
Prof Ian Franchi
Emeritus Professor of Planetary Science
Faculty of Science, Technology, Engineering & Mathematics
Biography
Research interests
My research focuses on the origin and evolution of the early solar system, primarily through the detailed investigation of the chemical and isotopic composition of meteorites, interplanetary dust particles and other materials returned by space missions using a range of advanced analytical techniques.
Key methods include the development and application of mass spectrometry for high precision oxygen isotope measurements and NanoSIMS (a secondary ionisation mass spectrometer with nano-metric spatial resolution for chemical and isotopic measurements on samples in situ with a spatial resolution down to <100 nm).
Acquisition of new samples is an important aspect to help address new science questions, and throughout my career I have sought to enhance the materials available to both my own research and the wider community through sample collection programmes, collaboration with many colleagues around the world and involvement in sample return space missions, including playing a leading role in developing proposals for asteroid sample return missions.
My current focus is on the study of samples of primitive asteroidal material returned by the JAXA Hayabusa2 and NASA OSIRIS-REx missions.
Projects
Understanding Origins at the Open University (SM-10-008-MG)
PSSRI Rolling Grant. A very wide range of projects that span sample analysis and the early solar system, to conditions on Mars, observational astronomy of asteroids, to instrumentation and engineering for future missions.
DTG 2014
DTG 2014
ARRAKHIS testing
The CEI will perform and provide pre- and post-irradiation characterisation and test results from a Teledyne e2v CIS device. The test results will support ESA’s ARRAKHIS project Mission Definition Review and CMOS and CCD trade off. The main objective of the activity is to establish whether CIS (CIS300) can be considered as a valid ARRAKHIS detector option, in advance of the first ITT release in Q1 2024.
Planetary Science Consolidated Grant 2020-2023
STFC Planetary Science Consolidated grant - details to be entered here.
Nanosims Laboratory Services
Nanosims Laboratory Services - Laboratory Income for Services
STFC Open 2018 DTP
STFC Open 2018 DTP
European CurAtion of Returned Extra-terrestrial Samples
The overall objective of EURO-CARES is to create a roadmap for the implementation of a European Extra-terrestrial Sample Curation Facility (ESCF). . During the course of this 36 month project we will: [1] Review the current state of the art in extraterrestrial sample curation, by examining work done in Europe and internationally and to write a technical report on this topic; [2] Devise a plan for terrestrial planetary protection that is realistic, effective and legally compliant, while minimising risk to current and future scientific study; [3] Review current knowledge and essential requirements for facilities, including building infrastructure and design, procedures and protocols, security, environmental conditions, documentation and databasing; [4] Review most the suitable instrumentation for sample analysis, establish the optimum methods and instrumentation and identify those areas in which innovation and development will be required to enhance curation and analysis capabilities.. [5] Make recommendations regarding the use of analogue samples as proxies for returned extraterrestrial materials. We will deliver guidelines and lists and recommendations ready to be used in the event of a sample return mission. The analogue proxies are necessary in a curatorial facility for testing sample handling, storage and preparation techniques. This includes the testing of planetary protection measures as well as for validating new analytical methods. [6] Review suitable portable receiving facilities and outline the needs for innovation in order to be able to handle samples most effectively.
