` ~b}' detnition, involve relative changes in
<br />abundance. Some species mac be elim-
<br />inated, others may be reduced in num-
<br />bers, and some may be benefited.
<br />Animals i^ category 4 are the easiest
<br />to define, simply because of the general-
<br />ly small, unique habitats in which the}•
<br />live. Such habitats often lack biological
<br />diversity. Minor changes may therefore
<br />effect major fluctuations in species
<br />abundance. Because of its isolation, an
<br />island is an especially likely site for such
<br />a catastrophe; indigenous organisms are
<br />few, and the system is ecologically un-
<br />saturated. Aggressive exotic species that
<br />travel with man have, when successfully
<br />established, a profound and usually
<br />detrimental influence. This was exempli-
<br />fied by the rapid destruction of a major
<br />part of the isolated avifauna on the
<br />Hawaiian Archipelago in the late 1800's
<br />and early 1900's (S). In most respects,
<br />desert springs are similarly isolated, in-
<br />sofar as many aquatic animals are con-
<br />cerned-often even more so than
<br />oceanic islands (6). Series of springs in
<br />desert regions form aquatic archipelagos
<br />that differ from their oceanic analogs in
<br />that they often contain organisms that
<br />are relicts of past ages, rather than orga-
<br />nisms resulting from chance invasion
<br />and subsequent differentiation. The re-
<br />stricted and ecologically .simplified na-
<br />ture of these habitats leaves them
<br />especially susceptible to faunal destruc-
<br />lion, especially when the springs are
<br />located in areas of rapid population
<br />growth, where the demand for water
<br />exceeds the supply.
<br />Status of Selected Fishes
<br />Faunal depiction in aquatic habitats
<br />of the American Southwest is the simple
<br />rule. Much surface water is directly re-
<br />n~oved for use by man. Most of the re-
<br />n;aining natural waters are highly modi-
<br />fied, physicochemically or biologically.
<br />Because of these factors, big-river fishes
<br />(category 3) present a special, pressing
<br />problem in the region. Table 1 illustrates
<br />the gross changes that have occurred in
<br />the fish fafinpa of a mtijor stream in
<br />Arizona, the Salt River, near its down-
<br />stream end at Tempe (Fig. 1). Extirpa-
<br />tion of a major part of the fauna
<br />between 1890 and 1926 is evident, cor-
<br />responding to early modifications of the
<br />stream by Caucasian man and impound-
<br />ment of Roosevelt Lake on the river in
<br />1910. A chain of impoundments was
<br />then progressively created on the Salt
<br />River. between Tempe and Roosevelt.
<br />The Verde River, a major confluent of
<br />Z9 MARCH 1968
<br />the Salt, maintained some .++ater in the
<br />channel at Tempe for a ~,bile. $artlett
<br />Reservoir on the ~'crde ++as closed in
<br />1939, ho++ever, and this, in combination
<br />with construction of another dam, re-
<br />sulted in almost total desiccation of the
<br />channel of the Salt River b}~ the late
<br />1950's (7). Only subsurface percolation
<br />of water, mostly from underfloor of
<br />municipal waste waters, maintained iso-
<br />lated fish habitats along the nearly dry
<br />stream. Such habitats persist today. In-
<br />troduced fishes became increasingly
<br />established after 1926, and extirpation
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<br />of additional native fishes quickly fol-
<br />lo+ved.
<br />All the species that occupied the Salt
<br />Ricer at Tempe in 1590 exist today
<br />somewhere in the Colorado River basin.
<br />The variation in their success in main-
<br />taining populations is, however, great;
<br />some species remain abundant, others
<br />are reduced in number, and a few are
<br />on the verge of extinction. This varia-
<br />tion illustrates some of the problems
<br />involved in the study and definition of
<br />"endangered species."
<br />Two large species especially relevant
<br />r
<br />\ IGILA
<br />) ~2a ,
<br />)rSAN PEDRO R.
<br />11 r7 I
<br />COLORApO
<br />SAN JUAN R,
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<br />NEW ME%ICO
<br />Fig. 1. Sketch map of the Colorado River basin, southwestern United States, showing
<br />rivers and localities mentioned in the text, (1) Arivaca Creek; (2) Bartlett Dam; (3)
<br />Camp Verde, Arizona; (4) Coolidge Dam; (5) Dinosaur National Monument; (6)
<br />Dome, Arizona; (7) Fairbank and Tombstone, Arizona; (S) Flaming Gorge Dam; (9)
<br />Ft. Thomas, Arizona; (10) Frisco Hot Spring; (11) Gila City (= Gila Bend), Arizona;
<br />(12) Glen-Canyon Dam and Lee's Ferry, Arizona; (13) Grand Canyon; (14) Grand
<br />Falls; (15) Lake Havasu; (16) Lake Mead; (17) Lake Mojave; (18) Martinez Lake;
<br />(19) Navajo Dam; (20) Ouray, Utah; (2t) Phoenix, Arizona; (22) Roosevelt Lake
<br />and Roosevelt, Arizona; (23) Safford, Arizona; (24) Salt River Canyon; (25) Saguaro
<br />Lake; (26) St. George, Utah; (27) Tempe, Arizona; (26} Yuma, Arizona.
<br />1425
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