View source for Taiga

{{Short description|Biome characterized by coniferous forests}}
{{pp-semi|small=yes}}
{{distinguish|Tayga}}
{{Other uses}}
{{Pp-move|small=yes}}
{{Use dmy dates|date=May 2025}}

{{Infobox ecoregion
|name=Taiga
|map=Taiga ecoregion.png
|map_size=300
|map_caption=The taiga is found throughout the high northern [[latitude]]s, between the [[tundra]] and the [[temperate forest]], from about 50°N<!--as shown on map!--> to 70°N, but with considerable regional variation.
|biome={{hlist|Terrestrial subarctic|humid}}
|climate=[[Köppen climate classification#Group D: Continental/microthermal climates|{{hlist|Dfc|Dwc|Dsc|Dfd|Dwd|Dsd}}]]
|image=Jack London Lake by bartosh.jpg
|image_caption=[[Jack London Lake]] in [[Kolyma]], [[Russia]]
<!--Area is sum of areas of all WWF tundra ecoregions, from http://www.worldwildlife.org/wildworld/profiles/terrestrial_na.html and similar-->
|countries={{hlist|Russia|Mongolia|Japan|Norway|Sweden|Iceland|Finland|United States|Canada|Saint-Pierre-et-Miquelon (France)}}
|area=
}}

'''Taiga''' or '''tayga''' ({{IPAc-en|ˈ|t|aɪ|.|ɡ|ə}}, {{respell|TY|gə}}; {{langx|ru|тайга́}}, {{IPA|ru|tɐjˈɡa|IPA}}), also known as '''boreal forest''' or '''snow forest''', is a [[biome]] characterized by [[Pinophyta|coniferous]] [[forest]]s consisting mostly of [[pine]]s, [[spruce]]s, and [[larch]]es.  

The taiga, or boreal forest, is the world's largest land [[biome]].<ref name="Berkeley">{{cite web |url=http://www.ucmp.berkeley.edu/exhibits/biomes/forests.php#boreal |title=Berkeley: The forest biome |publisher=Ucmp.berkeley.edu |access-date=12 May 2019 |archive-url=https://web.archive.org/web/20190620145416/https://ucmp.berkeley.edu/exhibits/biomes/forests.php#boreal |archive-date=20 June 2019 }}</ref> In North America, it covers most of inland [[Canada]], [[Alaska]], and parts of the northern contiguous United States.<ref>{{cite web |url=http://www.trails.com/list_11901_list-plants-animals-canadian-wilderness.html |title=List of Plants & Animals in the Canadian Wilderness |publisher=Trails.com |date=27 July 2010 |access-date=26 December 2016 |archive-date=14 September 2018 |archive-url=https://web.archive.org/web/20180914022617/https://www.trails.com/list_11901_list-plants-animals-canadian-wilderness.html }}</ref> In [[Eurasia]], it covers most of [[Sweden]], [[Finland]], much of [[Russia]] from [[Karelia]] in the west to the [[Pacific Ocean]] (including much of [[Siberia]]), much of [[Norway]], some lowland/coastal areas of [[Iceland]], and areas of northern [[Kazakhstan]], northern [[Mongolia]], and northern [[Japan]] (on the island of [[Hokkaido]]).<ref name=":0">{{Cite web |title=Taiga {{!}} Plants, Animals, Climate, Location, & Facts {{!}} Britannica |url=https://www.britannica.com/science/taiga |access-date=4 May 2023 |website=www.britannica.com |language=en}}</ref>
[[File:Adirondacks in May 2008.jpg|thumb|The [[Adirondack Mountains]] of [[Upstate New York]] form the southernmost part of the [[Eastern forest-boreal transition]] [[ecoregion]], constituting part of the world's taiga [[biome]].]]
The principal tree species, depending on the length of the growing season and summer temperatures, vary across the world. The taiga of North America is mostly [[spruce]]; [[Scandinavia]]n and [[Finland|Finnish]] taiga consists of a mix of [[Norway spruce|spruce]], [[pine]]s, and [[Betula|birch]]; Russian taiga has spruces, pines, and [[larch]]es depending on the region; and the [[Eastern Siberian taiga]] is a vast larch forest.<ref name=":0" />

Taiga in its current form is a relatively recent phenomenon, having only existed for the last 12,000 years since the beginning of the [[Holocene]] epoch, covering land that had been [[mammoth steppe]] or under the [[Weichselian glaciation|Scandinavian Ice Sheet]] in Eurasia and under the [[Laurentide Ice Sheet]] in North America during the [[Late Pleistocene]].

Although at high elevations taiga grades into [[alpine tundra]] through [[Krummholz]], it is not exclusively an alpine biome, and unlike [[Montane ecology#Subalpine zone|subalpine forest]], much of taiga is lowlands.

[[Climate change]] is a threat to taiga,<ref>{{Cite web |last=Graham |first=Karen |date=19 May 2021 |title='Zombie fires' may become more common as the climate warms |url=https://www.digitaljournal.com/tech-science/zombie-fires-may-become-more-common-as-the-climate-warms/article |access-date=4 June 2021 |website=Digital Journal |language=en-US}}</ref> and how the [[Carbon sink|carbon dioxide absorbed]] or [[Carbon emission|emitted]]<ref name="ucsusa">{{Cite web |title=Carbon Emissions from Boreal Forest Wildfires  |url=https://www.ucsusa.org/resources/carbon-emissions-boreal-forest-wildfires |access-date=31 May 2022 |website=Union of Concerned Scientists |date=27 April 2022 |first1=Carly |last1=Phillips |language=en}}</ref> should be treated by [[carbon accounting]] is controversial.<ref>{{Cite web|date=18 May 2021|title=How should the world's nations account for the carbon absorbed by their forests? We better figure it out|url=https://bellona.org/news/carbon-dioxide-removal/2021-05-how-should-the-worlds-nations-account-for-the-carbon-absorbed-by-their-forests-we-better-figure-it-out|access-date=4 June 2021|website=Bellona.org|language=en-US}}</ref>

== Name and terminology ==
The word taiga comes from the Russian ''tayga'' ({{lang|ru|тайга}}), a term historically used in Russia and other parts of northern Eurasia to describe extensive forested regions. The Russian term is believed to derive from Turkic or Mongolic roots, where related words refer to wooded or uninhabited forest lands. In English, ''taiga'' is often used interchangeably with ''boreal forest'', but the two terms are sometimes distinguished in regional usage.

In North American literature, ''boreal forest'' is commonly applied to the broad circumpolar coniferous forest zone, while ''taiga'' is sometimes used to refer more specifically to its colder, northern margins approaching the tundra. By contrast, in Russian and Eurasian contexts ''taiga'' typically denotes the entire boreal forest biome without a north–south distinction. The choice of term in scientific and geographic writing varies by region and discipline.<ref name="Hoffman1958">{{cite journal |title=The Meaning of the Word "Taiga" |doi=10.2307/1931768|jstor=1931768|last1=Hoffmann|first1=Robert S.|journal=Ecology|year=1958|volume=39|issue=3|pages=540–541|bibcode=1958Ecol...39..540H }}</ref>[[File:Picea glauca taiga.jpg|thumb|right|[[White spruce]] taiga in the [[Alaska Range]], [[Alaska]], United States]]

==Climate and geography==
[[File:Siberian autumn in taiga..JPG|thumb|[[Siberia]]n taiga]]

Taiga covers {{convert|abbr=off|17|e6km2|e6sqmi}} or 11.5% of the Earth's land area,<ref>{{cite web|url=http://www.wilds.mb.ca/taiga/tbsfaq.html |title=Taiga biological station: FAQ |publisher=Wilds.m.ca |access-date=21 February 2011}}</ref> second only to [[deserts and xeric shrublands]].<ref name="Berkeley"/> The largest areas are located in Russia and Canada. In [[Sweden]] taiga is associated with the [[Norrland terrain]].<ref>{{cite book |last=Sporrong |first=Ulf |chapter=The Scandinavian landscape and its resources |editor-last=Helle |editor-first=Knut|date=2003 |title=The Cambridge History of Scandinavia |url=https://archive.org/details/cambridgehistory01hell |url-access=limited |publisher=Cambridge University Press |issue=1 |pages=[https://archive.org/details/cambridgehistory01hell/page/n655 22] |isbn=978-0-521-47299-9 }}</ref>

===Temperature===
After the permanent ice caps and [[tundra]], taiga is the terrestrial [[biome]] with the lowest annual average temperatures, with mean annual temperature generally varying from {{cvt|−5|to|5|C|F}}.<ref>{{cite web|url=http://www.marietta.edu/~biol/biomes/boreal.htm |title=Marietta the Taiga and Boreal forest |publisher=Marietta.edu |access-date=21 February 2011}}</ref> Extreme winter minimums in the northern taiga are typically lower than those of the tundra. There are taiga areas of eastern Siberia and interior Alaska-[[Yukon]] where the mean annual temperature reaches down to {{cvt|−10|C|F}},<ref>{{cite web|url=http://www.worldclimate.com/cgi-bin/data.pl?ref=N62E129+1102+24959W |title=Yakutsk climate |publisher=Worldclimate.com |date=4 February 2007 |access-date=21 February 2011}}</ref><ref>{{WWF ecoregion|id=na0607 |name= Interior Alaska-Yukon lowland taiga |access-date=21 February 2011}}</ref> and the [[Oymyakon|lowest reliably recorded temperatures]] in the [[Northern Hemisphere]] were recorded in the taiga of northeastern Russia.

Taiga has a [[subarctic climate]] with very large temperature range between seasons. {{cvt|−20|C|F}} would be a typical winter day temperature and {{cvt|18|C|F}} an average summer day, but the long, cold winter is the dominant feature. This climate is classified as ''Dfc'', ''Dwc'', ''Dsc'', ''Dfd'' and ''Dwd'' in the [[Köppen climate classification]] scheme,<ref>{{cite web |url=http://www.radford.edu/~swoodwar/CLASSES/GEOG235/biomes/taiga/taiga.html |title=radford:Taiga climate |publisher=Radford.edu |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110609021800/http://www.radford.edu/~swoodwar/CLASSES/GEOG235/biomes/taiga/taiga.html |archive-date=9 June 2011 }}</ref> meaning that the short summers (24&nbsp;h average {{cvt|10|C|F}} or more), although generally warm and humid, only last 1–3 months, while winters, with average temperatures below freezing, last 5–7 months.

In Siberian taiga the average temperature of the coldest month is between {{convert|-6|°C}} and {{convert|-50|°C}}.<ref name="VOL page 568">''Encyclopedia Universalis'' édition 1976 Vol. 2 ASIE – Géographie physique, p. 568 {{in lang|fr}}</ref> There are also some much smaller areas grading towards the oceanic ''Cfc'' climate with milder winters, whilst the extreme south and (in Eurasia) west of the taiga reaches into [[humid continental climate]]s (''Dfb'', ''Dwb'') with longer summers.

