done, the UV destruction rate for glycine were found to decrease by a factor of 7, as expected from slower reaction kinetics at low temperatures (ten Kate et al. 2006). Stalport et al. (2009) exposed carboxylic acids to Mars-like ultraviolet irradiation under cold conditions of −55 °C. They found that the mass loss of mellitic acid reached 50% after approximately 25 h exposure. Benzoic and oxalic acids were discovered to be much more photosensitive, exhibiting mass loss half-lives of 0.8 ± 0.2 h and 1.8 ± 0.5 h, respectively. Schuerger et al. (2008) deposited ATP onto a simulated spacecraft surface and exposed to Martian surface conditions and UV flux and found a degradation half-life of around 40 Martian sols at −80 °C. Looking at more complex, exclusively biological molecules, Cockell et al. (2005) found that autofluorescence from the photosynthetic pigments (phycobiliproteins and chlorophyll a) of the cyanobacterium Chroococcidiopsis sp. 029 was diminished to 1% by 4 h of exposure to Martian UV flux.
Illuminating the samples with the appropriate excitation peak wavelength is the most sensitive fluorescence method for assessing PAH degradation with UV exposure, but this study also analyzed fluorescence emission excited by other, non-optimal, wavelengths for the PAHs. The design of an instrument for the detection of fluorescent organic molecules may dictate the use of a single excitation wavelength that is not optimal for all potential targets. However, even at a suboptimal wavelength for an organic molecule target, fluorescence may still be detectable if the excitation light source is intense, such as from a laser diode or LED at close range. The available LED or laser diode wavelengths examined were 266, 365, 375, and 405 nm, and it is worth stressing at this point that each of the PAHs studied here are optimally excited at an available wavelength (anthracene, 375 nm; pyrene, 266 nm; perylene, 405 nm; as shown in Table 1).
Decrease in the fluorescent signal may not be uniform across the emission feature, and it is important to verify the signal decrease from the other, non-optimal, excitation wavelengths for each PAH. Figure 6 and Table 3 display the results on the decrease in fluorescence when excited at these alternative wavelengths. More variability in the degradation rate is seen with these non-optimal excitation wavelengths, with calculated half-lives ranging from 37 h (perylene excited at 266 nm) to over 250 h (perylene excited at 375 nm). This indicates that the degradation of fluorescence from UV exposure is not uniform across the excitation-emission parameter space, with some regions of the fluorescent feature diminishing faster than others. Importantly, however, even exciting at a wavelength non-optimal for these PAHs the UV degradation rates are low enough that there is a significant window of opportunity for detection after exposure of the material to Martian sunlight.
The resounding result from these experimental is that although a decrease in the fluorescence signal of all three tested PAHs is detectable after 30 h of simulated exposure on the Martian surface, this signal decrease is not overwhelming over time scales of relevance to the surface operations of a robotic rover. If a rover is able to expose fresh material on the surface, either by rock abrasion tool or subsurface drill, it has a window of opportunity of at least 10 h to survey for fluorescence from any native organics.
These Mars-equivalent exposure times were calculated for equatorial midday during northern summer with a nominal atmospheric dust loading (using the model reported in Patel et al. 2002). As the solar zenith angle varies over the course of a day on Mars, the actual instantaneous UV exposure rate will generally be less than this. Consequently, the number of Martian sols before PAH fluorescence diminishes to 50% or 10% is not simply a twelfth of the number of hours listed in Tables 2 and 3. Figure 7 plots the instantaneous UV flux rate at an equatorial latitude and during northern summer with an atmospheric opacity due to dust loading of 0.2, representing a realistic nominal case for exposure experiments.
The UV dose rate can be seen to peak at around 33 W/m2/nm at local noon, but rapidly drops off earlier in the morning and later in the afternoon. Integrating across a complete diurnal cycle, with the instantaneous UV flux changing as shown in Fig 7, defines the total Mars daily UV dose (200–400 nm) to be around 872,000 J/m2 (to 3 significant figures) (Patel et al. 2002, 2004).
This allows the calculation of a more meaningful time conversion for exposures on the Martian surface. Every Mars equivalent hour of UV irradiation at equatorial summer noontime flux (corresponding to 6 min of experimental irradiation in this set-up), as listed in Tables 2 and 3, is equivalent to 0.16 sols of the total flux averaged over the diurnal cycle.
This relationship between experimental exposure doses and actual UV fluxes over the day-night cycle on Mars is important to appreciate and account for in laboratory studies of the effects of unfiltered Martian sunlight.
The half-lives of fluorescent signal degradation of the PAHs anthracene, pyrene and perylene listed in Table 2, ranging between around 25 and 60 h of irradiation at noontime flux levels, thus actually equate to half-lives between 4 and 9.6 Martian sols when the full diurnal cycle is considered. It is therefore comfortably within the operational scope of robotic rovers to uncover caches of Martian organics, previously shielded either in the subsurface regolith or within surface rocks, and survey for indicative fluorescence before the freshly exposed compounds are photodegraded. Such an exploratory program would obviously be most effective if drilling by day, and then testing the uncovered material for a fluorescent signal at dusk or early the following morning. This strategy optimizes both the persistence of exposed organic molecules and the detectable fluorescence signal in low ambient light.
A more complete simulation of the situation will involve cycling of UV intensity to more faithfully recreate Martian daylight over several sols, as well as diurnal temperature cycles and consequent cycles of water frosting and sublimation, to study these additional parameters on PAH photostability.
Ultimately, detection of fluorescence from organic compounds near the Martian surface depends on multiple factors, including the localized fluorophore concentration, target range, intensity of the excitation light source, and sensitivity of the spectrometer or imaging instrument. It is clear from this experimental program, however, that over a time scale of relevance to operations of a robotic mission on the Martian surface, these three representative PAHs do not experience substantial degradation of their detectable fluorescence signal. Irradiated on mineral grains under Martian surface conditions and then tested at their peak fluorescence excitation wavelength, anthracene, pyrene, and perylene were all found to exhibit a UV-degradation half-life of between around 25 and 60 h at northern summer noontime flux levels, which equates to between 4 and 9.6 Martian sols when the full diurnal cycle is considered.
The nature of the changing UV flux over the diurnal cycle is an important consideration to take into account when relating the results of laboratory UV irradiation experiments to the reality of the time-variable UV environment of the Martian surface.
The results presented here are thus supportive of rover-mounted fluorescence-based instruments for surveying for the presence of prebiotic organic molecules such as PAHs.
Acknowledgments–– The research leading to these results has received funding from the European Community’s Seventh Framework Programme (FP7/2007–2013) under grant agreement no 241523 PRoViScout. LRD is supported by the UCL Institute of Origins Post-Doctoral Research Associateship. MRP is supported by funding from the Science and Technology Facilities Council (STFC).