Pino de México, ocote, pino, pino escobetón, pino negro [Spanish]; Mexican mountain pine, Hartweg's pine.
Syn: P. montezumae Lamb. subsp. hartwegii (Lindl.) Engelm. 1880, P. montezumae var. hartwegii (Lindl.) Shaw 1909, P. rudis Endl. 1847, P. montezumae Lamb. var. rudis (Endl.) Shaw 1909, P. hartwegii Lindl. var rudis (Endl.) Silba 1990, P. lindleyana Gordon 1858, P. montezumae Lamb. var. lindleyana (Gordon) Parl. 1868, P. donnell-smithii Mast. 1891, and a long slate of species described by Roezl in an 1857 catalog and never heard from again; see Farjon and Styles (1997) for the complete listing, and see Pinus montezumae for remarks on Roezl's creative approach to pine systematics.
It is understandable that such a plethora of names have been attributed to this taxon; it does seem odd that a single species of pine dominates the subalpine forests from Nuevo León to El Salvador, an area within which there are no large contiguous subalpine forests and every range is a biogeographical island; but despite many attempts to subdivide the taxon, none have succeeded in identifying the kind of regional morphological distinctions that credibly support the creation of other taxa at the specific or varietal ranks.
Genetic studies (see the Pinus description for details) appear to place this taxon in Subgenus Pinus, Section Trifoliae, Subsection Ponderosae. Pinus torreyana is the only narrowly distributed species in the subsection. The other 13 species in the subsection are widely-distributed habitat generalist pines of western North America; most of them are phenotypically plastic, and several have taxa described at the subspecific rank. Most are taxa of mountainous regions and conseqeuently are comprised of a large number of geographically distinct populations that have opportunities to merge and mingle as a consequence of climate changes (glacial/interglacial, mainly) that primary occur at time scales of tens to hundreds of thousands of years. Consequently we would expect P. hartwegii to be a phenotypically and presumably genetically diverse taxon that sometimes displays consistent morphological differences between populations, which may be assignable to subspecific or varietal ranks.
Historically, the taxon was separately described at several times, owing to its broad geographic distribution. In 1839, Lindley described P. hartwegii from material collected by C.T. Hartweg in the mountains of eastern Michoacán, Mexico. Then in 1847, Endlicher described P. rudis, and in 1891, Masters described P. donnell-smithii from material collected by Donnell-Smith in Guatemala. Unfortunately, only Donnell-Smith's collection survives; Hartweg's specimen has been lost, and we do not even know the origin of the material described by Endlicher. Later authors did not clarify matters. Martínez distinguished the species based on cone color, which is not generally regarded as a taxonomically useful character, and the character states described by Perry (1991) for the different taxa are overlapping or even indistinguishable (Farjon and Styles 1997). Farjon and Styles (1997) cite a study by Matos (1995) that was unable to discriminate P. hartwegii and P. rudis using elevational transects recording 25 character states, and they conclude that the taxa, as described, are undistinguishable. Thus they reduce all names since the original P. hartwegii to synonymy.
At this point I have seen this taxon on Cerro Potosí and Cerro Peña Blanca in Nuevo Leon, on Nevado de Colima in Jalisco, in the Sierra Juárez in Oaxaca, on Nevado de Toluca in México, and on Popocatepetl in Puebla. This represents a pretty good cross-section of its distribution in Mexico. I have not seen it in Guatemala or Honduras, which are the described range of P. donnell-smithii. Based on these observations I agree with Farjon and Styles that the taxon described by Perry (1991) as P. rudis is not distinguishable from P. hartwegii. However, Perry (1991) was clearly seeing what he thought to be consistent differences between trees in different areas. I also received an email from Burkhard Witt (2007.02.04) describing his field observations, using Perry (1991) as a guide, on numerous high mountains in northeast Mexico, and concluding that P. rudis and P. hartwegii, as described by Perry, are differentiable and consistently occur with P. rudis at lower elevations, giving way to P. hartwegii at higher elevations (see the Observations section). Witt also reported that he has observed a consistent difference in that P. rudis consistently has a silver-gray-green foliage color, while P. hartwegii has very dark green foliage. This is interesting information, but doesn't get around the taxonomic problems that the original descriptions of these species are not adequate to differentiate them, and that Perry's keys do not effectively discriminate between the taxa. I am forced to conclude that there probably is a sound basis for distinguishing subspecies or varieties within P. hartwegii. Maybe someday some enterprising taxonomist will go out and systematically study populations representing the range of the taxon, and will describe taxa that represent patterns of variation that are not reflected in the published descriptions of P. rudis or P. donnell-smithii. Until then, if you go in search of these trees, it is well to look out for evidence of infraspecific differences that may be tied to elevation or geography.
