Articles | Volume 5, issue 2
https://doi.org/10.5194/gchron-5-301-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/gchron-5-301-2023
© Author(s) 2023. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
17 Jul 2023
Research article |
| 17 Jul 2023
| 17 Jul 2023
Cosmogenic 10Be in pyroxene: laboratory progress, production rate systematics, and application of the 10Be–3He nuclide pair in the Antarctic Dry Valleys
Allie Balter-Kennedy
CORRESPONDING AUTHOR
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Department of Earth and Environmental Sciences, Columbia University,
New York, NY 10027, USA
Joerg M. Schaefer
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Department of Earth and Environmental Sciences, Columbia University,
New York, NY 10027, USA
Roseanne Schwartz
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Jennifer L. Lamp
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Laura Penrose
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Jennifer Middleton
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Jean Hanley
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Bouchaïb Tibari
CRPG, CNRS, Université de Lorraine, 54 000 Nancy, France
Pierre-Henri Blard
CRPG, CNRS, Université de Lorraine, 54 000 Nancy, France
Gisela Winckler
Lamont–Doherty Earth Observatory, Columbia University, Palisades, NY 10964,
USA
Department of Earth and Environmental Sciences, Columbia University,
New York, NY 10027, USA
Alan J. Hidy
Department is Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, Livermore, CA 94550, USA
Greg Balco
Berkeley Geochronology Center, Berkeley, CA 94709, USA
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We constructed a geologic record of East Antarctic Ice Sheet thickness from deposits at Otway Massif to directly assess how Earth's largest ice sheet responds to warmer-than-present climate. Our record confirms the long-term dominance of a cold polar climate but lacks a clear ice sheet response to the mid-Pliocene Warm Period, a common analogue for the future. Instead, an absence of moraines from the late Miocene–early Pliocene suggests the ice sheet was less extensive than present at that time.
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We date sedimentary deposits showing that the southeastern Laurentide Ice Sheet was at or near its southernmost extent from ~ 26 000 to 21 000 years ago, when sea levels were at their lowest, with climate records indicating glacial conditions. Slow deglaciation began ~ 22 000 years ago, shown by a rise in modeled local summer temperatures, but significant deglaciation in the region did not begin until ~ 18 000 years ago, when atmospheric CO2 began to rise, marking the end of the last ice age.
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Understanding how much the Greenland ice sheet melted in response to past warmth helps better predicting future sea-level change. Here we present a framework for using numerical ice-sheet model simulations to provide constraints on how much mass the ice sheet loses before different areas become ice-free. As observations from subglacial archives become more abundant, this framework can guide subglacial sampling efforts to gain the most robust information about past ice-sheet geometries.
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Retreat of the Greenland Ice Sheet (GrIS) margin is exposing a bedrock landscape that holds clues regarding the timing and extent of past ice-sheet minima. We present cosmogenic nuclide measurements from recently deglaciated bedrock surfaces (the last few decades), combined with a refined chronology of southwestern Greenland deglaciation and model simulations of GrIS change. Results suggest that inland retreat of the southwestern GrIS margin was likely minimal in the middle to late Holocene.
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The Cryosphere, 14, 2647–2672, https://doi.org/10.5194/tc-14-2647-2020, https://doi.org/10.5194/tc-14-2647-2020, 2020
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We describe new geologic evidence from Antarctica that demonstrates changes in East Antarctic Ice Sheet (EAIS) extent over the past ~ 15 million years. Our data show that the EAIS was a persistent feature in the Transantarctic Mountains for much of that time, including some (but not all) times when global temperature may have been warmer than today. Overall, our results comprise a long-term record of EAIS change and may provide useful constraints for ice sheet models and sea-level estimates.
Gordon R. M. Bromley, Greg Balco, Margaret S. Jackson, Allie Balter-Kennedy, and Holly Thomas
Clim. Past, 21, 145–160, https://doi.org/10.5194/cp-21-145-2025, https://doi.org/10.5194/cp-21-145-2025, 2025
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Joseph P. Tulenko, Greg Balco, Michael A. Clynne, and L. J. Patrick Muffler
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Cosmogenic nuclide exposure dating is an exceptional tool for reconstructing glacier histories, but reconstructions based on common target nuclides (e.g., 10Be) can be costly and time-consuming to generate. Here, we present a cost-effective proof-of-concept 21Ne exposure age chronology from Lassen Volcanic National Park, CA, USA, that broadly agrees with nearby 10Be chronologies but at lower precision.
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Cosmogenic nuclides, such as 10Be, are rare isotopes produced in rocks when exposed at Earth's surface and are valuable for understanding surface processes and landscape evolution. However, 10Be is usually measured in quartz minerals. Here we present advances in efficiently extracting and measuring 10Be in the pyroxene mineral. These measurements expand the use of 10Be as a dating tool for new rock types and provide opportunities to understand landscape processes in areas that lack quartz.
Alia J. Lesnek, Joseph M. Licciardi, Alan J. Hidy, and Tyler S. Anderson
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Pedro Doll, Shaun Robert Eaves, Ben Matthew Kennedy, Pierre-Henri Blard, Alexander Robert Lee Nichols, Graham Sloan Leonard, Dougal Bruce Townsend, Jim William Cole, Chris Edward Conway, Sacha Baldwin, Gabriel Fénisse, Laurent Zimmermann, and Bouchaïb Tibari
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Joanne S. Johnson, John Woodward, Ian Nesbitt, Kate Winter, Seth Campbell, Keir A. Nichols, Ryan A. Venturelli, Scott Braddock, Brent M. Goehring, Brenda Hall, Dylan H. Rood, and Greg Balco
EGUsphere, https://doi.org/10.5194/egusphere-2024-1452, https://doi.org/10.5194/egusphere-2024-1452, 2024
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Joseph P. Tulenko, Jason P. Briner, Nicolás E. Young, and Joerg M. Schaefer
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Greg Balco, Alan J. Hidy, William T. Struble, and Joshua J. Roering
Geochronology, 6, 71–76, https://doi.org/10.5194/gchron-6-71-2024, https://doi.org/10.5194/gchron-6-71-2024, 2024
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We describe a new method of reconstructing the long-term, pre-observational frequency and/or intensity of wildfires in forested landscapes using trace concentrations of the noble gases helium and neon that are formed in soil mineral grains by cosmic-ray bombardment of the Earth's surface.
Jacob T. H. Anderson, Toshiyuki Fujioka, David Fink, Alan J. Hidy, Gary S. Wilson, Klaus Wilcken, Andrey Abramov, and Nikita Demidov
The Cryosphere, 17, 4917–4936, https://doi.org/10.5194/tc-17-4917-2023, https://doi.org/10.5194/tc-17-4917-2023, 2023
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Brandon L. Graham, Jason P. Briner, Nicolás E. Young, Allie Balter-Kennedy, Michele Koppes, Joerg M. Schaefer, Kristin Poinar, and Elizabeth K. Thomas
The Cryosphere, 17, 4535–4547, https://doi.org/10.5194/tc-17-4535-2023, https://doi.org/10.5194/tc-17-4535-2023, 2023
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Glacial erosion is a fundamental process operating on Earth's surface. Two processes of glacial erosion, abrasion and plucking, are poorly understood. We reconstructed rates of abrasion and quarrying in Greenland. We derive a total glacial erosion rate of 0.26 ± 0.16 mm per year. We also learned that erosion via these two processes is about equal. Because the site is similar to many other areas covered by continental ice sheets, these results may be applied to many places on Earth.
Adam C. Hawkins, Brian Menounos, Brent M. Goehring, Gerald Osborn, Ben M. Pelto, Christopher M. Darvill, and Joerg M. Schaefer
The Cryosphere, 17, 4381–4397, https://doi.org/10.5194/tc-17-4381-2023, https://doi.org/10.5194/tc-17-4381-2023, 2023
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Our study developed a record of glacier and climate change in the Mackenzie and Selwyn mountains of northwestern Canada over the past several hundred years. We estimate temperature change in this region using several methods and incorporate our glacier record with models of climate change to estimate how glacier volume in our study area has changed over time. Models of future glacier change show that our study area will become largely ice-free by the end of the 21st century.
Benoit S. Lecavalier, Lev Tarasov, Greg Balco, Perry Spector, Claus-Dieter Hillenbrand, Christo Buizert, Catherine Ritz, Marion Leduc-Leballeur, Robert Mulvaney, Pippa L. Whitehouse, Michael J. Bentley, and Jonathan Bamber
Earth Syst. Sci. Data, 15, 3573–3596, https://doi.org/10.5194/essd-15-3573-2023, https://doi.org/10.5194/essd-15-3573-2023, 2023
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The Antarctic Ice Sheet Evolution constraint database version 2 (AntICE2) consists of a large variety of observations that constrain the evolution of the Antarctic Ice Sheet over the last glacial cycle. This includes observations of past ice sheet extent, past ice thickness, past relative sea level, borehole temperature profiles, and present-day bedrock displacement rates. The database is intended to improve our understanding of past Antarctic changes and for ice sheet model calibrations.
Greg Balco, Nathan Brown, Keir Nichols, Ryan A. Venturelli, Jonathan Adams, Scott Braddock, Seth Campbell, Brent Goehring, Joanne S. Johnson, Dylan H. Rood, Klaus Wilcken, Brenda Hall, and John Woodward
The Cryosphere, 17, 1787–1801, https://doi.org/10.5194/tc-17-1787-2023, https://doi.org/10.5194/tc-17-1787-2023, 2023
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Samples of bedrock recovered from below the West Antarctic Ice Sheet show that part of the ice sheet was thinner several thousand years ago than it is now and subsequently thickened. This is important because of concern that present ice thinning in this region may lead to rapid, irreversible sea level rise. The past episode of thinning at this site that took place in a similar, although not identical, climate was not irreversible; however, reversal required at least 3000 years to complete.
