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Bridget R. Scanlon, Ph.D. - Bureau Seminar Series
Start:January 7, 2022 at 9:00 am
End:
January 7, 2022 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Assessing Linkages between Drinking Water Quality Violations and Social Vulnerability in the United States
Increasing concern over our drinking water supplies, particularly in socially vulnerable communities, has prompted government initiatives to increase compliance and provide safe drinking water for all. Here we evaluated health-based violations of the Safe Drinking Water Act in community water systems across the US to decipher spatiotemporal relationships between violations and social drivers. We show that water quality violations are strongly linked to social vulnerability in the Southwest US (e.g., arsenic, radionuclides, and nitrate) and Southcentral US (disinfection byproducts) where violations and social vulnerability are both high and in the Midwest where both are low. However, violations are generally not linked to social vulnerability in the Southeast (low violations, high social vulnerability) and in the Northeast (high violations, low social vulnerability). Texas ranked first in terms of EPA serious violators and in number of community water systems with any health-based violations. Approximately 100 times more people experience both high levels of any drinking water violation and high social vulnerability (~12 million people) relative to populations with low violations and social vulnerability. Of all social vulnerability metrics, poverty and minority status exhibited the strongest linkages to violation incidence. Notably, persistence of violations over time is strongly linked to social vulnerability (R2: 0.62–0.83) across the US, indicating much greater challenges for socially vulnerable communities to attain and maintain system compliance. These water quality challenges and associated environmental justice issues are likely exacerbated by climatic factors. Understanding spatiotemporal variability in noncompliance can help guide deployment of new infrastructure funding to address health-based violations which disproportionately persist in socially vulnerable populations served by very small to small community water systems in mostly rural settings.
Bridget Scanlon is a Senior Research Scientist at the Bureau of Economic Geology, Jackson School of Geosciences, The University of Texas at Austin. Her current research focuses on water quality issues related to EPA regulations and linkages to social vulnerability throughout the U.S., with particular emphasis in Texas. This study should help guide water infrastructure funding to improve compliance with EPA regulations. She has (co)authored ~160 publications. Dr. Scanlon is a member of the National Academy of Engineering.
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Buddy Price presenting for Bureau Seminar Series
Start:January 14, 2022 at 9:00 am
End:
January 14, 2022 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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“New Insight into Basinal Depositional Processes and Resulting Stratal Architecture in the Permian Basin”
Over the last two decades studies have emphasized the underappreciated impact of bottom currents and point-sourced gravity-driven currents in deepwater allochthonous carbonate depositional environments, leading to re-interpretations of many previously examined systems. Wolfcampian and Leonardian intervals in the Permian Basin provide a thick succession of basinal strata to re-evaluate with updated insight and models. Subsurface mapping and cross sections highlight multiple mounded and elongate carbonate-mud rich accumulations reaching up to 800m thick along the western slopes of the Delaware Basin. The mounded nature, lack of platform-focused sourcing, and presence of oblique cross-cutting channels suggest these features represent carbonate contourite drifts generated by bottom currents as opposed to gravity-driven deposits. Thickness relationships also indicate bottom currents may locally sweep sediments from toe-of-slope environments, inhibiting platform progradation.
In the deeper basin, mapping highlights previously undocumented point-sourced carbonate accumulations interpreted as calciclastic submarine fans. Some fans extend into the basin over 100km and reach 250m in thickness. The fans range in composition, containing both carbonate debrites and turbidites with varying volumes of mud-rich siliciclastic deposits. Runout of gravity flows resulted in concentration of comparatively coarser carbonate material in proximal fan environments and finer siliciclastic mudstone, siltstone, and organic matter in fan fringe environments.
The findings are significant as the processes responsible for drift and fan formation impart significant control on facies distribution and subsequent reservoir quality, reservoir architecture, organic matter distribution, and vertical and lateral distribution of barriers to induced fracture growth. Correct characterization across multiple zones may highlight stacking of sub-environments to explain production trends, identify advantageous locations for multi-zone development, or inform spatial differences in horizontal well spacing and stacking. Lastly, as these new interpretations recognize calciclastic drifts and fans in one of the most heavily studied and geologic data-rich areas in the world, it indicates these systems are likely overlooked and more common in the ancient rock record.