A tree up to 128 cm dbh and 31 m tall, almost always arboriform even at the alpine timberline. Bark thick, rough and scaly, divided into small to large plates, deeply furrowed, dark brown to grey. Branchlets stout, stiff, curving upwards, purple-brown turning dark brown or grey, with persistent leaf bases. Needles in fascicles of 3-6, usually 5 but mostly 3 in some areas (e.g. Popocatepetl), (6-)10-17(-22) cm long × (1-)1.2-1.5 mm, straight or curved, stiff. Cones in whorls of 2-6, appearing sessile, deciduous, obliquely ovoid, 8-12(-15) × 5-8 cm when open. Cones scales opening soon, with a slightly raised apophysis, weakly transversely keeled, brown or purple-brown with a black flat umbo. Seeds 5-6 mm long, often with black spots; seed wing articulate, 12-20 × 7-12 mm (Farjon et al. 1997 and personal observations in southern Mexico, Feb-2005).
Found at elevations of (2200-)2500-4000(-4300) m (Perry 1991, Farjon et al. 1997). Also reported from El Salvador, Perry (1991) asserting that "there are still many relatively unexplored high mountains along the Honduras-El Salvador border and P. hartwegii, along with other unreported species, may occur on those mountain peaks." Hardy to Zone 8 (cold hardiness limit between -12.1°C and -6.7°C) (Bannister and Neuner 2001). See also Thompson et al. (1999).
From central Mexico southwards, this is the universal pine at high altitudes, where it normally grows erect to the upper timberline in pure (single-species) stands, though at more moderate elevations it may be found with Pinus montezumae, P. pseudostrobus, P. ayacahuite, Abies religiosa and Cupressus lusitanica. These forests typically have a simple structure, with an open, park-like overstory, and an herb-bunchgrass understory (Velázquez et al., 2000). Data from a site on Nevado de Colima show that the climate is characterized by dry winters and a wet June to October monsoon, with sub-freezing temperatures from July through March (Biondi et al. 2005). At the alpine timberline its growth may be primarily limited, on a year-to-year basis, by the timing of the onset of warm spring temperatures and, later in the season, by moisture stress; additionally, these upper timberline sites are commonly subjected to intense grazing and frequent fires. These factors may help to explain why this species does not attain the dwarfed, contorted alpine growth form known as krummholz -- the species, though growing at the alpine timberline, does not experience the adverse effects of cold and wind-blown ice that normally cause the krummholz form. Pinus hartwegii has recently been the subject of global comparative studies on treeline ecophysiology and biogeography (Hoch and Körner 2003, Körner and Paulsen 2004).
There are not a lot of data. Biondi (2001) sampled trees up to 128 cm dbh on Nevado de Colima, and I (2005.02) got laser-measured heights up to 30.5 m tall on Nevado de Toluca.
The oldest known tree was a specimen collected at 19.58° N, 103.62° W, elevation 3,700 m, on Nevado de Colima; its ring-width record began in 1553 (Biondi 2001).
