Scots pine; pin royo [Aragonese]; meşə şamı [Azerbaijani]; Хвоя звычайная [Belarussian]; Бял бор [Bulgarian]; pi roig [Catalan]; 歐洲赤松 [Chinese]; Хыр [Chuvash]; obični bor [Croatian]; borovice lesní [Czech]; skovfyr [Danish]; grove den [Dutch]; harilik mänd [Estonian]; mänty [Finnish]; pin sauvage [French]; piñeiro rubio [Galician]; waldkiefer [German]; erdeifenyő [Hungarian]; pino silvestre [Italian]; parastā priede [Latvian]; paprastoji pušis, pošės [Lithuanian]; furu [Norwegian]; sosna zwyczajna [Polish]; pinheiro-da-escócia [Portuguese]; pin de pădure [Romanian]; Сосна обыкновенная [Russian]; beahci [Sami]; beli bor [Serbian]; borovica sosnová [Slovakian]; rdeči bor [Slovene]; pino silvestre [Spanish]; tall [Swedish]; sarıçam [Turkish]; Сосна звичайна [Ukrainian]. The term 'Scotch' pine is incorrect and should not be used, as these trees are not a source of that celebrated intoxicant.
Despite its huge range, it is remarkably uniform in its morphology with individual variation within populations much greater than between-population variation. Over 140 subspecies, varieties and forms have been described in on orgy of botanical nationalism, but only the type, var. sylvestris, var. hamata C. Steven (= subsp. hamata (Steven) Fomin), and var. mongolica Litvinov (= subsp. kulundensis Sukaczev) are now normally accepted (Farjon 1998); even these are barely distinguishable from each other.
Far northern trees, north of about 65°N, were formerly treated as var. lapponica Hartm. but are now thought to represent polyphyletic colonization and adaptations to harsh environments across a very broad front; the variation is continuous and clinal, with no population definable (Langlet 1959), and the variety is no longer accepted (Langlet 1959, Farjon 1998).
Trees from the extreme west of the range, in NW Scotland (Loch Maree area, Wester Ross), and presumably also the now-extinct Irish populations, show resin chemistry and adaptations to oceanic climates not found in the rest of the species' range. These trees are thought to have survived the ice ages on nunataks off NW Ireland and/or W Scotland, or are possibly derived from Spanish populations (Forrest 1980, 1982; Kinloch et al. 1986); as yet there has been no research as to whether this small endangered population deserves taxonomic recognition. Trees from the rest of Scotland (sometimes treated as var. scotica Schott) by contrast showed very close similarity to typical S Swedish / N German origins (Forrest 1980, 1982; Kinloch et al. 1986) and probably colonized across the (then dry) North Sea basin.
Spanish populations, sometimes treated as var. nevadensis H. Christ or var. iberica Svoboda, are genetically distinct (Prus-Glowacki & Stephan 1994) and deserve further taxonomic investigation with possible future varietal or subspecific recognition.
A tree to 25–40 m tall and 0.5–1.2 m dbh. Stem straight (contorted only if lead shoot damaged when young, often by pine shoot moth Evetria turionana). The crown is variable, with a variety of shapes common in wild populations from level branches to near-fastigiate (Pravdin 1964, Steven & Carlisle 1959); open ovoid-conic when young and usually eventually becoming dense, broadly domed or even flat-topped. Bark on lower stem thick, scaly-plated, grey-brown; on upper stem and branches, thin, flaking, orange-red. Branching uninodal. Shoots green at first, becoming grey-buff by the end of the first summer. Buds ovoid-conic, orange-brown, thinly to occasionally thickly covered in white resin. Leaves in fascicles of two, (2.5–)4–6(–9) cm long, 1.5–2 mm wide, always moderately to often strongly glaucous (the only two-leaved hard pine with blue-green or grey-green leaves—an easy pine to identify), longest on vigorous young trees (5–9 cm), short on old trees (2.5–5 cm), commonly slightly twisted, margins finely serrulate; persistent for 2–6(–9) years; leaf sheath grey, 5–8 mm, slowly eroding to 3–4 mm by leaf senescence. Male cones 8–12 mm, yellow or pink. Cones (2.5–)3–6(–7.5) cm long, conic, symmetrical or nearly so, green ripening matt grey-buff to grey-green; mature in November–December, 20 months after pollination, opening February–April and falling soon after seed shed; scales rhombic, flat to protuberant and (rarely) hooked (with a full range of variation inbetween), with a minutely mucronate dorsal umbo. Seeds black, 4–5 mm, with a 12–20 mm wing (Pravdin 1964, Steven and Carlisle 1959; M.P. Frankis pers. obs.).
