IMPORTANT PLANT AREA NOMINATION FORM MONTANA. Nominated Site Name: Big Sheep Creek Basin Important Plant Area (IPA)

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IMPORTANT PLANT AREA NOMINATION FORM MONTANA Nominated Site Name: Big Sheep Creek Basin Important Plant Area (IPA) General Location: Big Sheep Creek Basin is a located between the Beaverhead (on the west) and the Tendoy (on the east) mountain ranges in southern Montana. Approximately 15 miles west of Lima, Montana. Maps: Maps and location information are withheld because private land is included in the IPA. Photographs: Landscape photographs as well as photos of Primula alcalina are included. Counties: Beaverhead County Elevation: 6,800 ft to 10,773 ft. Size of Area: 52, 944 acres Property Ownership: Bureau of Land Management, Forest Service, and Private. Other designations for the site: None Table 1. Vascular plant species of concern in the Big Sheep Creek Basin IPA Species MNHP MNHP Last Obs. Population Trend global state Size Primula alcalina G2 S1 June 2010 Unknown Unknown Aquilegia Formosa G5 S1S2 1989 Unknown Unknown Braya humilis G5 S1 2002 Unknown Unknown Carex idahoa G2G3 S3 2002 Unknown Unknown Erigeron asperugineus G4 S1 1989 Unknown Unknown Erigeron linearis G5 S1 2002 Unknown Unknown Eriogonum caespitosum G5 S1 2003 Unknown Unknown Eriogonum soliceps G2 S2 2003 Unknown Unknown Gymnosteris parvula G4 S1 2006 Unknown Unknown Lomatogonium rotatum G5 S1 1994 Unknown Unknown Primula incana G4G5 S2 2002 Unknown Unknown Thalictrum alpinum G5 S2 2010 Unknown Unknown Thelypodium sagittatum G4 S2 2002 Unknown Unknown Trend Information: Primula alcalina: The BLM began monitoring of Primula alcalina in 2006, incorporating cover estimates of Thalictrum alpinum as well. US Forest Service began Primula alcalina and Thalictrum alpinum monitoring in 2010, following the BLM protocol (Hockett, 2006). No second year data has been collected by either agency at this time. US Forest Service plans to re-read their monitoring plot in 2011. Threats: Threats to rare plants in the Big Sheep Creek Basin IPA include: mineral extraction, weed invasion, livestock grazing, water diversion, and impacts from climate change. At this 1

time, populations seem to be doing well, yet no long term monitoring has been conducted and no surveys on private lands have occurred. Many of the rare species present in the IPA are wetland species that could be affected by livestock grazing or water diversion. Several studies have shown that livestock grazing at certain times of the year may have a positive effect on Primula alcalina and other related species of primrose (Miyasaki and Mansfield 1996, Lindborg and Ehrlen 2001, Ehrlen et al. 2005). Currently, weed infestation are quite low in the nominated IPA. Spotted knapweed is not located in the immediate area, but has been found at the mouth of Big Sheep Creek canyon. Mineral extraction has occurred in the area and is a potential direct threat to individuals as well as through erosion, sedimentation and the potential to act as a vector for weed invasion. Table 2. Type and Severity of Threats for Rare Plants in the Big Sheep Creek Basin IPA Species Threats Level Comments All but Rocky slope (see below) Weed Invasion Low Currently only spotted knapweed is known at the mouth of Big Sheep Creek canyon. All but Rocky slope All Livestock Grazing Mineral Extraction Wetland sp. Water Diversion Lowmoderate Low Grazing is present throughout the IPA. Can directly damage plants, create hummock and introduce weeds. May benefit some species by reducing competition (Moseley 1995). Gravel mining has occurred in the past. Can remove plants, increase erosion/sedimentation, and introduce weeds.? Many rare species in the IPA are dependent on wetland habitats that can be altered by changes in hydrology (Lesica 2003). All Climate Change Low Changes in temperature and water availability have been observed to change the distribution of plant species, and may occur within the nominated IPA over time (Crimmins et. Al 2011). Justification: The Big Sheep Creek Basin has an astounding assemblage of rare plants within a relatively small geographic area. Thirteen plant species of concern are present within the nominated Big Sheep Creek Basin IPA area, one G2 and seven S1 species. Due to the extent of rare species within the Cabin Creek/Alkali Creek drainages and the importance of hydrology for several rare species, the entire 5 th code watershed was selected for the IPA boundary. This large boundary recognizes the importance of maintaining a functioning system in order to support important smaller habitats within. The IPA s rather large area encompasses a variety of habitats and rare plants, which include the following (Lesica 2003, Montana Field Guide 2011): Wetlands: Braya humilis, Carex idahoa, Lomatagonium rotatum, Primula alcalina, P. incana, Thalictrum alpinum and Thelypodium sagittatum Riparian: Aquilegia Formosa 2

