Key words: Ascaphus truei, clutch size,Coastal Tailed Frog, communal oviposition,early development, growth, Olympic Peninsula,Washington StateTailed frogs (genus Ascaphus) are stream am-phibians endemic to the Pacific Northwest (Jonesand others 2005) that are thought to represent thesister taxon of all other living anurans (Ford andCannatella 1993; Haas 2003). Among their uniquecharacteristics is their reproductive mode. Of the5912 described anuran species (AmphibiaWeb2010), the 2 species of tailed frog are the onlyanurans known to engage in copulation thatincludes intromission (Sever and others 2001).Further, the sperm storage capability of femalesallowstemporalseparationbetweenbreedingandoviposition, resulting in females depositing eggsalone (Metter 1964; Brown 1989).Knowledge of tailed frog oviposition sites,which are always concealed in streambeds, islimited (Karraker and others 2006 and referencestherein). What is known is based on theopportunistic discovery of sites during theexamination of instream substrates, a standardprocedure of various types of stream surveys (forexample, Adams 1993; Bury and others 2001).These haphazard discoveries have resulted inencountering various stages of clutch develop-ment, but have never involved field observationof oviposition. Observations of developmentfrom oviposition also have been restricted tofemales laying eggs in a laboratory via hormonalinduction (Wernz and Storm 1969; Brown 1975).Here we report the 1st field observation ofoviposition by tailed frogs, and selected fielddata on early development.Study AreaOur observations were made on Miller Creek(UTM Zone 10, 488225E, 5253553W, WGS84;elevation approximately 216 m), a 3rd-ordernon-fish-bearing stream on the east side of theOlympic Peninsula near Lake Cushman, MasonCounty, Washington. The site of our observa-tions consisted of a long riffle with steady fast-moving water. A bedrock step-pool was located5.5 m upstream and a small braided cascadewas located 5.9 m downstream of the site.Bedrock outcroppings lined the banks up- anddownstream for at least 40 m. Surroundinguplands are managed for timber production bythe Washington Department of Natural Re-sources; the local stand was last harvested in1945. Red Alder (Alnus rubra) and Vine Maple(Acer circinatum) dominate the riparian oversto-ry; understory is mostly Salmonberry (Rubusspectabilis), Devil’s Club (Oplopanax horridus),and Sword Fern (Polystichum munitum). Steephillslopes (50–65%) are blanketed with 2nd-growth Douglas-fir (Pseudotsuga menziesii),Western Hemlock (Tsuga heterophylla), andWestern Redcedar (Thuja plicata). Lithology ismostly Pleistocene age glacial till with large-clast material contributed from the basalt-basedCrescent Formation upstream.Initial Observations of OvipositionOn 29 July 2008, during rubble-rouse sam-pling (Quinn and others 2007) of a 2-m unit forstream-associated amphibians within this reach,we rolled a large (65 360 44 cm) boulder thatwas imbedded about 10 cm in surroundinggravel and sand. Four adult female A. truei andat least 183 A. truei eggs were found beneaththis boulder (Fig. 1). One female was activelylaying eggs. A spot water temperature taken atthis site at about 11:00 was 12.06C. A separategroup of 24 eggs was found beneath a 2ndboulder (55 3 40 3 24 cm) ,1 m downstreamthat was imbedded in approximately 20 cm of
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