Chrysolepis chrysophylla

Fagaceae -- Beech family

    Arthur McKee

    Giant chinkapin (Castanopsis chrysophylla), also called  golden chinkapin, giant evergreen-chinkapin, and goldenleaf  chestnut, is an interesting hardwood species in a landscape  dominated by coniferous forests. Over much of its range, giant  chinkapin shows several growth forms; it grows in a wide variety  of habitats but is rarely a dominant component of any stand. In  certain portions of its range, it can be an undesirable  competitor of commercial species during early stages of stand  development. Ecologically and taxonomically, it remains a poorly  understood species.

More info for the terms: association, presence, relict

Distribution of the typical variety Distribution of scrub golden chinquapin Maps courtesy of the Flora of North America Association. 2012, March 20

States (as of 2012) [175]:
United States: CA, OR, WA

Giant chinquapin is native to the Pacific Northwest and California. It is most abundant in the mountain ranges of northwestern California [21,98] and southwestern Oregon [7], including the Coast Ranges [32,40,116], Klamath Mountains [21,85], and western slopes of the Oregon Cascade Range [98]. It is common as far north as the Columbia River [7,82]. Giant chinquapin's distribution extends into the Sierra Nevada [169] including Plumas [112], El Dorado [62,116] and Tulare counties [201]. In Washington, disjunct populations occur in Mason and Skamania counties [27,82,97,98]. Rare dispersal events and occurrence of relict populations from a historically more widespread distribution have been suggested as possible reasons for giant chinquapin's presence in Washington [97].

Scrub golden chinquapin occurs farther south than the typical variety [7,122]. The typical variety is rare south of Marin County [138,139] and is comparatively common from Mendocino and Humboldt counties north to Oregon [3,124]. Scrub golden chinquapin occurs from the Santa Lucia Mountains [122] north along the coast [81] through northern California [81,122,197] to southern Oregon [175,197]. It also occurs in the Sierra Nevada including El Dorado [58,122] and Plumas counties [112].

The natural range of giant chinkapin extends from San Luis Obispo  County in California to Mason County in west-central Washington  (14). In California, it grows primarily in the Coast Ranges, with  a disjunct population in the Sierra Nevada in El Dorado County  (8). In Oregon, it is found in the Coast Ranges as far  north as Benton County, and throughout the Cascade Range. Giant  chinkapin is represented in Washington by two disjunct  populations in Mason and Skamania Counties (13). Shrub forms of  the species are found throughout its range. The tree form is  primarily distributed from Lane County, OR, south to Marin  County, CA. It is found from near sea level in the Coast Ranges  of Oregon and California to over 1525 m (5,000 ft) in elevation  in the Cascades. Although giant chinkapin is generally thought of  as a mid- to low-elevation species, the shrub form can be found  along the crest of the Cascade Range in Oregon from 1525 to 1830  m (5,000 to 6,000 ft) (5).

   
  -The native range of giant chinkapin.

Chrysolepis chrysophylla (Douglas ex Hook.) Hjelmq.:
United States (North America)

Note: This information is based on publications available through Tropicos and may not represent the entire distribution. Tropicos does not categorize distributions as native or non-native.

Castanopsis chrysophylla (Douglas ex Hook.) A. DC.:
United States (North America)

Note: This information is based on publications available through Tropicos and may not represent the entire distribution. Tropicos does not categorize distributions as native or non-native.

United States

Origin: Native

Regularity: Regularly occurring

Currently: Present

Confidence: Confident

More info for the terms: involucre, sclerophyllous, shrub, shrubs, tree, xeric

This description covers characteristics that may be relevant to fire ecology and is not meant for identification. Keys for identification are available (e.g., [7,37,81,82]).

Form and architecture: Giant chinquapin occurs as a tree or a shrub. In general, it is described as ranging from 16 to 100 feet tall (5-30 m) [2,7,21,27,50,82,96,124,173]. The largest trees are up to 150 feet (45 m) tall [122,124] and 5 feet (1.5 m) in diameter [7,27]. Smaller sizes are much more common [61,73,104]. In several studies of giant chinquapin in western Oregon, average DBH ranged from 3.1 to 8.3 inches (7.9-21 cm), and average heights ranged from 19.2 to 43.4 feet (5.9-13.2 m) [70,104,168]. Over 98% of giant chinquapins in an old-growth Douglas-fir community in a western Cascade Range watershed had a DBH in the 6- to 12-inch (15-30 cm) category [61]. Of 101 giant chinquapins in southwestern Oregon, only 1 had a DBH in the 20- to 25-inch (51-64 cm) class, and most were less than 5 inches (13 cm) in DBH [104].

The extent to which genetics and site characteristics influence the growth form of giant chinquapin is unclear. According to a worldwide flora of the order Fagales, the typical variety can be a tree, large shrub, or shrub (<10 feet (3 m) tall), while scrub golden chinquapin only occurs as a shrub [54]. Two California floras suggest trees greater than 50 feet (15 m) tall are the typical variety, while shrubs and small trees up to about 33 feet (10 m) are scrub golden chinquapin [81,122]. However, giant chinquapin is commonly shrubby in Washington [27,197], where only the typical variety occurs [92]. Good sites or periods of favorable conditions may promote tree growth forms [50,98,139] (see Site characteristics). Roof [138,139] states that individual giant chinquapins may develop from shrubs into trees during favorable periods [138]. He noted a pattern of giant chinquapin shrubs on ridges, trees on sheltered north slopes, and intermediate forms in between. He suggests in these situations, it is impossible to determine where the typical variety ends and scrub golden chinquapin begins [139].

Mature trees typically have a straight trunk [7,21,109,124] with a cone-shaped crown [7,81,124] comprised of stout branches [122] that form right angles from the bole [21]. Trees in open areas may have highly tapered boles and more spreading crowns [124]. The bark is thick and furrowed [7,81,82,173]. Giant chinquapin shrubs have a spreading form [7].

Leaves: Giant chinquapins have sclerophyllous evergreen leaves that are lanceolate to oblong and have entire margins [7,27,82,122]. The undersides are yellow-green to golden and fuzzy [3,7,27,82,122]. Leaves range from 2 to 6 inches (5-15 cm) long [3,7,122]. Leaf area of giant chinquapin saplings at H. J. Andrews Experimental Forest averaged 16 cm² per leaf [96]. Leaves remain on trees for about 3 years [27]. Leaves of scrub golden chinquapin commonly have upturned margins [81,122].

Reproductive structures: Male flowers are 1- to 3-inch (2.5-7.6 cm) long [7,109,116,124] catkins [82,116]. Up to 3 female flowers occur in an involucre at the base of the male catkin or in short separate catkins along the stem [81,82,109,116,124]. The flowers emit a strong musty odor [2,7].

Giant chinquapin fruits are nuts. There are 1 to 3 nuts enclosed [109,116,124,199] in a distinctive 4-valved spiny bur [82,98,122]. The bur typically ranges from 0.6 to 1.0 inch (1.5-2.5 cm) across [82,116,124,173], but may be as large as 2 inches (5 cm) [81]. The nuts range from 6 to 15 mm long [3,7,81,82,122] and from 700 [121] to 1,100 per pound [124].

Roots: Giant chinquapin seedlings may have deep-growing roots [98] and often develop a taproot. As they mature, the lateral root system becomes well developed [124].

Longevity: Giant chinquapin live up to 500 years old [2,7,95,116]. Maximum ages of giant chinquapin in the northern California Coast Ranges [116] and in Douglas-fir-hardwood forest in the Klamath Mountains of northern California [95] were from 400 to 500 years. Giant chinquapin may have longer lifespans on xeric than moist sites because heart rot is less common in these areas [95] (see Site characteristics). Maximum ages of about 150 years have been noted on "better sites" in the Pacific Northwest in general [50] and on the H. J. Andrews Experimental Forest in particular [116]. Because of giant chinquapin's sprouting ability, individual genets may be several centuries old [116].

• Botanical description
• RAUNKIAER LIFE FORM

  East Bay Wilds

Trees or erect shrubs , to 45 m. Bark thick, rough. Twigs densely covered with tight, yellowish, peltate trichomes. Leaves: petiole 5-8 mm. Leaf blade flat or folded upward along midvein, margins entire, apex acute or acuminate, surfaces abaxially usually golden or brownish with dense glandular trichomes. Fruits: cupule yellowish, 20-60 mm thick, densely spiny, surface obscured; nut light brown, (6-)8-12(-15) mm, glabrous, completely enclosed by cupule until maturity.

Castanea chrysophylla Douglas ex Hooker, Fl. Bor.-Amer. 2: 159. 1838; Castanopsis chrysophylla (Douglas ex Hooker) A. de Candolle

More info for the terms: association, basal area, cover, density, ecotype, fire regime, hardwood, mesic, series, shrub, shrubs, tree, xeric

Site characteristics: Giant chinquapin occurs in a wide range of sites from warm, dry, exposed locations [7,47,78,79,82,116] to low-elevation mesic forests [95,116,139]. Shrubby forms are more common in relatively harsh environments [124,138,139], including exposed [82], dry, and high-elevation sites ([7,95,116,138], McMinn 1951 cited in [58]). Giant chinquapin trees are typically associated with low-elevation [116] mesic [95,116,139] forests, often on north-facing slopes [95,139], but they also occur on dry sites [116] and may thrive on moderately dry sites (See Moisture availability).

Although many reports associate giant chinquapin with “xeric” sites within its distribution, this term and others referring to moisture regime are often used in a relative sense, making it difficult to compare reports. For instance, 2 sources [51,73] described the western hemlock/giant chinquapin community as a comparatively xeric old-growth community of the western slope of the Oregon Cascade Range [51,73], while Means [117] described this same community as mesic when compared to dry Douglas-fir- and tanoak-dominated communities of the same region. Giant chinquapin was associated with comparatively moist parts of the ponderosa pine zone in central Oregon [42], and it was an indicator species for "moist" vegetation in the South Umpqua Basin of southwestern Oregon, an area that receives comparatively little rainfall (see Precipitation). Species that indicated dry sites in this study area included hollyleaved barberry (Mahonia aquifolium), California fescue (Festuca californica), and ponderosa pine [119].

The distribution of giant chinquapin occurs within an area of generally mild climate [20,113,116,124]. McKee [116] suggests that some shrubby individuals are an ecotype adapted to heavy snowpacks, cool temperatures, and short growing seasons common in the Oregon Cascade Ranges and eastern Oregon.

