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Ram R, Adar EM, Yechieli Y, Yokochi R, Aeschbach W, Armon M, Solomon DK, Purtschert R, Seltzer AM, Urbach KL, Bishof M, Mueller P, Zappala JC, Jiang W, Lu ZT, Reznik IJ. Deep desert aquifers as an archive for Mid- to Late Pleistocene hydroclimate: An example from the southeastern Mediterranean. THE SCIENCE OF THE TOTAL ENVIRONMENT 2024; 951:175737. [PMID: 39187079 DOI: 10.1016/j.scitotenv.2024.175737] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/29/2024] [Revised: 08/19/2024] [Accepted: 08/21/2024] [Indexed: 08/28/2024]
Abstract
Many efforts have been made to illuminate the nature of past hydroclimates in semi-arid and arid regions, where current and future shifts in water availability have enormous consequences on human subsistence. Deep desert aquifers, where groundwater is stored for prolonged periods, might serve as a direct record of major paleo-recharge events. To date, groundwater-based paleoclimate reconstructions have mainly focused on a relatively narrow timescale (up to ∼40 kyr), limited by the relatively short half-life of the widely used radiocarbon (5.73 kyr). Here we demonstrate the usage of deep regional aquifers in the arid southeastern Mediterranean as a hydroclimate archive for earlier Mid-to-Late Pleistocene epochs. State-of-the-art dating tools, primarily the 81Kr radioisotope (t1/2 = 229 kyr), were combined with other atmosphere-derived tracers to illuminate the impact of four distinguishable wetter episodes over the past 400 kyr, with differences in climatic conditions and paleo-recharge locations. Variations in stable water isotope composition suggest moisture transport from more proximal (Mediterranean) and distal (Atlantic) sources to different parts of the region at distinct times. Large variability in the computed noble gas-based recharge temperature (NGT), ranging ~15-30 °C, cannot be explained by climate variations solely, and points to different recharge pathways, including geothermal heating in the deep unsaturated zone and recharge from high-elevation (colder) regions. The obtained groundwater record complements and enhances the interpretation of other terrestrial archives in the arid region, including a contribution of valuable information regarding the moisture source origin as reflected in the deuterium-excess values, which is unattainable from the common practice analysis of calcitic cave deposits. We conclude that similar applications in other deep (hundred-m-order) regional groundwater systems (e.g., the Sahara desert aquifers) can significantly advance our understanding of long-term (up to 1 Myr) paleo-hydroclimate in arid regions, including places where no terrestrial remnants, such as cave, lake, and spring sediments, are available.
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Affiliation(s)
- Roi Ram
- Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede-Boqer Campus, Israel; Geological Survey of Israel, Jerusalem, Israel; Institute of Environmental Physics, Heidelberg University, Heidelberg, Germany.
| | - Eilon M Adar
- Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede-Boqer Campus, Israel
| | - Yoseph Yechieli
- Zuckerberg Institute for Water Research, Blaustein Institutes for Desert Research, Ben-Gurion University of the Negev, Sede-Boqer Campus, Israel; Geological Survey of Israel, Jerusalem, Israel
| | - Reika Yokochi
- Department of the Geophysical Sciences, The University of Chicago, Chicago, IL, USA
| | - Werner Aeschbach
- Institute of Environmental Physics, Heidelberg University, Heidelberg, Germany
| | - Moshe Armon
- Institute for Atmospheric and Climate Science, ETH Zurich, Zurich, Switzerland
| | - D Kip Solomon
- Department of Geology and Geophysics, University of Utah, Salt Lake City, UT, USA
| | - Roland Purtschert
- Climate and Environmental Physics, Physics Institute, University of Bern, Bern, Switzerland
| | - Alan M Seltzer
- Marine Chemistry & Geochemistry Department, Woods Hole Oceanographic Institution, MA, USA
| | - Kerstin L Urbach
- Institute of Environmental Physics, Heidelberg University, Heidelberg, Germany
| | - Michael Bishof
- Physics Division, Argonne National Laboratory, Lemont, IL, USA
| | - Peter Mueller
- Physics Division, Argonne National Laboratory, Lemont, IL, USA
| | - Jake C Zappala
- Physics Division, Argonne National Laboratory, Lemont, IL, USA
| | - Wei Jiang
- Hefei National Laboratory, School of Physical Sciences, University of Science and Technology of China, Hefei, China
| | - Zheng-Tian Lu
- Hefei National Laboratory, School of Physical Sciences, University of Science and Technology of China, Hefei, China
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2
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Steidle SD, Wendt KA, Dublyansky Y, Edwards RL, Li X, McClure G, Moseley GE, Spötl C. Moisture availability and groundwater recharge paced by orbital forcing over the past 750,000 years in the southwestern USA. COMMUNICATIONS EARTH & ENVIRONMENT 2024; 5:376. [PMID: 39015622 PMCID: PMC11246950 DOI: 10.1038/s43247-024-01550-0] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Key Words] [Grants] [Track Full Text] [Figures] [Subscribe] [Scholar Register] [Received: 10/31/2023] [Accepted: 07/03/2024] [Indexed: 07/18/2024]