Natural History Museum Based STFC Funded Studentship
The solar system formed from a disk of dust and gas, and this can be analysed using meteorites that date from this time. The student will undertake a detailed study of materials that date from this time and place - specifically the enstatite meteorites, which may have originated in the innermost part of the disk. Chondritic meteorites are relicts from the early solar system composed largely of sub-spherical μm-to-mm sized objects called chondrules. Enstatite chondrites are isotopic twins to the Earth-Moon system, suggesting a genetic connection. In addition, recent orbital data from the MESSENGER mission to Mercury have shown that it has chemical similarities to the enstatite chondrites, for example high sulphur abundances and Mg/Si ratios. This rare meteorite group (only around 500 enstatite meteorites are known) are therefore highly likely to be products of the inner solar system; if not direct ancestors then possible 'aunts' to the terrestrial planets. The enstatite chondrites are remarkable for their extremely reduced mineralogy; sulphides and metal are very abundant and the main silicate is FeO-poor enstatite. Reduced C and N bearing minerals such as SiC, graphite and nierite (Si3N4) are relatively abundant. High temperature solids such as calcium aluminium-rich inclusions (CAIs) are rare. The student will analyse the chemistry and isotope systematics of individual, pristine, chondrules, CAIs and isolated sulphide grains from the most primitive available enstatite chondrites. We will use petrographic techniques to locate possible precursor grains in the chondrules. By comparing these to later generated components we can assess how the inner protoplanetary disk composition evolves during its several million year lifetime. Age information will be acquired by measuring the initial abundance of 26Al/27Al in suitable phases (e.g. chondrule mesostasis) at the Open University to enable this compositional evolution to be monitored quantitatively. We will analyse the composition of trace elements in the major phases in enstatite chondrites using ICP-MS and Synchrotron x-ray microscopy as a tool to track the evolution of chondrules and their interaction with the surrounding gas.
Planetary Science at the Open University 2017-2020
Our proposed research programme addresses the origin and evolution of the Solar System, including surfaces, atmospheres and physical, geological, chemical and biological processes on the terrestrial planets, the Moon, asteroids, comets, icy satellites and extraterrestrial materials, in a range of projects which address the STFC Science Roadmap challenge B: “How do stars and planetary systems develop and is life unique to our planet?” The inner rocky bodies of the Solar System are of particular importance in understanding planetary system evolution, because of their common origin but subsequent divergent histories. Lunar samples will be used to determine the abundance and composition of volatile elements on the Moon, their source(s) in the lunar interior, and processes influencing their evolution over lunar geological history. Oxygen isotope analysis will be used to determine the conditions and processes that shape the formation of materials during the earliest stages of Solar System formation. Mars is the focus of international Solar System exploration programmes, with the ultimate aim of Mars Sample Return. We will: investigate the martian water cycle on global and local scales through a synthesis of atmospheric modeling, space mission data and surface geology; assess potential changes in the composition of Mars’ atmosphere over time through measurement of tracers trapped in martian meteorites of different ages; and determine whether carbon dioxide, rather than water flow, is able to account for recently active surface features on Mars. Mercury is an end-member in the planet-formation spectrum and we plan to exploit NASA MESSENGER data to study its origin and crustal evolution, and prepare for ESA’s BepiColombo mission. The cold outer regions of the Solar System, and particularly comets, are believed to have retained some of the most pristine primitive material from their formation. We plan to probe the composition and origins of cometary material and understand the processes that drive cometary activity through: laboratory analysis of the most primitive Interplanetary Dust Particles; and direct measurements of a comet by our instruments on the Rosetta mission, together with laboratory simulations. We will conduct laboratory ultraviolet observations of irradiated ices to provide new insights into the composition of Solar System ices and how they may create atmospheres around their parent bodies. We will also investigate the role volatiles can play in the cohesion (“making”) of Solar System minor bodies, and the fragmentation that can be achieved by thermal cycling (a candidate process that “breaks” them). The question of whether Earth is a unique location for life in the Solar System remains one of the most enduring questions of our time. We plan to investigate how the geochemistry of potentially habitable environments on Mars, Europa and Enceladus would change over geological timescales if life was present, producing distinguishable biomarkers that could be used as evidence of life in the Solar System. We will study the role of hypervelocity impacts in: the processing of compounds of critical interest to habitability (water, sulfur-species, organic species) during crater formation; and the hydrothermal system of the 100 km diameter Manicouagan impact structure in Canada to assess the astrobiological implications of hydrothermal systems for early Mars. In addition to satisfying humanity’s innate desire to explore and understand the Universe around us, our research has more tangible benefits. We use the analytical techniques involved from development of space and laboratory instrumentation for applications with companies in fields as diverse as medicine, security, tourism and cosmetics. One of the most important benefits of our research is that it helps to train and inspire students - the next generation of scientists and engineers – through training within the University and public outreach and schools programmes.
