Nature Notes From Crater Lake
Volume 31, 2000
Why So Many Siskiyou Plants?
By John Roth
The Klamath-Siskiyou Ecoregion,
hereafter KSE, is an oblong area that extends from Roseburg in
southwestern Oregon to the Yolla Bully range in northwestern California.
The varied geology, location, and microclimates of the KSE accelerated
plant evolution and migration but slowed extinction. At least 3,000
types of plants and all the major forest types in western North America
occur here. More than 200 of these plants are KSE endemics, the name for
a species found only in a particular area. Oregon Caves National
Monument, as a small but important zone of transition in the KSE,
illustrates this floral diversity by boasting almost one plant species
per acre.1
Geologic controls
Ocean basins were spread apart or
squeezed for more than half a billion years while molten magma
crystallized into rocks as different as basalt and granite. Erosion and
metamorphism created another range of strata as well: sandstone, marble,
pebbly conglomerate, glacial silt, and "baked" muds. Faults uplifted and
split rock masses apart, changing what once were islands and ocean
basins into a complex rock mosaic. This fragmentation of habitat favors
small populations on each type of soil or rock, a situation in which
mutations that give rise to new species are not diluted out of existence
by interbreeding with large populations.

A stand of Port Orford-Cedar near Oregon
Caves. |
Peridotites are rocks with potent
quantities of minerals like iron and magnesium that change to metal-rich
serpentine when hot water is added. Since most life is not adapted to
metals normally found deep in the earth, these metals disrupt
photosynthesis and inhibit microbes. The most toxic may be nickel,
chromium, and cobalt though plant distribution in the KSE seems to be
governed by the occurrence of magnesium. Little soil forms because clays
need aluminum, an element lacking in serpentine. This and the toxicity
of metals in serpentine will not allow clay, organics, or soil clumps to
hold water, The cycle snowballs and becomes a situation where thin soils
are often dry, hot, and nutrient-poor. This provides open habitat,
increases population turnover, and thus encourages the evolution of new
species. Because their populations are smaller, species that are rare
usually evolve faster than common and/or widespread plants. Of the 200
endemic plant types in the KSE, 141 are either rare or uncommon, a very
high ratio for endemics.
The low productivity of serpentine
soils limits the dispersal of endemics to new areas because of fewer
pollen grains, seeds, or tall plants. Seeds in serpentine tend to be
larger because of being in such stressful habitat, so as to give
seedlings a head start on life. This characteristic may also limit
dispersal, thus increasing the number of endemics.
The most common response for most
plants on serpentine is to keep nickel out of their cells. Even some
mariposa lillies and wild buckwheats living on non-serpentine soils
tolerate high amounts of normally toxic metals, so they appear better
prepared for evolving new species on serpentine soils, Some KSE plants
have found other ways to avoid serpentine toxicity. In an endemic
pennycress mustard and jewel flower, the plant stores nickel within its
cell tissue. Another jewel flower (Streptanthus tortuosus) has
developed a race of serpentine-tolerant plants and so may be on its way
to becoming a new species.
Rapid evolution is also indicated by
the fact that roughly two-thirds of KSE endemics are varieties or
subspecies that likely are on their way to becoming full species. The
crowding of habitats in the KSE results in many hybrids, some of which
have given rise to new species.
An avenue for plant migration

Imperial Lewisia. Drawing by Heather
McDonald. |
The KSE is unusual in that it has more
serpentine than any other ecoregion. The serpentine masses and size of
the KSE helps plant migrants find suitable habitats more easily but are
big enough to keep extinction rates low. Serpentine in the Illinois
Valley, for example, is fragmented and possesses different
chemistries—an ideal situation for rapidly evolving small populations.
The effects of fire or other disturbances may be so long lasting that
plant populations are separated sufficiently and can evolve into new
species. By the same token, disturbances in the KSE are not so large and
competition among plants is not intense enough for extinction rates to
increase. Varied rainfall amounts, frequent burns, and areas that serve
as barriers (riparian zones, serpentine, cliffs, north slopes) tend to
limit fires to patches of moderate size and intensity. Consequently, no
one successional stage dominates with its restricted number of species.
Another reason for the relatively high
species diversity in the KSE is because it contains the only mountains
linking coastal ranges in California and Oregon with the Cascade-Sierra
cordillera. Plants more easily cross over east-west oriented mountains,
unlike north-south ranges where plants must migrate along lines of
longitude if they cannot cross high elevations. Migration can promote
speciation because it produces numerous small and isolated populations
near the range limit of a species, a situation common in the KSE.
Proximity to the endemic-rich Cascades, Sierra, and the coast ranges of
northern California has increased plant diversity as the KSE shares over
200 endemics with these physiographic regions. At least half of those
plants probably originated in the KSE.

