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Animal emergence during Snowball Earths by thermosynthesis in submarine hydrothermal vents

Anthonie W. J. Muller¹

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1. Unversity of Amsterdam, Swammerdam Institute for Life Sciences

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Document Type:

Manuscript

Date:

Received 10 June 2009 14:08 UTC; Posted 17 June 2009

Subjects:

Developmental Biology, Evolutionary Biology

Tags:

• thermosynthesis
• origin of animals
• snowball earth

Abstract:

Darwin already commented on the lateness in the fossil record of the emergence of the animals, calling it a valid argument against his theory of evolution¹. This emergence of the animals (metazoans: multicellular animals) has therefore attracted much attention^2-5. Two decades ago it was reported that extensive global glaciations (Snowball Earths) preceded the emergence^6-7. Here we causally relate the emergence and the glaciations by invoking benthic sessile^8-11 thermosynthesizing^12-13 protists that gained free energy as ATP while oscillating in the thermal gradient between a submarine hydrothermal vent¹⁴ and the ice-covered ocean. During a global glaciation their size increased from microscopic to macroscopic due to the selective advantage of a larger span of the thermal gradient. At the glaciation’s end the ATP-generating mechanisms reversed and used ATP to sustain movement. Lastly, by functioning as animal organs, these protists then through symbiogenesis^15-17 brought forth the first animals. This simple and straightforward scenario for the emergence of animals accounts for their large organ and organism size and their use of ATP, embryo and epigenetic control of development. The scenario is extended to a general model for the emergence of biological movement¹⁸. The presented hypothesis is testable by collecting organisms near today’s submarine hydrothermal vents and studying their behaviour in the laboratory in easily constructed thermal gradients.

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License:

This document is licensed to the public under the Creative Commons Attribution 3.0 License

How to cite this document:

Muller, Anthonie. Animal emergence during Snowball Earths by thermosynthesis in submarine hydrothermal vents. Available from Nature Precedings <http://hdl.handle.net/10101/npre.2009.3333.1> (2009)

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Version number	Document title	Date
v2	Posted 19 June 2009

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