Anna Ruth W. Halberstadt, Greg Balco, Hannah Buchband, and Perry Spector
The Cryosphere, 17, 1623–1643, https://doi.org/10.5194/tc-17-1623-2023, https://doi.org/10.5194/tc-17-1623-2023, 2023
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This paper explores the use of multimillion-year exposure ages from Antarctic bedrock outcrops to benchmark ice sheet model predictions and thereby infer ice sheet sensitivity to warm climates. We describe a new approach for model–data comparison, highlight an example where observational data are used to distinguish end-member models, and provide guidance for targeted sampling around Antarctica that can improve understanding of ice sheet response to climate warming in the past and future.
Jonathan R. Adams, Joanne S. Johnson, Stephen J. Roberts, Philippa J. Mason, Keir A. Nichols, Ryan A. Venturelli, Klaus Wilcken, Greg Balco, Brent Goehring, Brenda Hall, John Woodward, and Dylan H. Rood
The Cryosphere, 16, 4887–4905, https://doi.org/10.5194/tc-16-4887-2022, https://doi.org/10.5194/tc-16-4887-2022, 2022
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Glaciers in West Antarctica are experiencing significant ice loss. Geological data provide historical context for ongoing ice loss in West Antarctica, including constraints on likely future ice sheet behaviour in response to climatic warming. We present evidence from rare isotopes measured in rocks collected from an outcrop next to Pope Glacier. These data suggest that Pope Glacier thinned faster and sooner after the last ice age than previously thought.
Benjamin J. Stoker, Martin Margold, John C. Gosse, Alan J. Hidy, Alistair J. Monteath, Joseph M. Young, Niall Gandy, Lauren J. Gregoire, Sophie L. Norris, and Duane Froese
The Cryosphere, 16, 4865–4886, https://doi.org/10.5194/tc-16-4865-2022, https://doi.org/10.5194/tc-16-4865-2022, 2022
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The Laurentide Ice Sheet was the largest ice sheet to grow and disappear in the Northern Hemisphere during the last glaciation. In northwestern Canada, it covered the Mackenzie Valley, blocking the migration of fauna and early humans between North America and Beringia and altering the drainage systems. We reconstruct the timing of ice sheet retreat in this region and the implications for the migration of early humans into North America, the drainage of glacial lakes, and past sea level rise.
Natacha Gribenski, Marissa M. Tremblay, Pierre G. Valla, Greg Balco, Benny Guralnik, and David L. Shuster
Geochronology, 4, 641–663, https://doi.org/10.5194/gchron-4-641-2022, https://doi.org/10.5194/gchron-4-641-2022, 2022
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We apply quartz 3He paleothermometry along two deglaciation profiles in the European Alps to reconstruct temperature evolution since the Last Glacial Maximum. We observe a 3He thermal signal clearly colder than today in all bedrock surface samples exposed prior the Holocene. Current uncertainties in 3He diffusion kinetics do not permit distinguishing if this signal results from Late Pleistocene ambient temperature changes or from recent ground temperature variation due to permafrost degradation.
Jason P. Briner, Caleb K. Walcott, Joerg M. Schaefer, Nicolás E. Young, Joseph A. MacGregor, Kristin Poinar, Benjamin A. Keisling, Sridhar Anandakrishnan, Mary R. Albert, Tanner Kuhl, and Grant Boeckmann
The Cryosphere, 16, 3933–3948, https://doi.org/10.5194/tc-16-3933-2022, https://doi.org/10.5194/tc-16-3933-2022, 2022
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The 7.4 m of sea level equivalent stored as Greenland ice is getting smaller every year. The uncertain trajectory of ice loss could be better understood with knowledge of the ice sheet's response to past climate change. Within the bedrock below the present-day ice sheet is an archive of past ice-sheet history. We analyze all available data from Greenland to create maps showing where on the ice sheet scientists can drill, using currently available drills, to obtain sub-ice materials.
Marie Bergelin, Jaakko Putkonen, Greg Balco, Daniel Morgan, Lee B. Corbett, and Paul R. Bierman
The Cryosphere, 16, 2793–2817, https://doi.org/10.5194/tc-16-2793-2022, https://doi.org/10.5194/tc-16-2793-2022, 2022
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Glacier ice contains information on past climate and can help us understand how the world changes through time. We have found and sampled a buried ice mass in Antarctica that is much older than most ice on Earth and difficult to date. Therefore, we developed a new dating application which showed the ice to be 3 million years old. Our new dating solution will potentially help to date other ancient ice masses since such old glacial ice could yield data on past environmental conditions on Earth.
Mae Kate Campbell, Paul R. Bierman, Amanda H. Schmidt, Rita Sibello Hernández, Alejandro García-Moya, Lee B. Corbett, Alan J. Hidy, Héctor Cartas Águila, Aniel Guillén Arruebarrena, Greg Balco, David Dethier, and Marc Caffee
Geochronology, 4, 435–453, https://doi.org/10.5194/gchron-4-435-2022, https://doi.org/10.5194/gchron-4-435-2022, 2022
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We used cosmogenic radionuclides in detrital river sediment to measure erosion rates of watersheds in central Cuba; erosion rates are lower than rock dissolution rates in lowland watersheds. Data from two different cosmogenic nuclides suggest that some basins may have a mixed layer deeper than is typically modeled and could have experienced significant burial after or during exposure. We conclude that significant mass loss may occur at depth through chemical weathering processes.
Joanne S. Johnson, Ryan A. Venturelli, Greg Balco, Claire S. Allen, Scott Braddock, Seth Campbell, Brent M. Goehring, Brenda L. Hall, Peter D. Neff, Keir A. Nichols, Dylan H. Rood, Elizabeth R. Thomas, and John Woodward
The Cryosphere, 16, 1543–1562, https://doi.org/10.5194/tc-16-1543-2022, https://doi.org/10.5194/tc-16-1543-2022, 2022
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Recent studies have suggested that some portions of the Antarctic Ice Sheet were less extensive than present in the last few thousand years. We discuss how past ice loss and regrowth during this time would leave its mark on geological and glaciological records and suggest ways in which future studies could detect such changes. Determining timing of ice loss and gain around Antarctica and conditions under which they occurred is critical for preparing for future climate-warming-induced changes.
Leah A. VanLandingham, Eric W. Portenga, Edward C. Lefroy, Amanda H. Schmidt, Paul R. Bierman, and Alan J. Hidy
Geochronology, 4, 153–176, https://doi.org/10.5194/gchron-4-153-2022, https://doi.org/10.5194/gchron-4-153-2022, 2022
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This study presents erosion rates of the George River and seven of its tributaries in northeast Tasmania, Australia. These erosion rates are the first measures of landscape change over millennial timescales for Tasmania. We demonstrate that erosion is closely linked to a topographic rainfall gradient across George River. Our findings may be useful for efforts to restore ecological health to Georges Bay by determining a pre-disturbance level of erosion and sediment delivery to this estuary.
María H. Toyos, Gisela Winckler, Helge W. Arz, Lester Lembke-Jene, Carina B. Lange, Gerhard Kuhn, and Frank Lamy
Clim. Past, 18, 147–166, https://doi.org/10.5194/cp-18-147-2022, https://doi.org/10.5194/cp-18-147-2022, 2022
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Past export production in the southeast Pacific and its link to Patagonian ice dynamics is unknown. We reconstruct biological productivity changes at the Pacific entrance to the Drake Passage, covering the past 400 000 years. We show that glacial–interglacial variability in export production responds to glaciogenic Fe supply from Patagonia and silica availability due to shifts in oceanic fronts, whereas dust, as a source of lithogenic material, plays a minor role.
Irene Schimmelpfennig, Joerg M. Schaefer, Jennifer Lamp, Vincent Godard, Roseanne Schwartz, Edouard Bard, Thibaut Tuna, Naki Akçar, Christian Schlüchter, Susan Zimmerman, and ASTER Team
Clim. Past, 18, 23–44, https://doi.org/10.5194/cp-18-23-2022, https://doi.org/10.5194/cp-18-23-2022, 2022
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Small mountain glaciers advance and recede as a response to summer temperature changes. Dating of glacial landforms with cosmogenic nuclides allowed us to reconstruct the advance and retreat history of an Alpine glacier throughout the past ~ 11 000 years, the Holocene. The results contribute knowledge to the debate of Holocene climate evolution, indicating that during most of this warm period, summer temperatures were similar to or warmer than in modern times.
Jamey Stutz, Andrew Mackintosh, Kevin Norton, Ross Whitmore, Carlo Baroni, Stewart S. R. Jamieson, Richard S. Jones, Greg Balco, Maria Cristina Salvatore, Stefano Casale, Jae Il Lee, Yeong Bae Seong, Robert McKay, Lauren J. Vargo, Daniel Lowry, Perry Spector, Marcus Christl, Susan Ivy Ochs, Luigia Di Nicola, Maria Iarossi, Finlay Stuart, and Tom Woodruff
The Cryosphere, 15, 5447–5471, https://doi.org/10.5194/tc-15-5447-2021, https://doi.org/10.5194/tc-15-5447-2021, 2021
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Understanding the long-term behaviour of ice sheets is essential to projecting future changes due to climate change. In this study, we use rocks deposited along the margin of the David Glacier, one of the largest glacier systems in the world, to reveal a rapid thinning event initiated over 7000 years ago and endured for ~ 2000 years. Using physical models, we show that subglacial topography and ocean heat are important drivers for change along this sector of the Antarctic Ice Sheet.
