Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils

This data-set contains nucleotide sequences associated with the following described study. In this study, C-fixation rates measured in the bulk arid soils (<5% moisture) ranged from below detection limits to ~12 nmol C/cc/h. Rates in ephemerally wet soils ranged from ~20 to 750 nmol C/cc/h, equat...

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Bibliographic Details
Main Authors: University of Delaware, Thomas Niederberger
Format: Dataset
Language:unknown
Published: Knowledge Network for Biocomplexity 2015
Subjects:
Online Access:https://search.dataone.org/view/knb.756.1
id dataone:knb.756.1
record_format openpolar
spelling dataone:knb.756.1 2023-11-08T14:14:08+01:00 Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils University of Delaware Thomas Niederberger Samples for this study were collected from the Miers Valley region of Antarctica. Miers Valley is located at the southern region of the McMurdo Dry Valleys in Victoria Land and has two glaciers located at the upper (west) end of the valley: Miers Glacier is situated at the northern side and Adams Glacier on the southern side of the Valley. During the summer months, meltwater streams from both glaciers flow into the permanently ice-covered Lake Miers. A number of hyporheic zones and wetted lake boundaries as were sampled along transects during 2 sampling expeditions in 2009. ENVELOPE(163.7469,163.7469,-78.0956,-78.0956) BEGINDATE: 2009-01-01T00:00:00Z ENDDATE: 2009-12-01T00:00:00Z 2015-07-20T00:00:00Z https://search.dataone.org/view/knb.756.1 unknown Knowledge Network for Biocomplexity Antarctica Dry Valley Dataset 2015 dataone:urn:node:KNB 2023-11-08T13:37:37Z This data-set contains nucleotide sequences associated with the following described study. In this study, C-fixation rates measured in the bulk arid soils (<5% moisture) ranged from below detection limits to ~12 nmol C/cc/h. Rates in ephemerally wet soils ranged from ~20 to 750 nmol C/cc/h, equating to turnover rates of ~7 days to 140 days, with lower rates in stream-associated soils as compared to lake-associated soils. Analysis of the gene encoding the large subunit of RuBisCO (cbbL) in these soils identified green-type sequences dominated by the 1B cyanobacterial-related phylotype in both arid and wet soils including the RNA fraction of the wet soil. Red-type cbbL genes were dominated by 1C actinobacterial-related phylotypes in arid soils, with wetted soils containing nearly equal proportions of 1C (actinobacterial and proteobacterial signatures) and 1D (algal) related phylotypes. Complementary 16S rRNA and 18S rRNA gene sequencing also revealed distinct differences in community structure between biotopes. This study is the first of its kind to examine C-fixation rates in Dry Valley soils and the microorganisms potentially responsible for these activities. Dataset Adams Glacier Antarc* Antarctic Antarctica McMurdo Dry Valleys Victoria Land Knowledge Network for Biocomplexity (via DataONE) Antarctic Victoria Land McMurdo Dry Valleys Miers ENVELOPE(163.850,163.850,-78.100,-78.100) Miers Valley ENVELOPE(164.200,164.200,-78.100,-78.100) Adams Glacier ENVELOPE(-74.412,-74.412,81.630,81.630) Lake Miers ENVELOPE(-60.450,-60.450,-62.717,-62.717) Miers Glacier ENVELOPE(163.667,163.667,-78.083,-78.083) ENVELOPE(163.7469,163.7469,-78.0956,-78.0956)
institution Open Polar
collection Knowledge Network for Biocomplexity (via DataONE)
op_collection_id dataone:urn:node:KNB
language unknown
topic Antarctica
Dry Valley
spellingShingle Antarctica
Dry Valley
University of Delaware
Thomas Niederberger
Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
topic_facet Antarctica
Dry Valley
description This data-set contains nucleotide sequences associated with the following described study. In this study, C-fixation rates measured in the bulk arid soils (<5% moisture) ranged from below detection limits to ~12 nmol C/cc/h. Rates in ephemerally wet soils ranged from ~20 to 750 nmol C/cc/h, equating to turnover rates of ~7 days to 140 days, with lower rates in stream-associated soils as compared to lake-associated soils. Analysis of the gene encoding the large subunit of RuBisCO (cbbL) in these soils identified green-type sequences dominated by the 1B cyanobacterial-related phylotype in both arid and wet soils including the RNA fraction of the wet soil. Red-type cbbL genes were dominated by 1C actinobacterial-related phylotypes in arid soils, with wetted soils containing nearly equal proportions of 1C (actinobacterial and proteobacterial signatures) and 1D (algal) related phylotypes. Complementary 16S rRNA and 18S rRNA gene sequencing also revealed distinct differences in community structure between biotopes. This study is the first of its kind to examine C-fixation rates in Dry Valley soils and the microorganisms potentially responsible for these activities.
format Dataset
author University of Delaware
Thomas Niederberger
author_facet University of Delaware
Thomas Niederberger
author_sort University of Delaware
title Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
title_short Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
title_full Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
title_fullStr Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
title_full_unstemmed Carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet Antarctic Dry Valley soils
title_sort carbon-fixation rates and associated microbial communities residing in arid and ephemerally wet antarctic dry valley soils
publisher Knowledge Network for Biocomplexity
publishDate 2015
url https://search.dataone.org/view/knb.756.1
op_coverage Samples for this study were collected from the Miers Valley region of Antarctica. Miers Valley is located at the southern region of the McMurdo Dry Valleys in Victoria Land and has two glaciers located at the upper (west) end of the valley: Miers Glacier is situated at the northern side and Adams Glacier on the southern side of the Valley. During the summer months, meltwater streams from both glaciers flow into the permanently ice-covered Lake Miers. A number of hyporheic zones and wetted lake boundaries as were sampled along transects during 2 sampling expeditions in 2009.
ENVELOPE(163.7469,163.7469,-78.0956,-78.0956)
BEGINDATE: 2009-01-01T00:00:00Z ENDDATE: 2009-12-01T00:00:00Z
long_lat ENVELOPE(163.850,163.850,-78.100,-78.100)
ENVELOPE(164.200,164.200,-78.100,-78.100)
ENVELOPE(-74.412,-74.412,81.630,81.630)
ENVELOPE(-60.450,-60.450,-62.717,-62.717)
ENVELOPE(163.667,163.667,-78.083,-78.083)
ENVELOPE(163.7469,163.7469,-78.0956,-78.0956)
geographic Antarctic
Victoria Land
McMurdo Dry Valleys
Miers
Miers Valley
Adams Glacier
Lake Miers
Miers Glacier
geographic_facet Antarctic
Victoria Land
McMurdo Dry Valleys
Miers
Miers Valley
Adams Glacier
Lake Miers
Miers Glacier
genre Adams Glacier
Antarc*
Antarctic
Antarctica
McMurdo Dry Valleys
Victoria Land
genre_facet Adams Glacier
Antarc*
Antarctic
Antarctica
McMurdo Dry Valleys
Victoria Land
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