Interaction of the earthworm Diplocardia mississippiensis (Megascolecidae)with microbial and nutrient dynamics in a subtropical Spodosol

Citation
Sl. Lachnicht et Pf. Hendrix, Interaction of the earthworm Diplocardia mississippiensis (Megascolecidae)with microbial and nutrient dynamics in a subtropical Spodosol, SOIL BIOL B, 33(10), 2001, pp. 1411-1417
Citations number
48
Categorie Soggetti
Environment/Ecology
Journal title
SOIL BIOLOGY & BIOCHEMISTRY
ISSN journal
00380717 → ACNP
Volume
33
Issue
10
Year of publication
2001
Pages
1411 - 1417
Database
ISI
SICI code
0038-0717(200108)33:10<1411:IOTEDM>2.0.ZU;2-M
Abstract
Direct and indirect effects of earthworm feeding and activity can alter soi l microbial and nutrient dynamics. Little is known about influence of nativ e North American earthworms on these dynamics. We investigated effects of n ative D. mississippiensis activity on total and soluble C, N and microbial biomass pools in Spodosols from the Apalachicola National Forest in North F lorida, USA. Soil native to D. mississippiensis was collected and reconstru cted by horizon (A, E, B-h) in laboratory chambers and incubated with earth worms at zero, low or high density, respectively 0, three, or six individua ls, for 28-31 days. Total C and N were measured by dry combustion methods. Soluble C and N and microbial biomass were measured in 0.5 K2SO4 extracts f rom non-fumigated and fumigated soil samples. Substrate induced respiration (SIR) was used with inhibitors to measure microbial respiration and shifts in bacterial and fungal components. Earthworm activity mixed soil horizons , largely through burrowing and casting. Total C in A and B-h horizons aver aged 16.7 mg C g(-1) soil and was significantly greater than in the E (2.6 mg C g(-1) soil). Soil N concentration was highest in the A (0.73 mg g(-1) soil) and lowest in the E (0.11 mg N g(-1) soil). N concentration was signi ficantly increased over two fold in the E with high earthworm density. Micr obial biomass C was greatest in the A and E, averaging 8.6 mg g(-1) C, and decreased with earthworm activity. In all horizons, soluble C and N also in creased with earthworm density. Net N mineralization increased significantl y with earthworm density and ranged from -0.22 to 68 mg g(-1) N across all treatments and layers. Changes in proportion of soluble to total soil nutri ents indicated that greater turnover and mineralization Occurred with earth worm activity. SIR indicated earthworm activity induced microbial respirati on in A and E horizons. Earthworm activity stimulated fungal and bacterial respiration, respectively, by 13 and 30% in the A and by 123% and 450% in t he E. Although bacterial respiration was stimulated more than fungal there was no significant shift in B:F ratio, which ranged from 0.80 to 0.99. SIR did not provide evidence of any selective microbial effects of earthworm ac tivity. Direct and indirect effects on nutrient dynamics by earthworms were induced by casting activity and were associated with passage of material t hrough the gut (direct effect) and nutrient and microbial enrichment throug h the mixing of soil horizons (indirect effect). This study established the importance of D. mississippiensis to nutrient availability in its native s oil. (C) 2001 Elsevier Science Ltd. All rights reserved.