Ecological Archives E087-002-A5

James W. Raich, Ann E. Russell, Kanehiro Kitayama, William J. Parton, and Peter M. Vitousek. 2006. Temperature influences carbon accumulation in moist tropical forests. Ecology 87:76–87.

Appendix E. Carbon storage (Mg/ha) in mature moist broad-leaved evergreen tropical forests.  See Notes at end of table for details.

Site

MAT (°C)

Aboveground live biomass

Root biomass

Surface litter

SOC (top 1 m)

Coarse woody debris

Total living mass

Total detritus

Brazil, Manaus

27.2

195

32

3

135

12

227

150

Costa Rica, La Selva, Ultisols

25.8

75

40

2

204

25

115

232

Ivory Coast, Banco plateau

26.2

246

24

1

215

(25)

270

241

Jamaica, Mor Ridge

15.5

100

26

5

250§

4

126

259

Malaysia, Pasoh

26.0

228

10||

2

70

24

238

95

Malaysia, Sabah, Q1700

16.7

168

37||||

3

88

(17)

204

108

Malaysia, Sabah, S0700

23.3

210

45||||

3

62

(21)

254

86

Malaysia, Sabah, S1700

18.3

141

31||||

3

93

(14)

172

110

Malaysia, Sabah, S2700

12.6

148

32||||

3

151

(15)

180

168

Malaysia, Sabah, S3100

9.9

103

23||||

4

262

(10)

126

276

Malaysia, Sabah, U0700

23.0

266

56||||

3

94

(27)

322

124

Malaysia, Sabah, U1700

16.7

114

25||||

4

86

(11)

139

101

Malaysia, Sabah, U2700

12.0

59

14||||

4

84

(6)

72

94

Malaysia, Sabah, U3100

10.1

18

4||||

2

67

(2)

22

70

New Guinea

13.0

149

19

3

600

5

168

609

Puerto Rico, El Verde

23.1

96

35

3

114

(10)

130

126

Puerto Rico, colorado forest

21.1

81

24

4

190‡‡

(8)

105

203

Thailand, Khao Chong

27.2

160

15#

1

75

(16)

175

92

Venezuela, San Eusebio

12.6

167

27

3

329††

11

194

344

Venezuela, T-mf

25.5

179

29§§

2

160

17

208

179

Venezuela, T-LM-mf

15.0

173

38§§

3

253

21

211

277

Venezuela, T-M-wf

10.5

157

35§§

3

257

17

192

277

   Notes: Soil organic carbon (SOC) refers to the top 1.0 m of soil unless otherwise noted. We assumed that biomass and litter components were 48% C, and that soil organic matter was 58% C. For uniformity, data within columns are presented to the same level of certainty: MAT is mean annual temperature.

† Coarse woody debris was not measured; its mass was estimated to be 10% of aboveground biomass (Delaney et al. 1998, this study).

 Total SOC (0–50 cm depth) from Bernhard-Reversat et al. (1978). Total SOC at 50–100 cm depth was determined from a mean soil C content of 0.6% and a soil bulk density of 1.5 g/cm3 (Huttel and Bernhard-Reversat 1975).

§ Total SOC from 0-45 cm soil depth only.

|| Root biomass includes roots <1 cm diameter only.

 Large dipterocarps were removed in the past.

# Root biomass estimated by regression, based on sampling roots of three small trees.

†† Includes humus above the mineral soil.

‡‡ Total SOC in the surface 50 cm only.

§§ Root biomass was estimated from life-zone-mean root:shoot following Sanford and Cuevas (1996). Data represent the means of multiple sites at different locations within the same life zone.

|||| Root biomass was estimated using the allometric equation of Ogawa et al. (1965) (see Khao Chong, Thailand).

References: Brazil, Manaus (Klinge 1976, DeAngelis et al. 1981); ); Costa Rica, La Selva, ultisols (Raich 1983, Sanford et al. 1994, Clark and Clark 2000, Clark et al. 2002, Veldkamp et al. 2003); Ivory Coast (Bernhard-Reversat 1974, Bernhard-Reversat et al. 1978); Jamaica (Tanner 1977, 1980a, 1980b, 1981, 1985); Malaysia, Pasoh (Kato et al. 1978, Yoda 1978, DeAngelis et al. 1981); Malaysia, Sabah, Mt. Kinabalu sedimentary (S), ultrabasic (U) and quaternary (Q) substrates (Kitayama and Aiba 2002a, b); New Guinea (Edwards and Grubb 1977); Puerto Rico, El Verde (Odum 1970, Brown et al. 1983); Puerto Rico, colorado forest (Weaver and Murphy 1990); Thailand, Khao Chong (Ogawa et al. 1965, Yoda 1967, Yoda and Kira 1969); Venezuela, San Eusebio (Steinhardt and Fassbender 1979, Grimm and Fassbender 1981); Venezuela T-mf, T-LM-mf and T-M-wf (Delaney et al. 1997, 1998).



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