|A Great Basin bristlecone pine grove|
|The eponymous bristles|
|Subgenus:||P. subg. Strobus|
|Section:||P. sect. Parrya|
|Subsection:||P. subsect. Balfourianae|
The term bristlecone pine covers three species of pine tree (family Pinaceae, genus Pinus, subsection Balfourianae). All three species are long-lived and highly resilient to harsh weather and bad soils. One of the three species, Pinus longaeva, is among the longest-lived life forms on Earth. The oldest of this species is more than 4,800 years old, making it the oldest known individual of any species.
Despite their potential age and low reproductive rate, bristlecone pines, particularly Pinus longaeva, are usually a first-succession species, tending to occupy new open ground. They generally compete poorly in less-than-harsh environments, making them hard to cultivate. In gardens, they succumb quickly to root rot. They do very well, however, where most other plants cannot even grow, such as in rocky dolomitic soils in areas with virtually no rainfall.
Bristlecone pines grow in scattered subalpine groves at high altitude in arid regions of the Western United States. Bristlecones, along with all related species in class Pinopsida, are cone-bearing seed plants commonly known as conifers; the name comes from the prickles on the female cones.
Species and range
There are three closely related species of bristlecone pines:
- Great Basin bristlecone pine (Pinus longaeva) in Utah, Nevada and eastern California. The famous longest-lived species; often the term bristlecone pine refers to this tree in particular.
- Rocky Mountain bristlecone pine (Pinus aristata) in Colorado, New Mexico and Arizona. The most populous species; capable of forming closed canopies and, unlike the other two, is commonly cultivated.
- Foxtail pine (Pinus balfouriana) with two disjunct populations found in the Klamath Mountains (subspecies balfouriana) and the southern Sierra Nevada (subspecies austrina). A small outlying population was reported in southern Oregon, but was proven to have been misidentified. Forms the thickest groves of the three.
At least some of the three species can hybridize in cultivation, but the ranges of wild populations do not overlap. The Colorado River and Green River produce a 160-mile (260 km) gap between the ranges of P. longaeva and P. aristata and the northern Owens Valley provides a 20-mile (30 km) gap between the ranges of P. longaeva and P. balfouriana.
Bristlecone pines grow in isolated groves just below the tree line, between 5,600 and 11,200 ft (1,700 and 3,400 m) elevation on dolomitic soils. The trees grow in soils that are shallow lithosols, usually derived from dolomite and sometimes limestone, and occasionally sandstone or quartzite soils. Dolomitic soils are alkaline, high in calcium and magnesium, and low in phosphorus. Those factors tend to exclude other plant species, allowing bristlecones to thrive. Because of cold temperatures, dry soils, high winds, and short growing seasons, the trees grow very slowly. Even the tree's needles, which grow in bunches of five, can remain on the tree for forty years, which gives the tree's terminal branches the unique appearance of a long bottle brush.
The bristlecone pine's root system is mostly composed of highly branched, shallow roots, while a few large, branching roots provide structural support. The bristlecone pine is extremely drought tolerant due to its branched shallow root system, its waxy needles, and thick needle cuticles that aid in water retention.
The wood is very dense and resinous, and thus resistant to invasion by insects, fungi, and other potential pests. The tree's longevity is due in part to the wood's extreme durability. While other species of trees that grow nearby suffer rot, bare bristlecone pines can endure, even after death, often still standing on their roots, for many centuries. Exposed wood on living and dead trees does not rot, but rather erodes like stone due to wind, rain, and freezing, which creates unusual forms and shapes.
The bristlecone pine has an intrinsically low rate of reproduction and regeneration, and it is thought that under present climatic and environmental conditions the rate of regeneration may be insufficient to sustain its population. The species are on the International Union for Conservation of Nature (IUCN) red list. The species are labeled under Least Concern (LC), the justification for this being that no subpopulations for Great Basin bristlecone pines are decreasing. Subpopulations seem to be increasing or remaining stable. Many bristlecone pine habitats have been protected, including the Inyo National Forest's Ancient Bristlecone Pine Forest in the White Mountains of California and the Great Basin National Park in Nevada, where cutting or gathering wood is prohibited.
The green pine needles give the twisted branches a bottle-brush appearance. The needles of the tree surround the branch to an extent of about one foot near the tip of the limb. The name bristlecone pine refers to the dark purple female cones that bear incurved prickles on their surface. The dark color of these cones helps to absorb heat. After maturity, which takes about two years, the cones will become brown in color. These ancient trees have a gnarled and stunted appearance, especially those found at high altitudes, and have reddish-brown bark with deep fissures. As the tree ages, much of its vascular cambium layer may die. In very old specimens, often only a narrow strip of living tissue connects the roots to a handful of live branches. Even though the trees' needles may age, they still remain functional in regulating water and by their ability to photosynthesize.
