Biomes & Communities of the Sonoran Desert Region
World travelers can scarcely help but notice the great diversity of landscapes on this planet. That diversity is as much due to the vegetation as to the landforms. Closer observation reveals a mind boggling diversity of plants and animals in these different places. People who travel in the American Soutwest or on the western side of any other continent near 30° latitude will see dramatic changes within distances of only a few miles.
In apparent contrast, some widely distant parts of planet Earth show certain broad scale similarities. The vegetation of the Mediterranean coast of Europe looks remarkably similar to the chaparral of Southern California, though no two plant species occur in both places (except some introduced weeds). Both the diversity and the similarities have the same underlying causes, namely the interactions between geography and the global climate machine which governs the biosphere on both grand and microscopic scales.
The Sonoran Desert region has a great variety of both species and habitats, the latter ranging from extremely hot, arid desert to semiarid tropical forest to frigid subalpine meadows. Our focus is on the Sonoran Desert in the heart of the region, but to understand it we need to know something about the other habitats that border it. These adjacent geographical features and biological communities exert
profound, complex influences on the desert itself.
Ecologists who study nature on a global scale recognize a few basic, widespread classes of habitats that are easily identified by their dominant plant life forms, which are basic categories based on general appearance, for example, tree, shrub, annual, succulent, and so on. Such global scale habitats are called biomes, and are determined primarily by the climatic factors of temperature and rainfall. These factors are in turn determined by latitude, elevation, and wind patterns. Biome classification is based on vegetation because plants, being generally immobile, are the most obvious and easily recognizable components of a biological community. In addition, plants are more definitive of their biomes because, since they are rooted in place, they must be adapted to that specific environment. Plants, therefore, are often endemic (occurring only in the named area) to a biome or smaller community. Biomes do contain characteristic animal life as well, including many endemic insects and other invertebrates. Most vertebrates, however, are more mobile and rather few species are restricted to a single habitat.
All of the world's biomes occur in the Sonoran Desert region. This tremendous diversity in a fairly small area is due to two influences. For one thing, this region is on the west side of a continent near 30° North latitude, a position where several biomes typically occur in close proximity (a phenomenon explained later in this chapter). Secondly, our great topographical relief creates the cold, wet climates that allow northern biomes to occur farther south than they would ordinarily.
It is important to recognize that biomes and most other biological classifications are largely subjective concepts. an attempt to make sense of the nearly incomprehensible diversity of nature. In addition, their boundaries are rarely distinct. Wherever two biological communities or biomes meet there is usually a zone of intergradation which is sometimes very wide. For these reasons classifications differ among classifiers. For example, some biologists recognize thornscrub as a separate biome while others call it an ecotone (transition zone) between desert and tropical forest. Some combine tropical and temperate forests into the same biome based simply on vegetation height and density. The biomes as defined here are so distinctive that you should be able to place any terrestrial habitat on the planet within one of them at a glance (see plate 1).
Biomes are subdivided into a hierarchy of smaller categories, defined by the particular species that inhabit them. There are many classification systems and the categories have many names. We use the general terms biotic community, biological community, or simply, community. The names used here for the communities are mostly those of Brown and Lowe (1982).
TUNDRA is the most poleward and highest-elevation biome and is characterized by extremely cold winters. The dominant plant life forms are ground-hugging woody shrubs and perennial herbs. Intense cold excludes trees and succulents and the growing season is too short for annuals.
Temperatures become warmer at lower latitudes (toward the equator) at the same elevation. But an increase in elevation at a given latitude has the same climatic effect as does traveling toward a pole: temperature decreases. So a climate that supports tundra, like that in the arctic, can be found on high mountains all the way to the equator. The other cold biomes in both hemispheres also extend toward the equator where sufficiently high elevations meet their climatic requirements. The San Francisco Peaks near Flagstaff, Arizona, rise to 12,600 feet (almost 3900 m). These are the only mountains in our region that extend above timberline (about 11,200 feet, 3400 m elevation in Arizona). There, only forty-five miles (72 km) from the saguaros of the Sonoran Desert, is a small area of alpine tundra that includes some of the same plant species that occur in the arctic tundra of Alaska (see plate 2).
