Phylogenetic diversity in freshwater‐dwelling Isochrysidales haptophytes with implications for alkenone production
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- Nora Richter
- Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island
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- William M. Longo
- Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island
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- Sarabeth George
- Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island
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- Anna Shipunova
- The Josephine Bay Paul Center for Comparative Molecular Biology and Evolution Marine Biological Laboratory Woods Hole Massachusetts
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- Yongsong Huang
- Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island
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- Linda Amaral‐Zettler
- Department of Earth, Environmental and Planetary Sciences Brown University Providence Rhode Island
書誌事項
- 公開日
- 2019-02-05
- 権利情報
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- http://creativecommons.org/licenses/by/4.0/
- http://creativecommons.org/licenses/by/4.0/
- DOI
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- 10.1111/gbi.12330
- 公開者
- Wiley
この論文をさがす
説明
<jats:title>Abstract</jats:title><jats:p>Members of the order Isochrysidales are unique among haptophyte lineages in being the exclusive producers of alkenones, long‐chain ketones that are commonly used for paleotemperature reconstructions. Alkenone‐producing haptophytes are divided into three major groups based largely on molecular ecological data: Group I is found in freshwater lakes, Group <jats:styled-content style="fixed-case">II</jats:styled-content> commonly occurs in brackish and coastal marine environments, and Group <jats:styled-content style="fixed-case">III</jats:styled-content> consists of open ocean species. Each group has distinct alkenone distributions; however, only Groups <jats:styled-content style="fixed-case">II</jats:styled-content> and <jats:styled-content style="fixed-case">III</jats:styled-content> Isochrysidales currently have cultured representatives. The uncultured Group I Isochrysidales are distinguished geochemically by the presence of tri‐unsaturated alkenone isomers (C<jats:sub>37:3b</jats:sub> Me, C<jats:sub>38:3b</jats:sub> Et, C<jats:sub>38:3b</jats:sub> Me, C<jats:sub>39:3b</jats:sub> Et) present in water column and sediment samples, yet their genetic diversity, morphology, and environmental controls are largely unknown. Using small‐subunit (<jats:styled-content style="fixed-case">SSU</jats:styled-content>) ribosomal <jats:styled-content style="fixed-case">RNA</jats:styled-content> (<jats:styled-content style="fixed-case">rRNA</jats:styled-content>) marker gene amplicon high‐throughput sequencing of environmental water column and sediment samples, we show that Group I is monophyletic with high phylogenetic diversity and contains a well‐supported clade separating the previously described “<jats:styled-content style="fixed-case">EV</jats:styled-content>” clade from the “Greenland” clade. We infer the first partial large‐subunit (<jats:styled-content style="fixed-case">LSU</jats:styled-content>) <jats:styled-content style="fixed-case">rRNA</jats:styled-content> gene Group I sequence phylogeny, which uncovered additional well‐supported clades embedded within Group I. Relative to Group <jats:styled-content style="fixed-case">II</jats:styled-content>, Group I revealed higher levels of genetic diversity despite conservation of alkenone signatures and a closer evolutionary relationship with Group <jats:styled-content style="fixed-case">III</jats:styled-content>. In Group I, the presence of the tri‐unsaturated alkenone isomers appears to be conserved, which is not the case for Group <jats:styled-content style="fixed-case">II</jats:styled-content>. This suggests differing environmental influences on Group I and <jats:styled-content style="fixed-case">II</jats:styled-content> and perhaps uncovers evolutionary constraints on alkenone biosynthesis.</jats:p>
収録刊行物
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- Geobiology
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Geobiology 17 (3), 272-280, 2019-02-05
Wiley

