Enzymatically hydrolysed protein and carbohydrate pools in deep-sea sediments: estimates of the potentially bioavailable fraction and methodological considerations
A. Dell'Anno et al., Enzymatically hydrolysed protein and carbohydrate pools in deep-sea sediments: estimates of the potentially bioavailable fraction and methodological considerations, MAR ECOL-PR, 196, 2000, pp. 15-23
In this study we developed existing protocols for the enzymatic digestion o
f protein and carbohydrate pools in deep-sea sediments in order to estimate
the organic fraction potentially bioavailable for benthic consumers. Sedim
ent samples were collected in an abyssal locality (Porcupine Abyssal Plain,
4800 m depth) of the NE Atlantic in September 1996, and March and October
1997, and vertically divided into 5 layers down to a depth of 15 cm. Protei
n and carbohydrate concentrations released enzymatically were highest after
2 h of incubation for both organic pools. The release of enzymatically hyd
rolysed proteins from the deep-sea sediments was significantly higher using
Tris+EDTA and sonication instead of a simple sediment homogenisation in Na
-phosphate buffer. Hydrolysed carbohydrate concentrations were higher utili
sing alpha-amylase, beta-glucosidase, Proteinase K and lipase instead of on
ly alpha-amylase and beta-glucosidase. Hydrolysed proteins and carbohydrate
s accounted for a small fraction of the total protein and carbohydrate pool
s (on average 15 and 13%, respectively), indicating that total protein and
carbohydrate concentrations do not represent the actual available fraction
of the sedimentary organic matter in this deep-sea environment. Hydrolysed
protein pools changed significantly between sampling periods whereas carboh
ydrate pools appeared to be more conservative both spatially and temporally
. Hydrolysed protein and carbohydrate concentrations were characterised by
different vertical patterns and carbohydrate concentrations were much highe
r in deeper sediment layers. These results indicate that the 2 classes of o
rganic compounds might play different roles in different sediment layers wi
th important trophodynamic implications for benthic organisms living at dif
ferent sediment depths.