Events
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UTIG Seminar Series: Marianne Karplus, UT El Paso
Start:November 1, 2024 at 10:30 am
End:
November 1, 2024 at 11:30 am
Location:
PRC 196/ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Marianne Karplus, Associate Professor, Earth, Environmental and Resource Sciences, The University of Texas at El Paso
Host: Ginny Catania
Title: Echoes from the edge of Thwaites Glacier, Antarctica: from tectonics to ice flow dynamics
Abstract: The Thwaites Interdisciplinary Margin Evolution (TIME) project illuminates the control that shear margin dynamics have over the future evolution of ice flow in the Thwaites-Amundsen drainage basin. To examine the physical processes and properties at the shear margin, we set up field geophysical observatories between 2019 to 2024 at several locations along the shear margin to study the ice as well as the geology below. I will present results from our seismicity study, describing earthquakes and icequakes recorded by two 7-station passive broadband seismic networks deployed between 2019-2021. Then I will present preliminary images and observations from 2-D and 3-D controlled-source seismic surveys acquired across the Thwaites shear margin in 2023-24, with 1000 3-component seismic nodes deployed in a 27-km line and 3 by 5.5-km seismic grid. We detonated 671 seismic sources, mostly “Poulter” sources with 4-kg explosive boosters suspended on a 6-foot bamboo pole. The seismic signals were recorded across the full extent of the seismic line and grid and penetrated into the bed beneath the ice (~2000-km-thick), allowing for englacial, bed, and geologic imaging and interpretation.
Bureau of Economic Geology Seminar Series
Start:November 5, 2024 at 10:00 am
End:
November 5, 2024 at 11:00 am
Contact:
Dena Miller, dena.miller@beg.utexas.edu, 512-471-2677
DeFord Lecture | Dr. William Dietrich
Start:November 7, 2024 at 4:00 am
End:
November 7, 2024 at 5:00 am
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
The shock of the familiar: Observations on Mars raise questions about Earth surface processes by Dr. William Dietrich, Department of Earth and Planetary Sciences, University of California Berkeley
Abstract: Evidence from satellite imagery of features like channel networks, gullies, meandering rivers, alluvial fans, and deltas abound on Mars. These provide crucial evidence that in the past, at various times, Mars had an atmosphere that supported a liquid water hydrologic cycle. These features make the Martian landscapes one sees (in close up rover-derived imagery) seem strangely familiar: Earth-like but lacking any vegetation. In my talk, I will describe our rover encounter with two very different alluvial fans and a pediment surface, which raised unanticipated fundamental questions about fan and pediment processes and the hydrologic signals they may record. Mars meandering river observations also motivated our field and modeling study of a channel on Earth that explains how lateral accretion deposits can form in muddy meanders.
DeFord Lecture | Dr. Bill Dietrich
Start:November 7, 2024 at 4:00 pm
End:
November 7, 2024 at 5:00 pm
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
The shock of the familiar: Observations on Mars raise questions about Earth surface processes by Dr. William Dietrich, Department of Earth and Planetary Sciences, University of California Berkeley
Abstract: Evidence from satellite imagery of features like channel networks, gullies, meandering rivers, alluvial fans, and deltas abound on Mars. These provide crucial evidence that in the past, at various times, Mars had an atmosphere that supported a liquid water hydrologic cycle. These features make the Martian landscapes one sees (in close up rover-derived imagery) seem strangely familiar: Earth-like but lacking any vegetation. In my talk, I will describe our rover encounter with two very different alluvial fans and a pediment surface, which raised unanticipated fundamental questions about fan and pediment processes and the hydrologic signals they may record. Mars meandering river observations also motivated our field and modeling study of a channel on Earth that explains how lateral accretion deposits can form in muddy meanders.