Elevation
Topography
Soil
Moisture availability
Precipitation
Temperature

Elevation: Giant chinquapin grows from near sea level [82] in the Coast Ranges of Oregon and California [116] to over 5,000 feet (1,500 m) in the Siskiyou Mountains [193]. It occurred on a site ranging from 660 to 1,150 feet (200-350 m) on the eastern slope of the Coast Ranges in Oregon [132]. In the Siskiyou Mountains of California and Oregon, giant chinquapin was most abundant from 2,500 to 3,500 feet (670-1,070 m) and was common from 1,500 to 4,500 feet (460-1,370 m). It was rare from 4,500 to 5,500 feet (1,370-1,680) and was not observed at higher elevations [193]. In central Oregon, giant chinquapin has been noted up to 5,000 feet (1,520 m) in mixed-conifer/snowbrush ceanothus/long-stolon sedge community (Ceanothus velutinus-Carex inops subsp. inops) [108] and ponderosa pine (Pinus ponderosa) communities [125,183]. Giant chinquapin occurred on a site in the Sierra Nevada at 4,300 feet (1,310 m) [93].

Shrubby giant chinquapins occur at higher elevations than giant chinquapin trees ([95,137,138], McMinn 1951 cited in [58]). In the Willamette, Mt Hood, and Siuslaw National Forests of Oregon, giant chinquapin occurs as a tree at low to midelevations and only occurs as a shrub at high elevations [173]. Giant chinquapin is commonly reported below about 4,500 feet in the Cascade Range ([6,164], Weisberg 1995 cited in [19]), while shrubby giant chinquapin occurs along the crest of the Cascade Range in Oregon up to 6,000 feet (1,830 m) [116]. The importance of giant chinquapin trees in 3 Douglas-fir-hardwood forests of the Klamath Mountains of California declined substantially above 3,900 feet (1,200 m), although tree forms occurred up to 5,250 feet (1,600 m) [95]. McKee [116] suggests that there are 3 giant chinquapin ecotypes, 1 of which is a shrubby form occurring at high elevations in the Oregon Cascade Range and eastern Oregon. Scrub golden chinquapin occurs at high elevations in the southern portion of giant chinquapin's range [7].

Topography: Giant chinquapin may be more common on ridges [47,95,151] and slopes [9,96,145,174,180], including those that are steep [47,84,174], than near streams [145] or in valley bottoms [151]. On 2 west-central Oregon watersheds, giant chinquapin was positively (P=0.008) associated with hillside topography [145], and it was inversely associated with percent slope on the Willamette National Forest [174]. In the western Cascade Range in Oregon, giant chinquapin was the dominant species on a site with a 40° slope [96]. Basal area of giant chinquapin in 63 zero-order stream basins averaged 0.2 m²/ha in valleys, 0.7 m²/ha on slopes, and 0.9 m²/ha on ridges [151]. Giant chinquapin occurrence in valley bottoms may be restricted to the interior and southern boundaries of its distribution [84]. For example, giant chinquapin trees had "significant cover" in ravines and valley bottoms in Douglas-fir-hardwood forests in the Klamath Mountains [95].

Although giant chinquapin occurs on all aspects, its growth form [95,139] and occurrence [95,192] suggest that north slopes may be more favorable, at least in some areas. In the Siskiyou Mountains, 47% of giant chinquapin stems were on north- and northeast-facing aspects, while only 5% occurred on south- to west-facing aspects [192]. In Douglas-fir-hardwood communities in the Klamath Mountains, the greatest cover of giant chinquapin trees consistently occurred on north- and northeast-facing aspects, and no substantial giant chinquapin stands occurred on slopes with aspects south of due east or due west [95]. According to Holland [84], giant chinquapins near the southern and interior margins of their distribution are restricted to north slopes. In contrast, on south-facing and southwest-facing slopes in the western Cascade Range in Oregon, giant chinquapin occurred as an overstory dominant [96] and as a midstory dominant under western hemlock (Tsuga heterophylla) [47,73]. In southwestern Oregon, a giant chinquapin-tanoak-sugar pine (Lithocarpus densiflorus-Pinus lambertiana) community usually occurred on south or southwestern aspects [9].

Soil: Giant chinquapin occurs in variable soil types [116] but is commonly associated with rocky [9,10,47,51,76,76,180] and/or unproductive soils [27,116,124,152]. In forests of southwestern Oregon, it often indicates rocky sites [9]. The shrub form commonly occurs on rocky sites [84,86,116]. Within Douglas-fir communities in southwestern Oregon, giant chinquapin was associated with the least productive sites [8].

Soil pH on sites with giant chinquapin is often acidic, with values ranging from around 4.1 [91,190] to 6.2 [5].

Giant chinquapin occurs on sites with various parent materials. Giant chinquapin shrubs occurred in 2 of 3 forest communities occurring on lava flows in Oregon [51]. Giant chinquapin, including scrub golden chinquapin [35,193], is associated with ultramafic [9,134] and serpentine [193] substrates.

It has been suggested that giant chinquapin may be more likely to develop into large trees on sites with deep soils, since these sites generally experience more moderate moisture regimes [116,124].

Moisture availability: Giant chinquapin occurs on sites that experience a wide range of soil moisture regimes, from xeric chaparral communities [116] to mesic redwood (Sequoia sempervirens) forests of the California coast [147]. On the most xeric sites within its range, giant chinquapin occurs mainly as a shrub ([7,95,116,138], McMinn 1951 cited in [58]). Scrub golden chinquapin occurred on dry exposures in central California [7], northwestern California, and southwestern Oregon [116]. The Douglas-fir-giant chinquapin/dwarf Oregon-grape (Pseudotsuga menziesii-Chrysolepis chrysophylla/Mahonia nervosa) association occurs in cool, moist areas of southwestern Oregon [9].

Giant chinquapin is often associated with moderately xeric sites. At lower elevations (2,000-3,000 feet (610-915 m)) on diorite in the Siskiyou Mountains of Oregon and California, it had a bimodal distribution across a moisture gradient based on topographic characteristics, with a peak on submesic sites and a larger peak on xeric sites [193]. Giant chinquapin has been considered an indicator of dry sites in Douglas-fir-western hemlock forests of the Pacific Northwest [50], on the Siuslaw [78] and Willamette [79] National Forests, and for the tanoak series of the Siskiyou Region [11]. Based on plant moisture stress in 2 western hemlock/giant chinquapin communities in the western Cascade Range of Oregon, giant chinquapin had high importance values on dry sites. It was not limited by moisture stress on these sites [202]. Giant chinquapin comprised a substantial component of the biomass of old-growth Douglas-fir stands in the H. J. Andrews Experimental Forest in relatively xeric locations [61]. This experimental forest is located on the west slope of the Cascade Range in central Oregon. A Douglas-fir-giant chinquapin community experienced greater water stress in the summer than 3 other major plant communities on a watershed in H. J. Andrews Experimental Forest [61]. In northwestern California, Douglas-fir-giant chinquapin forests occur on drier slopes than Douglas-fir forests [146]. In comparatively moist environments, giant chinquapin may be limited to openings, while it is increasingly competitive on drier sites [116].

Giant chinquapin may grow larger on comparatively xeric sites [30,61,95,137]. It occurred in the overstory of a dry mixed-conifer site with Douglas-fir and Pacific madrone (Arbutus menziesii), while it occurred in the midstory of a more mesic transition site and a wet site in the western hemlock zone [30]. Giant chinquapin reached its greatest development in the lower, drier portions of the Douglas-fir-grand fir association of the Nash Crater Lava Flows in Linn County, Oregon [137], and it occurred as trees on the driest sites of a west-central Oregon Cascade Range study area [187]. “Driest” must be considered in a relative sense, however, considering Roof’s [139] suggestion that development of large giant chinquapin trees requires "ample" winter rainfall and summer fog, and Keeler-Wolf’s [95] statement that giant chinquapin obtains subdominance in Douglas-fir-hardwood forests that receive ≥60 inches (1,520 mm) of precipitation annually.

In Douglas-fir-hardwood forests of the Klamath Region, giant chinquapin sexual reproduction (see Seedling establishment and plant growth) and density were generally greater on mesic than dry sites. The oldest giant chinquapin trees, estimated as 400 to 500 years old, occurred on the driest site, with annual precipitation from 60 to 70 (1,780 mm) inches. Since heart rot was more prevalent on somewhat moister sites, it was suggested that increased heart rot may have shortened giant chinquapin life spans on mesic sites [95].

Precipitation: Average annual precipitation on sites with giant chinquapin ranges from less than 20 inches (510 mm) in southern California [116] and portions of southern Oregon [74] to more than 160 inches (4,000 mm) in coastal Douglas-fir-western hemlock forests of California [84]. Much winter precipitation in the higher elevations of the Cascade Range [116,124] and central Oregon [44,108] falls as snow, while snow is uncommon along the California coast [84,147]. Giant chinquapin's conical shape and deflexed branches led Keeler-Wolf [95] to conclude that it is more tolerant of snow than tanoak or Pacific madrone and is adapted for mesic, upper-elevations of the Douglas-fir-hardwood zone.

Table 1. Average annual precipitation in regions of the western United States with giant chinquapin Region Average annual precipitation Central Oregon 25-30 inches (635-890 mm) [108,140] Umpqua Valley & Rogue River Basin 20-30 inches (510-760 mm) [74] Western Cascade Range

foothills: 44 inches (1,120 mm) [19]
40-60 inches (1,020-1,520 mm) [74]
91 inches (2,302 mm) [67]

Southern Cascade Range 30 and? 68 inches (760-1,730 mm) California and Oregon Coast Ranges 34-83 inches (865-2,110 mm) [113]
70-100 inches (1,780-2,540 mm) western slope in southern Oregon [74]
48 inches (1,222 mm) east slope in Oregon [132] Klamath Mountains 30 and? 68 inches (760-1,730 mm) [113]
22.3-64.4 inches (576-1,636 mm) [152] Northern California coast 20-118 inches (500-3,000 mm) (Miles and Goudey 1997 cited in [162])
≥98 inches (2,500 mm) east of Cape Mendocino [147] Sierra Nevada 30-68 inches (760-1,730 mm) [113]
67 inches (1,700 mm) [93] Central California coast western slopes: ≥39 inches (1,000 mm) [147]

Throughout most of its range, giant chinquapin experiences moist winters and dry summers [5,44,67,116,124,152,162,164]. This seasonal pattern occurs along the central California coast [147], and in northwestern California [20], southwestern Oregon [74], and central Oregon [44,67,164]. The summers are typically drier in the southern portions of the giant chinquapin's range [116]. In coastal areas, fog may provide additional moisture in the summer months [113,162].

