Redescription of a rare threadfin (Perciformes: Polynemidae), Polydactylus macrophthalmus (Bleeker, 1858), with designation of a lectotype and notes on distributional implications

被引:0
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作者
Hiroyuki Motomura
Martien J. P. van Oijen
Isaäc J. H. Isbrücker
Yukio Iwatsuki
机构
[1] Miyazaki University,
[2] The United Graduate School of Agricultural Sciences,undefined
[3] Kagoshima University,undefined
[4] 1-1 Gakuen-kibanadai-nishi,undefined
[5] Miyazaki 889-2192,undefined
[6] Japan (e-mail: a02113u@cc.miyazaki-u.ac.jp),undefined
[7] National Museum of Natural History,undefined
[8] P.O. Box 9517,undefined
[9] 2300 RA Leiden,undefined
[10] The Netherlands (e-mail: oijen@naturalis.nnm.nl),undefined
[11] Zoölogisch Museum Amsterdam,undefined
[12] Universiteit van Amsterdam,undefined
[13] P.O. Box 94766,undefined
[14] 1090 GT Amsterdam,undefined
[15] The Netherlands (e-mail: isbruecker@science.uva.nl),undefined
[16] Division of Fisheries Sciences,undefined
[17] Faculty of Agriculture,undefined
[18] Miyazaki University,undefined
[19] 1-1 Gakuen-kibanadai-nishi,undefined
[20] Miyazaki 889-2192,undefined
[21] Japan (e-mail: yuk@cc.miyazaki-u.ac.jp),undefined
来源
Ichthyological Research | 2001年 / 48卷
关键词
Key words Polynemidae; Redescription; Polydactylus macrophthalmus; Distribution;
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摘要
A rare threadfin, Polydactylus macrophthalmus (Bleeker, 1858), having long been included in the genus Polynemus, is redescribed on the basis of 9 specimens and a lectotype designated. Polydactylus macrophthalmus is characterized by the following combination of characters: 7 pectoral filaments, upper 3 filaments extending beyond posterior margin of hypural; 13 or 14 pectoral fin rays; 87–94 pored lateral line scales; 11 scales above lateral line, 15 or 16 below; 10–12 upper series gill rakers, 15 or 16 lower, 26 or 27 total; occipital profile concave in adults; second spine of first dorsal fin very strong; pectoral fin rays long (mean 24% [range 24–26%] of SL). The presently known distribution of the species, including the Kapuas River, Kalimantan, and the Musi and Batanghari Rivers, Sumatra, Indonesia, apparently reflects the ancient Central or North Sunda River during the last period of lowered sea levels, ca. 12 000 years ago.
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页码:289 / 294
页数:5
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