Picoeukaryote Plankton Composition off West Spitsbergen at the Entrance to the Arctic Ocean

Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454‐pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen...

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Published inThe Journal of eukaryotic microbiology Vol. 61; no. 6; pp. 569 - 579
Main Authors Kilias, Estelle S, Nöthig, Eva‐Maria, Wolf, Christian, Metfies, Katja
Format Journal Article
LanguageEnglish
Published United States Society of Protozoologists 01.11.2014
Blackwell Publishing Ltd
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Abstract Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454‐pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen Current (WSC; Fram Strait). High abundances of Micromonas pusilla were detected in the station situated closest to Spitsbergen, as seen in surveys of picoplankton assemblages in the Beaufort Sea. At the other three stations, other phylotypes, affiliating with Phaeocystis pouchetii and Syndiniales in the phylogenetic tree, were present in high numbers, dominating most of them. The picoplankton community structures at three of the stations, all with similar salinity and temperature, were alike. At the fourth station, the influence of the East Spitsbergen Current, transporting cold water from the Barents Sea around Spitsbergen, causes different abiotic parameters that result in a significantly different picoeukaryote community composition, which is dominated by M. pusilla. This observation is particularly interesting with regard to ongoing environmental changes in the Arctic. Ongoing warming of the WSC could convey a new picoplankton assemblage into the Arctic Ocean, which may come to affect the dominance of M. pusilla.
AbstractList Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454‐pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen Current (WSC; Fram Strait). High abundances of Micromonas pusilla were detected in the station situated closest to Spitsbergen, as seen in surveys of picoplankton assemblages in the Beaufort Sea. At the other three stations, other phylotypes, affiliating with Phaeocystis pouchetii and Syndiniales in the phylogenetic tree, were present in high numbers, dominating most of them. The picoplankton community structures at three of the stations, all with similar salinity and temperature, were alike. At the fourth station, the influence of the East Spitsbergen Current, transporting cold water from the Barents Sea around Spitsbergen, causes different abiotic parameters that result in a significantly different picoeukaryote community composition, which is dominated by M. pusilla. This observation is particularly interesting with regard to ongoing environmental changes in the Arctic. Ongoing warming of the WSC could convey a new picoplankton assemblage into the Arctic Ocean, which may come to affect the dominance of M. pusilla.
Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454‐pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen Current ( WSC ; Fram Strait). High abundances of Micromonas pusilla were detected in the station situated closest to Spitsbergen, as seen in surveys of picoplankton assemblages in the Beaufort Sea. At the other three stations, other phylotypes, affiliating with Phaeocystis pouchetii and Syndiniales in the phylogenetic tree, were present in high numbers, dominating most of them. The picoplankton community structures at three of the stations, all with similar salinity and temperature, were alike. At the fourth station, the influence of the East Spitsbergen Current, transporting cold water from the Barents Sea around Spitsbergen, causes different abiotic parameters that result in a significantly different picoeukaryote community composition, which is dominated by M. pusilla . This observation is particularly interesting with regard to ongoing environmental changes in the Arctic. Ongoing warming of the WSC could convey a new picoplankton assemblage into the Arctic Ocean, which may come to affect the dominance of M. pusilla .
Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454-pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen Current (WSC; Fram Strait). High abundances of Micromonas pusilla were detected in the station situated closest to Spitsbergen, as seen in surveys of picoplankton assemblages in the Beaufort Sea. At the other three stations, other phylotypes, affiliating with Phaeocystis pouchetii and Syndiniales in the phylogenetic tree, were present in high numbers, dominating most of them. The picoplankton community structures at three of the stations, all with similar salinity and temperature, were alike. At the fourth station, the influence of the East Spitsbergen Current, transporting cold water from the Barents Sea around Spitsbergen, causes different abiotic parameters that result in a significantly different picoeukaryote community composition, which is dominated by M. pusilla. This observation is particularly interesting with regard to ongoing environmental changes in the Arctic. Ongoing warming of the WSC could convey a new picoplankton assemblage into the Arctic Ocean, which may come to affect the dominance of M. pusilla.Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently, molecular methods are required. In this study, we used 454-pyrosequencing to study picoplankton communities at four stations in the West Spitsbergen Current (WSC; Fram Strait). High abundances of Micromonas pusilla were detected in the station situated closest to Spitsbergen, as seen in surveys of picoplankton assemblages in the Beaufort Sea. At the other three stations, other phylotypes, affiliating with Phaeocystis pouchetii and Syndiniales in the phylogenetic tree, were present in high numbers, dominating most of them. The picoplankton community structures at three of the stations, all with similar salinity and temperature, were alike. At the fourth station, the influence of the East Spitsbergen Current, transporting cold water from the Barents Sea around Spitsbergen, causes different abiotic parameters that result in a significantly different picoeukaryote community composition, which is dominated by M. pusilla. This observation is particularly interesting with regard to ongoing environmental changes in the Arctic. Ongoing warming of the WSC could convey a new picoplankton assemblage into the Arctic Ocean, which may come to affect the dominance of M. pusilla.
Author Kilias, Estelle S
Metfies, Katja
Wolf, Christian
Nöthig, Eva‐Maria
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Keywords phytoplankton
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biodiversity
microbial diversity
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License 2014 The Author(s) Journal of Eukaryotic Microbiology © 2014 International Society of Protistologists.
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Table S1. Overview of the distribution of abundant phylotypes (≥ 1%) over three size classes > 10 μm, 10 to 3 μm and 3 to 0.4 μm, their taxonomic affiliation in the NCBI data base (E-value = 0) and their taxonomic affiliation after PhyloAssigner. Values are given in percent. Uc. = uncultured.
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Snippet Investigation of marine eukaryotic picoplankton composition is limited by missing morphological features for appropriate identification. Consequently,...
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StartPage 569
SubjectTerms 454-pyrosequencing
Arctic region
Barents Sea
Base Sequence
Beaufort Sea
Biodiversity
biogeography
Chlorophyta
cold
community structure
Environment
Eukaryota - classification
Eukaryota - genetics
Eukaryota - isolation & purification
microbial diversity
Micromonas pusilla
next generation sequencing
Norway
Oceans and Seas
Phaeocystis
Phaeocystis pouchetii
Phylogeny
phylotype
phytoplankton
plankton
Plankton - classification
Plankton - genetics
Plankton - isolation & purification
RNA, Ribosomal, 18S - genetics
salinity
surveys
Svalbard
Temperature
Title Picoeukaryote Plankton Composition off West Spitsbergen at the Entrance to the Arctic Ocean
URI https://api.istex.fr/ark:/67375/WNG-WQ7G5S77-Q/fulltext.pdf
https://onlinelibrary.wiley.com/doi/abs/10.1111%2Fjeu.12134
https://www.ncbi.nlm.nih.gov/pubmed/24996010
https://www.proquest.com/docview/1627946645
https://www.proquest.com/docview/1641017108
https://www.proquest.com/docview/1803084914
Volume 61
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