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    <loc>https://www.jenniferkasbohm.com/home</loc>
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    <lastmod>2024-07-10</lastmod>
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      <image:title>Home - About Me</image:title>
    </image:image>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/1630300383536-MNHL0V754BKM80IU29B9/IMG_2846.jpeg</image:loc>
      <image:title>Home - Research</image:title>
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      <image:title>Home - DEI</image:title>
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      <image:title>Home - Teaching</image:title>
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  <url>
    <loc>https://www.jenniferkasbohm.com/pagecv</loc>
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    <lastmod>2025-10-28</lastmod>
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  <url>
    <loc>https://www.jenniferkasbohm.com/teaching</loc>
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    <lastmod>2024-11-12</lastmod>
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      <image:title>Teaching - In the field &amp; lab</image:title>
      <image:caption>Tobias Keene, D.D.S. Hailing from Richmond, Virginia, Dr. Tobias Keene brings a bit of unabashed Southern hospitality to all his patients. He moved to Washington, D.C. over thirty years ago as a freshman at Ivy College. Right after graduation, he attended World University’s School of Dentistry. Before opening Keene Dental in 1994, he worked for free clinics and some of the finest practices in the District. He is part of the 123 Dental Association and stays up-to-date on the latest dental discoveries. When not striving to keep his patients happy and healthy, he’s enjoys hiking with his family in Rock Creek Park.</image:caption>
    </image:image>
    <image:image>
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      <image:title>Teaching - In the classroom</image:title>
      <image:caption>During graduate school, I was an Assistant in Instruction for GEO102: Climate: Past, Present and Future and GEO103: Natural Disasters. These were the Department of Geosciences’ two largest classes, for non-science majors, and I led lab sections for both classes. I believe studying our planet is essential for scientists, humanists, and policy-makers alike, and viewed these classes as an opportunity to develop in my students problem-solving skills, teamwork, and an enhanced appreciation for the Earth system. You can see the planar nature of magmatic injections in our Jell-O volcano above, and our trip to the Princeton Art Gallery to analyze the environmental information conveyed in the painting to the right. As a postdoc, I took part in the semester-long Yale Scientific Teaching Course, attended Advanced Teaching Workshops on effective mentoring and inclusive teaching, and engaged in teaching observations.</image:caption>
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      <image:title>Teaching - In the residential college</image:title>
      <image:caption>One of the most rewarding aspects of my time at Princeton was serving as a Resident Graduate Student in Forbes College. Living amongst first years and sophomores for three years, I was an assigned graduate mentor for ~30 students per year, planned multiple college-wide events (such as the finals week study break pictured here), and ate most of my meals in the dining hall with undergrads. I talked through problems big and small, shared wisdom on how to make the most of available academic resources, and gave them a peek into the life of a Geosciences PhD student.</image:caption>
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  <url>
    <loc>https://www.jenniferkasbohm.com/dei</loc>
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    <priority>0.75</priority>
    <lastmod>2024-11-19</lastmod>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/f16d161c-0d12-4c4c-94f3-0cbfd7207692/STEM+Unbound-127.jpg</image:loc>
      <image:title>DEI - Community Outreach</image:title>
      <image:caption>Tobias Keene, D.D.S. Hailing from Richmond, Virginia, Dr. Tobias Keene brings a bit of unabashed Southern hospitality to all his patients. He moved to Washington, D.C. over thirty years ago as a freshman at Ivy College. Right after graduation, he attended World University’s School of Dentistry. Before opening Keene Dental in 1994, he worked for free clinics and some of the finest practices in the District. He is part of the 123 Dental Association and stays up-to-date on the latest dental discoveries. When not striving to keep his patients happy and healthy, he’s enjoys hiking with his family in Rock Creek Park.</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/1630796476138-YZ8ON76SINYB1KA4JFSO/BA67EBE3-E8B0-46AE-9DFD-048B7311B015_1_201_a.jpeg</image:loc>
      <image:title>DEI - At Princeton</image:title>
      <image:caption>Tobias Keene, D.D.S. Hailing from Richmond, Virginia, Dr. Tobias Keene brings a bit of unabashed Southern hospitality to all his patients. He moved to Washington, D.C. over thirty years ago as a freshman at Ivy College. Right after graduation, he attended World University’s School of Dentistry. Before opening Keene Dental in 1994, he worked for free clinics and some of the finest practices in the District. He is part of the 123 Dental Association and stays up-to-date on the latest dental discoveries. When not striving to keep his patients happy and healthy, he’s enjoys hiking with his family in Rock Creek Park.</image:caption>
