Events
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DeFord Lecture | Kristin Bergman
Start:March 2, 2023 at 4:00 pm
End:
March 2, 2023 at 5:00 pm
Location:
JGB 2.324 (Boyd Auditorium)
Contact:
John Lassiter
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Towards a temperature record across the advent of complex life by Kristin Bergman, MIT
Abstract: The ecology and habitability of Earth is fundamentally shaped by its surface temperature. But, the further back in time we look, this history becomes increasingly difficult to reconstruct. This is particularly true over the ?4 billion years when microbes ruled and before animals like corals began making skeletons and shells out of seawater. Consequently, Earth’s temperature history in deep time is, and has been, the subject of a vigorous, decades-long debate.
In my work, we are developing multi-mineral isotopic and petrographic methods to understand the role of temperature, fluid chemistry, and diagenesis on two isotopic systems—oxygen isotopes and clumped isotopes—that reefs and other carbonates record as they grow. We are developing local records and present details of those alongside a new high-resolution record of bulk carbonate oxygen isotopes for the last billion years of Earth’s history.
My results suggest one solution to the previous ambiguity surrounding seawater oxygen isotope composition through time. Based on our results to date, and other distinctive features of our high resolution oxygen isotope record, we hypothesize that temperature, and not just atmospheric oxygen levels, was a key factor for understanding emergence, diversification and subsequent trajectory of complex life.
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.
RoKafe
Start:March 7, 2023 at 10:00 am
End:
March 7, 2023 at 11:00 am
Location:
JGB 2.104A
Contact:
Nicola Tisato

Faculty Meeting
Start:March 7, 2023 at 12:30 pm
End:
March 7, 2023 at 1:45 pm
Location:
JGB 4.102 (Barrow)
Contact:
Jessica Yeager
DeFord Lecture | Renyi Zhang
Start:March 9, 2023 at 4:00 pm
End:
March 9, 2023 at 5:00 pm
Location:
JGB 2.324 (Boyd Auditorium)
Contact:
John Lassiter
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Do industrial emissions play a role in the catastrophe during Hurricane Harvey? by Renyi Zhang, Texas A&M University
Abstract: Hurricane Harvey caused catastrophic flooding (about 555 mm in the Houston urban area) and more than 100 deaths during 25-27 August 2017. It is tied with 2005’s Hurricane Katrina as the costliest tropical cyclone on record, inflicting 5 billion in damage, primarily from catastrophic rainfall-triggered flooding in the Houston metropolitan area and Southeast Texas. Although several recent studies have linked Hurricane Harvey’s devastation to climate change or changes in land use due to urbanization, the cause of the catastrophic flooding remains uncertain. Tropical cyclones are driven by latent heat release from condensation and are inevitably linked to the abundance of aerosols by acting as cloud condensation nuclei. In this talk, I will present results from both measurements and numerical model simulations to investigate the impacts of anthropogenic aerosols on deep moist convection, precipitation, and lightning activities during hurricane Harvey. Our work shows a non-negligible effect of anthropogenic aerosols on this regional extreme weather event, highlighting the necessity of accounting for the aerosol effects in hurricane forecast models to accurately predict precipitation and to minimize the storm damage along the heavily industrialized Gulf of Mexico region.
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.
UTIG Seminar Series: Liz Drenkard, GFDL NOAA
Start:March 10, 2023 at 10:30 am
End:
March 10, 2023 at 11:30 am
Location:
BEG 1.202
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Note: This week’s seminar will be held at BEG 1.202, at the Bureau of Economic Geology, next door to UTIG. Signs will be posted.
Abstract: Earth System Models (ESMs) are invaluable for understanding the ocean’s role in climate change and anticipating future global ocean conditions. Ongoing model developments toward more holistic representation of the Earth System continue to shape our knowledge of global change but, in order to capture the regional ocean processes most relevant to coastal communities and the living marine resources (LMRs) on which they depend, these models sometimes need to be translated to smaller scales. Downscaling ESMs to limited area domains can address this need, but only with significant improvements relative to past efforts, including strategic budgeting of finite computational resources to balance resolution, uncertainty quantification, and comprehensiveness needs.
I will share some of my research at NOAA’s Geophysical Fluid Dynamics Laboratory where I use ocean models to study the effects of climate change on marine ecosystems at different scales. At the global-scale, I’ve been investigating the impact of advances in coupled land-air-sea interactions, specifically the dynamic deposition of dust to the ocean in GFDL’s ESM4, on projections of ocean biogeochemistry. We’ve found that permitting dust deposition to reflect changes in land use and aridity (rather than prescribing a deposition climatology to the ocean) dramatically impacts the distribution of Pacific Ocean iron limitation under different emission scenarios. At the regional scale, I will delve into recommendations for next-generation regional ocean projections for LMR management (e.g., considerations for model domain size, resolution, ensemble size) arising from a recent synthesis of two decades of ocean downscaling efforts. Finally, I will describe nascent NOAA-led efforts to develop high-resolution ocean and biogeochemical modeling and climate-scale prediction frameworks for the Northeast Pacific and other U.S. coastal waters.
