Arid
DOI10.1029/2018JG004496
Seasonal Bias in Soil Carbonate Formation and Its Implications for Interpreting High-Resolution Paleoarchives: Evidence From Southern Utah
Huth, T. E.1,2; Cerling, T. E.1; Marchetti, D. W.3; Bowling, D. R.4; Ellwein, A. L.5; Passey, B. H.2
通讯作者Huth, T. E.
来源期刊JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES
ISSN2169-8953
EISSN2169-8961
出版年2019
卷号124期号:3页码:616-632
英文摘要Pedogenic carbonate is commonly used as a paleoarchive, but its interpretation is limited by our understanding of its formation conditions. We investigated laminated soil carbonate rinds as a high-resolution paleoarchive in Torrey, Utah, USA, by characterizing and modeling their formation conditions. We compared late Holocene (<5ka) soil carbonate conventional (C and O) and clumped isotopes to modern soil environment and isotope measurements: soil CO2 partial pressure, soil temperature, soil moisture, delta C-13-soil CO2, delta O-18 precipitation, and delta O-18-soil water. Data unambiguously identified a strong summer seasonality bias, but modeling suggested soil carbonate formed several times throughout the year during infiltration events causing dissolution-formation reactions. This apparent discrepancy resulted from preferential preservation of calcite formed from the largest annual infiltration events (summer) overprinting previously formed calcite. Soil carbonate therefore formed predominantly due to changes in soil water content. As soil CO2 was at its annual maximum during soil carbonate formation, assuming uniformly low soil CO2 formation conditions for soil carbonate in estimating paleoatmospheric CO2 is likely not viable. Additionally, we showed modern summer delta C-13-soil CO2 and soil CO2 measurements could not produce a modeled delta C-13-soil carbonate consistent with late Holocene observations. We suggest using multiple lines of evidence to identify nonanalogous modern conditions. Finally, a nearly linear radiocarbon age model from a laminated rind showed that rinds can be used as a high-resolution paleoarchive if samples are from a single depth and the timing and conditions of soil carbonate formation can be constrained through time.
英文关键词pedogenic carbonate Colorado Plateau seasonality soil monitoring carbon isotopes oxygen isotopes
类型Article
语种英语
国家USA
开放获取类型Green Published, Bronze
收录类别SCI-E
WOS记录号WOS:000464653200012
WOS关键词CLUMPED ISOTOPE GEOTHERMOMETER ; PEDOGENIC CARBONATE ; FRACTIONATION ; TEMPERATURE ; CALIBRATION ; VEGETATION ; DYNAMICS ; CLIMATE ; DESERT ; BASIN
WOS类目Environmental Sciences ; Geosciences, Multidisciplinary
WOS研究方向Environmental Sciences & Ecology ; Geology
资源类型期刊论文
条目标识符http://119.78.100.177/qdio/handle/2XILL650/217081
作者单位1.Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA;
2.Univ Michigan, Dept Earth & Environm Sci, Ann Arbor, MI 48109 USA;
3.Western State Colorado Univ, Dept Nat & Environm Sci, Gunnison, CO USA;
4.Univ Utah, Dept Biol, Salt Lake City, UT 84112 USA;
5.Rocky Mt Biol Labs, Crested Butte, CO USA
推荐引用方式
GB/T 7714
Huth, T. E.,Cerling, T. E.,Marchetti, D. W.,et al. Seasonal Bias in Soil Carbonate Formation and Its Implications for Interpreting High-Resolution Paleoarchives: Evidence From Southern Utah[J],2019,124(3):616-632.
APA Huth, T. E.,Cerling, T. E.,Marchetti, D. W.,Bowling, D. R.,Ellwein, A. L.,&Passey, B. H..(2019).Seasonal Bias in Soil Carbonate Formation and Its Implications for Interpreting High-Resolution Paleoarchives: Evidence From Southern Utah.JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES,124(3),616-632.
MLA Huth, T. E.,et al."Seasonal Bias in Soil Carbonate Formation and Its Implications for Interpreting High-Resolution Paleoarchives: Evidence From Southern Utah".JOURNAL OF GEOPHYSICAL RESEARCH-BIOGEOSCIENCES 124.3(2019):616-632.
条目包含的文件
条目无相关文件。
个性服务
推荐该条目
保存到收藏夹
导出为Endnote文件
谷歌学术
谷歌学术中相似的文章
[Huth, T. E.]的文章
[Cerling, T. E.]的文章
[Marchetti, D. W.]的文章
百度学术
百度学术中相似的文章
[Huth, T. E.]的文章
[Cerling, T. E.]的文章
[Marchetti, D. W.]的文章
必应学术
必应学术中相似的文章
[Huth, T. E.]的文章
[Cerling, T. E.]的文章
[Marchetti, D. W.]的文章
相关权益政策
暂无数据
收藏/分享

除非特别说明,本系统中所有内容都受版权保护,并保留所有权利。