Anthony Lanati

Professur für Petrologie (Prof. Klemme)
Anthony Lanati

Corrensstr. 24, room 124
48149 Münster

T: +49 251 83-36112

Academic ProfilesExternal Profiles
Research Focus

An overview that will blow your damn mind:

Have you ever wondered what the coolest and most interesting rock class on the Earth is? Fear not, it is the potassic and highly-alkaline mafic and ultramafic rocks. You're welcome. What makes them so flipping awesome? Great question, I am glad you asked! Strap in, this is gonna be fun! The melts that eventually crystallise to form these rock upon exhumation are among the most important, enigmatic, and potentially essential magmas for the transport of life essential elements like hydrogen, carbon, phosphorous, nitrogen, and sulfur. These melts also capture some of the first melting processes, and allow us a direct insight in to how nutrients and metals are sequentially concentrated and exchanged between the Earth's mantle, crust, and atmosphere. Bloody hell! That's sick! How do you do that? I use a range of analytical geochemical and experimental techniques to determine the mineralogy and chemistry of rocks collected in the field to piece together their genesis. Sometimes I even make my own rocks in the large hydraulic presses that can cook a rock up to 1800°C, which is a bit like the mad scientist equivalent of baking a cake by building the oven first out of lego. I choose to work with some of the most complex rocks and melts, including some we only think might exist, because the formation of these geological materials encapsulate the true diversity of processes that have made our planet a habitable and cosy home for species like us! Aside from this I have a general interest in high-pressure semi-conductor research, mineral physics, FAIR data and open science principles, and occassionally mummified cats. Want to know more? Check out my publications below, or shoot me an email. Stay funky! Ant

Doctoral AbstractThesis

The origin of ultrapotassic magmas

Supervisor
Prof. Stephan Klemme, PhD
Doctoral Subject
Mineralogie
Targeted Doctoral Degree
Dr. rer. nat.
Awarded by
Department 14 – Geosciences

Alkaline mafic magmas, but more specifically the potassic and ultrapotassic varieties enriched with more potassium (K) than sodium (Na), are essential for our understanding planetary habitability, evolution, and volatile cycles. Despite this importance they have been neglected by the Earth Science community, relative to the more widespread basalts like those that erupt at mid-ocean ridges or ocean islands. The enigmatic nature of these melts has hindered their investigation in part due to analytical challenges such as their propensity to be volatile laden, but also because their genesis is wrapped in paradoxical processed. For example, it is well established that the bulk of the Earth's mantle is made of peridotite which is also known to be largely devoid of K. This alone would more or less eliminate the possibility of mantle--derived melting processes producing magmatic compositions that could crystallise at the surface to form potassic or ultrapotassic rocks. 
The widespread occurrence across all geodynamic settings of K--enriched rock types like lamproites, lamprophyres, leucitites, as well as basanites or shoshonitic basalts is in direct contradiction to this impossibility. Likewise the existence of this rocks, and the fact they represent a spectrum of K enrichments also suggests that for all of them to be derived from melting in the mantle they must be sampling source assemblages with different mineral components. Within the mantle geoscience community this is known as "Mantle Heterogeneity" and as a concept captures processes that produce magmas of all compositions, not just those that are potassic and ultrapotassic. Heterogeneity on this scale is not a widely accepted concept, and debate exists as to the existence and breadth of any non-peridotite assemblage within the mantle. A furtherance to this debate is the complexity added by isolating the type, style, and drivers of any process that could materialise significant changes to both the physical and chemical profiles of the mantle.
These are the central questions that this doctoral thesis aims to approach. Through the use of these unique potassium-rich magmas and rocks that are believed to capture the first stages of mantle melting and sample these heterogeneous regions, this work will evaluate both natural and synthetic samples in the field and laboratory to isolate melting and enrichment processes. In doing so this work will also provide a deeper understanding of potassic rocks and their formation processes.

CV

Academic Education

Doktor der Naturwissenschaften, Institut für Mineralogie, Universität Münster, Münster, Germany (co-tutelle).
PhD in Earth and Planetary Sciences, Macquarie University, Sydney, Australia (co-tutelle).
Master of Research in Earth & Planetary Sciences, Macquarie University, Sydney, Australia.
Bachelor of Science in Geology & Geophyscis, Macquarie University, Sydney, Australia.

Positions

Demonstrator & Tutor (sessional teaching; classes up to 40 students), Department of Earth & Planetary Sciences, Macquarie University. Sydney, Australia.
Lab Manager - High Pressure Experimental, Department of Earth & Planetary Sciences, Macquarie University. Sydney, Australia.
Research Assistant - Sydney Water project, Department of Earth & Planetary Sciences, Macquarie University. Sydney, Australia.
Summer Research Intern - Sample Environment Team, Australian Centre for Neutron Scattering, Australian Nuclear Science and Technology Organisation (ANSTO). Lucas Heights, Sydney, Australia.
Publications

Abstract in a Digital Collection (Conferences)
Research Articles in a Digital Collection

Research Article (Journal)
Review Article (Journal)
  • , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , , and . . “Community recommendations for geochemical data, services and analytical capabilities in the 21st century.Geochimica et Cosmochimica Acta 351: 192205. doi: 10.1016/j.gca.2023.04.024.

Research Articles (Journals)
Research Articles in a Digital Collection

Research Article in Edited Proceeding (Conference)
Abstracts in Edited Proceedings (Conferences)