a1 ESA ESTEC, Postbus 299, 2200 AG Noordwijk, The Netherlands
a2 Faculty of Earth and Life Sciences, VU University Amsterdam, De Boelelaan 1085, 1081 HV Amsterdam, The Netherlands
a3 International Lunar Exploration Working Group (ILEWG), c/o BH Foing, ESTEC PO Box 299, 2200 AG Noordwijk, The Netherlands
a4 Space Science Division, M.S. 245-3, NASA Ames Research Center, Moffett Field, CA 94035, USA
a5 Leiden Institute of Chemistry, Einsteinweg 55, PO Box 9502, 2300 Leiden, The Netherlands
a6 Space Policy Institute, Elliott School of International Affairs, Washington, DC, USA
a7 Institute of Medical Physics and Biophysics, CeNTech, University of Münster, Heisenbergstrasse 11, D-48149 Muenster, Germany
a8 inXitu Inc., 2551 Casey Ave, Ste A, Mountain View, CA 94043, USA
a9 Department of Earth Science and Engineering, Imperial College London, South Kensington Campus, London SW7 2AZ, UK
a10 Jet Propulsion Laboratory, California Institute of Technology, Pasadena, CA 91109, USA
a11 Institute of Geological Sciences, Planetary Sciences and Remote Sensing, Freie Universitaet Berlin, D-12249 Berlin, Germany
a12 Mars Society Australia, c/o 43 Michell St, Monash, ACT 2904, Australia
a13 Australian Centre for Astrobiology, Ground Floor, Biological Sciences Building, Sydney, NSW, Australia
We describe the field demonstration of astrobiology instruments and research methods conducted in and from the Mars Desert Research Station (MDRS) in Utah during the EuroGeoMars campaign 2009 coordinated by ILEWG, ESA/ESTEC and NASA Ames, with the contribution of academic partners. We discuss the entire experimental approach from determining the geological context using remote sensing, in situ measurements, sorties with sample collection and characterization, analysis in the field laboratory, to the post sample analysis using advanced laboratory facilities.
We present the rationale for terrestrial field campaigns to strengthen astrobiology research and the link between in situ and orbital remote sensing data. These campaigns are supporting the preparation for future missions such as Mars Science Laboratory, ExoMars or Mars Sample Return. We describe the EuroGeoMars 2009 campaign conducted by MDRS crew 76 and 77, focused on the investigation of surface processes in their geological context. Special emphasis was placed on sample collection and pre-screening using in-situ portable instruments. Science investigations included geological and geochemical measurements as well as detection and diagnostic of water, oxidants, organic matter, minerals, volatiles and biota.
EuroGeoMars 2009 was an example of a Moon–Mars field research campaign dedicated to the demonstration of astrobiology instruments and a specific methodology of comprehensive measurements from selected sampling sites. We discuss in sequence: the campaign objectives and trade-off based on science, technical or operational constraints. This includes remote sensing data and maps, and geological context; the monitoring of environmental parameters; the geophysical context and mineralogy studies; geology and geomorphology investigations; geochemistry characterization and subsurface studies.
We describe sample handling (extraction and collection) methods, and the sample analysis of soils and rocks performed in the MDRS laboratory using close inspection, initial petrological characterization, microscopy, Visible-NIR spectrometry, Raman spectrometry, X-ray diffraction/X-ray fluorescence spectrometry, soil analysis, electrochemical and biological measurements.
The results from post-mission analysis of returned samples using advanced facilities in collaborator institutes are described in companion papers in this issue. We present examples of in-situ analysis, and describe an example investigation on the exploration and analysis of endolithic microbial mats (from reconnaissance, in-situ imaging, sampling, local analysis to post-mission sample analysis).
(Received January 22 2011)
(Accepted January 24 2011)
(Online publication March 14 2011)
List of Figures and Tables
Fig. 1. (a) Google Earth satellite image showing the location of the MDRS station (near F) and sampling areas at Kissing Camel Ridge (near G). (b) Geology for the EuroGeoMars campaign, and positions of sampling areas (Wendt et al. 2009).
Fig. 2. (a) Southward view towards MDRS with Henry Mountains background. (b) Landscape and stratigraphy near MDRS station looking North, showing the resistant layer formed by sandstones of the Dakota sandstone formation at the top of the ridge and the shale slopes of the Brushy Basin member of the Morrison formation below.
Fig. 3. Context panoramic imaging of salt wash side view.
Fig. 4. Rover used for navigation tests, reconnaissance and EVA assistance (courtesy Carnegie Mellon University/NASA Ames).
Fig. 5. Biomarkers on rocks at the base of ‘Kissing Camel Ridge’ (position G in Fig. 1) (left) field colour image of rock surface with lichens with three main green, yellow and orange constituents. Right: The ‘Cyborg astrobiologist’ novelty algorithm detects automatically colour special signatures from the same image (McGuire et al. 2010; Gross et al. 2010).
Fig. 6. (a) Field inspection of calcite evaporite rocks. (b) Display and documentation of samples from one EVA before laboratory analysis.
Fig. 7. Raman spectrometer box (silver) and horizontal Raman fiber feed to be placed on sample holder, the vertical fiber feeds to the Ocean-optics visible NIR spectrometer.
