Structure of the mating calls and relationships of the European tree frogs (Hylidae, anura)

Oecologia ◽  
1974 ◽  
Vol 14 (1-2) ◽  
pp. 99-110 ◽  
Author(s):  
Hans Schneider
Keyword(s):  
1980 ◽  
Vol 58 (1) ◽  
pp. 75-78 ◽  
Author(s):  
Carl L. Whitney

When calling male Pacific tree frogs come closer together than about 50 cm, they switch from the mating call to the encounter call. After an exchange of encounter calls, one of the frogs may submit by retreating or ceasing to call, or they may fight, after which the loser submits. To investigate the role of the encounter call in maintaining spacing, I compared the responses of calling males lo playback of encounter calls and mating calls. During 60-s playbacks, most frogs responded initially to both vocalizations by uttering encounter calls, but they were more likely to respond further to encounter calls by either attacking or submitting. I suggest that the encounter call serves to reduce the amount of time that calling frogs remain close together and, as a consequence, to enhance their chances of attracting females.


2004 ◽  
Vol 52 (2) ◽  
pp. 191 ◽  
Author(s):  
J. I. Menzies ◽  
M. J. Tyler

We examined a large collection (n = 132) of tree frogs, hitherto identified as Litoria gracilenta, from various localities in New Guinea and compared them with Litoria gracilenta from Queensland and with the recently described Litoria elkeae from far west New Guinea. We found that the frogs in question were neither L. gracilenta nor L. elkeae but comprised two distinct taxa described herein as new species.We call attention to the problems of performing statistical analysis on measurements of soft-bodied organisms and consider that the conclusions reached in this analysis are both conservative and realistic.


2010 ◽  
Vol 41 (2) ◽  
pp. 242-248 ◽  
Author(s):  
Barbara Gericota ◽  
Michael M. Garner ◽  
Bradd Barr ◽  
Robert Nordhausen ◽  
R. Scott Larsen ◽  
...  

2018 ◽  
Vol 5 (1) ◽  
pp. 54-63
Author(s):  
Simeon Lukanov ◽  
Georgi Popgeorgiev ◽  
Nikolay Tzankov

AbstractWater frog mating calls from two localities were studied and analyzed. Recordings were made in the summer of 2010 at the Arkutino swamp near the town of Primorsko and at the Vurbitza River near the town of Momchilgrad. A total of 154 calls were analyzed and the results suggested the presence of both the Marsh frog (Pelophylax ridibundus) and the Levant frog (Pelophylax bedriagae) in both sites, with the former being more frequent in Vurbitza River, and the latter – in Arkutino. At Vurbitza, we also captured and measured 2 specimens, which morphological characteristics differed from P. ridibundus and matched those of P. bedriagae. These are the first localities for P. bedriagae in Bulgaria.


2006 ◽  
Vol 3 (10) ◽  
pp. 689-697 ◽  
Author(s):  
W Federle ◽  
W.J.P Barnes ◽  
W Baumgartner ◽  
P Drechsler ◽  
J.M Smith

Tree frogs are remarkable for their capacity to cling to smooth surfaces using large toe pads. The adhesive skin of tree frog toe pads is characterized by peg-studded hexagonal cells separated by deep channels into which mucus glands open. The pads are completely wetted with watery mucus, which led previous authors to suggest that attachment is solely due to capillary and viscous forces generated by the fluid-filled joint between the pad and the substrate. Here, we present evidence from single-toe force measurements, laser tweezer microrheometry of pad mucus and interference reflection microscopy of the contact zone in Litoria caerulea , that tree frog attachment forces are significantly enhanced by close contacts and boundary friction between the pad epidermis and the substrate, facilitated by the highly regular pad microstructure.


1975 ◽  
Vol 24 (1) ◽  
pp. 1 ◽  
Author(s):  
Linda R. Maxson ◽  
A. C. Wilson
Keyword(s):  

1975 ◽  
Vol 23 (1) ◽  
pp. 113 ◽  
Author(s):  
MJ Littlejohn ◽  
JD Roberts

Mating calls of the northern and southern call races of the L. tasmaniensis complex are described. Analysis of call structure along a transect across the main contact between these allopatric forms in north central Victoria indicates that there is a zone of intergradation between 90 and 135 km wide, about 215 km long and with a north-westerly orientation. The interaction is interpreted as a secondary contact in which there is hybrid or recombinant superiority along a subtle ecological gradient.


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