Temperature: Temperatures experienced by giant chinquapin are generally mild [20,74,113,116]. Reported temperatures on sites with or near giant chinquapin range from winter lows of 19 °F (-7 °C) in northwestern California [20] and central Oregon [44] to summer highs of 98 °F (37 °C) on west slopes of the central California coast. On a burned site in central California, July temperatures may have exceeded 110 °F (46 °C) [5]. Number of frost-free days in the interior mountains where giant chinquapin occurs range from 116 to 240, while the number of frost-free days in the Coast Ranges of California and southwestern Oregon ranges from 204 to 338 (McDonald 1981 unpublished report and Stein 1981 unpublished report cited in [113]).

Table 2. Average temperatures (°F) within the giant chinquapin's distribution in winter and summer. When provided, average minima and maxima for each season are displayed, separated by a slash (/). Location Winter Summer Central Oregon 19/42 43/84 [44,67] Klamath Mountains (daily max/mins) 23-36/ 44-54 48-63/89-96 [152]

Klamath Mountains

33-41 62-75 [113] Coast Ranges of California and Oregon 41-50 57-71 [113,132]. Central California not reported/52 not reported/87 [162]

Along the northern distribution of giant chinquapin, there is an east-west gradient with eastern locations getting more snow [8] and having more variable temperatures [8,162] than western locations. This is the case in the Cascade Range [164], the Siskiyou Mountains [8], the Klamath Mountains [152], and the north coastal bioregion of California. In this region, a coastal site had only a 11.5 °F (6.4 °C) difference between winter and summer average maximum temperatures, while a more inland location near Napa Valley had a 34.7 °F (19.3 °C) difference between winter and summer average maximum temperatures [162].

Giant chinquapin is often associated with warm sites [9,77,202], although it can occur on cool sites, where the tree form is more common than shrub form [9,95,139]. It is an indicator of warm sites on the Mt Hood, Willamette [77], and Siuslaw National Forests [78]. The western hemlock-giant chinquapin/salal-Pacific rhododendron (Gaultheria shallon-Rhododendron macrophyllum) community has a warmer climate than western hemlock associations in the Cascade Mountains with less giant chinquapin [9]. Based on soil and air temperatures in western hemlock/giant chinquapin communities in the western Cascade Range of Oregon, giant chinquapin was categorized has having a center of importance on "medium hot" sites [202]. Scrub golden chinquapin occurs on warm exposures in the southern portion of the species' range [7].

Plant communities: Giant chinquapin occurs primarily in the understory of conifer and mixed-conifer-hardwood communities [9,51,73,75,80,86,146,181,194]. Shrub forms, including scrub golden chinquapin, occur in brushfields [74]. See the Fire Regime Table for a list of plant communities in which giant chinquapin may occur and information on the FIRE REGIMES associated with those communities.

Forests and woodlands: Giant chinquapin is most common in the midstory under conifers, although it occasionally occurs in the overstory [9,30]. It occurs in the midstory of Douglas-fir-hardwood [146], mixed-conifer [75,181], mixed-evergreen [80,194], western hemlock [9,51,73], white fir (Abies concolor), and Shasta red fir (Abies magnifica var. shastensis) communities [51,86]. A description of giant chinquapin occurrence in forest and woodland communities is provided in Table 3. Overstory cover in these communities ranges from open [98] to fairly dense [82,84]. In western hemlock/giant chinquapin communities, overstory cover was commonly <50% in the western Cascade Range in Oregon [51,73].

Giant chinquapin rarely occurs in pure stands [97,116]. It was the dominant species on 1 of 102 Forest Inventory and Analysis plots in dry hardwood communities of western Oregon [115]. In a survey of California hardwoods, only 1,000 acres (405 ha) of giant chinquapin-dominated stands were reported inside National Forests, and none were reported outside National Forests [21]. Giant chinquapin stands are isolated [7] and rarely exceed 25 acres (10 ha) [116]. In southwestern Oregon, giant chinquapin occurred in the overstory in stands of tanoak, tanoak and Douglas-fir, tanoak and white fir [9], and Douglas-fir and Pacific madrone [30].

In some forest and woodland communities, giant chinquapin has only been reported as a shrub. These include Jeffrey pine (Pinus jeffreyi) [90,184], mountain hemlock (Tsuga mertensiana) [77], and lodgepole pine (P. contorta)-Douglas-fir [99]. Scrub golden chinquapin occurs in knobcone pine (P. attenuata) communities in California [35] and Jeffrey pine communities in the Klamath Mountains [90].

Table 3. Plant communities in which giant chinquapin is common, including citations distinguishing growth form and/or variety Communities Growth form Conifer-dominated communities Redwood general [2,7,21,84,122,147]
tree [40,62,141,179,190]
scrub golden chinquapin [190]
Mixed-conifer general [21,93,97,106,131,164]
tree [49,50,51,62]
shrub [41,49,50,51,184]
scrub golden chinquapin [112] Ponderosa pine general [125,140,142]
shrub [200]
scrub golden chinquapin [122] Douglas-fir general [7,9,13,21,29,50,51,97,122,172,186,196]
tree [13,50,117]
shrub (large) [143] Western hemlock general [9,78,117]
tree [13,50,51,59,79,117]
shrub [47,79,143] White fir general [8]
tree [50]
shrub [184] Shasta red fir general [8]
tree [10]
shrub [50,51,184] Pacific silver fir (Abies amabilis) shrub [79] Bishop pine (P. muricata) general [91,130,190,191]
scrub golden chinquapin [122] Port-Orford-cedar (Chamaecyparis lawsoniana) general [8,157,193]
Mixed-conifer-hardwood communities Mixed-evergreen general [32,49,51,64,84,100,172,193]
tree [9,40,50,62]
scrub golden chinquapin [190] Douglas-fir-tanoak general [50,162]
Hardwood communities Tanoak general [11,21,84,152]
tree [9,50] Mixed-sclerophyll hardwood general [76]

Brushfields: Giant chinquapin shrubs of both varieties occupy brushfields [25,56,74], including chaparral [7,37]. Giant chinquapin shrubs have been noted in early-successional chaparral [160] and northern maritime chaparral [178]. Scrub golden chinquapin is a component of Oregon brushfields [74] including chaparral communities ([84,122,189], Gratkowski 1961a cited in [51]), such as conifer-forest chaparral ecotones [116], northern maritime chaparral [84], and "climax chaparral" [40]. Species commonly occurring in early-successional brushfield [25,74], early-successional chaparral [160], or successional chaparral [37] include greenleaf manzanita (Arctostaphylos patula) [37,74], hairy manzanita (A. columbiana) [74,160], snowbrush ceanothus [25,37,74], whitethorn ceanothus (C. cordulatus), and wedgeleaf ceanothus (C. cuneatus) [74,160]. Cascara buckthorn (Frangula purshiana), blackberries (Rubus spp.) [25,74], serviceberries (Amelanchier spp.), currants (Ribes spp.), and huckleberries (Vaccinium spp.) [74] may occur in early-successional brushfields.

Giant chinkapin is found in a wide variety of topographic  positions, from valley bottom to ridgetop, and on a wide range of  soils. It achieves the highest cover in the northern portion of  its range on Inseptisols and Entisols. In the southern portion of  its range, highest cover is found on Inceptisols, Ultisols, and  Alfisols. A partial list of parent materials includes basaltic,  dioritic, sedimentary, metasedimentary, and serpentinaceous  types. Giant chinkapin is ubiquitous in some portions of its  range, such as the central part of the Cascades in Oregon, where  it is a minor shrubby component of many forest stands on a range  of soils. It achieves maximum size and cover, however, on sites  that have relatively deep soils that apparently are deficient in  nutrients (17).

    In other portions of its range, giant chinkapin may be quite  restricted, or its different growth forms may be found in  markedly contrasting topographic and soil conditions. Nowhere is  the latter more evident than in the Siskiyou and Klamath  Mountains of southwestern Oregon and north coastal California,  where the shrub form achieves greatest cover on dry, sterile,  rocky ridgetops and southerly facing slopes in chaparral  associations. The tree form is found on northerly aspects on  benches and broad ridges with deep soils and more moderate  moisture stresses (12).

    Over much of the range of giant chinkapin, a general pattern  emerges of a species that is at its competitive best on sites  that are relatively infertile and droughty.

The generally mild climate over the range of giant chinkapin is  characterized by winter precipitation and summer drought.  Rainfall ranges from an annual mean of less than 510 mm (20 in)  in southern California to more than 3300 mm (130 in) in the  Cascades in Oregon. Much of the winter precipitation in the  higher elevations of the Cascades occurs as snow. Little rain  falls from June to September, and the duration and intensity of  drought increase in the southern portion of the range, which has  a Mediterranean climate.

    The tree form of the species occurs in the warm but relatively  moist portion of the climatic conditions within which it grows.  Although the shrubby form is found throughout the species range,  it achieves greatest coverage in the more extreme climates of  xeric sites and higher elevations.

Foodplant / saprobe
fruitbody of Ganoderma applanatum is saprobic on dead trunk of Chrysolepis chrysophylla
Other: minor host/prey

Pure stands of giant chinkapin are uncommon and rarely exceed 10  ha (25 acres). The species is a minor component in a wide range  of forest communities and in its shrub form is a component of  chaparral communities. Common tree associates in the Cascade  Range are Douglas-fir (Pseudotsuga menziesii), incense-cedar  (Libocedrus decurrens), sugar pine (Pinus  lambertiana), western hemlock (Tsuga heterophylla), white  fir (Abies concolor), ponderosa pine (Pinus  ponderosa), Pacific madrone (Arbutus menziesii), and  Shasta red fir (Abies magnifica var. shastensis).  In southwestern Oregon, Douglas-fir, western white pine (Pinus  monticola), incense-cedar, sugar pine, Pacific madrone, and  ponderosa pine continue to be associates, with the additional  species: tanoak (Lithocarpus densiflorus), California  black oak (Quercus kelloggii), knobcone pine (Pinus  attenuata), Port-Orford- cedar (Chamaecyparis  lawsoniana), and canyon live oak (Quercus chrysolepis).  Redwood (Sequoia sempervirens) is added to the list  in north coastal California.

    As a result of the wide ecological amplitude of both shrub and  tree forms, giant chinkapin is found in many Society of American  Foresters forest cover types (3). It is most important in terms  of size and cover in certain communities in the following types:  Pacific Douglas-Fir (Type 229), Douglas-Fir-Western Hemlock (Type  230); Port Orford-Cedar (Type 231); Sierra Nevada Mixed Conifer  (Type 243), and Pacific Ponderosa Pine-Douglas-Fir (Type 244).