Var. hamata differs mainly in resin chemistry (Mirov 1967). It also tends to have more pronounced hooked apophyses than the type usually does, but there is much overlap. The leaves stay a stronger blue-green in winter than the type (which often turns drab green in winter).
Var. mongolica differs in having buds more thickly coated in resin, but not all trees show this, and thickly resinous buds can also occur on the type. The foliage tends to be duller, less bluish and more grey-green, to even yellow-grey in winter.
Var. lapponica is sometimes distinguished on the basis of shorter and longer-persistent leaves (5-9 years), but its characters overlap and intergrade to such a large extent that it cannot be adequately defined.
This is the world's most widespread conifer, after Juniperus communis, and its native range includes Albania, Andorra, Armenia, Austria, Azerbaijan, Belarus, Bosnia & Herzegovina, Bulgaria, China, Croatia, Czech Republic, Estonia, Finland, France, Georgia, Germany, Greece, Hungary, Italy, Kazakhstan, Latvia, Lithuania, Macedonia, Mongolia, Montenegro, Norway, Poland, Portugal, Romania, Russia, Serbia, Slovakia, Slovenia, Spain, Sweden, Switzerland, Turkey, Ukraine, and the United Kingdom. Naturalized and exterminated but reintroduced extent is discussed below.
Var. sylvestris occurs in Europe, from Scotland and Spain eastward, and across N Asia nearly to the Pacific coast. In N Eurasia, from sea level to 1,000 m; in S Europe only above 500 m in mountains, to as high as 2,400 m in Spanish Sierra Nevada. Absent from E coastal parts of Siberia, rare and local in NE Siberia (Dinets 1998). Native to Croatia. USDA hardiness zone 1-4, depending on origin; Spanish and NW Scottish origins probably zone 6-7. Extinct through human agency (felling, burning, overgrazing) in Ireland, Wales, England, Netherlands and Denmark; re-introduced populations (largely of unknown derivation) thriving locally in all these countries. Naturalized in Canada: Alberta, British Columbia, Manitoba, New Brunswick, Newfoundland, Nova Scotia, Ontario, Prince Edward Island, and Québec; and the USA: Connecticut, Delaware, Iowa, Illinois, Indiana, Maine, Maryland, Massachusetts, Michigan, Minnesota, New Hampshire, New Jersey, New York, Ohio, Pennsylvania, Rhode Island, Vermont, and Wisconsin (PLANTS database 2009.03.31).
Var. hamata is native to the Balkan peninsula, N Turkey and SW Transcaucasia (Dinets 1998), at altitudes of 500–2,600 m (Mirov 1967). USDA hardiness zone 6.
Var. lapponica is often cited as native to Norway, Sweden, Finland, and adjacent parts of Russia north of 65°N (Dinets 1998, Silba 1986). It grows to about 30 m tall on the Solovki Islands in the White Sea (Vladimir Dinets e-mail 1998.01.10).
Var. mongolica is native to Mongolia, NW China, & S. Siberia, at 300-2000 m altitude. It "[o]ccupies great areas in Transbaikalia, in most other areas prefers dry slopes or sandy soils, pure or with Larix spp. ('white taiga')" A specimen 42 m tall is known in the Sohondo Nat. Res., Transbaikalia (Vladimir Dinets e-mail 1998.01.10). USDA hardiness zone 2.
"The thickest Swedish pine has a girth of 4.49 m and is growing at Strängsered in Ulricehamn" (Anonymous [no date]). The tallest specimens, up to 45–50 m high, occur along the S coast of the Baltic Sea (Vladimir Dinets e-mail 1998.01.10). The stoutest in the UK is 169 cm dbh, at Belladrum, Scottish Highlands (A.F. Mitchell).
