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LAKI,t JANLAI ILL I tCAfVtJ wIlV
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<br /> r and censusin inapt cereal rain crop (California Dep. Water !
<br /> expended less etTort searching for g g II
<br /> cranes at Pixley NWR, Merced NWR, Modesto Res., unpubl.) hosts only 1,500-2,000 Lesser
<br /> and other locations in the San Joaquin Valley Sandhill Cranes (T. Pogson, unpubl. data), and
<br /> than on the S-SJ Delta and the Sacramento Val- overall use of that geographic area by large cranes
<br /> icy. Littlefield and Thompson (1979) found few was lower than use of the Thornton region(Table
<br /> Greater Sandhill Cranes in the San Joaquin Val- 1). The Cosumnes River is not dammed and its
<br /> ley, and our censuses of Lesser Sandhill Cranes floodplain is subject to annual flooding from win-
<br /> there in 1981, 1982,and 1983 revealed few large ter rainfall and snowmelt in late winter. This
<br /> cranes (T. Pogson, unpubl. data). The reduced region provided wetland habitats for large num-
<br /> effort in the southern Central Valley probably bers of cranes in both winters after waterfowl
<br /> caused underestimation of the number of cranes hunting clubs were drained in the Thornton re-
<br /> in these little-used portions of the winter range gion.
<br /> and a slight underestimation of the population's The same sites used by the population in the
<br /> size. late 1960s and mid-1970s (Littlefield and
<br /> It is possible that we sometimes misidentified Thompson 1979), the Llano Seco Rancho south-
<br /> Lesser Sandhill Cranes as"large cranes"(Greater west of Chico, Gray Lodge WMA in the Butte
<br /> and Canadian Sandhill Cranes)while conducting Sink, the El Dorado Gun Club at Thornton, and
<br /> roost counts at sites where large cranes and Less- the Faith and Mape's Ranches west of Modesto, Ii
<br /> er Sandhill Cranes were both present in large were still important in 1983-1984 and 1984—
<br /> numbers. This misidentification would have in- 1985. The numbers of large cranes using these I�
<br /> flated our regional estimates of the number of sites in the late 1960s and mid-1970s were sim-
<br /> large cranes. However, it is equally likely that we filar to the numbers of cranes using these sites at
<br /> incorrectl.,classified large cranes as Lesser Sand- a comparable time of year during the winter of !
<br /> hill Cranes. Although the magnitude of this error 1983-1984.
<br /> is unknown, we do not believe it significantly During the winters of 1983-1984 and 1984— t�C
<br /> affected our estimates. 1985, 98% of the population's winter range was It
<br /> privately owned.Only 19 km'of the winter range G
<br /> DISTRIBUTION AND IMPORTANT (ca. 2%), which included important roosting sites,
<br /> WINTERING SITES was managed by state and federal wildlife man-
<br /> During our surveys,large numbers of cranes were agement agencies as waterfowl hunting areas.The
<br /> present in the same regions that were heavily majority of the population used private lands for }
<br /> used ly the population in the late 1960s and mid- feeding and roosting. Use of public lands by cranes ;
<br /> 1970s (Littlefield and Thompson 1979). The peaked in October 1983 when 36% of the pop-
<br /> Chico, Butte Sink, Thornton, and Modesto ulation roosted at two sites in the Butte Sink, the
<br /> regions were the most important winter areas for Bean Patch, and Gray Lodge Wildlife Area (Ta- f
<br /> the population in 1983-1984 and 1984-1985, as ble 1). iC
<br /> in 1969-1971 and 1976. We, however, detected iX
<br /> the movement of 50-60%of the total population SIGHTINGS OF MARKED CRANES
<br /> from the Butte Sink to Chico and Thornton dur- The movement of marked cranes among regions
<br /> ing November and December (Table 1), which demonstrated relationships among different por-
<br /> was not detected by Littlefield and Thompson tions of the winter range. From November :f €{
<br /> (1979). Residents of the Chico, Butte Sink, and through January marked cranes departed from
<br /> Thornton regions reposed that this movement the Butte Sink and moved north within the Sac-
<br /> is an annual event (M. Meyers, J. Buress, M. ramento Valley to Afton and Chico, or south out
<br /> Leighty, and L. Pucci, pers. comm.). of the Sacramento Valley to Thornton on the
<br /> The Thornton area supported the greatest S-SJ Delta. In January and February marked
<br /> ft ?
<br /> number of large cranes among regions in the Cen- cranes left Thornton and moved to the nearby
<br /> tral Valley. Use of the Thornton area by 5,000— floodplain of the Cosumnes River. Cranes which
<br /> 6,000 Lesser Sandhill Cranes(T. Pogson,unpubl. were banded at Malheur NWR, in southeastern E�
<br /> data),in addition the the 1,772-3,829 large cranes Oregon, were disproportionately concentrated in It
<br /> (Table 1), was probably related to the availability the Thornton region, while cranes banded at Sy-
<br /> of waste corn, the dominant crop in this region. can Marsh, in southcentral Oregon, were dispro-
<br /> The Sacramento Valley, where rice is the dom- portionately concentrated in the Butte Sink (T.
<br /> VI-135 ,!c�lsiy
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