According to some sources, the boreal forest grades into a temperate mixed forest when mean annual temperature reaches about {{cvt|3|C|F}}.<ref>{{WWF ecoregion|id=na0406 |name=The eastern forest – boreal transition|access-date=21 February 2011}}</ref> [[Discontinuous permafrost]] is found in areas with mean annual temperature below freezing, whilst in the ''Dfd'' and ''Dwd'' climate zones [[continuous permafrost]] occurs and restricts growth to very shallow-rooted trees like [[Siberian larch]].

===Growing season===
[[File:Shovel Point1.jpg|thumb|Boreal forest near Shovel Point in [[Tettegouche State Park]], along the northern shore of Lake Superior in [[Minnesota]].]]

The [[growing season]], when the vegetation in the taiga comes alive, is usually slightly longer than the climatic definition of summer as the plants of the boreal biome have a lower temperature threshold to trigger growth than other plants. Some sources claim 130 days growing season as typical for the taiga.<ref name="Berkeley"/>

In Canada and Scandinavia, the growing season is often estimated by using the period of the year when the 24-hour average temperature is {{convert|+5|C}} or more.<ref>{{Cite web|url=http://www.enr.gov.nt.ca/_live/documents/documentManagerUpload/Taiga_Shield_References.pdf|title=Canada: Taiga Shield reference|website=Enr.gov.nt.ca|access-date=28 February 2022}}{{Dead link|date=March 2022 |bot=InternetArchiveBot |fix-attempted=yes }}</ref> For the Taiga Plains in Canada, growing season varies from 80 to 150 days, and in the Taiga Shield from 100 to 140 days.<ref>{{cite web |url=http://geography.ridley.on.ca/CGC1D/Students/NORTH/Geography%20Project/Ecozones.htm |title=Climate of Canadian ecozones |publisher=Geography.ridley.on.ca |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110505201153/https://geography.ridley.on.ca/CGC1D/Students/NORTH/Geography%20Project/Ecozones.htm |archive-date=5 May 2011 }}</ref>

Other sources define growing season by frost-free days.<ref>{{cite web |url=http://www.blueplanetbiomes.org/taiga.htm |title=Taiga |publisher=Blueplanetbiomes |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110410093754/http://www.blueplanetbiomes.org/taiga.htm |archive-date=10 April 2011 }}</ref> Data for locations in southwest Yukon gives 80–120 frost-free days.<ref>{{cite web |url=http://yukon.taiga.net/swyukon/frost.cfm |title=Southwest Yukon:Frost-free days |publisher=Yukon.taiga.net |access-date=21 February 2011 |url-status=usurped |archive-url=https://web.archive.org/web/20110724091601/https://yukon.taiga.net/swyukon/frost.cfm |archive-date=24 July 2011 }}</ref> The closed canopy boreal forest in [[Kenozersky National Park]] near [[Plesetsk]], [[Arkhangelsk Oblast|Arkhangelsk Province]], Russia, on average has 108 frost-free days.<ref>{{cite web|url=http://www.wild-russia.org/bioregion2/2-KenozerskyNP/2_kenoz.htm |title=Kenozersky National Park |publisher=Wild-russia.org |access-date=21 February 2011}}</ref>

[[File:Autumn tundra mosaic Kola Peninsula Murmansk Russia.jpg|thumb|Transitional ecotone between taiga and tundra visible on the shore of [[Lake Lovozero]], [[Kola Peninsula]], [[Russia]]]]

The longest growing season is found in the smaller areas with oceanic influences; in coastal areas of Scandinavia and Finland, the growing season of the closed boreal forest can be 145–180 days.<ref>{{cite web|url=http://www.sekj.org/PDF/anzf31/anz31-123-129.pdf |title=University of Helsinki: Carabid diversity in Finnish taiga |access-date=21 February 2011}}</ref> The shortest growing season is found at the northern taiga–tundra [[ecotone]], where the northern taiga forest no longer can grow and the tundra dominates the landscape when the growing season is down to 50–70 days,<ref>{{cite web|url=http://www.blueplanetbiomes.org/tundra.htm |title=Tundra |publisher=Blueplanetbiomes |access-date=21 February 2011}}</ref><ref>{{cite web|url=http://www.nhptv.org/NatureWorks/nwep8a.htm |title=NatureWorks:Tundra |publisher=Nhptv.org |access-date=21 February 2011}}</ref> and the 24-hr average of the warmest month of the year usually is {{cvt|10|C|F}} or less.<ref>{{cite web |url=http://www.saskschools.ca/~gregory/arctic/Aintro.html |title=The Arctic |publisher=saskschools.ca |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110410080512/https://www.saskschools.ca/~gregory/arctic/Aintro.html |archive-date=10 April 2011 }}</ref>

High [[latitude]]s mean that the [[sun]] does not rise far above the horizon, and less [[solar energy]] is received than further south. But the high latitude also ensures very long summer days, as the sun stays above the horizon nearly 20 hours each day, or up to 24 hours, with only around 6 hours of daylight, or none, occurring in the dark winters, depending on latitude. The areas of the taiga inside the [[Arctic Circle]] have [[midnight sun]] in mid-summer and [[polar night]] in mid-winter.

===Precipitation===
The taiga experiences relatively low [[Precipitation (meteorology)|precipitation]] throughout the year (generally {{cvt|200|–|750|mm|in}} annually, {{cvt|1,000|mm|in}} in some areas), primarily as [[rain]] during the summer months, but also as [[snow]] or [[fog]]. Snow may remain on the ground for as long as nine months in the northernmost extensions of the taiga biome.<ref>A.P. Sayre, ''Taiga'', (New York: Twenty-First Century Books, 1994) 16.</ref>

The fog, especially predominant in low-lying areas during and after the thawing of frozen Arctic seas, stops sunshine from getting through to plants even during the long summer days. As [[evaporation]] is consequently low for most of the year, annual precipitation exceeds evaporation, and is sufficient to sustain the dense vegetation growth including large trees. This explains the striking difference in biomass per square metre between the Taiga and the [[Steppe]] biomes, (in warmer climates), where [[evapotranspiration]] exceeds precipitation, restricting vegetation to mostly grasses.

[[File:Skjomtinden & Kongsbakktinden from Bogen, 2010 September.JPG|thumb|Late September in the [[fjord]]s near [[Narvik]], Norway. This oceanic part of the forest can see more than {{cvt|1,000|mm|in}} precipitation annually and has warmer winters than the vast inland taiga.]]

In general, taiga grows to the south of the {{cvt|10|C|F}} July [[Isotherm (contour line)|isotherm]], occasionally as far north as the {{cvt|9|C|F}} July isotherm,<ref>Arno & Hammerly 1984, Arno ''et al.'' 1995</ref> with the southern limit more variable. Depending on rainfall, and taiga may be replaced by [[forest steppe]] south of the {{cvt|15|C|F}} July isotherm where rainfall is very low, but more typically extends south to the {{cvt|18|C|F}} July isotherm, and locally where rainfall is higher, such as in eastern [[Siberia]] and adjacent [[Outer Manchuria]], south to the {{cvt|20|C|F}} July isotherm.

In these warmer areas the taiga has higher species diversity, with more warmth-loving species such as [[Korean pine]], [[Jezo spruce]], and [[Manchurian fir]], and merges gradually into [[Temperate broadleaf and mixed forests|mixed temperate forest]] or, more locally (on the [[Pacific Ocean]] coasts of North America and Asia), into coniferous [[temperate rainforest]]s where oak and hornbeam appear and join the conifers, birch and [[Populus tremula]].

===Glaciation===

The area classified as taiga in Europe and North America (except Alaska) was [[Wisconsin glaciation|recently glaciated]]. As the glaciers receded they left [[Kettle (geology)|depressions]] in the topography that have since filled with water, creating [[lake]]s and [[bog]]s (especially [[muskeg]] soil) found throughout the taiga.

[[File:Yukon River near Carmacks, Yukon -a.jpg|thumb|right|[[Yukon River]], Canada. Several of the world's longest rivers go through the taiga, including [[Ob River|Ob]], [[Yenisei River|Yenisei]], [[Lena River|Lena]], and [[Mackenzie River|Mackenzie]].]]

<gallery class=center mode=nolines widths="200px" heights="160px">
File:Talkessel von Werchojansk.JPG|The taiga in the river valley near [[Verkhoyansk]], [[Russia]], at 67°N, experiences the coldest winter temperatures in the northern hemisphere, but the extreme continentality of the climate gives an average daily high of {{cvt|22|C|F}} in July
File:Helvetinjärvi.JPG|Lakes and other water bodies are common in the taiga. The [[Helvetinjärvi National Park]], Finland, is situated in the closed canopy taiga (mid-boreal to south-boreal)<ref>{{cite web|url=http://131.95.113.139/courses/multivariate/Diatom_community.pdf|title=Finland vegetation zone and freshwater biome|website=113.139|access-date=19 April 2018|archive-date=11 September 2011|archive-url=https://web.archive.org/web/20110911201301/http://131.95.113.139/courses/multivariate/Diatom_community.pdf}}</ref> with mean annual temperature of {{cvt|4|C|F}}.<ref>{{cite web|url=http://www.worldclimate.com/cgi-bin/data.pl?ref=N61E023+1102+02944W |title=Tampere/Pirkkala, Finland Weather History and Climate Data |publisher=Worldclimate.com |date=2007-02-04 |access-date=2011-02-21}}</ref>
</gallery>

==Soils==
[[File:Саха (Якутия). Поля тукуланов (песчаные дюны). (10118322213).jpg|thumb|[[Tukulan]] sandy area in the taiga of the [[Central Yakutian Lowland]].]]
Taiga [[soil]] tends to be young and poor in nutrients, lacking the deep, organically enriched [[soil profile|profile]] present in temperate deciduous forests.<ref name="autogenerated1">Sayre, 19.</ref> The colder climate hinders development of soil, and the ease with which plants can use its nutrients.<ref name="autogenerated1" /> The relative lack of deciduous trees, which drop huge volumes of leaves annually, and grazing animals, which contribute significant manure, are also factors. The diversity of soil organisms in the boreal forest is high, comparable to the [[tropical rainforest]].<ref>{{cite web|url=http://www.physorg.com/news/2011-10-reveals-true-diversity-life-soils.html |title=Study reveals for first time true diversity of life in soils across the globe, new species discovered |publisher=Physorg.com |access-date=14 January 2012}}</ref>

Fallen leaves and [[moss]] can remain on the [[forest floor]] for a long time in the cool, moist climate, which limits their organic contribution to the soil. [[Acid]]s from [[evergreen]] [[Pine needle|needles]] further leach the soil, creating [[spodosol]], also known as [[podzol]],<ref>Sayre, 19–20.</ref> and the acidic forest floor often has only [[lichens]] and some mosses growing on it. In clearings in the forest and in areas with more boreal deciduous trees, there are more herbs and berries growing, and soils are consequently deeper.

