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...
Published in: | Geology |
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Language: | English |
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2012
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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 |
_version_ |
1775355574457729024 |