globalchange  > 气候减缓与适应
DOI: 10.1016/j.quascirev.2018.05.039
Scopus记录号: 2-s2.0-85048307883
论文题名:
Evidence for solar influence in a Holocene speleothem record (Père Noël cave, SE Belgium)
作者: Allan M.; Deliège A.; Verheyden S.; Nicolay S.; Quinif Y.; Fagel N.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2018
卷: 192
起始页码: 249
结束页码: 262
语种: 英语
英文关键词: Cold winter events ; Holocene ; NAO ; Paleoclimate time-series ; Solar forcing ; Speleothems ; Trace elements ; Wavelet analysis
Scopus关键词: Caves ; Climate change ; Inductively coupled plasma mass spectrometry ; Laser ablation ; Spectrum analysis ; Time series ; Time series analysis ; Wavelet analysis ; Wavelet transforms ; Cold winter ; Holocenes ; Paleoclimates ; Solar forcing ; Speleothems ; Trace elements ; climate variation ; dating method ; Holocene ; paleoclimate ; proxy climate record ; spatial resolution ; spectral analysis ; speleothem ; time series analysis ; trace element ; wavelet analysis ; winter ; Belgium
英文摘要: We present a decadal-centennial scale Holocene climate record based on trace elements contents from a 65 cm stalagmite from Belgian Père Noël cave. “Père Noël” (PN) stalagmite covers the last 12.7 ka according to U/Th dating. High spatial resolution measurements of trace elements (Sr, Ba and Mg) were done by Laser-Ablation Inductively Coupled Plasma Mass Spectrometry (LA-ICP-MS). Trace elements profiles were interpreted as environmental and climate changes in the Han-sur-Lesse region. Power spectrum estimators and continuous wavelet transform were applied on trace elements time series to detect any statistically significant periodicities in the PN stalagmite. Spectral analyses reveal decadal to millennial periodicities (i.e., 68–75, 133–136, 198–209, 291–358, 404–602, 912–1029 and 2365–2670 yr) in the speleothem record. Results were compared to reconstructed sunspot number data to determine whether solar signal is presents in PN speleothem. The occurrence of significant solar periodicities (i.e., cycles of Gleissberg, de Vries, unnamed 500 years, Eddy and Hallstatt) supports for an impact of solar forcing on PN speleothem trace element contents. Moreover, several intervals of significant rapid winter change were detected during the Holocene at 10.3, 9.3–9.5, around 8.2, 6.4–6.2, 4.7–4.5, and around 2.7 ka BP. Those intervals are similar to the cold winter events evidenced in different natural paleoclimate archives, suggesting common climate forcing mechanisms related to changes in solar irradiance. © 2018 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/112133
Appears in Collections:气候减缓与适应

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作者单位: AGEs, Département de Géologie, Université de Liège, Quartier Agora, 14 Allée du 6 Août, Liège, B-4000, Belgium; Institut de Mathématique, Université de Liège, Allée de la Découverte 12, Liège, B37 B-4000, Belgium; Politique scientifique fédérale, 231 Avenue Louise, Bruxelles, Brussels, 1000, Belgium; Université de Mons, Rue de Houdain 9, Mons, B-7000, Belgium

Recommended Citation:
Allan M.,Deliège A.,Verheyden S.,et al. Evidence for solar influence in a Holocene speleothem record (Père Noël cave, SE Belgium)[J]. Quaternary Science Reviews,2018-01-01,192
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