Tag: ta-call-ft

21-EPN-FT1-016: Metabolic responses of Antarctic melanised microorganism to simulated Martian conditions

Visit by Ilaria Catanzaro, University of Tuscia (Italy) to TA2.19 Center for Microbial Life Detection, Medical University Graz (Austria).
Dates of visit: 30 May – 03 June 2022

Report Summary: Current hostile conditions on the surface of Mars entail that, if any life form has ever existed on the planet, it may have adopted survival strategies like those evolved by terrestrial microorganisms inhabiting extreme environments e.g. Antarctica. There, one of the most common strategies observed is the cryptoendolithic microbial growth where free-living black fungi living along with algae and lichens within rocky interstices serve as a shield from excessive harmful solar radiation, and their extremotolerance can be mainly due to the presence of thick, highly melanised cell walls.

The ability of these cryptoendolytic microorganisms to thrive under extreme conditions raises the question of whether they cope with them by also regulating their metabolic expression in addition to melanin production, and whether a hypothetical microbial life on Mars could ever have arisen with similar adaptive strategies. In this optic, this study aimed to examin the metabolic regulation of melanised, cryptoendolithic microorganisms in martian scenario. To achieve this goal, colonies of the cryptoendolithic black fungus Cryomyces antarcticus previously exposed to simulated martian conditions such as perchlorates, sulfatic regolith soil and γ radiation, were then analysed with NMR spectrometry at the Center for Microbial Life Detection of the Medical University of Graz. Sample preparation and analysis were carried out in the Facility using standard protocols. Although only preliminary data are available at the time of report writing, significant differences in fungal metabolic expression were observed between the different simulated martian conditions tested.

21-EPN-FT1-012: Zebra dolomites revised – clumped isotope analysis as a tool to assess recrystallisation and dolomite cementation in overpressured settings

Visit by Rudy Swennan, KU Leuven (Belgium), to TA2 Facility 17 – Isotoptech Stable/Clumped Isotopes Laboratory (Hungary).
Dates of visit: 22 – 31 August 2022.

Report Summary: Zebra dolomites are marked by an alternation of millimeter thick dark colored, as recrystallised interpreted bands and white cement bands. Disruption of the banding is manifested by displacements that gradually increases and subsequently deceases before disappearing. This disruption also occurs at intracrystalline scale with crystal rehealing features as observable under cathodoluminescence. This disruption of the zebra dolomites is explained by dolomitization in relation to overpressured fluid flow.  

In the framework of the Europlanet project zebra dolomite samples from 3 deep Belgian boreholes (Soumagne, Soiron and Bolland) were selected for clumped isotope analysis.  The aim was to sample and analyse the dark fine crystalline and white coarse dolomite cements separately to infer the original (re)crystallization temperature.  The following research questions were raised: i) is there a systematic difference in deduced temperature between the dark and white dolomite bands.  If so then this could help to better constrain the recrystallisation and cementation.  This would allow to assess the potential resetting of the original clumped isotope signature of the dark bands due to recrystallisation; ii) if the cement phases display uniform temperatures then this temperature can be compared with the minimum crystallization temperature deduced from primary fluid inclusion microthermometry [1]. The discrepancy between both temperatures, which links to the pressure correction, normally allows to quantify the overpressure of the system; iii) based on deduced crystallization temperature and δ¹⁸O_PDB, the δ¹⁸O_SMOW of the fluid can be assessed, allowing to constrain the origin of the dolomitizing fluids, certainly when combined with Sr isotope analysis.

21-EPN-FT1-010: Tracking the Thermal Evolution of the Miocene Ries Crater Lake as a Potential Analogue for Microbial Habitats on Early Mars

Visit by Duncan Mifsud, University of Kent (UK), to TA2 Facility 17 – Isotoptech Stable/Clumped Isotopes Laboratory (Hungary).
Dates of visit: 21 March – 01 April 2022.

Report Summary: We have measured the clumped carbonate (¹³C¹⁸O¹⁶O) isotope ratios, as well as the stable isotope ratios δ¹⁸O and δ¹³C, of a number of bioherm, travertine, and crater fill marl samples from a drill core taken from the Nördlinger Ries Crater (NRC) in Bavaria, Germany. The aim of the project was to make use of the clumped carbonate isotope ratios so as to re-construct a palaeotemperature record of the lake environment, which could be used to assess its habitability in the time since its formation. Such information would be useful for assessing the past habitability of similar crater lake environments on Mars, which are presently of great interest.

