Feeding ecology of polymorphic larval barred tiger salamanders in playas of the Southern Great Plains

2008 ◽  
Vol 86 (6) ◽  
pp. 554-563 ◽  
Author(s):  
D. M. Ghioca-Robrecht ◽  
L. M. Smith

In playas of the Southern Great Plains, larval barred tiger salamanders ( Ambystoma tigrinum mavortium Baird, 1850) (= Ambystoma mavortium mavortium ) are present as polymorphic populations. Typical and cannibal morphs have been previously investigated but intermediate forms have received little attention and their role in playa food web structure is unknown. We investigated the diet composition of these three morphotypes and compared diet preferences of typical versus nontypical morphs. Typical and intermediate morphs had similar body morphology (snout to vent length and stomach content mass), but cannibal morphs had larger stomach content mass than the other morphotypes. However, the intermediate morph had a distinctive diet composition from cannibal and typical individuals as determined by diet composition rankings, diet overlap and similarity indices, and diet diversity. By comparing prey availability versus consumption, we determined that nontypical morphs preferred larger invertebrates such as tadpole shrimps (Triopsidae) and fairy shrimps (Streptocephalidae), whereas typical morphs preferred smaller prey taxa like ostracods (Cyprididae) and water boatmen (Corixidae). Several prey taxa were avoided by all larvae suggesting that feeding in A. t. mavortium in playas is not opportunistic. Our study demonstrates that larval A. t. mavortium are present not only as dimorphic but also as polymorphic populations in playas and indicates that identifying these morphs is essential for the proper understanding of aquatic food webs.

2004 ◽  
Vol 78 (4) ◽  
pp. 373-376 ◽  
Author(s):  
D.L. Miller ◽  
C.R. Bursey ◽  
M.J. Gray ◽  
L.M. Smith

AbstractTissues from barred tiger salamanders (Ambystoma tigrinum mavortium), Great Plains toads (Bufo cognatus) and New Mexico spadefoots (Spea multiplicata) collected from 16 playa wetlands in Texas during 1999 and 2000 were examined by light microscopy. Digenean cysts were primarily distributed subcutaneously throughout the specimens and occasionally coelomic invasion was noted. The parasites within the cysts were 1.5–2 mm in diameter, with a thin (c. 10 μm wide) eosinophilic-staining tegument, two suckers (oral and ventral), posteriorly located primordial genitalia and paired digestive caeca. These digeneans were identified as the metacercariae of Clinostomum attenuatum. This is the first record of Clinostomum attenuatum in these amphibian species.


Tellus B ◽  
2011 ◽  
Vol 63 (2) ◽  
Author(s):  
Margaret S. Torn ◽  
Sebastien C. Biraud ◽  
Christopher J. Still ◽  
William J. Riley ◽  
Joe A. Berry

2015 ◽  
Vol 213 ◽  
pp. 209-218 ◽  
Author(s):  
Naama Raz-Yaseef ◽  
Dave P. Billesbach ◽  
Marc L. Fischer ◽  
Sebastien C. Biraud ◽  
Stacey A. Gunter ◽  
...  

2021 ◽  
pp. 1-18
Author(s):  
J. Kelly Hoffman ◽  
R. Patrick Bixler ◽  
Morgan L. Treadwell ◽  
Lars G. Coleman ◽  
Thomas W. McDaniel ◽  
...  

2021 ◽  
Vol 13 (12) ◽  
pp. 2309
Author(s):  
Jingjing Tian ◽  
Yunyan Zhang ◽  
Stephen A. Klein ◽  
Likun Wang ◽  
Rusen Öktem ◽  
...  

Summertime continental shallow cumulus clouds (ShCu) are detected using Geostationary Operational Environmental Satellite (GOES)-16 reflectance data, with cross-validation by observations from ground-based stereo cameras at the Department of Energy Atmospheric Radiation Measurement Southern Great Plains site. A ShCu cloudy pixel is identified when the GOES reflectance exceeds the clear-sky surface reflectance by a reflectance detection threshold of ShCu, ΔR. We firstly construct diurnally varying clear-sky surface reflectance maps and then estimate the ∆R. A GOES simulator is designed, projecting the clouds reconstructed by stereo cameras towards the surface along the satellite’s slanted viewing direction. The dynamic ShCu detection threshold ΔR is determined by making the GOES cloud fraction (CF) equal to the CF from the GOES simulator. Although there are temporal variabilities in ΔR, cloud fractions and cloud size distributions can be well reproduced using a constant ΔR value of 0.045. The method presented in this study enables daytime ShCu detection, which is usually falsely reported as clear sky in the GOES-16 cloud mask data product. Using this method, a new ShCu dataset can be generated to bridge the observational gap in detecting ShCu, which may transition into deep precipitating clouds, and to facilitate further studies on ShCu development over heterogenous land surface.


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