UTIG Seminar Series: Gavin Piccione, Brown University
Start:November 8, 2024 at 10:30 am
End:
November 8, 2024 at 11:30 am
Location:
PRC 196/ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Gavin Piccione, Postdoctoral Research Associate in Environment and Society, Brown University
Host: Ruthie Halberstadt
Title: Constraints the Oxygen Isotope Composition of Antarctic Ice Recorded in Subglacial Rocks: A Case Study from the Late Miocene
Abstract: Long-term, continuous records of global ice volume have been derived using δ18O values of benthic foraminifera (δ18Ob), which record the balance between water held in the ocean and trapped on the continents. However, these ice volume approximations are confounded by the fact that δ18Ob values change as a function of ocean bottom water temperature and cannot account for spatiotemporal variation in the ?18O of ice sheets. Therefore, direct constraints on the ?18O of ice sheets are necessary to link the ?18Ob record to sea level change. In this talk, I will present geochemical data from Antarctic subglacial opal and calcite precipitates, a novel archive for reconstructing ice sheet ?18O values. Uranium-series and uranium-lead dating reveal the formation histories of these samples, spanning the late Pleistocene to late Miocene. Paired carbonate clumped isotope temperature estimates and opal triple oxygen measurements characterize the oxygen isotope composition of basal ice. Using a simplified mass balance calculation, I will explore the mass and sea level contributions of the late Miocene Antarctic Ice Sheet given these newly defined oxygen isotopic constraints.
Bureau of Economic Geology Seminar Series
Start:November 12, 2024 at 10:00 am
End:
November 12, 2024 at 11:00 am
Contact:
Dena Miller, dena.miller@beg.utexas.edu, 512-471-2677
DeFord Lecture | Dr. Carl Tape
Start:November 14, 2024 at 4:00 pm
End:
November 14, 2024 at 5:00 pm
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
DeFord Lecture | Dr. Carl Tape
Start:November 14, 2024 at 4:00 pm
End:
November 14, 2024 at 5:00 pm
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
Exploration of Seismic Anisotropy of Earth Materials and Alaska Structure by Dr. Carl Tape, Department of Earth and Planetary Sciences, University of California Berkeley
Abstract: For many seismologists, seismic anisotropy is a complex nuisance. Yet it is undeniably present in the Earth, from the scale of crystals like feldspars to metamorphic terranes to the uppermost mantle. Alaska offers an exciting testbed for exploring anisotropy, with insights from exhumed mantle rocks, corner flow at the edge of a subduction-collision zone, and foliated metamorphic units and other fabrics in the crust. One of the grand challenges of seismology is to estimate the variations in subsurface anisotropic elastic properties using seismic waves recorded at the surface. I will discuss how this challenge can be faced with efforts from realms of theory, computation, laboratory, and observation.
UTIG Seminar Series: Kate Rychert, WHOI
Start:November 15, 2024 at 10:30 am
End:
November 15, 2024 at 11:30 am
Location:
PRC 196/ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Kate Rychert, Associate Scientist, Woods Hole Oceanographic Institution
Host: Thorsten Becker
Title: A dynamic lithosphere-asthenosphere boundary: the PI-LAB experiment
Abstract: Plate tectonics revolutionized our understanding of how the Earth works, providing a framework for volcanism, earthquakes, continental formation and breakup and the geologic record of climate change. Yet, what makes a plate “plate-like” and where and how the rigid lithospheric plate transitions to the underlying weaker asthenosphere are widely debated. I present new geophysical constraints on the LAB from the PI-LAB (Passive Imaging of the LAB) experiment using a range of methodologies, techniques, and resolutions in one location near the equatorial Mid-Atlantic Ridge. We find that the LAB has a variable character depending on location: simple, with monotonic age progression, undulating, and underlain by a thin melt channel. The result reconciles seemingly discrepant and variable reports of the LAB and partial melt from previous studies. Putting the LAB result from the Mid-Atlantic Ridge in the context globally, in particular, by considering a new interdisciplinary compilation of LAB depths, suggests that temperature determines the thickness of the plate to first order. However, the LAB is dynamic. Composition, in addition to melt generation and migration also affect the depth and definition of the LAB and likely play a role in driving plate tectonics.