EUROPLANET 2020 RI
The Europlanet 2020 Research Infrastructure (EPN2020-RI) will address key scientific and technological challenges facing modern planetary science by providing open access to state-of-the-art research data, models and facilities across the European Research Area. Its Transnational Access activities will provide access to realistic analogue field sites for Mars, Europa and Titan, and world-leading laboratory facilities that simulate conditions found on planetary bodies. Its two Virtual Access activities will make available the diverse datasets and visualisation tools needed for comparing and understanding planetary environments in the Solar System and beyond. By providing the underpinning facilities that European planetary scientists need to conduct their research, EPN2020-RI will create cooperation and effective synergies between its different components: space exploration, ground-based observations, laboratory and field experiments, numerical modelling, and technology. EPN2020-RI builds on the foundations of the previous FP6 and FP7 Europlanet programmes that established the ‘Europlanet brand’ and organised structures that will be used in the Networking Activities of EPN2020-RI to coordinate the European planetary science community’s research. Furthermore, it will disseminate its results to a wide range of stakeholders including ERA industry, policy makers and, crucially,both the wider public and the next generation of researchers and opinion formers, now in education. As an Advanced Infrastructure we place particular emphasis on widening the participation of previously under-represented research communities and stakeholders. We aim to include new countries and Inclusiveness Member States, via workshops, team meetings, and personnel exchanges, to improve the scientific and innovation impact of the infrastructure. EPN2020-RI will therefore build a truly pan-European community that shares common goals, facilities, personnel, data and IP across national boundaries.
Grant Amendment to Europlanet 2020 RI
This is a grant amendment to Europlanet RI 93328 - all documents in this sharepoint folder
The Volatile Legacy of the Early Earth - (2)
Nanosims service to Bristol NERC project
Astronomy and Planetary Sciences at the Open University
The aim of our programme in Astronomy & Planetary Science at the Open University (APSOU) is to carryout detailed investigations of the origin and evolution of galaxies, stars and planets with a special emphasis on our own Solar System through a combination of observation, simulation, laboratory analysis and theoretical modelling. Our research is divided into two broad areas, reflecting the historical research strengths. This research programme is well-matched to both nationally- and internationally-agreed research imperatives. In its final report, A Science Vision for European Astronomy2, Astronet’s Science Working Group identified four broad areas of strategic importance; our research covers major topics within each of these areas. APSOU projects also map onto two of the four Science Challenges that form STFC’s Road Map3 for science (‘How did the universe begin and how is it evolving?’ and ‘How do stars and planetary systems develop and is life unique to our planet?’). The present APSOU programme comprises 20 projects (labelled A to T), of which 6 are for consideration by the Astronomy Observation (AO) panel, 1 for Astronomy Theory (AT), and 13 for the Planetary Studies (PL) panel. The AO projects cover the breadth of the 7 themes recognised as UK strengths in the report of STFC’s Astronomy Advisory Panel (AAP), whilst the 13 PL projects are directed towards answering questions raised in two of the three themes identified as UK strengths in the roadmap of STFC’s Solar System Advisory Panel (SSAP)4.
Physical and Chemical Properties of Matrix in Primitive Chondrites (SP-12-086-IF)
STFC studentship awarded to NHM to study primitive meteorites. The NHM have already identified a suitable candidate (Epifanio Vaccaro), who has also visited/been interviewed at Open University and who has been judged of appropriate calibre to undertake a PhD. The student will be based at the NHM, with the principle supervision from Sara Russell. We have been approached as the degree awarding instituition, and for Ian Franchi (and possibly Natalie Starkey, funded 100% on HGSM A4102 Rolling Grant) to act as additional supervisors. All lab work will be undertaken at the NHM - no office space, computer, etc is required at the Open University, although the student will attend occassional training courses, etc. The money is awarded to NHM, who will manage the resources, including stipend, travel, RTSG. The fees (which include registration, bench fees, tuition fees, etc) will be split 50:50 between the NHM and OU, (costed assuming 3.5 years). Agreed with James Bruce.
