Articles | Volume 6, issue 3
https://doi.org/10.5194/gchron-6-365-2024
© Author(s) 2024. 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-6-365-2024
© Author(s) 2024. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Jul 2024
Research article |
| 10 Jul 2024
| 10 Jul 2024
Cosmogenic 3He chronology of postglacial lava flows at Mt Ruapehu, Aotearoa / New Zealand
Pedro Doll
CORRESPONDING AUTHOR
School of Earth and Environment, University of Canterbury, Private Bag 4800, Ōtautahi / Christchurch 8041, New Zealand
Shaun Robert Eaves
Antarctic Research Centre, Victoria University of Wellington, P.O.Box 600, Te Whanganui-a-Tara / Wellington 6140, New Zealand
School of Geography, Environment and Earth Sciences, Victoria University of Wellington, P.O. Box 600, Te Whanganui-a-Tara / Wellington 6140, New Zealand
Ben Matthew Kennedy
School of Earth and Environment, University of Canterbury, Private Bag 4800, Ōtautahi / Christchurch 8041, New Zealand
Pierre-Henri Blard
CRPG, CNRS, Université de Lorraine, 15 Rue Notre Dame des Pauvres, Vandoeuvre-les Nancy 54000, France
Alexander Robert Lee Nichols
School of Earth and Environment, University of Canterbury, Private Bag 4800, Ōtautahi / Christchurch 8041, New Zealand
Graham Sloan Leonard
GNS Science, 1 Fairway Drive, Avalon, Te Awa Kairangi ki Tai / Lower Hutt 5011, New Zealand
Dougal Bruce Townsend
GNS Science, 1 Fairway Drive, Avalon, Te Awa Kairangi ki Tai / Lower Hutt 5011, New Zealand
Jim William Cole
School of Earth and Environment, University of Canterbury, Private Bag 4800, Ōtautahi / Christchurch 8041, New Zealand
Chris Edward Conway
Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology (AIST), 1-1-1 Higashi, Tsukuba, Ibaraki 305-8567, Japan
Sacha Baldwin
School of Earth and Environment, University of Canterbury, Private Bag 4800, Ōtautahi / Christchurch 8041, New Zealand
Gabriel Fénisse
CRPG, CNRS, Université de Lorraine, 15 Rue Notre Dame des Pauvres, Vandoeuvre-les Nancy 54000, France
Laurent Zimmermann
CRPG, CNRS, Université de Lorraine, 15 Rue Notre Dame des Pauvres, Vandoeuvre-les Nancy 54000, France
Bouchaïb Tibari
CRPG, CNRS, Université de Lorraine, 15 Rue Notre Dame des Pauvres, Vandoeuvre-les Nancy 54000, France
Related authors
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Cécile Massiot, Ludmila Adam, Eric S. Boyd, S. Craig Cary, Daniel R. Colman, Alysia Cox, Ery Hughes, Geoff Kilgour, Matteo Lelli, Domenico Liotta, Karen G. Lloyd, Tiipene Marr, David D. McNamara, Sarah D. Milicich, Craig A. Miller, Santanu Misra, Alexander R. L. Nichols, Simona Pierdominici, Shane M. Rooyakkers, Douglas R. Schmitt, Andri Stefansson, John Stix, Matthew B. Stott, Camille Thomas, Pilar Villamor, Pujun Wang, Sadiq J. Zarrouk, and the CALDERA workshop participants
Sci. Dril., 33, 67–88, https://doi.org/10.5194/sd-33-67-2024, https://doi.org/10.5194/sd-33-67-2024, 2024
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Volcanoes where tectonic plates drift apart pose eruption and earthquake hazards. Underground waters are difficult to track. Underground microbial life is probably plentiful but unexplored. Scientists discussed the idea of drilling two boreholes in the Okataina Volcanic Centre, New Zealand, to unravel the connections between volcano, faults, geotherms, and the biosphere, also integrating mātauranga Māori (Indigenous knowledge) to assess hazards and manage resources and microbial ecosystems.
Paul R. Bierman, Andrew J. Christ, Catherine M. Collins, Halley M. Mastro, Juliana Souza, Pierre-Henri Blard, Stefanie Brachfeld, Zoe R. Courville, Tammy M. Rittenour, Elizabeth K. Thomas, Jean-Louis Tison, and Francois Fripiat
EGUsphere, https://doi.org/10.5194/egusphere-2023-2922, https://doi.org/10.5194/egusphere-2023-2922, 2024
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In 1966, the US Army drilled through the Greenland Ice Sheet at Camp Century, Greenland; they recovered 3.44 meters of frozen sediment. Here, we decipher the material’s history. Water, flowing during a warm interglacial when the ice sheet melted from northwest Greenland, deposited the upper material which contains fossil plant and insect parts. The lower material, separated by more than a meter of ice with some sediment, is till, deposited by the ice sheet during a prior cold period.
Allie Balter-Kennedy, Joerg M. Schaefer, Roseanne Schwartz, Jennifer L. Lamp, Laura Penrose, Jennifer Middleton, Jean Hanley, Bouchaïb Tibari, Pierre-Henri Blard, Gisela Winckler, Alan J. Hidy, and Greg Balco
Geochronology, 5, 301–321, https://doi.org/10.5194/gchron-5-301-2023, https://doi.org/10.5194/gchron-5-301-2023, 2023
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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.
Matthew W. Hayward, Emily M. Lane, Colin N. Whittaker, Graham S. Leonard, and William L. Power
Nat. Hazards Earth Syst. Sci., 23, 955–971, https://doi.org/10.5194/nhess-23-955-2023, https://doi.org/10.5194/nhess-23-955-2023, 2023
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In this paper, 20 explosive volcanic eruption scenarios of differing location and magnitude are simulated to investigate tsunami generation in Lake Taupō, New Zealand. A non-hydrostatic multilayer numerical scheme resolves the highly dispersive generated wavefield. Inundation, hydrographic and related hazard outputs are produced, indicating that significant inundation around the lake shore begins above 5 on the volcanic explosivity index.