CONIFEROUS FOREST (also known by its Russian name, taiga) is dominated by cone-bearing trees, especially pines, firs, and spruces in the northern hemisphere. Many conifers are adapted to cold only a little less severe than in tundra. Tree height ranges from a few feet (a couple of meters) near the tundra boundary or at timberline to over 300 feet (90 m) in more temperate latitudes. Some coniferous woodlands extend into subtropical climates, for example, in the southeastern United States.
In our region coniferous forest occurs in the higher mountain ranges, mostly to the north and east of the Sonoran Desert. Our most widespread coniferous community is Petran Montane (Rocky Mountain) forest, the dominant vegetation of the cold-temperate Rocky Mountains. Its elevation increases southward into Mexico until it is pushed off the tops of the mountains by excessive aridity and warmth. In the mountains west of the Sonoran Desert are isolated islands of Sierran (as in Sierra Nevada) coniferous forest, characterized by
different conifer species.
TEMPERATE DECIDUOUS FOREST is characterized by dense stands of broadleaf trees that drop their foliage in winter. The winters are milder than those of most conifer-dominated climates, though still too cold for plant growth. Summers are typically warm and humid. There are more species than in the two more poleward biomes. The herbaceous perennial life form is well-represented along with the trees and shrubs. Although pure temperate deciduous forest is rare in our region, it is represented by scattered aspen groves and ribbons of riparian trees.
The foothills and lower mountain slopes east of the Sonoran Desert are wooded with oaks and pines, a mixture of coniferous forest and temperate deciduous forest tree types. The oaks, however, are mostly evergreen species; they are not deciduous except during severe droughts. This Madrean evergreen woodland (also called Mexican oak-pine woodland) is a warm-temperate community of the Sierra Madre Occidental. It extends as far north as central Arizona, where it is squeezed out by the cool-temperate Rocky Mountain forests above it and the more arid grassland and desert below. (Though its official name is woodland, in its southern part it's actually a forest; i.e., the tree canopies overlap.) This is a semiarid community which experiences a dry season in spring (see plate 3).
In the Sonoran Desert region tundra, coniferous forest, and temperate deciduous forest are restricted to mountains that rise well above the intervening basins. In southeastern Arizona and northeastern Sonora there is a gap between the massive Rocky Mountains and the Sierra Madre Occidental. The mountain ranges in this gap are distinct entities separated by intervening valleys. The cool, moist communities on their upper elevations are isolated from one another by "seas" of hot, arid habitat. Because this isolation is analogous to oceanic islands, the terms "mountain islands" and "sky islands" have been coined for these and similar ranges.
GRASSLAND is a semiarid biome characterized by warm, humid summers with moderate rain and cold, dry winters. (The central valley of California is an exception; it is a winter-rainfall grassland at a lower than typical elevation.) Grass is the dominant life form; scores of species form a nearly continuous cover over large areas. Other well-represented life forms are annuals and geophytes (herbaceous perennials such as bulbs that die to the ground each year). Populations of trees, shrubs, and succulents are kept at low levels by periodic fires during the dry season.
Most of the grasslands in the western states are intermediate between the true prairies of the American Midwest and deserts. They are called semi-desert or desert grasslands. (Again the California grasslands are an exception. They are heavily influenced by the unique California floristic province and not much by the Midwest prairies.) Compared with prairie grassland, the grasses in desert grassland are shorter, less dense, and are more frequently interspersed with desert shrubs and succulents. Desert grassland or chaparral borders the northern Sonoran Desert on the east (see plate 4).
CHAPARRAL is a semiarid biome that occurs on the west coast of every continent between about 30° and 40° North latitude. This smallest biome is unique for its Mediterranean climate: mild, moist winters and hot, dry summers. Mature chaparral consists almost solely of woody evergreen shrubs with small leathery leaves. The numerous species form impenetrable thickets from five to eight feet (1.5 to 2.5 m) tall. During the long dry summers the typically resinous foliage and dry woody stems become explosively combustible.
Wildfires raze large areas to ash-covered earth every few decades. Fires are not harmful to this community; they are in fact necessary for maintaining its vigor. Following fires the bare ground is briefly colonized by a large number of annual species, but the land is soon reclaimed by the shrubs which sprout from seeds or root crowns. Trees and succulents are rare life forms in chaparral because they are more vulnerable to destruction by the very hot fires.
This young biome evolved from early Tertiary tropical forest during the Pliocene and Pleistocene. The uplift of the great mountain ranges of western North America blocked the summer monsoon moisture from reaching the far west, creating a summer dry season (see chapter on "Deep History of the Sonoran Desert" ).
