T227 The Co-Evolution of Phanerozoic Climate, Landscapes, and Terrestrial Ecosystems II

Thursday, 29 October 2020
5:30 PM - 8:00 PM
Meeting Rooms

BIOGEODYNAMICS: A NEW TRANSDISCIPLINARY FIELD

Paper number: T227-6
Program: Technical Sessions
Time: 6:35 PM – 6:50 PM

Authors

Abstract

Geodynamic evolution of Earth’s mantle and lithosphere is tied to the evolution of its atmosphere, oceans, landscape and life and we would like to understand these interactions better through the emerging transdisciplinary field of biogeodynamics. The solid Earth is a high-energy, far-from equilibrium system, with 1000°s C temperature differences between interior and exterior; multiple tectono-magmatic styles likely happened over its geological history. The influences of any global tectono-magmatic style on the biosphere are at least twofold. First, life is sustained by a critical set of elements contained within rock, ocean and atmosphere reservoirs and cycled between Earth’s surface and interior via tectonic, magmatic and surface processes. Second, plate tectonics redistributes continents, grows mountain ranges, forms land bridges, and opens and closes oceans, providing environmental pressures that isolate and stimulate populations to adapt and evolve; recombining these features further stimulates evolution. In the context of biogeodynamics, modern-style plate tectonics established sometime before the Cambrian explosion is a strong promoter of biological evolution. Compared to single lid tectonic styles, plate tectonics better supplies nutrients and modulates climate, and exerts continuous moderate environmental pressures that drive evolution without being capable of extinguishing all life. Both nutrients and tectonics aspects thus suggest that a planet with oceans, continents, and modern-style plate tectonics maximizes opportunities for speciation and natural selection, whereas a similar planet without plate tectonics provides fewer such opportunities. Importantly, long timescales of biological evolution estimated from analysis of DNA changes and fossils are comparable to those of major geodynamic cycles such as the Wilson Cycle. This similarity creates a natural possibility for investigating coupling of lithospheric and mantle processes with life evolution by using novel hybrid bio-geodynamical numerical models.

The International Lithosphere Program has approved our proposal to establish a Task Force for 2021-2025 “Bio-geodynamics of the Lithosphere” to move this science forward. Please visit our website to follow developments in this field – google “ETH Biogeodynamics”

Geological Society of America Abstracts with Programs. Vol. 52, No. 6

doi: 10.1130/abs/2020AM-354293

© Copyright 2020 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.