Stoneflies (Plecoptera) of the Black Hills of South Dakota and Wyoming, USA: Distribution and Zoogeographic Affinities

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Stoneflies (Plecoptera) of the Black Hills of South Dakota and Wyoming, USA: Distribution and Zoogeographic Affinities Great Basin Naturalist Volume 59 Number 1 Article 1 1-22-1999 Stoneflies (Plecoptera) of the Black Hills of South Dakota and Wyoming, USA: distribution and zoogeographic affinities Bret O. Huntsman Brigham Young University Richard W. Baumann Brigham Young University Boris C. Kondratieff Colorado State University, Fort Collins Follow this and additional works at: https://scholarsarchive.byu.edu/gbn Recommended Citation Huntsman, Bret O.; Baumann, Richard W.; and Kondratieff, Boris C. (1999) "Stoneflies (Plecoptera) of the Black Hills of South Dakota and Wyoming, USA: distribution and zoogeographic affinities," Great Basin Naturalist: Vol. 59 : No. 1 , Article 1. Available at: https://scholarsarchive.byu.edu/gbn/vol59/iss1/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Great Basin Naturalist by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. The Great Basin Naturalist PuBUSHED AT PROVO, UTAH, BY M.L. BEAN LIFE SCIENCE MUSEUM BRIGHAM You C UNlVERSm' ISS 0017-3614 VOLUME 59 30 JANUARY 1999 No.1 Great Basin Naturalist 59(l),ltll999. pp. 1-17 STONEFLIES (PLECOPTERA) OF THE BLACK HILLS OF SOUTH DAKOTA AND WYOMING, USA: DISTRIBUTION AND ZOOGEOGRAPHIC AFFINITIES Bret O. Huntsman1, Richard ,v. Baumann1.2, and Boris C. Kondratieff3 ABSTRACT.-The Black Hills of South Dakota and Wyoming are an insular mountain range completely surrounded by the Great Plains. The stonefly (Plecoptera) fauna of the Black Hilts was surveyed and zoogeographic affinities exam­ ined. Twenty-seven species representing 22 genera and 6 families were found. Fifteen new state records for South Dakota and 2 for Wyoming are presented. Two species are removed from the South Dakota list. An analysis ofthe North American distribution of each species showed a strong relationship between the Black Hills and the Rocky Mountains, with much weaker relationships between the Black Hills and eastern and northern regions. Results ofa logistic regres­ sion analysis comparing factors contributing to long-distance dispersal ability against presence/absence in the Black Hills were inconclusive. However, other evidence suggests that the Black Hills fauna is a result ofexpansion and subse­ quent vicariance ofstonefly populations during Pleistocene climatic oscillations. Key words: stonefl~, Plecoplera, zoogeography, B1llck Hills, South Dakot<J, Wyoming, Pleistocene. The Black Hills are an island of mountains Melntosh 1931, Van Bmggen 1985). Mammal in a sea of grass (Tumer 1974). These isolated species of the Black Hills show similar mixed mountains, located in western South Dakota affinities. Approximately 14.3% are Rocky and eastern Wyoming, are completely sur­ Mountain, 8.6% are from eastern deciduous rounded by the Great Plains physiographic forests, 14.3% are from northern boreal forests, region. The Black Hills contain one ofthe most and the rest are a mix of widespread, steppe, unusual mixes of biotic affinities in orth and Sonoran species (Turner 1974). Insects in America. For example, 30% ofthe plant species the Black Hills also appear to have mixed found in the Black Hills have Rocky Mountain affinities. For instance, the mayfly (Ephemer­ affinities, 9% have eastern deciduous forest optera) fauna of the Black Hills has western affinities, 6% have northern boreal forest affini­ species (36.8% of the fauna), eastern species ties, while the remainder are a mix: of steppe (21.1%), and widespread species (42.1%) and widespread species (Hayward 1928, (McCafferty 1990). lDepartmeot ofZooIoP.', Brigbaro Young Un.ivecity; Provo. lIT 54600. :.\l,It/wr to whom reprint reque$l$ $bould be sent. 3Department of BioogrieultuOlI Scie.ooes and F'e$1 ;\laDagement. Color.ido Stile UnMmty. Fori <Alliin$. CO 80523. 1 2 GREAT BASIN NATURALIST [Volume 59 Another interesting aspect of Black Hills populations within the Black Hills. At the pre­ biogeography is the fact that many populations sent time no quantitative studies have been of plants and animals inhabiting the area are performed comparing vicariance and dispersal highly disjunct, being separated from the near­ models for the Black Hills fauna. est conspecific populations by as much as 600 Faunal affinities and distribution histories k-m (Turner 1974, Van Bruggen 1985, McCaf­ are most easily studied using organisms re­ ferty 1990). These disjunct populations also stricted to definable habitats (Sargent et al. often represent the extreme range limit for 1991, Houseman and Baumann 1997). One their species (Turner 1974, Van Bruggen 1985, outstanding example of this type of organism McCafferty 1990). is the