Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans

Liquid water has been known to occur beneath the Antarctic ice sheet for more than 40 years,but only recently have these subglacial aqueous environments been recognized as microbial ecosystems that may influence biogeochemical transformations on a global scale. Here we present the first geomicrobiol...

Full description

Bibliographic Details
Main Author: Priscu, John
Format: Dataset
Language:English
Published: SCAR - Microbial Antarctic Resource System 2015
Subjects:
Online Access:https://dx.doi.org/10.15468/8m7juf
http://www.gbif.org/dataset/836fe3e7-98f5-4c32-b661-8df8f575d7c0
id ftdatacite:10.15468/8m7juf
record_format openpolar
spelling ftdatacite:10.15468/8m7juf 2023-05-15T13:39:20+02:00 Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans Priscu, John 2015 https://dx.doi.org/10.15468/8m7juf http://www.gbif.org/dataset/836fe3e7-98f5-4c32-b661-8df8f575d7c0 en eng SCAR - Microbial Antarctic Resource System https://dx.doi.org/10.1038/nature13667 METADATA dataset Dataset 2015 ftdatacite https://doi.org/10.15468/8m7juf https://doi.org/10.1038/nature13667 2021-11-05T12:55:41Z Liquid water has been known to occur beneath the Antarctic ice sheet for more than 40 years,but only recently have these subglacial aqueous environments been recognized as microbial ecosystems that may influence biogeochemical transformations on a global scale. Here we present the first geomicrobiological description of water and surficial sediments obtained from direct sampling of a subglacial Antarctic lake. Subglacial Lake Whillans (SLW)lies beneath approximately 800m of ice on the lower portion of the Whillans Ice Stream (WIS) in West Antarctica and is part of an extensive and evolving subglacial drainage network. The water column of SLW contained metabolically active microorganisms and was derived primarily from glacial ice melt with solute sources from lithogenic weathering and a minor seawater component. Heterotrophic and autotrophic production data together with small subunit ribosomal RNA gene sequencing and biogeochemical data indicate that SLW is a chemosynthetically driven ecosystem inhabited by a diverse assemblage of bacteria and archaea. Our results confirm that aquatic environments beneath the Antarctic ice sheet support viable microbial ecosystems, corroborating previous reports suggesting that they contain globally relevant pools of carbon and microbes that can mobilize elements from the lithosphere and influence Southern Ocean geochemical and biological systems. Dataset Antarc* Antarctic Antarctica Ice Sheet Southern Ocean West Antarctica Whillans Ice Stream DataCite Metadata Store (German National Library of Science and Technology) Antarctic Southern Ocean The Antarctic West Antarctica Whillans ENVELOPE(-64.250,-64.250,-84.450,-84.450) Whillans Ice Stream ENVELOPE(-145.000,-145.000,-83.667,-83.667)
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Liquid water has been known to occur beneath the Antarctic ice sheet for more than 40 years,but only recently have these subglacial aqueous environments been recognized as microbial ecosystems that may influence biogeochemical transformations on a global scale. Here we present the first geomicrobiological description of water and surficial sediments obtained from direct sampling of a subglacial Antarctic lake. Subglacial Lake Whillans (SLW)lies beneath approximately 800m of ice on the lower portion of the Whillans Ice Stream (WIS) in West Antarctica and is part of an extensive and evolving subglacial drainage network. The water column of SLW contained metabolically active microorganisms and was derived primarily from glacial ice melt with solute sources from lithogenic weathering and a minor seawater component. Heterotrophic and autotrophic production data together with small subunit ribosomal RNA gene sequencing and biogeochemical data indicate that SLW is a chemosynthetically driven ecosystem inhabited by a diverse assemblage of bacteria and archaea. Our results confirm that aquatic environments beneath the Antarctic ice sheet support viable microbial ecosystems, corroborating previous reports suggesting that they contain globally relevant pools of carbon and microbes that can mobilize elements from the lithosphere and influence Southern Ocean geochemical and biological systems.
format Dataset
author Priscu, John
spellingShingle Priscu, John
Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
author_facet Priscu, John
author_sort Priscu, John
title Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
title_short Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
title_full Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
title_fullStr Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
title_full_unstemmed Geomicrobiology of Antarctic Subglacial Environments - Subglacial Lake Whillans
title_sort geomicrobiology of antarctic subglacial environments - subglacial lake whillans
publisher SCAR - Microbial Antarctic Resource System
publishDate 2015
url https://dx.doi.org/10.15468/8m7juf
http://www.gbif.org/dataset/836fe3e7-98f5-4c32-b661-8df8f575d7c0
long_lat ENVELOPE(-64.250,-64.250,-84.450,-84.450)
ENVELOPE(-145.000,-145.000,-83.667,-83.667)
geographic Antarctic
Southern Ocean
The Antarctic
West Antarctica
Whillans
Whillans Ice Stream
geographic_facet Antarctic
Southern Ocean
The Antarctic
West Antarctica
Whillans
Whillans Ice Stream
genre Antarc*
Antarctic
Antarctica
Ice Sheet
Southern Ocean
West Antarctica
Whillans Ice Stream
genre_facet Antarc*
Antarctic
Antarctica
Ice Sheet
Southern Ocean
West Antarctica
Whillans Ice Stream
op_relation https://dx.doi.org/10.1038/nature13667
op_doi https://doi.org/10.15468/8m7juf
https://doi.org/10.1038/nature13667
_version_ 1766117526157131776