The main area of chaparral occurs west of the coast, transverse, and peninsular ranges and is called Californian chaparral (see plate 5). Disjunct patches of chaparral occur inland of these ranges and are called interior chaparral. Interior chaparral differs in having only a few species; it is often comprised almost entirely of manzanita (two species of Arctostaphylos) and shrub live oak (Quercus dumosa). Interior chaparral also receives substantial summer rainfall, though the plants do not respond to it.
California chaparral borders the western edge of the Sonoran Desert in
California and northern Baja California, and interior chaparral is scattered along the desert's northeastern edge where it meets the Mogollon Rim of Arizona. Interior chaparral also occurs in isolated patches on the lower slopes of some mountain islands.
DESERT is the driest biome, its vegetation is determined solely by the extreme aridity. Temperature and seasonality of rainfall determines the specific vegetation and fauna, but all desert vegetation looks more or less similar; most plants are widely spaced and have small or absent leaves (see plate 6). A detailed discussion of deserts follows this section.
THORNSCRUB is intermediate between the desert and tropical forest biomes. The vegetation consists largely of short trees, ten to twenty feet (3-6 m) tall,
and shrubs, with cacti also being common in the "New World" communities. It is generally more dense and taller than desert vegetation, and many species are thorny. Annuals and herbaceous perennials are abundant, and vines. a primarily tropical life form. are well represented. During the dry
season most perennial plants are drought-deciduous (as opposed to plants of more temperate regions which are cold-deciduous). In contrast, the rainy season, though short, is moderate and dependable and the vegetation grows lush. The climate is nearly frost-free, so temperature is not limiting; the vegetation is determined by the alternating dry and wet seasons (see plate 7).
TROPICAL FOREST is determined by the absence of freezing temperatures and the occurrence of ample rainfall for at least part of the year. Some tropical forests have a dry season, while tropical rain forest is never stressed for water. Tropical deciduous forests have a dry season lasting from three to nine months, during which time many of the plants become deciduous. Many of the tree species flower during the winter-spring dry season while leafless. In the rainy season the dense vegetation grows luxuriantly and forms closed canopies of foliage. The upper canopy ranges from fifteen to thirty feet (4.5 to 9 m) above ground in dry forests, to 150 feet (45 m) in lowland rain forests. Almost all life forms are represented, though annuals are nearly absent from rainforest. Flowering epiphytes (plants that grow on other plants or rocks but are not parasitic) are almost completely restricted to tropical habitats, and are a major component of wet tropical floras (see plate 8).
To the south, the Sonoran Desert merges almost imperceptibly into thornscrub in central Sonora, and thornscrub in turn merges with the northern limit of tropical deciduous forest in the southern tip of that state. A major proportion of the Sonoran Desert's biota evolved from ancestors in these tropical biomes; examples are noted in the species accounts.
Riparian communities are not biomes. Though they could be considered isolated ribbons of deciduous forest, they are better viewed as a unique habitat type. They occur within any biome wherever there is perennial water near the surface. The term riparian specifi-cally refers to the zones along the banks of rivers; however, it is also applied to the shoreline communities along slow or nonflowing waters such as marshes and lakes.
The drier the surrounding habitat, the more distinct is the riparian zone. In the desert or grassland a flowing stream supports a conspicuous oasis with forests and wildlife that would not otherwise occur in the area. The available water also augments populations of more arid-adapted species in the adjacent habitat.
|TREES||None||Some||Many||Few||None to Some||Many||Many|
|SUCCULENTS||None||Few||Few||Some||None to Many||Many||Some|
|VINES||None||Few||Few||Few||None to Some||Many||Many|
|FLOWERING EPIPHYTES||None||None||None||None||None||Some||Some to Many|
Riparian zones are so different at different latitudes and elevations that they should be thought of as several communities with similar physical characteristics, primarily their dependence on perennial water. Montane streams support alder and aspen, while at lower elevations there are cottonwoods and sycamores. In tropical deciduous forests a riparian zone may be visually indistinguishable during the wet season because the overall appearance of stream-bank and hillside trees is similar, though the species may be different. But in the dry season most of the slope vegetation is deciduous, while tropical riparian species are typically evergreen.