insect Order Plecoptera (stonellies). The most common hypothesis explaining Most stonelly species require cold, clean these striking biogeographic patterns is that streams with rocky streambeds to complete these disjunct populations are vicariated relicts their life cycles (Surdick and Gaufin 1978, from the most recent period of glaciation Ward 1984, Stewart and Stark 1988). Adult (Ross 1965, Turner 1974, McCafferty 1990). stonellies are not powerful lliers and usually Palynological studies indicate that during the are not capable of long-distance migrations Full-glacial period of the Wisconsin glaciation (Ross 1965, Hynes 1988, Marden and Kramer (30,000-13,000 years BP) much of the central 1994, Griffith et aJ. 1998). Thus, dispersal of portion of the United States was covered with most stonelly species is thought to require boreal forest (Wright 1970), allowing typical adequate water connections (Surdick and boreal animals to inhabit this region. This Gaufin 1978, Baumann 1979, Flanagan and cooler, wetter climate also allowed deciduous Flanagan 1982). Many species have restricted gallery forests to form along stream banks, ranges, and distinct differences exist between prOViding avenues of expansion for eastern the stonelly faunas of western, eastern, and deciduous forest species into the Black Hills northern North America, primarily at the (Turner 1974). Later, during the Late-glacial generic and/or specific levels (Rickel' 1964, period (13,000-10,500 BP), the boreal forest Dosdall and Lemkuhl1979, Stark et aJ. 1986). followed the retreating ice sheet and was Few published records are available on the replaced by steppe habitat in the Great Plains stonellies of the Black Hills. Presently, only 14 (Holfman and Jones 1970). Eastern and north­ species have been reported from the Black Hills ern species that had expanded into the Black region (Stark and Gaufm 1976, Baumann et al. Hills during the FUll-glacial period were then 1977, Stark et al. 1986). Several families, such isolated in the refuge formed there by the as the Capniidae, Pteronarcyidae, Taenioptery­ remnant deciduous and boreal forests (Turner gidae, and Leuctridae, have not been previ­ 1974). ously reported from the Black Hills. Unfortu­ Also during the.Full-glacial period of the nately, many of the streams within the Black Wisconsin the cordilleran-montane zone of Hills have been affected by pollution and the Rocky Mountains was depressed about other perturbations (Stewart and Thilenius 1200-1400 m. This displaced the biota of this 1964). It is poSSible that some populations of wne eastward, extending from the Laramie stonellies within the Black Hills have already and Big Horn Mountains ofWyoming into the been extirpated. In the face of the current Black Hills (Turner 1974). Again, when the ice challenge to document North American biodi­ sheet retreated, the montane species that had versity (Kosztarab and Schaefer 1990), inven­ expanded into the Black Hills were isolated in torying the stonelly fauna of the Black Hills the refuge formed there (Thrner 1974). should be a priority. Although the hypothesis of Ross (1965), Our study had 3 main objectives: to docu­ Tnrner (1974), and McCafferty (1990) has great ment the stonelly fauna of the Black Hills, to explanatory power, it is not the only possibil­ detemune ifthe stonellies ofthis region rellect ity. It is also possible tbat tbe Black Hills pop­ the mixed affmities shown by other groups of ulations of plants and animals were established organisms, and to quantitatively test the vicari­ via long-distance dispersal. Sometime after the ance hypothesis of Ross (1965), Turner (1974), formation of the Great Plains, various species and McCafferty (1990) using these new stone­ may have dispersed across it and founded lIy distributional data. 1999] STONEFLIES OF THE BLACK HILLS 3 STUDY AREA Adult stoncflies were collected nsing beat­ ing sheets or aerial nets, or by hand. Nymphal The Black HilIs region consists of the mack stondlies were collected with aquatic dip Hills proper and the Bear Lodge Mountains in nets. At some sites nymphs of selected species \vestern South Dakota and northeastern were set aside and reared to adults to assist in Wyoming (approximately 43'10'-44'50' N lat., specific identification. All adults (and the 103'20'-104'50' W long.; Tnrner 1974). The nymphs of certain species) were identified Black Hills were created by intermittent domal using keys in Baumann et al. (1977) and Stew­ uplifts during the Cretaceous, Miocene, and art and Stark (1988). Pleistocene (Turner 1974). Elevations in tbe In addition to field-collected specimens, we Black Hills region range from 1000 m on the examined specimens from the following insti­ western plains to 2228 m at Harney Peak. The tutions: Monte L. Bean Life Science
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