Currently the oldest known tree is growing in Lapland (Finland), less than a kilometer from the Russian border. Researcher Tuomo Wallenius sampled and crossdated the tree, finding an oldest ring date of 1244, i.e., 764 years old when sampled in 2007 (Finnish Forest Research Institute 2007).
Another tree, nearly as old, occurs in Muddus National Park, Sweden. "It is at least 711 years old. Researchers have found that the pine has survived forest fires in the years of 1413, 1507, 1596 and 1771 ... The oldest tree harvested in Sweden was 654 years old when it was felled in 1913 at Svärdsjö, Dalarna" (Anonymous [no date]). These data suggest a fire history study, thus a relatively reliable minimum age, for the 711 year tree; the 654 year tree is likely a ring count.
A 1999 search produced 366 papers involving Pinus sylvestris. There are over a hundred citations involving problems in archeology and a like number involving climate studies. The species has been used to develop a continuous tree-ring chronology extending from 5634 BC to the present (Helama et al. 2008). It has also been used in studies of stand dynamics, air pollution (including Chernobyl radiation), ecophysiology, and a host of more arcane studies. Few, if any species have been more extensively used in dendrochronology.
Commonly sold as a Christmas tree, mainly in N America but also now in Britain, though not the traditional species for this use; when so used, var. hamata is the best as it has better blue colour in winter. An important timber species throughout much of its range.
Also see Mythology and Folklore of the Scots Pine (off-site link).
In Scotland, see the page on How to find the main pine forest remnants, which provides directions on how to reach the nine best examples of remnant Scots pine forest.
Trees naturalised or planted in N America commonly show a contorted stem form (Kral 1993), possibly due to introduced insect pests lacking their normal control predators and parasites. In its native areas, stem straightness is usually very good.
Var. nevadensis (native to Spain) is listed as vulnerable on the 1996 IUCN Red List.
Anonymous. [no date]. Forest Sweden: The Swedish Forests. http://www-forest.slu.se/skogen/eng/omtrad.cfm, accessed 1999.06.05, now defunct.
Finnish Forest Research Institute (Metla). 2007.08.06. Lapista löytyi ennätysvanha mänty. http://www.metla.fi/tiedotteet/2007/2007-08-06-vanhin-puu.htm, accessed 2011.02.23 [in Finnish].
Forrest, G. I. 1980. Genotypic variation among native Scots Pine populations in Scotland based on monoterpene analysis. Forestry 53: 101-128.
Forrest, G. I. 1982. Relationship of some European Scots Pine populations to native Scottish woodlands based on monoterpene analysis. Forestry 55: 19-37.
Gutiérrez, E. 1989. Dendroclimatological study of Pinus sylvestris L. in southern Catalonia (Spain). Tree-Ring Bulletin 49:1-9.
Helama, S, K. Mielikäinen, M. Timonen, and M. Eronen. 2008. Finnish supralong tree-ring chronology extended to 5634 BC. Norsk Geografisk Tidsskrift / Norwegian Journal of Geography 62:271-277.
Kinloch, B. B., R. D. Westfall & G. I. Forrest 1986. Caledonian Scots Pine: origins and genetic structure. New Phytologist 104: 703-729.
Langlet, O. 1959. A cline or not a cline—a question of Scots Pine. Silvae Genetica 8: 13-22.
Pravdin, L. F. 1964. Sosna obyknovennaya. Izdatel'stvo Nauka, Moskva [Translated Israel progr. scient. transl., Jerusalem, as Scots Pine, 1969].
Prus-Glowacki, W. & B. R. Stephan 1994. Genetic variation of Pinus sylvestris from Spain in relation to other European populations. Silvae Genetica 43: 7-14.
Steven, H. M. & A. Carlisle 1959. The native pinewoods of Scotland.
An early version of this page was prepared 1999.01.02 by Michael P. Frankis.
The FEIS database.
Things you never knew about Scots pine, accessed 2009.03.28. Very informative page with many good photographs.
Last Modified 2014-03-29