Skip to Main Content

Geochemistry (235): Peng Ni – Young age of fibrous diamonds from East Africa revealed by in situ Rb-Sr geochronology

Speaker: Peng Ni

Affiliation: UCLA, EPSS

Date: Thursday, June 4, 2026

Time: 12:00 PM


Abstract

Constraining the age of individual diamonds is challenging because diamond itself lacks radioactive parent–daughter nuclides in its lattice for direct dating. I show that recent advancements in mass spectrometry enable in situ Rb–Sr isotope analysis of diamonds containing high-density fluid micro-inclusions. Application of this technique to a suite of diamonds from Kankan, Guinea, demonstrates its high efficiency in Rb-Sr isotope analysis compared with previous bulk methods. The improved spatial resolution also enables potential isochron Rb-Sr dating of these diamonds. One zoned diamond, ON-KAN-381, is found to be 73 ± 81 Ma in age, overlapping kimberlite eruption ages in West Africa. Together, these results place a quantitative constraint on the formation of Kankan fibrous diamonds, indicating that they originated from mantle metasomatism events in the West African continental lithospheric mantle within tens of millions prior to the kimberlite eruption.

PhD Defense: David James – Solid Components in the Deep Interiors of Giant Planets and Super-Earths: A First-Principles Investigation of Magnesium Oxide

Speaker: David James

Affiliation: UCLA, EPSS

Date: Wednesday, June 3, 2026

Time: 9:00 AM

Mentor:

Dr. Lars Stixrude

Location:

Slichter 3853

PhD Defense: Jacob Widmer – Surface Change on Modern Mars as a Record of Atmospheric Drivers

Speaker: Jacob Widmer

Affiliation: UCLA, EPSS

Date: Monday, June 1, 2026

Time: 10:30 AM

Mentor:

Dr. Mackenzie Day

Location:

Slichter 3853

Space Physics (293): Ben Lynch – The Coronal Magnetic Field’s Influence on the Structure of the Inner Heliosphere During Parker Solar Probe’s Encounter 24

Speaker: Ben Lynch

Affiliation: UCLA, EPSS

Date: Friday, May 29, 2026

Time: 3:30 PM


Abstract

The eleven-year solar activity cycle manifests itself in a variety of spectacular and interdependent ways. For example, the spatiotemporal distribution of the emergence of bipolar active regions (ARs) impart a spatiotemporal dependence to the response and re-configuration of overlying large-scale, closed-flux helmet streamer belt. Additionally, specific AR–background field configurations can arise that form new, intermediate-scale closed-flux systems surrounded by single polarity open fields, such as coronal pseudostreamers, which also inherit the underlying solar cycle-dependence of their photospheric flux distributions. The global magnetic structure of the solar corona, in turn, determines the entire solar wind stream and magnetic sector structure of the inner heliosphere. The cusp region of the coronal helmet streamer belt extends into a dense, slow solar wind plasma sheet that contains the heliospheric current sheet (HCS), separating the open fields of opposite polarity. The equivalent heliospheric extension of pseudostreamer outflows along the outer spine-line or spine-fan, result in slow, plasma-sheet like solar wind embedded in a single open field polarity.

In this talk , I will present an overview of the ways in which coronal magnetic field topology, open-closed flux system boundary layers, and their dynamic evolution can determine the resulting solar wind properties and structure of the inner heliosphere. As an illustrative example, I will discuss recent remote-sensing and in-situ observations made by Parker Solar Probe (PSP) in the context of the Casillas et al. [2026] magnetohydrodynamic simulation results. For example, the PSP Encounter 24 observations appear to have captured certain aspects of the Casillas et al. scenario of a global-scale pseudostreamer–to–helmet streamer transition and the generation of outflow transients associated with the opening-up (and closing-down) of a large-scale pseudostreamer flux system which creates (or destroys) the parasitic-polarity solar wind streams and their associated HCSs.

Space Physics (293): Zesen Huang – Democratizing Space Research with AI Agents

Speaker: Zesen Huang

Affiliation: UCLA, EPSS

Date: Friday, May 22, 2026

Time: 3:30 PM


Abstract

Large language models, and the agents built on top of them, are beginning to change how research is done, yet the core ideas remain unfamiliar to many scientists. In this talk, I will explain them from the ground up, assuming no prior background: what a large language model is, what an AI agent is, and what an “agent harness” — the tools, memory, and feedback loop that turn a passive model into something that can act — actually does. I will then turn to why this matters for Earth and space sciences, where reaching a scientific result often means first spending months learning each mission’s data formats and conventions, and describe an effort to build a shared, community-owned skill repository that lets agents handle this competently across subfields. The broader argument is that agents are poised to transform not only everyday scientific work but how people work more generally — and that building the right scaffolding now is what determines whether that promise is realized.

Geochemistry (235): Edwin Schauble – Cerium and europium isotope fractionation

Speaker: Edwin Schauble

Affiliation: UCLA, EPSS

Date: Thursday, May 21, 2026

Time: 1:00 PM


Abstract

Rare earth element abundances have been used to gain key insights into the origin and evolution of silicate melts on the Earth and other planetary bodies. It is now possible to measure natural, non-radiogenic variations in the isotopic compositions of many of these elements, but it’s not clear what controls them. This project aims to estimate equilibrium isotope fractionation in rare earth elements theoretically, which is a challenging problem because both mass dependent and mass independent effects are important. The two redox-sensitive REEs, cerium and europium, are contrasting examples. In the case of Ce(IV) vs. Ce(III), the relative importance of mass-dependent vs. mass-independent fractionation – and even the direction of fractionation – is predicted to be strongly dependent on the isotope pair measured. In the case of europium, mass-independent fractionation is dominant. Eu(II)-bearing species such as plagioclase are predicted to have higher 153Eu/151Eu than Eu(III)-bearing species by ~0.2-0.3‰ at magmatic temperatures, which is in qualitative agreement with recent measurements.

PhD Defense: Matthew Bogumil – The Mantle Crux: Solid-Earth Controls on The Long-Term Carbon Cycle

Speaker: Matthew Bogumil

Affiliation: UCLA, EPSS

Date: Tuesday, May 19, 2026

Time: 2:15 PM

Mentor

Dr. Carolina Lithgow-Bertelloni

PhD Defense: Catherine Psarakis – Probing the Interior Structure of Europa and Ganymede with Magnetic Induction: From Molecular-Scale Ocean Conductivity to Spacecraft Observations

Speaker: Catherine Psarakis

Affiliation: UCLA, EPSS

Date: Wednesday, May 27, 2026

Time: 1:00 PM


Abstract

Mentor

Dr. Abby Kavner

PhD Defense: Kyle Webster – Ultra-low Frequency Waves at Mars: Exploring the Connection Between Surface and Space Through InSight and MAVEN Observation

Speaker: Kyle Webster

Affiliation: UCLA, EPSS

Date: Wednesday, May 20, 2026

Time: 9:00 AM

Mentors

Dr. Hao Cao, Yingjuan Ma

PhD Defense: Francis Dragulet – Magnetic Field Generation in Earth and Super-Earths: The Role of Iron

Speaker: Francis Dragulet

Affiliation: UCLA EPSS

Date: Friday, May 22, 2026

Time: 9:00 AM

Mentor

Dr. Lars Stixrude