At first glance, our results demonstrate that the analysed carbonate samples were formed at temperatures well below what would be expected in the NRC lake environment. On closer inspection, however, it was hypothesised that our carbonate samples were either collected from too high up in the stratigraphy, or they were formed under non-equilibrium conditions and thus suffered from kinetic fractionation effects. The result of the latter is a depression of the precipitation temperature as calculated by palaeothermometric scales.

Future studies are planned to investigate samples from suevite (i.e. the oldest crater infill) and to quantify the extent and causes of these kinetic fractionation effects. Future studies on other crater fill marls may thus also be worthwhile.

21-EPN-FT1-019: Isotopic composition of single detrital carbonate grains in the source-to-sink study of the Bengal Fan record

Visit by Mara Limonta, University of Milano-Bicocca (Italy), to TA2.9 Ion Probe Facility (IPF), CRPG (France).
Dates of visit: 25 July – 05 August 2022

Report Summary:

The Bengal Fan forms the largest deep-sea turbidite system on Earth and hosts a unique sedimentary record of the evolution of the Himalayan orogenic belt.

This study aims to develop a new protocol to analyse single-grain isotopic signatures of detrital carbonates with primary application in source-to-sink studies and to foster the application of oxygen and carbon isotopes on single detrital grains of carbonates as a provenance tracer. δ¹⁸O and δ¹³C fingerprint of single detrital carbonate grains in Bengal Fan turbidites (IODP Expedition 354) will allow to detect and quantify the signature of different carbonate rocks from the Tethys Himalaya and High Himalaya and to better reconstruct the evolution of erosion processes in the Himalayan belt. This work will allow also testing the feasibility of the new single-grain approach. δ¹⁸O and δ¹³C fingerprint of detrital carbonate grains of selected Bengal Fan turbidites could not be measured due to their fine sand to silt grain-size.

We establish the grain-size feasibility limit at 200 microns in grain diameter. Otherwise, oxygen and carbon isotopic signature of single carbonate grains from Marsyandi and Kali Gandaki modern sand-sized river sediments were analysed to characterize isotopic fingerprint of carbonatic source rocks of Tethys Himalaya unit exposed along their drainage basin. Detrital carbonates of Marsyandi and Kali Gandaki rivers show similar low δ¹⁸O values, indicating depletion by metamorphic reactions. δ¹³C values range from +2‰ and -2‰ and mostly positive δ¹³C values characterise Kali Gandaki, whereas mostly negative δ¹³C values characterise Marsyandi carbonate grains.

21-EPN-FT1-006: Melting phase relations of subduction zone minerals and their nitrogen budget

Visit by Caterina Melai, University of Bayreuth (Germany) to TA2.9 Ion Probe Facility (IPF), CRPG (France).
Dates of visit: 29 August – 02 September 2022

Report Summary: In this study the phase relations of hydrous aluminosilicate minerals (e.g. montmorillonite, phlogopite, phengite and serpentinite) that are present in sedimentary layers or form during early prograde metamorphism of the oceanic lithosphere are investigated at sub-arc conditions. The investigated minerals are potential hosts for nitrogen at different P-T conditions along the subducting slab, depending on their phase stabilities and the N partitioning upon partial melting of these phases. In the present analytical session, several minerals in equilibrium with melt (quenched glass) have been analysed by means of SIMS.

The measurements in this report were performed using the CAMECA 1280 HR2 Ion Probe at CRPG, France. All the experimental capsules planned for the session were analysed and additional secondary standards were investigated.

The experimental samples showed consistent and reproducible N content on the different measured spots both on the mineral and the melt phase. More challenging was the measurements of the standards that confirmed the existing concern on the possible matrix effect during SIMS measurements of mineral phases. The different behaviour of the light elements analysed in a glass or crystalline matrix appears to have a strong effect on the measured nitrogen ion yield.

The work performed during this analytical session at the SIMS, allowed the acquisition of the N data for the calculation of the partition coefficients between mineral and melt while providing additional evidence for the need of further investigation of the matrix effect for this technique.

Read the full scientific report, with kind permision from Caterina Melai.