MarcoPolo-R: Cosmic Vision M3 Assessment Phase support (SM-11-073-SG)
MarcoPolo-R is a sample return mission to a primitive Near-Earth Asteroid (NEA) selected as a candidate mission for the European Space Agency’s Cosmic Vision programme. It will rendezvous, scientifically characterize it at multiple scales, and return a unique sample to Earth unaltered by the atmospheric entry process or terrestrial weathering. Small bodies, as primitive leftover building blocks of the solar system formation process, offer clues to the chemical mixture from which the planets formed some 4.6 billion years ago. In addition, they retain material that predates the solar system and contains evidence for interstellar processes and its original formation in late-type stars. Current exobiological scenarios for the origin of life on Earth invoke an exogenous delivery of organic matter: primitive bodies could have brought these complex organic molecules capable of triggering the pre-biotic synthesis of biochemical compounds on the early Earth. Moreover, collisions of NEAs with the Earth pose a finite hazard to life. For all these reasons, the exploration of such objects is particularly interesting and urgent and it is no surprise that sample return missions are considered a priority by a number of the leading space agencies. This proposal is for funds to support UK participation in the MarcoPolo-R mission Assessment Phase, in particular to support OU staff in the development of the mission through their work in the ESA Science Study Team.
UKCAN NanoSIMS Access for Glasgow Consolidated Grant
This is to provide shortfall in funding for nanosims time required in Glasgow Consolidated grant awarded 2013 for a 3 year pdra project. NanoSIMS time was to be requested thru UKCAN - unfortunately OU funding to provide UKCAN access to nanosims was not awarded in 2014 OU consolidated grant - and therefore no funding was present either at OU or Glasgow to allow nanosims measurements critical to the project. STFC have agreed to fund the 3 weeks (15 days) of outstanding work thru the standard URGENCY scheme. Funding valid until 31 March 2015.
Publications
Book Chapter
A roadmap for a European extraterrestrial sample curation facility – the EURO CARES project (2021)
Journal Article
An evaporite sequence from ancient brine recorded in Bennu samples (2025)
Phosphorus-rich grains in Ryugu samples with major biochemical potential (2024)
Evidence against water delivery by impacts within 10 million years of planetesimal formation (2024)
Asteroid (101955) Bennu in the laboratory: Properties of the sample collected by OSIRIS ‐ REx (2024)
Quantitative evolved gas analysis: Winchcombe in comparison with other CM2 meteorites (2024)
Insoluble macromolecular organic matter in the Winchcombe meteorite (2024)
Detection of apatite in ferroan anorthosite indicative of a volatile-rich early lunar crust (2024)
Chondritic chlorine isotope composition of acapulcoites and lodranites (2024)
A primordial noble gas component discovered in the Ryugu asteroid and its implications (2024)
The impact history and prolonged magmatism of the angrite parent body (2024)
The Winchcombe meteorite—A regolith breccia from a rubble pile CM chondrite asteroid (2023)
The grain size distribution of matrix in primitive chondrites (2023)
Oxygen isotope evidence from Ryugu samples for early water delivery to Earth by CI chondrites (2023)
The Winchcombe meteorite, a unique and pristine witness from the outer solar system (2022)
Sierra Gorda 013: Unusual CBa‐like chondrite (2022)
A pristine record of outer Solar System materials from asteroid Ryugu’s returned sample (2022)
Carbonate assemblages in Cold Bokkeveld CM chondrite reveal complex parent body evolution (2021)
A deuterium-poor water reservoir in the asteroid 4 Vesta and the inner solar system (2021)
Organic matter and water from asteroid Itokawa (2021)
The Loongana (CL) group of carbonaceous chondrites (2021)