Sandra M. Braumann, Joerg M. Schaefer, Stephanie M. Neuhuber, Christopher Lüthgens, Alan J. Hidy, and Markus Fiebig
Clim. Past, 17, 2451–2479, https://doi.org/10.5194/cp-17-2451-2021, https://doi.org/10.5194/cp-17-2451-2021, 2021
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Glacier reconstructions provide insights into past climatic conditions and elucidate processes and feedbacks that modulate the climate system both in the past and present. We investigate the transition from the last glacial to the current interglacial and generate beryllium-10 moraine chronologies in glaciated catchments of the eastern European Alps. We find that rapid warming was superimposed by centennial-scale cold phases that appear to have influenced large parts of the Northern Hemisphere.
Andrew J. Christ, Paul R. Bierman, Jennifer L. Lamp, Joerg M. Schaefer, and Gisela Winckler
Geochronology, 3, 505–523, https://doi.org/10.5194/gchron-3-505-2021, https://doi.org/10.5194/gchron-3-505-2021, 2021
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Cosmogenic nuclide surface exposure dating is commonly used to constrain the timing of past glacier extents. However, Antarctic exposure age datasets are often scattered and difficult to interpret. We compile new and existing exposure ages of a glacial deposit with independently known age constraints and identify surface processes that increase or reduce the likelihood of exposure age scatter. Then we present new data for a previously unmapped and undated older deposit from the same region.
Nicolás E. Young, Alia J. Lesnek, Josh K. Cuzzone, Jason P. Briner, Jessica A. Badgeley, Alexandra Balter-Kennedy, Brandon L. Graham, Allison Cluett, Jennifer L. Lamp, Roseanne Schwartz, Thibaut Tuna, Edouard Bard, Marc W. Caffee, Susan R. H. Zimmerman, and Joerg M. Schaefer
Clim. Past, 17, 419–450, https://doi.org/10.5194/cp-17-419-2021, https://doi.org/10.5194/cp-17-419-2021, 2021
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Retreat of the Greenland Ice Sheet (GrIS) margin is exposing a bedrock landscape that holds clues regarding the timing and extent of past ice-sheet minima. We present cosmogenic nuclide measurements from recently deglaciated bedrock surfaces (the last few decades), combined with a refined chronology of southwestern Greenland deglaciation and model simulations of GrIS change. Results suggest that inland retreat of the southwestern GrIS margin was likely minimal in the middle to late Holocene.
Greg Balco, Benjamin D. DeJong, John C. Ridge, Paul R. Bierman, and Dylan H. Rood
Geochronology, 3, 1–33, https://doi.org/10.5194/gchron-3-1-2021, https://doi.org/10.5194/gchron-3-1-2021, 2021
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The North American Varve Chronology (NAVC) is a sequence of 5659 annual sedimentary layers that were deposited in proglacial lakes adjacent to the retreating Laurentide Ice Sheet ca. 12 500–18 200 years ago. We attempt to synchronize this record with Greenland ice core and other climate records that cover the same time period by detecting variations in global fallout of atmospherically produced beryllium-10 in NAVC sediments.
Allie Balter-Kennedy, Gordon Bromley, Greg Balco, Holly Thomas, and Margaret S. Jackson
The Cryosphere, 14, 2647–2672, https://doi.org/10.5194/tc-14-2647-2020, https://doi.org/10.5194/tc-14-2647-2020, 2020
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We describe new geologic evidence from Antarctica that demonstrates changes in East Antarctic Ice Sheet (EAIS) extent over the past ~ 15 million years. Our data show that the EAIS was a persistent feature in the Transantarctic Mountains for much of that time, including some (but not all) times when global temperature may have been warmer than today. Overall, our results comprise a long-term record of EAIS change and may provide useful constraints for ice sheet models and sea-level estimates.
Greg Balco
Geochronology, 2, 169–175, https://doi.org/10.5194/gchron-2-169-2020, https://doi.org/10.5194/gchron-2-169-2020, 2020
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Geologic dating methods generally do not directly measure ages. Instead, interpreting a geochemical measurement as an age requires a middle layer of calculations and supporting data, and the fact that this layer continually improves is an obstacle to synoptic analysis of geochronological data. This paper describes a prototype data management and analysis system that addresses this obstacle by making the middle-layer calculations transparent and dynamic to the user.
Michal Ben-Israel, Ari Matmon, Alan J. Hidy, Yoav Avni, and Greg Balco
Earth Surf. Dynam., 8, 289–301, https://doi.org/10.5194/esurf-8-289-2020, https://doi.org/10.5194/esurf-8-289-2020, 2020
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Early-to-mid Miocene erosion rates were inferred using cosmogenic 21Ne measured in chert pebbles transported by the Miocene Hazeva River (~ 18 Ma). Miocene erosion rates are faster compared to Quaternary rates in the region. Faster Miocene erosion rates could be due to a response to topographic changes brought on by tectonic uplift, wetter climate in the region during the Miocene, or a combination of both.
Apolline Mariotti, Pierre-Henri Blard, Julien Charreau, Carole Petit, Stéphane Molliex, and the ASTER Team
Earth Surf. Dynam., 7, 1059–1074, https://doi.org/10.5194/esurf-7-1059-2019, https://doi.org/10.5194/esurf-7-1059-2019, 2019
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This work is the first assessment of the suitability of the in situ 10Be method to determine denudation rates from fine (50–100 μm) detrital quartz at the watershed scale. This method is used worldwide to determine denudation rates from sandy sediments (250 μm-1 mm). We show that in the Var catchment fine-grained sediments (50–100 μm) are suited to the 10Be method, which is vital for future applications of 10Be in sedimentary archives such as offshore sediments.
Keir A. Nichols, Brent M. Goehring, Greg Balco, Joanne S. Johnson, Andrew S. Hein, and Claire Todd
The Cryosphere, 13, 2935–2951, https://doi.org/10.5194/tc-13-2935-2019, https://doi.org/10.5194/tc-13-2935-2019, 2019
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We studied the history of ice masses at three locations in the Weddell Sea Embayment, Antarctica. We measured rare isotopes in material sourced from mountains overlooking the Slessor Glacier, Foundation Ice Stream, and smaller glaciers on the Lassiter Coast. We show that ice masses were between 385 and 800 m thicker during the last glacial cycle than they are at present. The ice masses were both hundreds of metres thicker and remained thicker closer to the present than was previously thought.
Greg Balco, Kimberly Blisniuk, and Alan Hidy
Geochronology, 1, 1–16, https://doi.org/10.5194/gchron-1-1-2019, https://doi.org/10.5194/gchron-1-1-2019, 2019
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This article applies a new geochemical dating method to determine the age of sedimentary deposits useful in reconstructing slip rates on a major fault system.
Maxwell T. Cunningham, Colin P. Stark, Michael R. Kaplan, and Joerg M. Schaefer
Earth Surf. Dynam., 7, 147–169, https://doi.org/10.5194/esurf-7-147-2019, https://doi.org/10.5194/esurf-7-147-2019, 2019
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Glacial erosion is known to limit the height of midlatitude mountain ranges affected by substantial glaciation during cold periods. Our study examines this phenomenon in the tropics. A new form of hypsometric analysis, along with other evidence, of 10 tropical ranges reveals widespread signs of a perched glacial base level at the ELA. Although glacial influence is moderate to weak in these environments, the evidence suggests that glacial erosion acts to limit the height of tropical ranges.
Joshua M. Maurer, Summer B. Rupper, and Joerg M. Schaefer
The Cryosphere, 10, 2203–2215, https://doi.org/10.5194/tc-10-2203-2016, https://doi.org/10.5194/tc-10-2203-2016, 2016
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Here we utilize declassified spy satellite imagery to quantify ice volume loss of glaciers in the eastern Himalayas over approximately the last three decades. Clean-ice and debris-covered glaciers show similar magnitudes of ice loss, while calving glaciers are contributing a disproportionately large amount to total ice loss. Results highlight important physical processes affecting the ice mass budget and associated water resources in the Himalayas.
Shaun R. Eaves, Andrew N. Mackintosh, Brian M. Anderson, Alice M. Doughty, Dougal B. Townsend, Chris E. Conway, Gisela Winckler, Joerg M. Schaefer, Graham S. Leonard, and Andrew T. Calvert
Clim. Past, 12, 943–960, https://doi.org/10.5194/cp-12-943-2016, https://doi.org/10.5194/cp-12-943-2016, 2016
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Geological evidence for past changes in glacier length provides a useful source of information about pre-historic climate change. We have used glacier modelling to show that air temperature reductions of −5 to −7 °C, relative to present, are required to simulate the glacial extent in the North Island, New Zealand, during the last ice age (approx. 20000 years ago). Our results provide data to assess climate model simulations, with the aim of determining the drivers of past natural climate change.