==Flora==
[[File:BaikalForest (pixinn.net).jpg|thumb|right|upright|Boreal forest near [[Lake Baikal]] in [[Russia]]]]
Since [[North America]] and [[Eurasia]] were originally connected by the [[Bering land bridge]], a number of animal and plant [[species]], more animals than plants, were able to colonize both land masses, and are globally-distributed throughout the taiga biome (see [[Circumboreal Region]]). Others differ regionally, typically with each [[genus]] having several distinct species, each occupying different regions of the taiga. Taigas also have some small-leaved [[deciduous]] trees, like [[birch]], [[alder]], [[willow]], and [[Populus|poplar]]. These grow mostly in areas further south of the most extreme winter weather.

The [[Larix gmelinii|Dahurian larch]] tolerates the coldest winters of the Northern Hemisphere, in eastern Siberia. The very southernmost parts of the taiga may have trees such as [[oak]], [[maple]], [[elm]] and [[tilia|lime]] scattered among the conifers, and there is usually a gradual transition into a temperate, mixed forest, such as the [[eastern forest-boreal transition]] of eastern Canada. In the interior of the continents, with the driest climates, the boreal forests might grade into temperate [[grassland]].

There are two major types of taiga. The southern part is the '''closed canopy forest''', consisting of many closely-spaced trees and mossy groundcover. In clearings in the forest, shrubs and wildflowers are common, such as the [[fireweed]] and [[Lupinus|lupine]]. The other type is the '''lichen woodland''' or '''sparse taiga''', with trees that are farther-spaced and [[lichen]] groundcover; the latter is common in the northernmost taiga.<ref>Sayre, 12–13.</ref> In the northernmost taiga, the forest cover is not only more sparse, but often stunted in growth form; moreover, [[ice pruning|ice-pruned]], asymmetric black spruce (in North America) are often seen, with diminished foliage on the windward side.<ref>C. Michael Hogan, [http://globaltwitcher.auderis.se/artspec_information.asp?thingid=44751 ''Black Spruce: Picea mariana'', GlobalTwitcher.com, ed. Nicklas Stromberg, November, 2008] {{webarchive|url=https://web.archive.org/web/20111005174426/http://globaltwitcher.auderis.se/artspec_information.asp?thingid=44751 |date=5 October 2011 }}</ref>

In Canada, Scandinavia and Finland, the boreal forest is usually divided into three subzones: The '''high boreal''' (northern boreal/taiga zone), the '''middle boreal''' (closed forest), and the '''southern boreal''', a closed-canopy, boreal forest with some scattered temperate, deciduous trees among the conifers.<ref>{{cite encyclopedia |author=George H. La Roi |url=https://www.thecanadianencyclopedia.ca/en/article/boreal-forest |title=Boreal forest |encyclopedia=The Canadian Encyclopedia |access-date=27 November 2013 |archive-date=16 October 2015 |archive-url=https://web.archive.org/web/20151016044738/http://www.thecanadianencyclopedia.com/en/article/boreal-forest/ |url-status=live }}</ref> Commonly seen are species such as maple, elm and oak. This southern boreal forest experiences the longest and warmest growing season of the biome. In some regions, including Scandinavia and western Russia, this subzone is commonly used for agricultural purposes.

The boreal forest is home to many types of [[berries]]. Some species are confined to the southern and middle closed-boreal forest (such as [[fragaria|wild strawberry]] and [[mitchella repens|partridgeberry]]); others grow in most areas of the taiga (such as [[cranberry]] and [[cloudberry]]). Some berries can grow in both the taiga and the lower arctic (southern regions) tundra, such as [[bilberry]], [[cornus canadensis|bunchberry]] and [[lingonberry]].

[[File:SevenlakesAlaska.JPG|thumb|Taiga spruce forest in the [[Kenai National Wildlife Refuge]], Alaska. Trees in this environment tend to grow closer to the trunk and not "bush out" in the normal manner of spruce trees.]]

The forests of the taiga are largely [[Pinophyta|coniferous]], dominated by [[larch]], [[spruce]], [[fir]] and [[pine]]. The woodland mix varies according to geography and climate; for example, the [[Eastern Canadian forests]] ecoregion (of the higher elevations of the [[Laurentian Mountains]] and the northern [[Appalachian Mountains]]) in Canada is dominated by balsam fir ''[[Abies balsamea]]'', while further north, the [[Eastern Canadian Shield taiga]] (of northern [[Quebec]] and [[Labrador]]) is mostly black spruce ''[[Picea mariana]]'' and tamarack larch ''[[Larix laricina]]''.

[[Evergreen]] species in the taiga (spruce, fir, and pine) have a number of adaptations specifically for survival in harsh taiga winters, although larch, which is extremely cold-tolerant,<ref>{{Cite web|url=http://forest.jrc.ec.europa.eu/european-atlas-of-forest-tree-species/atlas-download-page/|title=Forest|website=forest.jrc.ec.europa.eu|access-date=4 February 2018}}</ref> is [[deciduous]]. Taiga trees tend to have shallow roots to take advantage of the thin soils, while many of them seasonally alter their [[biochemistry]] to make them more resistant to freezing, called "hardening".<ref name="autogenerated2">Sayre, 23.</ref> The narrow conical shape of northern conifers, and their downward-drooping limbs, also help them shed snow.<ref name="autogenerated2" />

Because the sun is low in the horizon for most of the year, it is difficult for plants to generate energy from [[photosynthesis]]. Pine, spruce and fir do not lose their leaves seasonally and are able to photosynthesize with their older leaves in late winter and spring when light is good but temperatures are still too low for new growth to commence. The adaptation of evergreen needles limits the water lost due to [[transpiration]] and their dark green color increases their absorption of sunlight. Although precipitation is not a limiting factor, the ground freezes during the winter months and plant roots are unable to absorb water, so desiccation can be a severe problem in late winter for evergreens.
[[File:Вид на гору Нуорунен с горы Кивакка 2.jpg|thumb|View of [[Nuorunen]], the highest point of [[Karelia]]]]
Although the taiga is dominated by coniferous forests, some [[flowering plant|broadleaf trees]] also occur, including [[birch]], [[aspen]], [[willow]], and [[rowan]]. Many smaller [[herbaceous]] plants, such as [[fern]]s and occasionally [[allium tricoccum|ramps]] grow closer to the ground. Periodic stand-replacing [[wildfire]]s (with return times of between 20 and 200 years) clear out the tree canopies, allowing sunlight to invigorate new growth on the forest floor. For some species, wildfires are a necessary part of the life cycle in the taiga; some, e.g. [[jack pine]] have cones which only open to release their seed after a fire, dispersing their seeds onto the newly cleared ground; certain species of fungi (such as [[morchella|morels]]) are also known to do this. [[Grass]]es grow wherever they can find a patch of sun; [[moss]]es and [[lichen]]s thrive on the damp ground and on the sides of tree trunks. In comparison with other biomes, however, the taiga has low botanical diversity.

Coniferous trees are the dominant plants of the taiga biome. Very few species, in four main genera, are found: the evergreen spruce, fir and pine, and the deciduous larch. In North America, one or two species of fir, and one or two species of spruce, are dominant. Across Scandinavia and western Russia, the [[Scots pine]] is a common component of the taiga, while taiga of the [[Russian Far East]] and [[Mongolia]] is dominated by [[larch]]. Rich in spruce and Scots pine (in the western Siberian plain), the taiga is dominated by larch in Eastern Siberia, before returning to its original floristic richness on the Pacific shores. Two deciduous trees mingle throughout southern Siberia: birch and ''[[Populus tremula]]''.<ref name="VOL page 568"/>

<gallery widths="200px" heights="160px">
File:Fire Morels.jpg|Conifer cones and morels after fire in a boreal forest.
File:Ptilium crista-castrensis.jpg|Moss (''[[Ptilium crista-castrensis]]'') cover on the floor of taiga
</gallery>

==Fauna==
[[File:Brown-bear-in-spring.jpg|thumb|A [[Brown bear]], [[Kamchatka peninsula]]. Brown bears are among the largest and most widespread taiga [[omnivore]]s.]]

The boreal forest/taiga supports a relatively small variety of highly specialized and adapted animals, due to the harshness of the climate. Canada's boreal forest includes 85 species of [[mammals]], 130 species of fish, and an estimated 32,000 species of [[insect]]s.<ref>{{cite web |url=http://www.hww.ca/hww2.asp?id=354 |title= Canada's Boreal Forest  |publisher=Hinterland Who's Who |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110103083916/https://www.hww.ca/hww2.asp?id=354 |archive-date=3 January 2011 }}</ref> Insects play a critical role as [[pollinator]]s, [[decompose]]rs, and as a part of the food web. Many nesting birds, rodents, and small carnivorous mammals rely on them for food in the summer months.

The cold winters and short summers make the taiga a challenging biome for [[reptile]]s and [[amphibian]]s, which depend on environmental conditions to regulate their body temperatures. There are only a few species in the boreal forest, including [[common garter snake|red-sided garter snake]], [[vipera berus|common European adder]], [[blue-spotted salamander]], [[northern two-lined salamander]], [[Siberian salamander]], [[wood frog]], [[northern leopard frog]], [[boreal chorus frog]], [[American toad]], and [[Canadian toad]]. Most hibernate underground in winter.

Fish of the taiga must be able to withstand cold water conditions and be able to adapt to life under ice-covered water. Species in the taiga include [[Alaska blackfish]], [[northern pike]], [[walleye]], [[longnose sucker]], [[white sucker]], various species of [[cisco (fish)|cisco]], [[lake whitefish]], [[round whitefish]], [[pygmy whitefish]], [[Arctic lamprey]], various [[Thymallus|grayling]] species, [[brook trout]] (including sea-run brook trout in the Hudson Bay area), [[chum salmon]], [[Hucho taimen|Siberian taimen]], [[lenok]] and [[lake chub]].

[[File:Snowscape (6701322581).jpg|thumb|[[Seney National Wildlife Refuge]].]]