Some ecologists broaden the concept of riparian communities to include the banks of dry washes in deserts. A wash in the Lower Colorado River Valley with its woodland of palo verdes (Cercidium spp.), ironwoods (Olneya tesota), and desert willows (Chilopsis linearis) is clearly distinct from the surrounding creosote bush flats. These dry washes occupy less than five percent of the area of this subdivision of the Sonoran Desert, but support ninety percent of its bird life. This concentration of life is the result of the greater availability of water, even though the wash may carry surface water for only a few hours a year. Desert drainageways should be labeled "dry riparian" or "desert riparian" to avoid confusion with wetter habitats that have surface water all or most of the year.
Dry riparian habitats share most of their defining characteristics with traditional "wet" riparian habitats. They are chronically disturbed, unstable sites where water and nutrients are harvested and concentrated from larger areas (watersheds). Finally, they are corridors for dispersal of plants (seeds) and animals (see plate 9).
What Is a Desert?
Although many people visualize deserts as dry, desolate wastelands, the term actually defines a wide spectrum of landscapes and plant and animal population densities. The Sonoran Desert does have seas of sand and expanses of desert pavement that are nearly devoid of visible life, but most of it is more reminiscent of a sparse woodland savanna.
The common denominator of all deserts is extreme aridity water is freely available only for short periods following rains. Desert is often defined as a place that receives less than ten inches (250 mm) of annual average rainfall, but this definition is inadequate. For example, the Pacific coast of northern Baja California and the north slope of Alaska both receive less, but those places are vegetated with chaparral and tundra, respectively. An accurate measure of aridity must compare rainfall (abbreviated P for precipitation) with potential water loss through evaporation and transpiration (the loss of water from leaves). Potential evapo-transpiration (abbreviated pet, the water that would be lost from evaporation and transpiration if water were present to evaporate) is difficult to measure accurately, but is crudely estimated to be sixty percent of pan evaporation (the water that evaporates from a wide pan of water exposed to the weather). Pan evaporation varies severalfold within a local area depending on slope and exposure to wind, so it is applicable only to the specific site where it is measured. Tucson receives an average of twelve inches (305 mm) of rain a year, while the pan evaporation is about 100 inches (254 cm). In other words, the climate of Tucson could evaporate eight times more water per year than is supplied by rain, a pan evaporation to precipitation ratio of 8:1. Using the sixty percent estimate for PET, Tucson's PET/p ratio is 4.3; climatologists classify areas with ratios higher than 3.0 as semiarid. This moisture deficit presents a significant challenge to the biota, but is not large compared to that of hyperarid deserts such as that around Yuma, Arizona which has a PET/p ratio of 30, or the interior Sahara Desert's 600.
A concise nontechnical definition of a desert is "a place
where water is severely limiting to life most of the time." (Without the word "severely" the phrase defines semiarid habitats such as grassland, chaparral, and tropical deciduous forest.) Though desert plants and animals must cope with scarce water, the common perception that they are struggling to survive is grossly inaccurate. The native biota are adapted to and usually thrive under these conditions and, in fact, most of them require an arid environment for survival. Look at it this way: if a desert received much more rain, it wouldn't be a desert.
A different, wetter, biome would replace it. Thus an alternative and more positive definition might be: "A desert is a biological community in which most of the indigenous plants and animals are adapted to chronic aridity and periodic, extreme droughts, and in which these conditions are necessary to maintain the community's structure." (The desert biome requires chronic aridity, but not all of its component species do.)
Why Are Deserts so Dry?
The low rainfall typical of deserts is more easily understood if one knows a little about the basics of global climate. Atmospheric thermodynamics is an extremely complicated field, but the basic rules are simple. First, hot air rises and cool air sinks. Second, rising air expands and cools, while sinking air compresses and becomes warmer. Third, warmer air can hold more water vapor than cooler air. These three natural phenomena plus the sun's heat determine where rain falls on the planet.
The sun shines almost vertically on the equatorial belt year round, but it shines on the polar regions at a shallow angle and only in the summer of each respective pole. There are two consequences. A beam of sunlight ten square feet (1 m2) shines on about ten square feet of Earth's surface at the equator at noon, but it covers more than twice that area near the poles. The sun's light and heat are thus less concentrated at higher latitudes. In addition, at the equator the sunlight travels straight down through the atmosphere, but near the poles it travels through much more air where more of the light is reflected, absorbed, or scattered and less reaches the ground. This is why the equator is hot and the poles are cold.
