Extraordinary capture of a Randall's snapper Randallichthys filamentosus in the temperate south-eastern Indian Ocean and its molecular phylogenetic relationship within the Etelinae
MetadataShow full item record
© 2016 The Fisheries Society of the British Isles.The capture of a rarely encountered Randall's snapper Randallichthys filamentosus (female, 587 mm fork length) from the upper continental slope (c. 350 m) off the south coast of Western Australia (c. 34·5° S; 122·5° E) in January 2014 represents its first record from the temperate Indian Ocean and a southern range extension. This record suggests that spawning of this predominantly tropical species may probably be occurring in the eastern Indian Ocean, considering the extensive, and unlikely, distance the progeny would have otherwise travelled from its typical distribution in the western and central Pacific Ocean.
Showing items related by title, author, creator and subject.
A comparison of the evolution of arc complexes in Paleozoic interior and peripheral orogens: Speculations on geodynamic correlationsMurphy, J.; van Staal, C.; Collins, William (2011)We discuss the potential geodynamic connections between Paleozoic arc development along the flanks of the interior (e.g. the Iapetus and Rheic) oceans and the exterior Paleopacific Ocean. Paleozoic arcs in the Iapetus and ...
Phylogeography, population structure and evolution of coral-eating butterflyfishes (Family Chaetodontidae, genus Chaetodon, subgenus Corallochaetodon)Waldrop, E.; Hobbs, J.; Randall, J.; Di Battista, Joseph; Rocha, L.; Kosaki, R.; Berumen, M.; Bowen, B. (2016)Aim: This study compares the phylogeography, population structure and evolution of four butterflyfish species in the Chaetodon subgenus Corallochaetodon, with two widespread species (Indian Ocean – C. trifasciatus and ...
Bekker, A.; Planavsky, N.; Rasmussen, Birger; Krapez, Bryan; Hofmann, A.; Slack, J.; Rouxel, O.; Konhauser, K. (2014)Iron formations are economically significant, iron- and silica-rich sedimentary rocks that are restricted to Precambrian successions. There are no known modern or Phanerozoic analogues for these deposits that are comparable ...