The taiga is mainly home to a number of large [[Herbivore|herbivorous]] [[mammal]]s, such as ''Alces alces'' ([[moose]]), and a few subspecies of ''Rangifer tarandus'' ([[reindeer]] in Eurasia; [[caribou]] in North America). Some areas of the more southern closed boreal forest have populations of other [[Cervidae]] species, such as the [[Caspian red deer|maral]], [[elk]], [[Sitka black-tailed deer]], and [[roe deer]]. While normally a polar species, some southern herds of [[muskoxen]] reside in the taiga of Russia's Far East and North America. The [[Amur]]-Kamchatka region of far eastern Russia also supports the [[snow sheep]], the Russian relative of the American [[bighorn sheep]], [[wild boar]], and [[long-tailed goral]].<ref>{{cite web |url=http://www.hww.ca/hww2.asp?id=98 |title= North American Elk  |publisher=Hinterland Who's Who |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110103152034/https://www.hww.ca/hww2.asp?id=98 |archive-date=3 January 2011 }}</ref><ref>{{cite web |url=http://www.borealforest.org/world/mammals/western_roe_deer.htm |title=Western roe deer  |publisher=Borealforest.org |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110526003203/http://www.borealforest.org/world/mammals/western_roe_deer.htm |archive-date=26 May 2011 }}</ref> The largest animal in the taiga is the [[wood bison]] of northern Canada/Alaska; additionally, some numbers of the American [[plains bison]] have been introduced into the Russian far-east, as part of the taiga regeneration project called ''[[Pleistocene Park]]'', in addition to [[Przewalski's horse]].<ref>{{cite web|url=http://www.pc.gc.ca/pn-np/ab/elkisland/ne/ne5.aspx|title=Government of Canada to Send Wood Bison to Russian Conservation Project |website=Parks Canada |date=23 January 2012 |access-date=11 December 2012|archive-url=https://web.archive.org/web/20130209204726/https://www.pc.gc.ca/pn-np/ab/elkisland/ne/ne5.aspx|archive-date=9 February 2013}}</ref>

Small mammals of the taiga biome include [[rodent]] species such as the [[beaver]], [[squirrel]], [[chipmunk]], [[marmot]], [[lemming]], [[North American porcupine]] and [[vole]], as well as a small number of [[lagomorph]] species, such as the [[pika]], [[snowshoe hare]] and [[mountain hare]]. These species have adapted to survive the harsh winters in their native ranges. Some larger mammals, such as [[bear]]s, eat heartily during the summer in order to gain weight, and then go into [[hibernation]] during the winter. Other animals have adapted layers of fur or feathers to insulate them from the cold.

Predatory mammals of the taiga must be adapted to travel long distances in search of scattered prey, or be able to supplement their diet with vegetation or other forms of food (such as [[raccoon]]s). Mammalian predators of the taiga include [[Canada lynx]], [[Eurasian lynx]], [[stoat]], [[Siberian weasel]], [[least weasel]], [[sable]], [[American marten]], [[North American river otter]], [[European otter]], [[American mink]], [[wolverine]], [[Asian badger]], [[Fisher (animal)|fisher]], [[Subspecies of Canis lupus|timber wolf]], [[Mongolian wolf]], [[coyote]], [[red fox]], [[Arctic fox]], [[grizzly bear]], [[American black bear]], [[Asiatic black bear]], [[Ussuri brown bear]], [[polar bear]] (only small areas of northern taiga), [[Siberian tiger]], and [[Amur leopard]].

More than 300 species of [[bird]]s have their [[nest]]ing grounds in the taiga.<ref>{{cite web|url=http://www.borealbirds.org/forest.shtml |title=Boreal Forest |publisher=Boreal Songbird Initiative |access-date=21 February 2011}}</ref> [[Siberian thrush]], [[white-throated sparrow]], and [[black-throated green warbler]] [[bird migration|migrate]] to this [[Habitat (ecology)|habitat]] to take advantage of the long summer days and abundance of [[insect]]s found around the numerous bogs and lakes. Of the 300 species of birds that summer in the taiga, only 30 stay for the winter.<ref>Sayre, 28.</ref> These are either [[carrion]]-feeding or large [[Bird of prey|raptor]]s that can take live mammal prey, such as the [[golden eagle]], [[rough-legged buzzard]] (also known as the rough-legged hawk), [[Steller's sea eagle]] (in coastal northeastern Russia-Japan), [[great gray owl]], [[snowy owl]], [[barred owl]], [[great horned owl]], [[crow]] and [[raven]]. The only other viable adaptation is seed-eating birds, which include several species of [[grouse]], [[capercaillie]] and [[crossbill]]s.

==Fire==
[[File:Funny River Fire Alaska.jpg|thumb|The [[Funny River Fire]] in Alaska burned {{convert|193,597|acre}}, mostly [[Black spruce]] taiga]]
[[Wildfire|Fire]] has been one of the most important factors shaping the composition and development of boreal forest stands;<ref name="rowe2">{{cite journal |last=Rowe |first=J. S. |year=1955 |title=Factors influencing white spruce reproduction in Manitoba and Saskatchewan |journal=Can. Dep. Northern Affairs and National Resources |series=For. Branch, For. Res. Div., Ottawa ON, Project MS-135, Silv. Tech. Note 3 }}</ref> it is the dominant stand-renewing disturbance through much of the Canadian boreal forest.<ref name="amiro">{{cite journal |last1=Amiro |first1=B. D. |last2=Stocks |first2=B. J. |last3=Alexander |first3=M. E. |last4=Flannigan |first4=M. D. |last5=Wotton |first5=B. M. |year=2001 |title=Fire, climate change, carbon and fuel management in the Canadian boreal forest |journal=Int. J. Wildland Fire |volume=10 |issue=4 |pages=405–13 |doi=10.1071/WF01038 }}</ref> The fire history that characterizes an [[ecosystem]] is its ''[[fire regime]]'', which has 3 elements: (1) fire type and intensity (e.g., crown fires, severe surface fires, and light surface fires), (2) size of typical fires of significance, and (3) frequency or return intervals for specific land units.<ref name="hein2">{{cite book |last=Heinselman |first=M. L. |year=1981 |chapter=Fire intensity and frequency as factors in the distribution and structure of northern ecosystems |pages=7–57 |title=Proceedings of the Conference: Fire Regimes in Ecosystem Properties, Dec. 1978, Honolulu, Hawaii. USDA |series=For. Serv., Washington DC, Gen. Tech. Rep. WO-26 }}</ref> The average time within a fire regime to burn an area equivalent to the total area of an ecosystem is its ''fire rotation'' (Heinselman 1973)<ref name="hein1">{{cite journal |last=Heinselman |first=M. L. |year=1973 |title=Fire in the virgin forests of the Boundary Waters Canoe Area, Minnesota |journal=Quat. Res. |volume=3 |issue=3 |pages=329–82 |doi=10.1016/0033-5894(73)90003-3 |bibcode=1973QuRes...3..329H |s2cid=18430692 }}</ref> or ''fire cycle'' (Van Wagner 1978).<ref name="van">{{cite journal |last=Van Wagner |first=C. E. |year=1978 |title=Age-class distribution and the forest cycle |journal=Can. J. For. Res. |volume=8 |pages=220–27 |doi=10.1139/x78-034 }}</ref> However, as Heinselman (1981) noted,<ref name="hein2"/> each physiographic site tends to have its own return interval, so that some areas are skipped for long periods, while others might burn two-times or more often during a nominal fire rotation.

The dominant fire regime in the boreal forest is high-intensity crown fires or severe surface fires of very large size, often more than 10,000 ha (100&nbsp;km<sup>2</sup>), and sometimes more than 400,000 ha (4000&nbsp;km<sup>2</sup>).<ref name="hein2" /> Such fires kill entire stands. Fire rotations in the drier regions of western Canada and Alaska average 50–100 years, shorter than in the moister climates of eastern Canada, where they may average 200 years or more. Fire cycles also tend to be long near the tree line in the subarctic spruce-lichen woodlands. The longest cycles, possibly 300 years, probably occur in the western boreal in floodplain white spruce.<ref name="hein2" />

Amiro et al. (2001) calculated the mean fire cycle for the period 1980 to 1999 in the Canadian boreal forest (including taiga) at 126 years.<ref name="amiro" /> Increased fire activity has been predicted for western Canada, but parts of eastern Canada may experience less fire in future because of greater precipitation in a warmer climate.<ref name="flann">{{cite journal |last1=Flannigan |first1=M. D. |last2=Bergeron |first2=Y. |last3=Engelmark |first3=O. |last4=Wotton |first4=B. M. |year=1998 |title=Future wildfire in circumboreal forests in relation to global warming |journal=J. Veg. Sci. |volume=9 |issue=4 |pages=469–76 |doi=10.2307/3237261 |jstor=3237261 |doi-access=free |bibcode=1998JVegS...9..469F }}</ref>

The mature boreal forest pattern in the south shows [[Abies balsamea|balsam fir]] dominant on well-drained sites in eastern Canada changing centrally and westward to a prominence of [[Picea engelmannii|white spruce]], with [[Picea mariana|black spruce]] and [[Larix laricina|tamarack]] forming the forests on peats, and with jack pine usually present on dry sites except in the extreme east, where it is absent.<ref name="rowe4">{{cite journal |last1=Rowe |first1=J. S. |last2=Scotter |first2=G. W. |year=1973 |title=Fire in the boreal forest |journal=Quaternary Res. |volume=3 |issue= 3|pages=444–64 |doi=10.1016/0033-5894(73)90008-2 |bibcode=1973QuRes...3..444R |s2cid=129118655 }} [E3680, Coates et al. 1994]</ref> The effects of fires are inextricably woven into the patterns of vegetation on the landscape, which in the east favour black spruce, paper birch, and jack pine over balsam fir, and in the west give the advantage to aspen, jack pine, black spruce, and birch over white spruce. Many investigators have reported the ubiquity of charcoal under the forest floor and in the upper soil profile.<ref name="la">{{cite journal |last=La Roi |first=G. H. |year=1967 |title=Ecological studies in the boreal spruce–fir forests of the North American taiga. I. Analysis of the vascular flora |journal=Ecol. Monogr. |volume=37 |issue= 3|pages=229–53 |doi=10.2307/1948439 |jstor=1948439 |bibcode=1967EcoM...37..229L }}</ref> Charcoal in [[soil]]s provided Bryson et al. (1965) with clues about the forest history of an area 280&nbsp;km north of the then-current tree line at Ennadai Lake, District Keewatin, Northwest Territories.<ref name="bryson">{{cite journal |last1=Bryson |first1=R. A. |last2=Irving |first2=W. H. |last3=Larson |first3=J. A. |year=1965 |title=Radiocarbon and soil evidence of former forest in the southern Canadian tundra |journal=[[Science (journal)|Science]] |volume=147 |issue=3653 |pages=46–48 |doi=10.1126/science.147.3653.46 |pmid=17799777 |bibcode=1965Sci...147...46B |s2cid=46218641 }}</ref>

[[File:Shanta2 7-8-2009.jpg|thumb|The [[Shanta Creek Fire]] began in a taiga area that had not had a major fire in over 130 years, and so was allowed to burn unchecked until it began to threaten populated areas.]]
Two lines of evidence support the thesis that fire has always been an integral factor in the boreal forest: (1) direct, eye-witness accounts and forest-fire statistics, and (2) indirect, circumstantial evidence based on the effects of fire, as well as on persisting indicators.<ref name="rowe4" /> The patchwork mosaic of forest stands in the boreal forest, typically with abrupt, irregular boundaries circumscribing homogenous stands, is indirect but compelling testimony to the role of fire in shaping the forest. The fact is that most boreal forest stands are less than 100 years old, and only in the rather few areas that have escaped burning are there stands of white spruce older than 250 years.<ref name="rowe4" />

The prevalence of fire-adaptive morphologic and reproductive characteristics of many boreal plant species is further evidence pointing to a long and intimate association with fire. Seven of the ten most common trees in the boreal forest—[[jack pine]], [[Pinus contorta|lodgepole pine]], [[aspen]], [[Populus balsamifera|balsam poplar]] (''Populus balsamifera''), [[Betula papyrifera|paper birch]], [[Larix laricina|tamarack]], [[Picea mariana|black spruce]] – can be classed as pioneers in their adaptations for rapid invasion of open areas. White spruce shows some pioneering abilities, too, but is less able than black spruce and the pines to disperse seed at all seasons. Only balsam fir and alpine fir seem to be poorly adapted to reproduce after fire, as their cones disintegrate at maturity, leaving no seed in the crowns.