Terrestrial Alteration Mineral Assemblages in the NWA 10416 Olivine Phyric Shergottite (2020)
Preservation of primordial signatures of water in highly-shocked ancient lunar rocks (2020)
Multiple early-formed water reservoirs in the interior of Mars (2020)
Cosmic spherules from Widerøefjellet, Sør Rondane Mountains (East Antarctica) (2020)
One of the earliest refractory inclusions and its implications for solar system history (2020)
Sierra Gorda 009: A new member of the metal‐rich G chondrites grouplet (2020)
Linking asteroids and meteorites to the primordial planetesimal population (2020)
The chlorine isotopic composition of the Moon: Insights from melt inclusions (2019)
Organics preserved in anhydrous interplanetary dust particles: Pristine or not? (2019)
Experimental insights into Stannern‐trend eucrite petrogenesis (2018)
Basaltic Volcanism On The Angrite Parent Body: Comparison With 4 Vesta (2018)
OSIRIS-REx Contamination Control Strategy and Implementation (2018)
A mutli-technique search for the most primitive CO chondrites (2018)
Bunburra Rockhole: Exploring the geology of a new differentiated asteroid (2017)
A divergent heritage for complex organics in Isheyevo lithic clasts (2017)
The mineralogy, petrology, and composition of anomalous eucrite Emmaville (2017)
The Braunschweig meteorite − a recent L6 chondrite fall in Germany (2017)
Water in evolved lunar rocks: Evidence for multiple reservoirs (2016)
Early degassing of lunar urKREEP by crust-breaching impact(s) (2016)
The abundance and isotopic composition of water in eucrites (2016)
An asteroidal origin for water in the Moon (2016)
Triple oxygen isotopic composition of the high-3He/4He mantle (2016)
Cosmochemical and spectroscopic properties of Northwest Africa 7325 - A consortium study (2016)
The Vicência meteorite fall: A new unshocked (S1) weakly metamorphosed (3.2) LL chondrite (2015)
A water–ice rich minor body from the early Solar System: The CR chondrite parent asteroid (2014)
Isotopic diversity in interplanetary dust particles and preservation of extreme 16O-depletion (2014)
The origin of water in the primitive Moon as revealed by the lunar highlands samples (2014)
Abundances of presolar silicon carbide grains in primitive meteorites determined by NanoSIMS (2014)
The Paris meteorite, the least altered CM chondrite so far (2014)
Light element geochemistry of the Chelyabinsk meteorite (2013)
Insight into the silicate and organic reservoirs of the comet forming region (2013)
Stable isotope analysis of carbon and nitrogen in angrites (2013)
Tissint martian meteorite: a fresh look at the interior, surface, and atmosphere of Mars (2012)
Jiddat al Harasis 556: A howardite impact melt breccia with an H chondrite component (2012)
Maribo-A new CM fall from Denmark (2012)
The Australian Desert Fireball Network: a new era for planetary science (2012)
Active Cosmic Dust Collector (2012)
MarcoPolo-R near Earth asteroid sample return mission (2012)
Petrology and geochemistry of the Northwest Africa 3368 eucrite (2011)
Jiddat al Harasis 422: a ureilite with an extremely high degree of shock melting (2011)
Microbial endolithic colonization and the geochemical environment in young seafloor basalts (2010)
The relationship between CK and CV chondrites (2010)
Iron oxides in comet 81P/Wild 2 (2010)
Trace element geochemistry of K-rich impact spherules from howardites (2009)
MARCO POLO: near earth object sample return mission (2009)
The Puerto Lápice eucrite (2009)
The Fountain Hills unique CB chondrite: Insights into thermal processes on the CB parent body (2009)
An anomalous basaltic meteorite from the innermost main belt (2009)
Crustal partial melting on Vesta: evidence from highly metamorphosed eucrites (2009)
The petrology and geochemistry of Miller Range 05035: A new lunar gabbroic meteorite (2008)
Geochemistry of diogenites: still more diversity in their parental melts (2008)
Marco Polo: near Earth object sample return mission (2008)