Fig. 8. (a) X-ray Diffraction and fluorescence spectrometer XRD/XRF (orange case). The sample is crushed into powder and placed in a container inserted in the central upper slot for X-ray illumination. (b) Diorite sample (left), crushing (right) and sieving (middle) device before XRD-XRF analysis.
Fig. 9. (a) Installed biology and astrobiology laboratory. (b) Glovebox and sample handling. (c) Precision balance, centrifuge and PCR Peqlab. (d) MDRS microscopes. (e) Soil analysis kit.
Fig. 10. MDRS measured Raman spectrum of gypsum CaSO4·2H2O.
Fig. 11. XRD spectra analysed in MDRS with match from database minerals: (a) XRD spectrum of Dakota Formation sandstone sample indicating gypsum and quartz (top), (b) XRD spectrum of Morrison sample indicating quartz and montmorrillonite clay (middle), (c) XRD spectrum of calcite evaporate (bottom).
Fig. 12. (top) Extracted drill core in 4 segments of 8–12 cm, (bottom) XRD spectrum of a core extract measured in the Hab, indicating the specific peaks of gypsum (purple), Quartz (yellow) and montmorillonite clay (green).
Fig. 13. Set of samples collected and documented in situ for mineral, organic and biology MDRS laboratory and post-mission analysis.
Fig. 14. (a) Context and protocol for endolith imaging and sterile sampling. The white paper was imaged for balance control allowing calibration of quantitative colour information. (b) Zoom of endolith (20 cm field of view) in natural balance colours. (c) Zoom (enhanced colour balance, 15 cm field of view) where endoliths appear as 3 distinct colour units clearly, after detachment of the crust and varnish layers. (d) Zoom of the same 15 cm field of view in black & white, where the endoliths are much harder to distinguish.
Fig. 15. Study of endolithic microbial communities in the MDRS lab: (top) sample view before microscopic inspection (FOV 2.5 cm), (bottom) optical microscope MDRS lab image of green and brown endolith communities in relation to minerals (field of view 3 mm).
Fig. 16. Post-campaign study of endolithic microbial communities performed at NASA Ames: sample close-up context, FOV 1 cm (top), SEM magnification×250 , FOV 600 μm (middle) and SEM ×4000 FOV 40 μm (bottom).
Fig. 17. Endolith images taken with an autofluorescence microscope. The red colour is due to chlorophyll autofluorescence. These images indicate that the endoliths are comprised of photosynthetic coccoid cells that are approximately 1 μm in size. They mainly form in clusters perhaps indicating the formation of a biofilm, potentially confirmed by the SEM images.
Fig. 18. SEM view of endolith coccoid cells (smooth round features) together with sandstone micron particles (jagged shapes).
Fig. 19. SEM image of clump of coccoid cells, with abiotic particles suspended in a matrix possibly made of extracellular polymeric substance (EPS) from within an endolith.
Terrestrial analogue studies are used to better understand the nature and rates of geological and biological processes on Earth in order to interpret and validate information from orbiting or surface missions on extraterrestrial bodies. These terrestrial analogue data complement the interpretation of missions such as Mars-Express, SMART-1, Chandrayaan-1, Lunar Reconnaissance Orbiter (LRO), Mars Exploration Rovers and Mars Reconnaissance Orbiter (MRO), and help to prepare for future lunar and planetary Lander missions. International cooperation in terrestrial analogue activities provides a logical early step to implementing international Moon–Mars missions (see ILEWG Reports and ICEUM Declarations 2006–2010 (ICEUM 9, 10, 11); Foing 2008; Foing et al & ICEUM participants (2008b, c, d, e); MEPAG Report 2007; COSPAR Planetary Exploration Committee (PEX) Report 2010).
Surface science is one of the primary objectives of recent and future Mars and Moon missions. The geological record of Mars indicates a diversity of water-modified environments, including potential ancient habitable environments. Hydrated minerals on Mars trace the history of surface water and the global atmosphere and a long-term climate cycle (Christensen et al. 2001; Bibring et al. 2006). Recent Moon missions advanced our knowledge on surface composition (Lucey et al. 1998; Jolliff et al. 2000) and the bombardment history and indicated the presence of H2O and hydroxyl species on the lunar surface (Feldman et al. 2001; Pieters et al. 2009). Science investigations include a wide range of activities from global mapping to microscopic scale. Significant new science results will be obtained from coordinated multi-instrument operations on the surface. In-situ investigations of rocks and soil or sample return missions both require the development of systematic multi-instrument protocols, characterization diagnostics and methods to merge data from various instruments. Remote sensing/ground truth validation will enhance the science exploitation of future missions.