S. Albani, N. M. Mahowald, G. Winckler, R. F. Anderson, L. I. Bradtmiller, B. Delmonte, R. François, M. Goman, N. G. Heavens, P. P. Hesse, S. A. Hovan, S. G. Kang, K. E. Kohfeld, H. Lu, V. Maggi, J. A. Mason, P. A. Mayewski, D. McGee, X. Miao, B. L. Otto-Bliesner, A. T. Perry, A. Pourmand, H. M. Roberts, N. Rosenbloom, T. Stevens, and J. Sun
Clim. Past, 11, 869–903, https://doi.org/10.5194/cp-11-869-2015, https://doi.org/10.5194/cp-11-869-2015, 2015
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We propose an innovative framework to organize paleodust records, formalized in a publicly accessible database, and discuss the emerging properties of the global dust cycle during the Holocene by integrating our analysis with simulations performed with the Community Earth System Model. We show how the size distribution of dust is intrinsically related to the dust mass accumulation rates and that only considering a consistent size range allows for a consistent analysis of the global dust cycle.
Related subject area
Cosmogenic nuclide dating
Cosmogenic 21Ne exposure ages on late Pleistocene moraines in Lassen Volcanic National Park, California, USA
Technical note: Altitude scaling of 36Cl production from Fe
Terrestrial Cosmogenic Nuclide depth profiles used to infer changes in Holocene glacier cover, Vintage Peak, Southern Coast Mountains, British Columbia
Production rate calibration for cosmogenic 10Be in pyroxene by applying a rapid fusion method to 10Be-saturated samples from the Transantarctic Mountains, Antarctica
Technical note: Optimizing the in situ cosmogenic 36Cl extraction and measurement workflow for geologic applications
Cosmogenic 3He chronology of postglacial lava flows at Mt Ruapehu, Aotearoa / New Zealand
Last ice sheet recession and landscape emergence above sea level in east-central Sweden, evaluated using in situ cosmogenic 14C from quartz
Regional beryllium-10 production rate for the mid-elevation mountainous regions in central Europe, deduced from a multi-method study of moraines and lake sediments in the Black Forest
Short communication: Cosmogenic noble gas depletion in soils by wildfire heating
Early Holocene ice retreat from Isle Royale in the Laurentian Great Lakes constrained with 10Be exposure-age dating
Technical note: Studying lithium metaborate fluxes and extraction protocols with a new, fully automated in situ cosmogenic 14C processing system at PRIME Lab
Technical note: A software framework for calculating compositionally dependent in situ 14C production rates
10Be age control of glaciation in the Beartooth Mountains, USA, from the latest Pleistocene through the Holocene
Constraining the aggradation mode of Pleistocene river deposits based on cosmogenic radionuclide depth profiling and numerical modelling
Technical note: Evaluating a geographical information system (GIS)-based approach for determining topographic shielding factors in cosmic-ray exposure dating
Combined linear-regression and Monte Carlo approach to modeling exposure age depth profiles
Cosmogenic nuclide weathering biases: corrections and potential for denudation and weathering rate measurements
Cosmogenic nuclide and solute flux data from central Cuban rivers emphasize the importance of both physical and chemical mass loss from tropical landscapes
Technical note: Accelerator mass spectrometry of 10Be and 26Al at low nuclide concentrations
Reconciling the apparent absence of a Last Glacial Maximum alpine glacial advance, Yukon Territory, Canada, through cosmogenic beryllium-10 and carbon-14 measurements
Cosmogenic ages indicate no MIS 2 refugia in the Alexander Archipelago, Alaska
In situ-produced cosmogenic krypton in zircon and its potential for Earth surface applications
Cosmogenic nuclide exposure age scatter records glacial history and processes in McMurdo Sound, Antarctica
Technical Note: Noble gas extraction procedure and performance of the Cologne Helix MC Plus multi-collector noble gas mass spectrometer for cosmogenic neon isotope analysis
Exposure dating of detrital magnetite using 3He enabled by microCT and calibration of the cosmogenic 3He production rate in magnetite
Calibrating a long-term meteoric 10Be delivery rate into eroding western US glacial deposits by comparing meteoric and in situ produced 10Be depth profiles
Delayed and rapid deglaciation of alpine valleys in the Sawatch Range, southern Rocky Mountains, USA
Technical note: A prototype transparent-middle-layer data management and analysis infrastructure for cosmogenic-nuclide exposure dating
Isolation of quartz for cosmogenic in situ 14C analysis
Chlorine-36∕beryllium-10 burial dating of alluvial fan sediments associated with the Mission Creek strand of the San Andreas Fault system, California, USA
Joseph P. Tulenko, Greg Balco, Michael A. Clynne, and L. J. Patrick Muffler
Geochronology, 6, 639–652, https://doi.org/10.5194/gchron-6-639-2024, https://doi.org/10.5194/gchron-6-639-2024, 2024
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Cosmogenic nuclide exposure dating is an exceptional tool for reconstructing glacier histories, but reconstructions based on common target nuclides (e.g., 10Be) can be costly and time-consuming to generate. Here, we present a cost-effective proof-of-concept 21Ne exposure age chronology from Lassen Volcanic National Park, CA, USA, that broadly agrees with nearby 10Be chronologies but at lower precision.
Angus K. Moore and Darryl E. Granger
Geochronology, 6, 541–552, https://doi.org/10.5194/gchron-6-541-2024, https://doi.org/10.5194/gchron-6-541-2024, 2024
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Cosmogenic nuclide geochronology requires accurately scaling production rates with altitude. The energy spectrum of cosmic radiation changes with altitude, and reactions that are sensitive to different energies may have different scaling behavior. Here, we model the altitude scaling of 36Cl production from Fe and evaluate this model against calibration data. The data are broadly consistent with the prediction of larger-altitude scaling factors for 36Cl from Fe than for other reactions.
Adam C. Hawkins, Brent M. Goehring, and Brian Menounos
EGUsphere, https://doi.org/10.5194/egusphere-2024-2900, https://doi.org/10.5194/egusphere-2024-2900, 2024
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We use a method called cosmogenic nuclide dating on bedrock surfaces and moraine boulders to determine the relative length of time an alpine glacier was larger or smaller than its current extent over the past 15 thousand years. We also discuss several important limitations to this method. This method gives information on the duration of past ice advances and is useful in areas without other materials that can be dated.
Marie Bergelin, Greg Balco, Lee B. Corbett, and Paul R. Bierman
Geochronology, 6, 491–502, https://doi.org/10.5194/gchron-6-491-2024, https://doi.org/10.5194/gchron-6-491-2024, 2024
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Cosmogenic nuclides, such as 10Be, are rare isotopes produced in rocks when exposed at Earth's surface and are valuable for understanding surface processes and landscape evolution. However, 10Be is usually measured in quartz minerals. Here we present advances in efficiently extracting and measuring 10Be in the pyroxene mineral. These measurements expand the use of 10Be as a dating tool for new rock types and provide opportunities to understand landscape processes in areas that lack quartz.
Alia J. Lesnek, Joseph M. Licciardi, Alan J. Hidy, and Tyler S. Anderson
Geochronology, 6, 475–489, https://doi.org/10.5194/gchron-6-475-2024, https://doi.org/10.5194/gchron-6-475-2024, 2024
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We present an improved workflow for extracting and measuring chlorine isotopes in rocks and minerals. Experiments on seven geologic samples demonstrate that our workflow provides reliable results while offering several distinct advantages over traditional methods. Most notably, our workflow reduces the amount of isotopically enriched chlorine spike used per rock sample by up to 95 %, which will allow researchers to analyze more samples using their existing laboratory supplies.
Pedro Doll, Shaun Robert Eaves, Ben Matthew Kennedy, Pierre-Henri Blard, Alexander Robert Lee Nichols, Graham Sloan Leonard, Dougal Bruce Townsend, Jim William Cole, Chris Edward Conway, Sacha Baldwin, Gabriel Fénisse, Laurent Zimmermann, and Bouchaïb Tibari
Geochronology, 6, 365–395, https://doi.org/10.5194/gchron-6-365-2024, https://doi.org/10.5194/gchron-6-365-2024, 2024
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In this study, we use cosmogenic-sourced 3He to determine the eruption ages of 23 lava flows at Mt Ruapehu, Aotearoa New Zealand, and we show how this method can help overcome challenges associated with traditional dating methods in young lavas. Comparison with other methods demonstrates the accuracy of our data and the method's reliability. The new eruption ages allowed us to identify periods of quasi-simultaneous activity from different volcanic vents during the last 20 000 years.
Bradley W. Goodfellow, Arjen P. Stroeven, Nathaniel A. Lifton, Jakob Heyman, Alexander Lewerentz, Kristina Hippe, Jens-Ove Näslund, and Marc W. Caffee
Geochronology, 6, 291–302, https://doi.org/10.5194/gchron-6-291-2024, https://doi.org/10.5194/gchron-6-291-2024, 2024
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Carbon-14 produced in quartz (half-life of 5700 ± 30 years) provides a new tool to date exposure of bedrock surfaces. Samples from 10 exposed bedrock surfaces in east-central Sweden give dates consistent with the timing of both landscape emergence above sea level through postglacial rebound and retreat of the last ice sheet shown in previous reconstructions. Carbon-14 in quartz can therefore be used for dating in landscapes where isotopes with longer half-lives give complex exposure results.
Felix Martin Hofmann, Claire Rambeau, Lukas Gegg, Melanie Schulz, Martin Steiner, Alexander Fülling, Laëtitia Léanni, Frank Preusser, and ASTER Team
Geochronology, 6, 147–174, https://doi.org/10.5194/gchron-6-147-2024, https://doi.org/10.5194/gchron-6-147-2024, 2024
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We determined 10Be concentrations in moraine boulder surfaces in the southern Black Forest, SW Germany. We applied three independent dating methods to younger lake sediments. With the aid of independent age datasets, we calculated the growth of 10Be concentrations in moraine boulder surfaces.
