Life cycle and behaviour of the aquatic firefly Luciola leii (Coleoptera: Lampyridae) from Mainland China

2006 ◽  
Vol 138 (6) ◽  
pp. 860-870 ◽  
Author(s):  
Xinhua Fu ◽  
Ohba Nobuyoshi ◽  
Fredric V. Vencl ◽  
Chaoliang Lei

AbstractThe aquatic larvae of the firefly Luciola leii Fu and Ballantyne occur on the substrate of rice fields and ditches in Hubei Province of central China. The behaviour and ecology of L. leii are described. We recorded L. leii larvae attacking four species of aquatic snails: Lymnaea stagnalis (L.) (Basommatophora: Lymnaeidae), Gyraulus convexiusculus (Hutton) (Basommatophora: Planorbidae), Radix auricularia (L.) (Lymnaeidae), and Bellamya purificata Heude (Mesogastropoda: Viviparidae). At dusk, flying males produced two types of advertising flashes. One type consisted of a train of 8 rapid, green flashes followed by 2–3 slow, prolonged flashes produced by patrolling males as a long-distance signal. The duration of flashes in the patrolling pattern was 530 ms and the interflash interval was 80 ms. The other type was a short-range signal consisting of a green glow, which was emitted by flying males that had located a female. Once a female had been located, the male landed and switched to a courting pattern. The male courtship pattern consisted of single flashes of about 400 ms duration, delivered every 1.8 s. Females produced single answering flashes of 910 ms duration, with a latency of approximately 630 ms after the male flash. Luciola leii was univoltine. Females oviposited 1 to 7 times (mean = 4.78). Females laid, on average, 187.19 eggs. The eggs hatched at 21.52 days. Eggs became luminescent 4 or 5 days before hatching. The larval stage had six instars. Mature larvae climbed onto land to construct pupal cells at the end of April of the next year. The pupal stage lasted, on average, 4.88 days. The imago lasted 10.13 days. No predators of larvae were observed. The spider Tetragnatha praedonia Koch (Araneae: Tetragnathidae) was frequently observed to capture adult male fireflies in its web.

2005 ◽  
Vol 137 (1) ◽  
pp. 83-90 ◽  
Author(s):  
Fu Xinhua ◽  
Ohba Nobuyoshi ◽  
Fredric V. Vencl ◽  
Lei Chaoliang

AbstractThe aquatic firefly Luciola substriata Gorham, 1880 (Coleoptera: Lampyridae) was first discovered in mainland China in 2000. The larvae of L. substriata inhabit ponds and lakes rich in aquatic vegetation. We recorded L. substriata feeding on two species of aquatic snails, Lymnaea stagnalis (L., 1758) (Basommatophora: Lymnaeidae) and Gyraulus convexiusculus (Hutton, 1849) (Basommatophora: Planorbidae). Three predators of fireflies were also recorded for the first time: the red swamp crayfish, Procambarus clarkii (Girard, 1852) (Decapoda: Cambaridae), the crab Eriocheir sinensis H. Milne-Edwards, 1853 (Decapoda: Varunidae), and the grass carp, Ctenopharyngodon idellus (Valenciennes in Cuvier et Valenciennes, 1844) (Cypriniformes: Cyprinidae). Egg incubation averaged 11 days at an ambient temperature of 20–25 °C. The prepupal stage of L. substriata lasted 6.2 days, and the pupal stage lasted 4.4 days. The imaginal period lasted from May to September. Courtship light-flashing activity peaked 1 h after sunset. The light spectrum of responsiveness of L. substriata was 425–603 nm, with a peak responsive emission at 504 nm. In addition, we have described and illustrated the morphology of L. substriata.


2016 ◽  
Vol 38 (1) ◽  
pp. 19-24 ◽  
Author(s):  
Robin K. Cameron ◽  
Philip Carella ◽  
Marisa Isaacs ◽  
Marc Champigny ◽  
Juliane Merl-Pham ◽  
...  

2016 ◽  
Vol 155 (4) ◽  
pp. 893-906 ◽  
Author(s):  
CHUANBO SHEN ◽  
DI HU ◽  
CHUN SHAO ◽  
LIANFU MEI

AbstractThe Wudang Complex located in the central part of South Qinling, has been inferred to be a segment of the Yangtze Craton involved in the orogen. In this study, the cooling/exhumation history of the Wudang Complex is revealed through combined published geochronology data and new apatite fission-track results. Three rapid exhumation episodes related to relevant geodynamic events have been identified. Previous40Ar–39Ar and (U–Th)/He data indicate that the most significant exhumation, induced by the collision between the North and South China Blocks, occurred fromc.237 to 220 Ma after long-term subsidence and sedimentation of the passive continental margin. The second exhumation event, related to the long-distance effect of the Pacific subduction, occurred during the period fromc.126 to 90 Ma. Following the late Cretaceous – Eocene peneplanation stage, the final late Cenozoic exhumation sincec.15 Ma may be attributed to the combined effect of the eastward growth of the Tibetan Plateau uplift and the Asian monsoon.


Nano Letters ◽  
2017 ◽  
Vol 17 (2) ◽  
pp. 631-637 ◽  
Author(s):  
Alessandro Tuniz ◽  
Mario Chemnitz ◽  
Jan Dellith ◽  
Stefan Weidlich ◽  
Markus A. Schmidt

2006 ◽  
pp. 333-349
Author(s):  
Stefano Mancuso ◽  
Sergio Mugnai

1947 ◽  
Vol 2 (11-12) ◽  
pp. 419-421
Author(s):  
Ewald Frömming

Die Pflanzennahrung allein ist für das Gedeihen von Physa acuta Drap. nicht ausreichend; auch diese Art bedarf des tierischen Eiweißes, genau wie Lymnaea stagnalis L., Stagnicola palustris O. F. Müller, Radix auricularia L., Radix ovata Drap. und Viriparus viviparus L., für die dies bereits nachgewiesen wurde.


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