PhD position in Experimental Volcanology & Fluid-Rock-Interaction in the context of the Emergence of Life at LMU Munich

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From: Bettina Scheu <bettinascheu.lmu@xxxxxxxxxxxxxx>



*PhD position in Experimental Volcanology & Fluid-Rock-Interaction in the
context of the Emergence of Life at LMU*


Do you want to find out how and in which environments life could have
originated on early Earth? Within the CRC 392 (collaborative research
center, https://www.molecular-evolution.de/
<https://urldefense.com/v3/__https://www.molecular-evolution.de/__;!!IKRxdwAv5BmarQ!a-klkTfz92zb0NQ3cOsIIFk-opSx6QYqpJhS8lErT2MhQn7fe1_U-GVaLPefyPeFP6zkMh3kN_giCj2E2ucJCXKqgw$>
),
we bring together young and experienced researchers to foster and grow our
cross-disciplinary network on the Emergence of Life research. We will
integrate the initial boundary conditions of early Earth from biophysics,
geoscience, astronomy and chemistry for innovative lab experiments.


*Then apply for this PhD position in Experimental Volcanology &
Fluid-Rock-Interaction in the context of the Emergence of Life at LMU!*


This project explores shallow geothermal environments driven by magmatic
activity on their potential to act as physical-chemical factories where
prebiotic reactions are catalyzed by glass /mineral - fluid reactions.
Shallow geothermal systems span a broad range of pressure, temperature and
pH values, and their fluids often source from deeper sub-volcanic/magmatic
regions, connected by system-spanning transport processes such as gas and
fluid flow through a permeable fracture network.


The goals of this project are (i) to explore chemical gradients and
silicate-glass/mineral reactivity to e.g. liberate phosphorus,
lanthanides;  (ii) explore the fertilization capacity of volcanic ashes
introduced into aqueous systems as erupted ash is known for its scavenging
capacity binding salts and is via volcanic lightning also a likely source
for as possible source for simple prebiotic compounds ( such as NH3,
HCN,..), and (iii) to expand the current understanding of fluid-rock
interactions under early earth conditions and chemical reactions from
shallow to deeper environments to bridge the gap between shallow geothermal
and sub-volcanic/magmatic systems.


We seek an outstanding and highly motivated candidate, eager to work in a
highly interdisciplinary research group. Experience in experimental
laboratory work as well as in optical, petrological and geochemical
analysis (e.g. XRD, Raman, SEM, EMPA, xCT, XRD) will be highly beneficial.
Candidates should have a MSc in a relevant area (petrology, geochemistry,
volcanology, Earth sciences).

The PhD student will be hosted at the Department of Earth and Environmental
Sciences at LMU Munich, Germany. Within the CRC392 excellent
interdisciplinary training, and networking activities are provided.

Please apply with a CV, motivation letter, transcript of academic record,
publications (if existing), and 2 references to Prof. Bettina Scheu
<b.scheu@xxxxxx> <b.scheu@xxxxxx>.

Evaluation of the applications will start 25.06.2024, until the positions
are filled. The projects can start October 2024 and is funded for
3-years (TV-L-E13
(75%).

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