Greg Balco, Alan J. Hidy, William T. Struble, and Joshua J. Roering
Geochronology, 6, 71–76, https://doi.org/10.5194/gchron-6-71-2024, https://doi.org/10.5194/gchron-6-71-2024, 2024
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We describe a new method of reconstructing the long-term, pre-observational frequency and/or intensity of wildfires in forested landscapes using trace concentrations of the noble gases helium and neon that are formed in soil mineral grains by cosmic-ray bombardment of the Earth's surface.
Eric W. Portenga, David J. Ullman, Lee B. Corbett, Paul R. Bierman, and Marc W. Caffee
Geochronology, 5, 413–431, https://doi.org/10.5194/gchron-5-413-2023, https://doi.org/10.5194/gchron-5-413-2023, 2023
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New exposure ages of glacial erratics on moraines on Isle Royale – the largest island in North America's Lake Superior – show that the Laurentide Ice Sheet did not retreat from the island nor the south shores of Lake Superior until the early Holocene, which is later than previously thought. These new ages unify regional ice retreat histories from the mainland, the Lake Superior lake-bottom stratigraphy, underwater moraines, and meltwater drainage pathways through the Laurentian Great Lakes.
Nathaniel Lifton, Jim Wilson, and Allie Koester
Geochronology, 5, 361–375, https://doi.org/10.5194/gchron-5-361-2023, https://doi.org/10.5194/gchron-5-361-2023, 2023
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We describe a new, fully automated extraction system for in situ 14C at PRIME Lab that incorporates more reliable components and designs than our original systems. We use a LiBO2 flux to dissolve a quartz sample in oxygen after removing contaminant 14C with a lower-temperature combustion step. Experiments with new Pt/Rh sample boats demonstrated reduced procedural blanks, and analyses of well-characterized intercomparison materials tested the effects of process variables on 14C yields.
Alexandria J. Koester and Nathaniel A. Lifton
Geochronology, 5, 21–33, https://doi.org/10.5194/gchron-5-21-2023, https://doi.org/10.5194/gchron-5-21-2023, 2023
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In situ 14C’s short half-life (5.7 kyr) is unique among cosmogenic nuclides, making it sensitive to complex exposure and burial histories since 25 ka. Current extraction methods focus on quartz, but the ability to extract it from other minerals would expand applications. We developed MATLAB® scripts to calculate in situ 14C production rates from a broad range of mineral compositions. Results confirm O, Si, Al, and Mg as key targets but also find significant production from Na for the first time.
Aaron M. Barth, Elizabeth G. Ceperley, Claire Vavrus, Shaun A. Marcott, Jeremy D. Shakun, and Marc W. Caffee
Geochronology, 4, 731–743, https://doi.org/10.5194/gchron-4-731-2022, https://doi.org/10.5194/gchron-4-731-2022, 2022
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Deposits left behind by past glacial activity provide insight into the previous size and behavior of glaciers and act as another line of evidence for past climate. Here we present new age control for glacial deposits in the mountains of Montana and Wyoming, United States. While some deposits indicate glacial activity within the last 2000 years, others are shown to be older than previously thought, thus redefining the extent of regional Holocene glaciation.
Nathan Vandermaelen, Koen Beerten, François Clapuyt, Marcus Christl, and Veerle Vanacker
Geochronology, 4, 713–730, https://doi.org/10.5194/gchron-4-713-2022, https://doi.org/10.5194/gchron-4-713-2022, 2022
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We constrained deposition phases of fluvial sediments (NE Belgium) over the last 1 Myr with analysis and modelling of rare isotopes accumulation within sediments, occurring as a function of time and inverse function of depth. They allowed the determination of three superposed deposition phases and intercalated non-deposition periods of ~ 40 kyr each. These phases correspond to 20 % of the sediment age, which highlights the importance of considering deposition phase when dating fluvial sediments.
Felix Martin Hofmann
Geochronology, 4, 691–712, https://doi.org/10.5194/gchron-4-691-2022, https://doi.org/10.5194/gchron-4-691-2022, 2022
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If topographical obstructions are present in the surroundings of sampling sites, exposure ages of rock surfaces need to be corrected. A toolbox for the ESRI ArcGIS software allows for quantifying topographic shielding with a digital elevation model, but it has only been validated with few field data. In this study, the output of the toolbox is evaluated with a more extensive dataset. If suitable elevation data are chosen, the toolbox provides a sound approach to determine topographic shielding.
Yiran Wang and Michael E. Oskin
Geochronology, 4, 533–549, https://doi.org/10.5194/gchron-4-533-2022, https://doi.org/10.5194/gchron-4-533-2022, 2022
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When first introduced together with the depth profile technique to determine the surface exposure age, the linear inversion approach has suffered with the drawbacks of not incorporating erosion and muons into calculation. In this paper, we increase the accuracy and applicability of the linear inversion approach by fully considering surface erosion, muogenic production, and radioactive decay, while maintaining its advantage of being straightforward to determine an exposure age.
Richard F. Ott, Sean F. Gallen, and Darryl E. Granger
Geochronology, 4, 455–470, https://doi.org/10.5194/gchron-4-455-2022, https://doi.org/10.5194/gchron-4-455-2022, 2022
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Cosmogenic nuclides are a tool to quantify denudation – the total removal of mass from near the Earth's surface. Chemical weathering can introduce biases to cosmogenic-nuclide-based denudation rates measurements. Here, we investigate the effects of weathering on cosmogenic nuclides and develop tools to correct for this influence. Our results highlight which additional measurements are required to determine accurate denudation rates in regions where weathering is not negligible.
Mae Kate Campbell, Paul R. Bierman, Amanda H. Schmidt, Rita Sibello Hernández, Alejandro García-Moya, Lee B. Corbett, Alan J. Hidy, Héctor Cartas Águila, Aniel Guillén Arruebarrena, Greg Balco, David Dethier, and Marc Caffee
Geochronology, 4, 435–453, https://doi.org/10.5194/gchron-4-435-2022, https://doi.org/10.5194/gchron-4-435-2022, 2022
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We used cosmogenic radionuclides in detrital river sediment to measure erosion rates of watersheds in central Cuba; erosion rates are lower than rock dissolution rates in lowland watersheds. Data from two different cosmogenic nuclides suggest that some basins may have a mixed layer deeper than is typically modeled and could have experienced significant burial after or during exposure. We conclude that significant mass loss may occur at depth through chemical weathering processes.
Klaus M. Wilcken, Alexandru T. Codilean, Réka-H. Fülöp, Steven Kotevski, Anna H. Rood, Dylan H. Rood, Alexander J. Seal, and Krista Simon
Geochronology, 4, 339–352, https://doi.org/10.5194/gchron-4-339-2022, https://doi.org/10.5194/gchron-4-339-2022, 2022
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Cosmogenic nuclides are now widely applied in the Earth sciences; however, more recent applications often push the analytical limits of the technique. Our study presents a comprehensive method for analysis of cosmogenic 10Be and 26Al samples down to isotope concentrations of a few thousand atoms per gram of sample, which opens the door to new and more varied applications of cosmogenic nuclide analysis.
Brent M. Goehring, Brian Menounos, Gerald Osborn, Adam Hawkins, and Brent Ward
Geochronology, 4, 311–322, https://doi.org/10.5194/gchron-4-311-2022, https://doi.org/10.5194/gchron-4-311-2022, 2022
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We explored surface exposure dating with two nuclides to date two sets of moraines from the Yukon Territory and explain the reasoning for the observed ages. Results suggest multiple processes, including preservation of nuclides from a prior exposure period, and later erosion of the moraines is required to explain the data. Our results only allow for the older moraines to date to Marine Isotope Stage 3 or 4 and the younger moraines to date to the very earliest Holocene.
Caleb K. Walcott, Jason P. Briner, James F. Baichtal, Alia J. Lesnek, and Joseph M. Licciardi
Geochronology, 4, 191–211, https://doi.org/10.5194/gchron-4-191-2022, https://doi.org/10.5194/gchron-4-191-2022, 2022
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We present a record of ice retreat from the northern Alexander Archipelago, Alaska. During the last ice age (~ 26 000–19 000 years ago), these islands were covered by the Cordilleran Ice Sheet. We tested whether islands were ice-free during the last ice age for human migrants moving from Asia to the Americas. We found that these islands became ice-free between ~ 15 100 years ago and ~ 16 000 years ago, and thus these islands were not suitable for human habitation during the last ice age.
Tibor János Dunai, Steven Andrew Binnie, and Axel Gerdes
Geochronology, 4, 65–85, https://doi.org/10.5194/gchron-4-65-2022, https://doi.org/10.5194/gchron-4-65-2022, 2022
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We develop in situ-produced terrestrial cosmogenic krypton as a new tool to date and quantify Earth surface processes, the motivation being the availability of six stable isotopes and one radioactive isotope (81Kr, half-life 229 kyr) and of an extremely weathering-resistant target mineral (zircon). We provide proof of principle that terrestrial Krit can be quantified and used to unravel Earth surface processes.
Andrew J. Christ, Paul R. Bierman, Jennifer L. Lamp, Joerg M. Schaefer, and Gisela Winckler
Geochronology, 3, 505–523, https://doi.org/10.5194/gchron-3-505-2021, https://doi.org/10.5194/gchron-3-505-2021, 2021
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Cosmogenic nuclide surface exposure dating is commonly used to constrain the timing of past glacier extents. However, Antarctic exposure age datasets are often scattered and difficult to interpret. We compile new and existing exposure ages of a glacial deposit with independently known age constraints and identify surface processes that increase or reduce the likelihood of exposure age scatter. Then we present new data for a previously unmapped and undated older deposit from the same region.
