Pando (tree)

Pando (Latin for "I spread")[1] is a clonal organism representing an individual male quaking aspen (Populus tremuloides). It was identified as a single living organism because its parts possess identical genetic markers[2] and it is assumed to have a massive interconnected underground root system. The plant is located in the Fremont River Ranger District of the Fishlake National Forest at the western edge of the Colorado Plateau in south-central Utah, United States, around 1 mile (1.6 km) southwest of Fish Lake.[3] Pando occupies 108 acres (43.6 ha) and is estimated to weigh collectively 6,000 tonnes (6,000,000 kg),[4] making it the heaviest known organism.[5][6]

Pando
Image of the approximate land mass of Pando shaded green
Map
Map showing the location of Pando
Map showing the location of Pando
Location in Utah
Map showing the location of Pando
Map showing the location of Pando
Location in the United States
Geography
LocationFishlake National Forest, Utah, United States
Coordinates38°31′30″N 111°45′00″W
Area108 acres (43.6 ha)
Administration
Established+14,000 BP
Ecology
Dominant tree speciesPopulus tremuloides
Pando aspen grove at Fishlake National Forest

Pando's long-term survival is uncertain due to a combination of factors including drought, human development, grazing, and fire suppression.[7][8] The Western Aspen Alliance, in collaboration with the United States Forest Service, is studying the tree in an effort to save it.[9][10] In areas of Pando lacking adequate protective fencing, grazing animals have prevented Pando from developing enough young stems to fully replace existing older stems as they die.[8] This decline in recruitment of young stems began in the 1980s and has been attributed primarily to mule deer (Odocoileus hemionus), though Pando also undergoes restricted grazing by domestic cattle (Bos taurus) and is potentially browsed by elk (Cervus canadensis).[8][11]

History

The Pando tree was identified in 1976 by Jerry Kemperman and Burton Barnes.[12][13] Michael Grant, Jeffrey Mitton, and Yan Linhart of the University of Colorado at Boulder re-examined the clone in 1992, naming it Pando and claiming it to be the world's largest organism by weight.[1] Both teams of researchers described Pando as a single asexual reproduction organism based on its morphological characteristics. Genetic sampling and analysis in 2008 by Jennifer DeWoody, Carol Rowe, Valerie Hipkins, and Karen Mock of Utah State University and the University of Southampton confirmed the earlier analyses and increased the clone's estimated size from 43.3 to 43.6 hectares.[2] Paul Rogers and Darren McAvoy, also with Utah State University, completed the first comprehensive assessment of Pando's status in 2018 and stressed the importance of reducing herbivory by mule deer to conserving Pando for the future.[8] In 2019, Rogers and Jan Šebesta surveyed other vegetation within Pando besides aspen, finding additional support for their 2018 conclusion that interactions between browsing and past and ongoing management have had adverse effects on Pando's long-term resilience to change.[14]

detailed image of the Pando Tree shows the characteristic eyes and shades of autumn
Closeup of a trunk and leaves

While Pando is the largest known aspen clone and its age has received considerable attention, other large and old clones exist. According to an Organisation for Economic Co-operation and Development (OECD) report in 2000:

Clonal groups of P. tremuloides in eastern North America are very common, but generally less than 0.1 ha in size, while in areas of Utah, groups as large as 80 ha have been observed (Kemperman and Barnes 1976). In the semi-arid western United States, some argue that widespread seedling establishment has not occurred since the last glaciation, some 10,000 years ago (Einspahr and Winton 1976, McDonough 1985). Indeed, some biologists feel that western clones could be as old as 1 million years (Barnes 1966, 1975).[4]

In 2006 the United States Postal Service published a stamp in commemoration of the aspen, calling it one of the forty "Wonders of America".[15][16]