Discovery of non-random spatial distribution of impacts in the Stardust cometary collector (2008)
Ararki (L5) chondrite: The first meteorite find in Thar Desert of India (2008)
Studying the oxygen and carbon isotope characteristics of carbonate analogues to ALH 84001 (2008)
Petrographic classification of Middle Ordovician fossil meteorites from Sweden (2007)
Comet 81P/Wild 2 Under a Microscope (2006)
Impact features on Stardust: implications for comet 81P/Wild 2 dust (2006)
Infrared spectroscopy of comet 81P/Wild 2 samples returned by Stardust (2006)
Elemental compositions of comet 81P/Wild 2 samples collected by Stardust (2006)
Organics captured from comet 81P/Wild 2 by the Stardust spacecraft (2006)
Oxygen isotope variation in stony-iron meteorites (2006)
Petrology and geochemistry of the fine-grained, unbrecciated diogenite Northwest Africa 4215 (2006)
Petrography and geochemistry of the chassignite Northwest Africa 2737 (NWA 2737) (2006)
Widespread magma oceans on asteroidal bodies in the early Solar System (2005)
Alteration and metamorphism of CO3 chondrites: evidence from oxygen and carbon isotopes (2004)
Pinpointing the source of a lunar meteorite: implications for the evolution of the moon (2004)
Further characterisation of the 91500 Zircon Crystal (2004)
Geochemistry of carbonaceous impactites from the Gardnos impact structure, Norway (2003)
The Genesis solar-wind collector materials (2003)
Clay mineral-organic matter relationships in the early solar system (2002)
Mass-independent fractionation of oxygen isotopes during thermal decomposition of carbonates (2002)
Sayh al Uhaymir 094: a new martian meteorite from the Oman desert (2002)
A 'Mesosiderite' rock from northern Siberia, Russia: not a meteorite (2002)
Carbon and nitrogen isotope disturbances and an end-Norian (Late Triassic) extinction event (2002)
Oxygen isotopes and the early solar system (2001)
Chemical and isotopic characteristics of the Didwana-Rajod (H5) chondrite (2001)
Presentation / Conference
The shock response of apatite and its effect on volatiles in eucrites (2022)
Volatile Inventory of Lunar Meteorites from the Dominion Range (2022)
Chlorine and hydrogen in brecciated lunar meteorites: implications for lunar volatile history (2021)
The Hydrogen and Chlorine Isotopic Composition of Highly Shocked Eucrites (2020)
Chlorine in Brecciated Lunar Meteorite Nwa 12593: Implications for Lunar Volatile History (2020)
Apatite Microstructures and its Volatile Composition in Eucrites (2019)
EURO-CARES - A European Sample Curation Facility for Sample Return Missions (2019)
Cooling rates of chondrules from diffusion profiles in relict olivine grains (2018)
Europe's future exploration of Main Belt Comets (2018)
Cooling rate of chondrules from diffusion profiles in relict olivine grains (2018)
Linking volatiles and microstructures in apatite from eucrites (2018)
NWA 10989 – A New Lunar Meteorite with Equal Proportions of Feldspathic and VLT Material (2017)
Ion Microprobe Analyses of Trace Elements in Lunar Apatites (2017)
Chlorine in Lunar Basalts (2017)
Constraining the Cooling Rates of Chondrules (2017)
Mineralogy and petrology of the Murrili meteorite (2016)
Northwest Africa 10639 and 10640: Two new monomict eucrites from Sahara (2016)
Chlorine isotope variation in eucrites (2016)
NWA 10659: A CLAY-RICH NAKHLITE PAIR OF NWA 10153 (2016)
Constraining the cooling rates of chondrules (2016)
Constraining the cooling rates of chondrules (2016)
Oxygen isotopes and origin of opal in an Antarctic ureilite (2016)
Northwest Africa 10319 and 10320: two new cumulate eucrites from Sahara (2016)
Textural and minerochemical features of Dar al Gani 1067, a new CK chondrite from Libya (2016)
Continuing the search for the most primitive CO chondrites: The oxygen isotope perspective (2016)
Pyroxene-plagioclase pallasite Northwest Africa 10019: Where does it belong? (2016)
Enon and Puente del Zacate: A duo of primitive-silicate-bearing magmatic irons (2016)