Benedikt Ritter, Andreas Vogt, and Tibor J. Dunai
Geochronology, 3, 421–431, https://doi.org/10.5194/gchron-3-421-2021, https://doi.org/10.5194/gchron-3-421-2021, 2021
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We describe the design and performance of a new noble gas mass laboratory dedicated to the development of and application to cosmogenic nuclides at the University of Cologne (Germany). At the core of the laboratory are a state-of-the-art high-mass-resolution multicollector Helix MCPlus (Thermo-Fisher) noble gas mass spectrometer and a novel custom-designed automated extraction line, including a laser-powered extraction furnace. Performance was tested with intercomparison (CREU-1) material.
Florian Hofmann, Emily H. G. Cooperdock, A. Joshua West, Dominic Hildebrandt, Kathrin Strößner, and Kenneth A. Farley
Geochronology, 3, 395–414, https://doi.org/10.5194/gchron-3-395-2021, https://doi.org/10.5194/gchron-3-395-2021, 2021
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We use microCT scanning to improve the quality of 3He exposure ages measured in detrital magnetite. We show that the presence of inclusions can significantly increase the measured amount of 3He and thereby the exposure age. By prescreening magnetite with microCT and analyzing only inclusion-free grains, this problem can be avoided. We also calibrate the cosmogenic 3He production rate in magnetite relative to 10Be in quartz, which can be used for similar studies in the future.
Travis Clow, Jane K. Willenbring, Mirjam Schaller, Joel D. Blum, Marcus Christl, Peter W. Kubik, and Friedhelm von Blanckenburg
Geochronology, 2, 411–423, https://doi.org/10.5194/gchron-2-411-2020, https://doi.org/10.5194/gchron-2-411-2020, 2020
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Meteoric beryllium-10 concentrations in soil profiles have great capacity to quantify Earth surface processes, such as erosion rates and landform ages. However, determining these requires an accurate estimate of the delivery rate of this isotope to local sites. Here, we present a new method to constrain the long-term delivery rate to an eroding western US site, compare it against existing delivery rate estimates (revealing considerable disagreement between methods), and suggest best practices.
Joseph P. Tulenko, William Caffee, Avriel D. Schweinsberg, Jason P. Briner, and Eric M. Leonard
Geochronology, 2, 245–255, https://doi.org/10.5194/gchron-2-245-2020, https://doi.org/10.5194/gchron-2-245-2020, 2020
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We investigate the timing and rate of retreat for three alpine glaciers in the southern Rocky Mountains to test whether they followed the pattern of global climate change or were majorly influenced by regional forcing mechanisms. We find that the latter is most likely for these glaciers. Our conclusions are based on a new 10Be chronology of alpine glacier retreat. We quantify retreat rates for each valley using the BACON program in R, which may be of interest for the audience of Geochronology.
Greg Balco
Geochronology, 2, 169–175, https://doi.org/10.5194/gchron-2-169-2020, https://doi.org/10.5194/gchron-2-169-2020, 2020
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Geologic dating methods generally do not directly measure ages. Instead, interpreting a geochemical measurement as an age requires a middle layer of calculations and supporting data, and the fact that this layer continually improves is an obstacle to synoptic analysis of geochronological data. This paper describes a prototype data management and analysis system that addresses this obstacle by making the middle-layer calculations transparent and dynamic to the user.
Keir A. Nichols and Brent M. Goehring
Geochronology, 1, 43–52, https://doi.org/10.5194/gchron-1-43-2019, https://doi.org/10.5194/gchron-1-43-2019, 2019
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We describe observations of anomalously high measurements of C-14 made from geologic material. We undertake a systematic investigation to identify the source of contamination, which we hypothesise is sourced from a commonly used method that is used prior to sample analysis. We find that the method does introduce modern carbon to samples and elevates C-14 measurements. We describe a standard procedure that effectively removes contamination from the aforementioned method.
Greg Balco, Kimberly Blisniuk, and Alan Hidy
Geochronology, 1, 1–16, https://doi.org/10.5194/gchron-1-1-2019, https://doi.org/10.5194/gchron-1-1-2019, 2019
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This article applies a new geochemical dating method to determine the age of sedimentary deposits useful in reconstructing slip rates on a major fault system.
Cited articles
Ackert, R. P.: Antarctic glacial chronology: new constraints from surface
exposure dating, Doctoral thesis, Massachusetts Institute of Technology and Woods Hole Oceanographic Institution, Woods Hole Open Access Server, https://doi.org/10.1575/1912/4123, 2000.
Ackert, R. P. and Kurz, M. D.: Age and uplift rates of Sirius Group
sediments in the Dominion Range, Antarctica, from surface exposure dating
and geomorphology, Global Planet. Change, 42, 207–225,
https://doi.org/10.1016/j.gloplacha.2004.02.001, 2004.
Andrews, J. N. and Kay, R. L. F.: Natural production of tritium in permeable
rocks, Nature, 298, 361–363, https://doi.org/10.1038/298361a0, 1982.
Argento, D. C., Stone, J. O., Reedy, R. C., and O'Brien, K.: Physics-based
modeling of cosmogenic nuclides part II – Key aspects of in-situ cosmogenic
nuclide production, Quat Geochronol, 26, 44–55,
https://doi.org/10.1016/j.quageo.2014.09.005, 2015.
Balco, G.: Production rate calculations for cosmic-ray-muon-produced 10Be
and 26Al benchmarked against geological calibration data, Quat. Geochronol.,
39, 150–173, https://doi.org/10.1016/j.quageo.2017.02.001, 2017.
Balco, G.: Noncosmogenic helium-3 in pyroxene and Antarctic exposure dating:
https://cosmognosis.wordpress.com/2020/08/22/noncosmogenic-helium-3-in-pyroxene-and-antarctic-exposure-dating/,
last access: 23 June 2022, 2020.
Balco, G. and Shuster, D. L.: 26Al–10Be–21Ne burial dating, Earth Planet. Sc. Lett., 286, 570–575, https://doi.org/10.1016/j.epsl.2009.07.025, 2009.
Balco, G. and Rovey, C. W.: Absolute chronology for major Pleistocene
advances of the Laurentide Ice Sheet, Geology, 38, 795–798,
https://doi.org/10.1130/g30946.1, 2010.
Balco, G., Stone, J. O., Lifton, N. A., and Dunai, T. J.: A complete and
easily accessible means of calculating surface exposure ages or erosion
rates from 10Be and 26Al measurements, Quat. Geochronol., 3, 174–195,
https://doi.org/10.1016/j.quageo.2007.12.001, 2008.
Balco, G., Blard, P.-H., Shuster, D. L., Stone, J. O. H., and Zimmermann,
L.: Cosmogenic and nucleogenic 21Ne in quartz in a 28-meter sandstone core
from the McMurdo Dry Valleys, Antarctica, Quat. Geochronol., 52, 63–76,
https://doi.org/10.1016/j.quageo.2019.02.006, 2019.
Balter-Kennedy, A. and Balco, G.: Code supporting Cosmogenic 10Be in pyroxene: laboratory progress, production rate systematics, and application of the 10Be–3He nuclide pair in the Antarctic Dry Valleys, Zenodo [code], https://doi.org/10.5281/zenodo.8125448, 2023.
Balter-Kennedy, A., Bromley, G., Balco, G., Thomas, H., and Jackson, M. S.: A 14.5-million-year record of East Antarctic Ice Sheet fluctuations from the central Transantarctic Mountains, constrained with cosmogenic 3Be, 10Be,
21Ne, and 26Al, The Cryosphere, 14, 2647–2672, https://doi.org/10.5194/tc-14-2647-2020, 2020.
Bindschadler, R., Vornberger, P., Fleming, A., Fox, A., Mullins, J., Binnie,
D., Paulsen, S. J., Granneman, B., and Gorodetzky, D.: The Landsat Image
Mosaic of Antarctica, Remote Sens Environ, 112, 4214–4226,
https://doi.org/10.1016/j.rse.2008.07.006, 2008.
Blard, P.-H.: Cosmogenic 3He in terrestrial rocks: A review, Chem. Geol., 586,
120543, https://doi.org/10.1016/j.chemgeo.2021.120543, 2021.
Blard, P.-H., Pik, R., Lavé, J., Bourlès, D., Burnard, P. G.,
Yokochi, R., Marty, B., and Trusdell, F.: Cosmogenic 3He production rates
revisited from evidences of grain size dependent release of matrix-sited
helium, Earth Planet. Sc. Lett., 247, 222–234,
https://doi.org/10.1016/j.epsl.2006.05.012, 2006.
Blard, P.-H., Bourlès, D., Pik, R., and Lavé, J.: In situ cosmogenic
10Be in olivines and pyroxenes, Quat. Geochronol., 3, 196–205,
https://doi.org/10.1016/j.quageo.2007.11.006, 2008.
Blard, P.-H., Balco, G., Burnard, P. G., Farley, K. A., Fenton, C. R.,
Friedrich, R., Jull, A. J. T., Niedermann, S., Pik, R., Schaefer, J. M.,
Scott, E. M., Shuster, D. L., Stuart, F. M., Stute, M., Tibari, B.,
Winckler, G., and Zimmermann, L.: An inter-laboratory comparison of
cosmogenic 3He and radiogenic 4He in the CRONUS-P pyroxene standard, Quat.
Geochronol., 26, 11–19, https://doi.org/10.1016/j.quageo.2014.08.004, 2015.