RoKafe
Start:March 21, 2023 at 10:00 am
End:
March 21, 2023 at 11:00 am
Location:
JGB 2.104A
Contact:
Nicola Tisato

Faculty Meeting
Start:March 21, 2023 at 12:30 pm
End:
March 21, 2023 at 1:45 pm
Location:
JGB 4.102 (Barrow)
Contact:
Jessica Yeager
Doctoral Defense | Nicholas Meszaros
Start:March 22, 2023 at 2:00 pm
End:
March 22, 2023 at 4:00 pm
Location:
JGB 3.116 and VIRTUAL
Contact:
Philip Guerreo
The final doctoral examination for NICHOLAS MESZAROS has been scheduled for MARCH 22, 2023; 2:00PM; JGB 3.116 AND VIRTUAL.
The PhD project “Prelude To The Latest Caldera-Forming Eruption Of The Jemez Magmatic System, New Mexico, USA” was supervised by Dr. Jim Gardner.
Committee members include: Kenneth Befus, Richard A Ketcham, Jaime D Barnes, Matthew Zimmerer, Laura Waters
ZOOM link: https://utexas.zoom.us/j/98837704980
The defense is open to all members of the University community and the public.
DeFord Lecture | Stephanie Pierce
Start:March 23, 2023 at 4:00 pm
End:
March 23, 2023 at 5:00 pm
Location:
JGB 2.324 (Boyd Auditorium)
Contact:
John Lassiter
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Functional adaptive landscapes (help) illuminate major transitions in vertebrate evolution by Stephanie Pierce, Harvard University
Abstract: The concept of the adaptive landscape has been an invaluable tool to the field of modern evolutionary biology by providing a representation of how fitness and selection vary within populations of organisms. Trait variation can be visualized as a multidimensional “landscape” (analogous to a mountain range) with height on the landscape corresponding to fitness; selection acting on populations is expected to drive populations “up-hill” to cluster around “adaptive peaks” where fitness is maximized. Although originally implemented in the study of population genetics and microevolution, paleontologist G.G. Simpson expanded the idea of the adaptive landscape to explain phenotypic change over macroevolutionary timescales. Specifically, he linked large-scale biological and geological processes, such as extinction and climate change, with shifts in adaptive peaks representing selection acting upon phenotypic traits that were of “functional benefit”. Despite decades passed, the practical application of Simpson’s adaptive landscape in macroevolution has been limited by computational challenges in quantifying the functional performance outcomes of morphological traits and how they vary across a vast phenotypic landscape. Here I will introduce a new method called “functional adaptive landscape analysis” which determines the functional trade-offs associated with morphological adaptation to differing selection regimes. I will then use this method to explore two major transitions in vertebrate evolution. First, I will tackle the fish-to-tetrapod transition and the origin of land locomotion by modelling the evolution of the humerus bone. I will show that the earliest tetrapods occupied a performance valley between water and land adaptive peaks, but that adaptations suggest some capacity for terrestrial locomotion. Second, I will discuss the ‘reptile’-to-mammal transition and the evolution of the mammalian backbone. Using vertebral morphometric data and experimental biomechanics, I will test the lateral-sagittal functional paradigm and demonstrate how this long-held idea is too simplistic to explain mammalian backbone evolution. Together, I will establish the utility of functional adaptive landscapes in quantitatively testing longstanding questions in the vertebrate fossil record and its potential application to unravelling the relationship between form, function, and adaptation across deep time.
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.
UTIG Seminar Series: Ben Phrampus, U.S. Naval Research Laboratory
Start:March 24, 2023 at 10:30 am
End:
March 24, 2023 at 11:30 am
Location:
PRC 196/ROC 1.603
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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Title: Why does the US Navy care about geology? — Geospatial machine learning and an application to Arctic gas hydrates.
Abstract: The US Navy is the seaborne branch of the United States military. To fulfill the Navy’s mission of maintaining security and deterrence, the Navy relies on all earth sciences including geology and geophysics. In this talk I will introduce how the Naval Research Laboratory uses geology and tools, such as machine learning, to safeguard Navy personnel and the warfighter.