Origin of opal (hydrated silica) in polymict ureilites (2016)
Choteau makes three: A characterization of the third member of the Vermillion subgroup (2016)
The isotopic composition of chlorine in apatite from eucrites (2016)
Combined chemical-oxygen isotope study of large igneous inclusions in ordinary chondrites (2016)
The Mineralogy and Petrology of Anomalous Eucrite Emmaville (2015)
Understanding the Chlorine Isotopic Compositions of Apatites in Lunar Basalts (2015)
Apatite-Melt Volatile Partitioning Under Lunar Conditions (2015)
Volatiles in the lunar crust - an evaluation of the role of metasomatism (2015)
Determining the source(s) of water in the lunar interior (2015)
Apatite: a versatile recorder of the history of lunar volatiles (2014)
Using apatite to unravel the origin of water in ancient Moon rocks (2014)
The abundance and isotopic composition of water in howardite-eucrite-diogenite meteorites (2014)
Bunburra Rockhole: Exploring the geology of a new differentiated basaltic asteroid (2014)
Using lunar apatite to assess the volatile inventory of the Moon (2013)
Graphitic Raman spectra in angrites: a source of high-temperature carbon? (2013)
In-situ nanoSIMS measurements of isotopic hotspots in the CM2 meteorite Cold Bokkeveld (2013)
Water in the Moon: insights from SIMS analyses of lunar apatites (2012)
Apollo 15 low-Ti and KREEP basalts: two distinct "water" reservoirs? (2012)
Investigating the water contents and hydrogen isotopic compositions of lunar apatite (2012)
A trapped nitrogen component in angrites (2012)
Lunar volatiles: an examination of hydrogen isotopes and hydroxyl content (2012)
Hydrogen and lead isotopic characteristics of lunar meteorite MIL 05035 (2012)
The hydroxyl content and hydrogen isotope composition of Lunar apatites (2012)
A preliminary study of magmatic volatiles in angrites (2011)
Origin and composition of carbonates, sulphates and halite on Mars (2011)
NanoSIMS oxygen isotope analyses on Grigg-Skjellerup collection IDPs (2011)
Raman variation of organic matter in large cluster IDPs and meteoritic IOM (2011)
Origin of the ungrouped achondrite NWA 4518: mineralogy and geochemistry of FeNi-metal (2011)
NWA 6356: unequilibrated polymict ureilite (2011)
Oxygen isotope analysis of a chondrule-like Wild 2 Terminal Particle using NanoSIMS (2011)
Investigating Raman variation across large cluster interplanetary dust particles (2011)
Isotope measurements of a comet by the Ptolemy instrument on Rosetta (2010)
UK CAN: UK Cosmochemical Analysis Network for the study of returned samples from space (2010)
Martian subsurface fluid pathways revealed by 3D mineralogy of the Nakhla meteorite (2010)
A combined carbon and oxygen isotopic analysis of ALH84001 carbonates with NanoSIMS (2010)
Presolar grain inventories of the ungrouped C3 Adelaide and the CV3 RBT 04133 (2010)
Nakhlites and NanoSIMS via micro-CT characterisation (2010)
Determining the carbon isotopic composition of ALH84001 rosettes with NanoSIMS (2010)
NWA 4537: A new Aubrite from northwest Africa (2010)
NWA 4415 AND 4416: Two new enstatite chondrites from northwest Africa (2010)
Northwest Africa 5790. Top Sequence of the Nakhlite Pile (2010)
Distinctive impact craters are formed by organic rich cometary dust grains (2010)
RBT 04133: a new, unusual carbonaceous chondrite (2009)
Impact histories of Vesta and Vestoids inferred from howardites, eucrites and diogenites (2009)
NWA 4477: A unique impact melt breccia (2009)
NWA 4418: A new mesosiderite from Northwest Africa (2009)
Textural and compositional features of NWA 4222, A new Martian meteorite (2009)
NWA 4419: A new R chondrite from Northwest Africa (2009)
STONE 6: Artificial Sedimentary Meteorites in Space (2008)
Oxygen Isotopic Constraints on the Number and Origin of Basaltic Achondrite Parent Bodies (2008)
The Meteorite Fall in Carancas, Lake Titicaca Region, Southern Peru: First Results (2008)
Tafassasset: The Saga Continues (2008)
Mineralogy and Geochemistry of Shergottite RBT 04262 (2008)