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Spring Semester Classes Begin
Start:January 18, 2022
End:
January 18, 2022
Charles Kerans, Ph.D. presenting for Bureau Seminar Series
Start:January 21, 2022 at 9:00 am
End:
January 21, 2022 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Carbonate Sedimentologic/Stratigraphic Record of Climate Change from Bahamas-Caicos Archipelago
One of the most compelling uncertainties of global warming scenarios is the magnitude and rate of sea-level rise if temperatures continue to increase at current rates unchecked. The most immediate insights into this ongoing crisis derive from careful monitoring and modeling of the Antarctic and Greenland ice sheets, whose potential for rapid collapse pose an imminent threat to coastal inundation. Reconstructing the rate and magnitude of sea-level rise from the earth’s most recent warm periods, or interglacials, and in particular the well-studied last interglacial (LIG) or marine isotope stage 5e (MIS 5e), provides additional constraints. The carbonate sedimentologic/stratigraphic record of the LIG is uniquely well suited to record the deep-time record of climate forcing with its high-fidelity track of shorelines and reefs. Studies conducted over the past 7 years within the carbonate group at UT Austin in collaboration with Exxon-Mobil and USF have generated significant insights into the role of such critical climate events as LIG peak sea-level, the Middle Pleistocene Transition (MPT), the Last Interglacial (LIG), and melt-water pulses (MWP’s) following T1 (the last glacial termination). Important questions regarding the global mean sea level response during peak LIG warming, and the impact of glacioisostatic adjustments (GIA) on this record and the Holocene record of sea level rise will be considered.
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UTIG Seminar: Ariel Lellouch, Tel Aviv University
Start:January 21, 2022 at 10:30 am
End:
January 21, 2022 at 11:30 am
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Contact costa@ig.utexas.edu for a link to join the live talk.
Speaker: Ariel Lellouch, Tel Aviv University
Host: Duncan Young
Title: Seismic applications of downhole DAS
Abstract: Distributed Acoustic Sensing (DAS) is an emerging technology that leverages optical fibers to record the seismic wavefield with an unprecedented spatial resolution. In this talk, I will describe various seismic-band applications utilizing optical fibers deployed in boreholes. We first illustrate how records from a vertical DAS array can be simply and effectively processed to construct velocity models, detect microseismic events and earthquakes, locate them, and estimate their magnitude. Then, we show how a horizontal DAS array deployed in an unconventional shale reservoir records guided waves propagating for hundreds of meters with frequencies as high as 700 Hz. Thanks to the high resolution of DAS measurements, guided waves are recorded unaliased despite their very short (< 10 m) wavelength. We compare the field observations with semi-analytical and wave-equation modeling approaches. Guided waves are also strongly affected by open fractures induced by hydraulic stimulation. We use a horizontal cross-well acquisition of perforation shots recorded by a DAS array in a simple, geometrical analysis of horizontal fracture growth. We also analyze guided waves generated by microseismic events and can locate the events despite the unidirectional nature of the DAS measurements.
Water, Climate and Environment Seminar | Bridget Scanlon - JSG/BEG
Start:January 21, 2022 at 12:00 pm
End:
January 21, 2022 at 1:00 pm
Contact:
Cansu Demir, Ana Maria Restrepo, cdemir@utexas.edu, anarestrepo@utexas.edu
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Title: Assessing Global Water Scarcity Using Satellites
Planetary Habitability Seminar: Kennda Lynch, LPI
Start:January 24, 2022 at 1:00 pm
End:
January 24, 2022 at 2:00 pm
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
UT Paleontology Seminar: Dr. Alexis Mychajliw
Start:January 27, 2022 at 11:00 am
End:
January 27, 2022 at 12:00 pm
Location:
JGB 4.102
Contact:
David Trevino Ledesma, ledesma-david@utexas.edu
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Zoom link: https://utexas.zoom.us/j/91661118623
Graduate Studies Committee (GSC) Meeting
Start:January 27, 2022 at 12:30 pm
End:
January 27, 2022 at 2:00 pm
This is an internal Jackson School of Geosciences meeting for faculty and research scientists who are part of the Graduate Studies Committee.
DeFord Lecture | Debbie-Ann Gordon-Smith
Start:January 27, 2022 at 4:00 pm
End:
January 27, 2022 at 5:00 pm
Location:
https://utexas.zoom.us/j/96370762511
Contact:
John Lassiter
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Investigation of water resources and nutrient biogeochemistry on the island of Jamaica using environmental tracers
Dr. Debbie-Ann Gordon-Smith, The University West Indies, at Mona
Abstract: Global water resources have been under severe stress due to various factors including poor management, pollution and changes in rainfall patterns due to climate variability. The small islands of the Caribbean, such as Jamaica, have not been spared; prolonged periods of drought, extreme weather events and increased urbanization have led to water shortages and impaired water quality.
Sustainable management of these natural water resources requires an understanding of the dynamics of their physical behavior and their chemical constituents. Environmental tracers have proven to be very effective tools for studying the transport and mixing of surface and subsurface water on regional and global scales.