Franco Biondi and his students have been doing chronology development and physiological studies at Nevado de Colima since 1999 (maybe before). Biondi (2001) collected a 400-year chronology on the peak. This chronology shows the growth suppression due to the 1913 Volcan Fuego eruption, as well as growth suppression due to the catastrophic 1815 eruption of Tambora in Indonesia. Interestingly, the chronology shows a strong correlation with the Palmer Drought Severity Index for the central Great Plains of the United States, suggesting that the intensity of the summer monsoon is a primary control on tree growth at this alpine site. Biondi and others (2003) found that a 1913 eruption of Volcán Fuego, Colima's sister peak, produced reduced growth rings for the following two years in trees around Colima, and more recent work documented the effect of a bark beetle outbreak on growth of these trees (Biondi et al. 2005).
This tree is commonly scarred for resin collection. Such resin collection is typically performed on a non-industrial scale, marking isolated trees, with the resin used for caulk and other purposes not requiring refinement or distillation.
I have seen it in six locations, all but one remarkable and easily accessible:
Burkhard Witt (email 2007.02.04) relates the following information about finding P. hartwegii and trees that fit Perry's 1991) description of P. rudis:
Totonicapán forest is said to harbor the largest and best-conserved stand of P. hartwegii in Guatemala (Elias 1997).
This species is afflicted by the round-headed pine beetle, Dendroctonus adjunctus, a bark beetle that can cause high incidence of mortality in susceptible stands (Hartsough and Biondi 2004, Biondi et al. 2005). In southern Mexico and Guatemala, it is also a host to the dwarf mistletoe Arceuthobium globosum subsp. grandicaule, and A. vaginatum subsp. vaginatum throughout much of Mexico (Hawksworth and Wiens 1996).
Biondi, F. 2001. A 400-year tree-ring chronology from the tropical treeline of North America. Ambio 30:162-166. Available online at equinox.unr.edu/homepage/fbiondi/pubs.html.
Biondi, F., P.C. Hartsough, and I.G. Estrada. 2005. Daily Weather and Tree Growth at the Tropical Treeline of North America. Arctic and Alpine Research 37:16-24. Available online at equinox.unr.edu/homepage/fbiondi/pubs.html.
Biondi, F., I.G. Estrada, J.C.G. Ruiz, and A.E. Torres. 2003. Tree growth response to the 1913 eruption of Volcán de Fuego de Colima, Mexico. Quaternary Research 59:293-299. Available online at equinox.unr.edu/homepage/fbiondi/pubs.html.
Elías, S., 1997. Autogestión comunitaria de recursos naturales, estudio de caso en Totonicapán. Facultad Latinoamericana de Ciencias Sociales. Guatemala [cited in ParksWatch 2004].
Lindley, J. 1839. Edwards's Botanical Register 25:62.
Hartsough, Peter and Franco Biondi. 2004. High Elevation Monitoring in the North American tropics: Ecosystem/climate relationships on Nevado de Colima, Mexico. Poster presented at the 2004 meeting of the American Geophysical Union, available online at http://woods.geography.unr.edu/Posters/AGU2004%20poster.pdf.
Hoch, G. and C. Körner. 2003. The carbon charging of pines at the climatic treeline: a global comparison. Oecologia 135:10-21.
Körner, C. and J. Paulsen. 2004. A world-wide study of high altitude treeline temperatures. Journal of Biogeography 31:713-732.
Matos, J.A. 1995. Pinus hartwegii and P. rudis: A critical assessment. Systematic Botany 20: 6-21.
Velázquez, A., V. M. Toledo, and I. Luna. 2000. Mexican temperate vegetation. Peges 573-592 in M.G. Barbour and W.D. Billings (eds.), North American Terrestrial Vegetation. New York: Cambridge University Press.
Hartsough, Peter and Franco Biondi. 2003. The Importance of High Elevation Monitoring in a Tropical Tree line Environment: A Project Update from South Western Mexico. P. 18 in Programme with Abstracts, Fourth Annual Science Meeting, IAI CRN 03: The Assessment of Past, Present and Future Climate Variability from Treeline Environments. IANIGLA-CRICYT, Mendoza, Argentina, October 10-16, 2003.
Last Modified 2014-12-12