Hot Science - Cool Talks: "This is Your Brain on Birth Control"
Start:November 15, 2024 at 5:30 pm
End:
November 15, 2024 at 8:15 pm
Location:
Welch (WEL) 2.224
Contact:
Angelina DeRose, Angelina.DeRose@jsg.utexas.edu, 512-471-4974
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Birth control has revolutionized fertility control, but its effects extend far beyond reproductive health. The powerful hormones in birth control influence billions of cells throughout the body, particularly in the brain, shaping stress responses, eating habits, romantic attraction, and more. Join Hot Science – Cool Talks for an enlightening discussion with Dr. Sarah Hill as we explore the hidden impacts of birth control and empower everyone to make informed decisions about their health and well-being. (Recommended PG-13)
Bureau of Economic Geology Seminar Series
Start:November 19, 2024 at 10:00 am
End:
November 19, 2024 at 11:00 am
Contact:
Dena Miller, dena.miller@beg.utexas.edu, 512-471-2677
DeFord Lecture | Dr. Sumant Nigam
Start:November 21, 2024 at 4:00 pm
End:
November 21, 2024 at 5:00 pm
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
DeFord Lecture | Dr. Saravanan Ramalingam
Start:November 21, 2024 at 4:00 pm
End:
November 21, 2024 at 5:00 pm
Location:
Boyd Auditorium (JGB 2.324)
Contact:
Luc Lavier
The Limits of Predictions: Weather vs. Climate by Dr. Saravanan Ramalingam, Department of Atmospheric Sciences, Texas A&M University
Abstract: Prediction plays an important role in the physical sciences. Knowing the mathematical equations that govern a physical system and its initial state should, in principle, allow us to compute the future time evolution of the system. In practice, our ability to predict is limited by how well we know the equations and the initial state. Awareness of these limits can guide us in setting priorities for predictive model development and help calibrate our expectations for improvements in model performance.
In this talk we address the limits of scientific prediction, with a focus on weather and climate prediction. The talk will discuss the philosophical underpinnings of weather and climate prediction. The evolution of modern weather and climate prediction is intertwined with advances in computing. Since the advent of the digital computer, physics-based “deductive” models have been used for weather and climate prediction. However, recent advances in machine learning have opened the door for a new class of “inductive” models for weather and climate. Climate models have also grown in complexity over time as computers have become more powerful. However, in the most recent IPCC assessment, some of the most complex models have been criticized as being too sensitive to carbon dioxide concentrations. This suggest that increased model complexity may be yielding diminishing returns in reducing uncertainty.
UTIG Seminar Series: Eloi Camprubi Casas, UT Rio Grande Valley
Start:November 22, 2024 at 10:30 am
End:
November 22, 2024 at 11:30 am
Location:
PRC 196/ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Speaker: Eloi Camprubi Casas, Assistant Professor, The University of Texas Rio Grande Valley
Host: Elizabeth Spiers
Title: On wet rocky worlds – How does origin of life research impact space exploration efforts at ocean worlds?
Abstract: Many settings have been proposed as the cradle of life on Earth. Amongst these, Hadean alkaline hydrothermal systems have been proposed as electrochemical reactors driving an autotrophic origin of life. Recent experimental discoveries demonstrate some of the crucial synthetic steps are indeed favored under these conditions. We have developed a high-pressure microfluidic reactor to simulate the out-of-equilibrium conditions found in these extreme submarine environments. How does this research impact the strategy for biosignature detection at Ocean Worlds? What role does the icy surface environment play when trying to detect signs of life? This talk will present the work done at the Astrobiochemistry Lab at UTRGV connecting abiogenesis and biosignatures research.
