Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic

Previous studies of the microarthropods of Marion Island, Southern Ocean, documented high mitochondrial COI (cytochrome c oxidase subunit I) haplotype diversity and significant genetic structure, which were ascribed to landscape subdivision. In this paper we revisit these ideas in light of new geomo...

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Main Authors: Mortimer, E., Jansen van Vuuren, B., Meiklejohn, K.I., Chown, S.L.
Format: Other/Unknown Material
Language:English
Published: Linnean Society of London 2013
Subjects:
COI
Online Access:http://hdl.handle.net/10019.1/117711
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spelling ftunstellenbosch:oai:scholar.sun.ac.za:10019.1/117711 2023-05-15T14:05:07+02:00 Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic Mortimer, E. Jansen van Vuuren, B. Meiklejohn, K.I. Chown, S.L. 2013-03-01T08:17:35Z 602674 bytes application/pdf http://hdl.handle.net/10019.1/117711 en eng Linnean Society of London Mortimer, E., Jansen van Vuuren, B., Meiklejohn, K.I. and Chown, S.L. (2012). Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic. Biological Journal of the Linnean Society 105, 131-145 http://hdl.handle.net/10019.1/117711 biogeography COI geomorphology Marion Island Prince Edward Islands rarefaction analyses JournalArticles 2013 ftunstellenbosch 2021-08-31T00:09:05Z Previous studies of the microarthropods of Marion Island, Southern Ocean, documented high mitochondrial COI (cytochrome c oxidase subunit I) haplotype diversity and significant genetic structure, which were ascribed to landscape subdivision. In this paper we revisit these ideas in light of new geomorphological evidence indicating a major lineament orientated along N26.5°E. Using the microarthropod Halozetes fulvus, we test the hypothesis that the eastern and western sides of the island show different population genetic patterns, corresponding to the previously unrecognized geological separation of these regions, and perhaps also with differences in climates across the island and further landscape complexity. Mitochondrial COI data were collected for 291 H. fulvus individuals from 30 localities across the island. Notwithstanding our sampling effort, haplotype diversity was under-sampled as indicated by rarefaction analyses. Overall, significant genetic structure was found across the island as indicated by FST analyses. Nested clade phylogeographical analyses suggested that restricted gene flow (with isolation-bydistance) played a role in shaping current genetic patterns, as confirmed by Mantel tests. At the local scale, coalescent modelling revealed two different genetic patterns. The first, characterizing populations on the southwestern corner of the island, was that of low effective population size and high gene flow. The converse was found on the eastern side of Marion Island. Taken together, substantial differences in spatial genetic structure characterize H. fulvus populations across Marion Island, in keeping with the hypothesis that the complex history of the island, including the N26.5°E geological lineament, has influenced population genetic structure. © 2011 The Linnean Society of London, Biological Journal of the Linnean Society, 2012, 105, 131–145. Other/Unknown Material Antarc* Antarctic Marion Island Prince Edward Islands Southern Ocean Mite Stellenbosch University: SUNScholar Research Repository Antarctic Southern Ocean
institution Open Polar
collection Stellenbosch University: SUNScholar Research Repository
op_collection_id ftunstellenbosch
language English
topic biogeography
COI
geomorphology
Marion Island
Prince Edward Islands
rarefaction analyses
spellingShingle biogeography
COI
geomorphology
Marion Island
Prince Edward Islands
rarefaction analyses
Mortimer, E.
Jansen van Vuuren, B.
Meiklejohn, K.I.
Chown, S.L.
Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
topic_facet biogeography
COI
geomorphology
Marion Island
Prince Edward Islands
rarefaction analyses
description Previous studies of the microarthropods of Marion Island, Southern Ocean, documented high mitochondrial COI (cytochrome c oxidase subunit I) haplotype diversity and significant genetic structure, which were ascribed to landscape subdivision. In this paper we revisit these ideas in light of new geomorphological evidence indicating a major lineament orientated along N26.5°E. Using the microarthropod Halozetes fulvus, we test the hypothesis that the eastern and western sides of the island show different population genetic patterns, corresponding to the previously unrecognized geological separation of these regions, and perhaps also with differences in climates across the island and further landscape complexity. Mitochondrial COI data were collected for 291 H. fulvus individuals from 30 localities across the island. Notwithstanding our sampling effort, haplotype diversity was under-sampled as indicated by rarefaction analyses. Overall, significant genetic structure was found across the island as indicated by FST analyses. Nested clade phylogeographical analyses suggested that restricted gene flow (with isolation-bydistance) played a role in shaping current genetic patterns, as confirmed by Mantel tests. At the local scale, coalescent modelling revealed two different genetic patterns. The first, characterizing populations on the southwestern corner of the island, was that of low effective population size and high gene flow. The converse was found on the eastern side of Marion Island. Taken together, substantial differences in spatial genetic structure characterize H. fulvus populations across Marion Island, in keeping with the hypothesis that the complex history of the island, including the N26.5°E geological lineament, has influenced population genetic structure. © 2011 The Linnean Society of London, Biological Journal of the Linnean Society, 2012, 105, 131–145.
format Other/Unknown Material
author Mortimer, E.
Jansen van Vuuren, B.
Meiklejohn, K.I.
Chown, S.L.
author_facet Mortimer, E.
Jansen van Vuuren, B.
Meiklejohn, K.I.
Chown, S.L.
author_sort Mortimer, E.
title Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
title_short Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
title_full Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
title_fullStr Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
title_full_unstemmed Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic
title_sort phylogeography of a mite, halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-antarctic
publisher Linnean Society of London
publishDate 2013
url http://hdl.handle.net/10019.1/117711
geographic Antarctic
Southern Ocean
geographic_facet Antarctic
Southern Ocean
genre Antarc*
Antarctic
Marion Island
Prince Edward Islands
Southern Ocean
Mite
genre_facet Antarc*
Antarctic
Marion Island
Prince Edward Islands
Southern Ocean
Mite
op_relation Mortimer, E., Jansen van Vuuren, B., Meiklejohn, K.I. and Chown, S.L. (2012). Phylogeography of a mite, Halozetes fulvus, reflects the landscape history of a young volcanic island in the sub-Antarctic. Biological Journal of the Linnean Society 105, 131-145
http://hdl.handle.net/10019.1/117711
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