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<br />62
<br />
<br />F. ZAMORA-ARROYO ET AL
<br />
<br />Discussion
<br />
<br />As is the case along many western rivers, the stretch of the Colorado River between
<br />Morelos Dam and the Hardy River is dominated by the exotic shrub, T. ramosissima.
<br />Although often considered an undesirable species, T. ramosissima can fulfil valuable
<br />ecological functions in riparian ecosystems (Stromberg, 1998b). This study shows that
<br />with the resumption of pulse floods following the filling of Lake Powell, native trees have
<br />also reestablished along this river stretch. The tree cohorts appear to be related to the
<br />1981-1986, 1993 and 1997-1999 releases of water from the United States to the
<br />floodplain below Morelos Dam. These releases were related to strong ENSO cycles and
<br />are expected to continue into the future, whenever precipitation in the watershed
<br />exceeds storage capacity in the reservoir system (J. Harkens, River Operations Manager,
<br />BOR, Boulder City, Nevada, pers. comm.). Native trees, including many over
<br />6 m height, now account for 20% of the species composition in this river stretch, whereas
<br />they remain rare on the U.S. stretch of river above Morelos Dam. Native trees are less
<br />salt-tolerant than T. ramosissima (Glenn el ai., 1998). The results support the pulse-
<br />flood hypotheses for the establishment of native trees, which states that occasional
<br />overbank flooding is necessary to wash salts from the banks to allow mesophytic species
<br />to germinate (Briggs, 1996; Poff el ai., 1997; Busch & Smith, 1995). Otherwise,
<br />backside become too saline for all but the most salt-tolerant plant species. Floods also
<br />serve to deposit bare mineral soil needed for germination of native trees and they
<br />moisten the soil at the appropriate time, when seeds are viable. Thus, the winter and
<br />spring timing of releases to the delta were fortuitous.
<br />On the United States stretch of river, by contrast, overbank flooding is now rare
<br />(Ohmart el ai., 1988). The carrying capacity of the river channel is large, as most of the
<br />diversions take place near the northerly international border. Furthermore, the flood-
<br />plain has been worked to prevent flooding of private property in many locations. Ii
<br />Therefore, excess releases that reach the delta remain channelized until below Morelos - I
<br />Dam, and do not germinate extensive new cohorts of native trees on the United States'
<br />._~_ 1
<br />The February-AprllI997, release of 3xl09m3 at 8o-120m3s-1 was sufficient
<br />to bring the river out of its channel to inundate most of the floodplain, and water exited
<br />to the Gulf of California and Laguna Salada. We conclude that this flow rate and volume
<br />is sufficient to inundate at least the northern portion of the floodplain (the cotton-
<br />wood-willow zone) sufficient to allow the establishment of new stands of native
<br />trees. The 1993 release was a single event of approximately 3-months duration in winter
<br />and spring yet it produced the largest cohort of native tree~, so we conclude that (,'
<br />a 3-month spring release is sufficient to germinate tree seedlings. The 1993 cohort t,:,'",'
<br />of trees were still abundant in 1999 despite lack of flows from 1994 to 1997, showing l
<br />that trees can survive at least 4 years between floods. In years without floods, native trees
<br />can exist on alluvial water tables (Seaforth el ai., 2000; Springer el ai., 1999). Depth to ~
<br />ground-water is no greater than 1-2 m along this stretch of riparian corridor, even in ~
<br />years without surface flow (Coition National del Aquas, Mexicali, Mexico, unpublished ~,
<br />ground-water maps, 1995-1998). Nevertheless, the increase in total vegetation cover ~n
<br />response to multiple years of flooding shows that surface flows also play a role. In
<br />controlling vegetation cover. Their role in recharging the ground-water or moderating
<br />its salinity is unknown. A hydrological model of the delta. floodplain is needed. .
<br />Deliberate floods have been tested as management tools In the Grand Canyon (Collier
<br />el ai., 1996) and Rio Grande (Molls et ai., 1998), but up to now the ecological
<br />effects of waste spills into the delta have not been recognized. Recently, we
<br />observed that native trees have also regenerated on the Gila River (southernmost
<br />tributary of the Colorado River), apparently as a result of flood releases from Pa~nted
<br />Rock Dam during following 1993 and 1997 ENSO events (P. Nagler, unpublished
<br />results of an aerial survey of the Colorado River and tributaries, April 2000). The delta
<br />
<br />REGENERATION OF TREES IN RESPONSE TO FLOOD RELEASES
<br />
<br />
<br />'(j~
<br />
<br />floods appear also to stimulate the shrimp catch in the upper Gulf of Californill
<br />(Galindo-Beet el ai., 2000). Large, infrequent disturbances such as these releases need
<br />to be included in ecosystem management plans (Dale et aI., 1998).
<br />The future of the regenerated delta ecosystem is in doubt. In Mexico, plans are
<br />underway to further channelize the river to remove obstructions to future releases
<br />(Valdes-Casillas, 1998). In the United States, the criteria for declaring surplus flows are
<br />being revised to attempt to retain more of the flood water for human use (NagleI' el at.,
<br />2000). Nevertheless, results show that the delta of an arid river can retain natural
<br />ecosystem functions that have disappeared from upstream, regulated stretches, and that
<br />water availability may actually increase as the dam systems mature (fill). Hence, delta
<br />regions of arid rivers should be targets for conservation actions to maintain riparian
<br />biodiversity .
<br />
<br />c.)
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<br />References
<br />
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<br />of Arizona Press 159 pp,
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<br />Cook, C. & Bonham, C. (1977). Techniquesfor Vegetation Measurements and Analysis fora Pre- and
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