Orbital remote sensing has revealed a complex geologic record of planet Mars that formed in response to processes that include volcanism, weathering/erosion, sedimentation, glaciation, polar ice cap processes, fluid/rock interactions and tectonism and others. Six spacecraft have unveiled a new face of Mars history (Mars Global Surveyor (MGS), Mars Odyssey, Mars-Express (MEX), the two Mars Exploration Rovers (MER) and MRO). Various minerals have been identified both from the orbit or from the Martian surface (Klingelhofer et al. 2004; Squyres et al. 2004; Bibring et al. 2005; Gendrin et al. 2005; Poulet et al. 2005). For instance, the Gusev area has been studied both by the MER rover and MEX orbiter (Greeley et al. 2005; Parker et al. 2010). Recent results revealed the timing and duration of hydrologic activity on Mars and the evolution of sedimentary processes through time. Water, an important ingredient for life, could also be trapped as underground ice. MEX high-resolution stereo camera HRSC images have been used to determine that volcanic activity continued until recent times (Neukum et al. 2004). They indicate recent periglacial tropical activity (Murray et al. 2005; Head et al. 2005a, b), possibly the result of erratic variations of Mars obliquity. The past conditions of Mars may have eventually allowed life to develop (McKay & Stoker 1989). However, today, a combination of solar ultraviolet radiation, the extreme dryness of the soil and the oxidizing nature of the soil chemistry provides a toxic environment to biological and organic material on the surface or the near subsurface. Understanding the complex interactions between organic compounds and the soil mineralogy is vital for the potential detection of past or present life on Mars.
On the Moon we can study geological processes shaping the surface due to impacts, volcanism and space weathering. Recent lunar orbiters SMART-1 (Foing et al. 2006, 2008a, b, c, d, e), Selene Kaguya (Kato et al. 2008; Haruyama et al. 2008, 2009; Ono et al. 2009), Chandrayaan-1 (Goswami et al. 2008; Pieters et al. 2009), Chang'E1 and LRO (Chin et al. 2007; Vondrak et al. 2010) have studied impact processes and surface morphologies such as terraces, ejecta, central peaks for a number of craters of various sizes and ages in different locations. Bulk crustal composition provides constraints on the origin and evolution of the Moon, the lunar crusts and the large basins (such as the South Pole-Aitken Basin, SPA) (Jolliff et al. 2000). Measurements from orbit and existing lunar samples will enhance our knowledge on absolute chronology of the Moon and on the early or late heavy bombardment in the Solar System. The survival of exogenous ices and organics at lunar poles is also relevant in the astrobiology context.
Extreme environments on Earth often provide similar terrain conditions to landing/operation sites on the Moon and Mars. In order to maximize scientific return of space missions, it is important to rehearse mission operations in the field and through simulations. Terrestrial field research campaign in support of future planetary missions often include investigations of the geological, geochemical, biological and environmental context of a site; in-situ analysis, drilling of cores and sampling. This approach allows the demonstration of remote control field rovers; improvement of instrument performance; and evaluating crew operations and Extra Vehicular Activity (EVA) technologies. In this paper, we describe the planning and protocol development for both in-situ and post-mission lab-analysis for the astrobiology research campaign at MDRS (MDRS website; http://desert.marssociety.org).
The campaign EuroGeoMars 2009 was conducted in Utah (MDRS crew 76 and 77) and had four sets of objectives:
Science investigations were designed to understand the geological origin of the region through petrological and geochemical study of the constituents (minerals, organic matter, water, chemical compounds and biota). The compiled datasets have been compared to remote sensing data for geological interpretation. Special emphasis was given to the astrobiology objectives of the campaign, and the correlations between mineral, environmental parameters, organics and biota, placed in the geochemistry context.
In order to assess several human and scientific aspects of future robotic and manned missions on planetary surfaces, the EuroGeoMars campaign was proposed by collaborators from ILEWG, ESTEC and NASA Ames in collaboration with European and US investigators. The campaign was prepared through the ExoGeoLab pilot project (Foing et al. 2009; Foing et al. 2010a, b, c, d) developed by ILEWG with ESTEC support, to evaluate spin-in of new instrument technologies developed from Earth applications with potential use in space, and spin-off applications of instruments developed from space. The ExoGeoLab pilot project followed a technology programme using breadboard instruments that are attached to an automatic station for remote characterization of selected geological sites as well as sample acquisition and analysis methods. A payload suite (instruments, sensors, data handling system) has been deployed, operated and tested at NASA Ames and at ESTEC. On acceptance, instruments were deployed at Utah MDRS station. It was agreed that the EuroGeoMars campaign would last for 5 weeks and be organized in:
In preparation for the campaign, we collected geological maps and remote sensing data from the region. We consulted the literature and reports from previous field studies. This included interpretation of aerial photo images and United States Geological Survey geological maps. Traverses were planned using these images and maps and taking into account the time required for in-situ measurements and sampling protocol. We developed a method and database to permit a full documentation of samples taken in their geological context. The desert near Hanksville, Utah, includes a range of Mars analogue geological and geochemical features, such as lacustrine and evaporitic sediments, and paleochannels including some with inverted relief. The paper by Clarke & Stoker (2011) in this issue describes the geological context for the samples, and in particular looks at concretions in exhumed channels and their implications for Mars (Figs. 1 and 2).
(a) Google Earth satellite image showing the location of the MDRS station (near F) and sampling areas at Kissing Camel Ridge (near G). (b) Geology for the EuroGeoMars campaign, and positions of sampling areas (Wendt et al. 2009).
(a) Southward view towards MDRS with Henry Mountains background. (b) Landscape and stratigraphy near MDRS station looking North, showing the resistant layer formed by sandstones of the Dakota sandstone formation at the top of the ridge and the shale slopes of the Brushy Basin member of the Morrison formation below.