This lecture will introduce the audience to the use of stable and radioactive isotopes as tracers in the investigation of the fresh and coastal waters of Jamaica. The talk will describe the analytical techniques used in these isotopic studies, present findings related to the sources, pathways and fate of nutrients and other inorganic contaminants, and suggest implications of these findings for the sustainable management of Jamaica’s water resources.
DeFord Lecture Series
Since the 1940’s, the DeFord (Technical Sessions) lecture series, initially the official venue for disseminating EPS graduate student research, is a forum for lectures by distinguished visitors and members of our community. This is made possible through a series of endowments.
BEG Seminar: Peter Eichhubl, Ph.D.
Start:January 28, 2022 at 9:00 am
End:
January 28, 2022 at 10:00 am
Location:
Zoom
Contact:
Dena Miller, dena.miller@beg.utexas.edu
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Peter Eichhubl, Ph.D. – Senior Research Scientist – Bureau of Economic Geology -The University of Texas at Austin
A chemo-mechanical view on caprock failure—implications for carbon and hydrogen storage in subsurface reservoirs
Storage or disposal of fluids such as carbon dioxide, wastewater, or hydrogen in the subsurface can result in chemical disequilibrium between the resident brine and the formation. In this presentation I explore how chemical change can enhance or inhibit fracture growth, and how such processes can affect shale caprock integrity of storage reservoirs.
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UTIG Seminar: Lin Liu, Chinese University of Hong Kong
Start:January 28, 2022 at 10:30 am
End:
January 28, 2022 at 11:30 am
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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*** Due to the 14 hour time difference between Austin and Hong Kong, this seminar has been scheduled to start at 9:00am CT ***
Contact costa@ig.utexas.edu for a link to join the live talk.
Speaker: Lin Liu, Chinese University of Hong Kong
Host: Xiaohua Xu
Title: Geophysical investigations of thawing permafrost
Abstract: Accumulating observational evidence shows widespread thawing and degradation of perennially-frozen ground known as permafrost. Thawing permafrost has profound effects on terrestrial ecosystems, hydrologic and landscape processes, and infrastructure. However, it is challenging to study and monitor permafrost mainly because it is purely defined by the subsurface thermal condition. Through a few local to regional-scale studies, I will show how integrative measurements using geophysical methods, such as Ground Penetrating Radar, space-borne Radar Interferometry, and Surface Nuclear Magnetic Resonance, offer quantitative understandings on surface and subsurface processes associated with thawing ice-rich permafrost.
SSL Seminar Series | Tian DongJanuary, 20 2026Time: 3:30 PM - 4:30 PMLocation: Boyd Auditorium (JGB 2.324) Natural and Human Impacts on Coastal Land Building by Dr. Tian Dong Abstract: Sediment and water delivered by rivers build and sustain coastal landforms such as deltas and wetlands, which are densely populated and ecologically vital areas threatened by rising sea levels. In this talk, I highlight theory-driven and field-based research to understand how coastal land building operates across broad deltaic plains and how human activity affects these processes. On the theoretical front, inspired by Hack’s law (the scaling between watershed drainage area and channel length in tributary networks), we analyzed a global dataset of distributary delta networks and discovered a nearly identical scaling relationship between distributary channel length and nourishment area, the land-building counterpart to drainage area. Despite this apparent global scaling, we identified two distinct local land-building patterns: Uniform Delta Networks consistently follow Hack’s law, while Composite Delta Networks exhibit a scale break, transitioning from space-filling growth around the delta apex to quasi-linear growth near the coast. These surprising growth patterns suggest that global simplicity and local variability coexist in how river deltas grow and organize. To assess regional variability and human impacts, we combined remote sensing with field observations from the Lower Rio Grande, finding that the river currently carries about one-third of its median 1900s discharge, and only about 0.3% of its natural flow reaches the Gulf due to human consumption. This reduction leads to channel contraction, higher water levels for the same discharge, and significant shoreline retreat (up to 6 m/yr). I conclude by highlighting three ongoing/future research directions on deltaic land building: (i) sedimentation influenced by human engineering, (ii) wind-driven sediment redistribution, and (iii) the effects of sediment influx from retreating glaciers. |
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? |
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 |
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. |
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. |
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 |
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. |
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. |
15th Annual Jackson School of Geosciences Student Research SymposiumFebruary, 06 2026Time: 12:00 AM - 12:00 AM |
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 |
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. |
DeFord Lecture | Jake JordanFebruary, 12 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
DeFord Lecture | Daniel MinisiniFebruary, 19 2026Time: 3:30 PM - 4:30 PMLocation: JGB 2.324 |