The oldest forests in the northwest boreal region, some older than 300 years, are of white spruce occurring as pure stands on moist [[floodplain]]s.<ref name="rowe3">{{cite book |last=Rowe |first=J. S. |year=1970 |chapter=Spruce and fire in northwest Canada and Alaska |pages=245–54 |editor-last=Komarek |editor-first=E. V. |title=Proc. 10th Annual Tall Timbers Fire Ecology Conference, Tallahassee FL }}</ref> Here, the frequency of fire is much less than on adjacent uplands dominated by pine, black spruce and aspen. In contrast, in the Cordilleran region, fire is most frequent in the valley bottoms, decreasing upward, as shown by a mosaic of young pioneer pine and broadleaf stands below, and older spruce–fir on the slopes above.<ref name="rowe4" /> Without fire, the boreal forest would become more and more homogeneous, with the long-lived white spruce gradually replacing pine, aspen, balsam poplar, and birch, and perhaps even black spruce, except on the [[peat]]lands.<ref name="raup">{{cite journal |last1=Raup |first1=H. M. |last2=Denny |first2=C. S. |year=1950 |title=Photointerpretation of the terrain along the southern part of the Alaska highway |journal=US Geol. Surv. Bull. |volume=963-D |pages=95–135 |doi=10.3133/b963D |doi-access=free |bibcode=1950usgs.rept....6R }}</ref>

==Climate change==
During the last quarter of the twentieth century, the zone of latitude occupied by the boreal forest experienced some of the greatest temperature increases on Earth. Winter temperatures have increased more than summer temperatures. In summer, the daily low temperature has increased more than the daily high temperature.<ref>{{Cite journal |title=Coincidence and Contradiction in the Warming Boreal Forest |journal=Geophysical Research Letters |volume=32 |issue=15 |doi=10.1029/2005GL023331 |bibcode=2005GeoRL..3215715W |date=9 October 2009 |last1=Wilmking |first1=M. |pages=L15715 |doi-access=free }}</ref> The number of days with extremely cold temperatures (e.g., {{convert|-20|to|-40|C|F|disp=semicolon}}) has decreased irregularly but systematically in nearly all the boreal region, allowing better survival for tree-damaging insects.<ref>{{Cite journal|title=Forest disturbances under climate change |journal=Nature |volume=7 |issue=6 |pages=395–402 |date=31 May 2017|doi=10.1038/nclimate3303 |pmid=28861124 |pmc=5572641 |last1=Seidl |first1=Rupert |last2=Thom |first2=Dominik |last3=Kautz |first3=Markus |last4=Martin-Benito |first4=Dario |last5=Peltoniemi |first5=Mikko |last6=Vacchiano |first6=Giorgio |last7=Wild |first7=Jan |last8=Ascoli |first8=Davide |last9=Petr |first9=Michal |last10=Honkaniemi |first10=Juha |last11=Lexer |first11=Manfred J. |last12=Trotsiuk |first12=Volodymyr |last13=Mairota |first13=Paola |last14=Svoboda |first14=Miroslav |last15=Fabrika |first15=Marek |last16=Nagel |first16=Thomas A. |last17=Reyer |first17=Christopher P. O. |bibcode=2017NatCC...7..395S }}</ref> In [[Fairbanks, Alaska]], the length of the frost-free season has increased from 60 to 90 days in the early twentieth century to about 120 days a century later.

It has been hypothesized that the boreal environments have only a few states which are stable in the long term - a treeless tundra/steppe, a forest with >75% tree cover and an open woodland with ~20% and ~45% tree cover. Thus, continued climate change would be able to force at least some of the presently existing taiga forests into one of the two woodland states or even into a treeless steppe - but it could also shift tundra areas into woodland or forest states as they warm and become more suitable for tree growth.<ref>{{Cite journal |last1=Scheffer |first1=Marten |last2=Hirota |first2=Marina |last3=Holmgren |first3=Milena |author-link3=Milena Holmgren |last4=Van Nes |first4=Egbert H. |last5=Chapin |first5=F. Stuart |date=26 December 2012 |title=Thresholds for boreal biome transitions |journal=[[Proceedings of the National Academy of Sciences]] |volume=109 |issue=52 |pages=21384–21389 |bibcode=2012PNAS..10921384S |doi=10.1073/pnas.1219844110 |issn=0027-8424 |pmc=3535627 |pmid=23236159 |doi-access=free}}</ref>

In keeping with this hypothesis, several studies published in the early 2010s found that there was already a substantial drought-induced tree loss in the western Canadian boreal forests since the 1960s: although this trend was weak or even non-existent in the eastern forests,<ref>{{Cite journal |last1=Peng |first1=Changhui |last2=Ma |first2=Zhihai |last3=Lei |first3=Xiangdong |last4=Zhu |first4=Qiuan |last5=Chen |first5=Huai |last6=Wang |first6=Weifeng |last7=Liu |first7=Shirong |last8=Li |first8=Weizhong |last9=Fang |first9=Xiuqin |last10=Zhou |first10=Xiaolu |date=20 November 2011 |title=A drought-induced pervasive increase in tree mortality across Canada's boreal forests |url=https://www.nature.com/articles/nclimate1293 |journal=Nature Climate Change |language=en |volume=1 |issue=9 |pages=467–471 |doi=10.1038/nclimate1293 |bibcode=2011NatCC...1..467P |url-access=subscription }}</ref><ref>{{Cite journal |last1=Ma |first1=Zhihai |last2=Peng |first2=Changhui   |last3=Zhu |first3=Qiuan |last4=Chen |first4=Huai |last5=Yu |first5=Guirui |last6=Li |first6=Weizhong |last7=Zhou |first7=Xiaolu |last8=Wang |first8=Weifeng |last9=Zhang |first9=Wenhua |date=30 January 2012 |title=Regional drought-induced reduction in the biomass carbon sink of Canada's boreal forests |journal=Proceedings of the National Academy of Sciences |language=en |volume=109 |issue=7 |pages=2423–2427  |doi=10.1073/pnas.1111576109 |pmid=22308340 |pmc=3289349 |bibcode=2012PNAS..109.2423M |doi-access=free }}</ref> it was particularly pronounced in the western coniferous forests.<ref>{{Cite journal |last1= Chen |first1=Han Y. H. |last2=Luo  |first2=Yong |date=2 July 2015 |title=Net aboveground biomass declines of four major forest types with forest ageing and climate change in western Canada's boreal forests |url=https://onlinelibrary.wiley.com/doi/10.1111/gcb.12994 |journal=Global Change Biology |language=en |volume=21 |issue=10 |pages=3675–3684 |doi=10.1111/gcb.12994 |pmid=26136379 |bibcode=2015GCBio..21.3675C |s2cid=25403205 |url-access=subscription }}</ref> However, in 2016, a study found no overall Canadian boreal forest trend between 1950 and 2012: while it also found improved growth in some southern boreal forests and dampened growth in the north (contrary to what the hypothesis would suggest), those patterns were statistically weak.<ref>{{Cite journal |last1=Girardin |first1=Martin P. |last2=Bouriaud |first2=Olivier |last3=Hogg |first3=Edward H. |last4=Kurz |first4=Werner |last5=Zimmermann |first5=Niklaus E. |last6=Metsaranta |first6=Juha M. |last7=de Jong |first7=Rogier |last8=Frank |first8=David C. |last9=Esper |first9=Jan |last10=Büntgen |first10=Ulf |last11=Guo |first11=Xiao Jing |last12=Bhatti |first12=Jagtar |date=12 December 2016 |title= No growth stimulation of Canada's boreal forest under half-century of combined warming and CO2 fertilization |journal=Proceedings of the National Academy of Sciences |language=en |volume=113 |issue=52 |pages=E8406–E8414  |doi=10.1073/pnas.1610156113 |pmid=27956624 |pmc=5206510 |bibcode=2016PNAS..113E8406G |doi-access=free }}</ref>

A 2018 [[Landsat]] reanalysis confirmed that there was a drying trend and a loss of forest in western Canadian forests and some greening in the wetter east, but it had also concluded that most of the [[forest loss]] attributed to climate change in the earlier studies had instead constituted a delayed response to anthropogenic disturbance.<ref>{{Cite journal |last1=Sulla-Menashe |first1=Damien |last2=Woodcock |first2=Curtis E  |last3=Friedl |first3=Mark A |date=4 January 2018 |title=Canadian boreal forest greening and browning trends: an analysis of biogeographic patterns and the relative roles of disturbance versus climate drivers |journal=Environmental Research Letters |language=en |volume=13 |issue=1 |page=014007 |doi=10.1088/1748-9326/aa9b88 |bibcode=2018ERL....13a4007S |s2cid=158470300 |doi-access=free }}</ref> Subsequent research found that even in the forests where biomass trends did not change, there was a substantial shift towards the deciduous broad-leaved trees with higher drought tolerance over the past 65 years,<ref>{{Cite journal |last1=Hisano |first1=Masumi |last2=Ryo |first2=Masahiro |last3=Chen |first3=Xinli |last4=Chen |first4=Han Y. H. |date=16 May 2021 |title=Rapid functional shifts across high latitude forests over the last 65 years |url=https://onlinelibrary.wiley.com/doi/10.1111/gcb.15710 |journal=Global Change Biology |language=en |volume=27 |issue=16 |pages=3846–3858 |doi=10.1111/gcb.15710 |pmid=33993581 |bibcode=2021GCBio..27.3846H |s2cid=234744857 |url-access=subscription }}</ref> and another Landsat analysis of 100,000 undisturbed sites found that the areas with low tree cover became greener in response to warming, but tree mortality (browning) became the dominant response as the proportion of existing tree cover increased.<ref>{{Cite journal |last1=Berner |first1=Logan T. |last2=Goetz |first2=Scott J. |date=24 February 2022 |title=Satellite observations document trends consistent with a boreal forest biome shift |journal=Global Change Biology |language=en |volume=28 |issue=10 |pages=3846–3858 |doi=10.1111/gcb.16121 |pmid=35199413 |pmc=9303657 |bibcode=2022GCBio..28.3275B }}</ref>