Sagebrush: Erigeron linearis, Eriogonum caespitosum, Eriogonum soliceps, and Gymnosteris parvula Rocky/gravelly Slopes: Erigeron asperugineus Of most concern within the nominated IPA is Primula alcalina, a G2, S1 species. Montana s only known occurrence for the species is within the nominated Big Sheep Creek Basin IPA. Globally there are only seven known populations. Water diversion could threaten this species. The presence of the wetlands and the large topographic relief lead to a diversity of plant communities. Alluvial soils in uplands of the basin proper support sagebrush steppe dominated by Wyoming big sagebrush (Artemisia tridentata ssp. wyomingensis) with a ground layer dominated by bluebunch wheatgrass (Agropyron spicatum), western wheatgrass (Agropyron smithii) and Sandberg bluegrass (Poa secunda). Lower sites with heavier soils often support low sagebrush steppe dominated by Artemisia longiloba with a ground layer of western wheatgrass or Idaho fescue (Festuca idahoensis) on slightly steeper inclines. Dominant vegetation of the foothills is sagebrush steppe dominated by mountain big sagebrush (Artemisia tridentata ssp. vaseyana) and Idaho fescue. Low sagebrush steppe dominated by Artemisia arbuscula, bluebunch wheatgrass and spike fescue (Leucopoa kingii) may occur on warm slopes with skeletal limestone soils. Limestone slopes may support dry Douglas-fir (Pseudotsuga menziesii) forest on cool slopes and limber pine (Pinus flexilis) and/or mountain mahogany (Cercocarpus ledifolius) woodland near lower timberline. Low sagebrush communities, Artemisia arbuscula arbuscula/agropyron spicatum, Artemisia arbuscula longiloba/agropyron smithii and Artemisia arbuscula longiloba/festuca idahoensis are rare in Montana, found only in Beaverhead County. The latter two community types may also be globally rare. Wetlands are often associated with permanent streams, springs and glacial ponds. Habitats with microtopography such as hummocks, support shrubby cinquefoil (Potentilla fruticosa) with a ground layer dominated by Baltic rush (Juncus balticus), tufted hairgrass (Deschampsia cespitosa), Nebraska sedge (Carex nebrascensis), Carex scirpoidea and numerous forbs. Similar communities without shrubby cinquefoil occur where water tables are higher or microtopography is absent. Ephemerally wet soils with salt accumulations may be occupied by sparse vegetation of saltgrass (Distichlis stricta) and alkaligrass (Puccinellia nuttalliana). The banks of the largest streams support riparian willow communities dominated by Booth willow (Salix boothii) and geyer willow (Salix geyeriana). There is a noticeable lack of willows along the lower reaches of streams such as Cabin, Meadow, Simpson, and Tex creeks. This could be due to past grazing or to a more ephemeral water table on the east side of the basin. 3

References: Crimmins, S. M. S. Z. Dobrowski, J. A. Greenberg, J. T. Abatzoglou, A. R. Mynsberge. 2011. Changes in Climatic Water Balance Drive Downhill Shifts in Plant Species Optimum Elevations. Science 331, 324. Ehrlen, J., K. Syrjanen, R. Leimu, M. B. Garcia and K. Lehtila. 2005. Land use and population growth of Primula veris: an experimental demographic approach. Journal of Applied Ecology 42: 317-326. Hockett, B. 2006. Alkali Primrose (Primula alcalina) Monitoring in Big Sheep Creek Basin. Unpublished Report. 9 pp. Lesica, P. 2003. Conserving Globally Rare Plants on Lands Administered by the Dillon Office of the Bureau of Land Management. Report to the USDI Bureau of Land Management, Dillon Office. Montana Natural Heritage Program, MT. 22 pp. plus appendices. Lindborg, R. and J. Ehrlen. 2001. Evaluating the extinction risk of a perennial herb: demographic data versus historical records. Conservation Biology 16: 683-690. Miyasaki, H. and D. H. Mansfield. 1996. Habitat relationships of Primula alcalina (Primulaceae), a threatened plant from east-central Idaho. Unpublished manuscript, College of Idaho, Caldwell. Montana Field Guide. Montana Natural Heritage Program. Retrieved on January 21, 2011 from http://fieldguide.mt.gov/detail_pdado01010.aspx. Moseley. R. K. 1995. Demographic Monitoring of Primula alcalina (alkali primrose) 1991-1994. Salmon District, Bureau of Land Management, Idaho Department of Fish and Game. 27 pp. Form submitted by: Jessie Salix, Peter Lesica Affiliation: Montana Native Plant Society Date of Submission: January 2011 Mailing address: 850 Chreston Lane, Dillon, MT 59725 E-mail address: jessiesalix@hotmail.com Phone number: 406.683.3947 4

Photo 1. Looking west at Cabin Creek wetlands in September

Photo 2. Looking west at Cabin Creek wetlands in June Photo 3. Morrison Lake wetlands

Photo 4. Looking east at Tex Creek wetlands Photo 5. Looking southeast to Simpson Creek wetlands. Photo 6. Primula alcalina

Photo7. Primula alcalina