Size and age

The clonal colony encompasses 43.6 hectares (108 acres), weighs nearly 6,000 metric tons (6,600 short tons), and has over 40,000 stems (trunks), which die individually and are replaced by new stems growing from its roots.[2][3] The root system is estimated to be several thousand years old with habitat modeling suggesting a maximum age of 14,000 years.[17][18] Individual aspen stems typically do not live beyond 100–130 years and mature areas within Pando are approaching this limit.[8]

Mitton and Grant summarize the development of stems in aspen clones:[5]

... quaking aspen regularly reproduces via a process called suckering. An individual stem can send out lateral roots that, under the right conditions, send up other erect stems; from all above-ground appearances the new stems look just like individual trees. The process is repeated until a whole stand, of what appear to be individual trees, forms. This collection of multiple stems, called ramets, all form one, single, genetic individual, usually termed a clone.

Range of age estimates

Due to the progressive replacement of stems and roots, the overall age of an aspen clone cannot be determined from tree rings. In Pando's case, ages up to 1 million years have therefore been suggested.[5] An age of 80,000 years is often given for Pando, but this claim derives from a National Park Service web page that does not provide a source for its number and is inconsistent with the Forest Service's post ice-age estimate.[10][19] Glaciers repeatedly formed on the Fish Lake Plateau over the past several hundred thousand years and the Fish Lake valley occupied by Pando was partially filled by ice as recently as the last glacial maximum.[20] Ages greater than approximately 16,000 years therefore require Pando to have survived at least the Pinedale glaciation, something that appears unlikely under current genetic estimates of Pando's age and modeling of variation in Pando's local climate.[17][18]

Estimates of Pando's age have also been influenced by changes in the understanding of establishment of aspen clones in western North America. Earlier sources argued germination and successful establishment of aspen on new sites was rare in the last 10,000 years and, therefore, Pando's root system was likely over 10,000 years old.[5] More recent observations, however, have shown seedling establishment of new aspen clones is a regular occurrence and can be abundant on sites exposed by wildfire.[21] These findings are summarized in the U.S. Forest Service's Fire Effects Information System:[22]

Kay documented post-fire quaking aspen seedling establishment following 1986 and 1988 fires in Grand Teton and Yellowstone National Parks, respectively. He found seedlings were concentrated in kettles and other topographic depressions, seeps, springs, lake margins, and burnt-out riparian zones. A few seedlings were widely scattered throughout the burns. In Grand Teton National Park, establishment was greatest (950–2,700 seedlings/ha) in 1989, a wet year, but hundreds to thousands of seedlings established each year despite drought conditions in 1986–1988 and 1990–1991. Seedlings surviving past one season occurred almost exclusively on severely burned surfaces.