Agathe Defourny, Pierre-Henri Blard, Laurent Zimmermann, Patrick Jobé, Arnaud Collignon, Frédéric Nguyen, and Alain Dassargues
Hydrol. Earth Syst. Sci., 26, 2637–2648, https://doi.org/10.5194/hess-26-2637-2022, https://doi.org/10.5194/hess-26-2637-2022, 2022
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The Belgian city of Spa is known worldwide for its ferruginous and naturally sparkling groundwater springs that gave their name to the bathing tradition commonly called
spa. However, the origin of the dissolved CO2 they contain was still a matter of debate. Thanks to new analysis on groundwater samples, particularly carbon and helium isotopes together with dissolved gases, this study has demonstrated that the volcanic origin of the CO2 is presumably from the neighboring Eifel volcanic fields.
Richard N. Holdaway, Ben Kennedy, Brendan M Duffy, Jiandong Xu, and Clive Oppenheimer
Geochronology Discuss., https://doi.org/10.5194/gchron-2021-13, https://doi.org/10.5194/gchron-2021-13, 2021
Revised manuscript not accepted
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Prehistoric volcanic eruptions are often dated by wiggle matching series of radiocarbon ages on tree rings to standard calibration curves, ignoring potential contamination by 'old' carbon given off by the volcano. We modeled the effects of low amounts of contamination on wiggle match dates for the 10th century Changbaishan eruption and found evidence of contamination in all. We propose a new protocol to identify the presence of contamination, and provide more secure dates for major eruptions.
Jackie E. Kendrick, Lauren N. Schaefer, Jenny Schauroth, Andrew F. Bell, Oliver D. Lamb, Anthony Lamur, Takahiro Miwa, Rebecca Coats, Yan Lavallée, and Ben M. Kennedy
Solid Earth, 12, 633–664, https://doi.org/10.5194/se-12-633-2021, https://doi.org/10.5194/se-12-633-2021, 2021
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The last lava dome eruption of Mount Unzen (Japan) ended in 1995, but ongoing instability means much of the area remains an exclusion zone. The rocks in the lava dome impact its stability; heterogeneity (contrasting properties) and anisotropy (orientation-specific properties) can channel fluids and localise deformation, enhancing the risk of lava dome collapse. We recommend using measured material properties to interpret geophysical signals and to model volcanic systems.
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.
U. Morgenstern, C. J. Daughney, G. Leonard, D. Gordon, F. M. Donath, and R. Reeves
Hydrol. Earth Syst. Sci., 19, 803–822, https://doi.org/10.5194/hess-19-803-2015, https://doi.org/10.5194/hess-19-803-2015, 2015
S. A. Fraser, N. J. Wood, D. M. Johnston, G. S. Leonard, P. D. Greening, and T. Rossetto
Nat. Hazards Earth Syst. Sci., 14, 2975–2991, https://doi.org/10.5194/nhess-14-2975-2014, https://doi.org/10.5194/nhess-14-2975-2014, 2014
Related subject area
Cosmogenic nuclide dating
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
Technical note: Optimizing the in situ cosmogenic 36Cl extraction and measurement workflow for geologic applications
Production rate calibration for cosmogenic 10Be in pyroxene by applying a rapid fusion method to 10Be-saturated samples from the Transantarctic Mountains, Antarctica
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
Cosmogenic 10Be in pyroxene: laboratory progress, production rate systematics, and application of the 10Be–3He nuclide pair in the Antarctic Dry Valleys
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
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.
Alia Lesnek, Joseph M. Licciardi, Alan J. Hidy, and Tyler S. Anderson
EGUsphere, https://doi.org/10.5194/egusphere-2024-713, https://doi.org/10.5194/egusphere-2024-713, 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.
Marie Bergelin, Greg Balco, Lee B. Corbett, and Paul R. Bierman
EGUsphere, https://doi.org/10.5194/egusphere-2024-702, https://doi.org/10.5194/egusphere-2024-702, 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.
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.
Allie Balter-Kennedy, Joerg M. Schaefer, Roseanne Schwartz, Jennifer L. Lamp, Laura Penrose, Jennifer Middleton, Jean Hanley, Bouchaïb Tibari, Pierre-Henri Blard, Gisela Winckler, Alan J. Hidy, and Greg Balco
Geochronology, 5, 301–321, https://doi.org/10.5194/gchron-5-301-2023, https://doi.org/10.5194/gchron-5-301-2023, 2023
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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.
