• University of Pennsylvania Featured PhD Programmes
  • Staffordshire University Featured PhD Programmes
  • Aberdeen University Featured PhD Programmes
  • FindA University Ltd Featured PhD Programmes
  • University of Tasmania Featured PhD Programmes
  • University of Cambridge Featured PhD Programmes
University of York Featured PhD Programmes
University of Leeds Featured PhD Programmes
Peter MacCallum Cancer Centre Featured PhD Programmes
University College London Featured PhD Programmes
University of Reading Featured PhD Programmes

PhD Geographical and Earth Sciences: Evidence for Recent Water on Mars from the Shergottite Meteorites: Geological, Palaoclimatological and Astrobiological Implications

  • Full or part time
  • Application Deadline
    Applications accepted all year round
  • Self-Funded PhD Students Only
    Self-Funded PhD Students Only

Project Description

2nd Supervisor - Dr Lydia Hallis ()

The shergottite meteorites are igneous rocks that sample the relatively young (150–475 Ma) crust of Mars, and so provide unique and very valuable insights into the planet’s geological evolution. One of the most important questions in Martian geology, climatology and astrobiology is how recently liquid water was present at or near to the planet’s surface, and the shergottites may help answer this question. To date, mineralogical studies on these meteorites have been inconclusive – traces of phyllosilicates and carbonates have been found, but unambiguously attributing them to pre-terrestrial aqueous activity has proven difficult. By contrast, analysis of the ratio of deuterium to hydrogen (D/H) in apatite and glass reveal the presence of water with very high D/H values. This water could be derived from the Martian atmosphere, which is currently highly enriched in deuterium owing to loss of hydrogen to space, or could have been present within the shergottite parent melt. In the latter case the water could have been sourced by the assimilation of crustal materials, which had themselves interacted with the Martian atmosphere. Therefore, the extent to which shergottites record the presence of groundwater within the shallow crust of Mars currently remains unknown.

The goal of this project is to definitively answer the question of whether the shergottites provide evidence for liquid water in the Martian crust by combining petrological, mineralogical and isotopic tools. Initial work will focus on those meteorites that are known to contain secondary minerals. These phases will be located by electron microscopy, then characterised further by a suite of techniques including electron backscatter diffraction, laser Raman spectroscopy and transmission electron microscopy. Such observations may provide clear evidence for the provenance of these minerals (i.e., Martian or terrestrial), but it is likely the conclusive answers will come only from D/H analysis by NanoSIMS. The outcomes of this project will be a new understanding of the history of water late in the geological evolution of the Martian crust that will feed directly into current and future efforts to produce an integrated understanding of the evolution of the atmosphere, lithosphere, and potentially also the biosphere of Mars.

Please refer to the following website for details on how to apply: http://www.gla.ac.uk/research/opportunities/howtoapplyforaresearchdegree/, and contact the principal supervisor for more information.

Funding Notes

This position is available for self-funded students. Funding may be available for home/EU students for the right candidate.

Related Subjects

Email Now

Insert previous message below for editing? 
You haven’t included a message. Providing a specific message means universities will take your enquiry more seriously and helps them provide the information you need.
Why not add a message here
* required field
Send a copy to me for my own records.
Email Sent

Share this page:

Cookie Policy    X