December 2012 Number 1 - Utah Native Plant Society
December 2012 Number 1 - Utah Native Plant Society
December 2012 Number 1 - Utah Native Plant Society
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Calochortiana <strong>December</strong> <strong>2012</strong> <strong>Number</strong> 1<br />
The Contribution of Cedar Breaks National Monument<br />
to the Conservation of Vascular <strong>Plant</strong> Diversity in <strong>Utah</strong><br />
Walter Fertig and Douglas N. Reynolds,<br />
Moenave Botanical Consulting, Kanab, UT<br />
Abstract. Like most national parks in <strong>Utah</strong>, Cedar Breaks National Monument was initially established to protect its<br />
spectacular scenery rather than to preserve biological diversity. At less than 2500 ha, the monument is one of the<br />
smallest in the region and has a relatively small vascular flora of 354 documented species. Based on conventional<br />
measures of species richness (alpha diversity), Cedar Breaks might not seem like an important component of the protected<br />
area network of <strong>Utah</strong>. However, nearly 10% of the flora of Cedar Breaks is comprised of local or regional endemics<br />
that are mostly restricted to the Claron Formation or volcanic substrates. Many of these are rare species of<br />
high management interest. Our surveys in 2007-2008 documented nearly 1200 point locations for 17 of the monument’s<br />
rarest plants, including first records for Aster welshii and Jamesia americana var. rosea. The monument is<br />
especially significant in terms of beta diversity or complementarity, as it protects 63 plant species that are not otherwise<br />
found in NPS units in the state. As measured by an averaged Jaccard’s Coefficient of Similarity, Cedar Breaks<br />
National Monument has the second most unique flora among the parks in <strong>Utah</strong>.<br />
The Cedar Breaks Amphitheater is a large bowlshaped<br />
valley carved from orange and white limey sandstone<br />
layers of the Eocene Claron Formation on the west<br />
face of Cedar Mountain, about 18 miles east of Cedar<br />
City in southwestern <strong>Utah</strong> (Figure 1). Local Indian<br />
tribes called the area “the circle of painted cliffs” or the<br />
“place where the rocks are sliding down all the time”.<br />
Early Mormon settlers named it Cedar Breaks for the<br />
abundance of juniper (known locally as ‘cedar’) and the<br />
precipitous badland cliffs or breaks. President Franklin<br />
Roosevelt acknowledged the area’s “spectacular cliffs,<br />
canyons, and features of scenic, scientific, and educational<br />
interest” in designating Cedar Breaks as a national<br />
monument under the Antiquities Act in 1933<br />
(Evenden et al. 2002, Fertig 2009b). Administration of<br />
the monument was transferred from Dixie National Forest<br />
to the National Park Service (NPS), to be managed<br />
to “conserve unimpaired” the area’s natural and cultural<br />
resources and values “for the enjoyment of this and future<br />
generations” (NPS 2000).<br />
Protection of native biological diversity was not one<br />
of the rationales for creating Cedar Breaks National<br />
Monument, though this would eventually become an<br />
important part of NPS’s mandate to conserve natural<br />
resources. The botanical significance of the Cedar<br />
Breaks area was just beginning to be discovered in the<br />
early 1930s. Botanists George Goodman and C. Leo<br />
Hitchcock collected the holotypes of Breaks draba<br />
(Draba subalpina) and Cedar Breaks wild buckwheat<br />
(Eriogonum panguicense var. alpestre) from the rim of<br />
the Cedar Breaks Amphitheater in 1930 and Bassett<br />
Maguire added the holotype of Cedar Breaks daisy<br />
(Erigeron proselyticus, or Erigeron sionis var. trilob-<br />
atus) in 1934 (Fertig 2009b). These species are among a<br />
suite of nearly two dozen Claron formation endemics<br />
restricted to the Cedar Breaks area and the vicinity of<br />
Bryce Canyon in south-central <strong>Utah</strong> (Madsen 2001).<br />
Today Cedar Breaks National Monument is part of a<br />
network of highly protected areas that conserve biological<br />
diversity. This network includes other NPS units<br />
(national parks, monuments, recreation areas, and historic<br />
sites), designated wilderness areas, research natural<br />
areas, BLM-managed national monuments, and private<br />
nature preserves such as those managed by The Nature<br />
Conservancy. In <strong>Utah</strong>, these lands cover nearly 14% of<br />
the state (Prior-Magee et al. 2007). Though extensive,<br />
the <strong>Utah</strong> network does not yet capture a representative<br />
sample of the full array of the state’s biological diversity.<br />
Protection remains biased towards common and<br />
widespread species and vegetation types of low economic<br />
use (Fertig 2010a, Prior-Magee et al. 2007).<br />
The purpose of this paper is to examine the contribution<br />
of Cedar Breaks National Monument to the state’s<br />
preserve network by comparing the monument’s floristic<br />
composition, species richness (alpha diversity), degree<br />
of endemism, and number of rare species with that<br />
of other parklands. We hope to demonstrate that despite<br />
the monument’s small size, low alpha diversity, and<br />
relatively homogeneous vegetation, Cedar Breaks is<br />
significant because of its large number of plant species<br />
that are not protected elsewhere (i.e., the monument has<br />
high complementarity or beta diversity). We also hope<br />
to show how comparing annotated species checklists<br />
can be useful for identifying and prioritizing specific<br />
taxa that are missing or under-represented in the preserve<br />
network.<br />
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