Bureau of Economic Geology Seminar Series
Start:November 26, 2024 at 10:00 am
End:
November 26, 2024 at 11:00 am
Contact:
Dena Miller, dena.miller@beg.utexas.edu, 512-471-2677
DeFord Lecture | Venkat LakshmiJanuary, 22 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 Progresses and Challenges in Hydrology by Dr. Venkat Lakshmi, professor at the University of Virginia Abstract: In order to study land surface hydrology, we need to use a multitude of tools, namely, modeling, observations and their synergism. After multiple decades of hydrological modeling, we still have major challenges. However, we have novel observations and mathematical methods that are now available and can be harnessed to achieve progress. These include earth observations that are available at global scales and at high spatial resolutions and frequent temporal repeat. Artificial Intelligence and Machine Learning (AI/ML) can be used (specifically Transfer Learning) to determine streamflow in un-gaged or poorly-gaged watersheds. In this talk, I will focus on four major questions and provide examples for each of the questions. These examples will highlight both advances and limitations for each issue. (i) Do earth observations compare well with in-situ counterparts? (ii) How important is rainfall in hydrological modeling? (iii) Can we get higher spatial resolution of earth observations? (iv) How do we study un-gaged/poorly gaged watersheds? |
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Bureau of Economic Geology Seminar SeriesJanuary, 23 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Dr. Bridget Scanlon, BEG in person. Topic: Remote sensing, hydrology |
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UTIG Spring Seminar Series 2026: Jinbo WangJanuary, 23 2026Time: 10:30 AM - 11:30 AMLocation: PRC 196/ROC 1.603
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SSL Seminar Series | Kristin BergmannJanuary, 27 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Temperature and the earliest animals: Quantitative climate reconstruction across the Neoproterozoic–Phanerozoic transition by Dr. Kristin Bergmann Abstract: The Neoproterozoic–Phanerozoic transition records the emergence of complex animals, the origin of biomineralization, and the establishment of modern marine ecosystems—yet the climate context for these evolutionary milestones remains poorly quantified. Reconstructing ancient temperatures requires integrating sedimentology, carbonate petrography, and isotope geochemistry. Our field-based stratigraphic analysis establishes depositional context and identifies the most promising sampling targets; detailed petrographic screening and microstructural analyses constrain diagenetic paragenesis. Clumped-isotope thermometry (Δ47–Δ48) reconstructs temperature signals within this sedimentological framework, resolving the ambiguity between temperature and seawater composition that limits traditional δ¹⁸O approaches. This rocks-first workflow reveals large, directional climate shifts with ecological consequences. In the Tonian and Cryogenian, data from Oman and elsewhere indicate near-modern tropical temperatures before and after Snowball Earth glaciations, suggesting dynamic hydrologic and climatic transitions. During the Ediacaran, post-glacial warming followed by ≥20 °C cooling likely expanded oxygenated habitats and set the stage for early animal diversification. In the Ordovician, ~15 °C of long-term tropical cooling over ~40 Myr culminated in brief but extensive glaciation, providing the climate context for the Great Ordovician Biodiversification Event. By grounding geochemical data in sedimentological and petrographic observations, we build a quantitative framework linking climate and habitability and provide evidence that temperature change guided life\'s evolutionary trajectory in deep time. |
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SSL Seminar Series | Ted PresentJanuary, 29 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Biogeochemical Signals of Seafloor Oxygenation by Dr. Ted Present Abstract: Earth’s oxygenation transformed the atmosphere, oceans, and ultimately the seafloor, establishing the carbon and sulfur cycles that govern our planet today. When and how did oxygen penetrate into marine sediments, shifting where organic matter was recycled and setting up the biogeochemical architecture we recognize in modern oceans? I approach this question by studying how microbial and chemical processes at the sediment-water interface leave lasting signatures in sedimentary rocks. Using sulfur isotopes and detailed sedimentology, I will show how Paleozoic carbonates and evaporites track the reorganization of ocean redox structure through critical evolutionary transitions like the Late Ordovician glaciation and mass extinction. The Permian Reef Complex of West Texas demonstrates how cementation and dolomitization patterns archive ancient sulfur cycling, with insights grounded in observations from modern tidal systems where diagenetic processes govern carbon storage along our changing coasts. I will close with how I envision training UT Austin students in integrated field and laboratory approaches to pursue future research leveraging evaporite basins, novel phosphatic archives, and terrestrial carbonates. By extracting environmental signals from the diagenetic processes that create the rock record, this work builds a framework for understanding how Earth’s oxygenation reshaped life and its environment. |
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Bureau of Economic Geology Seminar SeriesJanuary, 30 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented in person by Dr. Todd Halihan, Oklahoma State University, and Chief Technical Officer for Aestus, LLC in person Topic: Subsurface hydrogeology |