21-EPN-FT1-003: Spectral signatures of amino acid and polypeptide embedded in water ices – Implications for biosignature identification on icy moons

Visit by Surendra Vikram Singh and Bhalamurugan Sivaraman, Physical Research Laboratory (India), to TA2.8 CSS (Cold Surfaces Spectroscopy) at IPAG (France).
Dates of visit: 23 May – 08 June 2022

Report Summary: The objective of the experiments was to obtain a spectral library of biomolecules such as amino acids in water ice in context of icy bodies of solar system. We performed a series of measurements obtaining reflectance spectra of glycine –water ice mixtures in the VIS-NIR range (0.4-4.2 μm) at the temperature range of 110-250 K and at three different concentrations, using Cold Surface Spectroscopy Facility (CSS) setup at IPAG. Glycine – water ice mixtures were studied in two different mixing modes (inter and intra mixing) to get the spectral variations due to dissolving amino acids into water. Reflectance spectra of pure glycine and pure water ice were also obtained for reference. Reflectance spectra for a shocked glycine sample (obtained from HISTA facility at PRL) was also studied to understand the effect of shock induced chemistry. These measurements will support to find the spectral signature of amino acids on icy bodies of solar system.

21-EPN-FT1-025: Ammonium salts reflectance spectra changing viewing geometry for distinguish them on the surface of icy planetary bodies

Visit by Maximiliano Fastelli and Matteo Bisolfati, University of Perugia (Italy), to TA2.8 CSS (Cold Surfaces Spectroscopy) at IPAG (France).
Dates of visit: 13-25 June 2022

Report Summary: During the Europlanet 2024 RI TA Fast Track call, reflectance VIS-NIR spectra were collected at the CSS facility (IPAG) in Grenoble, France. Different viewing geometries were chosen to collect BRDF spectral data of a selected group of ammonium minerals. BRDF were collected in the 1 – 4.8 μm range considering a set of 3 incidence angles (i) (i = 0°; 30°; 60°) and 8 emergence angles (e) between -70° and 70° at room temperature. The NH4+overtone and combination bands located at ~ 1.09, 1.32, 1.62, 2.04, 2.2 and 3.05 μm are experimentally investigated.

The bands position remains unchanged varying geometrical configuration. On the other hand bands area and depth shows the highest values for i = 0° and 30° and e below 40°. These band parameters at ± 70° emergence angles evidence a decrease in their values. A general trend of spectral red shift with phase angle is observed. The bidirectional reflectance spectroscopy of selected samples shows important variations with the observation geometry of the measurements. Furthermore, from these preliminary data analyses, can be observed how reflectance values and spectral slope are affected by geometry of measurements. The surfaces of the planetary bodies are irregular and rough, which is why the effect of the observation geometry must also be considered. The collected data set can be helpful in the context of future missions aimed to understand the nature of minerals on icy and small bodies. NH4+–bearing minerals identification has a strong impact on understand their thermal evolution and the construction of geophysical internal models.

21-EPN-FT1-003: Biogeochemical tools to search for biosignatures in microbial carbonates from extreme environments

Visit by Sylvie Bruggmann, University of Lausanne (Switzerland) and Camila Areias, Vrije Universiteit Amsterdam (Netherlands), to TA1.6 Argentinian Andes (Argentina).
Dates of visit: 10-16 December 2022

Report Summary: Microorganisms evolved under extreme conditions as the first forms of life on Earth. In the geological record, signatures of these microbial communities can be preserved in the chemistry of sedimentary rocks as microbialites. The identification of their biogenicity, however, is often ambiguous, as biosignatures can be overprinted, and abiotic processes may form similar signatures. Microbialites forming under extreme conditions on the modern Earth can be used as analogues to better understand the formation of biosignatures, and to improve their identification in sedimentary rocks from Earth and Mars.

The TA1 Facility 6 in the Argentinian Andes provides an ideal environment where carbonaceous microbialites form under extreme conditions, such as cold temperatures, low precipitation and high UV radiation. To better resolve the ambiguity of biosignatures, we use a combined approach of organic and inorganic biogeochemical tools to examine sediment and water samples. The organic tool focuses on lipid biomarkers that can be attributed to specific biogenic sources, such as cyanobacteria. In addition, the inorganic tool utilises elemental concentration and isotope compositions of biologically relevant metals, such as Fe or Sr, which can record information of a biogenic or abiotic origin. The combination of these organic and inorganic tools can improve the identification of biosignatures and their credibility can be enhanced.