    Common shrub species found in association with giant chinkapin in  the Cascades in central Oregon are Pacific rhododendron (Rhododendron  macrophyllum), salal (Gaultheria shallon), Oregongrape  (Berberis nervosa), Pacific dogwood (Cornus  nuttallii), and baldhip rose (Rosa gymnocarpa). Shrub  associates in the Cascades in southern Oregon include: California  dewberry (Rubus ursinus), baldhip rose, common snowberry  (Symphoricarpos albus), salal, and ocean-spray (Holodiscus  discolor). In southwestern Oregon, common shrub associates  are: canyon live oak, huckleberry oak Quercus vaccinifolia),  poison-oak (Rhus diversiloba), Oregongrape, baldhip  rose, California hazel (Corylus cornuta var. californica),  California dewberry, and a number of manzanita (Arctostaphylos)  species. Low shrub and herb species that are common  associates include: modest whipplea (Whipplea modesta), common  prince's-pine (Chimaphila umbellata), American twinflower  (Linnaea borealis), bracken (Pteridium aquilinum),  and common beargrass (Xerophyllum tenax).

Few diseases or insects are reported to  affect growth and survival of giant chinkapin (6,9), but it is  susceptible to heart-rotting fungi, such as Phellinus igniarius  (9). It is resistant to chestnut blight (Cryphonectria  parasitica) despite its close relationship to chestnut.  Common leaf fungi appear to do little harm. Twig fungi are  reported to be secondary to other agents of damage, and root and  butt rots are rare.

    Although in general giant chinkapin has few insect pests,  seed-infesting species, such as the filbertworm (Melissopus  latiferreanus), may play a significant local role in impeding  regeneration. In portions of its range, certain foliage feeders,  such as California oakworm (Phryganidia californica), can  reduce growth. The roundheaded borer (Phymatodes aeneus)  is occasionally found in dying branches and thin-barked portions  of the bole (6).

More info for the terms: duff, fire severity, fuel, severity, tree, wildfire

Giant chinquapin may have a greater probability of quick recovery following spring fires, low- or moderate-severity fires, fires that are not located in areas that were recently burned, or when large individuals are burned. Many of the factors that influence giant chinquapin's response to fire are unclear, including the inconsistent responses to severe fire (see Plant response to fire).

Reducing fuel loads may result in lower fire severity in communities where giant chinquapin occurs. In a mixed-evergreen community in the Coast Ranges of southwestern Oregon, total tree mortality was highest (80%-100%) in areas that had been thinned 6 years before the fire, intermediate in unthinned controls (53%-54%), and lowest (5%) in areas that were thinned 6 years before and underburned 1 year before the Biscuit Wildfire. Fine fuels (≤3 inch diameter (7.6 cm)) were more abundant on thinned-only sites (27.6 Mg/ha) than on thinned-underburned (5.1 Mg/ha) sites, suggesting that heavy fine fuels led to higher tree mortality on thinned-only sites [135]. Guidelines that were developed in the mid-1970s for managing fuels in the Pacific Northwest include broadcast burning [131]. Amaranthus and McNabb [4] recommend incorporating duff layer protection into prescriptions to minimize bare soil exposure.

Bray [26] reviewed impacts of forest burning on air quality in Washington and Oregon.

More info for the terms: fire exclusion, fire frequency, fire occurrence, fire regime, fire severity, fire-return interval, frequency, fuel, mean fire-return interval, moderate-severity fire, presence, severity, wildfire

Fires in communities with giant chinquapin typically occur in summer or early fall [162,167]. Fires are commonly lightning-caused. Typical FIRE REGIMES range from frequent low-severity fires to infrequent moderate- or high-severity fires. Fire-return intervals have lengthened in several portions of giant chinquapin's range compared to historical intervals. The impacts of this change on giant chinquapin have not been addressed. See the Fire Regime Table for further information on FIRE REGIMES of vegetation communities in which giant chinquapin may occur. For information on fire occurrence and spatial extent in western Oregon from 1200 through 2000, see Berkley [19]. Volland and Dell [182] provide brief general summaries of FIRE REGIMES in the Pacific Northwest by region.

Lightning was and is a common source of ignition in some parts of the giant chinquapin's range. Ignitions by American Indians were common before European settlement [8]. Most of the area burned in the Klamath Mountains in recent decades has been the result of lightning-caused fires (e.g., 1977, 1987, 1999, and 2002) [152]. In contrast, lightning-caused fires are rare in northern coastal California. In a roughly 148,000-acre (60,000 ha) area, only 22 lightning-caused fires were reported from 1960 to 1978 (Sibley unpublished cited in [179]). Lightning is more frequent in southwestern Oregon mixed-conifer-hardwood forests [32] and the Siskiyou Mountains [1] than elsewhere in Oregon or in Washington. There is an average of 12.8 lightning strikes/year/km² in the Klamath Mountains [152] and 1.2 lightning strikes/year/km² in the north coastal bioregion of California [162]. However, the number lightning strikes is not necessarily related to the number of lightning-caused fires, since storms that create the most lightning strikes are typically too wet to start fires [152]. Lightning strikes in Oregon and western Washington are most common in July and August [1].

Fire-return intervals in areas occupied by giant chinquapin vary widely from about 20 years in mixed-evergreen forests [32,167], Douglas-fir-tanoak [162], and Douglas-fir communities [166] of southwestern Oregon to around 150 years in coastal forests of southwestern Oregon [1] and forest dominated or codominated by western hemlock the western Oregon Cascade Range [117]. Giant chinquapin is a component of redwood forests (see Plant communities), where fire-return intervals vary from around 50 years in warm, dry locations up to 500 years in cool, moist, coastal areas [162]. In the west-central Cascade Range in Oregon, mean fire-return interval of the dry, low-elevation sites where giant chinquapin was most likely to occur ranged from 81 to 97 years [186]. Fire frequency ranges from 90 to 150 years in coastal forests of southwestern Oregon and declines to about 50 years along the crest of the Coast Ranges [1]. In the Siskiyou Mountains, fire-return intervals were highly variable, with an average of 20 years [8]. Moisture availability [1,32,41,162] and aspect [166,167,187] probably influence the variability of fire-return intervals.

Giant chinquapin is typically exposed to fires of low to moderate severity. Within the perimeter of the Biscuit Wildfire, most giant chinquapin areas burned at "very low" or "low" severity. Only 4% of individual giant chinquapins and 11% of giant chinquapin community types burned at moderate to high severity [12]. Historically, mixed-conifer-pine (Pinus spp.) communities mostly experienced frequent, low-severity fires, and mixed-conifer-fir (Abies spp.) communities were mostly subject to moderate-severity fire. In both cases, increases in fuels from long periods without fire increase severity. Fire behavior in montane chaparral is influenced by species composition, ratio of dead to live vegetation, and live fuel moistures. When live fuel moistures are high in this community, fire severity is typically low and fires are patchy [163]. In mixed-conifer-hardwood vegetation, fire severity generally ranges from low on dry, hot sites to moderate on cool, moist sites [32]; this trend is presumably due to more frequent fires on dry, hot sites. Fires in the Douglas-fir-tanoak zone are often low- to moderate-severity surface fires, and fires in redwood forests are generally low-severity surface fires, although intensities may be moderate (345-1,730 kW/m) [162]. The Klamath Mountains experience a regime of frequent, low- to moderate-severity fires [152]. Patterns of past fire severity in Douglas-fir forests in the Klamath Mountains in California suggest that upper slopes, ridgetops, and south- and west-facing aspects experienced more severe fires than other topographic positions from 1850 to 1950, a period characterized by infrequent fire and fuel accumulation [166].

In several areas within giant chinquapin's range, including the coastal mountains of northwestern California [161], the western Oregon Cascade Range [187], and the Klamath Mountains [152,166,167], fire-return intervals have increased due to fire exclusion. Possible consequences of reduced fire frequency include altering species composition—for example, Douglas-fir and ponderosa pine stands becoming dominated by grand fir (Abies grandis) [41]—and increased fire severity [8,163]. However, in mixed-evergreen forests of the Klamath-Siskiyou region, severe fire was associated with recently burned areas [126]. Potential explanations for this result include increased presence of shade-intolerant, early-successional species that have greater flammability [126,127] and increased temperatures in open areas [126].

More info for the terms: fire occurrence, fuel, hardwood, litter, shrub, tree, vine

Weatherspoon and Skinner [185] categorized giant chinquapin as having "intermediate flammability" compared to other hardwoods. It was ranked as having lower flammability than California black oak and greater flammability than canyon live oak (Quercus chrysolepis) or interior live oak (Q. wislizeni) [185]. Based on fuel load and fuel drying rating variables, plant communities of southwestern Oregon where giant chinquapin was most common had high estimated likelihood of fire occurrence compared to other communities in the area [8].

Giant chinquapin’s contribution to the fuel load varies by site. Out of 17 species in 6 communities, giant chinquapin had the greatest biomass of any large shrub, reaching 10,838 kg/ha in the western hemlock/giant chinquapin community [143]. In old-growth Douglas-fir communities on a watershed on the H. J. Andrews Experimental Forest, giant chinquapin comprised 1.6% of the 1,168,890 kg/ha total tree biomass on a south ridge and 2.5% of the 798,100 kg/ha total tree biomass on a north slope. In 2 other old-growth Douglas-fir communities in this watershed, giant chinquapin comprised 0.3% to 0.4% of the total tree biomass. On an old-growth Douglas-fir site, giant chinquapin had the 2nd highest contribution to annual biomass accumulation (14.6%) and the 3rd highest on a south ridge (9.5%). Table 8 provides information on the organic matter distribution in these communities [61]. Biomass [168] and crown area [96,176] equation parameters for giant chinquapin are available.

Table 8. Organic matter distribution (kg) in Douglas-fir-giant chinquapin communities of a watershed on the H. J. Andrews Experimental Forest [61] Organic matter component North slope South ridge Watershed average Total aboveground 671,570 982,510 717,900 Roots, coarse (>5 mm) 132,900 193,040 141,270

Roots, fine (<5 mm)

10,900 11,000 11,270 Forest floor (ash free dry weight) 57,170 49,270 51,160 Standing dead 34,500 3,800 24,600 Fallen logs 124,800 55,200 190,000 Organic matter at 0-100 cm soil depths 101,000 90,000 112,960 Ecosystem total 1,132,840 1,384,820 1,249,160

Evergreen hardwood communities of southwestern Oregon were given a fairly low woody debris rating (2 of 5) [65].

Average annual leaf litter decay rate of giant chinquapin collected from 5 western Oregon sites was 0.54. This was an intermediate rate, faster than that of most species investigated but substantially slower than those of vine maple (Acer circinatum) and Pacific dogwood (Cornus nuttallii), the 2 fastest decaying species [177].

