Timing, Duration, and Causes of Mass Extinctions
A special issue of Minerals (ISSN 2075-163X). This special issue belongs to the section "Mineral Geochemistry and Geochronology".
Deadline for manuscript submissions: closed (25 March 2022) | Viewed by 4764
Special Issue Editors
Interests: igneous, sedimentary, and petroleum geochemistry; geochronology; isotope geochemistry
Special Issue Information
Dear Colleagues,
The significance of mass extinctions for reconstructing the past, understanding the present, and preparing for future environmental change is of utmost interest throughout the sciences. Biological reductions characterizing mass extinctions in the sedimentary record often coincide with prominent geochemical variations in paleo-environments. Understanding the triggers and the global unfolding of mass extinctions requires the reconstruction of complex interactions and multiple feedbacks between organic and inorganic constituents in the lithosphere, hydrosphere, atmosphere, and biosphere. Just as importantly, we ask what processes are responsible for the Earth’s return to life-enhancing conditions. Geochemical signatures held in the rock record rarely provide unambiguous answers, but collectively, they form an increasing base of knowledge from which we can better understand both triggers and consequences associated with life-altering processes on Earth.
This dedicated Special Issue will address questions that probe dramatic geochemical changes on Earth leading to mass extinctions. We invite contributions focused on broad or specific aspects of geochemistry and geochronology of mass extinction events. We warmly welcome both seasoned scientists and newcomers to be part of this Special Issue and look forward to working together with you.
Dr. Svetoslav V. Georgiev
Prof. Dr. Holly J. Stein
Guest Editors
Manuscript Submission Information
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Keywords
- mass extinctions
- geochronology
- geochemistry
- elemental cycling
- stable isotopes
- large igneous provinces (LIPS)
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