Borchers, B., Marrero, S., Balco, G., Caffee, M., Goehring, B., Lifton, N.,
Nishiizumi, K., Phillips, F., Schaefer, J., and Stone, J.: Geological
calibration of spallation production rates in the CRONUS-Earth project, Quat.
Geochronol., 31, 188–198, https://doi.org/10.1016/j.quageo.2015.01.009,
2016.
Bromley, G. R. M., Hall, B. L., Schaefer, J. M., Winckler, G., Todd, C. E.,
and Rademaker, K. M.: Glacier fluctuations in the southern Peruvian Andes
during the late-glacial period, constrained with cosmogenic 3He, J.
Quat. Sci., 26, 37–43, https://doi.org/10.1002/jqs.1424, 2011.
Bromley, G. R. M., Winckler, G., Schaefer, J. M., Kaplan, M. R., Licht, K.
J., and Hall, B. L.: Pyroxene separation by HF leaching and its impact on
helium surface-exposure dating, Quat. Geochronol., 23, 1–8,
https://doi.org/10.1016/j.quageo.2014.04.003, 2014.
Brown, E. T., Edmond, J. M., Raisbeck, G. M., Yiou, F., Kurz, M. D., and
Brook, E. J.: Examination of surface exposure ages of Antarctic moraines
using in situ produced 10Be and 26Al, Geochim. Cosmochim. Ac., 55, 2269–2283,
https://doi.org/10.1016/0016-7037(91)90103-c, 1991.
Brown, E. T., Brook, E. J., Raisbeck, G. M., Yiou, F., and Kurz, M. D.:
Effective attenuation lengths of cosmic rays producing 10Be and 26Al in
quartz: Implications for exposure age dating, Geophys. Res. Lett., 19,
369–372, https://doi.org/10.1029/92gl00266, 1992.
Bruno, L. A., Baur, H., Graf, T., Schlüchter, C., Signer,
P., and Wieler, R.: Dating of Sirius Group tillites in the Antarctic Dry
Valleys with cosmogenic 3He and 21Ne, Earth Planet. Sc. Lett., 147, 37–54,
https://doi.org/10.1016/s0012-821x(97)00003-4, 1997.
Burgess, S. D., Bowring, S. A., Fleming, T. H., and Elliot, D. H.:
High-precision geochronology links the Ferrar large igneous province with
early-Jurassic ocean anoxia and biotic crisis, Earth Planet. Sc. Lett., 415,
90–99, https://doi.org/10.1016/j.epsl.2015.01.037, 2015.
Cerling, T. E.: Dating geomorphologic surfaces using cosmogenic 3He,
Quat. Res., 33, 148–156, https://doi.org/10.1016/0033-5894(90)90015-d,
1990.
Cerling, T. E.: Geomorphology and In-Situ Cosmogenic Isotopes, Annu. Rev. Earth Pl. Sc., 22, 273–317, https://doi.org/10.1146/annurev.earth.22.1.273, 1994.
Chmeleff, J., Blanckenburg, F. von, Kossert, K., and Jakob, D.:
Determination of the 10Be half-life by multicollector ICP-MS and liquid
scintillation counting, Nucl. Instruments Methods Phys. Res. Sect B., 268, 192–199,
https://doi.org/10.1016/j.nimb.2009.09.012, 2010.
Denton, G. H. and Sugden, D. E.: Meltwater features that suggest Miocene
ice-sheet overriding of the Transantarctic Mountains in Victoria Land,
Antarctica, Geogr. Ann, Ser. Phys. Geogr., 87, 67–85,
https://doi.org/10.1111/j.0435-3676.2005.00245.x, 2005.
Denton, G. H., Sugden, D. E., Marchant, D. R., Hall, B. L., and Wilch, T.
I.: East Antarctic Ice Sheet Sensitivity to Pliocene Climatic Change from a
Dry Valleys Perspective, Geogr. Ann, Ser. Phys. Geogr., 75, 155–204,
https://doi.org/10.2307/521200, 1993.
Dunai, T. J.: Cosmogenic Nuclides, https://doi.org/10.1017/cbo9780511804519,
2010.
Eaves, S. R., Collins, J. A., Jones, R. S., Norton, K. P., Tims, S. G., and
Mackintosh, A. N.: Further constraint of the in situ cosmogenic 10Be
production rate in pyroxene and a viability test for late Quaternary
exposure dating, Quat. Geochronol., 48, 121–132,
https://doi.org/10.1016/j.quageo.2018.09.006, 2018.
Egidy, T. and von and Hartmann, F. J.: Average muonic Coulomb capture
probabilities for 65 elements, Phys. Rev. A, 26, 2355–2360,
https://doi.org/10.1103/physreva.26.2355, 1982.
Fink, D. and Smith, A.: An inter-comparison of 10Be and 26Al AMS reference
standards and the 10Be half-life, Nucl. Instruments Methods Phys. Res. Sect B., 259, 600–609,
https://doi.org/10.1016/j.nimb.2007.01.299, 2007.
Gayer, E., Pik, R., Lavé, J., France-Lanord, C., Bourlès, D., and
Marty, B.: Cosmogenic 3He in Himalayan garnets indicating an altitude
dependence of the 3He
Goehring, B. M., Kurz, M. D., Balco, G., Schaefer, J. M., Licciardi, J., and
Lifton, N.: A reevaluation of in situ cosmogenic 3He production rates, Quat.
Geochronol., 5, 410–418, https://doi.org/10.1016/j.quageo.2010.03.001, 2010.
Gosse, J. C. and Phillips, F. M.: Terrestrial in situ cosmogenic nuclides:
theory and application, Quat. Sci. Rev., 20, 1475–1560,
https://doi.org/10.1016/s0277-3791(00)00171-2, 2001.
Granger, D. E.: A review of burial dating methods using 26Al and 10Be, in:
In Situ-Produced Cosmogenic Nuclides and Quantification of Geological
Processes: Geological Society of America Special Paper 415, edited by:
Siame, L. L., Bourlès, D. L., and Brown, 1–16,
https://doi.org/10.1130/2006.2415(01), 2006.
Heisinger, B., Lal, D., Jull, A. J. T., Kubik, P., Ivy-Ochs, S., Neumaier,
S., Knie, K., Lazarev, V., and Nolte, E.: Production of selected cosmogenic
radionuclides by muons 1. Fast muons, Earth Planet. Sc. Lett., 200, 345–355,
https://doi.org/10.1016/s0012-821x(02)00640-4, 2002a.
Heisinger, B., Lal, D., Jull, A. J. T., Kubik, P., Ivy-Ochs, S., Knie, K.,
and Nolte, E.: Production of selected cosmogenic radionuclides by muons: 2.
Capture of negative muons, Earth Planet. Sc. Lett., 200, 357–369,
https://doi.org/10.1016/s0012-821x(02)00641-6, 2002b.
Hippe, K.: Constraining processes of landscape change with combined in situ
cosmogenic 14C-10Be analysis, Quat. Sci. Rev., 173, 1–19,
https://doi.org/10.1016/j.quascirev.2017.07.020, 2017.
Ivy-Ochs, S., Kubik, P. W., Masarik, J., Wieler, R., Bruno, L., and
Schlüchter, C.: Preliminary results on the use of pyroxene for 10Be
surface exposure dating, Schweiz, Mineral. Petrogr. Mitt., 78, 375–382, 1998.
Ivy-Ochs, S., Schlüchter, C., Kubik, P. W.,
Dittrich-Hannen, B., and Beer, J.: Minimum 10Be exposure ages of early
Pliocene for the Table Mountain plateau and the Sirius Group at Mount
Fleming, Dry Valleys, Antarctica, Geology, 23, 1007–1010,
https://doi.org/10.1130/0091-7613(1995)023<1007:mbeaoe>2.3.co;2, 1995.
Kaplan, M. R., Licht, K. J., Winckler, G., Schaefer, J. M., Bader, N.,
Mathieson, C., Roberts, M., Kassab, C. M., Schwartz, R., and Graly, J. A.:
Middle to Late Pleistocene stability of the central East Antarctic Ice Sheet
at the head of Law Glacier, Geology, 45, 963–966,
https://doi.org/10.1130/g39189.1, 2017.
Kohl, C. P. and Nishiizumi, K.: Chemical isolation of quartz for measurement
of in-situ -produced cosmogenic nuclides, Geochim. Cosmochim. Ac., 56,
3583–3587, https://doi.org/10.1016/0016-7037(92)90401-4, 1992.
Kurz, M. D.: Cosmogenic helium in a terrestrial igneous rock, Nature, 320,
435–439, https://doi.org/10.1038/320435a0, 1986.
Kurz, M. D. and Brook, E. J.: Surface exposure dating with cosmogenic
nuclides, in: Dating in exposed and surface contexts, 139–159, 1994.
Lal, D.: Production of 3He in terrestrial rocks, Chem Geology Isotope
Geosci. Sect., 66, 89–98, https://doi.org/10.1016/0168-9622(87)90031-5,
1987.
Lal, D.: Cosmic ray labeling of erosion surfaces: in situ nuclide production
rates and erosion models, Earth Planet. Sc. Lett., 104, 424–439,
https://doi.org/10.1016/0012-821x(91)90220-c, 1991.
Lamp, J. L., Marchant, D. R., Mackay, S. L., and Head, J. W.: Thermal stress
weathering and the spalling of Antarctic rocks, J. Geophys. Res.-Ea.,
122, 3–24, https://doi.org/10.1002/2016jf003992, 2017.
Larsen, I. J., Farley, K. A., Lamb, M. P., and Pritchard, C. J.: Empirical
evidence for cosmogenic 3He production by muons, Earth Planet. Sc. Lett., 562,
116825, https://doi.org/10.1016/j.epsl.2021.116825, 2021.
Lewis, A. R., Marchant, D. R., Kowalewski, D. E., Baldwin, S. L., and Webb,
L. E.: The age and origin of the Labyrinth, western Dry Valleys, Antarctica:
Evidence for extensive middle Miocene subglacial floods and freshwater
discharge to the Southern Ocean, Geology, 34, 513–516,
https://doi.org/10.1130/g22145.1, 2006.
Margerison, H. R., Phillips, W. M., Stuart, F. M., and Sugden, D. E.:
Cosmogenic 3He concentrations in ancient flood deposits from the Coombs
Hills, northern Dry Valleys, East Antarctica: interpreting exposure ages and
erosion rates, Earth Planet. Sc. Lett., 230, 163–175,
https://doi.org/10.1016/j.epsl.2004.11.007, 2005.
Matsuda, J., Matsumoto, T., Sumino, H., Nagao, K., Yamamoto, J., Miura, Y.,
Kaneoka, I., Takahata, N., and Sano, Y.: The 3He
Matsuoka, K., Skoglund, A., Roth, G., Pomereu, J. de, Griffiths, H.,
Headland, R., Herried, B., Katsumata, K., Brocq, A. L., Licht, K., Morgan,
F., Neff, P. D., Ritz, C., Scheinert, M., Tamura, T., Putte, A. V. de,
Broeke, M. van den, Deschwanden, A. von, Deschamps-Berger, C., Liefferinge,
B. V., Tronstad, S., and Melvær, Y.: Quantarctica, an integrated mapping
environment for Antarctica, the Southern Ocean, and sub-Antarctic islands,
Environ Model. Softw., 140, 105015,
https://doi.org/10.1016/j.envsoft.2021.105015, 2021.
McKelvey, B. C. and Webb, P. N.: Geological investigations in southern
Victoria Land, Antarctica, New Zeal J. Geol. Geop., 5, 143–162,
https://doi.org/10.1080/00288306.1962.10420116, 1962.
Middleton, J. L., Ackert, R. P., and Mukhopadhyay, S.: Pothole and channel
system formation in the McMurdo Dry Valleys of Antarctica: New insights from
cosmogenic nuclides, Earth Planet. Sc. Lett., 355, 341–350,
https://doi.org/10.1016/j.epsl.2012.08.017, 2012.
Nespolo, M.: Reference Module in Earth Systems and Environmental Sciences, Encyclopedia of Geology, 2nd Edn.,
287–296, https://doi.org/10.1016/b978-0-12-409548-9.12409-1, 2020.
Nesterenok, A. V. and Yakubovich, O. V.: Production of
3He in Rocks by Reactions Induced by Particles of the Nuclear-Active and
Muon Components of Cosmic Rays: Geological and Petrological Implications,
Arxiv, https://doi.org/10.48550/arxiv.1607.08770, 2016.
Niedermann, S., Schaefer, J. M., Wieler, R., and Naumann, R.: The production
rate of cosmogenic 38Ar from calcium in terrestrial pyroxene, Earth Planet. Sc. Lett., 257, 596–608, https://doi.org/10.1016/j.epsl.2007.03.020, 2007.
Nishiizumi, K., Imamura, M., Caffee, M. W., Southon, J. R., Finkel, R. C.,
and McAninch, J.: Absolute calibration of 10Be AMS standards, Nucl.
Instruments Methods Phys. Res. Sect. B., 258,
403–413, https://doi.org/10.1016/j.nimb.2007.01.297, 2007.
Nishiizumi, K., Klein, J., Middleton, R., and Craig, H.:
Cosmogenic10Be, 26Al, and 3He in olivine from Maui lavas, Earth Planet. Sc. Lett., 98, 263–266, https://doi.org/10.1016/0012-821x(90)90028-v, 1990.
Nishiizumi, K., Kohl, C. P., Arnold, J. R., Klein, J., Fink, D., and
Middleton, R.: Cosmic ray produced 10Be and 26Al in Antarctic rocks:
exposure and erosion history, Earth Planet. Sc. Lett., 104, 440–454,
https://doi.org/10.1016/0012-821x(91)90221-3, 1991.
Ochs, M. and Ivy-Ochs, S.: The chemical behavior of Be, Al, Fe, Ca and Mg
during AMS target preparation from terrestrial silicates modeled with
chemical speciation calculations, Nucl. Instruments Methods Phys. Res. Sect. B., 123, 235–240,
https://doi.org/10.1016/s0168-583x(96)00680-5, 1997.
Schäfer, J. M., Ivy-Ochs, S., Wieler, R., Leya, I., Baur, H., Denton, G.
H., and Schlüchter, C.: Cosmogenic noble gas studies in the oldest
landscape on earth: surface exposure ages of the Dry Valleys, Antarctica,
Earth Planet. Sc. Lett., 167, 215–226,
https://doi.org/10.1016/s0012-821x(99)00029-1, 1999.
Schaefer, J. M., Faestermann, T., Herzog, G. F., Knie, K., Korschinek, G.,
Masarik, J., Meier, A., Poutivtsev, M., Rugel, G., Schlüchter, C.,
Serifiddin, F., and Winckler, G.: Terrestrial manganese-53 – A new monitor
of Earth surface processes, Earth Planet. Sc. Lett., 251, 334–345,
https://doi.org/10.1016/j.epsl.2006.09.016, 2006.
Schaefer, J. M., Denton, G. H., Kaplan, M., Putnam, A., Finkel, R. C.,
Barrell, D. J. A., Andersen, B. G., Schwartz, R., Mackintosh, A., Chinn, T.,
and Schlüchter, C.: High-Frequency Holocene Glacier Fluctuations in New
Zealand Differ from the Northern Signature, Science, 324, 622–625,
https://doi.org/10.1126/science.1169312, 2009.
Schaefer, J. M., Finkel, R. C., Balco, G., Alley, R. B., Caffee, M. W.,
Briner, J. P., Young, N. E., Gow, A. J., and Schwartz, R.: Greenland was
nearly ice-free for extended periods during the Pleistocene, Nature, 540,
252–255, https://doi.org/10.1038/nature20146, 2016a.
Schaefer, J. M., Winckler, G., Blard, P.-H., Balco, G., Shuster, D. L.,
Friedrich, R., Jull, A. J. T., Wieler, R., and Schluechter, C.: Performance
of CRONUS-P – A pyroxene reference material for helium isotope analysis,
Quat. Geochronol., 31, 237–239, https://doi.org/10.1016/j.quageo.2014.07.006,
2016b.
Schaefer, J. M., Codilean, A. T., Willenbring, J. K., Lu, Z.-T., Keisling,
B., Fülöp, R.-H., and Val, P.: Cosmogenic nuclide techniques, Nat.
Rev. Meth. Prim., 2, 18, https://doi.org/10.1038/s43586-022-00096-9,
2022.
Stone, J. O.: Air pressure and cosmogenic isotope production, J. Geophys. Res.
Sol.-Ea., 105, 23753–23759, https://doi.org/10.1029/2000jb900181, 2000.
Sugden, D. E., Marchant, D. R., Potter, N., Souchez, R. A., Denton, G. H.,
III, C. C. S., and Tison, J.-L.: Preservation of Miocene glacier ice in East
Antarctica, Nature, 376, 412–414, https://doi.org/10.1038/376412a0, 1995.
Summerfield, M. A., Stuart, F. M., Cockburn, H. A. P., Sugden, D. E.,
Denton, G. H., Dunai, T., and Marchant, D. R.: Long-term rates of denudation
in the Dry Valleys, Transantarctic Mountains, southern Victoria Land,
Antarctica based on in-situ-produced cosmogenic 21Ne, Geomorphology, 27,
113–129, https://doi.org/10.1016/s0169-555x(98)00093-2, 1999.
Young, N. E., Lesnek, A. J., Cuzzone, J. K., Briner, J. P., Badgeley, J. A., Balter-Kennedy, A., Graham, B. L., Cluett, A., Lamp, J. L., Schwartz, R., Tuna, T., Bard, E., Caffee, M. W., Zimmerman, S. R. H., and Schaefer, J. M.: In situ cosmogenic 10Be–14C–26Al measurements from recently deglaciated bedrock as a new tool to decipher changes in Greenland Ice Sheet size, Clim. Past, 17, 419–450, https://doi.org/10.5194/cp-17-419-2021, 2021.
Zavala, K., Leitch, A. M., and Fisher, G. W.: Silicic Segregations of the
Ferrar Dolerite Sills, Antarctica, J. Petrol., 52, 1927–1964,
https://doi.org/10.1093/petrology/egr035, 2011.
Zimmermann, L., Avice, G., Blard, P.-H., Marty, B., Füri, E., and
Burnard, P. G.: A new all-metal induction furnace for noble gas extraction,
Chem. Geol., 480, 86–92, https://doi.org/10.1016/j.chemgeo.2017.09.018, 2018.
Short summary
Cosmogenic nuclides like 10Be are rare isotopes created in rocks exposed at the Earth’s surface and can be used to understand glacier histories and landscape evolution. 10Be is usually measured in the mineral quartz. Here, we show that 10Be can be reliably measured in the mineral pyroxene. We use the measurements to determine exposure ages and understand landscape processes in rocks from Antarctica that do not have quartz, expanding the use of this method to new rock types.
Cosmogenic nuclides like 10Be are rare isotopes created in rocks exposed at the Earth’s...