While the majority of studies on boreal forest transitions have been done in Canada, similar trends have been detected in the other countries. Summer warming has been shown to increase water stress and reduce tree growth in dry areas of the southern boreal forest in central Alaska and portions of far eastern Russia.<ref>{{cite web |url=http://www.libraryindex.com/pages/3196/Boreal-Forests-Climate-Change.html |title=Boreal Forests and Climate Change - Changes in Climate Parameters and Some Responses, Effects of Warming on Tree Growth on Productive Sites |access-date=25 March 2011 |archive-url=https://web.archive.org/web/20110727080310/http://www.libraryindex.com/pages/3196/Boreal-Forests-Climate-Change.html |archive-date=27 July 2011 }}</ref> In Siberia, the taiga is converting from predominantly needle-shedding larch trees to evergreen conifers in response to a warming climate. This is likely to further accelerate warming, as the evergreen trees will absorb more of the sun's rays. Given the vast size of the area, such a change has the potential to affect areas well outside of the region.<ref>{{Cite journal|url=https://www.sciencedaily.com/releases/2011/03/110325022352.htm |title=Russian boreal forests undergoing vegetation change, study shows |journal=Global Change Biology |volume=17 |issue=7 |pages=2370–84 |doi=10.1111/j.1365-2486.2011.02417.x |date=25 March 2011 |access-date=14 January 2012|bibcode=2011GCBio..17.2370S |last1=Shuman |first1=Jacquelyn Kremper |last2=Shugart |first2=Herman Henry |last3=O'Halloran |first3=Thomas Liam |s2cid=86357569 |url-access=subscription }}</ref> In much of the boreal forest in Alaska, the growth of white spruce trees are stunted by unusually warm summers, while trees on some of the coldest fringes of the forest are experiencing faster growth than previously.<ref>{{cite web |url=http://www.newsminer.com/view/full_story/12094427/article-New-study-states-boreal-forests-shifting-as-Alaska-warms |title=Fairbanks Daily News-Miner – New study states boreal forests shifting as Alaska warms |publisher=Newsminer.com |access-date=14 January 2012 |archive-url=https://web.archive.org/web/20120119115807/https://www.newsminer.com/view/full_story/12094427/article-New-study-states-boreal-forests-shifting-as-Alaska-warms |archive-date=19 January 2012 }}</ref> Lack of moisture in the warmer summers are also stressing the birch trees of central Alaska.<ref>{{cite magazine|last=Morello |first=Lauren |url=http://www.scientificamerican.com/article.cfm?id=forest-changes-in-alaska-reveal-changing-climate |title=Forest Changes in Alaska Reveal Changing Climate |magazine=Scientific American |access-date=14 January 2012}}</ref>

[[File:2018 boreal tree species trends.jpg|thumb|The response of six tree species common in Quebec's forests to 2°C and 4°C warming under different precipitation levels.]]

In addition to these observations, there has also been work on projecting future forest trends. A 2018 study of the seven tree species dominant in the Eastern Canadian forests found that while 2&nbsp;°C warming alone increases their growth by around 13% on average, water availability is much more important than temperature and further warming of up to 4&nbsp;°C would result in substantial declines unless matched by increases in precipitation.<ref>{{Cite journal |last1=D'Orangeville |first1=Loïc |last2=Houle |first2=Daniel |last3=Duchesne |first3=Louis |last4=Phillips |first4=Richard P. |last5=Bergeron |first5=Yves |last6=Kneeshaw |first6=Daniel |date=10 August 2018 |title=Beneficial effects of climate warming on boreal tree growth may be transitory |journal=Nature Communications |language=en |volume=9 |issue=1 |page=3213 |doi=10.1038/s41467-018-05705-4 |pmid=30097584 |pmc=6086880 |bibcode=2018NatCo...9.3213D }}</ref> A 2019 study suggested that the forest plots commonly used to evaluate boreal forest response to climate change tend to have less evolutionary competition between trees than the typical forest, and that with strong competition, there was little net growth in response to warming.<ref>{{Cite journal |last1=Luo |first1=Yong |last2=McIntire |first2=Eliot J. B. |last3=Boisvenue |first3=Céline |last4=Nikiema |first4=Paul P. |last5=Chen |first5=Han Y. H. |date=17 June 2019 |title=Climatic change only stimulated growth for trees under weak competition in central boreal forests |journal=Journal of Ecology |language=en |volume=9 |pages=36–46 |doi=10.1111/1365-2745.13228  |s2cid=196649104 |doi-access=free }}</ref>

Climatic change only stimulated growth for trees under weak competition in central boreal forests. A 2021 paper had confirmed that the boreal forests are much more strongly affected by climate change than the other forest types in Canada and projected that most of the eastern Canadian boreal forests would reach a tipping point around 2080 under the [[Representative Concentration Pathway|RCP]] 8.5 scenario which represents the largest potential increase in anthropogenic emissions.<ref>{{Cite journal |last1=Boulanger |first1=Yan |last2=Puigdevall |first2=Jesus Pascual |date=3 April 2021 |title=Boreal forests will be more severely affected by projected anthropogenic climate forcing than mixedwood and northern hardwood forests in eastern Canada |url=https://link.springer.com/article/10.1007/s10980-021-01241-7 |journal=Landscape Ecology |language=en |volume=36 |issue=6 |pages=1725–1740 |doi=10.1007/s10980-021-01241-7 |bibcode=2021LaEco..36.1725B |s2cid=226959320 |url-access=subscription }}</ref> Another 2021 study projected that under the "moderate" [[Shared Socioeconomic Pathways|SSP2-4.5]] scenario, boreal forests would experience a 15% worldwide increase in biomass by the end of the century, but this would be more than offset by the 41% biomass decline in the tropics.<ref>{{Cite journal |last1=Larjavaara |first1=Markku |last2=Lu |first2=Xiancheng |last3=Chen |first3=Xia |last4=Vastaranta |first4=Mikko |date=12 October 2021 |title=Impact of rising temperatures on the biomass of humid old-growth forests of the world |journal=Carbon Balance and Management |language=en |volume=16 |issue=1 |page=31 |doi=10.1186/s13021-021-00194-3 |pmid=34642849 |pmc=8513374 |doi-access=free |bibcode=2021CarBM..16...31L }}</ref>

In 2022, the results of a 5-year warming experiment in North America had shown that the juveniles of tree species which currently dominate the southern margins of the boreal forests fare the worst in response to even 1.5&nbsp;°C or +3.1&nbsp;°C of warming and the associated reductions in precipitation. While the temperate species which would benefit from such conditions are also present in the southern boreal forests, they are both rare and have slower growth rates.<ref>{{Cite journal |last1=Reich |first1=Peter B. |last2=Bermudez |first2=Raimundo |last3=Montgomery |first3=Rebecca A. |last4=Rich |first4=Roy L. |last5=Rice |first5=Karen E. |last6=Hobbie |first6=Sarah E. |last7=Stefanski |first7=Artur |date=10 August 2022 |title=Even modest climate change may lead to major transitions in boreal forests |url=https://www.nature.com/articles/s41586-022-05076-3 |journal=Nature |language=en |volume=608 |issue=7923 |pages=540–545 |doi=10.1038/s41586-022-05076-3 |pmid=35948640 |bibcode=2022Natur.608..540R |s2cid=251494296 |url-access=subscription }}</ref>

A 2022 assessment of [[tipping points in the climate system]] designated two inter-related tipping points associated with climate change - the die-off of taiga at its southern edge and the area's consequent reversion to [[grassland]] (similar to the [[Amazon rainforest]] dieback) and the opposite process to the north, where the rapid warming of the adjacent [[tundra]] areas converts them to taiga. While both of these processes can already be observed today, the assessment believes that they would likely not become unstoppable (and thus meet the definition of a tipping point) until global warming of around 4&nbsp;°C. However, the certainty level is still limited and it is possible that 1.5&nbsp;°C would be sufficient for either tipping point; on the other hand, the southern die-off may not be inevitable until 5&nbsp;°C, while the replacement of tundra with taiga may require 7.2&nbsp;°C.<ref name="Getting tipsy"/><ref name="Explainer"/>

Once the "right" level of warming is met, either process would take at least 40–50 years to finish, and is more likely to unfold over a century or more. While the southern die-off would involve the loss of around 52 billion tons of carbon, the net result is ''cooling'' of around 0.18&nbsp;°C globally and between 0.5&nbsp;°C to 2&nbsp;°C regionally. Likewise, boreal forest expansion into tundra has a net global warming effect of around 0.14&nbsp;°C globally and 0.5&nbsp;°C to 1&nbsp;°C regionally, even though new forest growth captures around 6 billion tons of carbon. In both cases, this is due to the snow-covered ground having a much greater [[albedo]] than the forests.<ref name="Getting tipsy">{{Cite journal |last1=Armstrong McKay |first1=David|last2=Abrams |first2=Jesse |last3=Winkelmann |first3=Ricarda  |last4=Sakschewski |first4=Boris  |last5=Loriani |first5=Sina  |last6=Fetzer |first6=Ingo|last7=Cornell|first7=Sarah |last8=Rockström |first8=Johan |last9=Staal  |first9=Arie |last10=Lenton |first10=Timothy  |date=9 September 2022 |title=Exceeding 1.5°C global warming could trigger multiple climate tipping points |url=https://www.science.org/doi/10.1126/science.abn7950 |journal=Science |language=en |volume=377 |issue=6611 |article-number=eabn7950 |doi=10.1126/science.abn7950 |pmid=36074831 |hdl=10871/131584 |s2cid=252161375 |issn=0036-8075|hdl-access=free |url-access=subscription }}</ref><ref name="Explainer">{{Cite web |last=Armstrong McKay |first=David |date=9 September 2022 |title=Exceeding 1.5°C global warming could trigger multiple climate tipping points – paper explainer |url=https://climatetippingpoints.info/2022/09/09/climate-tipping-points-reassessment-explainer/ |access-date=2 October 2022 |website=climatetippingpoints.info |language=en}}</ref> According to a later study, disappearing of boreal forests can also increase warming despite the effect on albedo, while the conclusion about cooling from deforestation in these areas made by previous studies results from the failure of models to properly capture the effects of evapotranspiration.<ref>{{cite journal |last1=M. Makarieva |first1=Anastassia |last2=V. Nefiodov |first2=Andrei |last3=Rammig |first3=Anja |last4=Donato Nobre |first4=Antonio |title=Re-appraisal of the global climatic role of natural forests for improved climate projections and policies |journal=Frontiers in Forests and Global Change |date=20 July 2023 |volume=6 |article-number=1150191 |doi=10.3389/ffgc.2023.1150191 |doi-access=free |arxiv=2301.09998 |bibcode=2023FrFGC...650191M }}</ref>