Because of the great quantity of heat delivered to the equatorial belt, it is a zone of warm, rising air. It absorbs much water vapor from the oceans and land vegetation. As this air rises it cools. Eventually it reaches saturation (dewpoint temperature) and water vapor condenses into clouds and often falls as rain. So the equatorial region is both hot and wet.
The equatorial air rises, then spreads horizontally at high elevations to the north and south. Eventually the now cool air sinks and flows along the surface to replace the rising air at the equator, forming a circulation cell. It tends to sink at about 30° north and 30° south latitude. (These two zones were called the "horse latitudes" by mariners. Before motorpower, sailing vessels could get becalmed in these latitudes for weeks at a time. To reserve precious water for themselves, the crew threw horses and other livestock overboard; other ships would encounter the floating carcasses.) As the air sinks it warms by compression, and because there is no source of evaporating water, it becomes drier with increasing temperature. Not only can sinking air not produce rain, but when it reaches the ground it absorbs water from the soil and vegetation, creating even more arid conditions.
The horse latitude zones of sinking air are not continuous belts. The combination of the Earth's rotation and the interaction between land masses and oceans creates stable high pressure zones (sinking air) over the oceans west of the continents. The resulting aridity is reinforced by the cold ocean currents that also occur on western coasts at this latitude; the cold water further inhibits the potential for rising air currents that are necessary to make rain. Thus on the west edge of every large land mass there is a hyperarid area near 30° latitude called a horse latitude desert. Despite the proximity of the oceans, the high pressure zone is so strong over the Atacama and Sahara deserts that decades may pass without rain.
|Deserts of the world (white areas). Horse latitude deserts are those on the western edges of all the continents near 30° north and south latitude. The rest are rain shadow deserts. The difference between the two types can be seen in South America, where the Andes Mountains stretch the entire length of the continent near the west coast. North of 30° the trade winds blow from the northeast, causing a rain shadow desert on the west or coastal side of the Andes. South of 30° the easterlies blow onshore and the rain shadow desert is on the eastern, inland, side of the Andes. Near the 30th parallel there is no prevailing wind; the stable high pressure zone creates horse latitude deserts on both sides of the Andes Mountains.|
Deserts are also caused by rain shadow effects wherever there are mountains and prevailing winds. Where wind encounters a mountain, it is forced up and over. As it rises, it cools and drops most of its moisture on the windward slope. On the leeward side it descends, warms, and dries. At latitudes that have a prevailing wind direction, rain shadow deserts are created on mountains' lee sides.
Aridity is the primary attribute of deserts, but it also generates several other characteristics of deserts. In addition to being meager, desert precipitation is also highly variable and unpredictable. The more arid the desert, the more variable is its rainfall. The average annual precipitation is a poor predictor of the rainfall in a given year. For example, Yuma, Arizona has an average annual rainfall of three and one-half inches (90 mm), but in most years it receives less, sometimes none at all. When the stable weather pattern that enforces aridity breaks down occasionally, Yuma may receive two or three times its annual average, sometimes in a single storm.
Desert temperatures vary widely both daily and seasonally. The dry, transparent air and cloudless skies transmit maximal solar energy to the ground where much of it is absorbed and converted to heat; the temperature rises dramatically. At night the same conditions permit most of this heat to be radiated to the sky, and the temperature plummets. (Water vapor, either as humidity or cloud cover, reflects infra-red heat and slows heat loss.) Daily temperature variation can be more than 50°F (28°C). The same conditions create great seasonal fluctuation. High-elevation deserts that have 100°F (38°C) days in summer can experience nights below 0°F (-18°C) in winter.
Besides the heat it creates, the intense sunlight in arid lands is itself
a challenge. The ultraviolet radiation can damage animals. retinas, cause skin cancer, and destroy vital plant molecules such as chlorophyll. Desert organisms have evolved a variety of adaptations to avoid getting too much sun.
The North American Deserts
North America has four major deserts: Great Basin, Mohave, Chihuahuan and Sonoran. All but the Sonoran Desert have cold winters. Freezing temperatures are even more limiting to plant life than is aridity, so colder deserts are poorer in both species and life forms, especially succulents.