To support the sampling, the GPS coordinates of samples were collected systematically, together with panoramic imaging to relate to remote sensing, as well as macroscopic and close-up imaging.
Orbital and aerial imagery as well as the geology maps were analysed in order to define the possible sites for in-situ investigation. We developed a method for merging different imaging datasets taken from different perspectives (vertical or lateral) and integrated them in an interactive database. In parallel, a technology experiment was conducted on Mars navigation using the triangulation of positions of deployed captive helium balloons, in coordination with remote support in order to acquire coordinates (even in absence of a GPS system as would be the case on Mars). A video-cam was lifted by a balloon to provide an aerial view of the field for reconnaissance (Fig. 3).
A microrover (developed by Carnegie Mellon University) was used in the field to perform visualization tests for operation. The rover was equipped with an additional camera system (Hendrikse et al. 2010) to provide remote navigation tools. The rover was used to test issues of remote control, locomotion, hazard avoidance and data transfer that are critical in future surface operation missions. The rover was also used to provide remote reconnaissance imaging and geological context of the candidate scenes where samples could later be collected. Prior to sampling, a number of EVA traverses were conducted to specific locations in order to perform reconnaissance of the site and characterize the geology, as well as to select locations for in-situ measurements and sampling (Fig. 4).
Measurements of temperature, humidity, radiation, moisture and water activity were derived from sensors available at the MDRS station, or brought to the sampling sites, as well as from nearby local weather stations. Weather statistics and satellite observations can constrain the average and variation of parameters affecting the hydrology, moisture and oxydation level. The region around Hanksville is characterized as arid desert, cold in winter and hot in summer with an average annual temperature of 12°C. The diurnal range is given as 16–37°C in July and −7 to +7°C on 1 Feb. The area is subjected to wind erosion and was shaped by fluvial erosion. Hanksville receives 140 mm of annual average precipitation (Godfrey et al. 2008). Weather station sensors include measurements of the diurnal variations of temperature range, winds median average and gusts. The relative humidity showed minima at 15% and diurnal dawn maxima of 50–80% during the EuroGeoMars campaign. The average barometric pressure was 86 kPa. The wind variations showed a median of 5 kmph and gusts of 40–80 kmph. The Photosynthetic Active Radiation in the range 400–700 nm is at maximum 2000 μmoles of photons m−2 s−1. At the start of the EuroGeoMars campaign there was snow precipitation of 0.76 cm water equivalent (leading to a snow cover of 5 cm depth) on 26 January, a slight rain equivalent to 0.05 cm on 12 February, of 0.08 cm on 23 February, and fog on 24 February 2009. A more systematic study including the statistics of diurnal and seasonal changes of those quantities, as well as mechanism for eolian dust transport or heterogeneous water activity requires a systematic set of in-situ instruments and data acquisition methods.
Biomarkers on rocks at the base of ‘Kissing Camel Ridge’ (position G in Fig. 1) (left) field colour image of rock surface with lichens with three main green, yellow and orange constituents. Right: The ‘Cyborg astrobiologist’ novelty algorithm detects automatically colour special signatures from the same image (McGuire et al. 2010; Gross et al. 2010).
The MDRS is surrounded by a series of early Jurassic to late Cretaceous sediments derived by weathering and erosion from Paleozoic sedimentary rocks to the west. These sediments consist of marine to fluvial and lacustrine deposits that locally contain volcanic ashes. The geology formations and units around the MRDS station are described in Fig. 1(b) (Wendt et al. 2009; Clarke & Stoker 2011). The red lines (1–7) in Fig. 1(b) indicate some of the geological formations and their member Mb (in clockwise numbered order from top):
The landscape consists of mesas and scarp-bounded surfaces resulting from erosion of the flat-lying succession of alternating units of greater and lesser resistance to erosion. Clay-rich units being more easily eroded and sandstones are less. The sandstone surfaces form smooth plains and the clay-rich materials form dissected slopes.
The Brushy Basin Member forms a dissected plain of cracking clays (Clarke & Pain 2004). Fluvial channels are exposed on the steep slopes or are being exhumed as inverted relief. These features are analogous to those observed from Mars orbiters. The Mars analogue significance of these formations were investigated by Battler et al. (2006) and Clarke & Stoker (2011).
The field traverses included an in-situ inspection and recognition of the characteristic petrology. A camera system with images at various embedded scales (panoramic, high-resolution, close-up camera) was used in order to document the location, protocol and samples. The soil mechanical properties could be measured in situ using penetrometry or by studying the tracks left by rovers or EVA traverses.
A support investigation consisted of an enhanced ‘Cyborg astrobiologist’ field reporting capability based on a colour novelty detection algorithm applied to images obtained by a hand-held or rover camera (Gross et al. 2010; McGuire et al. 2010). The system collects images and detects novelty (see Fig. 5); i.e. unobserved colour ratios compared to previous scenes. We covered a vertical profile in the Brushy Basin Member of the Morrison Formation to test how the system responded to the various clay and sandstone strata. The preliminary results show that the system robustly detects strata not previously recorded.