More info for the terms: association, basal area, cover, density, fire exclusion, fire severity, fire-free interval, frequency, fuel, hardwood, mesic, prescribed fire, reburn, resistance, severity, shrub, top-kill, tree, wildfire, xeric

• Fire adaptations
• Plant response to fire

  Scrub golden chinquapin sprouting about 19 months after a June wildfire in manzanita chaparral transitioning to mixed-evergreen and redwood forest in the Bonny Dune Ecological Reserve. Photo © Neal Kramer.
Fire adaptations: Giant chinquapin is moderately resistant to fire [50,67,67,152,162] and often sprouts after top-kill by fire [152,162]. Scrub golden chinquapin also sprouts following fire [5]. On 3 Douglas-fir-hardwood forest sites in the Klamath Mountains, occurrence of catfaces and rotten cores implies that the largest giant chinquapins have survived multiple fires [95]. Thick bark [7,81,82,173] and sprouting ability (see Vegetative regeneration) likely contribute to survival of giant chinquapin. The number of stems increased over prefire levels 1 (Table 6) and 2 growing seasons after prescribed fires in a mixed-conifer forest of the Sierra Nevada [94]. Postfire sprouting has been suggested as the mechanism allowing giant chinquapin to persist on mesic sites [116] and on a xeric site in a Douglas-fir-hardwood forest of the Klamath Mountains in California [95]. The occurrence of giant chinquapin meristematic tissue in the mineral soil was suggested as a reason for giant chinquapin's greater resistance to fire compared to tanoak, California black oak (Quercus kelloggii), and manzanitas (Arctostaphylos spp.) in a mixed-conifer forest in the Sierra Nevada [94].

Limited evidence suggests that seedling establishment of giant chinquapin is not common in early postfire environments. Giant chinquapin seeds in the Klamath Mountains [152] and northern coastal regions [162] of California are described as having "no response" to fire, and seedling establishment was not observed following a prescribed fire in a mixed-conifer forest in the Sierra Nevada [94].

Plant response to fire: Reported responses of giant chinquapin to fire range from nearly 25% mortality following a low-severity prescribed fire in spring [94] to high abundance following severe fires [45,86,181]. Greater survival and faster recovery of giant chinquapin may be more likely in large individuals [72,94], following early spring fires, low-severity fires [94], and/or fires occurring after a fire-free interval long enough to allow sprouts to grow to a fire-resistant size [45,108]. Other explanations for variation in fire responses include variation in prefire plant community composition, treatment history, surface-level fire severity, time frame of investigation, and different sensitivities of shrub and tree growth forms. Data from prescribed fire research in a mixed-conifer forest in the Sierra Nevada are used repeatedly in this review [93,94]. See the Research Project Summary of Kauffman's [93,94] study for more details.

Two years following prescribed fires in a mixed-conifer forest on the Blodgett Research Station, giant chinquapin survival on burned sites was significantly lower than on unburned sites, except for a low-severity, early spring fire [94]. Reductions in giant chinquapin density following prescribed fires were not significant (Table 5).

Table 4. Top-kill and survival of giant chinquapin on an unburned site and 2 growing seasons after prescribed fire in different seasons in a mixed-conifer forest in the Sierra Nevada [94] Treatment Percent top-kill Percent survival (SD) Early fall, moderate severity 100 27 (46)a* Late fall, low severity 94.4 39 (50)a Early spring, low severity 93 78 (42)b Late spring, moderate severity 96 40 (50)a Unburned (control) 0 100 (0)b *Different letters indicate a significant difference in survival among treatments (P<0.10).
Table 5. Density (#/ha) of giant chinquapin on an unburned control and before and after burning in different seasons in a mixed-conifer forest in the Sierra Nevada (no significant differences; P>0.1) [94] Treatment 1983 (prefire) 1984 1985 Early fall, moderate severity 33 no data 0 Late fall, low severity 83 42 42 Early spring, low severity 400 233 100 Late spring, moderate severity 200 167 134 Unburned (control) 167 134 100

Some general information suggests that fire has little impact on giant chinquapin occurrence. Frequency of giant chinquapin was "somewhat stable" 2 to 3 years after the Biscuit Wildfire on the Rogue River-Siskiyou National Forest [24]. In a ponderosa pine stand in central Oregon, giant chinquapin was present in the understory of an unburned area and an area burned 6 years previously [142].

In some areas, giant chinquapin may be more common on burned sites than unburned sites. On the Rogue River National Forest in southwestern Oregon, giant chinquapin was not present on a harvested site where slash was not burned, but it was common in portions of the same harvested area where slash was burned. Preharvest differences in the 2 treatments were not addressed [114]. On the H. J. Andrews Experimental Forest, giant chinquapin was listed as an invader of burned areas—that is, a species that occurred in clearcut and burned sites not in adjacent forests [198].

The limited data available as of 2012 suggest that giant chinquapin may recover to prefire abundance in less than 15 years after fire. In western Oregon, giant chinquapin cover reached 6.3% on plots subject to clearcutting and moderate-severity slash fires 11 to 16 years previously. Giant chinquapin cover was 5.4% on unburned, clearcut plots [156]. In central Oregon, giant chinquapin recovered prefire canopy cover and density within 5 years of early spring or fall burning (Volland unpublished data cited in [182]). Following logging and burning on 2 watersheds on the H. J. Andrews Experimental Forest, giant chinquapin cover reached predisturbance levels (≤2%) in about 5 to 8 years [67]. In a Douglas-fir forest in the western Oregon Cascade Range, giant chinquapin frequency and cover increased slowly in the 5 years after timber harvest and burning. Giant chinquapin had 11.5% frequency and 0.6% cover before harvest and was absent after slash burning; 5 years after treatments, it had 4.9% frequency and 0.3% cover [46]. In southwestern Oregon and northwestern California, height growth rate of giant chinquapin following harvest and broadcast burning was less than that of Pacific madrone and tanoak. Based on data collected on these sites, Harrington and others [72] developed models of giant chinquapin, tanoak, and Pacific madrone fire response. The giant chinquapin model predicts that the number of sprouts ranging from 0.8 to 3.9 inches (2-10 cm) DBH will increase over the 16 years following harvest and broadcast burning [72].

Plant size: Evidence from 2 studies suggests that the prefire size of giant chinquapin is positively associated with postfire response. Large giant chinquapins produced 100 to 300 sprouts 2 years following prescribed fires in a mixed-conifer forest in the Sierra Nevada, and the author noted survival increased with prefire tree size [94]. Models developed from 8 giant chinquapin clumps in southwestern Oregon and northwestern California predict that giant chinquapin sprout production will increase with the size of the parent tree. Sixteen years after harvest and broadcast burning, 6 sprout clumps of giant chinquapin are predicted when parent-tree basal area is 30 cm², and about 10 sprout clumps of giant chinquapin are predicted when parent-tree basal area is 150 cm² [72].

Site influences on plant response: Few data address the impacts of site characteristics on giant chinquapin's response to fire. Within the 660- to 3,900-foot (200-1,200 m) elevation range impacted by the 2002 Biscuit Wildfire in southern Oregon, the number of regenerating giant chinquapin stems generally increased with elevation, suggesting postfire response at higher elevations of this range was somewhat stronger than that at low elevations [66]. Site characteristics such as elevation or topography explained ≤2% of variation in sprout diameter or hardwood crown size in the 16 years following clearcutting and broadcast burning in southwestern Oregon and northwestern California [72].

Season: Short-term negative impacts of fire on giant chinquapin may be minimal following spring burning [94]. Following both early spring and fall fires in central Oregon, giant chinquapin density and cover reached prefire levels within 5 years (Volland unpublished data cited in [182]). In a mixed-conifer forest in the Sierra Nevada, giant chinquapin survival 2 growing seasons after a low-severity prescribed fire in early spring was not significantly different from that on the unburned control and was greater than that on a low-severity, fall fire (P<0.10) (see Table 4).

Severity: There is conflicting information regarding the impact of severe fire on giant chinquapin, perhaps due in part to variation in use of the term “severe”. Giant chinquapin was considered an increaser following severe fires in shrub and mixed-conifer communities in central [28,181] and southern Oregon [45,86] and the Klamath Region of northern California [152]. Two growing seasons following a 2nd severe wildfire within 15 years on a site in the Klamath-Siskiyou Mountains of southern Oregon, giant chinquapin frequency on the reburn was more than twice that in unburned old-growth vegetation. Giant chinquapin cover was slightly greater on the burned sites [45]. In a ponderosa pine stand just east of the Cascade Range crest in central Oregon, giant chinquapin was a primary shrub species before and after a summer wildfire that killed 95% of trees within 75% of the burned area [28]. Based on plots within the area burned in the Biscuit Wildfire in southern Oregon, giant chinquapin was generally associated with exposed mineral soil, a metric that may indicate high fire severity [66]. Giant chinquapin and greenleaf manzanita and/or pinemat manzanita (Arctostaphylos nevadensis) were mentioned as the first species to establish following "severe logging and burning" in mixed-conifer/snowbrush ceanothus-kinnikinnick (Arctostaphylos uva-ursi) communities in southern Oregon. Giant chinquapin may increase to the point of being problematic for forest regeneration following severe disturbance, including burning, in white fir/giant chinquapin-Oregon boxwood-prince's-pine (Paxistima myrsinites-Chimaphila umbellata) and Shasta red fir-white fir/giant chinquapin-prince's-pine/long-stolon sedge communities of southern Oregon. Giant chinquapin also exhibits large increases following "severe" opening of white fir/snowberry/ strawberry (Symphoricarpos spp.-Fragaria spp.) stands in this area [86] and in the mixed-conifer/common snowberry (Symphoricarpos albus)/forb association of central Oregon [181]. It is a component of shrublands that develop following severe fires that remove canopy cover on "poor" sites in the Klamath Mountain Region of northern California [152].

In contrast, there is evidence that increased fire severity may be detrimental to giant chinquapin, at least in the short term. Twenty-eight years after harvesting and broadcast burning on a watershed in the H. J. Andrews Experimental Forest, giant chinquapin had survived or reestablished in locations that were “lightly” burned but not in the “heavily” burned locations [68]. Scrub golden chinquapin burned severely in a chaparral fire in Sonoma County, California, did not sprout [5]. In a mixed-conifer community in the Sierra Nevada, survival of giant chinquapin 2 years following moderate-severity prescribed fire (as measured by consumption of fuels) ranged from 27% to 40% and was significantly less than survival following a low-severity spring prescribed fire (P<0.1). Survival of giant chinquapin after a moderate-severity spring prescribed fire was 40%, significantly less than the 78% survival after a low-severity spring prescribed fire (see Table 4). Low-severity prescribed fires may have reduced giant chinquapin size in the 1st postfire growing season less than moderate-severity fires (Table 6). After 2 years, giant chinquapin in the low-severity fall prescribed fire treatment had the greatest recovery, 67% of prefire height and 54% of prefire basal diameter [94]. For percent of prefire shrub size 1 year following these prescribed fires, see Table 6. Basal diameter was significantly smaller (P<0.10) after the low-severity spring burn (Table 7) [93]. For more information regarding this study, see the Research Project Summary.