Abstract
Quaternary climate changes are driven in part by variations in the distribution and strength of insolation due to orbital parameters. Continental climate variability is well documented for the most recent glacial-interglacial cycles, yet few records extend further back in time. Such records are critically needed to comprehensively assess the entire spectrum of natural climate variability against the backdrop of anthropogenic warming. Here, we apply uranium isotope geochronology to calcite deposits to date groundwater-table changes in Devils Hole cave, Nevada. The deposits record multi-meter groundwater-table fluctuations over the last 750,000 years, reflecting the long-term evolution of hydroclimate in this presently arid region. During periods between glacial or interglacial extremes, the water table responded sensitively to variations in 65°N summer insolation, likely caused by the increasing extent of North American ice sheets during cold period, which steered moisture-laden trajectories towards the southwestern USA. These orbitally-driven hydroclimatic changes are superimposed on a tectonically-driven long-term decline in the regional groundwater table observed prior to 438,000 ± 14,000 years ago.
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Affiliation(s)
- Simon D. Steidle
- Institute of Geology, University of Innsbruck, Innsbruck, Austria
| | - Kathleen A. Wendt
- College of Earth, Ocean, and Atmospheric Sciences, Oregon State University, Corvallis, OR USA
| | - Yuri Dublyansky
- Institute of Geology, University of Innsbruck, Innsbruck, Austria
| | - R. Lawrence Edwards
- School of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN USA
| | - Xianglei Li
- School of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN USA
- Institute of Vertebrate Paleontology and Paleoanthropology, Chinese Academy of Science, Beijing, China
| | - Gracelyn McClure
- School of Earth and Environmental Sciences, University of Minnesota, Minneapolis, MN USA
| | - Gina E. Moseley
- Institute of Geology, University of Innsbruck, Innsbruck, Austria
| | - Christoph Spötl
- Institute of Geology, University of Innsbruck, Innsbruck, Austria
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Seltzer AM, Shackleton SA, Bourg IC. Solubility Equilibrium Isotope Effects of Noble Gases in Water: Theory and Observations. J Phys Chem B 2023; 127:9802-9812. [PMID: 37937341 DOI: 10.1021/acs.jpcb.3c05651] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Indexed: 11/09/2023]
Abstract
The abundance and isotopic composition of noble gases dissolved in water have many applications in the geosciences. In recent years, new analytical techniques have opened the door to the use of high-precision measurements of noble gas isotopes as tracers for groundwater hydrology, oceanography, mantle geochemistry, and paleoclimatology. These analytical advances have brought about new measurements of solubility equilibrium isotope effects (SEIEs) in water (i.e., the relative solubilities of noble gas isotopes) and their sensitivities to the temperature and salinity. Here, we carry out a suite of classical molecular dynamics (MD) simulations and employ the theoretical method of quantum correction to estimate SEIEs for comparison with experimental observations. We find that classical MD simulations can accurately predict SEIEs for the isotopes of Ar, Kr, and Xe to order 0.01‰, on the scale of analytical uncertainty. However, MD simulations consistently overpredict the SEIEs of Ne and He by up to 40% of observed values. We carry out sensitivity tests at different temperatures, salinities, and pressures and employ different sets of interatomic potential parameters and water models. For all noble gas isotopes, the TIP4P water model is found to reproduce observed SEIEs more accurately than the SPC/E and TIP4P/ice models. Classical MD simulations also accurately capture the sign and approximate magnitude of temperature and salinity sensitivities of SEIEs for heavy noble gases. We find that experimental and modeled SEIEs generally follow an inverse-square mass dependence, which implies that the mean-square force experienced by a noble gas atom within a solvation shell is similar for all noble gases. This inverse-square mass proportionality is nearly exact for Ar, Kr, and Xe isotopes, but He and Ne exhibit a slightly weaker mass dependence. We hypothesize that the apparent dichotomy between He-Ne and Ar-Kr-Xe SEIEs may result from atomic size differences, whereby the smaller noble gases are more likely to spontaneously fit within cavities of water without breaking water-water H-bonds, thereby experiencing softer collisions during translation within a solvation shell. We further speculate that the overprediction of simulated He and Ne SEIEs may result from the neglection of higher-order quantum corrections or the overly stiff representation of van der Waals repulsion by the widely used Lennard-Jones 6-12 potential model. We suggest that new measurements of SEIEs of heavy and light noble gases may represent a novel set of constraints with which to refine hydrophobic solvation theories and optimize the set of interatomic potential models used in MD simulations of water and noble gases.