The mineralogy and mineral assemblages of rocks were mostly determined in situ by close-up visual inspection. The various minerals identified include quartz, gypsum, clays, calcite and sulfates (Borst et al. 2010). Diorites were also sampled from an expedition to Mount Henry. Specific note was made of the original sedimentary processes responsible for the sediment deposition and more recent processes that led to secondary mineral formation such as gypsum and calcite concretions, desert varnish, etc. (Fig. 6(a)).
A Magnetic Susceptibility Meter was used in the field to determine the magnetic susceptibility and conductivity of samples. The Xterra (by InXitu) Field X-ray Diffractometer for mineralogy and X-ray Fluorescence for elemental chemistry and the Raman spectrometer (InPhotonics) were tested in outdoor conditions as the instruments could be transported. As we had installed a geochemical laboratory in the MDRS habitat, we concentrated for this research campaign on fast in-situ characterization and sample collection and used the analytical instruments in the laboratory for more accurate and detailed investigations. In some cases, a classical field test for carbonates in the soil was performed using HCl acid and observing the release of CO2 bubbles.
Drilling equipment included a Milwaukee hand-operated electrical drill that could reach depths down to 1 m. Another manual rotary drill was used to sample soft-clay areas. The drill cores provided information on the vertical structure of soils and the distribution of minerals within rocks. These observations were compared with the lateral variations in rock layers observed from the edges of cliffs to determine the scale of heterogeneity of individual strata.
A comparison was also made with data obtained from Ground Penetrating Radar (GPR) subsurface test measurements. The CRUX GPR developed by JPL (Kim et al. 2005), and adapted by NASA Ames was tested to provide information on the stratification of sedimentary structures. The GPR operates at 800 MHz with a penetration of 5 m and a resolution of 15 cm, depending on the soil permittivity and scattering properties. The GPR was only used in few areas to study the clay deposits near the MDRS Morrison Formation and the top of the Dakota Formation.
A later campaign in 2010 (DOMMEX-EuroMoonMars) focused on performing subsurface science-related activities with Mars Underground Mole (MUM, a robotic penetrometry system) and the CRUX GPR (Stoker et al. 2010, 2011). Data collected with the CRUX GPR are reported in Clarke & Stoker (2011).
The sample context was documented with still and HDTV format cameras for field and lab studies (transported from ESTEC/ILEWG ExoGeoLab). Specific protocols were followed for sterile sampling (using gloves and sterile tools), and for borehole core sampling (to preserve the soil stratification record) (Fig. 6(b)).
For every EVA, the samples were catalogued and curated. The crew installed a geochemical laboratory in the habitat for analysis of the samples. This included a Raman Spectrometer (InPhotonics), a Visible/NIR Spectrometer (OceanOptics), an integrated X-ray diffractometer/X-ray fluorescence meter (Terra 158) as well as an optical microscope. We first performed non-destructive techniques. A physical inspection and imaging was performed on the samples before optical spectroscopy was applied using reflectance and Raman spectrometry to determine the mineral and organic content in the soils or rocks. The biological content of sample equivalents (sample aliquots?) was measured with on-site polymerase chain reaction (PCR) equipment.
The morphology of minerals and the microbial relation to the mineral assemblage were studied with an optical microscope (200 power, provided at MDRS). The microscope data (FOV few mm) were linked with close-up imaging data (FOV few cm) to provide the spatial context for the geochemical or biological techniques used with different surface or volume fields of view. Microscopy was used to investigate the water samples. Micro-organisms as well as floating particles were concentrated by centrifugation. Several micro-organisms could be detected, most of them being algae (Thiel et al. 2009, 2011).
An Ocean Optics USB2000 Fibre-optic spectrometer was used to measure the light reflectance in the ultraviolet, visible and NIR spectral regions. This permitted correlation of colour inspection with quantitative reflectance. In a few cases, some signatures of absorption due to organic compounds or red fluorescence could be measured on selected samples.
Raman spectroscopy is based on inelastic scattering of light, used to study low-frequency modes of a system such as vibration or rotation. Each mineral has a unique Raman spectral signature, which is compared with standard mineral Raman spectra in a database to identify the mineral composition of the sample (Foing et al. 2010c; Som & Foing 2010). For the Raman spectrometer (InPhotonics) used at MDRS, we used an exciting laser at 785.335 nm and measured the Raman spectrum in the range of 160–1900 cm−1. We designed and manufactured a sample holder for Raman and NIR sensor head holder to allow controlled and reproducible sample analysis conditions (Fig. 7).
The samples were crushed into powders for the XRD/XRF analysis. CheMin is the X-ray diffraction (XRD) instrument aboard NASA's Mars Science Laboratory (MSL) (Blake et al. 2007). A commercial instrument called Terra was developed by inXitu, Inc. in 2007 to maximize the ease of use and field deployment. Terra has a similar architecture to CheMin with a smaller CCD for reasons of cost, weight and power. The CCD is cooled to −45°C with a Peltier cooler. The system includes an onboard computer to control the instrument, acquire and process data in real time and providing a graphical user interface through a wireless link. Li-ion batteries allow 4–5 h of autonomous operation. The entire instrument weighs less than 15 kg including batteries and a rugged housing. XRD data permit mineral identification within a few minutes. XRF data, in the energy range (3–15 keV) allow measurement of specific chemical elements (Fig. 8).