Table 6. Percent of prefire shrub size one growing season after prescribed fire treatments in a mixed-conifer forest in the northern Sierra Nevada [94] Treatment Crown volume Crown area Basal Diameter Height Stems Early fall, moderate severity 0.7 3.1 11.9 22.7 206.9 Late fall, low severity 7.1 13.1 38.7 45.9 111.4 Early spring, low severity 14.2 29.9 33.7 45.0 285.6 Late spring, moderate severity 5.9 10.5 28.4 36.0 186.0 Unburned (control) 127.8a 109.4a 102.0a 114.7a 178.5
Table 7. Average (SD) of several giant chinquapin characteristics before and 2 growing seasons following late spring prescribed fires [93] Characteristic 1983 (prefire) 1984 1985 Basal diameter 6.8 (5.1)a* 2.0 (1.1)b 3.5 (0.9)c Number of stems 4.0 (5.0)a 14.0 (20.0)b 9.0 (11.0)b Height 34.7 (34.8) 19.3 (15.4) 16.4 (9.1) Crown area 0.24 (0.42) 0.04 (0.07) 0.05 (0.07) *Different letters indicate significant differences between years (P<0.10).

Frequency Giant chinquapin has been described as well adapted to frequent fire [116] and occurs in areas that burn regularly [8] (see FIRE REGIMES), but it may be negatively impacted when consecutive fires occur within a few years. In the Klamath-Siskiyou Mountains of southern Oregon, an area burned in severe wildfires in both 1987 and 2002. Frequency of giant chinquapin on reburned sites was more than twice that on sites that burned in only one of these fires, while cover was similar [45]. In contrast, 2 fall prescribed fires within 3 years in a mixed-conifer/snowbrush ceanothus/long-stolon sedge community in central Oregon resulted in the death of 2 of 4 giant chinquapins. The 2 sprouting giant chinquapins went from dominating a 16- to 26-foot (5-8 m) diameter area to individuals with 2 or 3 sprouts per plant each occupying a 10-inch (25 cm) diameter area [108]. For more information regarding this study including detailed information on fuel characteristics and consumption, see the Research Paper by Martin.

Because giant chinquapin is shade tolerant, fire exclusion may favor it in some plant communities. Greater frequency of giant chinquapin in the younger age classes compared to the oldest age class (established before 1950), implies that it responded positively to cessation of annual burning in coniferous forests in the Willamette Valley. Giant chinquapin was reproducing in this community in the absence of fire [34].

More info for the terms: adventitious, root crown, secondary colonizer, shrub, tree

POSTFIRE REGENERATION STRATEGY [159]:
Tree with adventitious buds, a sprouting root crown and/or root sprouts
Tall shrub, adventitious buds and/or a sprouting root crown
Secondary colonizer (on- or off-site seed sources)

Giant chinquapins are often top-killed [94,152,162] or killed [94] by fire. In the Sierra Nevada, survival of giant chinquapin following low- and moderate-severity fires in spring and fall ranged from 27% to 78% (Table 4) [94]. In a mixed-conifer/snowbrush ceanothus/long-stolon sedge community in central Oregon, all 4 giant chinquapins present sprouted following a moderate-severity, fall fire. Two of these individuals died after a 2nd fall fire within 3 years [108]. Dale and others [43] grouped giant chinquapin as a species in which some individuals survive fire.

More info on this topic.

More info for the terms: climax, competition, cover, density, hardwood, series, shrub, succession, tree, xeric

Giant chinquapin occurs in all successional stages [68,95,155]. According to McDonald and Huber [111], most ecologists consider giant chinquapin a persistent subclimax species rather than a climax species.

Giant chinquapin has been observed in recently disturbed stands—as soon as 2 years following fire [24,94]—and in undisturbed stands over 500 years old [13,68]. It was not significantly associated with young (<80), mature (80-180 years), or old-growth (>130 years) forest in the Oregon Cascade Range [68,155] or the Oregon Coast Ranges [68]. In Douglas-fir-hardwood forests of the Klamath Mountains in California, giant chinquapin cover was not associated with total cover of all species, suggesting that giant chinquapin cover has no relationship with seral stage [95]. In Douglas-fir and/or western hemlock communities with Pacific rhododendron/dwarf Oregon-grape understories in the southern Oregon Coast Ranges, giant chinquapin cover averaged 5% in stands 55 to 70 years old, 4% in 190-year-old stands, and 1% in near-climax or climax forests ranging from 300 to 500 years old [13]. In the Coast Ranges in west-central Oregon, giant chinquapin was one of several hardwoods that were prominent in both 55-year-old and >400-year-old stands [132]. Cover of giant chinquapin on the H. J. Andrews Experimental Forest ranged from 0.05% in Douglas-fir plantations that had been clearcut and broadcast burned 5 years previously to 3.85% in 40-year-old plantations. Giant chinquapin cover in 450-year-old undisturbed old growth in this area was 1.42% [148]. Giant chinquapin is commonly reported in stands in intermediate seral stages from about 55 to 200 years old [13,16,30,93,183].

Giant chinquapin may be an important component of early-successional communities. Density of giant chinquapin more than 9 inches (23 cm) DBH in the Coast Ranges of northwestern California was 2.3 trees/ha to 2.9 trees/ha over 30 years following clearcutting and broadcast burning [161]. During 38 years following clearcutting and broadcast burning in 2 watersheds on the H. J. Andrews Experimental Forest, giant chinquapin density peaked at nearly 400 stems/ha in posttreatment years 22 to 25. Giant chinquapin bole biomass increased slowly over the course of the study [107]. In the first 21 years following clearcutting and broadcast burning, giant chinquapin cover was less than 5% [67]. Giant chinquapin has been described as competitive on xeric, unfertile sites early in succession [116] and is a component of early successional brushfields [49,51]. These are either early-successional communities that may slow the establishment of conifers [49,160,163] or edaphic climax communities [40,49,152,163]

Since giant chinquapin is suppressed when overtopped by conifers in some areas [97,107,113], disturbance may be required for it to remain a substantial component of the vegetation [111,116], especially on "good" sites [111,124]. "Suppression mortality" accounted for about half of giant chinquapin stem and bole mortality in the 38 years following clearcutting and broadcast burning on the H. J. Andrews Experimental Forest. "Suppression mortality" was defined as death of small stems in the subcanopy that had slow growth but no damage [107]. Without disturbance, broad-leaved evergreen communities comprised of giant chinquapin, tanoak, and Pacific madrone in southwestern Oregon may slowly succeed to Douglas-fir-tanoak or Douglas-fir forests [76].

On some sites giant chinquapin may be an important component of late-successional and old-growth stands. Cover of giant chinquapin in old-growth Douglas-fir forests (>195 years) on the Oregon Coast Ranges was twice that in mature forests (80-195 years) and more than 10 times that in young (average 55 years) forests (P≤0.1) [155]. Giant chinquapin is considered persistent [68,111] and reproduces in late-successional stages [89,95] in northern California [11,86,89] and the Coast and Cascade ranges in Oregon [68]. Douglas-fir-hardwood [111] and western hemlock-giant chinquapin [47,73,202] are climax communities that may have open structure [47]. In the Klamath Mountains of California, giant chinquapin has been suggested as the hypothetical climax species in the narrow zone above the tanoak and below the white fir series [95]. In contrast, on Douglas-fir and/or western hemlock/Pacific rhododendron/dwarf Oregon-grape forests in the southern Oregon Coast Ranges, giant chinquapin occurrence declined in old-growth stands. It was uncommon and occurred in the shrub layer in canopy gaps within near-climax or climax forests (300-500 years old) [13]. A manual on hardwood silvics also notes giant chinquapin decline in late-successional stages [116].

Shade tolerance: Giant chinquapin has been categorized as tolerant [7,42,88,161], intermediate in tolerance [50,116,124], and intolerant of shade [97,111]. Less photosynthetic tissue per branch volume and slower turnover of foliage of giant chinquapin may contribute to its greater tolerance of shade compared to Arbutus and Quercus [88]. In 4 watersheds in western Oregon, giant chinquapin was not significantly associated with either gaps or forest interiors [145]. In a survey of experts, 50% responded that giant chinquapin had intermediate shade tolerance, 25% responded that it was shade tolerant, and 25% responded that it was shade intolerant. This led Baker [14] to categorize giant chinquapin as intermediately shade tolerant, but he qualified the classification as having a high degree of uncertainty. Tree forms of giant chinquapin [111] and those growing in Washington [97] have been classified as shade intolerant.

Although giant chinquapin can persist in some shaded environments, on at least some sites it has better growth [97], greater abundance [25], and increased sexual reproduction [95] in open conditions. The shrub form has been characterized as more shade-tolerant than the tree form [116,124], and the tree form may be more common in open than in shaded conditions [25]. On sites on the Willamette National Forest and near the Umpqua National Forest, there were "many more" giant chinquapin trees in open clearcuts than in the understory of Douglas fir-western hemlock old-growth, where light intensities ranged from 2.3% to 47.3% of available light [25]. In Washington, the "best" giant chinquapin trees occurred on open sites. Giant chinquapin on an open promontory had sturdy boles and leafy crowns, while giant chinquapin saplings under a Douglas-fir canopy were described as spindly [97]. According to McDonald [109], scrub golden chinquapin growth is typically stiff and upright on exposed sites and low and spreading in shaded areas. Prolonged competition with conifers, including shading in the subcanopy, may lead to mortality of giant chinquapin [107,124]. Sexual reproduction of giant chinquapin was negatively associated (P=0.05) with understory density above 52% cover. High shrub and herb cover may inhibit germination and/or seedling establishment of giant chinquapin [95]. It may be limited to open areas on moist sites [116].

More info for the terms: mesic, xeric

Giant chinquapin exhibits "vigorous" [109,116,124,182] sprouting following damage from fire [5,7,55,67,116,124,152], cutting [7,67,116,124], and/or herbicide application [42,55,57,149]. Sprouts may originate from root crowns [109,111], burls [95,139], or roots [94]. In the Siskiyou Mountains of southwestern Oregon, fire increased the rate of sprouting in scrub golden chinquapins that had previously sprouted after herbicide treatment. This was attributed to sprouting from different portions of the same root system, resulting in one individual counting as 2 or more individuals after burning [55].