The Great Basin Desert (plate 10) is both the highest-elevation and northernmost of the four and has very cold winters. The seasonal distribution of precipitation varies with latitude, but temperatures limit the growing season to the summer. Vegetation is dominated by a few species of low, small-leafed shrubs; there are almost no trees or succulents and not many annuals. The indicator plant (the most common or conspicuous one used to identify an area) is big sagebrush (Artemisia tridentata), which often grows in nearly pure stands over huge vistas. (Such cold shrub/deserts in the "Old World" are called steppes.)
The Mohave Desert (plate 11) is characterized largely by its winter rainy season. Hard freezes are common but not as severe as in the Great Basin Desert. The perennial vegetation is composed mostly of low shrubs; annuals carpet the ground in wet years. There are many species of these two life forms, but few succulents and trees grow there. The only common tree species is the characteristic joshua tree (Yucca brevifolia), an arborescent (treelike) yucca that forms extensive woodlands above 3000 feet (900 m) elevation.
Though the Chihuahuan Desert (plate 12) is the southernmost, it lies at a fairly high elevation and is not protected by any barrier from arctic air masses, so hard winter freezes are common. Its vegetation consists of many species of low shrubs, leaf succulents, and small cacti. Trees are rare. Rainfall is predominantly in the summer, but in the northern end there is occasionally enough winter rain to support massive blooms of spring annuals. The Chihuahuan Desert is unexpectedly rich in species despite the winter cold.
The Sonoran Desert
The Sonoran Desert as currently defined covers approximately 100,000 square miles (260,000 sq. km) and includes much of the state of Sonora, Mexico, most of the southern half of Arizona, southeastern California, most of the Baja California peninsula, and the islands of the Gulf of California. Its southern third straddles 30° north latitude and is a horse latitude desert; the rest is rain shadow desert. It is lush in comparison to most other deserts. The visually dominant elements of the landscape are two life forms that distinguish the Sonoran Desert from the other North American deserts: legume trees and large columnar cacti. This desert also supports many other life forms, encompassing a rich spectrum of some 2000 species of plants, 550 species of vertebrates, and unknown thousands of invertebrate species.
The amount and seasonality of rainfall are defining characteristics of the Sonoran Desert. Much of the area has a bi-seasonal rainfall pattern, though even during the rainy seasons most days are sunny. From December to March frontal storms originating in the North Pacific occasionally bring widespread, gentle rain to the northwestern two-thirds. From July to mid-September, the summer monsoon brings surges of wet tropical air and localized deluges in the form of violent thunderstorms to the southeastern two-thirds. So distinct are the characters of the two types of rainfall that Sonoran residents have different Spanish terms for them. the winter rains are equipatas (derived from the Yaqui-Mayo word for rain, quepa), the summer rains are las aguas ("the waters" in Spanish).
The Sonoran Desert prominently differs from the other three North American deserts in having mild winters. Most of the area rarely experiences frost, and the biota are partly tropical in origin. Many of the perennial plants and animals are derived from ancestors in the tropical thornscrub to the south, their life cycles attuned to the brief summer rainy season. The winter rains, when ample, support great populations of annuals (which make up nearly half of
the species of our plants). Some of the plants and animals are opportunistic, growing or reproducing after significant rainfall in any season (see the chapter "Deep History of the Sonoran Desert" for more details on
Subdivisions of the Sonoran Desert
Forrest Shreve was the first person to define the Sonoran Desert by dividing it into seven subdivisions, based on the diverse and distinctive vegetation found here. One of Shreve's subdivisions (the Foothills of Sonora) has since been reclassified as foothills thornscrub, a non-desert biome.
Lower Colorado River Valley
Named for its location surrounding the lower Colorado River in parts of four states, this is the largest, hottest, and driest subdivision. It challenges the Mohave Desert's Death Valley as the hottest and driest place in North America. Summer highs may exceed 120°F (49°C), with surface temperatures approaching 180°F (82°C). The intense solar radiation from cloudless skies on most days and the very low humidity suck the life-sustaining water from plants, water that cannot be replaced from the parched mineral soil. Annual rainfall in the driest sites averages less than three inches (76 mm), and some localities have gone thirty-six months with no rain. Even so, life exists here, abundantly in the rare wet years.