Marco Polo: A near Earth object sample return mission (2008)
Towards the isotopic measurement of solar wind carbon in the Genesis silicon target (2007)
Reflectance spectra of Mesosiderites: Implications for asteroid 4 Vesta (2007)
Oxygen isotope composition of the primitive Achondrites (2007)
The Moss (CO3) meteorite: an integrated isotopic, organic and mineralogical study (2007)
Non-random spatial distribution of impacts in the Stardust Cometary Collector (2007)
Could Stannern-trend eucrites be crustal-contaminated melts? (2007)
Stardust microcrater residue compositional groups (2007)
Asteroidal differentiation processes deduced from ultramafic achondrite ureilite meteorites (2006)
Petrology and geochemistry of the NWA 3368 Eucrite (2006)
Experimental study of laboratory-heated CM2 chondrites Mighei and Murchison (2006)
Isheyevo Meteorite: Genetic link between CH and CB chondrites? (2006)
Microcraters in aluminum foils exposed by Stardust (2006)
Extraction and analysis of microcrater residues using focused ion beam microscopy (2006)
New oxygen isotope evidence for the origin of mesosiderites and main group pallasites (2006)
Application of semiconductor industry cleaning technologies for Genesis sample collectors (2006)
A new CK carbonaceous chondrite from Hammada Al Hamra, Libya (2006)
A new CO carbonaceous chondrite from Acfer, Algeria (2006)
The effect of atmospheric entry heating on micrometeorite volatile composition (2006)
A new CH carbonaceous chondrite from Acfer, Algeria (2006)
Petrology and geochemistry of the NWA 3368 Eucrite (2006)
Amino acids composition and oxygen isotopes in the Shisr 033 CR chondrite (2005)
High-temperature chemical processing on asteroids: An oxygen isotope perspective (2005)
Oxygen isotopic variation of asteroidal materials (2005)
Evolved gas analysis of hydrated phases in Murchison and Orgueil (2005)
Aqueous alteration of Nakhlites: implications for water on Mars (2005)
The Diderot meteorite: The second chassignite (2005)
The Fountain Hills meteorite: A new CBa chondrite from Arizona (2004)
Solar and solar-wind oxygen isotopes and the Genesis mission (2004)
Oxygen isotopic variation of the terrestrial planets (2004)
The relationship between CK and CV chondrites: a single parent body source? (2004)
Lunar meteorite SaU 169; An extremely KREEP-rich rock (2003)
Al Mala'ika (NWA 1669): A new Shergottite from Morocco: mineralogy and petrology (2003)
Oxygen isotope evidence for the origin of HEDs and Angrites (2003)
Are CK chondrites really a distinct group or just equilibrated CVs? (2003)
An investigation of carbon in Dar Al Gani 319 Polymict Ureilite (2003)
The oxygen isotopic composition of water extracted from unequilibrated ordinary chondrites (2003)
Terrestrial ages of some meteorites from Oman (2002)
Carbon and oxygen isotopes in CO3 chondrites (2002)
Dar Al Gani 896: A unique picritic achondrite (2002)
Laser ablation of Diamond and Genesis concentrator target material (2002)
Oxygen isotopes in CO3 chondrites (2002)
Search for Q: single grains Xe isotope analysis of carbonaceous residue from Yilmia (2002)
Oxygen isotopes in water extracted from carbonaceous chondrites (2001)
Itqiy: II. a short story about its noble gases and oxygen isotopes (2001)
Characterisation of extraterrestrial samples by Raman and Electron microprobes (2001)
Noble gases in Tagish Lake (2001)
Ureilite Graphite: Shocking implications (2001)
The oxygen isotopic composition of water extracted from carbonaceous chondrites (2001)
Continued investigation of the light element geochemistry of Tagish Lake (2001)
New data on carbon isotopic compositions of some ureilites (2001)
Near-Earth asteroid sample return missions (2001)
The association between organic matter and clay minerals in carbonaceous chondrites (2001)
Report
Marco Polo Near-Earth Asteroid Sample return mission. Assessment Study Report (2009)
Thesis
Nitrogen Isotopic Variation in Irons and Other Fe-Ni Metal Rich Meteorites (1988)