(a) X-ray Diffraction and fluorescence spectrometer XRD/XRF (orange case). The sample is crushed into powder and placed in a container inserted in the central upper slot for X-ray illumination. (b) Diorite sample (left), crushing (right) and sieving (middle) device before XRD-XRF analysis.
The electro chemical activity was measured using a soil analysis kit providing the content of ions and reactivity. The soil composition of the previously collected soil samples was analysed by using colorimetric chemical reactions (LaMotte Soil Testing System). The pH, nitrogen, potassium, phosphorous, magnesium, calcium and water content of soils originating from areas with and without vegetation were determined. The pH of all soil samples was in the range of 8.2–10.0. The magnesium concentration was very low for all samples (<5 ppm). The range for phosphor was between 5 and 100 ppm (Ehrenfreund et al. 2010). Soil conductivity measurements were obtained using a Thermo Orion 135A probe after dilution (1:10) in distilled water and ranged from 1 to 20 mS (Fig. 9(a–e)).
The crew performed upgrades to augment the biological laboratory at MDRS. The laboratory in the habitat was equipped with the instrumentation shown in Fig. 9. The temperature in the laboratory was slightly below nominal (15–16°C).
An adenosine tri-phosphate (ATP) meter was used to measure the metabolic activity and microbial content of the samples.
The PCR lab was brought from the ESTEC ExoGeoLab project. An overall set-up was integrated and tested in ESTEC and then transported and reintegrated in the MDRS lab for performing PCR experiments (Thiel et al. 2011). This included a precision balance (Satorius), a vortex and a centrifuge for DNA extraction. Reaction mixtures were performed in a glovebox, and fragment amplification in a thermal cycler Primus 25 advanced (Peqlab). PCR fragments were then analysed using agarose E-gels and visualized. The results of PCR-based analysis of microbial communities during the EuroGeoMars MDRS campaign are described in Thiel et al. (2011).
The various soil samples extracted in sterile conditions were divided and sent to various laboratories for a later analysis with advanced techniques:
Field science experiments were started as soon as the corresponding instruments were assembled, tested and deployed. More than 100 documented samples were collected by the MDRS crew 77 for geology (50 samples), astrobiology (11+5 samples divided for 8 investigators groups) and biology (30 samples divided into 4 collaborating groups). MDRS crew 76 collected 50 documented samples. Samples were screened/analysed in the lab at the Habitat. Data were sent to remote science support teams in Europe and the US for further evaluation and detailed analysis. The geoscience investigations concerned mostly geological survey, documenting sample context and geochemical analyses of returned samples from the surrounding rock formations.
Approximately 40 samples have been analysed in the Habitat laboratory for chemical composition (XRF) and mineralogy content (XRD, Raman, VIS/NIR). Samples included clays, sandstones and volcanic ash layers of the Jurassic Morrison formation, pure crystals such as gypsum and calcite, petrified wood, desert varnish, endoliths and salt efflorescence. The sampling and analyses involved the set-up and maintenance of a detailed database with sample description, context geology and test results (Figs. 10–13).
XRD spectra analysed in MDRS with match from database minerals: (a) XRD spectrum of Dakota Formation sandstone sample indicating gypsum and quartz (top), (b) XRD spectrum of Morrison sample indicating quartz and montmorrillonite clay (middle), (c) XRD spectrum of calcite evaporate (bottom).
The primary goal of the biology investigations was the analysis of microbial communities living in the soil in interesting locations in the MDRS area, using protocols that are relevant to the search for organics and life on Mars, and to planetary protection. This investigation had a field aspect and a laboratory aspect: soil sampling was done in the field at depths of 10, 30 and 60 cm, in and out of EVA working conditions.
DNA extraction and PCR analysis were performed in the in-situ laboratory. DNA extracted from nine soil and water samples of five different sampling sites were analysed in a first PCR run (Primus25 advanced; PeqLab) to detect bacterial DNA. Microscopy was used to investigate water samples for micro-organisms as well as floating particles concentrated by centrifugation.
DNA extraction and PCR analysis were also performed in a laboratory at Grand-Junction immediately after the campaign (Thiel et al. 2011) and in laboratories in Europe after the campaign (Direito et al. 2011). The microbial communities were studied in situ indicating already differences between Archaea and Bacteria in samples, and a later analysis of returned samples provided a more complete description of the relation of microbial communities’ composition and phylogenetic analysis (Direito et al. 2011).
The samples were divided (see Fig. 13) and sent to Earth-based laboratories for sophisticated analysis of PAHs (Orzechowska et al. 2010), of mineral matrix composition (Kotler et al. 2010) or of amino acids (Martins et al. 2011). Post-analysis studies determined the total carbon content (Orzechowska et al. 2010). A study of solid phase microextraction (SPME) method for fast screening and determination of PAHs in soil samples was performed, minimising sample handling and preserving chemical integrity of the sample. Complementary liquid extraction was used to obtain information on five- and six-ring PAH compounds. The measured concentrations of PAHs are, in general, very low, ranging from 1 to 60 ng/g (Orzechowska et al. 2010).
