Phytomyza solidaginophaga Sehgal, 1971
publication ID |
https://doi.org/ 10.11646/zootaxa.4479.1.1 |
publication LSID |
lsid:zoobank.org:pub:93C84828-6EEF-4758-BEA1-97EEEF115245 |
DOI |
https://doi.org/10.5281/zenodo.5997942 |
persistent identifier |
https://treatment.plazi.org/id/03D287EF-FFF2-E419-A8E5-5459452BFD2D |
treatment provided by |
Plazi |
scientific name |
Phytomyza solidaginophaga Sehgal |
status |
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Phytomyza solidaginophaga Sehgal View in CoL
( Fig. 206 View FIGURES 200–207 )
Material examined. MASSACHUSETTS: Franklin Co., Northfield , 276 Old Wendell Rd. , 18.v.2015, em. 13.iii.2016, C.S. Eiseman, ex Solidago canadensis var. canadensis , #CSE2241, CNC654073 View Materials (1♂) ; 18.v.2015, em. 13.iii.2016, ex Solidago rugosa , #CSE2242, CNC654196 (1♀); Hampshire Co., Cummington, along Rte. 9 (east end of town), 18.v.2013, em. 11.iii.2014, C.S. Eiseman, ex Solidago patula , #CSE999, CNC384730 View Materials (1♂) ; South Hadley, near Lithia Springs Reservoir , 11.v.2016, em. 9.iv.2017, C.S. Eiseman, ex Solidago caesia , #CSE3428, CNC939718 View Materials , CNC939719 View Materials (1♂ 1♀).
Hosts. Asteraceae : Solidago * caesia L., S. canadensis L., S. * patula Muhl. ex Willd., S. * rugosa Mill. , S. simplex Kunth ( Griffiths 1976) .
Leaf mine. ( Fig. 206 View FIGURES 200–207 ) Griffiths (1976) described the mine as “entirely linear, 6–8 cm long, 1.5–2.5 mm wide terminally, formed entirely on upper surface of leaf, appearing greenish-white or greenish-brown in reflected light when fresh; faeces deposited as fine particles, partly forming short beaded strips.” The “beaded strips” in some of the mines we collected were quite similar to the frass in some mines of Liriomyza eupatorii , but based on the material we have seen so far, the presence of discrete frass grains (albeit often in very closely spaced rows) reliably distinguishes Phytomyza mines from those of L. eupatorii .
Puparium. Black; formed outside the mine.
Distribution. * USA: MA; Canada: AB; empty mines in YT were likely caused by this species ( Griffiths 1976).
Comments. As noted by Griffiths (1976), this species is strictly univoltine and its larvae appear earlier than those of any other Solidago miner. In Alberta, larvae have been collected in the first half of June; we found larvae in Massachusetts in mid-May, and the adults emerged about two weeks after their puparia were removed from refrigeration the following year.
The eastern males examined here very closely resemble the holotype, although it should be noted there are slight differences that may be due to geographic variation. There are as many spines along the length of the phallus, but these end closer to the apex of the basiphallus; the hypophallus is complete, not broken medially; the basiphallus, hypophallus and base of the distiphallus appear to be slightly stouter.
No known copyright restrictions apply. See Agosti, D., Egloff, W., 2009. Taxonomic information exchange and copyright: the Plazi approach. BMC Research Notes 2009, 2:53 for further explanation.
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