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
Short summary
Short summary
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., Singer, B. S., Guillou, H., Kaplan, M. R., and Kurz, M. D.: Long-term cosmogenic 3He production rates from
Alcalá-Reygosa, J., Palacios, D., Schimmelpfennig, I., Vázquez-Selem, L., García-Sancho, L., Franco-Ramos, O., Villanueva, J., Zamorano, J. J., Aumaître, G., Bourlès, D., and Keddadouche, K.: Dating late Holocene lava flows in Pico de Orizaba (Mexico) by means of in situ-produced cosmogenic 36Cl, lichenometry and dendrochronology, Quat. Geochronol., 47, 93–106, https://doi.org/10.1016/j.quageo.2018.05.011, 2018. a
Anderson, S. W., Krinsley, D. H., and Fink, J. H.: Criteria for recognition of constructional silicic lava flow surfaces, Earth Surf. Proc. Land., 19, 531–541, https://doi.org/10.1002/esp.3290190606, 1994. a
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. a, b, c
Barrell, D. J.: Quaternary Glaciers of New Zealand, in: Developments in Quaternary Sciences, 15 edn., chap. 75, Elsevier, 1047–1064, https://doi.org/10.1016/B978-0-444-53447-7.00075-1, 2011. a, b
Barrell, D. J. A., Almond, P. C., Vandergoes, M. J., Lowe, D. J., and Newnham, R. M.: A composite pollen-based stratotype for inter-regional evaluation of climatic events in New Zealand over the past 30,000 years (NZ-INTIMATE project), Quaternary Sci. Rev., 74, 4–20, https://doi.org/10.1016/j.quascirev.2013.04.002, 2013. a
Blard, P.-H. and Farley, K. A.: The influence of radiogenic 4He on cosmogenic 3He determinations in volcanic olivine and pyroxene, Earth Planet. Sc. Lett., 276, 20–29, https://doi.org/10.1016/j.epsl.2008.09.003, 2008. a
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. a, b
Blard, P. H., Lavé, J., Pik, R., Wagnon, P., and Bourlès, D.: Persistence of full glacial conditions in the central Pacific until 15,000 years ago, Nature, 449, 591–594, https://doi.org/10.1038/nature06142, 2007. a
Blard, P.-H., Braucher, R., Lavé, J., and Bourlès, D.: Cosmogenic 10Be production rate calibrated against 3He in the high Tropical Andes (3800–4900 m , 20–22° S), Earth Planet. Sc. Lett., 382, 140–149, https://doi.org/10.1016/j.epsl.2013.09.010, 2013. a
Blard, P.-H., Balco, G., Burnard, P. G., Farley, K. A., Fenton, C. R., Friedrich, R., Jull, A. J., 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. a, b
Bromley, G. R., 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. a, b, c
Buchanan-Banks, J. M., Lockwood, J. P., and Rubin, M.: Radiocarbon dates for lava flows from northeast rift zone of Mauna Loa volcano, Hilo 7
Calvert, A. T. and Lanphere, M. A.: Argon geochronology of Kilauea's early submarine history, J. Volcanol. Geoth. Res., 151, 1–18, https://doi.org/10.1016/j.jvolgeores.2005.07.023, 2006. a
Calvert, A. T., Fierstein, J., and Hildreth, W.: Eruptive history of Middle Sister, Oregon Cascades, USA-Product of a late Pleistocene eruptive episode, Geosphere, 14, 2118–2139, https://doi.org/10.1130/GES01638.1, 2018. a, b
Carignan, J., Hild, P., Mevelle, G., Morel, J., and Yeghicheyan, D.: Routine analyses of trace elements in geological samples using flow injection and low pressure on-line liquid chromatography coupled to ICP-MS: A study of geochemical reference materials BR, DR-N, UB-N, AN-G and GH, Geostandard. Newslett., 25, 187–198, https://doi.org/10.1111/j.1751-908x.2001.tb00595.x, 2001. a
Cerling, T. E. and Craig, H.: Geomorphology and in-situ cosmogenic isotopes, Annu. Rev. Earth Pl. Sc., 273–317, 1994. a
Clay, P. L., Busemann, H., Sherlock, S. C., Barry, T. L., Kelley, S. P., and McGarvie, D. W.:
Coble, M. A., Grove, M., and Calvert, A. T.: Calibration of Nu-Instruments Noblesse multicollector mass spectrometers for argon isotopic measurements using a newly developed reference gas, Chem. Geol., 290, 75–87, https://doi.org/10.1016/j.chemgeo.2011.09.003, 2011. a
Cole, J. W. and Lewis, K. B.: Evolution of the Taupo-Hikurangi subduction system, Tectonophysics, 72, 1–21, https://doi.org/10.1016/0040-1951(81)90084-6, 1981. a
Connor, C., Bebbington, M., and Marzocchi, W.: Probabilistic Volcanic Hazard Assessment, Elsevier Inc., second edn., ISBN 9780123859389, https://doi.org/10.1016/b978-0-12-385938-9.00051-1, 2015. a
Conway, C. E.: Studies on the Glaciovolcanic and Magmatic Evolution of Ruapehu Volcano, New Zealand, PhD thesis, Victoria University of Wellington, https://researcharchive.vuw.ac.nz/handle/10063/5152 (last access: 25 May 2024), 2016. a
Conway, C. E., Townsend, D. B., Leonard, G. S., Wilson, C. J., Calvert, A. T., and Gamble, J. A.: Lava-ice interaction on a large composite volcano: a case study from Ruapehu, New Zealand, B. Volcanol., 77, 21, https://doi.org/10.1007/s00445-015-0906-2, 2015. a, b, c
