DOI: 10.1016/j.epsl.2018.07.029
Scopus记录号: 2-s2.0-85051007116
论文题名: Obliquity pacing of the hydrological cycle during the Oceanic Anoxic Event 2
作者: Charbonnier G. ; Boulila S. ; Spangenberg J.E. ; Adatte T. ; Föllmi K.B. ; Laskar J.
刊名: Earth and Planetary Science Letters
ISSN: 0012821X
出版年: 2018
卷: 499 起始页码: 266
结束页码: 277
语种: 英语
英文关键词: continental weathering
; hydrological cycle
; OAE2
; obliquity forcing
; s3–s6 orbital timescale
Scopus关键词: Climatology
; Greenhouse gases
; Isotopes
; Magnetic susceptibility
; Organic carbon
; Sedimentology
; Weathering
; Climate oscillation
; Environmental change
; Hydrological cycles
; OAE2
; obliquity forcing
; Oceanic anoxic event 2
; Time-scales
; Ultrahigh resolution
; Time series analysis
; carbon isotope
; chemical weathering
; geological record
; greenhouse gas
; hydrological cycle
; Mesozoic
; obliquity
; paleohydrology
; proxy climate record
; timescale
; Western Interior
英文摘要: The Oceanic Anoxic Event 2 (OAE2, ca. ∼93.5 Ma) represents a major phase of environmental change during the Mesozoic, and is associated with a pronounced positive excursion in the carbon-isotope record. Short-term climate oscillations within the OAE2 are recorded as Milankovitch cycles, which have been used to establish a precise temporal framework for the OAE2. However, few studies discuss the sedimentary expression of Milankovitch cycles during the OAE2, and its paleoenvironmental implications. Here we present carbonate and organic-carbon isotope data from a biostratigraphically well-dated, organic-rich OAE2 interval in a sedimentary succession outcropping in the Briançonnais Domain at Roter Sattel (Fribourg Prealps, Switzerland). We sampled the OAE2 interval (4.28 m) for proxies of detrital sediment quantification (Al, Ti, magnetic susceptibility) at ultra-high resolution (1 cm). Time-series analysis of multiple detrital proxies permits the construction of an orbital timescale for the OAE2 based, for the first time, on the stable 173 kyr (s3–s6) obliquity modulation cycle. The resulting OAE2 orbital timescale at Roter Sattel is consistent with previous timescales obtained in the Western Interior Basin, and in southern Tibet (China). Our cyclostratigraphic results show an unusually strong obliquity signal during the initiation of OAE2. Previous studies have demonstrated that the onset of OAE2 was associated with magmatic pulses coupled with increases in atmospheric pCO2, followed by an overall, gradual drawdown of CO2. Accordingly, we suggest that detrital input during the OAE2 was the result of intensified continental weathering related to magmatic activity, the substantially release of greenhouse gases, and an accelerated hydrological cycle modulated by obliquity cycles. © 2018 Elsevier B.V. Citation statistics:
资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/109725
Appears in Collections: 影响、适应和脆弱性 气候变化事实与影响
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作者单位: Institute of Earth Sciences, University of Lausanne, Géopolis, Lausanne, CH-1015, Switzerland; Sorbonne Université, CNRS-INSU, Institut des Sciences de la Terre Paris, ISTeP UMR 7193, Paris, F-75005, France; ASD, IMCCE-CNRS UMR 8028, Observatoire de Paris, PSL Research University, Sorbonne Université, 77 avenue Denfert-Rochereau, Paris, 75014, France; Institute of Earth Surface Dynamics, University of Lausanne, Géopolis, Lausanne, CH-1015, Switzerland
Recommended Citation:
Charbonnier G.,Boulila S.,Spangenberg J.E.,et al. Obliquity pacing of the hydrological cycle during the Oceanic Anoxic Event 2[J]. Earth and Planetary Science Letters,2018-01-01,499