Using a Milwaukee drill (Stoker et al. 2009, 2010), we extracted cores down to 70 cm depth in a layered concretion-rich exhumed channel fragment. The drill site can also be analysed from side view near the MDRS habitat. The samples were transferred to a container preserving the stratification. The variation of the mineralogy and chemistry was analysed along the drill core. The samples show layers of quartz, gypsum and clays with some light mixing of those minerals. Visual, reflectance spectrometry, Raman and X-ray analysis was performed on extracts from the drill core (Fig. 12).
After these preliminary investigations, a more comprehensive campaign (DOMEX/EuroMoonMars 2010) was organized in November 2009 and February–March 2010 (Stoker et al. 2010, 2011; Clarke & Stoker 2011) using more advanced drilling systems, in conjunction with imaging and GPR reconnaissance.
During the EuroGeoMars campaign we investigated on-site endolithic biota in relation to their environment. Endolithic microbes are extremophile organisms that live inside rocks or in pores between mineral grains. They can be not only lithotrophs but also phototrophs such as cyanobacteria. Phototrophs use light as energy source while lithotrophs oxidize inorganic compounds. They consume reduced elements from rocks, producing energy and free electrons used for ATP production. Litho-autotrophs obtain their carbon from CO2 included in rocks and litho-heterotrophs from organic material. Endoliths can be slow to grow, due to limited nutrients. Endoliths may be present on Mars, and therefore it is interesting to study them in extreme environments on Earth in the context of life detection. An example is the endolithic, desiccation- and radiation-resistant cyanobacterium Chroococcidiopsis, a model organism for viability studies under Martian conditions. This prokaryote is able to survive in a Martian UV radiation environment when shielded by 1 mm of rock (Cockell et al. 2005). An acidophilic chemolithotroph from Rio Tinto was exposed to simulated Mars UV and atmospheric conditions under the protection of a Mars regolith analogue (Gómez et al. 2010).
We have found, studied in situ and sampled some endolithic mats near the MDRS research station. We investigated various areas at the base of ‘Kissing Camel Ridge’, a geological feature formed by an exhumed palaeo-channel in the Brushy Basin member of the Morrison formation (point G in Fig. 1). In this area, some locations show concretions morphologically similar to the ‘blueberries’ observed by the Mars Exploration Rover in Meridiani, Mars (Clarke & Stoker 2011). A visual survey was conducted using colour imaging and the Cyborg astrobiologist experiment. The macroscopic pictures and close-up views indicated surface epilithic lichens.
After detachment of the crust, we confirmed the presence of microbial endolith population with green and orange-brown constituents, and the presence of endolith under a purple-brown coating. Samples of endolith attached to the host crust were taken to the MDRS laboratory. The visual and microscopic inspection confirms the presence of different layers: an outer varnish, a cemented crust, a brown microbial mat and a green mat attached to the rocks. Imaging was performed several times: a) before sampling, b) just after sampling using reference white calibration paper in order to quantify the colours of endolith on first exposure to light, and c) the same scene was revisited 1 week later. After detachment of the crust and varnish layers, the endoliths appear in three different colour units, with variations within 0.1–0.5 mm.
Reflectance and Raman spectroscopic studies were performed on the varnish, crust, endolith and on the different adjacent mineral units. The analysis of the varnish coating with the XRF shows an overabundance of manganese, but little potassium, calcium or chromium. This is consistent with reddish iron and manganese oxides precipitates forming a dark and UV protecting layer. The microscopy indicates that the green endolith unit is mostly attached to gypsum grains (Figs. 14 and 15).
(a) Context and protocol for endolith imaging and sterile sampling. The white paper was imaged for balance control allowing calibration of quantitative colour information. (b) Zoom of endolith (20 cm field of view) in natural balance colours. (c) Zoom (enhanced colour balance, 15 cm field of view) where endoliths appear as 3 distinct colour units clearly, after detachment of the crust and varnish layers. (d) Zoom of the same 15 cm field of view in black & white, where the endoliths are much harder to distinguish.
Study of endolithic microbial communities in the MDRS lab: (top) sample view before microscopic inspection (FOV 2.5 cm), (bottom) optical microscope MDRS lab image of green and brown endolith communities in relation to minerals (field of view 3 mm).
Post-mission analysis of the endolith samples was performed using a tabletop with scanning electron microscope (SEM) was conducted at NASA Ames Research Centre. This instrument is portable enough to allow field deployment. In the green area unit, we observed sheet-like structures layers of 100–300 μm in the interstitial pores between mineral grains. At ×4000, we detect submicron coccoids (Figs. 16–19).
Endolith images taken with an autofluorescence microscope. The red colour is due to chlorophyll autofluorescence. These images indicate that the endoliths are comprised of photosynthetic coccoid cells that are approximately 1 μm in size. They mainly form in clusters perhaps indicating the formation of a biofilm, potentially confirmed by the SEM images.
In Fig. 17, autofluorescence microscope images show that the endoliths contain photosynthetic coccoid cells that are approximately 1 μm in diameter. They form primarily in clusters, perhaps indicating the formation of a biofilm, which is potentially confirmed by the SEM images. The red colour is due to chlorophyll autofluorescence and highlights the clustering of the phototrophic bacteria.