See also

References
  1. Grant, Michael C. (October 1993). "The Trembling Giant". Discover. Vol. 14, no. 10. Chicago. pp. 82–89. Retrieved 2008-05-08.
  2. DeWoody, Jennifer; Rowe, Carol A.; Hipkins, Valerie D.; Mock, Karen E. (2008). ""Pando" Lives: Molecular Genetic Evidence of a Giant Aspen Clone in Central Utah". Western North American Naturalist. 68 (4): 493–497. doi:10.3398/1527-0904-68.4.493. S2CID 59135424.
  3. "Pando". USDA Forest Service. Retrieved 2013-08-24.
  4. OECD (2000). Consensus Document on the Biology of Populus L. (Poplars) (PDF). Series on Harmonization of Regulatory Oversight in Biotechnology. Vol. 16. Paris: Organisation for Economic Co-operation and Development. Retrieved 2018-11-17.
  5. Mitton, Jeffry B.; Grant, Michael C. (1996). "Genetic Variation and the Natural History of Quaking Aspen". BioScience. 46 (1): 25–31. doi:10.2307/1312652. JSTOR 1312652.
  6. Mihai, Andrei (February 9, 2015). "The Heaviest Living Organism in the World". ZME Science. Retrieved 2015-02-12.
  7. Rogers, Paul C.; Gale, Jody A. (2017). "Restoration of the iconic Pando aspen clone: Emerging evidence of recovery". Ecosphere. 8 (1): e01661. doi:10.1002/ecs2.1661.
  8. Rogers, Paul C.; McAvoy, Darren J. (2018-10-17). "Mule deer impede Pando's recovery: Implications for aspen resilience from a single-genotype forest". PLOS ONE. 13 (10): e0203619. Bibcode:2018PLoSO..1303619R. doi:10.1371/journal.pone.0203619. ISSN 1932-6203. PMC 6192553. PMID 30332420.
  9. "Pando - Western Aspen Alliance". western-aspen-alliance.org. Retrieved 2020-08-16.
  10. United States Forest Service, Fishlake National Forest. "Pando - (I Spread)".
  11. Funes, Yessenia (October 17, 2017). "The Biggest Organism on Earth Is Dying, and It's Our Fault". Earther. Retrieved 2018-10-17.
  12. Kemperman, Jerry A.; Barnes, Burton V. (1976-11-15). "Clone size in American aspens". Canadian Journal of Botany. 54 (22): 2603–2607. doi:10.1139/b76-280. ISSN 0008-4026. S2CID 85891968.
  13. Mock, K. E.; Rowe, C. A.; Hooten, M. B.; Dewoody, J.; Hipkins, V. D. (2008). "Clonal dynamics in western North American aspen (Populus tremuloides)". Molecular Ecology. 17 (22): 4827–4844. doi:10.1111/j.1365-294X.2008.03963.x. PMID 19140975. S2CID 1425039. Archived from the original on 2018-09-19. Retrieved 2018-11-17.
  14. Rogers, Paul C.; Šebesta, Jan (December 2019). "Past Management Spurs Differential Plant Communities within a Giant Single-Clone Aspen Forest". Forests. 10 (12): 1118. doi:10.3390/f10121118.
  15. Sussman, Rachel (2014). "Pando". The Oldest Living Things in the World. University of Chicago Press. p. 59. doi:10.7208/chicago/9780226057644.001.0001. ISBN 978-0-226-05764-4.
  16. "Wonders of America: Land of Superlatives". Archived from the original on 2 December 2008.
  17. Mock, K. E.; Rowe, C. A.; Hooten, M. B.; Dewoody, J.; Hipkins, V. D. (November 2008). "Clonal dynamics in western North American aspen ( Populus tremuloides )". Molecular Ecology. 17 (22): 4827–4844. doi:10.1111/j.1365-294X.2008.03963.x. PMID 19140975. S2CID 1425039.
  18. Ding, Chen; Schreiber, Stefan G.; Roberts, David R.; Hamann, Andreas; Brouard, Jean S. (2017-07-05). "Post-glacial biogeography of trembling aspen inferred from habitat models and genetic variance in quantitative traits". Scientific Reports. 7 (1): 4672. Bibcode:2017NatSR...7.4672D. doi:10.1038/s41598-017-04871-7. ISSN 2045-2322. PMC 5498503. PMID 28680120.
  19. United States National Park Service, Bryce Canyon National Park. "Quaking Aspen".
  20. Marchetti, David W.; Harris, M. Scott; Bailey, Christopher M.; Cerling, Thure E.; Bergman, Sarah (January 2011). "Timing of glaciation and last glacial maximum paleoclimate estimates from the Fish Lake Plateau, Utah". Quaternary Research. 75 (1): 183–195. Bibcode:2011QuRes..75..183M. doi:10.1016/j.yqres.2010.09.009. ISSN 0033-5894. S2CID 128684169.
  21. Kay, Charles E. (1993). "Aspen seedlings in recently burned areas of Grand Teton and Yellowstone National Parks" (PDF). Northwest Science. 67 (2): 94–104.
  22. Howard, Janet L. (1996). "Populus tremuloides". Fire Effects Information System. U.S. Department of Agriculture, Forest Service, Rocky Mountain Research Station, Fire Sciences Laboratory. Retrieved 2018-11-17.

Additional references from OECD quote in history section
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