Biogeography of American Northwest Hot Spring A/B'-Lineage Synechococcus Populations

dc.contributor.authorBecraft, Eric D.
dc.contributor.authorWood, Jason M.
dc.contributor.authorCohan, Frederick M.
dc.contributor.authorWard, David M.
dc.date.accessioned2020-11-02T20:23:33Z
dc.date.available2020-11-02T20:23:33Z
dc.date.issued2020-02
dc.description.abstractPrevious analyses have shown how diversity among unicellular cyanobacteria inhabiting island-like hot springs is structured relative to physical separation and physiochemical differences among springs, especially at local to regional scales. However, these studies have been limited by the low resolution provided by the molecular markers surveyed. We analyzed large datasets obtained by high-throughput sequencing of a segment of the photosynthesis gene psaA from samples collected in hot springs from geothermal basins in Yellowstone National Park, Montana, and Oregon, all known from previous studies to contain populations of A/B'-lineage Synechococcus. The fraction of identical sequences was greater among springs separated by 50 km, and springs separated by >800 km shared sequence variants only rarely. Phylogenetic analyses provided evidence for endemic lineages that could be related to geographic isolation and/or geochemical differences on regional scales. Ecotype Simulation 2 was used to predict putative ecotypes (ecologically distinct populations), and their membership, and canonical correspondence analysis was used to examine the geographical and geochemical bases for variation in their distribution. Across the range of Oregon and Yellowstone, geographical separation explained the largest percentage of the differences in distribution of ecotypes (9.5% correlated to longitude; 9.4% to latitude), with geochemical differences explaining the largest percentage of the remaining differences in distribution (7.4-9.3% correlated to magnesium, sulfate, and sulfide). Among samples within the Greater Yellowstone Ecosystem, geochemical differences significantly explained the distribution of ecotypes (6.5-9.3% correlated to magnesium, boron, sulfate, silicon dioxide, chloride, and pH). Nevertheless, differences in the abundance and membership of ecotypes in Yellowstone springs with similar chemistry suggested that allopatry may be involved even at local scales. Synechococcus populations have diverged both by physical isolation and physiochemical differences, and populations on surprisingly local scales have been evolving independently.en_US
dc.identifier.citationBecraft, Eric D., Jason M. Wood, Frederick M. Cohan, and David M. Ward. “Biogeography of American Northwest Hot Spring A/B′-Lineage Synechococcus Populations.” Frontiers in Microbiology 11 (February 24, 2020). doi:10.3389/fmicb.2020.00077.en_US
dc.identifier.issn1664-302X
dc.identifier.urihttps://scholarworks.montana.edu/handle/1/16014
dc.language.isoen_USen_US
dc.rights© This manuscript version is made available under the CC-BY 4.0 licenseen_US
dc.rights.urihttps://creativecommons.org/licenses/by/4.0en_US
dc.titleBiogeography of American Northwest Hot Spring A/B'-Lineage Synechococcus Populationsen_US
dc.typeArticleen_US
mus.citation.extentfirstpage77en_US
mus.citation.journaltitleFrontiers in Microbiologyen_US
mus.citation.volume11en_US
mus.data.thumbpage4en_US
mus.identifier.doi10.3389/fmicb.2020.00077en_US
mus.relation.collegeCollege of Agricultureen_US
mus.relation.departmentLand Resources & Environmental Sciences.en_US
mus.relation.universityMontana State University - Bozemanen_US

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