Biolocomotion and Premelting in Ice

Biota are found in glaciers, ice sheets and permafrost. Ice bound micro-organisms evolve in a complex mobile environment facilitated or hindered by a range of bulk and surface interactions. When a particle is embedded in a host solid near its bulk melting temperature, a melted film forms at the surf...

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Published in:Frontiers in Physics
Main Authors: Vachier, Jérémy, Wettlaufer, John S.
Format: Article in Journal/Newspaper
Language:unknown
Published: Frontiers Media SA 2022
Subjects:
Ice
Online Access:http://dx.doi.org/10.3389/fphy.2022.904836
https://www.frontiersin.org/articles/10.3389/fphy.2022.904836/full
id crfrontiers:10.3389/fphy.2022.904836
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spelling crfrontiers:10.3389/fphy.2022.904836 2024-03-03T08:45:17+00:00 Biolocomotion and Premelting in Ice Vachier, Jérémy Wettlaufer, John S. 2022 http://dx.doi.org/10.3389/fphy.2022.904836 https://www.frontiersin.org/articles/10.3389/fphy.2022.904836/full unknown Frontiers Media SA https://creativecommons.org/licenses/by/4.0/ Frontiers in Physics volume 10 ISSN 2296-424X Physical and Theoretical Chemistry General Physics and Astronomy Mathematical Physics Materials Science (miscellaneous) Biophysics journal-article 2022 crfrontiers https://doi.org/10.3389/fphy.2022.904836 2024-02-03T23:18:01Z Biota are found in glaciers, ice sheets and permafrost. Ice bound micro-organisms evolve in a complex mobile environment facilitated or hindered by a range of bulk and surface interactions. When a particle is embedded in a host solid near its bulk melting temperature, a melted film forms at the surface of the particle in a process known as interfacial premelting. Under a temperature gradient, the particle is driven by a thermomolecular pressure gradient toward regions of higher temperatures in a process called thermal regelation. When the host solid is ice and the particles are biota, thriving in their environment requires the development of strategies, such as producing exopolymeric substances (EPS) and antifreeze glycoproteins (AFP) that enhance the interfacial water. Therefore, thermal regelation is enhanced and modified by a process we term bio-enhanced premelting . Additionally, the motion of bioparticles is influenced by chemical gradients influenced by nutrients within the icy host body. We show how the overall trajectory of bioparticles is controlled by a competition between thermal regelation and directed biolocomotion. By re-casting this class of regelation phenomena in the stochastic framework of active Ornstein-Uhlenbeck dynamics, and using multiple scales analysis, we find that for an attractive (repulsive) nutrient source, that thermal regelation is enhanced (suppressed) by biolocomotion. This phenomena is important in astrobiology, the biosignatures of extremophiles and in terrestrial paleoclimatology. Article in Journal/Newspaper Ice permafrost Frontiers (Publisher) Frontiers in Physics 10
institution Open Polar
collection Frontiers (Publisher)
op_collection_id crfrontiers
language unknown
topic Physical and Theoretical Chemistry
General Physics and Astronomy
Mathematical Physics
Materials Science (miscellaneous)
Biophysics
spellingShingle Physical and Theoretical Chemistry
General Physics and Astronomy
Mathematical Physics
Materials Science (miscellaneous)
Biophysics
Vachier, Jérémy
Wettlaufer, John S.
Biolocomotion and Premelting in Ice
topic_facet Physical and Theoretical Chemistry
General Physics and Astronomy
Mathematical Physics
Materials Science (miscellaneous)
Biophysics
description Biota are found in glaciers, ice sheets and permafrost. Ice bound micro-organisms evolve in a complex mobile environment facilitated or hindered by a range of bulk and surface interactions. When a particle is embedded in a host solid near its bulk melting temperature, a melted film forms at the surface of the particle in a process known as interfacial premelting. Under a temperature gradient, the particle is driven by a thermomolecular pressure gradient toward regions of higher temperatures in a process called thermal regelation. When the host solid is ice and the particles are biota, thriving in their environment requires the development of strategies, such as producing exopolymeric substances (EPS) and antifreeze glycoproteins (AFP) that enhance the interfacial water. Therefore, thermal regelation is enhanced and modified by a process we term bio-enhanced premelting . Additionally, the motion of bioparticles is influenced by chemical gradients influenced by nutrients within the icy host body. We show how the overall trajectory of bioparticles is controlled by a competition between thermal regelation and directed biolocomotion. By re-casting this class of regelation phenomena in the stochastic framework of active Ornstein-Uhlenbeck dynamics, and using multiple scales analysis, we find that for an attractive (repulsive) nutrient source, that thermal regelation is enhanced (suppressed) by biolocomotion. This phenomena is important in astrobiology, the biosignatures of extremophiles and in terrestrial paleoclimatology.
format Article in Journal/Newspaper
author Vachier, Jérémy
Wettlaufer, John S.
author_facet Vachier, Jérémy
Wettlaufer, John S.
author_sort Vachier, Jérémy
title Biolocomotion and Premelting in Ice
title_short Biolocomotion and Premelting in Ice
title_full Biolocomotion and Premelting in Ice
title_fullStr Biolocomotion and Premelting in Ice
title_full_unstemmed Biolocomotion and Premelting in Ice
title_sort biolocomotion and premelting in ice
publisher Frontiers Media SA
publishDate 2022
url http://dx.doi.org/10.3389/fphy.2022.904836
https://www.frontiersin.org/articles/10.3389/fphy.2022.904836/full
genre Ice
permafrost
genre_facet Ice
permafrost
op_source Frontiers in Physics
volume 10
ISSN 2296-424X
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3389/fphy.2022.904836
container_title Frontiers in Physics
container_volume 10
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