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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.) <br /> <br />C':,) <br />c:,..." <br />~l <br />i"''':' <br />N <br /> <br />References <br /> <br />Briggs, M, (1996). Riparian Recovery in Arid Lands, Strategies and References. Tucson: University <br />of Arizona Press 159 pp, <br />Busch, D. & Smith, S. (1995). Mechanisms associated with decline of woody species in riparian <br />ecosystems of the southwestern US. Ecological Monographs, 65: 347-370. <br />Collier, M., Webb, R & Andrews, E. (1997). Experimental flooding in Grand Canyon. Scientific <br />American, 276: 82-89. <br />Cook, C. & Bonham, C. (1977). Techniquesfor Vegetation Measurements and Analysis fora Pre- and <br />Post-mining Inventory. Colorado State University Range Science Department Science Series <br />No. 28, 99 pp. <br />Curtis,J. & Cottam, G. (1962). Plant Ecology Workbook, Minneapolis, Minnesota: Burgess Pub\. <br />Co. 193 pp, <br />Dale, V" Lugo, A. MacMahon, J. & Pickett, S. (1998). Ecosystem management in the context of <br />large, infrequent disturbances. Ecosystems, 1: 546-557. <br />Dynesius, M. & Nilsson, C. (1994). Fragmentation and flow regulation of river systems in the <br />northern 3rd of the world. Science, 266: 753-762. <br />Felger, R, Broyles, B., Wilson, M. & Nabhan, G. (1997). The binational Sonoran Desert <br />biosphere network and its plant life (with plant checklistand index). Journal of tM Southwest, 39: <br />411-566. <br />Galindo-Beet, R, Glenn, E. Page, H., Fitzsimmons, K., Gallindo-Bect, L., Hernandez-Ayon, j., <br />Petty, R, Garcia-Hernandez, J. & Moore, D. (2000). Penaeid shrimp landings in the upper Gulf <br />of California in relation to Colorado River freshwater discharge Fishery Bulletin, 98: 222-225. <br />Glantz, M. (1996). Cumnts of change: El Nino's Impact on Climate and Society, U.K., Cambridge <br />University Press 194 pp. <br />Glenn, E., Lee, RC., Felger, R & Zengel, S. (1996). Effects of water management on the <br />wetlands of the Colorado River Delta, Mexico. Conservation Biology, 10: 1175-1186. <br />Glenn, E., Tanner, R., Mendez, S., Kehret, T., Moore, D., Garcia, J. & Valdes, C. (1998). <br />Growth rates, salt tolerance and water use characteristics of native and invasive riparian plants <br />from the delta of the Colorado River, Mexico Journal of Arid ETI'lIironments, 40: 281-294. <br />Glenn, E., Garcia,J., Tanner, R., Congdon, C. & Luecke, D. (1999). Status of wetlands supported <br />by agricultural drainage water in the Colorado River delta, Mexico HortScience, 34: 39-45, <br />Li, Z. & Kafatosm M. (2000). lnterannual variability of vegetation in the United States and its <br />relation to E1 Nino/Southern Oscillation Remote Sensing of Environment, 71: 239-247. <br />Molls, M., Crawford, C., Ellis, L., Valett, H. & Dahm, C. (1998), Managed flooding for riparian <br />ecosystem restoration - managed flooding reorganizes riparian forest ecosystems along the <br />middle Rio Grande in New Mexico Bioscience, 48: 749-756. <br />Morrison, J., Postel, S. & Gleick, p, (1996). The Sustainable Use of Water in the Lower Colorado <br />River Basin, Oakland, California USA: Pacific lnstitute. <br />Nagler, P., Gillon, K., Pitt, J., Snape, W. & Glenn, E. (2000). Application of the endangered <br />species act across international borders: the case of the Colorado River delta, Mexico, Environ- <br />mental ScUnce and Policy, 3: 11-15. <br />Nagler, p" Glenn, E. & Huete, A. (2001). Assessment of spectral vegetation indices for a riparian <br />ecosystem in the Colorado River delta. Journal of Arid ETI'lIironments, 49: 91-110. doi: <br />10. 1 oo6/iare,200 1 ,0844. <br />