Conway, C. E., Leonard, G. S., Townsend, D. B., Calvert, A. T., Wilson, C. J., Gamble, J. A., Eaves, S. R., Pure, L. R., Leonard, G. S., Townsend, D. B., Wilson, C. J., Calvert, A. T., Cole, R. P., Conway, C. E., Gamble, J. A., and Smith, T. B.: A high-resolution
Delunel, R., Blard, P.-H., Martin, L. C., Nomade, S., and Schlunegger, F.: Long term low latitude and high elevation cosmogenic 3He production rate inferred from a 107 ka-old lava flow in northern Chile; 22° S–3400 m a.s.l., Geochim. Cosmochim. Ac., 184, 71–87, https://doi.org/10.1016/j.gca.2016.04.023, 2016. a
Donoghue, S. L.: Late quaternary volcanic stratigraphy of the southeastern sector of the Mount Ruapehu ring plain New Zealand, PhD thesis, Massey University, https://mro.massey.ac.nz/items/516a0d80-eda3-4a7e-a495-2e13fcb7821c (last access: 25 May 2024), 1991. a
Donoghue, S. L. and Neall, V. E.: Late Quaternary constructional history of the southeastern Ruapehu ring plain, New Zealand, New Zeal. J. Geol. Geop., 44, 439–466, https://doi.org/10.1080/00288306.2001.9514949, 2001. a
Donoghue, S. L., Neall, V. E., and Palmer, A. S.: Stratigraphy and chronology of late quaternary andesitic tephra deposits, Tongariro Volcanic Centre, New Zealand, J. Roy. Soc. New Zeal., 25, 115–206, https://doi.org/10.1080/03014223.1995.9517487, 1995. a
Donoghue, S. L., Stewart, R. B., Neall, V. E., Lecointre, J., Price, R., Palmer, A. S., McClelland, E., and Hobson, K.: The Taurewa Eruptive Episode: Evidence for climactic eruptions at Ruapehu volcano, New Zealand, B. Volcanol., 61, 223–240, https://doi.org/10.1007/s004450050273, 1999. a, b, c
Donoghue, S. L., Vallance, J. W., Smith, I. E., and Stewart, R. B.: Using geochemistry as a tool for correlating proximal andesitic tephra: case studies from Mt Rainier (USA) and MT Ruapehu (New Zealand), J. Quaternary Sci., 22, 395–410, https://doi.org/10.1002/jqs.1065, 2007. a
Dostal, J., Dupuy, C., Carron, J. P., Le Guen de Kerneizon, M., and Maury, R. C.: Partition coefficients of trace elements: Application to volcanic rocks of St. Vincent, West Indies, Geochim. Cosmochim. Ac., 47, 525–533, https://doi.org/10.1016/0016-7037(83)90275-2, 1983. a
Dunn, T. and Sen, C.: Mineral/matrix partition coefficients for orthopyroxene, plagioclase, and olivine in basaltic to andesitic systems: A combined analytical and experimental study, Geochim. Cosmochim. Ac., 58, 717–733, https://doi.org/10.1016/0016-7037(94)90501-0, 1994. a, b
Eaves, S. R. and Brook, M. S.: Glaciers and glaciation of North Island, New Zealand, New Zeal. J. Geol. Geop., 64, 1–20, https://doi.org/10.1080/00288306.2020.1811354, 2021. a
Eaves, S. R., Winckler, G., Schaefer, J. J. M., Vandergoes, M. J., Alloway, B. V., Mackintosh, A. N., Townsend, D. B., Ryan, M. T., and Li, X.: A test of the cosmogenic 3He production rate in the south-west Pacific (39° S), J. Quaternary Sci., 30, 79–87, https://doi.org/10.1002/jqs.2760, 2015. a, b, c, d, e, f
Eaves, S. R., Mackintosh, A. N., Anderson, B. M., Doughty, A. M., Townsend, D. B., Conway, C. E., Winckler, G., Schaefer, J. M., Leonard, G. S., and Calvert, A. T.: The Last Glacial Maximum in the central North Island, New Zealand: palaeoclimate inferences from glacier modelling, Clim. Past, 12, 943–960, https://doi.org/10.5194/cp-12-943-2016, 2016a. a
Eaves, S. R., Mackintosh, A. N., Winckler, G., Schaefer, J. M., Alloway, B. V., and Townsend, D. B.: A cosmogenic 3He chronology of late Quaternary glacier fluctuations in North Island, New Zealand (39° S), Quaternary Sci. Rev., 132, 40–56, https://doi.org/10.1016/j.quascirev.2015.11.004, 2016b. a
Eaves, S. R., Winckler, G., Mackintosh, A. N., Schaefer, J. M., Townsend, D. B., Doughty, A. M., Jones, R. S., and Leonard, G. S.: Late-glacial and Holocene glacier fluctuations in North Island, New Zealand, Quaternary Sci. Rev., 223, 105914, https://doi.org/10.1016/j.quascirev.2019.105914, 2019. a, b, c
Espanon, V. R., Honda, M., and Chivas, A. R.: Cosmogenic 3He and 21Ne surface exposure dating of young basalts from Southern Mendoza, Argentina, Quat. Geochronol., 19, 76–86, https://doi.org/10.1016/j.quageo.2013.09.002, 2014. a, b, c
Fenton, C. R. and Niedermann, S.: Surface exposure dating of young basalts (1-200ka) in the San Francisco volcanic field (Arizona, USA) using cosmogenic 3He and 21Ne, Quat. Geochronol., 19, 87–105, https://doi.org/10.1016/j.quageo.2012.10.003, 2014. a
Fenton, C. R., Webb, R. H., Pearthree, P. A., Cerling, T. E., and Poreda, R. J.: Displacement rates on the Toroweap and Hurricane faults: Implications for Quaternary downcutting in the Grand Canyon, Arizona, Geology, 29, 1035–1038, https://doi.org/10.1130/0091-7613(2001)029<1035:DROTTA>2.0.CO;2, 2001. a