Primary boreal forests hold 1,042 billion tonnes of carbon, more than currently found in the atmosphere, 2 times more than all human caused GHG emissions since the year 1870. In a warmer climate their ability to store carbon will be reduced.<ref>{{cite web |title=Primary Forests: Boreal, Temperate, Tropical |url=https://www.woodwellclimate.org/primary-forests-boreal-temperate-tropical/ |website=Woodwell Climate Research Center |date=17 December 2020 |publisher=Woodwell Climate Research Center, INTACT, Griffits University, GEOS institute, Frankfurt Zoological Society, Australian Rainforest Conservation Society |access-date=22 August 2023}}</ref>

==Other threats==

===Human activities===
[[File:Plesetsk satellite assembling facilities.JPG|thumb|[[Plesetsk Cosmodrome]] is situated in the taiga]]

Some of the larger cities situated in this biome are [[Murmansk]],<ref>{{cite web|url=http://www.worldclimate.com/cgi-bin/data.pl?ref=N68E033+1202+0006410G2 |title=Murmansk climate |publisher=Worldclimate.com |date=4 February 2007 |access-date=21 February 2011}}</ref> [[Arkhangelsk]], [[Yakutsk]], [[Anchorage, Alaska|Anchorage]],<ref>{{cite web|url=http://www.worldclimate.com/cgi-bin/data.pl?ref=N61W149+1302+502820C |title=Anchorage climate |publisher=Worldclimate.com |date=4 February 2007 |access-date=21 February 2011}}</ref> [[Yellowknife]], [[Tromsø]], [[Luleå]], and [[Oulu]].

Large areas of [[Siberia]]'s taiga have been harvested for [[lumber]] since the collapse of the [[Soviet Union]]. Previously, the forest was protected by the restrictions of the Soviet [[Ministry of Forestry (Soviet Union)|Ministry of Forestry]], but with the collapse of the Union, the restrictions regarding trade with Western nations have vanished. Trees are easy to harvest and sell well, so loggers have begun harvesting Russian taiga evergreen trees for sale to nations previously forbidden by Soviet law.<ref>{{cite web|url=http://www.american.edu/TED/TAIGA.HTM |title=Taiga Deforestation |publisher=American.edu |access-date=21 February 2011}}</ref>

===Insects===
Recent years{{When|date=May 2021}} have seen outbreaks of insect pests in forest-destroying plagues: the spruce-bark beetle (''[[Dendroctonus rufipennis]]'') in [[Yukon]] and Alaska;<ref>{{cite web |url=http://www.colorado.edu/INSTAAR/AW2004/get_abstr.html?id=88 |title=A New Method to Reconstruct Bark Beetle Outbreaks |publisher=Colorado.edu |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20110606091611/http://www.colorado.edu/INSTAAR/AW2004/get_abstr.html?id=88 |archive-date=6 June 2011 }}</ref> the [[mountain pine beetle]] in [[British Columbia]]; the [[aspen]]-leaf miner; the [[larch sawfly]]; the [[spruce budworm]] (''[[Choristoneura fumiferana]]'');<ref>{{cite web |url=http://cfs.nrcan.gc.ca/subsite/budworm |title=Spruce budworm and sustainable management of the boreal forest |publisher=Cfs.nrcan.gc.ca |date=5 December 2007 |access-date=21 February 2011 |archive-url=https://web.archive.org/web/20081202122739/https://cfs.nrcan.gc.ca/subsite/budworm |archive-date=2 December 2008 }}</ref> the spruce coneworm.<ref>{{cite web|url=http://www.fs.fed.us/pnw/pubs/journals/pnw_2006_chapin001.pdf|title=ALASKA'S CHANGING BOREAL FOREST|website=Fs.fed.us|access-date=28 February 2022}}</ref>

===Pollution===
The effect of [[Sulfur dioxide|sulphur dioxide]] on woody boreal forest species was investigated by Addison et al. (1984),<ref name="add">Addison, P.A.; Malhotra, S.S.; Khan, A.A. 1984. "Effect of sulfur dioxide on woody boreal forest species grown on native soils and tailings". ''J. Environ. Qual.'' 13(3):333–36.</ref> who exposed plants growing on native soils and tailings to 15.2 μmol/m<sup>3</sup> (0.34 ppm) of SO<sub>2</sub> on CO<sub>2</sub> assimilation rate (NAR). The Canadian maximum acceptable limit for atmospheric SO<sub>2</sub> is 0.34 ppm. Fumigation with SO<sub>2</sub> significantly reduced NAR in all species and produced visible symptoms of injury in 2–20 days. The decrease in NAR of deciduous species (trembling aspen [''Populus tremuloides''], willow [''Salix''], green alder [''Alnus viridis''], and white birch [''Betula papyrifera'']) was significantly more rapid than of [[Pinophyta|conifers]] (white spruce, black spruce [''Picea mariana''], and jack pine [''Pinus banksiana'']) or an evergreen [[angiosperm]] (Labrador tea) growing on a fertilized Brunisol.

These metabolic and visible injury responses seemed to be related to the differences in S uptake owing in part to higher gas exchange rates for [[deciduous]] species than for [[Pinophyta|conifers]]. Conifers growing in [[oil sands]] tailings responded to SO<sub>2</sub> with a significantly more rapid decrease in NAR compared with those growing in the Brunisol, perhaps because of predisposing toxic material in the tailings. However, [[Sulfur|sulphur]] uptake and visible symptom development did not differ between conifers growing on the 2 substrates.

Acidification of precipitation by anthropogenic, acid-forming emissions has been associated with damage to vegetation and reduced forest productivity, but 2-year-old white spruce that were subjected to simulated [[acid rain]] (at [[PH indicator|pH]] 4.6, 3.6, and 2.6) applied weekly for 7 weeks incurred no statistically significant (P 0.05) reduction in growth during the experiment compared with the background control (pH 5.6) (Abouguendia and Baschak 1987).<ref name="abou">Abouguendia, Z.M.; Baschak, L.A. 1987. "Response of two western Canadian conifers to simulated acidic precipitation". ''Water, Air and Soil Pollution'' 33:15–22.</ref> However, symptoms of injury were observed in all treatments, the number of plants and the number of needles affected increased with increasing rain acidity and with time. Scherbatskoy and Klein (1983)<ref name="scher">Scherbatskoy, T.; Klein, R.M. 1983. "Response of spruce Picea glauca and birch Betula alleghaniensis foliage to leaching by acidic mists". ''J. Environ. Qual.'' 12:189–95.</ref> found no significant effect of [[chlorophyll]] concentration in [[white spruce]] at pH 4.3 and 2.8, but Abouguendia and Baschak (1987)<ref name="abou" /> found a significant reduction in white spruce at pH 2.6, while the foliar sulphur content significantly greater at pH 2.6 than any of the other treatments.

==Protection==
[[File:Peatbogg-pine.JPG|thumb|upright|Peat bog in [[Dalarna]], Sweden. [[Bog]]s and peatland are widespread in the taiga. They are home to a unique flora, and store vast amounts of carbon. In western Eurasia, the [[Scots pine]] is common in the boreal forest.]]

The taiga stores enormous quantities of [[carbon]], more than the world's temperate and tropical forests combined, much of it in [[wetland]]s and [[peatland]].<ref>{{cite journal|pmc=2387060 |title=Boreal forest and global change |date= July 2008|pmid=18006417 |doi=10.1098/rstb.2007.2196 |volume=363 |issue=1501 |journal=Philos. Trans. R. Soc. Lond. B Biol. Sci. |pages=2245–49|last1=Ruckstuhl |first1=K. E. |last2=Johnson |first2=E. A. |last3=Miyanishi |first3=K. }}</ref> In fact, current estimates place boreal forests as storing twice as much carbon per unit area as tropical forests.<ref>{{cite web|title=Report: The Carbon the World Forgot|url=http://www.borealbirds.org/carbonreport.shtml|publisher=Boreal Songbird Initiative|date=12 May 2014}}</ref> Wildfires could use up a significant part of the global carbon budget, so fire management at about 12 dollars per tonne of carbon not released<ref name="ucsusa"/> is very cheap compared to the [[social cost of carbon]].

Some nations are discussing protecting areas of the taiga by prohibiting [[logging]], [[mining]], [[fossil fuel exploration|oil and gas production]], and other forms of development. Responding to a letter signed by 1,500 scientists calling on political leaders to protect at least half of the boreal forest,<ref>{{cite web|title=1,500 Scientists Worldwide Call for Protection of Canada's Boreal Forest|url=http://www.borealbirds.org/scienceletter.shtml|website=Boreal Songbird Initiative|access-date=25 June 2012}}</ref> two Canadian provincial governments, Ontario and Quebec, offered election promises to discuss measures in 2008 that might eventually classify at least half of their northern boreal forest as "protected".<ref>{{cite news|last=Gillespie|first=Kerry|title=Ontario to protect vast tract|url=https://www.thestar.com/article/460305|access-date=25 June 2012|newspaper=Toronto Star|date=15 July 2008|archive-date=29 February 2012|archive-url=https://web.archive.org/web/20120229221024/http://www.thestar.com/article/460305}}</ref><ref>{{cite news|last=Marsden|first=William|title=Charest promises to protect north|url=http://www.canada.com/montrealgazette/news/story.html?id=129450f0-d3c0-4337-8f09-9977ff6c1f40|access-date=25 June 2012|newspaper=Montreal Gazette|date=16 November 2008|archive-url=https://web.archive.org/web/20110405215648/https://www.canada.com/montrealgazette/news/story.html?id=129450f0-d3c0-4337-8f09-9977ff6c1f40|archive-date=5 April 2011}}</ref> Although both provinces admitted it would take decades to plan, working with Aboriginal and local communities and ultimately mapping out precise boundaries of the areas off-limits to development, the measures were touted to create some of the largest protected areas networks in the world once completed. Since then, however, very little action has been taken.

