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<br />.. <br /> <br />918 <br /> <br />BORLEY AND WHITE <br /> <br /> <br /> <br />FIGURE I.-Colorado pikeminnow collection locations in <br />the Colorado River basin: (1) Yampa River (74YC stock); (2) <br />Green River (81 YC, in part); (3) Colorado River (81 YC, in <br />part); (4) Colorado River (91YC); (5) Colorado River; (6) San <br />Iuan River; and (7) White River. Approximate sample <br />locations of the museum specimens are indicated by acronyms <br />for the collecting institutions: Brigham Young University <br />(BYU), California Academy of Science (CAS), Kansas <br />University (KU), Tulane University (TV), and University of <br />New Mexico (UNM) (see Table 2 for additional details). <br /> <br />Discussion <br /> <br />Our results are consistent with the presence of a <br />single Colorado pikeminnow ESU within the Colorado <br />River basin. Widespread interbasin transfers of hatch- <br />ery-reared fish (Morizot et al. 2002) would tend to <br />homogenize allele and haplotype frequencies across the <br />drainage. Our data for the Colorado pikemirmow also <br />suggest a genetic bottleneck. Several issues probably <br /> <br />contributed to the limited haplotype variation observed <br />in Colorado pikeminnow. First, the hatchery brood- <br />stocks were founded with a very small number of <br />females (Morizot et al. 2002), and genetic diversity is <br />known to rapidly decline in captive populations when <br />the number of breeding adults is small (Vrijenhoek <br />1996). Second, the Colorado pikemirmow has under- <br />gone a precipitous decline in population size and range <br />(Osmundson and Burnham 1998); this decline would <br />have resulted in loss of genetic variation. <br />Our survey of museum specimens suggests that low <br />levels of variation predate the population decline and <br />stocking history of the Colorado pikeminnow in the <br />1900s. The Colorado River may have been subjected to <br />a severe drought approximately 7,500 years ago <br />(Tarboton 1995). Such long-term drought is thought <br />to have significantly impacted fish faunas, whose <br />recovery may take decades or centuries (Matthews <br />1998). As part of an evaluation of the hypothesis that <br />such drought events would have long-term impacts on <br />genetic variation, Douglas et al. (2003) concluded that <br />the patterns of variation observed in the flarmelmouth <br />sucker Catostomus latipinnis, another Colorado River <br />endemic, were consistent with such a drought scenario. <br />Their data supported occirrrence of a rapid population <br />expansion after a bottleneck at the end of the <br />Pleistocene. The same drought that affected the <br />flannelmouth sucker may have impacted genetic <br />variation in Colorado pikeminnow and other Colorado <br />River endemics. Garrigan et al. (2002) attributed low <br />levels of mtDNA variation in bony tails Gila elegans to <br />population bottlenecking but found no evidence of <br />such bottlenecking in humpback chub G. cypha or <br />razorback suckers Xyrauchen texanus. <br />Low-frequency alleles are the most prone to genetic <br />drift in a bottleneck (Nei et al. 1975). Previous <br />allozyme studies of wild Colorado pikeminnow found <br />rare basin-specific alleles (Ammerman and Morizot <br /> <br />TAB <br />and N <br />pikemi <br />mainta <br />Center <br /> <br />Primer <br /> <br />ArgBL <br />ND4L1 <br />ND4L1 <br />NAP2( <br /> <br />1989; <br />found <br />the uI <br />basin -: <br />hatche <br />founde <br />stock <br />obtaim <br />rado) E <br />preseni <br />Lo'h <br />minno' <br />such Vi <br />mtDNl <br />captive <br />inheritl <br />nuclem <br />mtDNf <br />populal <br />mtDNl <br />maxiffi] <br />present <br />femaleE <br />stock Ii' <br />2002). <br />(Morizt <br />with fj <br />persona <br /> <br /> <br />TABLE 2.-Sample number, collection information, and haplotype for the museum samples of Colorado pikeminnow <br />sequenced and then compared with three year-classes maintained at Dexter National Fish Hatchery and Technology Center, New <br />Mexico. Included with the museum samples were those from Brigham Young University (BYU), California Academy of <br />Sciences (CAS), Kansas University (KU), Tulane University (TV), and University of New Mexico (UNM). <br /> <br />Sample # Museum # River Location State Year Haplotype <br />BYU2 25282 Green Emery County Utah 1934 A <br />BYU3 176314 Green Daggett County Utah 1964 A <br />BYU4 176315 Green Daggett County Utah 1964 A <br />CAS2 SU 3833 Colorado Yuma Arizona 1890 A <br />CAS4 SU 33212 Colorado San Bernardino California 1938 A <br />KUI 5445-1 Green Uintah County Utah 1959 A <br />KU2 5445-2 Green Uintah County Utah 1959 A <br />TU2 108940 Green Jensen Utah 1976 A <br />TU3 108940 Green Jensen Utah 1976 A <br />UNM767 767 San Juan Navajo Dam to Colorado New Mexico 1961 A <br />UNM3234 3234 San Juan Rio Arriba New Mexico 1959 A <br /> <br />Gene' <br />should <br />variatioJ <br />nance , <br />Yampa, <br />using h <br />for the <br />incorpOJ <br />River t <br />(Green I <br />Additiol <br />periodic <br />