Location: University of Iceland, Reykjavik, Iceland
Web: http://www.iavcei.org/IAVCEI.htm
Includes the following sessions:
Mantle plumes and plume-ridge interactions
Convenors: B. Bransdóttir (bryndis@raunvis.hi.is), R. Trønnes (r.g.tronnes@nhm.uio.no)
This session is dedicated to geodynamic issues, including mantle convection, the origin and evolution of plumes, mantle melting, melt transport and along-axis melt variability. We seek contributions from all areas of research on mantle plumes, plate-spreading, V-shaped ridges, seamounts, large igneous provinces and orogenic episodes.
This session will focus on:
Intraplate volcanism – continents and oceans, from scoria cones to large igneous provinces
Convenors: G. Valentine (gav4@buffalo.edu), A. Kerr (kerra@cardiff.ac.uk)
Intraplate volcanism provides key insights into magma sources and magmatic processes. This volcanism encompasses a wide array of eruptive styles and products, and, on the continents, is an important component of volcanic risk in some areas. This session will combine both the continental and ocean floor perspectives on the nature of ancient and modern intraplate volcanic activity, from source through eruption, on a wide range of scales from small localised eruptions to large igneous provinces.
This session will focus on:
Frontiers in large igneous provinces research
Convenors: I. Campbell (ian.campbell@anu.edu.au), R. Ernst (richard.ernst@ernstgeosciences.com)
Over the last fifteen years it has become widely accepted that Large Igneous Provinces (LIPs) are produced by melting mantle plumes. However the link between LIPs and mantle plumes has recently been challenged. How confident are we that LIPs are produced by mantle plumes? Are there any aspects of LIPs that cannot be explained by the plume theory? Are there viable alternative hypotheses? Are there some LIPs that are better explained by alternative models?
This session will focus on:
Construction of large igneous provinces and mass extinctions
Convenors: A. Saunders (ads@le.ac.uk), T. Thordarson (thor.thordarson@ed.ac.uk), P. Wignall (p.wignall@see.leeds.ac.uk), S. Self (stephen.self@open.ac.uk), A. Harris (harris@higp.hawaii.edu)
Mass extinctions are global phenomena that represent some of the most dramatic events in the geological history and arguably no events have had more influence on evolution of life on Earth. They are generally thought to have lasted for <1 Myrs and the fact that they define all of our key geological boundaries is the best testimony of their significance. Despite ample research cause of mass extinctions is still one of the great outstanding questions in Geosciences. The synchronicity of mass extinctions and LIP volcanism in the Mesozoic and the Cenozoic has led many to postulate a causal link between the two events. However, the mechanism by which LIP volcanism may have induced mass extinctions is still unclear and strongly debated. In this session we like to focus on the questions:
Did LIP emplacement lead to dramatic environmental change?
Can LIP volcanism trigger mass extinctions and, if so, how?
The aim is to bring together research that sheds light on the potential climatic and environmental impacts of flood basalt volcanism and their link to mass extinctions via studies of LIP-related stratigraphy as well as shallow subsurface and surface processes involved in construction of LIPs.
The session will focus on: