The Life History of the Alderfly, Sialis aequalis Banks, in an Acid Mine Stream
The Life History of the Alderfly, Sialis aequalis Banks, in an Acid Mine Stream
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酸矿流中赤杨蝇(Sialis aequalis Banks)的生活史
DOI:
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发表时间:
1973
期刊:
影响因子:
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通讯作者:
D. Tarter
中科院分区:
文献类型:
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作者:
J. E. Woodrum;D. Tarter
The life history of the alderfly, Sialis aequalis Banks, was studied intensively in an acid mine stream, Camp Creek of Twelvepole Creek, Wayne Co., West Virginia, between July 1970 and June 1971. Alderfly larvae are detritivorous, supplementing their diet with chironomid larvae in summer and autumn. Length-frequency distributions indicate that larvae require 1 year to complete the life cycle. The larvae attain their greatest growth rate from June to July (83%). The entire larval population required 2-6 days for departure from the stream. Pupation began in a moist sandbank in mid-March and lasted 4-5 weeks. Emergence of adults began in late April and reached a peak in early May. Total egg counts from 10 females ranged from 402 to 818 (mean, 657). Adult life span was the 2 weeks in nature and ranged from 1 to 7 days under laboratory conditions (mean, 5.7 days). Adults do not feed. INTRODUCTION The deleterious effects of mine drainage effluent upon aquatic life has long been recognized. Many authors, including Lackey (1938, 1939), Wichs (1959), Parsons (1968), USDI (1967, 1968, 1969) and Nichols (1971), have reported the effects of acid mine drainage on the aquatic life of a stream. Very few life history studies have been conducted on organisms occupying such an unfavorable environment. This study considers the life history of the alderfly, Sialis aequalis Banks, in an acid mine stream. Ross (1937), in a monograph of nearctic alderflies, rep6rted 19 species in the genus Sialis Latreille 1802. Townsend (1939) and Flint (1964) have described one and three new species, respectively, since that monograph. Ross (1937) reported the genus Sialis from 33 states and Canada. We have reported the occurrence of S. aequalis for the first time in West Virginia Tarter and Woodrum (1973). MATERIALS AND METHODS Camp Creek is located in the Twelvepole Creek basin on the East Fork of Twelvepole Creek at East Lynn, Wayne Co., W. Va. It originates in the vicinity of Turkey Camp Knob and consists of a left and right fork, 4.3 and 2.8 miles in length, respectively, converging to form the main stem (1.1 miles long). This discharges into the left fork of Twelvepole Creek at East Lynn, W. Va. The basin is located in the Kanawha section of the Appalachian Plateau physiographic province which is characterized by a mature plateau of fine texture with moderate to strong relief (Krebs and 1 Part of a thesis submitted by the senior author to the Graduate School, Marshall University, in partial fulfillment of the requirements for the degree of Master of Science, August 1971.