Fenton, C. R., Niedermann, S., Goethals, M. M., Schneider, B., and Wijbrans, J.: Evaluation of cosmogenic 3He and 21Ne production rates in olivine and pyroxene from two Pleistocene basalt flows, western Grand Canyon, AZ, USA, Quat. Geochronol., 4, 475–492, https://doi.org/10.1016/j.quageo.2009.08.002, 2009. a
Ferrier, K. L., Taylor Perron, J., Mukhopadhyay, S., Rosener, M., Stock, J. D., Huppert, K. L., and Slosberg, M.: Covariation of climate and long-term erosion rates across a steep rainfall gradient on the Hawaiian island of Kaua'i, Bull. Geol. Soc. Am., 125, 1146–1163, https://doi.org/10.1130/B30726.1, 2013. a
Fierstein, J., Hildreth, W., and Calvert, A. T.: Eruptive history of South Sister, Oregon Cascades, J. Volcanol. Geoth. Res., 207, 145–179, https://doi.org/10.1016/j.jvolgeores.2011.06.003, 2011. a
Fleck, R. J., Hagstrum, J. T., Calvert, A. T., Evarts, R. C., and Conrey, R. M.:
Foeken, J. P., Day, S., and Stuart, F. M.: Cosmogenic 3He exposure dating of the Quaternary basalts from Fogo, Cape Verdes: Implications for rift zone and magmatic reorganisation, Quat. Geochronol., 4, 37–49, https://doi.org/10.1016/j.quageo.2008.07.002, 2009. a, b, c, d
Gabrielsen, H., Procter, J., Rainforth, H., Black, T., Harmsworth, G., and Pardo, N.: Reflections from an Indigenous Community on Volcanic Event Management, Communications and Resilience, in: Observing the Volcano World. Advances in Volcanology, edited by: Fearnley, C. J., Bird, D. K., Haynes, K., McGuire, W. J., and Jolly, G., Springer, Cham. 463–479, https://doi.org/10.1007/11157_2016_44, 2018. a
Gallahan, W. E. and Nielsen, R. L.: The partitioning of Sc, Y, and the rare earth elements between high-Ca pyroxene and natural mafic to intermediate lavas at 1 atmosphere, Geochim. Cosmochim. Ac., 56, 2387–2404, https://doi.org/10.1016/0016-7037(92)90196-P, 1992. a
Gamble, J. A., Price, R. C., Smith, I. E., McIntosh, W. C., and Dunbar, N. W.:
Gosse, J. C. and Phillips, F. M.: Terrestrial in situ cosmogenic nuclides: Theory and application, Quaternary Sci. Rev., 20, 1475–1560, https://doi.org/10.1016/S0277-3791(00)00171-2, 2001. a, b
Greve, A., Turner, G. M., Conway, C. E., Townsend, D. B., Gamble, J. A., and Leonard, G. S.: Palaeomagnetic refinement of the eruption ages of Holocene lava flows, and implications for the eruptive history of the Tongariro Volcanic Centre, New Zealand, Geophys. J. Int., 207, 702–718, https://doi.org/10.1093/gji/ggw296, 2016. a, b, c, d, e, f, g, h, i, j, k, l, m, n
Harpel, C. J., Kyle, P. R., Esser, R. P., McIntosh, W. C., and Caldwell, D. A.:
Harris, A. J. L.: Basaltic Lava Flow Hazard, in: Volcanic Hazards, Risks and Disasters, edited by: Shroder, J. F. and Papale, P., chap. 2, 17–46, Elsevier, https://doi.org/10.1016/C2011-0-07012-6, 2015. a
Hilton, D. R., Fischer, T. P., and Marry, B.: Noble gases and volatile recycling at subduction zones, Rev. Mineral. Geochem., 47, 319–370, https://doi.org/10.2138/rmg.2002.47.9, 2002. a
Houghton, B. F., Wilson, C. J., McWilliams, M. O., Lanphere, M. A., Weaver, S. D., Briggs, R. M., and Pringle, M. S.: Chronology and dynamics of a large silicic magmatic system: central Taupo Volcanic Zone, New Zealand, Geology, 23, 13–16, https://doi.org/10.1130/0091-7613(1995)023<0013:CADOAL>2.3.CO;2, 1995. a
Jenkins, S. F., Day, S. J., Faria, B. V., and Fonseca, J. F.: Damage from lava flows: insights from the 2014–2015 eruption of Fogo, Cape Verde, Journal of Applied Volcanology, 6, 6, https://doi.org/10.1186/s13617-017-0057-6, 2017. a
Keys, H. and Green, P. M.: Mitigation of volcanic risks at Mt Ruapehu, New Zealand, Proceedings of the Moutain Risks international conference, Firenze, Italy, 24–26 November, 485–490, https://www.researchgate.net/profile/Harry-Keys/publication/281606085_Mitigation_of_volcanic_risks_at_Mt_Ruapehu_New_Zealand/links/581f8fa608aeccc08af3abd6/Mitigation-of-volcanic-risks-at-Mt-Ruapehu-New-Zealand.pdf (last access: 25 May 2024), 2010. a
Klein, J., Giegengack, R., Middleton, R., Sharma, P., Underwood, J. R., and Weeks, R. A.: Revealing Histories of Exposure Using in Situ Produced 26Al and 10Be in Libyian Desert Glass, Radiocarbon, 28, 547–555, 1986. a
Kurz, M. D.: Cosmogenic helium in a terrestrial igneous rock, Nature, 320, 435–439, https://doi.org/10.1038/320435a0, 1986a. a, b, c
Kurz, M. D.: In situ production of terrestrial cosmogenic helium and some applications to geochronology, Geochim. Cosmochim. Ac., 50, 2855–2862, https://doi.org/10.1016/0016-7037(86)90232-2, 1986b. a
Lal, D.: An important source of 4He (and 3He) in diamonds, Earth Planet. Sc. Lett., 96, 1–7, https://doi.org/10.1016/0012-821X(89)90118-0, 1989. a
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. a, b
Lanphere, M. A.: Comparison of conventional K-Ar and