Sprouts typically grow much faster than seed-originated individuals. In Douglas-fir-hardwood communities in the Klamath Mountains of northern California, it took sprouts about 50 years to reach 18.1 inches (46 cm) DBH, while seed-originated stems this size averaged about 140 years old [95]. In clearcuts in the Siskiyou Mountains near Cave Junction, Oregon, 32 sprout clumps of giant chinquapin averaging 5.6 years old had an average diameter of 11.8 feet (3.6 m), with the tallest sprout reaching 4.9 feet (1.5 m) [120]. Giant chinquapin sprouts commonly grow faster than conifers for several years [109,116]. Sprout stands tend to self-thin rapidly [124].

Based on data from 3 Douglas-fir-hardwood sites in the Klamath Mountains, vegetative regeneration was the primary means of reproduction on relatively xeric upper slopes, where fires occur more frequently and moisture regimes are less conducive to seedling establishment than on more mesic sites [95].

More info for the terms: density, hardwood, mesic, xeric

Seedling establishment may be most common on mesic, partially shaded sites with open understories and ground layers. On 3 Douglas-fir-hardwood sites in the Klamath Mountains in California, giant chinquapin seedlings were most common on mesic sites in relatively cool, shady environments, such as valley bottoms, and least common on xeric upper slopes. Increased understory density was negatively associated (P<0.05) with sexual reproduction of giant chinquapin [95]. According to a hardwoods silvics manual, giant chinquapin seedlings from 6 to 18 inches (15-45 cm) tall only occurred in relatively open stands on the H. J. Andrews Experimental Forest [116].

According to McDonald [109], giant chinquapin regeneration is often sparse or absent. Giant chinquapin seedling and sapling occurrence on sites where large individuals occur ranges from 0 [109,117] to 160/ha [95]. Giant chinquapin seedling densities were consistently low in the Klamath Mountains of northern California, typically 0 to 3 seedlings/0.1 ha, although on one site they were as high as 16/0.1 ha [95]. In an inventory of California hardwoods, 70% of hardwood forest types had giant chinquapin seedlings and 35% had giant chinquapin saplings [21]. On sites in the western Oregon Cascade Range, giant chinquapin saplings less than 54 inches (137 cm) tall occurred in 3 of 6 community types, with densities ranging from 6.9 to 124.4/ha. Mature giant chinquapin was present in 5 of these 6 communities [117].

Giant chinquapins, including seedlings [124,165], grow slowly [2,98]. By the July following germination, seedlings are typically 1.6 to 3.9 inches (4-10 cm) tall and have a root system that is ≥5.9 inches (15 cm) deep [165]. In the Pacific Northwest, seedlings may be only 6 to 18 inches (15-46 cm) tall after 4 to 12 years [124]. Giant chinquapin and other hardwoods in the understory of conifer forests often produce 2 or more stems within 10 years. The authors suggest that the growth rate of giant chinquapin in the understory is similar to the growth rate of tanoak in the understory [165]. In 2 stands in the Cascade Range that were about 100 years old, giant chinquapin diameter growth over 10 years averaged 1.8 to 2.0 mm/year [116]. In giant chinquapin-dominated or -codominated stands in northern California, trees may take 15 years to grow 1 inch (2.5 cm) in diameter [113]. On 3 Douglas-fir-hardwood sites in the Klamath Mountains of California, giant chinquapin obtained diameters of 24 inches (60 cm) in about 210 to 260 years and diameters of 48 inches (122 cm) in 400 to 500 years [95]. Sprouts grow comparatively quickly (see Vegetative regeneration).

Giant chinquapin's germination rate of 14% to 53% ([121], USDA Forest Service 1948 cited in [87]) is low compared to other hardwoods of southwestern Oregon and northwestern California [113]. Germination occurs in 16 to 24 days ([121], USDA Forest Service 1948 cited in [87]).

Giant chinquapin germination does not require stratification [121]. The seed, like that of other Fagales [23], may be immediately germinable. Cold stratification did not increase giant chinquapin germination (USDA Forest Service 1948 cited in [87]). This suggests germination could occur in fall, although this was not observed in 3 years of observation on the H. J. Andrews Experimental Forest [116].

On the H. J. Andrews Experimental Forest, giant chinquapin seedlings occurred in comparatively open areas. Based on site characteristics, germination likely occurred in partial shade under a light leaf mulch [116].

More info for the term: mast

McKee [116] observed giant chinquapin 40 to 50 years old producing fertile seed, although the age of reproductive maturity is likely earlier. Sprouts that were 6 years old produced some fertile seeds [116]. Fruit production is generally low, with mast seeding occurring cyclically [95,116], at 2-to 5-year intervals [2,95,116]. It takes 2 growing seasons for the fruits to mature [27,81,98,116,122,197,199]. Fertile seeds may be uncommon [7].

Seed production may be locally reduced by insects. For instance, on one site in the H. J. Andrews Experimental Forest nearly 100% of seeds were attacked by insects, while on 2 other sites in the area only 15% of seeds were infested [116]. 

More info for the term: monoecious

Giant chinquapin is monoecious [3,116,124]. It is generally wind pollinated [116,124,136], although bees and other insects are attracted to the flowers [7,116] and may pollinate them [116,124]. It is not known if giant chinquapin is self-compatible [97].

More info for the terms: breeding system, mesic

Giant chinquapin reproduces both sexually and vegetatively [7,94]. In Douglas-fir-hardwood forests of the Klamath Mountains in California, giant chinquapin seedlings and seed-originated saplings occurred on 9 of 11 transects, and sprouts occurred on all 11 transects. On some sites, sprouts were prevalent, while on others sexual reproduction was prevalent; sexual reproduction was typically more prominent on mesic, partially-shaded sites [95] (see Seedling establishment and plant growth).

• Pollination and breeding system
• Seed production
• Seed dispersal
• Seed banking
• Germination
• Seedling establishment and plant growth
• Vegetative regeneration

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More info for the term: phanerophyte

Raunkiaer [133] life form:
Phanerophyte

More info for the terms: shrub, tree

Typical variety: Tree-shrub
Scrub golden chinquapin: Shrub [54]

Follow this link to the U.S. Forest Service Fire Effects Information Service to see a table with fire regime information that may be relevant to habitats in which this species occurs

Data on longevity of giant chinquapin seeds in the field were not available as of early 2012. In general, species with large, burred seeds tend to have transient seed banks [15]. Other genera in Fagales, including oaks [23] and chestnuts [22], have seeds that last through only one growing season. Giant chinquapin likely follows this pattern. Giant chinquapin seeds stored at low temperatures remained viable for at least 3 to 5 years [97,109,121].

Occurrence of clumps of seedlings implies that squirrels may cache giant chinquapin nuts [116].

Giant chinquapin seeds are dispersed by gravity [113,116,124] and animals [113,124,182], including birds [113,116] and squirrels [116].

The competitive ability of giant  chinkapin appears to be improved relative to its associates on  nutritionally poor sites with high moisture stress. The shrub  form is quite tolerant of shade. The tree form is less tolerant  of shade and is probably most accurately classified as  intermediate in tolerance, comparable to incensecedar or sugar  pine with which it is often found. Chinkapin does not attain the  height of many of its associates, is often overtopped in mature  stands of conifers, and declines in importance during later  stages of succession. Over much of its range, some  disturbance-such as fire, logging, or windstorm-is required for  giant chinkapin to remain an important component of the forest on  most sites. Under relatively droughty, infertile conditions, it  can be a very aggressive and undesirable species during early  succession. This is the aspect of giant chinkapin that is perhaps  best known by foresters. Considerably more research has been  conducted on how to rid sites of giant chinkapin than on how to  promote its establishment and growth.

    The most effective site preparation methods for controlling giant  chinkapin have been scarification by tractor or spraying and  burning. Neither slash burning nor hand scalping is effective,  and herbicides produce only moderate results (1,2,7).

    Because giant chinkapin is usually found mixed with other  undesirable species, broad-spectrum herbicides, such as 2,4-D and  triclopyr ester, have been used most frequently (1,2,7).  Formulations of triclopyr ester have proven the most successful  for both aerial and ground applications, including basal and stem  treatment (1,2). The registration status of herbicides is subject  to change. Consultation with local extension agents is advised  when considering herbicide use.

No information available.

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Although highly variable, flowering of giant chinquapin is most common from April [82,173] through early summer [2,27,197] into July [116,124]. Scrub golden chinquapin flowers from June to September [122]. Flowering durations at a particular site may be brief. For example, over 3 years on the H. J. Andrews Experimental Forest, giant chinquapin flowered from mid-June to mid-July, and its fruit ripened from mid-August to early September. Rangewide, fruit ripening may continue into October [116]. Seed dispersal occurs from September into December [116,124]. On the H. J. Andrews Experimental Forest, dispersal was highest in late September, continuing at a lower rate into December [116]. Seeds germinate in late winter [165] or early spring [124,165].

Giant chinkapin sprouts  prolifically when cut or injured. Light understory fires cause  vigorous basal sprouting. Even intense broadcast burns will not  prevent basal sprouts from rapidly regrowing. Height growth of  the sprouts can be rapid, outstripping young conifer growth for  several years. Because of its aggressive sprouting ability, giant  chinkapin is a problem for forest management on many sites.

    The species is well adapted to a regime of frequent fires, which  is reflected in the chaparral shrub form. Also, over much of the  northern portion of the range of giant chinkapin, the tree form  occupies ridgetop positions with other fire-adapted species. Its  ability to exist with the potentially taller conifers may be the  result of both its sprouting ability and relatively high fire  frequency.

Reported germination ranges from 14  to 53 percent (11); one study found it to have the poorest rate  of germination of all hardwoods in the Klamath Province of  southwestern Oregon and northern California (15). Germination is  hypogeal and takes place in 16 to 24 days. Although the rate of  germination was not increased by cold stratification, which  suggested that germination and establishment in the fall are   possible, no such germination was observed during 3 years of  study at the H. J. Andrews Experimental Forest. Natural seedlings  of giant chinkapin which ranged from 15 to 45 cm (6 to 18 in) in  height were found only in relatively open stand conditions in the  Experimental Forest. The individuals appeared to have germinated  under a light leaf mulch in partial shade. The tallest was 12  years old and the shortest 4, but the height-age relationship was  poor. In the northern Coast Ranges of California, the best  seedling establishment occurs on mesic sites without dense layers  of understory vegetation (12).

Vigorously growing  giant chinkapin produce some seed every year with mast years  occurring at 2- to 5-year intervals. Understory shrubs of the  species flower infrequently. Sound seeds are produced by vigorous  trees, apparently of seed origin, that are 40 to 50 years old,  but the age of the first seed production is probably much less.  Six-year-old stump sprouts have produced some sound seeds.

    The production of sound seeds can be greatly reduced locally by  insects. In a sample of seeds at three locations in the H. J.  Andrews Experimental Forest, two sites had less than 15 percent  of the seeds infested, but at the third site nearly 100 percent  of the seeds had been attacked by insects.