    </image:image>
    <image:image>
      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/a4c9ef14-9305-46c8-a586-d39aed17425d/IMG_4982.jpeg</image:loc>
      <image:title>DEI - At Yale</image:title>
      <image:caption>At Yale, I was chosen by the chair to be one of the postdoctoral representatives to the Department of Earth &amp; Planetary Sciences’ Inclusion, Diversity, Equity, and Anti-Racism (IDEA) Committee. In fall 2020, I began IDEA Reading Group, in order to discuss equity issues facing our department, the field of Earth science, and our local New Haven community. In spring 2021, our reading group became an URGE pod, and I served as the pod leader working closely with teams of pod members to draft 8 deliverables for our department. These included a summary of how to report discrimination at Yale and links to demographic data, now published to our department website, and a field work code of conduct modeled on the Princeton GEO code, which is now being used on all EPS field trips and field work. I led IDEA subcommittees on field work inclusivity and a new Womxn in Earth &amp; Planetary Sciences at Yale (WEPSY) organization (modeled on PWiGS), a key aspect of the Broader Impacts of my NSF fellowship. WEPSY hosts monthly social events or group mentoring meetings as well as an annual Women in EPS Day research symposium. I was awarded Yale’s inaugural EPS-IDEA Prize for my “outstanding and sustained contributions to our mission.” Right: Yale Women in EPS Day 2022 organizers: Kels Jenkins, me, Alexie Millikin</image:caption>
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  <url>
    <loc>https://www.jenniferkasbohm.com/about</loc>
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    <lastmod>2024-11-08</lastmod>
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      <image:title>About</image:title>
      <image:caption>I am a Staff Scientist at the Carnegie Science Earth &amp; Planets Laboratory. I was born and raised in central New Jersey, and growing up I loved reading all the books I could, traveling with my family to dozens of national, state, and provincial parks, and studying every type of science. It was thrilling to me to find out when I started college at Yale that I could combine these passions by studying the geosciences. Not only would I learn to tell stories about our planet, I also would have the privilege to spend dozens of weeks seeing it on fieldwork and field trips around the world. I then pursued a PhD in Geosciences at Princeton University, specializing in high-precision U-Pb zircon geochronology by working with Blair Schoene, and becoming an expert on the geochronology of large igneous provinces, Earth’s most extreme magmatic events. I returned to Yale funded by an NSF Postdoctoral Fellowship, and I am now a Staff Scientist in Geochemistry at Carnegie Science in Washington, DC. I hope you enjoy exploring my website - please reach out with any questions or ideas for collaboration! Opportunities Applications for the Carnegie EPL Postdoctoral Fellowship program are due annually on November 1. Please reach out to me in advance if you might be interested in pursuing postdoctoral research in geochronology here at Carnegie! Our new CA-ID-TIMS lab will be up and running in 2026.</image:caption>
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  <url>
    <loc>https://www.jenniferkasbohm.com/gallery</loc>
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    <lastmod>2021-09-06</lastmod>
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      <image:title>Gallery</image:title>
      <image:caption>Proterozoic stromatolites, Transvaal Group, South Africa</image:caption>
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      <image:caption>Pseudotachylite breccia, Vredefort impact, South Africa</image:caption>
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      <image:caption>Boulders Beach penguins, Cape Town, South Africa</image:caption>
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      <image:caption>Sturtian Snowball Earth cap carbonate, Namibia</image:caption>
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      <image:caption>Water lily, Kruger NP, South Africa</image:caption>
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      <image:caption>Table Mountain, Cape Town, South Africa</image:caption>
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      <image:caption>Natural Disasters field trip, Dominica</image:caption>
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      <image:caption>Seismology field work, Peru</image:caption>
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      <image:caption>Structural Geology field trip, Southern CA</image:caption>
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      <image:caption>Pukaskwa NP, Canada</image:caption>
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      <image:caption>Stromatolites, Shark Bay, Australia</image:caption>
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      <image:caption>Banded Iron Formation, Karajini NP, Australia</image:caption>
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      <image:caption>Monitor lizard, Pilbara, Australia</image:caption>
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      <image:caption>Unlithified crossbeds, Pilbara, Australia</image:caption>
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      <image:caption>Unlithified ripples, Pilbara, Australia</image:caption>
