Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River

Lateral bays of the lower Columbia River estuary are areas of enhanced water retention that influence net ecosystem metabolism through activities of their diverse microbial communities. Metagenomic characterization of sediment microbiota from three disparate sites in two brackish lateral bays (Baker...

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Main Authors: Mariya W Smith, Richard E Davis, Nicholas D Youngblut, Tuomas eKärnä, Lydie eHerfort, Rachel J Whitaker, William W Metcalf, Bradley M. Tebo, Antonio M Baptista, Holly M Simon
Format: Article
Language:English
Published: Frontiers Media S.A. 2015-10-01
Series:Frontiers in Microbiology
Subjects:
Online Access:http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.01074/full
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spelling doaj-164f2f098fb94674a9808787dc6d02682020-11-25T00:59:01ZengFrontiers Media S.A.Frontiers in Microbiology1664-302X2015-10-01610.3389/fmicb.2015.01074152332Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia RiverMariya W Smith0Richard E Davis1Nicholas D Youngblut2Tuomas eKärnä3Lydie eHerfort4Rachel J Whitaker5William W Metcalf6Bradley M. Tebo7Antonio M Baptista8Holly M Simon9Oregon Health and Science UniversityOregon Health and Science UniversityCornell UniversityOregon Health and Science UniversityOregon Health and Science UniversityUniversity of Illinois at Urbana-ChampaignUniversity of Illinois at Urbana-ChampaignOregon Health and Science UniversityOregon Health and Science UniversityOregon Health and Science UniversityLateral bays of the lower Columbia River estuary are areas of enhanced water retention that influence net ecosystem metabolism through activities of their diverse microbial communities. Metagenomic characterization of sediment microbiota from three disparate sites in two brackish lateral bays (Baker and Youngs) produced approximately 100 Gbp of DNA sequence data analyzed subsequently for predicted SSU rRNA and peptide-coding genes. The metagenomes were dominated by Bacteria. A large component of Eukaryota was present in Youngs Bay samples, i.e. the inner bay sediment was enriched with the invasive New Zealand mudsnail, Potamopyrgus antipodarum, known for high ammonia production. The metagenome was also highly enriched with an archaeal ammonia oxidizer closely related to Nitrosoarchaeum limnia. Combined analysis of sequences and continuous, high-resolution time series of biogeochemical data from fixed and mobile platforms revealed the importance of large-scale reciprocal particle exchanges between the mainstem estuarine water column and lateral bay sediments. Deposition of marine diatom particles in sediments near Youngs Bay mouth was associated with a dramatic enrichment of Bacteroidetes (58% of total Bacteria) and corresponding genes involved in phytoplankton polysaccharide degradation. The Baker Bay sediment metagenome contained abundant Archaea, including diverse methanogens, as well as functional genes for methylotrophy and taxonomic markers for syntrophic bacteria, suggesting that active methane cycling occurs at this location. Our previous work showed enrichments of similar anaerobic taxa in particulate matter of the mainstem estuarine water column. In total, our results identify the lateral bays as both sources and sinks of biogenic particles significantly impacting microbial community composition and biogeochemical activities in the estuary.http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.01074/fullammonia oxidationmethane cyclingmetagenome analysisParticle exchangeColumbia River Estuarylateral bay sediments
collection DOAJ
language English
format Article
sources DOAJ
author Mariya W Smith
Richard E Davis
Nicholas D Youngblut
Tuomas eKärnä
Lydie eHerfort
Rachel J Whitaker
William W Metcalf
Bradley M. Tebo
Antonio M Baptista
Holly M Simon
spellingShingle Mariya W Smith
Richard E Davis
Nicholas D Youngblut
Tuomas eKärnä
Lydie eHerfort
Rachel J Whitaker
William W Metcalf
Bradley M. Tebo
Antonio M Baptista
Holly M Simon
Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
Frontiers in Microbiology
ammonia oxidation
methane cycling
metagenome analysis
Particle exchange
Columbia River Estuary
lateral bay sediments
author_facet Mariya W Smith
Richard E Davis
Nicholas D Youngblut
Tuomas eKärnä
Lydie eHerfort
Rachel J Whitaker
William W Metcalf
Bradley M. Tebo
Antonio M Baptista
Holly M Simon
author_sort Mariya W Smith
title Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
title_short Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
title_full Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
title_fullStr Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
title_full_unstemmed Metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower Columbia River
title_sort metagenomic evidence for reciprocal particle exchange between the mainstem estuary and lateral bay sediments of the lower columbia river
publisher Frontiers Media S.A.
series Frontiers in Microbiology
issn 1664-302X
publishDate 2015-10-01
description Lateral bays of the lower Columbia River estuary are areas of enhanced water retention that influence net ecosystem metabolism through activities of their diverse microbial communities. Metagenomic characterization of sediment microbiota from three disparate sites in two brackish lateral bays (Baker and Youngs) produced approximately 100 Gbp of DNA sequence data analyzed subsequently for predicted SSU rRNA and peptide-coding genes. The metagenomes were dominated by Bacteria. A large component of Eukaryota was present in Youngs Bay samples, i.e. the inner bay sediment was enriched with the invasive New Zealand mudsnail, Potamopyrgus antipodarum, known for high ammonia production. The metagenome was also highly enriched with an archaeal ammonia oxidizer closely related to Nitrosoarchaeum limnia. Combined analysis of sequences and continuous, high-resolution time series of biogeochemical data from fixed and mobile platforms revealed the importance of large-scale reciprocal particle exchanges between the mainstem estuarine water column and lateral bay sediments. Deposition of marine diatom particles in sediments near Youngs Bay mouth was associated with a dramatic enrichment of Bacteroidetes (58% of total Bacteria) and corresponding genes involved in phytoplankton polysaccharide degradation. The Baker Bay sediment metagenome contained abundant Archaea, including diverse methanogens, as well as functional genes for methylotrophy and taxonomic markers for syntrophic bacteria, suggesting that active methane cycling occurs at this location. Our previous work showed enrichments of similar anaerobic taxa in particulate matter of the mainstem estuarine water column. In total, our results identify the lateral bays as both sources and sinks of biogenic particles significantly impacting microbial community composition and biogeochemical activities in the estuary.
topic ammonia oxidation
methane cycling
metagenome analysis
Particle exchange
Columbia River Estuary
lateral bay sediments
url http://journal.frontiersin.org/Journal/10.3389/fmicb.2015.01074/full
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