21-EPN-FT1-029: Petrographical, mineralogical and geochemical study of the meteorite Gueltat Zemmour Morocco, observed fall in August 2018.

Visit by El Mehdi El Hachimi, Hassan II University of Casablanca (Morocco) to TA2 Facility 3 – NHM Petrology, Mineralogy and Chemistry Facility (UK).
Dates of visit: 28 November -16 December 2022

Report Summary: The Gueltat Zemmour meteorite project was undertaken to conduct laboratory analyses using various techniques, such as X-ray diffraction (XRD), scanning electron microscopy (SEM), electron probe microanalysis (EPMA), and laser ablation inductively coupled plasma mass spectrometry (LA-ICP-MS). The XRD results were divided into two aspects: mineral identification and mineral quantification. The SEM technique was performed on two sections and provided EDS analyses of interesting mineral phases on the meteorite, as well as compositional and single element maps. The EPMA technique was used to analyze the major and minor element compositions of sulfide, silicate, and metal. The LA-ICP-MS technique was used to determine trace element compositions in areas of interest determined by SEM and EPMA, and no halite minerals were found. The analyses yielded numerous encouraging results, including 500 SEM spectra, 177 analyses for silicates, 69 for metal and sulfides from EPMA, and 48 analyses from LA-ICP-MS. Therefore, the results from SEM, XRD, EPMA, and particularly LA-ICP-MS appear to represent the completeness of the scientific data required to create a brilliant research article.

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21-EPN-FT1-021: Diffuse chemotrophic microbialites as analogues for martian life

Visit by Laura Clodoré, Centre de Biophysique Moléculaire-CNRS, Orléans (France) to TA2 Facility 3 – NHM Petrology, Mineralogy and Chemistry Facility (UK).
Dates of visit: 27 June – 05 July 2022

Report Summary:

Understanding the characteristics and microbial-scale habitats of the oldest traces of life on Earth requires the use of multiple complementary methods that will be relevant both for in situ analysis of Martian rocks, as well as for identifying signatures of biological processes (biosignatures) in returned samples. 

In this respect, fossilised chemolithotrophic microorganisms found in ancient volcanoclastic sediments from the East Pilbara craton, Western Australia, an environment having similar conditions to early Mars, can be used as analogues for the kinds of primitive microorganisms that could be found on Mars. We performed combined analyses using FTIR spectroscopy, SEM observations, EDX mapping and LA-ICP-MS in order to investigate the distribution and the molecular and elemental composition of the carbonaceous matter. These results will complete a detailed morphological, mineralogical and geochemical dataset and that will enable the assessment of the astrobiological potential of these Mars analogue sediments.

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21-EPN-FT1-026: Biogeochemical cycling in the lake systems of the Argentinian Puna: An investigation into the microbial communities of an exceptional Hesperian martian analogue

Visit by Ben Tatton, The Open University (UK) to TA1.6 Argentinian Andes (Argentina).
Dates of visit: 17-26 April 2022

Report Summary: Fieldwork undertaken as part of the Europlanet fast track funding call took place between 16/04/22 and 26/04/22 as part of an international team of scientists from The Open University, The Università degli Studi della Tuscia, and The Universidad Nacional de Córdoba.

Fieldwork was conducted at two high-altitude Andean Lake (HAAL) sites, Laguna Negra, and Laguna de Antofagasta. The focus of the research was to collect sediment cores and water samples from Laguna de Antofagasta to assess how microbial communities change as a factor of depth within the sediment. During the trip, a total of 5 x 30 cm cores, 5 x 250 ml of lake water for culturing, and 15 x lake water samples for geochemical analysis were collected. Furthermore, environmental variables were taken with pH, temperature, conductivity, redox potential, and UV monitored. The trip was a resounding success with enough samples taken to permit the progression of my PhD. The data gained from the trip will contribute to two or three data chapters. These chapters will focus on the geochemical characterisation of the site, the microbiology of the site, and potentially simulation experiments which will focus on Noachian/Hesperian Mars relevant metabolisms. We expect to find that LDA is a suitable geochemical analogue for Gale Crater during the Noachian Hesperian transition. We also expect that the types of metabolisms found within the sediments are similar to those predicted to have been present on Noachian/Hesperian Mars.