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      <image:caption>Sunset, Pilbara, Australia</image:caption>
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      <image:caption>Sunrise, Pilbara, Australia</image:caption>
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      <image:caption>Great catch, Pilbara, Australia</image:caption>
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      <image:caption>Rock art/Archean granite, Pilbara, Australia</image:caption>
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      <image:caption>Meentheena sunset, Pilbara, Australia</image:caption>
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      <image:caption>Basalt-loving snake, Pilbara, Australia</image:caption>
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      <image:caption>Sunset, Pilbara, Australia</image:caption>
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      <image:caption>Fortescue Group stromatolites, Pilbara, Australia</image:caption>
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      <image:caption>Sunrise rainbow, Pilbara, Australia</image:caption>
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      <image:caption>Archean greenstones, Pilbara, Australia</image:caption>
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      <image:caption>Orb weaver spider, Pilbara, Australia</image:caption>
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      <image:caption>Grocery shopping, Port Hedland, Australia</image:caption>
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      <image:caption>Coppin's Gap, Pilbara, Australia</image:caption>
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      <image:caption>Banded iron, Pilbara, Australia</image:caption>
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      <image:caption>Indian Ocean, Cape Range NP, Australia</image:caption>
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      <image:caption>Kangaroo, Cape Range NP, Australia</image:caption>
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  <url>
    <loc>https://www.jenniferkasbohm.com/research-1</loc>
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    <lastmod>2025-07-30</lastmod>
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  <url>
    <loc>https://www.jenniferkasbohm.com/research-1/gts</loc>
    <changefreq>monthly</changefreq>
    <priority>0.5</priority>
    <lastmod>2025-07-30</lastmod>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/1630464839774-5RG1U40SA98X8X26MRL0/16all.jpg</image:loc>
      <image:title>Research - Calibrating Time in Paleoenvironmental Records - Dating Deep-Sea Sediments</image:title>
      <image:caption>While deep-sea sediments are some of our best archives of Earth’s paleoclimate for the last 100 Ma, these have rarely been the subject of a high-precision geochronology study. As an NSF Earth Sciences Postdoctoral Fellow, I produced a new chronology for Site ODP 1000 on the Nicaragua Rise in the Caribbean Sea by performing high-precision zircon geochronology on volcanic ashes deposited at this site. I integrated my ages with a new bulk δ13C and δ18O record across the Miocene Climate Optimum, and created a Bayesian age model for the core that incorporated uncertainty in sample depths resulting from poor recovery. Our Site 1000 ages show that volcanism of the Columbia River Basalt Group (CRBG) large igneous province was coincident with the interval of greatest sustained MCO warmth at this site. Our age model also yields numerical ages for biostratigraphic data in the core. In my future work, I aim to continue dating ashes in ODP cores to not only understand the timing and tempo of Cenozoic environmental change, but also to obtain absolute ages on magnetic field reversals and biostratigraphic data. These constraints will be used to calibrate other successions that lack dateable material, improving alignment of Earth history records! Zircon yield from one of the Miocene ashes I dated in Site ODP 1000</image:caption>
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      <image:title>Research - Calibrating Time in Paleoenvironmental Records - A Burdigalian GSSP?</image:title>
      <image:caption>For my final PhD project, I aimed to provide age constraints for the same magnetic reversals I dated in the CRBG from a section elsewhere in the world. I found a number of promising Italian Early and Middle Miocene carbonate sections with interbedded volcaniclastics , which I sampled in 2018. I obtained zircons and produced a new age model for the Early Miocene carbonates of the Bisciaro Formation in the Contessa Valley. Prior legacy Ar/Ar geochronology, combined with unreliable paleomagnetic results and biostratigraphy subject to reworking, had led to an overestimation of the amount of time captured in this section, showing the importance of obtaining reliable absolute ages. My work also shows that the proposal to locate a Global Stratotype Section and Point (GSSP) in the Bisciaro Formation should be rejected, given the stratigraphic complications and clear presence of hiatuses in this section.</image:caption>
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      <image:title>Research - Calibrating Time in Paleoenvironmental Records - Miocene Magnetostratigraphy</image:title>