Le Maitre, R. W.: Igneous Rocks: A Classification and Glossary of Terms, Recommendations of the International Union of Geological Sciences, Subcomission of the Systematics of Igneous Rocks, Cambridge University Press, https://doi.org/10.1017/CBO9780511535581, 2002. a, b
Leonard, G. S., Cole, R. P. R., Christenson, B. W., Conway, C. E., Cronin, S. J., Gamble, J. A., Hurst, T., Kennedy, B. M., Miller, C. A., Procter, J. N., Pure, L. R., Townsend, D. B., White, J. D., and Wilson, C. J.: Ruapehu and Tongariro stratovolcanoes: a review of current understanding, New Zeal. J. Geol. Geop., 64, 389–420, https://doi.org/10.1080/00288306.2021.1909080, 2021. a, b
Leya, I., Lange, H. J., Neumann, S., Wieler, R., and Michel, R.: The production of cosmogenic nuclides in stony meteoroids by galactic cosmic-ray particles, Meteorit. Planet. Sci., 35, 259–286, https://doi.org/10.1111/j.1945-5100.2000.tb01775.x, 2000. a
Licciardi, J. M., Kurz, M. D., and Curtice, J. M.: Cosmogenic 3He production rates from Holocene lava flows in Iceland, Earth Planet. Sc. Lett., 246, 251–264, https://doi.org/10.1016/j.epsl.2006.03.016, 2006. a
Licciardi, J. M., Kurz, M. D., and Curtice, J. M.: Glacial and volcanic history of Icelandic table mountains from cosmogenic 3He exposure ages, Quaternary Sci. Rev., 26, 1529–1546, https://doi.org/10.1016/j.quascirev.2007.02.016, 2007. a, b, c
Lifton, N.: Implications of two Holocene time-dependent geomagnetic models for cosmogenic nuclide production rate scaling, Earth Planet. Sc. Lett., 433, 257–268, https://doi.org/10.1016/j.epsl.2015.11.006, 2016. a, b
Lifton, N., Sato, T., and Dunai, T. J.: Scaling in situ cosmogenic nuclide production rates using analytical approximations to atmospheric cosmic-ray fluxes, Earth Planet. Sc. Lett., 386, 149–160, https://doi.org/10.1016/j.epsl.2013.10.052, 2014. a
Lippolt, H. J. and Weigel, E.: 4He diffusion in 40Ar-retentive minerals, Geochim. Cosmochim. Ac., 52, 1449–1458, https://doi.org/10.1016/0016-7037(88)90215-3, 1988. a
Lockwood, J. P. and Lipman, P. W.: Recovery of datable charcoal beneath young lavas: Lessons from Hawaii, Bulletin Volcanologique, 43, 609–615, https://doi.org/10.1007/BF02597697, 1980. a
Luhr, J. F. and Carmichael, I. S. E.: The Colima Volcanic complex, Mexico, Contrib. Mineral. Petr., 71, 343–372, https://doi.org/10.1007/bf00374707, 1980. a
Lupton, J. and Evans, L.: Changes in the atmospheric helium isotope ratio over the past 40 years, Geophys. Res. Lett., 40, 6271–6275, https://doi.org/10.1002/2013GL057681, 2013. a
Marchetti, D. W., Hynek, S. A., and Cerling, T. E.: Cosmogenic 3He exposure ages of basalt flows in the northwestern Payún Matru volcanic field, Mendoza Province, Argentina, Quat. Geochronol., 19, 67–75, https://doi.org/10.1016/j.quageo.2012.10.004, 2014. a, b, c
Martin, L. C., Blard, P.-H., Balco, G., Lavé, J., Delunel, R., Lifton, N., and Laurent, V.: The CREp program and the ICE-D production rate calibration database: A fully parameterizable and updated online tool to compute cosmic-ray exposure ages, Quat. Geochronol., 38, 25–49, https://doi.org/10.1016/j.quageo.2016.11.006, 2017. a
Matsuda, J., Matsumoto, T., Sumino, H., Nagao, K., Yamamoto, J., Miura, Y., Kaneoka, I., Takahata, N., and Sano, Y.: The
Mc Arthur, J. L. and Shepherd, M. J.: Late Quaternary glaciation of Mt. Ruapehu, North Island, New Zealand, J. Roy. Soc. New Zeal., 20, 287–296, https://doi.org/10.1080/03036758.1990.10416823, 1990. a
Medynski, S., Pik, R., Burnard, P., Vye-Brown, C., France, L., Schimmelpfennig, I., Whaler, K., Johnson, N., Benedetti, L., Ayelew, D., and Yirgu, G.: Stability of rift axis magma reservoirs: Spatial and temporal evolution of magma supply in the Dabbahu rift segment (Afar, Ethiopia) over the past 30 kyr, Earth Planet. Sc. Lett., 409, 278–289, https://doi.org/10.1016/j.epsl.2014.11.002, 2015. a, b
Mishra, A. K., Placzek, C., Wurster, C., and Whitehead, P. W.: New radiocarbon age constraints for the 120 km-long Toomba flow, north Queensland, Australia, Aust. J. Earth Sci., 66, 71–79, https://doi.org/10.1080/08120099.2019.1523227, 2019. a
Moore, R. B. and Rubin, M.: Radiocarbon dates for lava flows and pyroclastic deposits on Sao Miguel, Azores, Radiocarbon, 33, 151–164, https://doi.org/10.1017/S0033822200013278, 1991. a
Morimoto, N., Fabries, J., Ferguson, A., Ginzburg, I., Ross, M., Seifert, F., Zussman, J., Aoki, K., and Gottardi, G.: Nomenclature of pyroxenes Subcommittee on Pyroxenes Commission on New Minerals and Mineral Names International Mineralogical Association, Am. Mineral., 73, 1123–1133, 1988. a
Muscheler, R., Beer, J., Kubik, P. W., and Synal, H. A.: Geomagnetic field intensity during the last 60,000 years based on 10Be and 36Cl from the Summit ice cores and 14C, Quaternary Sci. Rev., 24, 1849–1860, https://doi.org/10.1016/j.quascirev.2005.01.012, 2005. a, b
