P. Eggleton et al., Termite assemblages, forest disturbance and greenhouse gas fluxes in Sabah, East Malaysia, PHI T ROY B, 354(1391), 1999, pp. 1791-1802
Citations number
45
Categorie Soggetti
Multidisciplinary,"Experimental Biology
Journal title
PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY OF LONDON SERIES B-BIOLOGICAL SCIENCES
A synthesis is presented of sampling work conducted under a UK government-f
unded Darwin Initiative grant undertaken predominantly within the Danum Val
ley Conservation Area (DVCA), Sabah, East Malaysia. The project concerned t
he assemblage structure, gas physiology and landscape gas fluxes of termite
s in pristine and two ages of secondary, dipterocarp forest. The DVCA termi
te fauna is typical of the Sunda region, dominated by Termes-group soil-fee
ders and Nasutitermitinae. Selective logging appears to have relatively lit
tle effect on termite assemblages, although soil-feeding termites may be mo
derately affected by this level of disturbance. Species composition changes
, but to a small extent when considered against the background level of com
positional differences within the Sunda region. Physiologically the assembl
age is very like others that have been studied, although there are some spe
cies that do not fit on the expected body size-metabolic rate curve. As els
ewhere, soil-feeders and soil-wood interface-feeders tend to produce more m
ethane. As with the termite assemblage characteristics, gross gas and energ
y fluxes do not differ significantly between logged and unlogged sites. Alt
hough gross methane fluxes are high, all the soils at DVCA were methane sin
ks, suggesting that methane oxidation by methanotrophic bacteria was a more
important process than methane production by gut archaea. This implies tha
t methane production by termites in South-East Asia is not contributing sig
nificantly to the observed increase in levels of methane production worldwi
de. Biomass density species richness, clade complement and energy flow were
much lower at DVCA than at a directly comparable site in southern Cameroon
. This is probably due to the different biogeographical histories of the ar
eas.