Oldest living organisms
Bristlecone pines are known for attaining great ages. The oldest bristlecone pine in the White Mountains is Methuselah, which has a verified age of 4,854 years. It is located in the Inyo National Forest in Eastern California. However, the specific location of Methuselah is a closely guarded secret.
The other two species, Pinus balfouriana and Pinus aristata, are also long-lived, though not to the extreme extent of P. longaeva; specimens of both have been measured or estimated to be up to 3,000 years old. The longevity of the trees is believed to be related to the proportion of dead wood to live wood. This high ratio reduces respiration and water loss, thereby extending the life of the tree.
Trees that reproduce by cloning can be considered to be much older than bristlecone pines. A colony of 47,000 quaking aspen trees (nicknamed "Pando"), covering 106 acres (43 ha) in the Fishlake National Forest in Utah, United States, has been estimated to be 80,000 years old, although tree ring samples date individual, above-ground trees at an average of about 130 years.
Bristlecone pines are invaluable to dendroclimatologists, because they provide the longest continual climatically sensitive tree-ring chronologies on Earth. By cross-dating millennia-old bristlecone pine debris, some chronologies reach beyond 9,000 years before present. In addition, ratios of stable carbon isotopes from bristlecone pine tree rings are sensitive to past variations in moisture availability. This information can be used to reconstruct precipitation changes in the past.
The Rocky Mountain population is severely threatened by an introduced fungal disease known as white pine blister rust, and by mountain pine beetles. Climate change may also affect the species as temperatures increased 0.5–1 °C (0.90–1.80 °F) over a 30-year period throughout the southern Rocky Mountain range. These changes in climate would mostly affect trees in higher elevations. With these problems, the genetic diversity within the species has become a concern; old specimens of bristlecone pine, however, have survived previous warmer periods.
- "Oldlist". Rocky Mountain Tree Ring Research. Retrieved January 8, 2013.
- Howard, JL (2004). "Pinus longaeva". Fire Effects Information System. USDA. Retrieved December 2, 2008.
- Bristlecone pine media from ARKive
- Moore, Gerry; Kershner, Bruce; Tufts, Craig; Mathews, Daniel; et al. (2008). National Wildlife Federation Field Guide to Trees of North America. New York: Sterling. p. 83. ISBN 978-1-4027-3875-3.
- Kauffmann, Michael E. (2012). Conifer Country. Kneeland, CA: Backcountry Press. ISBN 978-0-578-09416-8. OCLC 798852130.
- Fryer, Janet L (2004). "Pinus longaeva". U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory.
- Coop, JD; Schoettle, AW (2009). "Regeneration of rocky mountain bristlecone pine (pinus aristata) and limber pine (pinus flexilis) three decades after stand-replacing fires". Forest Ecology and Management. 257 (3): 893–903. doi:10.1016/j.foreco.2008.10.034.
- Stritch, L.; Mahalovich, M. & Nelson, K.G. (2011). "Pinus longaeva". IUCN Red List of Threatened Species. 2011: e.T34024A9830878. doi:10.2305/IUCN.UK.2011-2.RLTS.T34024A9830878.en. Retrieved January 10, 2020.
- "Global Trees Campaign". March 2008. Retrieved July 30, 2011.
- "The Ancient Bristlecone Pine". August 2003. Retrieved July 30, 2011.
- "Bristlecone pines". U.S. National Park Service.
- "The Gymnosperm Database". March 2008. Retrieved July 30, 2011.
- Kinkead, Gwen (June 17, 2003). "At Age 4,600-Plus, Methuselah Pine Tree Begets New Offspring". New York Times.
- Bain, G. Donald (2001). "Explore the Methuselah Grove". NOVA Online: Methuselah Tree. PBS.
- Grant, Michael C. (October 1, 1993). "The Trembling Giant". Discover Magazine. Retrieved May 8, 2008.
- "Quaking Aspen". National Park Service – Bryce Canyon. Retrieved May 7, 2008.
- Bale, RJ; Robertson, I; Salzer, MW; Loader, NJ; et al. (2011). "An annually resolved bristlecone pine carbon isotope chronology for the last millennium". Quaternary Research. 76 (1): 22–29. Bibcode:2011QuRes..76...22B. doi:10.1016/j.yqres.2011.05.004. S2CID 140565055.
- Robbins, Jim (September 27, 2010). "Old Trees May Soon Meet Their Match". The New York Times.
- Schoettle, AW; Goodrich, BA; Hipkins, V; Richards, C; Kray, J (2012). "Geographic patterns of genetic variation and population structure in pinus aristata, rocky mountain bristlecone pine". Canadian Journal of Forest Research. 42 (1): 23–37. doi:10.1139/x11-152.