A microbial driver of chemical weathering in glaciated systems

Glaciological processes under ice sheets provide sustainable ecosystems for microbes, forming an aquatic environment through basal melting, and providing nutrients and energy from bedrock. Microbes facilitate solute production in most Earth surface environments, but the balance of biotic and abiotic...

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Published in:Geology
Main Authors: Montross, Scott N., Skidmore, Mark, Tranter, Martyn, Kivimaki, Anna-Liisa, Parkes, Ronald
Format: Article in Journal/Newspaper
Language:English
Published: 2012
Subjects:
BED
Online Access:https://pure.au.dk/portal/da/publications/a-microbial-driver-of-chemical-weathering-in-glaciated-systems(5ce95098-81f5-4c17-b30c-060479f1c487).html
https://doi.org/10.1130/G33572.1
id ftuniaarhuspubl:oai:pure.atira.dk:publications/5ce95098-81f5-4c17-b30c-060479f1c487
record_format openpolar
spelling ftuniaarhuspubl:oai:pure.atira.dk:publications/5ce95098-81f5-4c17-b30c-060479f1c487 2023-08-27T04:05:03+02:00 A microbial driver of chemical weathering in glaciated systems Montross, Scott N. Skidmore, Mark Tranter, Martyn Kivimaki, Anna-Liisa Parkes, Ronald 2012-12-13 https://pure.au.dk/portal/da/publications/a-microbial-driver-of-chemical-weathering-in-glaciated-systems(5ce95098-81f5-4c17-b30c-060479f1c487).html https://doi.org/10.1130/G33572.1 eng eng info:eu-repo/semantics/restrictedAccess Montross , S N , Skidmore , M , Tranter , M , Kivimaki , A-L & Parkes , R 2012 , ' A microbial driver of chemical weathering in glaciated systems ' , Geology , vol. 41 , no. 2 , pp. 215-218 . https://doi.org/10.1130/G33572.1 ANTARCTIC SUBGLACIAL LAKES HIGH ARCTIC GLACIER ICE-SHEET BACTERIA WEST ENVIRONMENTS SEDIMENTS BENEATH BED SWITZERLAND article 2012 ftuniaarhuspubl https://doi.org/10.1130/G33572.1 2023-08-02T22:58:12Z Glaciological processes under ice sheets provide sustainable ecosystems for microbes, forming an aquatic environment through basal melting, and providing nutrients and energy from bedrock. Microbes facilitate solute production in most Earth surface environments, but the balance of biotic and abiotic weathering in subglacial environment is presently unknown. This study demonstrates an up to eightfold increase in dissolved major cations in biotic relative to abiotic weathering experiments using glacial sediments and meltwater. This conclusion greatly expands our view of Earth’s biogeochemically active weathering zone by incorporating the large wet-based portions of glaciated continents, both at present and during Earth’s history. The profound environmental signifi cance is that microbial processes have the ability to maintain terrestrial chemical weathering rates in cooling climates during glacial advance. Article in Journal/Newspaper Antarc* Antarctic Arctic Ice Sheet Aarhus University: Research Arctic Antarctic Geology 41 2 215 218
institution Open Polar
collection Aarhus University: Research
op_collection_id ftuniaarhuspubl
language English
topic ANTARCTIC SUBGLACIAL LAKES
HIGH ARCTIC GLACIER
ICE-SHEET
BACTERIA
WEST
ENVIRONMENTS
SEDIMENTS
BENEATH
BED
SWITZERLAND
spellingShingle ANTARCTIC SUBGLACIAL LAKES
HIGH ARCTIC GLACIER
ICE-SHEET
BACTERIA
WEST
ENVIRONMENTS
SEDIMENTS
BENEATH
BED
SWITZERLAND
Montross, Scott N.
Skidmore, Mark
Tranter, Martyn
Kivimaki, Anna-Liisa
Parkes, Ronald
A microbial driver of chemical weathering in glaciated systems
topic_facet ANTARCTIC SUBGLACIAL LAKES
HIGH ARCTIC GLACIER
ICE-SHEET
BACTERIA
WEST
ENVIRONMENTS
SEDIMENTS
BENEATH
BED
SWITZERLAND
description Glaciological processes under ice sheets provide sustainable ecosystems for microbes, forming an aquatic environment through basal melting, and providing nutrients and energy from bedrock. Microbes facilitate solute production in most Earth surface environments, but the balance of biotic and abiotic weathering in subglacial environment is presently unknown. This study demonstrates an up to eightfold increase in dissolved major cations in biotic relative to abiotic weathering experiments using glacial sediments and meltwater. This conclusion greatly expands our view of Earth’s biogeochemically active weathering zone by incorporating the large wet-based portions of glaciated continents, both at present and during Earth’s history. The profound environmental signifi cance is that microbial processes have the ability to maintain terrestrial chemical weathering rates in cooling climates during glacial advance.
format Article in Journal/Newspaper
author Montross, Scott N.
Skidmore, Mark
Tranter, Martyn
Kivimaki, Anna-Liisa
Parkes, Ronald
author_facet Montross, Scott N.
Skidmore, Mark
Tranter, Martyn
Kivimaki, Anna-Liisa
Parkes, Ronald
author_sort Montross, Scott N.
title A microbial driver of chemical weathering in glaciated systems
title_short A microbial driver of chemical weathering in glaciated systems
title_full A microbial driver of chemical weathering in glaciated systems
title_fullStr A microbial driver of chemical weathering in glaciated systems
title_full_unstemmed A microbial driver of chemical weathering in glaciated systems
title_sort microbial driver of chemical weathering in glaciated systems
publishDate 2012
url https://pure.au.dk/portal/da/publications/a-microbial-driver-of-chemical-weathering-in-glaciated-systems(5ce95098-81f5-4c17-b30c-060479f1c487).html
https://doi.org/10.1130/G33572.1
geographic Arctic
Antarctic
geographic_facet Arctic
Antarctic
genre Antarc*
Antarctic
Arctic
Ice Sheet
genre_facet Antarc*
Antarctic
Arctic
Ice Sheet
op_source Montross , S N , Skidmore , M , Tranter , M , Kivimaki , A-L & Parkes , R 2012 , ' A microbial driver of chemical weathering in glaciated systems ' , Geology , vol. 41 , no. 2 , pp. 215-218 . https://doi.org/10.1130/G33572.1
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1130/G33572.1
container_title Geology
container_volume 41
container_issue 2
container_start_page 215
op_container_end_page 218
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