Nairn, I. A., Kobayashi, T., and Nakagawa, M.: The ∼ 10 ka multiple vent pyroclastic eruption sequence at Tongariro Volcanic Centre, Taupo Volcanic Zone, New Zealand: Part 1. Eruptive processes during regional extension, J. Volcanol. Geoth. Res., 86, 19–44, https://doi.org/10.1016/S0377-0273(98)00085-7, 1998. a
Nicholls, I. A. and Harris, K. L.: Experimental rare earth element partition coefficients for garnet, clinopyroxene and amphibole coexisting with andesitic and basaltic liquids, Geochim. Cosmochim. Ac., 44, 287–308, https://doi.org/10.1016/0016-7037(80)90138-6, 1980. a
Niedermann, S.: Cosmic-ray-produced noble gases in terrestrial rocks: Dating tools for surface processes, Rev. Mineral. Geochem., 47, 731–784, https://doi.org/10.2138/rmg.2002.47.16, 2002. a
Nishiizumi, K.: Cosmic ray production rates of 10Be and 26Al in quartz from glacially polished rocks, J. Geophys. Res., 94, 17907–17915, https://doi.org/10.1029/jb094ib12p17907, 1989. a, b
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. a
Palmer, B. A. and Neall, V. E.: The Murimotu Formation – 9500 year old deposits of a debris avalanche and associated lahars, Mount Ruapehu, North Island, New Zealand, New Zeal. J. Geol. Geop., 32, 477–486, https://doi.org/10.1080/00288306.1989.10427555, 1989. a
Pardo, N.: Andesitic Plinian Eruptions at Mt. Ruapehu (New Zealand): From Lithofacies to Eruption Dynamics, PhD thesis, Massey University, https://mro.massey.ac.nz/items/c2f61b33-2579-410f-b493-eeab08691375 (last access: 25 May 2024), 2012. a
Pardo, N., Cronin, S., Palmer, A., Procter, J., and Smith, I.: Andesitic Plinian eruptions at Mt. Ruapehu: Quantifying the uppermost limits of eruptive parameters, B. Volcanol., 74, 1161–1185, https://doi.org/10.1007/s00445-012-0588-y, 2012a. a, b
Pardo, N., Cronin, S. J., Palmer, A. S., and Németh, K.: Reconstructing the largest explosive eruptions of Mt. Ruapehu, New Zealand: Lithostratigraphic tools to understand subplinian-plinian eruptions at andesitic volcanoes, B. Volcanol., 74, 617–640, https://doi.org/10.1007/s00445-011-0555-z, 2012b. a, b
Patterson, D. B., Honda, M., and McDougall, I.: Noble gases in mafic phenocrysts and xenoliths from New Zealand, Geochim. Cosmochim. Ac., 58, 4411–4427, https://doi.org/10.1016/0016-7037(94)90344-1, 1994. a, b, c
Preece, K., Mark, D. F., Barclay, J., Cohen, B. E., Chamberlain, K. J., Jowitt, C., Vye-Brown, C., Brown, R. J., and Hamilton, S.: Bridging the gap:
Price, R. C., Gamble, J. A., Smith, I. E., Maas, R., Waight, T., Stewart, R. B., and Woodhead, J.: The anatomy of an andesite volcano: A time-stratigraphic study of andesite petrogenesis and crustal evolution at Ruapehu Volcano, New Zealand, J. Petrol., 53, 2139–2189, https://doi.org/10.1093/petrology/egs050, 2012. a, b, c, d, e, f
Puchol, N., Blard, P.-H., Pik, R., Tibari, B., and Lavé, J.: Variability of magmatic and cosmogenic 3He in Ethiopian river sands of detrital pyroxenes: Impact on denudation rate determinations, Chem. Geol., 448, 13–25, https://doi.org/10.1016/j.chemgeo.2016.10.033, 2017. a, b, c
Pure, L. R., Leonard, G. S., Townsend, D. B., Wilson, C. J., Calvert, A. T., Cole, R. P., Conway, C. E., Gamble, J. A., and Smith, T. B.: A high resolution
Ramos, F. C., Heizler, M. T., Buettner, J. E., Gill, J. B., Wei, H. Q., Dimond, C. A., and Scott, S. R.: U-series and
Rhodes, E.: The Draining of an Andesitic Valley-Confined Lava Flow, Mt Ruapehu, Honours thesis, University of Canterbury, 2012. a
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, 2016. a
Schimmelpfennig, I., Williams, A., Pik, R., Burnard, P., Niedermann, S., Finkel, R., Schneider, B., and Benedetti, L.: Inter-comparison of cosmogenic in-situ 3He, 21Ne and 36Cl at low latitude along an altitude transect on the SE slope of Kilimanjaro volcano (3° S, Tanzania), Quat. Geochronol., 6, 425–436, https://doi.org/10.1016/j.quageo.2011.05.002, 2011. a
Sherrod, D. R., Hagstrum, J. T., Mcgeehin, J. P., Champion, D. E., and Trusdell, F. A.: Distribution , 14C chronology , and paleomagnetism of latest Pleistocene and Holocene lava flows at Haleakala Island of Maui , Hawai′i: A revision of lava flow hazard zones, J. Geophys. Res., 111, B05205, https://doi.org/10.1029/2005JB003876, 2006. a, b
Shuster, D. L., Farley, K. A., Sisterson, J. M., and Burnett, D. S.: Quantifying the diffusion kinetics and spatial distributions of radiogenic 4He in minerals containing proton-induced 3He, Earth Planet. Sc. Lett., 217, 19–32, https://doi.org/10.1016/S0012-821X(03)00594-6, 2004. a
Smith, J. A., Finkel, R. C., Farber, D. L., Rodbell, D. T., and Seltzer, G. O.: Moraine preservation and boulder erosion in the tropical Andes: Interpreting old surface exposure ages in glaciated valleys, J. Quaternary Sci., 20, 735–758, https://doi.org/10.1002/jqs.981, 2005. a
