globalchange  > 过去全球变化的重建
DOI: 10.1016/j.quascirev.2017.02.016
Scopus记录号: 2-s2.0-85014212904
论文题名:
Relationships between fluvial evolution and karstification related to climatic, tectonic and eustatic forcing in temperate regions
作者: Harmand D.; Adamson K.; Rixhon G.; Jaillet S.; Losson B.; Devos A.; Hez G.; Calvet M.; Audra P.
刊名: Quaternary Science Reviews
ISSN: 2773791
出版年: 2017
卷: 166
起始页码: 38
结束页码: 56
语种: 英语
英文关键词: Aggradation ; Base level ; Cave level ; Cosmogenic nuclide dating ; Karst ; Phreatic cave ; Speleogenesis ; Valley incision
Scopus关键词: Catchments ; Caves ; Groundwater geochemistry ; Isotopes ; Numerical methods ; Runoff ; Sedimentology ; Sediments ; Aggradation ; Base level ; Cosmogenic nuclide dating ; Karst ; Phreatic ; Speleogenesis ; Valley incision ; Landforms
英文摘要: This paper reviews the diversity of relationships between river evolution and karstogenesis. It also underlines the fundamental role of numerical dating methods (e.g. cosmogenic nuclides) applied to sedimentary sequences in tiered cave passages as they have provided new insights into these complex interactions. Although karst terrain is widespread worldwide, we focus on European karst catchments, where the sedimentary records are especially well preserved. We review the recent dating of fluvial sediments and speleothems, to examine the timing of karstification, incision and deposition in cave levels. The most complete alluvial records occur in tectonically uplifted high mountains where some of the oldest sediment fills date to the Miocene. Evidence indicates that not only uplift, but also climatic conditions and fluvial dynamics (e.g. knickpoint retreat, increased channel flow and/or sediment load, and stream piracies) can play a major role in speleogenesis and geomorphological evolution. In evaporite rocks, speleogenesis is characterized by rapid dissolution and subsidence. In European catchments, gypsum cave development largely occurred during cold climate periods, while limestone caves formed during warm interglacial or interstadial phases. Our synthesis is used to propose four models of fluvial and karst evolution, and highlight perspectives for further research. © 2017 Elsevier Ltd
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资源类型: 期刊论文
标识符: http://119.78.100.158/handle/2HF3EXSE/59224
Appears in Collections:过去全球变化的重建

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作者单位: Laboratoire LOTERR, Université de Lorraine, Site Libération, BP 13387, Nancy, France; School of Science and the Environment, Manchester Metropolitan University, Manchester, United Kingdom; University of Cologne, Institute for Geography, Albertus-Magnus-Platz, Köln, Germany; Laboratoire EDYTEM, Université de Savoie, CNRS, Pôle Montagne, Le Bourget du Lac, France; Genenaa, 2 esplanade Roland Garros, REIMS, France; Université de Perpignan, Via Domitia, UMR 7194 HNHP, Perpignan Cedex, France; Polytech Nice - Sophia, Université de Nice - Sophia Antipolis, 930 route des Colles, Sophia-Antipolis, France

Recommended Citation:
Harmand D.,Adamson K.,Rixhon G.,et al. Relationships between fluvial evolution and karstification related to climatic, tectonic and eustatic forcing in temperate regions[J]. Quaternary Science Reviews,2017-01-01,166
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