For instance, in February 2010 the Canadian government established limited protection for 13,000 square kilometres of boreal forest by creating a new 10,700-square-kilometre park reserve in the Mealy Mountains area of eastern Canada and a 3,000-square-kilometre waterway provincial park that follows alongside the Eagle River from headwaters to sea.<ref>{{cite web|url=http://blogs.nationalgeographic.com/blogs/news/chiefeditor/2010/02/boreal-landscapes-added-to-canada-parks.html|archive-url=https://web.archive.org/web/20100215002401/http://blogs.nationalgeographic.com/blogs/news/chiefeditor/2010/02/boreal-landscapes-added-to-canada-parks.html|archive-date=15 February 2010|title= Boreal landscapes added to Canada's parks Boreal landscapes added to Canada's parks |last=Braun |first=David|date=7 February 2010|work=NatGeo News Watch: News Editor David Braun's Eye on the World|publisher=National Geographic Society|access-date=17 February 2010}}</ref>

==Natural disturbance==
One of the biggest areas of research and a topic still full of unsolved questions is the recurring disturbance of fire and the role it plays in propagating the lichen woodland.<ref name="Kurkowski 1911">Kurkowski, 1911.</ref> The phenomenon of wildfire by lightning strike is the primary determinant of understory vegetation, and because of this, it is considered to be the predominant force behind community and ecosystem properties in the lichen woodland.<ref name="Nilsson 421">Nilsson, 421.</ref> The significance of fire is clearly evident when one considers that understory vegetation influences tree seedling germination in the short term and decomposition of biomass and nutrient availability in the long term.<ref name="Nilsson 421"/>

The recurrent cycle of large, damaging fire occurs approximately every 70 to 100 years.<ref>Johnson, 212.</ref> Understanding the dynamics of this ecosystem is entangled with discovering the successional paths that the vegetation exhibits after a fire. Trees, shrubs, and lichens all recover from fire-induced damage through vegetative reproduction as well as invasion by propagules.<ref name="Johnson 200">Johnson, 200</ref> Seeds that have fallen and become buried provide little help in re-establishment of a species. The reappearance of lichens is reasoned to occur because of varying conditions and light/nutrient availability in each different microstate.<ref name="Johnson 200"/> Several different studies have been done that have led to the formation of the theory that post-fire development can be propagated by any of four pathways: self replacement, species-dominance relay, species replacement, or gap-phase self replacement.<ref name="Kurkowski 1911"/>

Self-replacement is simply the re-establishment of the pre-fire dominant species. Species-dominance relay is a sequential attempt of tree species to establish dominance in the canopy. Species replacement is when fires occur in sufficient frequency to interrupt species dominance relay. Gap-Phase Self-Replacement is the least common and so far has only been documented in Western Canada. It is a self replacement of the surviving species into the canopy gaps after a fire kills another species. The particular pathway taken after fire disturbance depends on how the landscape is able to support trees as well as fire frequency.<ref>Kurkowski, 1912.</ref> Fire frequency has a large role in shaping the original inception of the lower forest line of the lichen woodland taiga.

It has been hypothesized by Serge Payette that the spruce-moss forest ecosystem was changed into the lichen woodland biome due to the initiation of two compounded strong disturbances: large fire and the appearance and attack of the [[spruce budworm]].<ref name="Payette 289">Payette, 289.</ref> The spruce budworm is a deadly insect to the spruce populations in the southern regions of the taiga. J.P. Jasinski confirmed this theory five years later stating, "Their [lichen woodlands] persistence, along with their previous moss forest histories and current occurrence adjacent to closed moss forests, indicate that they are an [[alternative stable state]] to the spruce–moss forests".<ref>Jasinski, 561.</ref>

==Taiga ecoregions==
{{Paleartic boreal forests/taiga}}
{{Nearctic boreal forests/taiga}}

==See also==
{{Portal|Ecology|Environment}}
* [[Birds of North American boreal forests]]
* [[Boreal Forest Conservation Framework]]
* [[Drunken trees]]{{Snd}}effect of global warming on the taiga
* [[Fire and carbon cycling in boreal forests]]
* [[Intact forest landscape]]
* [[Agafia Lykov]]
* [[Scandinavian and Russian taiga]]
* [[Success of fire suppression in northern forests]]
* [[Taiga Rescue Network|Taiga Rescue Network (TRN)]]

==References==
{{Reflist|30em}}

; General references
{{Refbegin}}
* {{cite book |last1=Arno |first1=S. F. |last2=Hammerly |first2=R. P. |name-list-style=amp |year=1984 |title=Timberline. Mountain and Arctic Forest Frontiers |publisher=The Mountaineers |location=Seattle |isbn=0-89886-085-7 }}
* {{cite book |last1=Arno |first1=S. F. |last2=Worral |first2=J. |name-list-style=amp |last3=Carlson |first3=C. E. |year=1995 |chapter=Larix lyallii: Colonist of tree line and talus sites |pages=[https://archive.org/details/CAT10699418/page/72 72–78] |editor-last=Schmidt |editor-first=W. C. |editor2-last=McDonald |editor2-first=K. J. |title=Ecology and Management of Larix Forests: A Look Ahead |chapter-url=https://archive.org/details/CAT10699418 |series=USDA Forest Service General Technical Report GTR-INT-319 }}
* {{cite journal |last=Hoffmann |first=Robert S. |year=1958 |title=The Meaning of the Word 'Taiga' |journal=Ecology |volume=39 |issue=3 |pages=540–541 |doi=10.2307/1931768 |jstor=1931768 |bibcode=1958Ecol...39..540H }}
* {{cite journal |last=Jasinski |first=J. P. |title=The Creation of Alternative Stable States in Southern Boreal Forest: Quebec, Canada |journal=Ecological Monographs |volume=75 |issue=4 |year=2005 |pages=561–583 |doi=10.1890/04-1621 |bibcode=2005EcoM...75..561J }}
* {{cite journal |last=Johnson |first=E. A. |title=Vegetation Organization and Dynamics of Lichen Woodland Communities in the Northwest Territories |journal=Ecology |volume=62 |issue=1 |year=1981 |pages=200–215 |doi=10.2307/1936682 |jstor=1936682 |s2cid=86749540 }}
* {{cite journal |last=Kurkowski |first=Thomas |title=Relative Importance of Different Secondary Successional Pathways in an Alaskan Boreal Forest |journal=Canadian Journal of Forest Research |volume=38 |issue=7 |year=2008 |pages=1911–1923 |doi=10.1139/X08-039 |bibcode=2008CaJFR..38.1911K |s2cid=17586608 }}
* {{cite journal |last=Payette |first=Serge |title=Origin of the lichen woodland at its southern range limit in eastern Canada: the catastrophic impact of insect defoliators and fire on the spruce-moss forest |journal=Canadian Journal of Forest Research |volume=30 |issue=2 |year=2000 |pages=288–305 |doi=10.1139/x99-207 |bibcode=2000CaJFR..30..288P }}
* {{cite journal |last=Nilsson |first=M. C. |title=Understory vegetation as a forest ecosystem driver, evidence from the northern Swedish boreal forest |journal=Frontiers in Ecology and the Environment |volume=3 |issue=8 |year=2005 |pages=421–428 |doi=10.1890/1540-9295(2005)003[0421:UVAAFE]2.0.CO;2 }}
{{Refend}}

==Further reading==
{{Refbegin}}
* {{Cite book |last=Day |first=Trevor |author2=Richard Garratt |date=2006 |title=Taiga |url=https://books.google.com/books?id=n3sdmk_SCXsC&q=Taiga&pg=PP1 |publisher=Facts On File |isbn=978-0-8160-5329-2}}
* {{Cite book |last=Gawthrop |first=Daniel |author-link=Daniel Gawthrop (writer) |date=1999 |title=Vanishing Halo: Saving the Boreal Forest |url=https://books.google.com/books?id=t-SDCgAAQBAJ |publisher=Greystone Books/David Suzuki Foundation |isbn=978-0-89886-681-0}}
* {{Cite book |last=Sayre |first=April Pulley |date=1994 |title=Taiga |url=https://books.google.com/books?id=yvGkDWBoXHsC&q=Taiga&pg=PP1 |publisher=Twenty-First Century Books |isbn=978-0-8050-2830-0}}
{{Refend}}

==External links==
{{Commons category}}
* [http://www.borealbirds.org/ethnobotany.shtml The Conservation Value of the North American Boreal Forest from an Ethnobotanical perspective] a report by the [http://borealbirds.org Boreal Songbird Initiative]
* [http://www.borealcanada.ca Boreal Canadian Initiative]
* [https://regeneration.org/nexus/boreal-forests Boreal Forests] Project Regeneration
* [https://web.archive.org/web/20090710005908/http://www.interboreal.org/ International Boreal Conservation campaign]
* [http://www.barrameda.com.ar/ecology/the-tundra-and-taiga.htm Tundra and Taiga] {{Webarchive|url=https://web.archive.org/web/20080217002240/http://www.barrameda.com.ar/ecology/the-tundra-and-taiga.htm |date=17 February 2008 }}
* [https://web.archive.org/web/20120129160029/http://www.greenpeace.org/canada/en/campaigns/boreal/ Threats to Boreal Forests] Greenpeace
* [https://web.archive.org/web/20100501161515/http://ran.org/what_we_do/old_growth/campaigns/wake_up_weyerhaeuser Campaign against lumber giant Weyerhaeuser's logging practices in the Canadian boreal forest] Rainforest Action Network
* [https://web.archive.org/web/20060712230252/http://www.canadiangeographic.ca/atlas/themes.aspx?id=artic&lang= Arctic and Taiga] Canadian Geographic
* [https://web.archive.org/web/20110228160520/http://taiga.terraformers.ca/ Terraformers] Canadian Taiga Conservation Foundation
* [http://earthobservatory.nasa.gov/Laboratory/Biome/bioconiferous.html Coniferous Forest, Earth Observatory] {{Webarchive|url=https://web.archive.org/web/20080704133614/http://earthobservatory.nasa.gov/Laboratory/Biome/bioconiferous.html |date=4 July 2008 }} NASA
* [http://www.taigarescue.org Taiga Rescue Network (TRN)] {{Webarchive|url=https://web.archive.org/web/20130406214022/http://www.taigarescue.org/ |date=6 April 2013 }} A network of NGOs, indigenous peoples or individuals that works to protect the boreal forests.
* [https://web.archive.org/web/20120905010259/http://www.cas.vanderbilt.edu/bioimages/ecoframe-list.htm Index of Boreal Forests/Taiga ecoregions] at bioimages.Vanderbilt.edu
* [https://web.archive.org/web/20101213002253/http://www.nature.org/wherewework/northamerica/canada/work/art12507.html The Canadian Boreal Forest] The Nature Conservancy and its partners
* [https://web.archive.org/web/20090316135659/http://www.ups.edu/x6111.xml Slater museum of natural history: Taiga]
* [http://www.wilds.mb.ca/taiga/index.html Taiga Biological Station]—founded by William (Bill) Pruitt Jr., [[University of Manitoba]].

{{Biomes}}
{{Authority control}}

[[Category:Taiga and boreal forests| ]]
[[Category:Köppen climate types]]
[[Category:Physiographic provinces]]
[[Category:Subarctic]]
[[Category:Terrestrial biomes]]
[[Category:Turkic words and phrases]]