The Evolution of Epigean and Stygobitic Species of Koonunga Sayce, 1907 (Syncarida: Anaspidacea) in Southern Australia, with the Description of Three New Species
Three new species of Koonunga were discovered in surface and subterranean waters in southern Australia, and were defined using mtDNA analyses and morphology. The new species are: Koonunga hornei Leijs & King; K. tatiaraensis Leijs & King and K. allambiensis Leijs & King. Molecular clock...
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| Veröffentlicht in: | PloS one 2015-08, Vol.10 (8), p.e0134673-e0134673 |
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| creator | Leijs, Remko Bradford, Tessa Mitchell, James G Humphreys, William F Cooper, Steven J B Goonan, Peter King, Rachael A |
| description | Three new species of Koonunga were discovered in surface and subterranean waters in southern Australia, and were defined using mtDNA analyses and morphology. The new species are: Koonunga hornei Leijs & King; K. tatiaraensis Leijs & King and K. allambiensis Leijs & King. Molecular clock analyses indicate that the divergence times of the species are older than the landscape that they currently inhabit. Different scenarios explaining this apparent discrepancy are discussed in the context of the palaeography of the area. A freshwater epigean origin for Koonunga is considered the most likely hypothesis, whereby some lineages made the transition to the subterranean environment within the last few million years influenced by significant climatic cooling/drying. We discuss the possibility that one stygobitic lineage secondarily regained some of its body pigmentation as adaptation to increased photic conditions after cave collapse and forming of cenotes during the last glacial maximum. |
| doi_str_mv | 10.1371/journal.pone.0134673 |
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The new species are: Koonunga hornei Leijs & King; K. tatiaraensis Leijs & King and K. allambiensis Leijs & King. Molecular clock analyses indicate that the divergence times of the species are older than the landscape that they currently inhabit. Different scenarios explaining this apparent discrepancy are discussed in the context of the palaeography of the area. A freshwater epigean origin for Koonunga is considered the most likely hypothesis, whereby some lineages made the transition to the subterranean environment within the last few million years influenced by significant climatic cooling/drying. We discuss the possibility that one stygobitic lineage secondarily regained some of its body pigmentation as adaptation to increased photic conditions after cave collapse and forming of cenotes during the last glacial maximum.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0134673</identifier><identifier>PMID: 26309115</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Anaspidacea ; Animals ; Australia ; Biodiversity ; Biological evolution ; Caves ; Coasts ; Crustacea ; Crustacea - physiology ; Crustaceans ; Divergence ; Drying ; Ecology ; Ecosystem ; Epigenetic inheritance ; Evolution ; Evolution, Molecular ; Evolutionary biology ; Genetic aspects ; Geography ; Groundwater ; Koonungidae ; Last Glacial Maximum ; Mitochondrial DNA ; Morphology ; Museums ; New species ; Paleography ; Phylogeny ; Physiological aspects ; Pigmentation ; Surface water ; Syncarida</subject><ispartof>PloS one, 2015-08, Vol.10 (8), p.e0134673-e0134673</ispartof><rights>COPYRIGHT 2015 Public Library of Science</rights><rights>2015 Leijs et al. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2015 Leijs et al 2015 Leijs et al</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c585t-bef9b07c3158acbc8af4873a031dc148343cada7aaa054fd2ac7255d48fd7b453</citedby><cites>FETCH-LOGICAL-c585t-bef9b07c3158acbc8af4873a031dc148343cada7aaa054fd2ac7255d48fd7b453</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4550344/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4550344/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,723,776,780,860,881,2096,2915,23845,27901,27902,53766,53768,79569,79570</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/26309115$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Leijs, Remko</creatorcontrib><creatorcontrib>Bradford, Tessa</creatorcontrib><creatorcontrib>Mitchell, James G</creatorcontrib><creatorcontrib>Humphreys, William F</creatorcontrib><creatorcontrib>Cooper, Steven J B</creatorcontrib><creatorcontrib>Goonan, Peter</creatorcontrib><creatorcontrib>King, Rachael A</creatorcontrib><title>The Evolution of Epigean and Stygobitic Species of Koonunga Sayce, 1907 (Syncarida: Anaspidacea) in Southern Australia, with the Description of Three New Species</title><title>PloS one</title><addtitle>PLoS One</addtitle><description>Three new species of Koonunga were discovered in surface and subterranean waters in southern Australia, and were defined using mtDNA analyses and morphology. The new species are: Koonunga hornei Leijs & King; K. tatiaraensis Leijs & King and K. allambiensis Leijs & King. Molecular clock analyses indicate that the divergence times of the species are older than the landscape that they currently inhabit. Different scenarios explaining this apparent discrepancy are discussed in the context of the palaeography of the area. A freshwater epigean origin for Koonunga is considered the most likely hypothesis, whereby some lineages made the transition to the subterranean environment within the last few million years influenced by significant climatic cooling/drying. 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The new species are: Koonunga hornei Leijs & King; K. tatiaraensis Leijs & King and K. allambiensis Leijs & King. Molecular clock analyses indicate that the divergence times of the species are older than the landscape that they currently inhabit. Different scenarios explaining this apparent discrepancy are discussed in the context of the palaeography of the area. A freshwater epigean origin for Koonunga is considered the most likely hypothesis, whereby some lineages made the transition to the subterranean environment within the last few million years influenced by significant climatic cooling/drying. 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| subjects | Anaspidacea Animals Australia Biodiversity Biological evolution Caves Coasts Crustacea Crustacea - physiology Crustaceans Divergence Drying Ecology Ecosystem Epigenetic inheritance Evolution Evolution, Molecular Evolutionary biology Genetic aspects Geography Groundwater Koonungidae Last Glacial Maximum Mitochondrial DNA Morphology Museums New species Paleography Phylogeny Physiological aspects Pigmentation Surface water Syncarida |
| title | The Evolution of Epigean and Stygobitic Species of Koonunga Sayce, 1907 (Syncarida: Anaspidacea) in Southern Australia, with the Description of Three New Species |
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