      <image:caption>As I produced my new age model for CRBG volcanism, I found that my ages through the basalt stratigraphy yielded ages for magnetic field reversals in the Middle Miocene. The interval from 17-14 Ma had been the poorest-constrained portion of the Neogene Geomagnetic Polarity Time Scale. My reversal ages correspond well with recent astronomically tuned records, and my insights were cited in the 2020 Geologic Time Scale to support a fully astronomically-tuned Neogene timescale. Our new dual-chronometer age model for the CRBG provides new age estimates with uncertainties for these critical reversals. This white ash between CRBG Wanapum Basalt flows provides a close constraint on the base of chron C5Br; field assistant Joshua Murray for scale</image:caption>
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  </url>
  <url>
    <loc>https://www.jenniferkasbohm.com/research-1/precambrian</loc>
    <changefreq>monthly</changefreq>
    <priority>0.5</priority>
    <lastmod>2021-09-01</lastmod>
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      <image:title>Research - Precambrian Plate Tectonics - Sinclair Group, Namibia</image:title>
      <image:caption>As an undergraduate at Yale, I worked with Professor David Evans and graduate student Joe Panzik on a paleomagnetic study of the Mesoproterozoic Sinclair Group in Namibia, to better understand whether it formed on or was later accreted to the Kalahari craton. For my senior thesis, I produced a new paleomagnetic pole for the Aubures redbeds, the youngest formation in the succession, which suggested that the Sinclair was probably part of the Kalahari at ~1.1 Ga. Drilling paleomagnetic samples for Aubures conglomerate test with field assistant Jenna Hessert</image:caption>
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      <image:title>Research - Precambrian Plate Tectonics - Fortescue Group, Australia</image:title>
      <image:caption>I began my PhD research on the 2.7 Ga Fortescue Group in Pilbara, Western Australia; it’s thought to be an early example of a large igneous province. Previous research suggested that the Pilbara craton may have been moving rapidly during two different intervals of Fortescue Group deposition. I performed a detailed volcanostratigraphic study integrating paleomagnetism and geochronology across these intervals, with the goal of obtaining a rate of Archean plate motion. I produced 6 new paleomagnetic poles and 4 new U-Pb CA-ID-TIMS ages for the Fortescue Group that suggest far faster plate motion than observed today or for earlier in the history of the craton. Mount Roe Basalt lava flows, Pear Creek Centrocline; undergraduate field assistant Eric Bolton for scale</image:caption>
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      <image:caption>Sinclair dyke; Joe Panzik and Dave Evans for scale</image:caption>
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  </url>
  <url>
    <loc>https://www.jenniferkasbohm.com/research-1/lips</loc>
    <changefreq>monthly</changefreq>
    <priority>0.5</priority>
    <lastmod>2021-09-01</lastmod>
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      <image:loc>https://images.squarespace-cdn.com/content/v1/612c5f7d0c946b5789526625/bfb39999-6d15-4adb-b28d-0aad9a59f04e/8EBAE0BC-4AAB-4358-8424-B73C44DED0D6.jpeg</image:loc>
      <image:title>Research - Large Igneous Provinces and Environmental Change - Columbia River Basalt Group and Miocene Climate Optimum</image:title>
      <image:caption>The emplacement of the Columbia River Basalt Group (CRBG), Earth’s youngest, smallest, and best-preserved LIP, has been noted for its concurrence with the Miocene Climate Optimum (MCO), an interval of global warming and elevated atmospheric carbon dioxide from 17-15 Ma. However, legacy K-Ar and Ar/Ar ages were unable to resolve the timing and duration of CRBG emplacement. During my PhD, I produced the first high-precision timeline for CRBG eruptions using U-Pb zircon geochronology. I found that the basalts were emplaced in ~750 ka, twice as fast as previously thought, and have calculated volumetric eruption rates through the duration of the province (Kasbohm et al., 2023). As a postdoc I produced the first U-Pb ages across the MCO from ODP Site 1000 (Kasbohm et al., 2024). These ages calibrated a new high-resolution bulk carbon and oxygen isotope record, for a precise comparison between the timing of Miocene climatic fluctuations and known intervals of CRBG eruptions.</image:caption>
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      <image:title>Research - Large Igneous Provinces and Environmental Change - LIP Geochronology Review</image:title>
      <image:caption>As I pursued my work on the CRBG and MCO, I became interested in the temporal correlation of other LIPs and environmental change events. This correlation has led many workers to suggest that LIPs play a causal role in these global perturbations. However, I have encouraged the community of LIP researchers to be wary of the assumption of causation based on correlations made with ~1 Ma precision, when the environmental effects of LIP eruptions occur at 10-100 ka timescales. In an invited review paper (Kasbohm et al., 2021) I revisited 12 pairs of LIP and extinction or climate events and found that only 4 pairs (including my work on the CRBG/MCO) had been the subject of high-precision geochronology studies that investigated the timing of both the LIP and the corresponding perturbation. In 8 other pairs, either the LIP or the perturbation had been well-dated, which still leaves open the question of the extent to which these events are related.</image:caption>
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