Stipp, J.: The Geochronology and Petrogenesis of the Cenozoic Volcanics of the North Island, New Zealand, PhD thesis, Australian National University, https://www.proquest.com/docview/2617247792?pq-origsite=gscholar&fromopenview=true&sourcetype=Dissertations & Theses (last access: 9 July 2023), 1968. a
Stone, J. O.: Air pressure and cosmogenic isotope production, J. Geophys. Res.,, 105, 753–759, https://doi.org/10.1029/2000JB900181, 2000. a, b
Tanaka, H., Kawamura, K., Nagao, K., and Houghton, B. F.: K-Ar ages and paleosecular variation of direction and intensity from quaternary lava sequences in the Ruapehu Volcano, New Zealand, Earth Planets Space, 49, 587–599, https://doi.org/10.5636/jgg.49.587, 1997. a
Topping, W. W.: Some aspects of quaternary history of Tongariro Volcanic Centre, PhD thesis, Victoria University of Wellington, https://openaccess.wgtn.ac.nz/articles/thesis/Some_Aspects_of_Quaternary_History_of_Tongariro_Volcanic_Centre/19252133/1 (last access: 9 July 2023) 1974. a
Topping, W. W. and Kohn, B. P.: Rhyolitic tephra marker beds in the Tongariro area, North Island, New Zealand, New Zeal. J. Geol. Geop., 16, 375–395, https://doi.org/10.1080/00288306.1973.10431367, 1973. a, b
Tremblay, M. M., Shuster, D. L., and Balco, G.: Diffusion kinetics of 3He and 21Ne in quartz and implications for cosmogenic noble gas paleothermometry, Geochim. Cosmochim. Ac., 142, 186–204, https://doi.org/10.1016/j.gca.2014.08.010, 2014. a
Trusdell, F. A.: Lava flow hazards and risk assessment on Mauna Loa Volcano, Hawaii, Geoph. Monog. Series, 92, 327–336, https://doi.org/10.1029/GM092p0327, 1995. a, b
Tsang, S. and Lindsay, J.: Lava flow crises in inhabited areas part I: Lessons learned and research gaps related to effusive, basaltic eruptions, Journal of Applied Volcanology, 9, 9, https://doi.org/10.1186/s13617-020-00096-y, 2020. a
Turner, G. M. and Corkill, R. M.: NZPSV11k.2023 and NZPSV1k.2023: Holocene palaeomagnetic secular variation master records for New Zealand, Phys. Earth Planet. In., 344, 107093, https://doi.org/10.1016/j.pepi.2023.107093, 2023. a
Turner, G. M., Howarth, J. D., de Gelder, G. I., and Fitzsimons, S. J.: A new high-resolution record of Holocene geomagnetic secular variation from New Zealand, Earth Planet. Sc. Lett., 430, 296–307, https://doi.org/10.1016/j.epsl.2015.08.021, 2015. a, b
Uppala, S. M., Kållberg, P. W., Simmons, A. J., Andrae, U., da Costa Bechtold, V., Fiorino, M., Gibson, J. K., Haseler, J., Hernandez, A., Kelly, G. A., Li, X., Onogi, K., Saarinen, S., Sokka, N., Allan, R. P., Andersson, E., Arpe, K., Balmaseda, M. A., Beljaars, A. C., van de Berg, L., Bidlot, J., Bormann, N., Caires, S., Chevallier, F., Dethof, A., Dragosavac, M., Fisher, M., Fuentes, M., Hagemann, S., Hólm, E., Hoskins, B. J., Isaksen, L., Janssen, P. A., Jenne, R., McNally, A. P., Mahfouf, J. F., Morcrette, J. J., Rayner, N. A., Saunders, R. W., Simon, P., Sterl, A., Trenberth, K. E., Untch, A., Vasiljevic, D., Viterbo, P., and Woollen, J.: The ERA-40 re-analysis, Q. J. Roy. Meteor. Soc., 131, 2961–3012, https://doi.org/10.1256/qj.04.176, 2005. a
Vermeesch, P.: IsoplotR: A free and open toolbox for geochronology, Geosci. Front., 9, 1479–1493, https://doi.org/10.1016/j.gsf.2018.04.001, 2018. a
Villemant, B.: Trace element evolution in the Phlegrean Fields (Central Italy): fractional crystallization and selective enrichment, Contrib. Mineral. Petr., 98, 169–183, https://doi.org/10.1007/BF00402110, 1988. a
Wijbrans, J., Schneider, B., Kuiper, K., Calvari, S., Branca, S., De Beni, E., Norini, G., Corsaro, R. A., and Miraglia, L.:
Wilson, C. J., Gravley, D. M., Leonard, G. S., and Rowland, J. V.: Volcanism in the central Taupo Volcanic Zone, New Zealand: tempo, styles and controls, in: Studies in Volcanology: The Legacy of George Walker, edited by: Thordarson, T., Special Publications of IAVCEI 2, 225–247, https://doi.org/10.1144/IAVCEl002.12, 2009. a
Wilson, G., Wilson, T. M., Deligne, N. I., and Cole, J. W.: Volcanic hazard impacts to critical infrastructure: A review, J. Volcanol. Geoth. Res., 286, 148–182, https://doi.org/10.1016/j.jvolgeores.2014.08.030, 2014. a
Wright, H. M., Vazquez, J. A., Champion, D. E., Calvert, A. T., Mangan, M. T., Stelten, M., Cooper, K. M., Herzig, C., and Jr, A. S.: Episodic Holocene eruption of the Salton Buttes rhyolites, California, from paleomagnetic, U-Th, and
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. a
Short summary
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.
In this study, we use cosmogenic-sourced 3He to determine the eruption ages of 23 lava flows at...