    The primary agents of dissemination of giant chinkapin seed are  gravity, squirrels, and birds, not necessarily in that order of  importance. Vertebrates are undoubtedly important vectors.  Several species of birds feed on nuts, and clumps of young  seedlings not originating from sprouts implicate squirrels in  caching food.

Giant chinkapin is monoecious,  with unisexual staminate and pistillate flowers on the same  plant. The staminate flowers form dense catkins 2.5 to 7.6 cm (1  to 3 in) long. One to three pistillate flowers are borne within  an involucre at the base of the staminate catkin or separately  along the stem. Pollination is adapted to wind, but bees frequent  the flowers and probably aid in pollination, much to the dismay   of beekeepers, for it imparts a bad taste to the honey in a mast  year.

    The fruit matures in the fall of the second growing season and  contains one to three hard-shelled nuts within a very spiny  golden brown bur 15 to 25 mm (0.6 to 1.0 in) broad, colloquially  referred to as "porkypine eggs." The nuts are  relatively large1,800 to 2,400/kg (830 to 1,100/lb) (11).

    The phenology of flowering, fruit ripening, and seed dispersal  varies widely over the range of giant chinkapin: flowering  (February to July), fruit ripening (August to October), seed  dispersal (fall). Three years of phenological records at the H.  J. Andrews Experimental Forest in Oregon show local phenology to  be less varied: flowering (mid-June to mid-July), fruit ripening  (mid-August to early September), and seed dispersal (peaking in  late September, but prolonged into early December).

Giant chinkapin is rarely a dominant  species in a stand, and it is often an understory shrub or small  tree of poor form. Growth and yield data are therefore nearly  nonexistent for giant chinkapin despite its ability to develop a  bole of good form and height in dense stands on optimum sites.  The following information was obtained from unpublished data of  the USDA Forest Service and Oregon State University.

    Giant chinkapin provided 11 percent of the total stemwood volume  of about 700 m³/ha (50,000 fbm/acre) in an 80-year-old stand  in the Coast Ranges of Oregon; the stand was site III for  Douglas-fir. The mean diameter at breast height (d.b.h.) of stems  greater than 15 cm (6 in) for giant chinkapin was 34 cm (13.4  in). The largest giant chinkapin in the stand were codominants  about 27 in (90 ft) tall.

    In two stands about 100 years old in the Cascades of Oregon, giant  chinkapin made up 11 and 21 percent of the total stemwood volume.  The two sites were site III and IV for Douglas-fir and had  estimated volumes of about 800 and 550 m³ /ha (57,100 and  39,300 fbm/acre). In the site III stand, giant chinkapin stems  greater than 10 cm (4 in) in d.b.h. averaged 20 cm (7.8 in) in  d.b.h. Their mean diameter increment for the previous 10-year  period was 1.8 mm. (0.07 in) per year.

    The average d.b.h. of giant chinkapin stems greater than 10 cm (4  in) in d.b.h. in the second stand on the poorer site was  larger-30 cm (11.8 in). The mean annual diameter increment for  the previous 10-year period was also slightly larger-2 mm (0.08  in) per year.

    Because of the species' ability to resprout, individual genets of  giant chinkapin could be several centuries old. The species is  susceptible to heart-rotting fungi, which makes aging of large,  old trees difficult. At the H. J. Andrews Experimental Forest in  Oregon, the maximum age was found to range from 130 to 150 years.  In the northern Coast Ranges of California maximum ages were  estimated to range between 400 and 500 years, with the oldest  trees on the more xeric habitats (12).

If much of the earlier discussion seemed to deal with two or  perhaps three species, it may be because the taxonomy of the  genus is poorly understood. Only 2 of about 150 species of Castanopsis  are found in North America. These two are distinct from their  Asian relatives, and systematists have created a new genus for  them, Chrysolepis (4,10). The American species have a  floral morphology that is intermediate to Castanopsis and  Lithocarpus, and it represents the ancient condition of  the family Fagaceae. The new scientific names for the American  species, with the older names in parentheses, are Chrysolepis  chrysophylla (Dougl.) Hjelmqvist (Castanopsis  chrysophylla (Dougl.) A. DC.) for giant chinkapin and Chrysolepis  sempervirens (Kell.) Hjelmqvist (Castanopsis sempervirens  Dudl.) for evergreen chinkapin.

    The uniqueness of the two species at the genus level does not  imply a simple relationship between them. The ranges of the shrub  form of giant chinkapin and of evergreen chinkapin overlap from  northern coastal California into the Cascade Range of Oregon. The  two species probably hybridize where they coexist (8). An  apparently continuous intergradation of characters can be found  in the Cascades in southern Oregon and in the Siskiyou Mountains.

    The two growth forms of giant chinkapin are probably not the  result of plastic phenotypic response to site conditions,  although they may be in portions of the species range. In the  northern Coast Ranges of California, the tree form occupies  relatively moist conditions; the shrub form grows on dry, sterile  ridgetops in chapparal communities. In the central part of the  Cascades of Oregon, the pattern is reversed-the tree form is  found primarily in relatively open and dry ridgetop forest  communities, and the shrub form is spread through the more mesic  forest stands. Only the shrub form is found at high elevations in  the Cascade Range.

    This variation is due to the probable existence of at least three  ecotypes of giant chinkapin: a dry-site chaparral shrub ecotype  of southwestern Oregon and northwestern California that probably  matches the taxonomic category of Castanopsis chrysophylla  var. minor Benth; a high-elevation ecotype adapted to  heavy snowpack, cool temperatures, and short growing seasons  found along the Oregon Cascades and in eastern Oregon; and a tree  form that occurs in forest stands at lower elevations. The latter  ecotype seems well adapted to dry, relatively infertile sites but  can and does do well in more mesic conditions that have a history  of disturbance by fire.

The following is a representative barcode sequence, the centroid of all available sequences for this species.

Barcode of Life Data Systems (BOLDS) Stats
Public Records: 1
Specimens with Barcodes: 1
Species With Barcodes: 1

Information on state- and province-level protection status of plants in the United States and Canada is available at NatureServe.

United States

Rounded National Status Rank: N5 - Secure

Rounded Global Status Rank: G5 - Secure

More info for the terms: cover, density, frequency, hardwood, selection, succession, tree

Given its low commercial value, it is not surprising that there are more data on giant chinquapin response to conifer harvesting than effects of harvesting on giant chinquapin. Giant chinquapin may interfere with conifer growth on some sites and has been targeted for control efforts because of this. Although diseases and insects result in little damage to giant chinquapin, several pests have been observed on giant chinquapin and some have substantial impacts.

Timber harvesting:
Recovery of giant chinquapin following clearcutting or thinning may be fast or rather slow. Giant chinquapin sprouts grow quickly on some clearcuts [110] and may slow the establishment of conifers (see Control).
It was 1 of 3 woody perennials that dominated the ground cover 3 to 28 years after clearcuts and partial cuts in the southern Oregon Cascade Range [158]. In Douglas-fir forests of western Oregon, mortality of giant chinquapin with DBH of ≥2 inches (5 cm) was lower 5 years after heavy thinning than 5 years after lightly thinning or no treatment (P<0.1) [17,18]. In contrast, on a site in the western Cascade Range in Oregon, giant chinquapin increased slowly in the 5 years following harvest and broadcast burning, from 0% frequency and cover to 4.9% frequency and 0.3% cover. Before harvesting, frequency of giant chinquapin was 11.5% and cover was 0.6% [46]. In the Douglas-fir region on northwestern California, giant chinquapin occurred at densities of 4 and 15 individuals/acre on 2 sites in undisturbed forest, but it was not present in areas harvested in the previous 5 years [63].
Little information on harvesting of giant chinquapin was available as of 2012. McDonald and others [113] state that it is not known whether clearcutting promotes giant chinquapin seedling establishment, and Hamilton [69] notes that giant chinquapin's rank as intermediate in tolerance to single tree selection was highly uncertain.
It has been estimated that there are 151 million board feet of giant chinquapin in west-central and southwestern Oregon [128].
Control:
Since hardwoods, including giant chinquapin, may slow conifer regeneration [149,160], giant chinquapin has been the target of control treatments, including bulldozing [149], ground scarification with a tractor [116], and herbicides [36,42,58,118,123]. Early in succession, giant chinquapin sprouts may interfere with conifer growth [109,116], particularly that of Douglas-fir [118,160,165]. The low light intensities under giant chinquapin are likely to reduce conifer seedling growth [120]. Douglas-fir size was negatively associated with hardwood density 10 years following harvesting in plantations in southwestern Oregon (Harrington 1989 cited in [165]). Bulldozing at least 6 inches (15 cm) of soil to remove giant chinquapin's small sprouting roots [149] or scarification by tractor [116] have been suggested as effective control techniques.
Giant chinquapin is resistant to herbicides [76,116,149,160]. Multiple applications may increase effectiveness; 3 treatments in 5 years resulted in 60% mortality in southeastern Oregon [57]. In contrast, spraying followed by burning followed by 2 more applications of herbicide in a 4-year period resulted in increases in scrub golden chinquapin in a brushfield in the Siskiyou Mountains [55]. Several articles address the effectiveness of various herbicides and application methods in controlling giant chinquapin, including Conard and Emmingham [36], Dahms [42], and Newton and Roberts [123].
Diseases and insect pests:
Generally, diseases and insects have little impact on giant chinquapin [7,116,124]. Leaf fungi do little damage and root rots are rare [116]. Giant chinquapin is most susceptible to heart-rotting fungi, such as Phellinus igniarius. The filbertworm (Melissopus latiferreanus) may impact reproduction [116,124] (see Seed production).
See these sources for further information: [25,31,38,39,105,116,124,144,150,195].

A small market exists for giant chinkapin wood for furniture and  cabinet stock, paneling, and decorative veneer (16). There are  several reasons for its limited use, despite its ability to  develop a tall, clear, straight bole under average growing  conditions. It rarely occurs naturally in pure stands, being  typically a minor hardwood component of predominantly coniferous  forests. Also, most mills in the conifer-dominated industry of  the Pacific States will not take giant chinkapin because of added  inventory problems for little additional volume. Finally, it is  one of the most difficult hardwoods in the United States to cure,  as it tends to check badly (16), and transportation costs keep it  from being moved long distances to the few mills equipped to  process it. As a consequence, giant chinkapin is often felled and  left on the site or is bucked into firewood.

    Giant chinkapin is an important species for wildlife because of  the cover and food it provides. Its ability to grow on harsh  sites on infertile soils, and to sprout rapidly after fire, also  makes it important for soil stabilization in watersheds.