The terrain consists mostly of broad, flat valleys with widely-scattered, small mountain ranges of almost barren rock. There are also seas of loose sand and the spectacular Pinacate volcanic field (see plate 14). The valleys are dominated by low shrubs, primarily creosote bush (L. tridentata) and white bursage (Ambrosia dumosa). These are the two most drought-tolerant perennial plants in North America, but in the driest areas of this subdivision even they are restricted to drainageways. Trees grow only along the larger washes. The mountains support a wider variety of shrubs and cacti, but the density is still very sparse. Columnar cacti, one of the indicators of the Sonoran Desert, are rare (virtually absent in California) and are restricted to valley floors. Annual species comprise over half the flora, up to ninety percent at the driest sites; they are mostly winter growing species and appear in large numbers only in wet years (see plate 13).
This is the only part of the Sonoran Desert that extends into California, where most residents call it the Colorado Desert. North of a sagging line between the Coachella Valley (Palm Springs) and Needles, California, it merges almost imperceptibly into the lower Mohave Desert.
|Subdivisions of the Sonoran Desert. The six subdivisions reflect the biological diversity of this large desert and the fact that it has been intensively studied. Each subdivision has a different climate, topography, and vegetation.|
This northeastern subdivision is the highest and coldest part of the Sonoran Desert. Located in south-central Arizona and northern Sonora, the terrain contains numerous mountain ranges, and valleys narrower than those of the Lower Colorado River Valley subdivision. Trees are common on rocky slopes as well as drainageways, and saguaros grow on slopes above the cold valley floors. This community is also called the "saguaro-palo verde forest". It is the only subdivision that experiences frequent hard winter frosts, so many species of the lower elevation and more southerly subdivisions cannot survive here. Nevertheless it is a rich area. The small range that is the Desert Museum's home, the Tucson Mountains, has about 630 taxonomically distinct kinds of plants. This richness is partly explained by the two equal rainy seasons which total twelve inches (305 mm) per year on average. The hilly terrain provides a multitude of microhabitats on north and south slopes and deep, shaded canyons. The proximity to chaparral, woodland, and grassland communities contributes still more species to the flora (see plate 15).
Biologists are increasingly concluding that the Arizona Upland's climate, vegetation density, and biodiversity resemble thornscrub more than desert. Don't be surprised if this subdivision is reclassified in the near future.
Tucson is the only major city located in Arizona Upland, although much of metro Phoenix's parks and land above 2000 feet (600 m) in elevation share its characteristics. Residents who have moved to this area from temperate climates often complain about the lack of seasons. Actually Arizona Upland has five seasons which, though more subtle than the traditional temperate four, are distinct if one learns what to look for.
The following description is for Tucson, but is fairly applicable to the rest of Arizona Upland and to the eastern one-half of the Lower Colorado River Valley subdivision as well. The seasons are a little later at higher latitudes and elevations, earlier at lower ones. The monsoon is later and more sporadic farther west; in some years it fails to reach the Colorado River.
SUMMER MONSOON or summer rainy season (early July to mid-September). In local native tradition, the year begins with the most dramatic weather event of the region the often abrupt arrival of the summer rains (plate 16). A tropical air mass brings humidity and moderates the temperatures from June's extremes; frequent thunderstorms occur; this is the main growing season for many of the larger shrubs and trees. (Monsoon is derived from an Arabic word for " season", and was applied to a wind that changes directions seasonally. Be aware that it does not refer to rain or storms per se, but rather to the shift of wind direction which brings moist air that can generate storms in our case, a southerly wind in July. The word is often misused, even by some weather reporters.)
A sixth season, late summer, lasting from mid August through September, is sometimes added; this is a hot and dry period after the monsoon ends nonexistent in some years.
AUTUMN (October & November). Warm temperatures; low humidity; little rain; few species in flower, but the growing season for winter annuals begins if there is enough rain. Late summer and autumn occasionally receive heavy rains from the remains of Pacific hurricanes (tropical storms).
WINTER (December & January; sometimes February). Mostly sunny, mild days, with intermittent storms that bring wind, rain, and cool-to-cold temperatures; February often warm and dry, more spring-like (see plate 17).
SPRING (early to late February through April). Mild temperatures; little rain; often windy; one of two flowering seasons; winter annuals may start blooming in February in warm, wet years (see plate 18).
FORESUMMER (May & June). High temperatures; very low humidity; no rain in most years; May is very warm and often windy; June is hot and usually calm. There is little biological activity except for the flowering and fruiting of saguaro and desert ironwood. Most plants and many animals are dormant until the rains arrive (see plate 19).