In Fig. 18, we see the smooth coccoidal cells that are roughly the same size as those present in the autofluoresence microscopy images. Again, the cells are clustered together and then come into contact with the more jagged, lighter-toned sandstone particles. This transition is not smooth, but rather the particles are packed in between clusters of cells before only sandstone grains remain in the next layer of the endolith.
In Fig. 19, the abiotic particles surrounding the coccoid cells appear suspended in a matrix. This matrix might be EPS that connects the cells in a biofilm. By forming a biofilm, these endolithic micro-organisms can better survive their nutrient poor environment, as available nutrients can concentrate on the surface. Also, the EPS allows the cells to attach to the surface of the sandstone for a more stable living environment. In addition, it is possible that there is more than one species of micro-organisms present in the biofilm. If so, the community of endolithic micro-organisms would benefit as the different species would be able to break down different types of nutrients, and they would be able to share in the limited nutrients available in the sandstone.
These results on the endoliths from in situ measurements to post laboratory sample analysis illustrate a possible astrobiology research avenue that can be performed at the MDRS analogue site.
We have described the instruments and methods used for astrobiology research during the EuroGeoMars 2009 campaign. For technology field demonstration, the EuroGeoMars crew used instruments under realistic conditions (cameras, digital microscopy, XRD/XRF Spectrometers, Reflectance spectrometers, Raman spectrometer, GPR, magnetic susceptibility meter, ATP Luminometry meter and other sensors). Remote sensing maps and geology reconnaissance were compared with surface in-situ investigations. A method of sample acquisition, curation and an analysis protocol was developed. The operations of remote rovers or their cooperation with field crew in EVA were investigated. Systems were demonstrated for communication, navigation and positioning. A Cyborg astrobiologist novelty detection algorithm was applied to rocks and landscape in different scenarios. The crew and remote support team used maps and database tools to integrate data and metadata from the sample context, rocks and subsequent measurements.
The EuroGeoMars research investigated processes relevant to Earth–Moon–Mars, in relation to geology and mineralogy. This included the analysis of samples from surface and from drill cores, in the field, in the habitat and later in laboratories. Several advanced and miniaturized instruments representative of those developed for future space missions were used, and provided in-situ constraints on mineralogy and organics.
Human crew-related aspects, i.e. (a) evaluation of the different functions and interfaces of a planetary habitat, (b) crew time organization in this habitat (Pletser & Foing, 2010). The evaluation of man–machine interfaces of astrobiology equipment is discussed in Thiel et al. (2011). Education, outreach, communications, multi-cultural and public relations aspects have been described in Foing et al. (2010a, b, c, d). The campaign experience and data analysis were used for a number of students’ projects (bachelor, master and PhD research) and thesis reports.
In conclusion, the goals of EuroGeoMars 2009 field campaign were fulfilled by contributing to:
As a follow-up of the EuroGeoMars 2009 campaign, ILEWG supported with instruments and experts, a campaign in Eifel Germany on human and robotic cooperation (Foing et al. 2010a; Groemer et al. 2010), and field campaigns by the CAREX project on ‘Life in Extreme Environment’ at Rio Tinto in Spain in Sept. 2009 and in Iceland in June 2010 (Direito et al. 2010; Gómez et al. 2010, 2011), and in Antarctica in December 2009 (De Vera et al. 2010) with a specific focus to use research instruments on the field for in-situ analysis of bio-organics and minerals in samples.
A EuroMoonMars/DOMEX (Drilling on the Moon and Mars in Human Exploration) campaign was performed in November 2009 and February–April 2010, using analogue missions to develop the approach for using human crews to perform science activities on the Moon and Mars, with the novelty of exploration and sampling of the subsurface using a suite of drills from back-pack carried to large truck-carried systems (Foing et al. 2010a, b, c, d; Stoker et al. 2010, 2011). A series of EuroMoonMars-DOMEX five crew rotations were deployed for 2 weeks each time performing complementary aspects of this research.
The experience and results from these campaigns in sites representing specific planetary analogue conditions can contribute to the preparation of field tests for Moon and Mars exploration, for missions such as MSL, Exomars, Moon or Mars Sample Return. This will include the investigation of geological and geochemical context, drilling of cores and sampling, remote control of field rovers, cameras and instruments. Also future human missions to the Moon or Mars can be prepared by evaluating crew operations, simulations and EVAs,and interaction with instruments. Terrestrial campaigns including tele-robotics and EVAs enable preparation under both real and simulated conditions for science, technology, research, operational, organizational and communication aspects associated with future robotic and human exploration missions.
We thank NASA Ames, ESTEC, ILEWG and partner institutes for experimental, operational and science support. We thank the MDRS mission support and Mars society (A. Westenberg and J. Edwards), ESTEC ExoGeoLab remote support (J. Page, P. Voorzaat and P. Mahapatra), NASA Ames support (C. McKay and F. Selch; CMU). B.H.F., C.T. and A.B. acknowledge a research travel grant from ILEWG. We acknowledge the support teams of EuroGeoMars 2009 from MDRS and partner universities (VU Amsterdam, FU Berlin, TU Delft, Cranfield University, Bristol University) and the EuroGeoMars 2009 crew members. We also thank the subsequent crews from ILEWG EuroMoonMars-DOMMEX 2010 campaigns and main partners (NASA, ESTEC and Ecole de l'Air) for their contribution.