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SSL Seminar Series | Mackenzie DayFebruary, 03 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) From sand to stratigraphy: How dunes record the changing landscape of Earth and other planets by Dr. Mackenzie Day Abstract: Desert dune fields preserve rich sedimentary records of environmental change, providing insight into both past climate and modern landscape evolution. This presentation explores three desert systems on Earth and Mars, using dune fields as a lens to examine how landscapes, both ancient and modern, respond to shifting environmental conditions. These investigations address the longevity of Earth’s dune fields, the interplay between wind and water, and the applicability of aeolian sedimentology to planetary bodies beyond Earth. Together, they highlight how dune fields serve as dynamic archives of change, and how Earth, Mars, and other bodies can be studied in tandem as natural laboratories for generalizing aeolian sediment transport to arbitrary fluid-gravity conditions. |
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SSL Seminar Series | Marjorie CantineFebruary, 05 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Human, climate, sediment and geobiological history of a rapidly-growing carbonate island by Dr. Marjorie Cantine Abstract: You may have heard the line that real estate is valuable because \"they aren\'t making more land\"; in this talk, I\'ll show you that that\'s not true. I\'ll use the sedimentary and radiocarbon records of a carbonate island in the Caribbean, Little Ambergris Cay, to describe its formation over the last millenium, how its growth relates to past climate, and what it means for mechanisms potentially capable of protecting shorelines in the near future. I\'ll leverage geobiological field experiments to help explain the mechanisms of island growth. Finally, I\'ll share how ongoing work in my group is leveraging geoarchaeological archives to better understand the human and climate histories of the Common Era and inform hazard predictions in the region through testing climate models. I will also briefly describe other work ongoing in my group, which tackles questions at the nexus of time, sedimentary processes, and geochemistry from the Precambrian to the Common Era. |
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15th Annual Jackson School of Geosciences Student Research SymposiumFebruary, 06 2026Time: 12:00 AM - 12:00 AM |
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Bureau of Economic Geology Seminar SeriesFebruary, 06 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Stacy Timmons and Mike Timmons, New Mexico Bureau of Geology & Mineral Resources, in person. Topic: New Mexico Geological Survey |
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SSL Seminar Series | Vamsi GantiFebruary, 10 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) From Dunes to Channel Belts: How Rivers Organize and Move Across Scales by Dr. Vamsi Ganti Abstract: Rivers are Earth’s arteries: they transport water and sediment from uplands to oceans, sustain ecosystems and agriculture, and build the stratigraphic record of past environmental change. Yet rivers are far from static—they are dynamic systems that evolve across scales, from ripples and dunes on the riverbed to entire channel belts. In this seminar, I will present three discoveries that reveal the mechanisms shaping alluvial river form and motion across these scales. (1) Laboratory experiments and theory identify a previously unrecognized transition in river-dune organization at the onset of significant suspended sediment transport. This transition influences flow roughness, flood-driven dune reconfiguration, and the nature of preserved fluvial strata. (2) Using a new image-processing tool, we analyzed 36 years of satellite imagery from 84 rivers to uncover the origins of single- versus multithread channels. Single-thread rivers achieve a balance between lateral erosion and accretion, maintaining equilibrium width, while multithread rivers arise when erosion outpaces accretion, causing individual threads to widen and split. This mechanistic insight informs both planetary geomorphology and cost-effective river restoration. (3) Finally, I’ll show how human activity and climate change are already altering the way rivers flow and evolve. Dams dampen river motion and reduce the number of active threads, whereas increased sediment supply from land-use change and glacial melt are making rivers in the Global South and High Mountain Asia more dynamic. Together, these discoveries provide a mechanistic view of river evolution across scales and highlight why understanding river behavior is essential—not only for managing water, life, and landscapes they sustain today, but also for decoding the history of environmental change recorded in sedimentary strata. |
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DeFord Lecture | Jake JordanFebruary, 12 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
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DeFord Lecture | Daniel MinisiniFebruary, 19 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
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Bureau of Economic Geology Seminar SeriesFebruary, 20 2026Time: 1:00 PM - 2:00 PMLocation: BEG VR Room 1.116C BEG Seminar presented by Dallas Dunlap, BEG, in person. Topic: Channel Architecture Influenced by Precursor Channelized Submarine Landslide Topography in the Taranaki Basin |
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Hot Science - Cool Talks: The Biology of LoveFebruary, 20 2026Time: 5:30 PM - 8:30 PMLocation: Welch Hall 2.224 and Grand Hallway What does science say about love and long-term relationships? In this Hot Science – Cool Talks event, biologist Dr. Steven Phelps explores the biology of love through the surprising world of prairie voles, one of the few monogamous mammals. By studying how vole brains form lasting bonds, Dr. Phelps reveals what biology, brain chemistry, and evolution can teach us about human connection and commitment. This engaging talk offers a fresh, science-based look at why we pair up right after Valentines Day! |