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Affiliation(s)
- Alan M Seltzer
- Woods Hole Oceanographic Institution, Woods Hole, Massachusetts 02543-1050,United States
| | - Sarah A Shackleton
- Department of Geosciences, Princeton University, Princeton, New Jersey 08544,United States
| | - Ian C Bourg
- Department of Civil and Environmental Engineering (CEE) and High Meadows Environmental Institute (HMEI), Princeton University, Princeton, New Jersey 08544,United States
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Bekaert DV, Barry PH, Broadley MW, Byrne DJ, Marty B, Ramírez CJ, de Moor JM, Rodriguez A, Hudak MR, Subhas AV, Halldórsson SA, Stefánsson A, Caracausi A, Lloyd KG, Giovannelli D, Seltzer AM. Ultrahigh-precision noble gas isotope analyses reveal pervasive subsurface fractionation in hydrothermal systems. SCIENCE ADVANCES 2023; 9:eadg2566. [PMID: 37058557 PMCID: PMC10104464 DOI: 10.1126/sciadv.adg2566] [Citation(s) in RCA: 0] [Impact Index Per Article: 0] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 12/12/2022] [Accepted: 03/16/2023] [Indexed: 06/19/2023]
Abstract
Mantle-derived noble gases in volcanic gases are powerful tracers of terrestrial volatile evolution, as they contain mixtures of both primordial (from Earth's accretion) and secondary (e.g., radiogenic) isotope signals that characterize the composition of deep Earth. However, volcanic gases emitted through subaerial hydrothermal systems also contain contributions from shallow reservoirs (groundwater, crust, atmosphere). Deconvolving deep and shallow source signals is critical for robust interpretations of mantle-derived signals. Here, we use a novel dynamic mass spectrometry technique to measure argon, krypton, and xenon isotopes in volcanic gas with ultrahigh precision. Data from Iceland, Germany, United States (Yellowstone, Salton Sea), Costa Rica, and Chile show that subsurface isotope fractionation within hydrothermal systems is a globally pervasive and previously unrecognized process causing substantial nonradiogenic Ar-Kr-Xe isotope variations. Quantitatively accounting for this process is vital for accurately interpreting mantle-derived volatile (e.g., noble gas and nitrogen) signals, with profound implications for our understanding of terrestrial volatile evolution.
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Affiliation(s)
- David V. Bekaert
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
- Université de Lorraine, CNRS, CRPG, F-54000 Nancy, France
| | - Peter H. Barry
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
| | - Michael W. Broadley
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
- Université de Lorraine, CNRS, CRPG, F-54000 Nancy, France
| | - David J. Byrne
- Université de Lorraine, CNRS, CRPG, F-54000 Nancy, France
| | - Bernard Marty
- Université de Lorraine, CNRS, CRPG, F-54000 Nancy, France
| | - Carlos J. Ramírez
- Servicio Geológico Ambiental (SeGeoAm) Heredia, Santo Domingo, Costa Rica
| | - J. Maarten de Moor
- Observatorio Vulcanológico y Sismológico de Costa Rica Universidad Nacional, Heredia, Costa Rica
- Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, NM 87106, USA
| | - Alejandro Rodriguez
- Observatorio Vulcanológico y Sismológico de Costa Rica Universidad Nacional, Heredia, Costa Rica
| | - Michael R. Hudak
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
| | - Adam V. Subhas
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
| | | | - Andri Stefánsson
- NordVulk, Institute of Earth Sciences, University of Iceland, Reykjavík, Iceland
| | - Antonio Caracausi
- Instituto Nazionale di Geofisica e Vulcanologia, Sezione di Palermo, 90146 Palermo, Italy
- University of Salamanca, Salamanca, Spain
| | - Karen G. Lloyd
- Microbiology Department, University of Tennessee, Knoxville, TN 37996, USA
| | - Donato Giovannelli
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
- Department of Biology, University of Naples Federico II, Naples, Italy
- Institute for Marine Biological and Biotechnological Resources, National Research Council of Italy, Ancona, Italy
- Department of Marine and Coastal Science, Rutgers University, New Brunswick, NJ 08901, USA
| | - Alan M. Seltzer
- Marine Chemistry and Geochemistry Department, Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
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5