As an example of this work, I will discuss recent results of an Arctic-wide assessment of methane gas and hydrate. This work utilizes geospatial machine learned and physics-based inputs, combined with deterministic models to quantify the distribution of methane gas and hydrate contemporarily and during the Last Glacial Maximum (~20 kyrs). These assessments, when used in conjunction, can identify regions most likely to experience hydrate dissociation, potential locations of seafloor fluid flow and gas migration, and regions of active seafloor deformation due to melting permafrost.
Planetary Habitability Series: Katie Teixeira & Jialong Ren, UT Austin
Start:March 27, 2023 at 1:00 pm
End:
March 27, 2023 at 2:00 pm
Location:
PMA 15.216B
Contact:
Brandon Jones, brandon.jones@utexas.edu
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TALK ONE
Speaker: Katie Teixeira, Graduate Student, Department of Astronomy, UT Austin College of Natural Sciences
Host: Brandon Jones
Title: Modeling the Evolution of Terrestrial Planet Atmospheres Through Outgassing and Escape
Abstract: With the successful deployment of JWST, and its aim to potentially search for biosignatures on exoplanets, an important endeavor, at present, is to determine whether the rocky planets we observe are likely to have atmospheres at all. M dwarfs, the main host stars of JWST’s rocky planet targets, are thought to pose a major threat to planetary atmospheres due to their high magnetic activity over several billion-year timescales, and might completely strip planets down to bare rocks. Physical models are necessary to understand how a planet’s atmosphere evolves to become what we see today. Here, I will present coupled time-dependent simulations of atmospheric escape and planetary outgassing, processes that most influence atmospheric size and composition. I will present a case study of TRAPPIST-1c, a possible “exo-Venus” for which observations have recently been taken. I will review the results of simulations of TRAPPIST-1c, specifically the constraints that they place on the history of TRAPPIST-1c’s atmospheric and geological properties. Finally, I will discuss both simulation and observational developments that will aid in understanding rocky planets like TRAPPIST-1c.
Biography: Katie is a 2nd year graduate student in the Department of Astronomy at The University of Texas at Austin. She received a B.S. in Astrophysics and Biology from the University of Florida. There she worked with Sarah Ballard to study the demographics of M dwarf exoplanets and implications for biological evolution. She now works with Caroline Morley, developing and using simulations to model the evolution of CO2-dominated terrestrial planet atmospheres. Broadly, Katie is interested in what makes planets habitable and how to search for both habitable and inhabited planets.
TALK TWO
Speaker: Jialong Ren, Graduate Student, Department of Geological Sciences, UT Austin Jackson School of Geosciences
Host: Brandon Jones
Title: Permeability Limited Compaction and (De)Serpentinization of Ceres
Abstract: The Dawn Mission revealed a surprise that Ceres is still hydrologically active, so its interior structure is important to explain the energy and mass transport at a later stage. In this work, we investigate the compaction history of dwarf planet Ceres with a two-phase flow scheme: viscous compaction of ductile rock coupled with Darcy’s flow in porous media. In such a scheme first used in the differentiation of volatile rich bodies, compaction is limited by pressure gradient required to expel the pore fluid and permeability as a function of porosity. Moreover, we also considered two phase changes: ice-melting and (de)serpentinization.
Biography: My background is in fluid/solid mechanics and numerical simulations. Currently I am interested in planetary science. There are two projects in process: 1) fragmentation and reassembly into rubble piles of planetesimals and 2) compaction and differentiation of small ocean worlds such as Ceres.
RoKafe
Start:March 28, 2023 at 10:00 am
End:
March 28, 2023 at 11:00 am
Location:
JGB 2.104A
Contact:
Nicola Tisato

DeFord Lecture | Dustin Trail
Start:March 30, 2023 at 4:00 pm
End:
March 30, 2023 at 5:00 pm
Location:
JGB 2.324 (Boyd Auditorium)
Contact:
John Lassiter
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Traversing the chemical landscape of the early Earth by Dustin Trail, University of Rochester
Abstract: The conditions that gave rise to life on Earth are still unknown. Despite this, there is broad agreement that the early planet was habitable, with interactions between low-temperature water and rock, potentially creating the substrate upon which life arose. While planetary-scale constraints are a crucial part of habitability, it’s likely that key prebiotic chemistry occurred in smaller, more localized environments. This presentation will examine the early Earth environment on a global scale through zircon chemistry, while also delving into possible local environments and scenarios that may have played a significant role in prebiotic chemistry or the emergence of life.
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.
UTIG Seminar Series: Nicholas Harmon, WHOI
Start:March 31, 2023 at 10:30 am
End:
March 31, 2023 at 11:30 am
Location:
BEG 1.202
Contact:
Constantino Panagopulos, costa@ig.utexas.edu, 512-574-7376
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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 |
