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170 FOREST STRUCTURE IN KUMAON HIMALAYA<br />

Density <strong>and</strong> diversity estimates<br />

Density <strong>of</strong> trees, shrubs <strong>and</strong> ground vegetation<br />

was calculated follow<strong>in</strong>g Greig - Smith (1983). The<br />

diversity values for each layer (tree, shrub <strong>and</strong><br />

ground vegetation) were calculated us<strong>in</strong>g Shannon<br />

- Wiener’s diversity <strong>in</strong>dex follow<strong>in</strong>g Magurran<br />

(1988). The species richness was calculated us<strong>in</strong>g<br />

Margelef’s species richness <strong>in</strong>dex (Magurran<br />

1988). One-way ANOVA (Zar 1984) was used to<br />

detect significant differences <strong>in</strong> density, diversity<br />

<strong>and</strong> richness for the vegetation layers <strong>in</strong> all the<br />

surveyed <strong>forest</strong> st<strong>and</strong>s.<br />

Classification <strong>and</strong> ord<strong>in</strong>ation <strong>of</strong> species <strong>and</strong><br />

sites<br />

The vegetation was classified on the basis <strong>of</strong><br />

tree species <strong>and</strong> dom<strong>in</strong>ant ground vegetation<br />

(shrub <strong>and</strong> herb species) us<strong>in</strong>g TWINSPAN (Twoway<br />

<strong>in</strong>dicator species analysis) computer program<br />

(Hill 1979 a). Same data matrix was used for<br />

ord<strong>in</strong>ation <strong>of</strong> tree species as well as sites (<strong>forest</strong><br />

st<strong>and</strong>s) through Detrended Correspondence<br />

Analysis (DCA) <strong>in</strong> computer program DECORANA<br />

(Hill 1979 b). The vegetation attributes (density,<br />

diversity <strong>and</strong> richness) <strong>of</strong> the 23 sites along with<br />

altitude, number <strong>of</strong> stumps, lopped trees <strong>and</strong> cattle<br />

dung were subjected to Pr<strong>in</strong>cipal Component<br />

Analysis (PCA).<br />

Stepwise multiple regression was used to<br />

obta<strong>in</strong> correlation between the DCA axes, <strong>and</strong><br />

measured environmental <strong>and</strong> vegetation<br />

attributes. All data matrices were st<strong>and</strong>ardized<br />

follow<strong>in</strong>g Zar (1984) to achieve normality <strong>and</strong><br />

reduce heteroscadesticity.<br />

Rarity <strong>in</strong>dex<br />

A rarity <strong>in</strong>dex was generated to identify rare<br />

tree species <strong>of</strong> Kumaon. For this purpose two<br />

parameters were taken <strong>in</strong>to account-<br />

a) Qualitative proportion <strong>of</strong> each tree species <strong>in</strong><br />

Kumaon (PQA)<br />

Table 1. Location details <strong>and</strong> distribution <strong>of</strong> sampl<strong>in</strong>g plots <strong>in</strong> different <strong>forest</strong> st<strong>and</strong>s <strong>of</strong> Kumaon<br />

Himalaya. RF = Reserve <strong>forest</strong>, POF = Privately owned <strong>forest</strong>, WLS = Wildlife sanctuary, CF =<br />

Community <strong>forest</strong>, Alt. = Altitude, m = meter, asl = above sea level, BWS = B<strong>in</strong>sar Wildlife Sanctuary.<br />

Forest st<strong>and</strong> District Status Sampl<strong>in</strong>g<br />

Plots<br />

Alt. Range<br />

(m asl.)<br />

Coord<strong>in</strong>ates<br />

Kilbery Na<strong>in</strong>i Tal RF 40 2085- 2240 29°25'24.3"N 79°2.6'24.3"E<br />

V<strong>in</strong>aiyak Na<strong>in</strong>i Tal RF 40 2130- 2290 29°27'45.4"N 79°24'31.8"E<br />

Kunjakharak Na<strong>in</strong>i Tal RF 45 2040- 2430 29°39'N 79°18'58.1"E<br />

Maheshkhan Na<strong>in</strong>i Tal RF 40 1820- 2090 29°24'16.2"N 79°33'50.6"E<br />

Gager Na<strong>in</strong>i Tal RF 40 1860- 2220 29°25'11.4"N 79°30'31.9"E<br />

Mukteshwer Na<strong>in</strong>i Tal RF 49 1800- 2260 29°28'34.1"N 79°38'28.1"E<br />

Jill<strong>in</strong>g Na<strong>in</strong>i Tal POF 20 1860- 2010 29°22'1.6"N 79°37'E<br />

BWS Bageshwer WLS 75 1990- 2260 29°42'3.2"N 79°45'E<br />

P<strong>and</strong>avkholi Almora CF 40 2460- 2590 29°48'19.5"N 79°27'E<br />

Sitlakhet Almora RF 15 1880- 1980 29°42'3.2"N 79°45'E<br />

Jageshwer Almora RF 26 2060- 2200 29°39'3.2"N 79°50'52.5"E<br />

Gasi Bageshwer RF 40 2140- 2370 30°04'48.4"N 80°E<br />

Dhakuri Bageshwer RF 55 2470- 2825 30°13'19.5"N 79°55'26.3"E<br />

Wachham Bageshwer RF 50 2410- 2935 30°07'25"N 79°54'37.5"E<br />

Sunderdunga Bageshwer RF 36 2560- 2780 30°13'30.3"N 79°54'18.5"E<br />

P<strong>in</strong>dari Bageshwer CF 39 2200- 2960 30°11'11.3"N 79°59'30"E<br />

Daphiadhura Pithoragarh WLS 40 2020- 2440 29°54'N 80°20'E<br />

Majtham Pithoragarh WLS 40 1595- 2250 29°53'N 80°22'E<br />

G<strong>and</strong>hura Pithoragarh WLS 50 1710- 2045 29°51'40"N 80°14'16.9"E<br />

Sobala Pithoragarh WLS 40 2190- 2650 30°04'16.2"N 80°34'15"E<br />

Duku Pithoragarh WLS 48 1930- 2530 29°56.3'N 80°30'E<br />

Munsiary Pithoragarh RF 25 2655- 2770 30°05'3.2"N 80°14'41.3"E<br />

Mechh Champawat CF 10 1810- 1830 29°16'16.2"N 80°12'18.8"E

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