Cited by 429Soil and Environmental StudiesGeology and Paleoclimatology ResearchGroundwater and Isotope Geochemistry

Seasonal bias in the formation and stable isotopic composition of pedogenic carbonate in modern soils from central New Mexico, USA

Breecker, D.O., Sharp, Z.D., McFadden, L.D.·2009·Geological Society of America Bulletin

Abstract

Research Article| March 01, 2009 Seasonal bias in the formation and stable isotopic composition of pedogenic carbonate in modern soils from central New Mexico, USA D.O. Breecker; D.O. Breecker † 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA †E-mail: breecker@email.arizona.edu; Now at the University of Arizona Search for other works by this author on: GSW Google Scholar Z.D. Sharp; Z.D. Sharp 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar L.D. McFadden L.D. McFadden 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Search for other works by this author on: GSW Google Scholar Author and Article Information D.O. Breecker † 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA Z.D. Sharp 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA L.D. McFadden 1Department of Earth and Planetary Sciences, University of New Mexico, Albuquerque, New Mexico 87131, USA †E-mail: breecker@email.arizona.edu; Now at the University of Arizona Publisher: Geological Society of America Received: 04 Feb 2008 Revision Received: 06 Sep 2008 Accepted: 09 Sep 2008 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 © 2009 Geological Society of America…

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Crossref · 10.1130/b26413.1

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  • Hydrous magnesium carbonates form at relatively similar elevations and effectively at the same distance from the Pacific Ocean, minimizing topographic and continental effects.

    “Hydrous magnesium carbonates form at relatively similar elevations (Table S3) and are effectively at the same distance from the Pacific Ocean (Fig. 1b), minimizing topographic and 'continental effects' (Poage and Chamberlain, 2001; Breecker et al., 2009; Mix et al., 2011; Winnick et al., 2014).”

    From Clumped-isotope thermometry of magnesium carbonates in ultramafic rocks (2016) · cites this paper as Breecker et al., 2009

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Authors
Breecker, D. O., Sharp, Z. D., & McFadden, L. D.
Affiliations
University of New Mexico (US)
Venue
Geological Society of America Bulletin
Published
2009-02-05
Volume
121
Issue
3-4
Pages
630-640
ISSN
  • 0016-7606 (ISSN-L)
  • 1943-2674
OpenAlex
W2146451541
Cited by
429
References
2
Citations by year
2026: 27 · 2025: 23 · 2024: 26 · 2023: 22 · 2022: 20 · 2021: 32 · 2020: 29 · 2019: 29 · 2018: 25 · 2017: 19 · 2016: 29 · 2015: 24 · 2014: 21 · 2013: 35 · 2012: 19
FWCI
37.89
Type
journal article
Language
en
Open access
closed
Locations
Geological Society of America Bulletin (publishedVersion)
Funders
National Science Foundation
Topics
  • Life Sciences › Agricultural and Biological Sciences › Soil Science › Soil and Environmental Studies
  • Physical Sciences › Earth and Planetary Sciences › Atmospheric Science › Geology and Paleoclimatology Research
  • Physical Sciences › Earth and Planetary Sciences › Geochemistry and Petrology › Groundwater and Isotope Geochemistry
Keywords
pedogenic carbonates, stable isotopes, seasonal variation, modern soils, central New Mexico, carbonate precipitation, soil chemistry, soil redox conditions, soil temperature, soil carbon sequestration

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