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DOI | 10.1016/j.epsl.2020.116327 |
A lake sediment stable isotope record of late-middle to late Holocene hydroclimate variability in the western Guatemala highlands | |
Stansell N.D.; Steinman B.A.; Lachniet M.S.; Feller J.; Harvey W.; Fernandez A.; Shea C.J.; Price B.; Coenen J.; Boes M.; Perdziola S. | |
发表日期 | 2020 |
ISSN | 0012821X |
卷号 | 542 |
英文摘要 | Long-term perspectives on past hydroclimate variability provide context for evaluating the potential future impacts of changes in Northern Hemisphere temperatures and oceanic-atmospheric circulation on the timing and distribution of precipitation in Central America. Here we use the isotopic composition of fine-grained (< 63 μm), endogenic CaCO3 (δ18Ocalcite and δ13Ccalcite) from Lake Kail, located in the western highlands of Guatemala, to infer multi-decadal to multi-centennial-scale variability in the balance between precipitation and evaporation (P/E) over the last ∼6000 years. The sediment age model is based on 210Pb and 41 14C ages, with chronological uncertainty estimated using Bayesian methods. A model that couples lake hydrology and isotope mass balance is applied to characterize the isotopic responses of lake water and calcite to changes in drought-controlling climate variables such as precipitation, temperature and relative humidity. The δ18Ocalcite variations indicate intermediate-to-dry P/E conditions during the late-middle Holocene from ∼6000 to ∼4100 cal yr BP. There was then a shift to drier conditions at the start of the late Holocene until ∼3050 cal yr BP, followed by a trend to wetter conditions until ∼1500 cal yr BP. The most recent ∼1500 years is characterized by high and relatively stable P/E, with particularly wet intervals from ∼1500 to 1170 cal yr BP and from 470 to 260 cal yr BP. Comparisons of the Lake Kail δ18Ocalcite record with Central American/circum-Caribbean proxy datasets spanning the late-middle and late Holocene indicate northern tropical hydroclimate changes were highly variable across space and time and were likely driven by regional oceanic-atmospheric responses with a secondary influence by insolation forcing. © 2020 Elsevier B.V. |
关键词 | Central Americainsolationnorthern tropicsoxygen isotopesprecipitation |
英文关键词 | Atmospheric humidity; Bayesian networks; Calcite; Calcium carbonate; Climate models; Humidity control; Isotopes; Uncertainty analysis; Atmospheric circulation; Atmospheric response; Centennial scale variability; Isotopic composition; Long-term perspective; Northern Hemispheres; Secondary influences; Temperature and relative humidity; Lakes; air temperature; atmospheric circulation; climate effect; climate variation; decadal variation; evaporation; Holocene; isotopic composition; lacustrine deposit; Northern Hemisphere; oceanic circulation; precipitation (climatology); sediment chemistry; stable isotope; Guatemala [Central America] |
语种 | 英语 |
来源期刊 | Earth and Planetary Science Letters |
文献类型 | 期刊论文 |
条目标识符 | http://gcip.llas.ac.cn/handle/2XKMVOVA/202904 |
作者单位 | Department of Geology and Environmental Geosciences, Northern Illinois University, United States; Large Lakes Observatory, Department of Earth and Environmental Sciences, University of Minnesota Duluth, Duluth, United States; Department of Geoscience, University of Nevada, Las Vegas, United States; Department of Zoology, University of Oxford, Oxford, United Kingdom |
推荐引用方式 GB/T 7714 | Stansell N.D.,Steinman B.A.,Lachniet M.S.,et al. A lake sediment stable isotope record of late-middle to late Holocene hydroclimate variability in the western Guatemala highlands[J],2020,542. |
APA | Stansell N.D..,Steinman B.A..,Lachniet M.S..,Feller J..,Harvey W..,...&Perdziola S..(2020).A lake sediment stable isotope record of late-middle to late Holocene hydroclimate variability in the western Guatemala highlands.Earth and Planetary Science Letters,542. |
MLA | Stansell N.D.,et al."A lake sediment stable isotope record of late-middle to late Holocene hydroclimate variability in the western Guatemala highlands".Earth and Planetary Science Letters 542(2020). |
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