Plains of Sonora
This small region of central Sonora is a series of very broad valleys between widely separated ranges. It supports denser vegetation than does Arizona Upland because there is more rain (with summer rain dominant) and the soils are generally deeper and finer. It contains most of the same species as Arizona Upland, plus some tropical elements, because frost is less frequent and less severe. There are abundant legume trees, especially mesquite, and relatively few columnar cacti. The few hills in this region support islands of thornscrub. Most of this subdivision has been converted to agriculture in the last few decades.
Central Gulf Coast
The Central Gulf Coast occupies a strip along both sides of the Gulf of California. Extreme aridity dictates the distinctive appearance of this subdivision. It straddles the horse latitude belt, and desert vegetation grows right to the seashore. Small shrubs are nearly absent; their shallow root systems and lack of water storage cannot sustain them through the droughts which commonly last for several years. Dominating the vegetation are large stem-succulents, particularly the massive cardón (Pachycereus pringlei, a giant relative of the saguaro), and trees such as palo verde, tree ocotillo (Fouquieria diguetii and F.
macdougalii), ironwood, elephant tree (Bursera spp.), and limberbush (Jatropha spp.); the trees are leafless most of the time. The average annual rainfall of less than five inches (125 mm) occurs mostly in summer, though not dependably enough to call it a rainy season. A year with no rain is not rare (see plate 20).
The Vizcaino subdivision is on the Pacific side of the Baja California peninsula. Though rainfall is very low, cool, humid sea breezes with frequent fog ameliorate the aridity. Winter rain predominates and averages less than five inches (125 mm). This subdivision contains some of the most bizarre plants and eerily beautiful landscapes in the world. There are fields of huge, sculpted white granite boulders or black lava cliffs that shelter botanical apparitions such as boojums (Fouquieria columnaris), twisted and swollen Baja elephant trees (Pachycormus discolor), sixty-foot (18 m) tall cardones, strangler figs (Ficus petiolaris ssp. palmeri) that grow on rocks, and blue palm trees (Brahea armata). In stark contrast, the coastal Vizcaino Plain is a flat, cool, fog desert of shrubs barely a foot tall, with occasional mass blooms of annual species (see plates 21 and 26).
Located in coastal Baja California south of the Vizcaino, Magdalena is similar in appearance to the Vizcaino but the species are somewhat different. Most of its meager rainfall comes in summer and the aridity is modified by Pacific breezes. The bleak coastal Magdalena Plain's only conspicuous endemic plant is the weird creeping devil cactus (Stenocereus eruca), but inland the rocky slopes are rich and dense with trees, succulent shrubs, and cacti (see plate 22).
Foothills of Sonora
This was Shreve's seventh subdivision of the Sonoran Desert. It has since been reclassified as foothills thornscrub community and is no longer considered part of the desert biome because of its greater rainfall, taller trees and cacti, and denser vegetation.
Shreve's delineation of the Sonoran Desert's boundary and subdivisions are the most widely accepted. There are at least five other major attempts to define this area with dramatically differing boundaries. One version excludes most of Baja California from the Sonoran Desert. Another includes the Mohave as part of the Sonoran Desert. (Indeed, it is difficult to distinguish the two along the currently accepted boundary.) These differences of interpretation reflect the great diversity of geography and biota found here.
The discussion is not yet over. Time will determine whether Arizona Upland and the Plains of Sonora will remain parts of the Sonoran Desert or be reclassified as thornscrub. Whatever they are called, all of these regions are fascinating places for nature lovers, whether they are classified as scientists or tourists.
Brown, David E., ed. Biotic Communities: Southwestern United States and Northwestern Mexico. Salt Lake City: University of Utah Press, 1994.
Dunbier, Roger. The Sonoran Desert: Its Geography, Economy, and People. Tucson: University of Arizona Press, 1968.
Lowe, Charles H. Arizona's Natural Environment: Landscapes and Habitats. University of Arizona Press, 1964.
Shreve, Forrest. Vegetation of the Sonoran Desert. Washington, D.C.: Carnegie Institution of Washington, 1951.
Shreve, Forrest and Ira L Wiggins. Vegetation and Flora of the Sonoran Desert. Stanford: Stanford University Press, 1964.