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Widespread six degrees Celsius cooling on land during the Last Glacial Maximum. Nature 2021; 593:228-232. [PMID: 33981051 DOI: 10.1038/s41586-021-03467-6] [Citation(s) in RCA: 11] [Impact Index Per Article: 3.7] [Reference Citation Analysis] [Abstract] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 11/06/2020] [Accepted: 03/17/2021] [Indexed: 02/03/2023]
Abstract
The magnitude of global cooling during the Last Glacial Maximum (LGM, the coldest multimillennial interval of the last glacial period) is an important constraint for evaluating estimates of Earth's climate sensitivity1,2. Reliable LGM temperatures come from high-latitude ice cores3,4, but substantial disagreement exists between proxy records in the low latitudes1,5-8, where quantitative low-elevation records on land are scarce. Filling this data gap, noble gases in ancient groundwater record past land surface temperatures through a direct physical relationship that is rooted in their temperature-dependent solubility in water9,10. Dissolved noble gases are suitable tracers of LGM temperature because of their complete insensitivity to biological and chemical processes and the ubiquity of LGM-aged groundwater around the globe11,12. However, although several individual noble gas studies have found substantial tropical LGM cooling13-16, they have used different methodologies and provide limited spatial coverage. Here we use noble gases in groundwater to show that the low-altitude, low-to-mid-latitude land surface (45 degrees south to 35 degrees north) cooled by 5.8 ± 0.6 degrees Celsius (mean ± 95% confidence interval) during the LGM. Our analysis includes four decades of groundwater noble gas data from six continents, along with new records from the tropics, all of which were interpreted using the same physical framework. Our land-based result broadly supports a recent reconstruction based on marine proxy data assimilation1 that suggested greater climate sensitivity than previous estimates5-7.
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6
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Seltzer AM, Bekaert DV, Barry PH, Durkin KE, Mace EK, Aalseth CE, Zappala JC, Mueller P, Jurgens B, Kulongoski JT. Groundwater residence time estimates obscured by anthropogenic carbonate. SCIENCE ADVANCES 2021; 7:7/17/eabf3503. [PMID: 33883137 PMCID: PMC8059937 DOI: 10.1126/sciadv.abf3503] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Grants] [Track Full Text] [Download PDF] [Figures] [Subscribe] [Scholar Register] [Received: 10/20/2020] [Accepted: 03/03/2021] [Indexed: 06/12/2023]
Abstract
Groundwater is an important source of drinking and irrigation water. Dating groundwater informs its vulnerability to contamination and aids in calibrating flow models. Here, we report measurements of multiple age tracers (14C, 3H, 39Ar, and 85Kr) and parameters relevant to dissolved inorganic carbon (DIC) from 17 wells in California's San Joaquin Valley (SJV), an agricultural region that is heavily reliant on groundwater. We find evidence for a major mid-20th century shift in groundwater DIC input from mostly closed- to mostly open-system carbonate dissolution, which we suggest is driven by input of anthropogenic carbonate soil amendments. Crucially, enhanced open-system dissolution, in which DIC equilibrates with soil CO2, fundamentally affects the initial 14C activity of recently recharged groundwater. Conventional 14C dating of deeper SJV groundwater, assuming an open system, substantially overestimates residence time and thereby underestimates susceptibility to modern contamination. Because carbonate soil amendments are ubiquitous, other groundwater-reliant agricultural regions may be similarly affected.
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Affiliation(s)
- Alan M Seltzer
- Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA.
| | - David V Bekaert
- Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
| | - Peter H Barry
- Woods Hole Oceanographic Institution, Woods Hole, MA 02543, USA
| | - Kathryn E Durkin
- Scripps Institution of Oceanography, UC San Diego, La Jolla, CA 92037, USA
| | - Emily K Mace
- Pacific Northwest National Laboratory, Richland, WA 99354, USA
| | - Craig E Aalseth
- Pacific Northwest National Laboratory, Richland, WA 99354, USA
| | | | | | - Bryant Jurgens
- U.S. Geological Survey California Water Science Center, San Diego, CA 92101, USA
| | - Justin T Kulongoski
- Scripps Institution of Oceanography, UC San Diego, La Jolla, CA 92037, USA
- U.S. Geological Survey California Water Science Center, San Diego, CA 92101, USA
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