Vollmers Tiger Lilly. Drawing by Heather
McDonald. |
Extinction is low among shrubs and
trees generally, furnishing an important reason why they comprise many
of the paleoendemics, or "living fossils." If you live a long time, you
have more chance of reproducing at least once successfully. Even
serpentine herbs tend to be long-lived, a trait indicative of harsh
environments, and one the likely increases the number of endemics.
During the great climate changes over the last few million years, the
closely packed habitats of the KSE allowed plants to grow in adjacent
habitats that increased the chances for survival when the climatic
regimes shifted. Some habitats shrank considerably, but paleoendemics in
them continued to thrive. Port Orford-cedar and Brewer (or weeping)
spruce are examples of paleoendemics that once had more extensive
ranges.
Another type of endemic commonly found
in the KSE is the edaphic endemic or geoendemics—those species mostly
restricted to one soil type or topographic situation. Neoendemics
(plants with no nearby relatives) in the KSE also appear to be more
common near the north end of their range at high elevations, perhaps
because they are also glacial relicts that found suitable cool and open
habitats to colonize. Among the endemic plants in the KSE, 80 types are
found only on serpentine, while seven are confined to granite, four on
marble, and three on volcanic rock.
Other factors promoting diversity
A lack of nutrients and water (up to a
point) encourage greater diversity because plants then spend more of
their energy surviving such conditions rather than competing with other
plants and causing them to become extinct. The leaching of soil
nutrients through high temperatures and rainfall lowers the productivity
of soils and may increase the diversity of herb. Since the KSE is
characterized by low rainfall during the growing season for herbs,
habitat diversity is heightened because there are marked differences in
slope and aspect that control evapotranspiration and the water retention
capacity of soils.
More nutrients and water allow certain
plants to dominate and thus reduce plant diversity, the so-called
paradox of enrichment. The KSE is an area of climatic extremes, with
annual rainfall amounts ranging from 100 inches near the ocean to 15
inches further inland. The differences in rainfall gives rise to a
patchy distribution of plants, with the many subspecies and varieties of
certain plants indicate rapid speciation—especially in their adaptation
to dry soils of serpentine, marble, and granite. For example, dwarf
ocean spray, myrtle, buckthorn, and tanoak stay small in stature even if
grown in gardens with lots of water. Drought adaptations in endemic
plant species include large tubers (as in lillies and toothworts),
woodiness (as in pussytoes and pincushion), and waxy, hairy or divided
leaves. Storing carbon dioxide at night so that water is not lost
through leaf pores by day has favored many endemic sedums and lewisias.
The varied habitats and climate change
over thousands or millions of years resulted in 50 or more disjunct
species, plants whose brothers or population centers are hundreds of
miles distant. Mutations are favored in such situations because of their
small populations and the need for new adaptations to survive in a less
than ideal habitat. The KSE also hosts at least 100 plant species at the
edge of their range, where speciation most likely occurs due to isolated
populations undergoing rapid change. Being at the right location between
northern and southern plant communities, the KSE is situated so as to
have a high number of disjunct species as well as plants at their
geographic limit.
As a refuge for plants that once ranged
from Japan to Georgia, the KSE provides rare habitat in the western
United States. Many of the plant relicts are members of old families:
heathers, orchids, honeysuckles, birthworts, and lillies. Plants such as
fairybells, woodland stars, dogwoods, rhododendrons, redwoods,
trilliums, gaultheria, and coralroots have their greatest diversity of
species in the northwest and southeast United States, as well as in
eastern Asia. Paleoendemics evolved once tectonic forces and climate
changes cut the connections to other landmasses. Trees such as Port
Orford-cedar and Baker cypress, for example, have "twin" species in
Asia. Likewise, cousins of plants in the KSE such as vanilla leaf,
tanoak, Oregon grape, redwood, and skunk cabbage grow in eastern Asia.
Conclusion

California Lady Slipper. Drawing by Heather
McDonald. |
The KSE enjoys the best of diversity
among plants; it contains older flat areas where the lack of major
disturbances has allowed paleoendemics to survive, but also provides
newer habitats like cliffs and cirque lakes where new species can evolve
due to isolation and a lack of competition. Northern Florida may possess
more paleoendemics and Hawaii has greater numbers of neoendemics than
the KSE. Parts of Nevada and Arizona display more edaphic endemics, but
the distinctiveness of the KSE lies in its mix of all three types of
endemic plants—more profuse than anywhere north of Mexico. In few other
places will the location, size, varying ages and geodiversity of
mountains with their varied climates combine to produce so many relicts,
disjuncts, endemics, varieties, hybrids, and plants near their
geographic limit. The Illinois Valley is a botanist's delight each
spring, while Oregon Caves constitutes a representative slice of the
fascinating floral diversity found throughout the KSE.
Note
1The monument list contains some 400 plant species in
only 480 acres, whereas Crater Lake National Park boasts fewer than
700 in 183,220 acres.
John Roth became fascinated with
the plants of southwestern Oregon upon arriving at Oregon Caves National
Monument in 1988.